^^M -"'^^m. ¥^-^--^i^ )& ? 'J :4^-Vas !i^*ii»t.;*/j.^^ #■ Nb^iM'^-^iii^'"- ■■'' 3l v##v Mh.^ .....:.j^ l«^ THE JOURNAL OF THE ROYAL AGRICULTURAL SOCIETY OF ENGLAND. VOLUME THE THIRD. 1842. PRACTICE WITH SCIENCE. LI^I^ARY LONDON: JOHN MURRAY. ALBEMARLE STREET. MDCCCXLII. These experiments, it is true, are not easy; still they are in the power of every thinking husbakdman. he who accomplishes but one, of however limited application, and takes care to report it faithfully, advances the science, and, consequently, the practice of aoriculture, and acquires thereby a right to the gratitude of his fellows, and of those who come after. to make many such, is beyond the power of most individuals, and cannot be expected. the first care of all societies formed for the improvement of our science should be to prepare the forms of such experiments, and to distribute the execution of these among their members. VoN Thaer, Principles of Agriculture. jondou : Printed "uy V\ illiam Clowes and Sons, Stamford Street. CONTENTS OF VOL. III. I. — On the Improvements which have taken place in West Norfolk. By the Right Hon. Earl Spencer . . i II. — On the Advantage of Testing the Draught of Ploughs. By Henry J. Hannam ...... 9 III. — Account of a Field Thorough-drained, at Drayton, in Staffordshire. By the Right Hon. Sir Robert Peel, Bart,, &c. &c. . . . . . . .18 IV. — On the Connection between Geology and Agriculture in Cornwall, Devon, and West Somerset. By Sir Henry T. De la Beche, Director of the Ordnance Geological Survey . . . . . . . .21 V. — Observations on the Wheat-midge. By the Rev. J. S. Henslow, Professor of Botany in the University of Cambridge ........ 36 VI. — On the Use of the Great or Jersey Trench-Plough, exhi- bited at the Society's Annual Meeting at Liverpool, in July, 1841. By Colonel Le Couteur . . .40 VII. — Observations on the Natural History and Economy of various Insects affecting the Turnip-Crops ; including the Plant-Lice, Maggots of Flies, Caterpillars of Moths, &c. By John Curtis, F.L.S 49 VIII. — On the Comparative Value of different kinds of Fodder. By the Rev. W. L. Rham 78 IX. — On Cottage Economy and Cookery. Compiled by French Burke, from Essays submitted to the Society . . 83 X. — On the Present State of Agricultural Mechanics, and on the Improvement of which the various Implements now in use may be susceptible. By John Morton, jun. Prize Essay . .100 XL— On the " Tchornoi Zem," or Black Earth of the Central Regions of Russia. By Roderick Impey Murchison, F.R.S., President of the Geological Society . . 125 XII. — Lecture on the Application of Science to Agriculture. Delivered before the Society, on Thursday the 9th of December, 1841. By Charles Daubeny, M.D., F.R.S., Professor of Rural Economy in the University of Oxford 136 IV CONTENTS. ARTICLE PAGE XIII. — On the Piof^ress of Agricultural Knowledj^e during the last Four Years. By Ph. Pusey, M.P., F.R. and G.S. 169 XIV. — Account of the Meeting of German Landowners in 1841. By Henry Handley . . ... 217 XV.— On the Marling of a Light Sandy Soil on the Duke of Bedford's Farm at Woburn. By Charles Burness . 233 XVI.— On Claying or Marling Land. By F. W. Overman . 234 XVII.— Early Vetches. By William Jones Williams . . 236 XVIII. — On the Cultivation of Lucerne. By Joshua Rodwell . 238 XIX. — Agriculture of the Netherlands. Part II. By the Rev. W. L. Rham 240 XX. — On the Planting and Management of Forest-Trees, By Charles Falkner 263 XXL— On Wheat. By C. Hillyard, of Thorpelands, near Northampton . . . . . . .297 XXII. — Observations on the Natural History and Economy of various Insects affecting the Turnip Crops, including the White Cabbage-Butterflies, the Turnip-seed Weevil, &c. By John Curtis, F.L.S., Corresponding Member of the Imperial and Royal Georgofili Society of Florence, &c. 306 XXIII.— On the Use of Burnt Clay as a Manure for Heavy Clay Soils. By Francis Pym 323 XXIV.— On the Failure of the Red Clover. By the Rev. W. Thorp ...,,.... 326 XXV.— On Measuring Cattle. By C. Hillyard, of Thorpelands, near Northampton . . . . . . .337 XXVI. — Report on the Exhibition of Implements at the Bristol Meeting in 1842 338 XXVIL — On the Public Institutions for the Advancement of Agri- cultural Science which exist in other Countries, and on the Plans which have been set on foot by In.lividuals with a similar intent in our own. By Charles Daubenv, M.D., F.R.S., Professor of Rural Economy in the Uni- versity of Oxford 364 XXVIII.— On the Dyock Oat. By the Rev. R. W. Fisher . . 387 XXIX. — Report on the Wheats selected for Trial at Cambridge, and on other Wheats. By W. Miles, M.P. . .391 XXX.— Report on Prize Wheats. By G. Kimberley . . 395 XXXL— Report on Prize-Wheats. By H. Handley . . .397 XXXH. — Account of Mr. Irving's New Machine for Constructing Tiles. By W. Ford 398 XXXIII. —Agricultural Tour in Denmark, Sweden, and Russia. By James F. W. Johnston, F.R.S. . . . 400 CONTENTS. V Miscellaneous Communications and Notices : — ARTICLE PAGE I. — Application of Blue Shale to the Surface of Land . .161 II. — Improved Dibbling-Wheel . . . . . .163 III.— On the Application of different Manures as a Substitute for Bones in the Growth of Turnips .... 164 IV. — On the Drainage of Land ...... 165 V. — Account of Experiments on the Growth of Swedes . . 423 VI. — On the Application of Clay to Moor-Land . . . 427 VII.— Simple and Effectual Method of destroying Rats and Mice VIIL- On the Use of Lime .... IX.— On the Feeding of Stock X. — On the Chemical Constituents of Crops XI. — On the Quantity of Minute Ingredients of Soil contained in an Acre of Land XII. — Experiments with Guano XIII. — New and Economical Oil-cake 428 429 430 433 434 437 439 APPENDIX: Council and Officers of the Royal AgricuUural Society of England . i Prizes for the Meeting at Bristol iii General Regulations for Exhibition at the Meeting at Bristol . . vii Prizes and Conditions for Essays and Reports on various Subjects . ix Rules of Competition for Prize Essays for 1843 .... xiii Council and Officers of the Royal Agricultural Society of England . xv Honorary Members ........ xvi Report of the Council to the Anniversary Meeting . . . xvii General Meetings of 1842-3 ....... xxiii Statement of Accounts from July to December, 1841 . . . xxiv Award of Prizes at the Meeting at Bristol ..... xxv Prizes for the Meeting at Derby ...... xxxii Prizes and Conditions for Essays and Reports on various Subjects . xxxvi LIST OF PLATES. Plate L (C) to face page . . . . . . . ,77 IL (D) „ 78 HI. (E) „ 321 IV. (F) „ 322 ERRATA. Part I. [n Mr. Murchison's paper, p. 130, line 21, for " hectares*' read " hectolitres. Parts II.— III. In Mr. Pusey's paper, p. 185, line 10,/or "36«," read "54s." THE JOURNAL OF THE ROYAL AGRICULTURAL SOCIETY OF ENGLAND. VOLUME THE THIRD. 1842. PART L PRACTICE WITH SCIENCE. LONDON: JOHN MURRAY, ALBEMARLE STREET. MDCCCXLII. These experiments, it is true, are not easy; stitx they are in the power of every thinkino husbandman. he who accomplishes but one, of however limited application. and takes care to report it faithfttlly, advances the science, and, consequently, the practice of agriculture, and acquires thereby a right to the gratitude of his fellows, and of those who come after. to make many such, is beyond the power of most individuals, and cannot be expected. the first c4re of all societies formed for the improvement of our science should be to prepare the forms of such experiments, and to distribute the execution of these among their members. VoN Thaer, Principles of ^Agriculture. CONTENTS OF PART I., VOL. III. I. — On the Improvements which have taken place in West Norfolk. By the Right Hon. Earl Spencer . . l II.— On the Advantage of Testing the Draught of Ploughs. By Henry J. Hannam ...... 9 III. — Account of a Field Thorough-drained, at Drayton, in Staffordshire. By the Right Hon. Sir Robert Peel, Bart., &c. &c 18 IV. — On the Connection between Geology and Agriculture in Cornwall, Devon, and West Somerset. By Sir Henry T. De la Beche, Director of the Ordnance Geological Survey . . . . . , . .21 V. — Observations on the Wheat-midge. By the Rev. J. S. Henslow, Professor of Botany in the University of Cambridge ........ 36 VI.— On the Use of the Great or Jersey Trench- Plough, exhi- bited at the Society's Annual Meeting at Liverpool, in July, 1841. By Colonel Le Couteur ... 40 VII.— Observations on the Natural History and Economy of various Insects affecting the Turnip-Crops; including the Plant-Lice, Maggots of Flies, Caterpillars of Moths, &c. By John Curtis, F.L.S. ... 49 VIIL— On the Comparative Value of different kinds of Fodder. By the Rev. W. L. Rham 78 IX. — On Cottage Economy and Cookery. Compiled by French Burke, from Essays submitted to the Society . 83 X.— On the Present State of Agricultural Mechanics, and on the Improvement of which the various Implements now in use may be susceptible. By John Morton, Jun. Prize Essay . . . . .100 XL— On the " Tchornoi Zem," or Black Earth of the Central Regions of Russia. By Roderick Impey Murchison, F.R.S., President of the Geological Society . . 125 XII.— Lecture on the Application of Science to Agriculture. Delivered before the Society, on Thursday the 9th of December, 1841. By Charles Daubeny, M.D., F.R.S., Professor of Rural Economy in the University of Oxford 136 iv CONTENTS. Council and Officers of the Koyal Agricultural Society of England Prizes for the Meeting at Bristol ..... General Regulations for Exhibition at the Meeting at Bristol . Prizes and Conditions for Essays and Reports on Various Subjects Rules of Competition for Prize Essays for 1843 PAGE Miscellaneous Communications and Notices:— I. — Application of Blue Shale to the Surface of Land . . 161 II. -Improved Dibbling-Wheel 163 III. — On the Application of different Manures as a Substitute for Bones in the Growth of Turnips . . . .164 IV. — On the Drainage of Land ...... 165 APPENDIX: ui vii ix xiii JOURNAL ROYAL AGRICULTURAL SOCIETY OF ENGLAND. I. — On the Improvements which have take?i place in West Norfolk. By the Right Hon. Earl Spencer. Every one connected with agriculture in this country^ and pro- bably in Europe and America, has heard of the improvements in the agriculture of West Norfolk, brought about by the exertions, liberality, and example of the Earl of Leicester. It is known that it is his boast, as it well may be, that he has converted West Norfolk from a rye-growing to a wheat-growing district. That this statement is well-founded, is proved by the fact that the small ports of Blakeney, Cley, Wells, Burnham, and Brancaster, which, when Lord Leicester came into possession of his estate, and for many years afterwards, constantly imported a large quantity of wheat, have become exporting ports, and that now for many years a great deal more wheat has been exported from them than has been imported into them, and this has occurred notwithstanding the great increase of population which has taken place, and con- sequently the great increase in the consumption of wheat which must have occurred in the district, which those ports used for- merly to supply. These are striking facts : they cannot be denied, nor can they be accounted for in any way but by the improvement in the culti- vation of the soil M^hich has taken place. They are not only in- teresting to those who are practically engaged in agricultural pursuits, but they are also interesting to the philosopher, because they prove, that, although the general principle must be admitted to be true, that population will press upon the means of subsist- ence, yet to a certain point at least the skill and industry of man may counteract this tendency, and supply a greatly increased population, not only with the same, but with a much better de- scription of food from the same district. VOL. III. B 2 On the Tmprovemenl.s in West Norfolk. It has appeared to me, that it would be interesting^ to our Society, not only to state these results, but to endeavour to point out the means by which they have been produced ; and with this view I have made the best inquiries I could from Lord Leicester, the only person now living who is able to recollect the former state of this district, and to tell the means by which it has been improved into its present flourishing condition. Lord Leicester came into possession of his estate in the year 1776. At this time the whole district round Holkham was unenclosed, and the cultivation was of the most miserable cha- racter ; the course of cropping, as long as the land would produce anything, was three white crops in succession, and then broad- cast turnips ; no manure was purchased, and very little, and that of no value, was produced on the farm. The sheep were of the old Norfolk breed, and, with the exception of a few milch cows, there were no cattle kept upon any of the farms. It happened that the lease of a large part of the land, which now forms Holkham Park, was within two years of its expiration. In the lease previous to the one then current, this land had been let at 1^. 6c?. an acre ; in the then current lease it had been raised to 3s. ; Lord Leicester offered to the tenant to renew it at bs., but Mr. Brett, the tenant, who deserves to have his name re- corded for the great good he unintentionally did to the country, refused to give so much for the land, upon which Lord Leicester determined to take it into his own hands. Thus the real origin of the great improvement of this district was, that Mr. Brett re- fused to give 5.S. an acre for land, which now, under an improved system of cultivation, usually produces nearly four quarters of wheat per acre. For nothing would have been much more im- probable than that Lord Leicester, then an extremely young man, fond of and excelling in field-sports, with a princely fortune, should have applied himself to the detailed management of a farm, had he not been compelled to take this tract of land into his own hands by the refusal of Mr. Brett to accept the terms which were offered to him. But having taken it, he found, as every man who will apply himself to agriculture will, the high interest of the pursuit, his taste was formed, the habits of his life accommodated themselves to it, and applying the whole energy of his mind to the collection and dissemination of all the knowledge which he could derive from practical and scientific farmers, he has effected the great improvements which, while they have been a source of continued happiness to himself, have produced the most incalculable benefits to the country. If, on the other hand, Mr. Brett had accepted the terms offered to him. Lord T^eicester would have granted him a lease for twenty-one years, and for that long period of time, and probably much longer, no improvement On the Improvements in West Norfolk. 3 would have taken place ; West Norfolk would still have been considered a district in which wheat could not be grown, and, what would have been a still greater misfortune, Lord Leicester might never have turned his attention to agricultural pursuits. The lease having thus expired in 1778, Lord Leicester com- menced farming. He was, however, necessarily ignorant of any of the knowledge necessary to conduct the management of a farm. But he took the only means which could give him the information he required ; he began at once to collect around him practical men, and invited to his house annually a party of farmers, at first only from the neighbouring districts ; at these meetings agricul- tural topics were discussed. Lord Leicester's farm was examined, and his management of it either criticised or approved, and by thus receiving information, and again communicating it to others, not only did Lord Leicester himself arrive at the knowledge of agricultural management, but the practical men who attended these meetings left them better informed than when they came. In the course of time, friends of Lord Leicester came from a dis- tance to attend them, and thus ultimately this small beginning expanded into the far-famed Holkham sheep -shearing. As one of the first consequences of these discussions, he adopted a somewhat improved course of cropping ; instead of growing three white crops in succession, he only grew two, and kept the land in pasture for two years in every course. This change ap- pears gradually to have improved the land, and I find from the old accounts of the farm that wheat was first sown upon it in 1 787. This improved course of cropping, though quite essential, was not of itself sufficient to enable him to grow wheat. The land, naturally very weak, was still more impoverished by the exhausting treatment it had received. In order to get it into better condition, it was absolutely necessary greatly to increase the number oi live stock which had hitherto been kept upon it ; but the production of food for them was so small, that it was impossible at first to adopt this mode of improvement to any great degree. The first thing to be done was the purchase of manure. Lord Leicester was induced to try rape- cake as a top dressing, and it answered admirably. Another much more effective source of fertility was adopted, and to a much greater degree than it hitherto had been. The surface-soil of the whole district is a very light sand, but nearly throughout it there is a stratum of rich marl at various depths underneath. Pits were opened, and the marl dug out and laid upon the surface. This not only increased its fertility, but gave to the soil the solidity which is essential to the growth of wheat. By these means clover and other artificial grasses were raised, and the power of keeping more live stock was obtained. As has been said, the only live stock then kept were the B 2 4 On the Improvements in West Norfolk. Norfolk sheep, there were no cattle. Lord Leicester made no change in the sort of sheep, and adopted Mr. Bakewell's Leicester breed of long-horned cattle. This, indeed, was the only breed of cattle to the improvement of which at that time any attention had been paid, and a young man applying himself to improved agri- culture would naturally have been led to select them. When, some time afterwards, he found that the Norfolk sheep were a very unprofitable sort, the same reasons induced him to try the new Leicester breed, a variety of sheep probably as ill calculated to succeed on such a soil as the one he occupied as any breed which he could have selected. He at last found that the best sort of sheep he could adopt were the South-downs. In this, however, as in every other of his farming experiments, Lord Leicester acted with great caution, and did not make the changes which he did make till thoroughly convinced by practical expe- rience that they v/ould answer. Accordingly, for several years he had upon his farm at the same time Norfolk sheep, new Leicesters, and South- downs: he also tried the Merinos, but he did not persevere long with them. I find that so late as the sheep-shearing of 1812 there were still at Holkham both Norfolk and Leicester sheep. Since that time South-downs have been the only sort which he has kept. With respect to cattle he persevered with the Leicester long- horned breed for many years ; but somewhere towards the close of the last century, Francis Duke of Bedford, with whom he lived on terms of the greatest intimacy, being aware that he was inclined to try the Devonshire cattle, in consequence of the success of a small experiment which he had made in feeding some Devonshire oxen bought from Lord Somervilie, bought at the late Lord Ossory's sale a Devonshire bull and some heifers without having had any commission from Lord Leicester, and sent them to Holkham. Upon trial this breed proved to be by far the best breed that could be adopted in such a soil as that of Holkham. Lord Leicester, therefore, gradually replaced the long-horned by increasing his stock of Devonshire cows, but, as in the case of the sheep, some of the long -horned cattle were still to be seen at Holkham as late as 181 '2 : from that time the only catde which he has bred have been Devons, and the only sheep South-downs. These latter, however, he has of late years crossed with the Hampshire Down sheep, and he considers that this cross has been very successful, by givdng greater strength to the constitution of the sheep, by increasing the value of the wool, and by giving a larger proportion of lean meat in the carcasses. It is not, however, to cattle and sheep only that Lord Leicester has turned his attention : a large portion of the manure produced upon his farm is owing to the number of pigs which he kept. On the Improvements in West Norfolk. 5 The Suffolk breed of pigs has always been one of the most valu- able in the kingdom, but Lord Leicester has found that, by cross- ing them with the Neapolitan breed, a much more profitable sort is produced. The pure Neapolitan pigs, though their meat is superior to that of any English pig, are such bad breeders, that they are not advantageous to a farmer, but when crossed with the Suffolk their constitution and breeding qualities are greatly im- proved, and the cross-breed continues to possess the extraordinary aptitude to feed of the Neapolitan without the weakness of their constitution. Llaving thus, by keeping animals of a thrifty and profitable sort, increased greatly the number of his live stock, and by the purchase of rape-cake and the application of marl, in addition to the increased quantity of manure which his live stock produced, improved the fertility of the land, he overcame the difficulty of growing wheat, and he adopted the present Norfolk course of husbandry. The farm at Holkham assumed the appearance of fertility which it has since ever held, and attracted the attention of every one at all interested in the improvement of agriculture. The stock upon this farm, and still more the annual exhibitions of the sheep-shearing proved the great superiority of the South- down over the Norfolk breed of sheep, the latter were abandoned rapidly by the neighbouring farmers, and now in the whole tract of country between Lynn and Llolkham such an animal as a Norfolk sheep is not to be seen. The Norfolks have been entirely superseded by the South-downs. Of late years indeed it has JDecomxC very much the custom both with the farmers gene- rally and also with Lord Leicester himself to put a portion of their South-down ewes to a long-wooUed ram, the produce from this cross having proved extremely profitable, but still in all cases the store flock continues to be of the South-down breed. With re- spect to cattle the example of Lord Leicester has not been sg universally followed. The polled Suffolk or Norfolk breed still hold their ground. But though his example in keeping a breed- ing herd of Devon cattle has been followed only to a limited extent, yet the more important object of carrying a large quantity of stock upon their farms is universally attended to by the Norfolk farmers. The nature of the soil and the scarcity of old pasture is such, that no improvement can be made in cattle by summer-grazing, but all the farm-yards are well stocked during the winter. By this system a large quantity of valuable manure is produced, and the occupiers of this light and weak soil are enabled to cultivate it to advantage. A very small proportion, however, of this stock is bred in Norfolk. There is scarcely any situation where it would be advantageous to a farmer to breed all the cattle which he fattens, although 1 6 On the Improvements in IVest Norfolk. am confident, from practical experience, that it would be advan- tageous in the best grazing districts to breed a considerably larger proportion than is now done. But in Norfolk, if any large pro- portion was bred, much of the advantage of carrying a numerous herd of cattle during the winter would be lost. It is perfectly well known that the more nutritious the food is on which cattle are fed, the better is the manure produced : it is therefore of great importance that the number of cattle preparing for the market should bear a large proportion to that of those kept in a store and growing state. It is, therefore, in a soil like that of Norfolk of peculiar importance that much the greater number of the cattle on the farm should only remain on it while they are feed- ing on the most nutritious food. No difficulty is found in effect- ing this object; for this district^ on which at the commencement of Lord Leicester's career scarcely a head of cattle could be found, has now become the centre of attraction for drovers from every part of the United Kingdom. Devonshire, Scotch, Lincoln- shire, and I believe even Irish cattle crowd the fairs throughout the county of Norfolk, and most certainly Norfolk now supplies more than its full share of the beef consumed in the metropolis. This is the present improved state at which Norfolk has arrived ; but in order to trace some of the other main causes of this im- provement, it is necessary to go back to the latter end of the last century. When Lord Leicester had proved by his ov*ai practice that wheat might be profitably grown, he endeavoured to persuade the neighbouring farmers to follow his example, but it was nine years before any of them did so: at last the late Mr. Overman, whose skill and ability are well known, made the attempt with perfect success, and from that time the old system fell into disrepute, and the present Norfolk agriculture gradually replaced it. But any attempt to grow wheat would have been an entire failure as long as the farmers persevered in growing three crops of white grain in succession. The land had been usually let on leases of twenty-one years, the occupying tenantry consequently had full security that they themselves would reap the benefit to be derived from any outlay of capital which they made, or any improvement in agriculture which they introduced ; but they were so ignorant of their true interests, that they would not forego the apparent immediate profit of growing corn as long as the land would produce it, although it is perfectly clear that, taking the whole period of their leases into consideration, they were enor- mous losers by pursuing this course. The leases contained no covenants, and the tenants were at perfect liberty to cultivate their land in any way they thought proper. Lord Leicester, however, having proved by his own experience, and having also On the In?2?roveme7its in TVest Norfolk. 7 been convinced by the information which he had received from the best practical farmers with whom he was in communication, that a better course of cropphig would be greatly to the benefit of the occupying" tenant, while it would permanently improve the value of his estate, determined to introduce covenants as to the mode of cultivation into all the leases which he granted. Al- though in the first instance the covenant only prevented the tenant from growing more than two crops of white grain in succession, yet so great was the ignorance of the farmers, that he met with great difficulty in enforcing even this very modified improvement of the old system. At last, however, he succeeded. The effect even of this altera- tion was such, that it proved how disadvantageous to all parties the old system had been ; and upon the late Mr. Overman taking a farm of Lord Leicester, he was allowed to draw the covenants of the lease himself. He then inserted the modern improved course of cropping well known as that best adapted to light turnip lands. This lease has been the model on which Lord Leicester's leases have since been drawn, making of course any changes which the peculiar nature of each farm may require. The tenants make no difficulty now about agreeing to adopt the covenants inserted in their leases. The able and skilful farmers whom Lord Leicester has been enabled to collect around him know full well that the course of husbandry enforced by the covenants in their leases, while it is the most advantageous for the improvement of the property of their landlord, is the most profitable for themselves. I have thus, in an imperfect and superficial manner, stated the course of the improvements which have taken place in West Norfolk. The results are, as I stated in the beginning of this Paper, most interesting and important ; the means by which they were brought about very simple and plain, and at first sight appa- rently inadequate to have produced such effects. As the first of these means, I would put the circumstance of a man in Lord Leicester's station applying himself practically to agriculture, and giving an example by his own practice of what might be effected by the skil- ful application of resources within the reach of all farmers of ordinary capital. But this example would have had but small effect had it not been for the periodical assemblage of men of in- telligence, of practical experience, and of enlightened views, to compare the results of their various systems, to discuss their respective merits, and to criticise their respective defects. This assemblage took place at the Holkham sheep-shearing : Lord Leicester was there ready to try any experiments the probable result of which was likely to be advantageous ; he was ready to listen to any suggestions, and to report upon the results at some 8 On the Imj^rovemenh in West Norfolk. subsequent meeting. This liberality, not only in the prizes he offered, but in the magnificent hospitaHty of these meetings, con- gregated men from all parts of the civilised world. None but agricultural subjects were discussed : on these the most conflict- ing opinions were freely given, and as freely canvassed, but every- thing political was excluded; and thus, although the political opinions of Lord Leicester and of most of his personal friends were not only very decided, but for a great period, and that the most brilliant era of the Holkham meetings, unpopular with the great majority of those connected with the landed interest, yet men of every shade of political opinion were heartily welcome, and confident that, although they might hear some favourite theory of farming ridiculed, they never would find anything hurt- ful to their political feelings advanced. The sheep-shearing of 1822, indeed, was an exception; political topics were then intro- duced — it was a bad omen. This sheep-shearing was the last. By means of these discussions the correct theory of agriculture was improved and made known : by theory I mean, Avhat it always should mean, the combination of the results of the best practice in various circumstances; not the fanciful schemes of clever but unpractised projectors, well informed perhaps on other subjects, but deriving the data from which they deduce their plans from the speculations of their own minds, and not from the results of practical experiments. But though the theory was thus made known, its practical effect would have been little upon the improvement of West Norfolk had it not been proved to be right by the experience of men engaged in the cultivation of the dis- trict itself. This was effected by the well-considered covenants introduced by Lord Leicester into his leases. Long leases are advantageous if properly regulated ; they give the tenant a security, which he cannot otherwise obtain, that he will reap the benefit of any out- lay of capital which he may make upon his farm : but long leases existed in West Norfolk w^hen its agriculture was in the wretched state which I have described. A prejudiced or an ignorant oc- cupier will gain nothing by having a lease ; and an unprincipled one, though sufficiently skilful, may leave his land so deteriorated in value, by an exhausting system, at the end of his lease, that it will be without value to his landlord, and unproductive of any benefit to the country, for years after the lease has expired. For this reason it is that the combination of judicious covenants with his long leases has enabled Lord Leicester to effect such great huprovement not only on his own estate, but, by the example thus set, to the whole district in which he resides. Covenants, skilfully drawn, while they secure the landlord, do not interfere with the husbandry of a good farmer, and are On the Improvements in West Norfolk. 9 not at all detrimental to hinij but thej are advantageous to a bad one. When we look at the results to which I am calling the attention of our Society, what an example do they hold out to all men of landed property, but more especially to young men ! We see what one man's exertions can do — we see by beginning in early life to apply himself to agricultural pursuits what immense improvement Lord Leicester has lived to see effected in his estate — what benefit he has conferred upon his country, and what an interesting pursuit he has secured to himself. This he has done without debarring himself at all from the more exciting pursuits of an English country gentleman : during a great part of this pe- riod, while he was effecting this great good, he kept a pack of fox-hounds; during the whole of it he has been distinguished for his success as a sportsman in shooting. He was undoubtedly the original and greatest cause of these beneficial results ; his energy, his perseverance, and his liberality were the great moving powers by which the improvements were pressed forward : but one of the means, and that one of the most important, which enabled him to effect what he wished, was the annual sheep-shearing. It is satisfactory to feel that our Society, having the same object of improving the agriculture of the country in view., has adopted the same means, by our annual country meetings, of effecting it. Our power of collecting and disseminating information must be vastly greater than that of any individual ; and, seeing the successful results which I have de- scribed, I hope and trust we may look forward to producing effects in the highest degree beneficial to the, country. IL — On the Advantage of Testing the Draught of Ploughs. By Henry J. Hannam. To Ph. Pusey, Esq., M.P. Dear Sir, — You and Mr. Handley have fully made known to the Society the use and value of the dynamometer in the draught of ploughs, and have furnished valuable data for the future guidance of the agricultural community. What chiefly remains to be done is to apply similar experiments to individual cases, that each farmer may make himself acquainted with the degree of power required to work his implements ; and whether others are to be found that will work with less strength, and equally answer his purpose. Your '' Inquiry on Draught in Ploughing," in vol. i. part iii.. 10 On the Draught of Ploughs. has shown us that great differences do exist in ph)iighs, and proves that a great portion of tlie kingdom are, in the important operation of ploughing, needlessly expending a large amount of labour. A spirit of improvement has existed for some years, and the exertions of plough- makers in many parts of the country have furnished the farmers with implements greatly improved in draught, working powers, and economy in wear. The principal object that now claims the zealous and diligent pursuit of both parties, is lightness of draught, for the important purpose of econo- mizing horse-labour. As a first step to this desirable attainment^ no better course, I think, can be pursued than endeavouring to ascertain in every district, by means of the dynamometer or draught-gauge, the lightest plough suited to soil and circumstances, and improving that to the greatest degree. No agricultural association or farmers' club should be without one of these instru- ments. Neighbours should subscribe to possess one in common ; and a farmer or country resident will do a kindness to his friends and neighbours by inviting them with their ploughs to a trial of their respective merits in draught as well as in other properties. It was a desire to satisfy my neighbours and myself of the great disparity in point of draught existing among the various ploughs used in this district, that led to the experiment of which you have requested me to send you the result; and with this I will com- bine others that I have made on my farm both before and since, and also one in Kent connected with a meeting of the Isle of Thanet Association. I shall be glad if others be induced to make and register simi- lar and more complete trials in their own neighbourhoods. The drauo-ht-o^auofe, to a certain extent, is as essential to the farmer as common weights and measures. To work an unne- cessarily heavy-drawing plough is like selling corn by a larger bushel than the standard. So many stones' draught gained in ploughing a given piece of ground are in fact a saving of so much hay and corn. In short, to pass over intermediate calculations, a stone marked on the face of the dynanometer should be considered to represent so many pounds, shillings, or pence. It might not be difficult to give an idea of what one of these stones in draught is worth in horse-keep ; and if I have time before closing this paper, I will enter into the calculation ; of course considering, along with mere draught, the relative cost also of time and speed. About fifteen years ago, in accordance with a movement which pretty generally took place in this part of Oxon and Berks, I re- linquished the old wooden plough, and adopted the lightest plough then manufactured by Messrs. Perry and Barrett of Reading, and was able to work it with a pair of horses. I have On the Draiicjlit of Ploughs. 11 never since used any other, till last summer, when they sent me a plough of a new make, which they considered of lighter draught. I could never perceive that I should be a gainer by exchanging this Reading L 2, which I had used so long, (a one-wheel plough with cast-iron body and wooden beam and handles,) for any other I saw at work : its performance, I thought, was seldom exceeded, and my men had little difficulty in miaintaining a more than re- spectable position at the ploughing-matches ; and no other I could so readily work with a pair of horses. I had rather a fancy for the Scotch plough, admiring on a neighbouring farm its apparent facility in cleaving and turning off the furrow ; but I always thought I had an advantage in the wheel, which secured me a regular depth, and an even-shaped furrow : however, I did not perceive that this wheel really gave my horses an easier draught. I found this L 2 at home in every species of work. In drilling turnips it laid a neater and more level ridge (27-inch) than my neighbour's Scotch plough. It was also applicable as a one-horse implement, and I used it extensively in ploughing be- tween ridges, stirring fallows, for the barley-seed furrow, &c., and latterly in forming turnip ridges, instead of the double ridging plough. Nevertheless, in many respects there was room in it for improvement. Previously to the Liverpool meeting, Messrs. Barrett and Exall sent me their new plough marked D P, to compare in draught with their L 2. I made several trials with them both, and on every occasion found the draught of D P full 2 stones the lighter. Experiment I. — At this time (early in last July) I collected a few of my neighbours' ploughs. First came the now old-fashioned wooden one-wheel plough, which I relinquished some years ago, and which has now ceased to appear upon almost all the consider- able farms except the most clayey. It is still occasionally used by my next neighbour. To the village carpenter and blacksmith, with its friction parts of wood and its wrought- iron share, it has been a profitable implement ; but neither in draught, as will be seen, any more than in repairs, can it have been very economical to the farmer. The Watlington plough followed, which, within a considerable circuit of the place in Oxfordshire from which it takes its name, has superseded the above wooden plough, and which is formed, like almost all the improved ploughs in the south of England, with cast-iron body and share attached to a wooden beam and handles. This has nothing very promising in its appearance, though it is a favourite in its district. Lastly came four varieties of Messrs. Barrett's ploughs, which are much used in these and the adjoining counties. Of these were the L 2 and the new make D P, and two, a single and a double-wheel, both marked No. 8, but not havino- their own mould-boards, as I have 12 On the Draught nf P/oifijhs. since discovered. I have, however, to include a double plough of Messrs. Barrett's that was on its way to Liverpool, and may be described as a double D P. The whole were tried on a lio^ht j^ravelly loam, moist from recent showers, from which a crop of Trifolium incarnatum had been mowed. One horse only, for reasons which I will explam when I come to the question of single-horse ploughing, was attached to each, except the double plough ; and the following statement is the result, in a furrow 8, in. wide by 5 in. deep : — Drawn by One Horse. Stones. 1. Old Oxfordshire, one wheel . . « . . 20 2. New ditto, Watlington . . i • • .18 3. Barrett's No. 8 two-wheel, with Ransome's mould-board 132 with ground-wrest . . . • . 17J 4. Barrett's No. 8 one-wheel, with Brightwell mould-board and ground-wrest . . . . ■. .16 5. Barrett's L 2, one-wheel ..... 14 6. Barrett's new plough D P, one wheel . . .11 Drawn by a Pair, 7. DP 12 8. Barrett's new double plough . . . . .24 Thus it will be seen that by my original transition from the wooden plough at 20 stones to the L 2 at 14, I gained 6 stones, equal nearly to 1 horse in 3 ; and thus showing that my two-horse teams had been working no harder than my three horses had originally. Next to this conviction, this experiment proved to me that I had made a valuable discovery — a still lighter plough — lighter than L 2, I had been so long using. I first had the satis- faction of confirming that I had for some years been undoubtedly saving 30 per cent, in ploughing, and now discover that I may again make a considerable saving by abandoning the L 2, and henceforth adopting the D P ; and of course 1 determined on so doing, should I on trial find the latter equal in other qualities to the former. I have so tried it, and have found it in general work a superior plough ; and I am only waiting some further improvements Messrs. Barrett have undertaken in it, to restock myself entirely with it. But I do not hesitate to say that, if I should have the good fortune to meet with a lighter in draught (sufficiently light to amount to a saving, and with qualities equal), this also must share the fate of its two predecessors. It may be worth while to consider what number of stones gained in draught would justify us in abandoning an old plough. If the power of one horse be put at 10 stones, one stone saved in pair-horse ploughing will be 5 per cent, on each horse. And this 5 per cent. I should consider myself at liberty to set down On the Draught of Ploi/ghs. 13 as a saving to that amount in horse-keep. Where the ploughing can be brought within tlie power of one horse this saving is doubled ; and in four-horse work the proportion of course is reduced to 2^ per cent. This will serve to give some idea of the saving effected by any amount of gain in the draught of ploughs ; but as I must proceed with my observations on our experiment, I will reserve calculations to a future time. The intermediate draughts (2, o, and 4 in the table) will speak for themselves. I will only express my strong doubts of the actual advantage derived from any shapes tliat cause such an excess of draught. This excess is occasioned in a considerable degree, as I imagine, by the full breast, which presents a greater resistance; and it is used because in adhesive soils in a certain state they accumulate the mould upon them in a less degree. It is yet to be decided whether this advantage is not obtained at too great a sacrifice of horse-strength. 1 tried D P again with a pair of horses for the purpose both of comparing it with the double plough, and seeing what the addition of the double whipper-tackle would have upon the draught ; and I found this latter caused an increase of a sttme— and thus much of saving in favour of one horse in a plough. There could not be a more conclusive trial of the respective draughts of double and single ploughs than was made in the above experiment. Messrs. Barrett's very complete double plough is simply two D P's combined, the mould-boards, &c. being the same casting. The very equal result shows in the first place its careful construction ; and the uniform working of both ploughs, whether single or combined, which was exhibited in other trials as well as the above, was a satisfactory proof of the correctness of the trials and of the soundness of the method of test. And again, this uniform result, namely, that the draught of the double was found almost always twice that of the single, supplies data on which to found a correct estimate of the merits and value of a double plough. The result of this and other little trials left no doubt which was the fitter plough for competition at the Annual Meeting at Liverpool. D P was there entered for trial as a one-horse plough, and, by the prize it obtained, was adjudged to be the lightest in draught of all the ploughs there brought forward. During the winter it was constantly at v/ork with L 2 ; and when I occasionally tested it with the draught-gauge, I always found it, as I had done before, more than 2 stones lighter. And on one occasion, when they were ploughing a good gravelly loam to the depth of 7 inches, I found L 2 working at a draught of 22^, and D P at 18 stones. Experiment II. — The trial you heard of and requested for the 14 On the Draught of Ploughs. Journal arose from a neighbour begging to have his wooden pk)ugh, of which he had a very good opinion, compared with my D P ; when I took tlie opportunity of collecting a few more, and inviting my neighbours to the inspection ; and with their assist- ance I was enabled to bring forward in this experiment a few of the ploughs that have engaged the attention of the Society : for example — Ransome's N L 7, the hghtest in Mr. Handley's ex- periments, and a prize-plough at Liverpool ; Hart's improved Berkshire; the Scotch iron swing-plough; Barrett's D P, before described, and the old Oxfordshire — which, like the old Berks, and the original plough in many districts, forms a useful addition to an experiment to show the advance new ploughs have made. But I will describe the whole in the order in which they took up a position by the draught gauge. They consisted of : — 1. The before- mentioned wooden plough from Cuddesdeu, which proved to be the old one-wheel of the county. 2. The old Burcott plough, which was tried in a former experiment. Both these were exactly of the same description, entirely of wood, and are of the same family as the Berkshire. 3. An iron Scotch (Roxburghshire) plough from the late Mr. Jona- than Peel's farm near Abingdon. 4. Barrett's No. 8 two-wheel on gallows, having on a Ransome mould- board marked 132, with a ground-wrest attached, and of general propor- tions stout enough for any work. 5. Barrett's No. 8 one-W'heel, fitted with a Brightwell (village in the neighboiu'hood) mould-board, with ground-wrest — a plough somewhat like, but much stouter than my L 2. 6. A Watlington one-wheel plough, which I have before described, and which has very strongly the common characteristics of tlie improved ploughs of these counties— a full-breasted mould-board, and a detached under mould-board called a ground-wrest, wliich sweeps out the furrow and forms a support for the plough at the heel. 7. Hart's one-wheel. I had rny doubts whether this was precisely the plough described in your "Inquiry" in vol. i. part iii. of the Journal, fancying it was a larger size, and adapted for heavy work, but I have since ascertained it to be the same. 8. Ransome N L 7, called in your paper the Rutland, and know^n as the lightest in Mr. Handley's experiments, and which is an excellent plough I should imagine in every kind of soil. Its heavy proportions and appearance are counteracted by its perfectly-formed mould- board, which enables it, where the soil is not in too adhesive a state, to take up a position among the lightest ploughs. 9. Barretfs J^ 2. 10. Barrett's D P, which is formed, as are all the others (except the Scotch and the old Oxon), of a cast-iron body and wooden beam and handles, and which possesses a whole mould-board, while the rest, with the exception of N L 7 and the Scotch, had a ground-wrest attached. On the Draught of Ploughs. 15 11. A Warwickshire iron double plough, well constructed, but of great weight. I have taken the liberty of putting down Barrett's double plough, though not present ; and of stating it at double the draught of D P, which I am confident, from the experience I have had with it, would have been as nearly as possible tiie number of stones it would have exhibited had it been tried on the present occasion. These single ploughs were all tried on the 3rd of March on a wheat stubble, in a gravelly sandy loam, after a good deal of wet; and the results following were noted down by those present. The furrow was kept at 9 inches wide and 5 inches deep : — Stones. 1. Cuddesden, Oxon, old one-wheel . . .22 2. Burcott, do. do. . . . .22 3. Scotch swing-plough . . . .20 4. Barrett's No. 8 two- wheel, with Ransome mould-board 20 5. Barrett's No. 8 one-wheel, with Biightwell mould-board 19 6. Watlington, Oxon, one-wheel . . .18 7. Hart's one-wheel . . . . .1*7 8. Ransome's N L 7, two low wdieels . . .16 9. Barrett's L 2, one-wheel . . . .15 10. Barrett's D P, one-wheel . . . * 13 Double ploughs. Warwickshire double plough, iron . . .38 Barrett's double plough, wooden beams . . 26 There is nothing particularly new in this experiment : it is similar in many respects to the one I have detailed before, and it resembles one or two of the trials you have* already recorded in the Journal. Its value consists chiefly in confirming the results previously arrived at, and going some way I trust in establishing them. 1. It is premised, as placed beyond a doubt, that the draught- gauge, properly constructed, is an unerring test of the amount of draught required by an implement, and of work performed by an animal or other moving power, and as such is useful as a practi- cal guide to every farmer. 2. It is made clear that the vague principles of village plough- making must give way to the better defined and more economical system of more instructed practitioners. 3. It is shown that the wheel has a decided advantage over the swing plough, and that this must necessarily be the case, on plain mechanical principles, I will show in another place. The supe- rior science of the Scotch plough, displayed particularly in its mould-board, is from this defect obliged to yield to less perfect implements. 4. That a great majority of the improved wheel- ploughs have hitherto been constructed so little with a view to lightness of * Trial iii. p. 228, vol. i. Part iii. Journal. 16 On the Draught of Ploughs. draught that a large portion of the cost of ploughing is needlessly wasted. My friend with the old wooden plough could not but come to the conclusion that he had been ploughing at a great unnecessary expenditure, and declared that I should be the cause of putting him to the farther expense of a new plough, and that the lightest in draught. Ransome's N L 7 exhibited here the same draujjht that it did in similar soil and circumstances in your trirds. What surprised me was the position which Hart's plough assumed ; and it was to satisfy myself that I had been making a trial of the correct im- plement, that I requested the loan of your plough ; and for greater satisfaction 1 sent it over to Mr. Chillingworth of Cuddesden, from whom I had the one I made this experiment with, to be compared and tested with his. The result which he and Mr. Gale returned to me perfectly verified our previous trial. Yours and two other Hart's, in Mr. Chillingworth's possession, in a sandy loam furrow 9x5, all agreed on the draught-gauge, i.e., were each 17 stones, at the same moment that D P, which I also sent over, exhibited 13 stones, being exactly the places both were found in at the trial on the 3rd of March. The Scotch, which was I believe in this instance of an excellent make, was held by its own, a superior ploughman. To the swing principle, and in some degree to its weight of iron, we must, I think, attribute that inferior position with regard to draught, w hich till of late it has not been suspected to hold. Barrett's D P justified the favourable judgment it had received, and corresponded with my previous experience of it. The ploughs 4, 5, and 6 serve to show the drain on farmers' resources that extensively exists by the use of imple- ments of unnecessary draught. Comparative Experiments during Barley-sowing. — I have taken the opportunity afforded by the loan of your plough to carry on a few trinls w^ith it during my tillage for barley along with three others, Barrett's L 2 and D P, and Ransome's N L 7, which my neighbour Mr. Davey allowed me to retain. The soil these four ploughs have been tried in is a fair gravelly loam that generally works well, but is rather sticky when wet, and sets hard when dry. The first trial (April 2nd) occurred while the seed-furrow was given to a well -pulverised surface on w hich the barley had been cast. The next trial (April 3rd) was during the breaking up of some turnip ground after sheep, which had been more or less trodden in a wet state ; and the surface had become dry and scrubbed, but w^as moist enough beneath. The spots trodden in the rain, and those sVighiiy poached, have been noted separately. The third trial (April 20th) made in the same field and under On tite Draught of Ploughs. 17 the same circumstances, except that the soil had become much harder and drier throughout. The fourth trial (April 11th) in which the hard trodden surface had been previously single-horse ploughed and reduced. The fifth trial (April 20th) during the stirring for barley (second furrow) with single horse, 4 inches deep, upon a surface harrowed and rolled. I made several minor experiments besides, to verify these, as well as for objects not immediately connected with our present inquiry. I made also several trials in order to arrive at some analysis of draught : they were made almost entirely by myself, assisted only by my man. I noted no draught down till my mind was perfectly satisfied about it ; and where there was room for doubt I threw the advantage to the side against which the test seemed to be going. There is a fifth place given to Hart's second mould-board, a whole one, to compare it with its more commonly used open one with detached ground-wrest. Comparatwe Experiments with Four light Draft Ploughs. Raiisome's Hart's. Barrett's B.irrett's ^ . Sil ^1 Furrow. N L 7. n 2:2 ?: 5 L2. DP. St.^ines. in. in. I. Apr. 2. Seed farrow, wiili single horse lOi 9 , , 10 8 2.} X 8 II. Apr. 3. Breaking up tarnip- groiind trodden in rain 23 21 22 22 19 5 X 9 Ditto. Breaking up turnip- ground less trodden . 19 18 20 20 17 5 X III. Apr. 20. Breaking up turnip- ground, drier and harder .. 25 2G 25 20 H X 9 IV. Apr. 11. Surface previously single-ploughed .... 19 .. 19 17 5i X 9 v. Apr. 20. Second furrow, with single horse .... lU 12 Ui 11 9 4X9 While the open mould-board of Hart's was a full stone lighter than the whole one, the reverse was the case with D P, which has a similar form of mould-board to shift. This arises, 1 believe, from greater fulness in the breast of Hart's open one. 7Vie comjmrative Average of each Plough, first, on the three occasions in which they were all engaged together ; then, where three ploughs only were togetheiv throughout, I think will be found as follows : — Average of Three Trials. Average of every Trial. Stones. Stones Ransome's N L 7 . 171 Barrett's L 2 . 17t Hart's \vhole-})oard . 17f Hart's with ground-wrest 17f Barrett's L 2 . . 17| Barrett s DP 15 Hart's with ground-wrest . 17 Barrett's DP. • . 15 VOL. III. C IS On Ihe Draught of Plonglis. It would be desirable to prosecute these experiments in wet seasons and in more adhesive soils. I have little doubt that I) P will g;enerally be found lighter than Hart's ; in comparing the two ploughs together, it is evidently constructed for lighter draught. Having satisfied my own mind about the relative position of the above four ploughs, I was led on to inquire a little into the cause of the difference, and thence to attempt to analyze the draught of ploughs as connected with the swing and wheel prin- ciple ; but, learning that the early publication of the Journal does not admit of my completing my experiments, I will reserve them (if thought sufficiently practical), together with other matter that I have promised in the course of this paper, for a future occasion. And believe me, dear Sir, Yours faithfully, Henry J. Hannam. Burcoit, May 12, 1842. HI. — Account of a, Field Thorovgh-dramrd, at Drayton, in Stafford.^hire, By the Right Hon. Sir Robert Peel, Bart., &c.' &c. To Ph. Pusey, Esq. My dear Sir, — I comply, with the greatest pleasure, with your wish that I should give you the particulars respecting the field which I drained and subsoiled, the produce of which was sent to you by our common friend Dr. Buckland. I was riding with him over a part of my estate in the autumn of 1840. He remarked a quantity of manure put upon a field, of poor soil, very wet, and in bad condition generally, and said, the tenant who placed it there went to very needless expense, for that manure would be of no service while the land remained undrained and in the state in which it then was. He said also, that the land in Scotland which had been so much improved by Mr. Smith, of Deanston, was naturally no better than that on which we were riding, and that in its original state it resembled that land in respect to the quality and properties of the soil in many particulars. These remarks of Dr. Buckland did not pass unheeded. I selected the worst field I could find, and determined strictly to follow the plan of Mr. Smith in respect to it, so far as draining and subsoiling are concerned. I first proposed to the tenant that he should retain the field and do the work under my directions ; Account of a Field Thoroufjh-drainecl. 19 but he thought it too expensive for his means, and preferred giving up the field and letting me take it into my own hands. Inclosed are the details with respect to the mode of treatment, conveyed in answers to queries put by me. The produce you have, I believe, from Dr. Buckland. The weight given is of the turnips, with the tops, but without the fibrous roots. I was ad- vised by very good practical farmers not to sow turnips, but to have a fallow for wheat : they thought the land not very well suited for turnips, and that the best period for sowing them was gone by. But I was desirous to exhibit the result of my experi- ment ; which I had mainly undertaken for the purpose of encou- raging others in my neighbourhood to follow my example. For that very reason, perhaps, I ought to have been less impatient. However, the turnip crop on one half the field far exceeded my expectations ; and the comparative failure on the other was clearly attributable to special causes. Believe me, my dear Sir, Very faithfully yours, Robert Peel. Whitehall, Jan. 13, 1842. Is'i. — Wlial was the nature of the subsoil in different parts of the field ? 2nd. — Was not the upper soil of a peaty nature ? 3rd. — What was tlie general depth of it above the sulisoil '? 4th. — Was that the best part naturally of the field where the best crop of turnips was? Or was the difference of produce in different parts of the field entirely arising from other causes? 5th. — Was the field very dry during the continued heavy rains of the season of 18il? Gth. — Did the drains act effectually? 7lh. — What was the depth of the several drains and main drain ? 8th. — When v/as the draining finished? 9lh. — What was the time when the tur- nips were sown ? 10th. — Was It the last sown that failed ? About one-third of tlie field was stiff clay ; the other part was a mixture of hard sand and gravel. Yes. From 4 to 6 inches. No : the greatest portion of it being stiff clay. The difference of produce arose from two causes ; viz., very heavy rains at the time of sowing, and the wire-grub. Yes ; very dry. Yes. Main drain, from 5 to 6 feet. Sub-main . . 3 to 4 ,, Other drains. . 2 feet 6 in. deep. 30th of April, 1841. Hertfordshire Whites, 21st of June. Red Giant. . . . 23rd „ Red Top .... 24th „ Globe 25th „ Yes ; the 24th and 25th of June. c 2 20 Account of a Field Tliorough-drainecl. lltli. — How were the tiles laid? ] 2tli.— What is the size of the field? 13th, — What was the coudition and aver- age produce before draining? 14(h. — What manure turnips? was used on the The drains being cut to their proper depth, and the tiles laid in, a thin covering of brushwood (spruce and Scotch firs) was laid upon them, and 6 inches in depth of small pebble-stones was laid upon the brushwood, a thin laj-er of turf (grass side downwards) was laid upon the stones, and then iilled up with the gravel or sand and soil which had been dug out of the drains. Five and a half acres. The preceding crop was oats, and seeded down with clover and grass seeds, which was almost a failure. The aver- age produce of the oats was 4 bags per acre ; the turnips were a mere brush crop ; the wheat about C^ bags per acre. 20 tons of lime were spread on the surface of the whole field, and 12 tons per acre of farm-yard manure. Scale of Chain. The field was twice ploughed with a single plough, then harrowed, rolled, and cleaned, ploughed again with a single plough, and followed by the subsoil-plough. Account: of a Field Tliorov fjh-drained. 21 After the field had been dramed upon Mr. Smith's plan, or nearly so (the principal difference being that the whole of the drains had drain- tiles placed therein, and Mr. Smith only names the main and sub-main to have drain-tiles), it was then limed with 4 tons of good lime per acre; then it was ridged up ; afterwards the ridges were split or opened with a plough, and rotten dung placed within the ridge or spht : it was immediately moulded up into ridge again, and the seed drilled on the ridge directly over the dung, so that the seed had the full benefit of the dung at the first stage of vegetation. I believe I can confidently state that the crop of turnips, after the above treatment, was four times the quantity in weight ever produced in the same field at any previous time. As to the quantity and the quality of the manure used, the manure was good town-made stable manure and your own good farm-yard dung, mixed ; the proportion used was 12 tons per acre. The best crop (27 tons per acre) was the Hertfordshire White : sown 21st of June. The second best (26 tons) was Mr. Skirving's Red Giant : sown 23rd of June. The next best was the Red Top : sown 24th of June : about 16 tons. The next best the White Globe : sown 25th of June : about 16 tons. The whole of the seed was from Mr. Skirving, of Liverpool ; and 2| lbs. of seed per acre was sown ; and the ridges were 24 inches dis- tant from each other. No portion of the field was either pared or burned. The distance between each drain is 21 feet. The strong clay which was dug out of the drains was spread upon the peaty soil, and was con- sidered almost as good as a dressing of manure. Every drain was open throughout before any tile was allowed to be laid ; and the field was almost free from water when the tiles were put in. The field was in a wretched state before, as to wet. (Signed) Thomas Hill. The Rt. Hon. Sir Robert PeeL Bart. IV. — 0)1 the Connection heticeen Geology and Agriculture in Cornwall, Devon, and West Somerset. By Sir Henry T. De la Beclie^ Director of the Ordnance Geological Survey. \_From tiis General Report on the Economic Geology of that district A It can scarcely escape the most casual observer^, that the fertility of this district varies most materially, and that very striking con- trasts in the productive character of the soil present themselves to his attention in different parts of it. If he will take a geolo- logical map in his hand and compare this variation in fertility with the colours marked upon it, he will scarcely fail to find that there 22 Connectlun between, Geoloijy ^ turns, may be sometimes owing to the mildness of the foregoing winter: in the instance just related, there had been no severe frosts either in the winter or spring, so that the previous autumnal , broods of caterpillars lived through the cold season, and it neces- sarily followed that an immense number of the moths were pro- duced, and the spring and summer which succeeded proving favour- able to their increase, they became more abundant than they had ever been known before. It is only surprising that such events do not oftener occur, when we consider the rapidity with which insects increase. Let us, for instance, suppose that no accident in- terfered with the progress of the different broods of this moth, of which there are two every year : it is believed that one female moth * Godart's Lepidop. de France, v. 7, part 2. p. 43. t Reaumur, Hist, des Ins, v. 2, p. 326. 74 Observations on Insects affecting the Turnip Crops. Avill lay about 400 eggs, which would be transformed in a few weeks to 400 moths : if we allow half of these to be females, they would lay at the same rate 80^000 eggSj which would in the following autumn (admitting that the first was a vernal moth) become per- fect insects^ whose eggs, taking again half of them as females, would amount to the prodigious number of 16,000,000, which would hatch the following spring, and be ready to devastate the spot on which they were bred : there must be, consequently, in- numerable agents in operation to stop their increase, although I do not happen to have met with the species of ichneumons, «Scc. which are destined to preserve our green crops from being anni- hilated by the caterpillars of the Y-moth. Plusia (jamma is a widely-dispersed insect, being found all over Europe, and it is said to extend even to the frontiers of China and Siberia : it likewise inhabits North America. Unlike most other species of Noctuidse, this moth flies about by day, not only in the sunshine, but regardless of the weather, it will be seen on dull and even damp days hovering over flowers, and^ like a sphinx-moth, thrusting in its long spiral proboscis or tongue to extract honey from the nectaries ; at other times, fluttering and running over the flowers, or resting upon them with its wings closed. There is no moth more shy and difficult to catch by day, for it will seldom allow any one to come near it, but whether it detects the approach of man by its eyes, which sparkle like living rubies, or by its hearing, is not knovv^n : it darts off, however, in an instant when disturbed, and stops again a few yards off, or entirely vanishes. Should the Y-moth caterpillars ever become fearfully abundant in our turnip-fields, it is not improbable that ducks, poultry, and fcheep might be very serviceable in diminishing their numbers, if employed as recommended in the last report upon the black caterpillar. Having nov/ given an account of several kinds of insects con- nected with the turnip crops, T must leave for a future opportu- nity some others which are equally interesting, and not less de- structive. The following summary will be useful, by placing before the reader in a concise form the results of my investiga- tions : — History of the Aphides, or Plant-Lice, Every crop, both in the fields and gardens, is subject to the attacks of various species. Two different sorts infest the leaves of the English turnips, one haunts the leaves of the swedes, and another the Jioiver-stalks . The green tops are rendered less fit for cattle when infested Observations on Insects affecting the Turnip Crops. 75 with aphides'^ and the growth of the plants and the roots is re- tarded. 168 aphides were seen upon one small turnip-leaf in July. It is by thrusting their beaks, called the rostrum^ into the plants, /, and imbibing the sap, that they injure our crops. The females are both oviparous and viviparous : they are winged and apterous. In autumn they lay e^^s , w hich hatgh th e fo llowing spring -. /^ The eggs are laid! upon the~l eaves, undertlie buds, and other secure places. The females bring forth young, without sexual intercourse, for many generations. ^ Their increase is prodigious : it is calculated that one female might be the progenitor of upwards of 5900 millions of de- scendants in one year. ^ The eggs hatch about the period ^f north and north-east winds, in M arch and A pril. Their increase is accelerated by damp sidtry weather as the season advances, i-^ Electricity probably often causes their simultaneous appearance. The aphides can wcdk about as soon as they are born^ and are able to do so until their lives are terminated. Abundant in August, September, and October, and even at the end of November, secreted beneath the diseased leaves. ^ It is doubtful if these species deposit the saccharine matter called honey-deiv. Cutting off the infested leaves and destroying them on the spot, or carrying them away in sacks to be burnt, is the best remedy. ^ To bacco and Um e_ water will kill the aphides^. Lime-dust, if strewed in cTry weather, is an effective cure^ . "^ i^ They often d p not suffer from heavy rains. Insectivorous birds, and various i7isects, our best friends in checking their increase. y_. The lady-birds and their larvw are particularly useful in de- stroying the aphides. Immense swarms of the lady-birds sometimes appear on our shores. A little fly called Aphidius lays its eggs in the aphides, and when they hatch the maggot destroys the aphis. These again become the victims of other small flies, called Ceraphron Carpenteri, Cyrtogaster vulgaris, and Colax aphidii. Some of the Cynipsidce, or gcdl-flies, are also parasites, which live in the aphides as maggots. Four other wasp-like flies collect the aphides as food for their young. 76 Observations on Insecls (tffedlnr) the Turnip Crops. The ApJiLS-llon, or larva of the Golden-eye fly, destroys the aphides; and \\\e maggots of some two-winged flies called Syrphi arc still more serviceable in their destruction. These are^ however^ in their turn infested with a parasite called Cerajjhron syrjjhi. Severe frosts destroy the aphides^ but they are able to propa- gate in mild winters. When immersed in ivatcr for sixteen hours^ it has not killed them. An atmosphere strongly im2:>regnated with camphor did not affect them in twenty-four hours. The Turnip- LEAF miners may generate diseases in cattle, when they greatly abound. One called Drosophila flava causes large blisters on the upper sides of the leaves, which contain the maggots. The other, named Fhytomyza nigrico7mis, is the parent of a maggot which eats galleries in the under-sides of the leaves. The Turnip diamond-back moth : the larvae feed upon the turnip-leaves, and sometimes nothing but the fibres are left. l^lie chrysalis is inclosed in a net-work cocoon, attached to the dried fibres, or formed upon the ground. It is found all over Europe from Midsummer to November, and does great mischief in the kitchen-gardens in the Mauritius. Upwards of 240 of the caterpillars have been found upon one plant. A parasitic Ichneumon lays its eggs in the caterpillars. The Y-MOTH lays its eggs on the under-side of turnip-leaves and other plants. The green caterpillar feeds upon the turnip-leaves and a variety of plants. The chrysalis is inclosed in a white web, often spun in the folds of the leaves. The 7?ioths are abundant from April till October, especially in the latter month and in July. Rainy seasons seem to be congenial to their increase. In October, 1816, the moths swarmed in the north of France. In 1735, the caterpillars ate up all the vegetables around Paris, excepting lentils. Their ravages extended to the centre and south of France, where they consumed the hemjj-crops, and did not refuse grasses and clover. They spared the corn-crops, but attacked the oats later in the season. The previous ivinier and spring had been very mild. One female Y-mothin the spring might become the progenitor Observations on Insects affecting the Turnip Crops. 77 of 16,000,000 of caterpillars, in the space of twelve months, viz. from the spring of one year to the following spring. It is dispersed over all Europe, to the confines of Siberia and China, and is also an inhabitant of North America. It flies by day as well as at night. Ducks, poultry, and sheep recommended to destroy the cater- pillars. EXPLANATION OF THE PLATES. Fig. 1*. Aphis Rapee, male, a The natural dimensions. Fig. 2*. , female, h The natural size. Fig. 3*. , a young one just excluded. Fig. 4*. Aphis dubia. c The natural size. Fig. 5*. Aphis Brassicss, male, d The natural dimensions. Fig. 6*. , female, e The natural size. Fig. 7*. Aphis Floris-Rapse, male. /The natural dimensions. Fig. 8*. ■ , female, g The natural size. Fig. 9*. Front view of head of an Aphis magnified. h The rostrum or beak. i The compound eyes. k The three ocelli or simple eyes. Fig. 10*. The head in profile of an Aphis magnified, showing the rostrum and antennae. Fig. II*. One of the antennae or horns greatly magnified. Fig. 12*. One of the six legs magnified. / The thigh or femur. m The shank or tibia. n The foot or tarsus. The claws and pulvilli or suckers. Fig. 13. The larva of a Coccinella or lady-bird. * The same magnified. . Fig. 14. The pupa or chrysalis of ditto. Fig. 15. The twin-spotted lady-bird. Fig. 16. The seven-spotted ditto. Fig. 17*. The indurated skin of a female Aphis, from vdiich a para- sitic fly has been hatched. p The natural size. Fig. 18*. Aphidius Rapse, the parasitic fly alluded to, q The natural size. Fig. 19. The larva of the golden-eye, called the Aphis-lion. * The same magnified, with the lichen removed. Fig. 20.- The cocoon formed by the larva. Fig. 21. The golden-eye, Chrysopa perla, a female, at rest. Fig. 22. The eggs of ditto, copied from Reaumur, Fig. 23. The maggot or larva of Syrphus pijra-^tri, sucking an Aphis. Fig. 24. The pupa of ditto. Fig. 25. Syrplius pyrasiii, male. 78 Ohfiervatioiis on Insects affecthg the Turnip Crops. Fig. 26. A turnip-leaf, upper-side. Fig. 27. The maggot of Drosophila flava, feeding under the cuticle. Fig. 28. The pupa of ditto. Fig. 29*. The same greatly magnified. Fig. 30*. Drosophila flava represented flying. r The natural dimensions. Fig. 31. The gallery formed on the iinder-side of a turnip-leaf by the maggot of Phytomyza nigricornis. Fig. 32. The pupa of ditto secured under the cuticle. Fig. 33*. Phytomyza nigricornis represented flying. s The natural dimensions. Fig. 34. The caterpillar of the Turnip diamond-back moth. Fig. 35. The pupa of the same inclosed in the cocoon. Fig. 36. The moth from the same represented at rest. Fig. 31*. The same flying and magnified. Fig. 38*. The egg of the Y-moth.' t The natural size. Fig. 39. The full-grown caterpillar walking. Fig. 40. The chrysalis in its web. Fig. 41. The Y-moth flying. Obs. All the figures are drawn from nature, excepting 22, 23, and 34, and the numbers with a * attached indicate that the objects referred to are represented much larger than life. London, February, 1842. [Tlie copyriglit of this paper is reserved by the writer.] VII T. — On the Comparative Value of different Kinds of Fodder. By the Rev. W. Riiam. As the following table of the comparative value of different kinds of fodder in feeding- cattle may not be a:enerally known, I have translated it from the French. It has been published by M. Antoine, at Nancy, and is the result of experiments made by the principal agriculturists of the Continent, Thaer, Gemerhausen, Petro, Rieder, Weber, Krantz, Andre, Block, De Dombasle, Boussingault, Meyer, Plotow, Pohl, Smee, Crud, Schwertz, Pabst. It is unnecessary to give the figures which each of these experi- mentalists have set down, but the mean of their experiments being taken, there is more chance of the result being near the truth. Allowance must be made for the different qualities of the same food on different soils and different seasons. In very dry summers the same weight of any green food will be much more nourishing than in a dripping season. So likewise any fodder 33 3& * :/^... D /. ,./,/zc- m..^./ -/A', Comparative Value of different Kinds of Fodder. 79 raised on a rich dry soil will be more nourishing than on a poor wet one. The standard of comparison is the best upland meadow- , hay, cut as the flower expands^ and properly made and stacked, without much heating- ; in short, hay of the best quality. With respect to hay, such is the difference in value, that if 100 lbs. of the best is used, it will require 120 lbs. of a second quality to keep the same stock as well, 140 lbs. of the tHrd, and so on, till very coarse and hard hay, not well made, will only be of half the value, and not so fit for cows or store catde, even when given in double the quantity. While good hay alone will fatten cattle, in- ferior hay will not do so without other food. I shall give the table as it stands, and add the notes which accompany it : — lbs. Good hay . . . . - , . . 100 is equal in nourishment to Lattermath hay 102 Clover, hay-made ..... 90 when the blossom is com- pletely developed. Ditto 88 before the blossom expands. Clover, second crop .... 98 Lucerne hay 98 Sainfoin hay 89 Tare hay 91 Spergula arvensis, dried ... 90 ' Clover hay, after the seed . . . 146 Green clover 410 Vetches or tares, green . . . 457 Green Indian corn 275 Green spergula 425 Stems and leaves of Jerusalem arti- choke 325 Cow-cabbage leaves . . , . 541 Beet-root leaves 600 Potatoe halm 300 Shelter wheat-straw .... 374 Rye straw 442 Oat straw 195 Peas halm . 1 53 Vetch halm 159 Bean halm 140 Buckwheat straw 195 Dried stalks of Jerusalem as ticliohes 170 Dried stalks of Indian corn , . 400 Millet straw 250 Raw potatoes 201 Boiled ditto 175 White Silesian beet .... 220 Mangold- wurzel 339 Turnips 504 80 Comparative Value of different Kinds of Fodder. lbs. Carrots 276 Cohlkalis 287 Swedish turnips 308 Ditto, with the leaves on , . . 350 Grain — Rye ■■ 54 Wheat . . , . . 45 Barlev 54 Oats ' 59 Vetches 50 Peas 45 Beans 45 Buckwheat .... 64 Indian corn .... 57 French heans, dried , . 32 Chestnuts 47 Acorns 68 Horse-chestnuts . . . 50 Sun -flower seed ... 62 Linseed cake .... 69 Wheat bran .... 105 Rye bran 109 W^heat, peas, and oat chaff . . 167 Rye and barley chaff . . . . 179 Dried lime-tree leaves , . . . 73 oak leaves 83 Canada poplar leaves . . 67 Observations. Lattermatli hay is g-ood for cows, not for horses. The second cut is generally considered as inferior in nourishment to the first. New hay is not wholesome. At Paris, when a load of 1000 kilos is bargained for, the seller must deliver — if between hay- making and October 1, 1300 kilos— from October 1 to April 1, 1 100 kilos — and after April, only 1000. This is fair, and allows for loss of weight in drying. In London, a load of new hay is 20 cwt. ; of old hay, only 18 cwt. Spurney (Spergula arvensis) is excellent food for cows ; but, except on poor moist sands, the crop is so light as not to pay for cultivation. It grows rapid) v, and makes a good intermediate crop between barley-harvest and winter. The dried halm of the Trifolium incarnatum, after the seed is ripe, is little better than straw. Clover, lucerne, and sainfoin are generally supposed to lose three-fourths of their weight in drying ; but in general they lose more, especially in moist climates, where the sap is more diluted. When touched by the frost, they become very unwholesome,, and should never be given to cattle except quite dry. Comparative Value of different Kinds of Fodder. 81 All beasts are fond of the green stems of the Indian corn or maize; but it has not yet been much cultivated in Britain. If sown in May, so as to be free from frost, after the seeds have been well soaked in water, the crop will come up well, and be ready to cut green in September and October, without ever pro- ducing any seed ; but v/ithin the stalk will be found the embryo of the seed ear, which is extremely svv^eet and pleasant to the taste. It is very good boiled as greens. Green spurrey gives excellent milk and butter when the cows are fed on it. There is a variety which is much larger than the common field-spurrey, and which is worth attention. The stems of Jerusalem artichokes when young may be good fodder, but they soon get hard and woody. The leaves of the cow-cabbage, when given quite fresh, and none of them v/ithered or decayed, are excellent for cows, and give no taste to the butter. Straw is, on the whole, but poor food, and unless cattle have something better with it, they will not keep in any condition ; when given with turnips or other roots, straw corrects their watery nature, and is very useful ; cut into chaff it is very good for sheep when fed on turnips and oil-cake, and when newly thrashed is as good nearly as hay. By a j udicious mixture of different kinds of food, a more economical mode of feeding may be substituted for a more expensive one, and the same result obtained. The value of straw depends much on the soil : a very clean crop will not give so nourishing straw as one containing many succulent weeds. Peas and vetch halm are superior to straw, especially when cut into chaff: it is by some thought equal to hay. The same may be said of bean halm not left too long in the field, and cut before it is completely dry. Buckwheat halm is of little value : it is thought unwholesome if given to sheep. The dried stems of the Jerusalem artichoke must be cut into chaff, and then boiled or macerated in water, otherwise the cattle cannot chew them. I'he same may be said of the stems of millet, sorgho, and maize. Raw potatoes increase the milk of cows, but they must be given \^ith caution, and only a few at first, till the stomach is accustomed to them; boiled, they fatten every kind of stock ; mixed with cut chaff, they are excellent for horses : 14 lbs. of boiled potatoes will allow a diminution of 8 lbs. of hay; hence their value in this w^ay is easily calculated. When hay is 4.1. 4-y. a load, it is just \d. per lb. ; the 14 lbs. of boiled potatoes are therefore worth 4d. And 56 lbs. being reduced by bailing to 42 lbs., the potatoes are equal in value to '2y. per cwt,, which is 405. per ton. From this must be deducted the expense of boiling; where fuel is cheap, this will be compensated by the dung, which would have been lost had the potatoes been sold. If 14 lbs. of boiled potatoes are equal to 16 lbs, raw, raw potatoes VOL. III. G 82 Comparative Value of different Kinds of Fodder. are one-half the value of hay; and if hay is Jc/. per lb., raw pota- toes are worth \d. per lb., \s. ''2d. the half cwt., and conse- quently more than when boiled. Every kind of cattle eat turnips except horses. Turnips will feed store pigs, but they will not fatten on them. Carrots and parsneps are excellent for horses, and, when boiled, will fatten hogs. Ruta-baga is liked by horses : it makes their coats fine, but must not be given in too great quantity, or it will gripe them. In France, the flour of buckwheat, seasoned with salt and mixed with water, is used to fatten oxen, sheep, and swine. Hogs fattened with chestnuts have fine-flavoured flesh. If the horse-chestnuts are boiled, the bitter part is boiled out, and cattle will eat them readily : mixed v.itli other food, they soon become accustomed to them. Oil-cake varies in nutriment, as in price : if linseed- cake is 17*50, rape-cake will be 16*60, cameline and hemp-seed cake 9, poppy-cake 8. Bran is good for horses mixed with oats, and for milch cows excellent. If it can be had good at \d. per lb., it is worth as much as the best hay. The value of dried leaves is taken chiefly from their analysis by Sprengel ', but they must be gathered when green, and dried like hay. On the Feeding of AnimaU. A certain quantity of food is required to keep an animal alive and in health : this is called his necessary ration of food : if he has more, he will gain flesh, or give milk or wool. An ox requires 2 per cent, of his live weight in hay per day; if he works, he requires 2^ per cent. : a milch cow, 3 per cent. : a fatting ox, 5 per cent, at first; 4 J per cent, when half fat ; and only 4 per cent, when fat ; or 41 on the average. Sheep grown up take 3^ per cent, of their weight in hay per day, to keep in store condition. Growing animals require more food, and should never be stinted. Winkfeld, March, 1842. ( 83 ) IX. — On Cottage Economy and Cookery. Compiled bj French Burke, Esq., from Essajs submitted to the Rojal English Agricultural Society. On directing their attention to improvement in the condition of our peasantry, it occurred to many Members of the Royal Agri- cultural Society of England, that few objects would tend more to add to the comforts of the labouring population than to furnish them with plain instructions for some better modes of preparing their food, without any increase of expense. To use without waste the food which Providence supplies for the w^ants of man is indeed of the greatest importance to those who have but little to spend ; and nothing so completely disarms the stings of poverty as the means of rendering a scanty pittance capable of producing a comfortable meal. If, therefore, by teaching them a little of simple cookery, it can be occasionally so changed as to make it somewhat more savoury at the same cost, there can be little doubt that it would materially add to their comforts, and thus attach them still more to their homes. For although they consume far more animal food than the foreign peasantry of Europe, they yet do not fare so well ; and that solely by their different mode of preparing their victuals. The Society therefore offered a premium, in the course of last year, " for the best directions to enable labourers to prepare wholesome, nutritive, and palatable food, in the most economical and easy manner:" not with any intention to lessen its quantity, but to point out some simple means of rendering it occasionally more pleasant to the palate, and withal more digestible and healthful. Numerous essays were accordingly presented to the Council, and, after careful examination, that written by a female — who describes herself '' as having, during a long life, passed it in a village some miles distant from London, where she has brought up a large family, with due attention to economy, and with con- stant opportunities of witnessing the modes of life of her poorer neighbours" — was deemed entitled to the prize. Some of the other essays, however, containing hints which were thought worthy of attention, portions of them have been made use of in the fol- lowing account, with the consent of the authors. It will be grati- fying to find that these and similar instructions have the effect intended ; but their success must depend in a great measure on the habits of the poor themselves : contentment will give a flavour to the poorest fare, and plenty goes hand-in-hand with frugality. It should be observed that the prices herein stated are those of the metropolis. Large deductions must, therefore, in some in- stances be made from them^ so as to meet those current in markets g2 84 On Cottage Economy and Cookery. far distant from London, and In remote parts of the comitry; but this can occasion no real inconvenience, as every one can reduce the cost of any article to the sum usually paid for it where he resides. There can be little doubt that bacon, household-bread, and cheese, washed down by a draught of strong beer, is a v/holesomc and substantial meal for a working man ; and, if he can but afford it, he will seldom find a better. Fresh animal food is, however, more nutritious ; as bacon, although it goes farthest in family use, and is therefore more commonly employed by the poor, yet occa- sions much greater perspirations after hard labour, and thus not only creates more exhaustion, but a little change, where it can be had, is both pleasant as well as wholesome. When a cottager has a garden and fattens a pig, he seldom goes to the l)utcher until the bacon is all consumed ; but he would do better by occa- sionally buying a pound or two of meat to eke out the bacon until he can kill another hog. With regard to strong beer, we are far from decrying its use in moderation ; but, independently of its cost, although its excite- ment gives momentary strength, yet we know, from those who have tried it, that continual labour will be better performed by a man who during the day drinks only water mixed with some powdered ginger, and leaves the beer to enjoyment with his wife at night; for although the malt liquor exhilarates the spirits, and enables a man to perform more work for an hour, yet this stimulus leaves him in a more exhausted state than before he drank it. The powder is extremely cheap : it warms the stomach, and a very small quantity, which can be mixed in a moment, with a pint of water, will be found a more invigorating draught in warm weather than the same quantity of common harvest-beer. It is a great error to suppose that butter and cheese are less expensive than meat, if it be judiciously purchased and economi- cally prepared ; but the poor are, in marketing, oftentimes more anxious to obtain a portion of the best joints than to content them- selves with those of inferior price, although these generally con- tain as much, and sometimes more, real nourishment. The trimmings of the joints and the coarse parts, as well as the bones, when flavoured with various sorts of vegetables, and thickened with either rice, barley, or oatmeal, can be converted into several savoury dishes at a very trifling cost. Of the various kinds of meat, beef and mutton are decidedly to be preferred; and, in regard to cookery, stews of different sorts are not only the most economical, but have the advantage of procuring for the family a warm supper of some variety after the toil of the day is over. Of these, perhaps, the cheapest may ]je made from a shin of beef, which usually weighs from 16 to 20 lbs. ; and, if the whole be On Cottage Economy and Cookery. 85 purchased, may commonly be got for 2s. or 2s. &d. ; or, if only a portion be taken, at 2^jl. to 3f/. the pound. The better way is, therefore, for two or three families to join; but as that can only rarely be done, then buy only so much as will serve a couple of days for a man, his wife, and two children under ten years of age (^for tchich number in family these instructions are in- tended), and dress it as follows : — Cut off the meat into slices, break the bone into small pieces, and put the whole into a saucepan, covered with a quart of water, until it boils. Then skim off the grease (but do not throw it away, as it will afterwards serve for frying), and add 2 quarts of water, 2 large onions, carrots, and turnips, cut into small squares, and a fev/ grains of whole pepper, with sufficient salt for season ing. Put the saucepan then on one side of the fire, to simmer gently until the meat is tender ; which, although it will take from lour to five hours, yet does not require any attendance. The half of it may be left to be warmed up the following day; and the bones should be again stewed down in a small quantity of water, to add to the soup. If this be done in that common kitchen utensil the iron digester (which no cottager should be without), a great deal of fatty substance will be extracted even from these bare bones, and made, with a little more vegetables, into tolerably good broth. The whole cost for the two days, even supposing the vegetables to be purchased, will be — Meat, say 4 lbs., at 2i [Finlaysoirs Patent Harrow.] clogging. Earth full of couch or other weeds coming against it will not stop there, but will rise over the tooth, and fall down on either side, the earth below and the weeds above, on the surface of the land. 'J'he faults of this machine are three : 1st. The wheels are always made too small, and the frame is too near the ground, so that in working rough land this clogging takes place in spite of the excellent form of the teeth. 2ndly. The clogging takes place also from another cause. It will be seen that the distance between any two adjacent teeth, according to the arrangement in this machine, is only double of the distance between the paths of the teeth — only 1 foot. Rough, cloddy, and couchy ground will thus soon stop the machine. This may be remedied by a different arrangement, as that in the annexed figure for instance, where the dis- tance between any two teeth is four times that of the space between any two adjacent paths of the teeth in the ground. Srdly. There are no simple means of lifting the machine wholly out of the ground : the front part may be raised, but the hind part remains. Kirkwood's grubber, an improvement on Finlayson's, was intended to remedy some of these faults. For the third one he had a very neat remedy, which is best understood by the drawing which represents the frame-work in two different portions, depending on the degree to which the handles are depressed. (See p. 98, Low's ' Practical Agriculture.') It wdll be seen that the frame-work is lifted partially out of the ground by this means, both ends being raised at once by depressing the handle. In this machine the 2nd fault is also remedied by an arrangement of the teeth, such as that represented in the annexed figure. It wuU be seen that the distance between any two teeth is much more than twice the On Agrlcidtiiral Mechanics. 1*21 distance between the paths of the teeth through the ground. Kirkwood, however, abandoned Finlayson's form of the toothy and substituted one such as that represented in page 123 ; and in his machine the first fault of Finlayson's grubber remains in full force, — the frame-work is too near the ground. Biddell's scarifier is another implement of this class, much stronger and more clumsy : the frame-work* is similar in form to Finlayson's, the teeth as before being arranged in two rows right across the direction of the path of the machine. It is supported on two large wheels behind, and two small ones in front, by which it is raised 20 inches oft" the ground, much higher than in Finlayson's. There is, above the machine, a complicated apparatus for lifting it out of the ground. The front part is raised by one lever, and the hinder part by another. The form of the tnoth has nothing to recommend it : it is necessarily strong and is attached to the frame-work by bolts : to this tooth either a chisel- edge or a duck-foot may be attached ; the one being intended to stir the ground merely, and the other to pare its surface. This machine, from its height oft" the ground and its great strength, is well calculated to work very rough and conchy land. If, however, the ground is damp when the paring-teeth are used, it is impossible to work it, as it immediately clogs. The whole of the machine is of cast-iron, and the teeth are therefore liable to break in stony ground. Four horses are required to work this machine; it is made nine teeth wide = 4 feet 6 inches j five teeth in the back row and four in the front. Another implement, a very great improvement on Finlayson's harrow, has been put forth by Scoular of Haddington, who supplies them there at 7/. each. The form of the frame-work, the form of the teeth, the arrangement of the teeth, and the height of the frame-work, ar ehowever the same, still faulty. The improvement consists in a simple means of raising or lowering the frame-work altogether, and of keeping it at any one depth. It will be understood from the annexed figures, which give a side-view and a ground -plan. It is much simpler than Kirkwood's, and possesses, by means of the notched upright, a very simple method of keeping the machine at one depth ; the lever or handle by which it is raised is merely fixed in one of these notches : this is effected in Kirk- wood's grubber in a complicated manner. Finlayson's, Kirkwood's, and Scoular's are wholly wrought-iron, except, of course, the wheels. Now taking Scoular's as the best of the four for general purposes — and here I may say, that having only five teeth, and working a width of 3 feet, it is perfectly manageable by two horses — if we first take Scoular's machine and point out all its faults, we shall see how these have been remedied in a machine, the invention of the managers of Lord Ducie's Iron- Works at Uley, in Gloucestershire. 1st. The wheels are too small; the frame- work is greatly too near to the ground. 2nd. The teeth, being in two rows right across the path of the machine, are only twice the distance from one another that exists be- tween any two adjacent paths or ruts made by them in the ground, * See Journal, vol. i., p. 357. 122 Gn jiijn' cultural Mechanics. 3rd. The teeth being in two rows, there is necessarily a tendency in the bars to which they are fixed to twist, for theie is not the strain of one only, but of three teeth, all acting on one bar, tending to twist it. 4th. The teeth, though of a good form with regard to their general figure, are not good, if we judge of their strength by their section. This is broader than it is thick ; whereas, to stand the great strain placed on them when at work, it should be much thicker than wide. This fault occasions, when the machine is at work, an almost constant recurrence to the smith's shop, the teeth becoming bent. 5th. The whole machine, being of wrought-iron, is expensive, 6th. Although the mode in whicli the implement is raised out of the ground answers the purpose perfectly, and is beautifully simple, yet it is difficult to manage. It is as much as a man can do to lift it out of the ground at the end of the field, when it is at work. And the difficulty is due in part to this circumstance : it will be observed that the cranks by which the hind wheels and front wheels are attached to the machine all lie behind their points of attachment, — they incline from the horses. Now, in consequence of this, in raising the machine, it is evidently by the action of the lever pulled towards the driver — pulled backwards, and thus in lifting it out of the ground the man has not only the mere weight of the im])lement to lift, but he has to overcome the whole force of the horses which pull it forward, and thus tend to keep it in the ground. These points, then, require alteration, and at the same. time an implement was required which should be as efficient and as easily drawn. With regard to the first point, the Uley Cultivator rests on four wheels; the front ones being 18 inches in diameter, and the hind ones 3 feet 4 inches in diameter. From the front ones rises an iron rod, having a circular section which passes through the point or nose of the frame- work ; the hindmost ones rest on cranks on an axle which runs straight through the frame-work : the frame-work is thus 20 inches off the ground. 2nd. The teeth are not placed in rows, but are arranged as in the annexed figure (p. 16), and somewhat similar to the arrangement in [Lord Ducie's Cultivator.] Kirkwood's grubber. The space between each is thus 2 feet — tvvic: that of Secular's — while the distance between the paths of each is only On Agricultural Mechanics. 123 6 inches, the same as in Scoular's. On the points of these teeth, either chisel-shaped or duck-foot or triangular edges for paring are slipped, the form of the tooth on which they slip being such as to hinder these teeth from slipping round. This, with the form of the teeth, is repre- sented in the figure; the teeth for paring are much more pointed Kirkwood's. Finlayson's. Biddell's. Uley Cultivator. than those of Biddell's, with which they are compared in the annexed figure. The implement has been tried for paring as well as for stirring, and is found to move the whole surface of the ground most perfectly. 3rd. The frame-work does not, as in Finlayson's harrow, consist of a series of cross-bars, into two of which the teeth are fixed in two rows, but it is as in the annexed figure; each tooth having its own bar, to W'hich it is affixed, and not being attached in a direction across the bar, but in the direction of its length, so that any strain on it cannot tend to twist it. 4th. The tooth is not of the same form as Finlayson's, but it has, as Finlayson's, a self-cleaning form. This will be understood from the figure of it given above. It will be seen that the rise for the first five inches is most gradual, and that any conchy earth or clods coming against it will not be stopped by it and clog it, but will rise and tumble over, and fall aside, and so pass by. This, with the height of the frame mentioned in No. 1, and the distance between the teeth, spoken of in No. 2, hinders any possibility of the machine being clogged in fast-land. 5th. The machine is partly cast-iron and partly wrought ; and thus while the liability of Biddell's to break is avoided, the advantage of having the cheapness of cast-metal is partly ensured. The sections of the teeth, given in a figure above, show that they are strong enough. Their strength is increased by having an abutment on the frame, against which they rest. The manner in which they are fixed to the frame is also such as to increase their strength. Ihey are made slightly taper at the place where they are keyed in, so that a blow of the hammer makes them fit perfectly accurately to the frame. They are not fixed by wedges, as the coulter of a plough, but by a key which passes through the frame, through both the mortice and tenon, and thus holds them fast. 6th. The mode in which it is raised out of the ground, and the plan by which its depth is regulated, is an invention of Mr. Clyburn, of Uley Works. The ease by which the operation is performed is greater, and the complication of Biddell's scarifier is avoided, while the regularity and parallelism of the motion of the frame-work, as it is raised or lowered, is as perfect as in Scoular's or Kirkwood's. The hinder part of the machine is, as in Scoular's implement, raised by increasing the inclination of the cranks which attach the hind-wheels 124 On J (jrkultnral Mechanics. to the frame. In this, however, instead of inclining backwards, and thus requiring, on lifting the machine, an exertion of force, as we before ex- plained, against the whole pull of the horses, the crank is thrown for- ward in exactly the other way; and thus the whole force of the horses, instead of being exerted against the effort of the driver to raise the implement out of the ground, is actually exerted in assi^ting him to do so. The front part of the machine is not raised in the same way as the hinder part, by a crank on the front wheel, but it slips up and down the vertical pole attached to them, and is raised in the following way : the cranks of the hinder wheels are attached to an axle, which passes through the frame, and thus supports it. On this axle a toothed wheel is fixed : this toothed wheel is worked by an endless screw on a shaft, which also works in the frame of the machine. This shaft working by means of this endless screw, a toothed wheel on the axle across the imple- ment is necessarily parallel to the length of the machine, and is turned by means of a crank- handle above. Turning this handle round in one direction, it is evident that the axle on which the toothed wheel is fixed will be turned round, and the crank of the hind wheels raised, and thus the frame brought nearer the surface of the ground, the teeth let deeper into it; by turning the handle the other way, the hind part of the machine is raised. In order to get the front part of the machine raised and lowered ex- actly as the hinder part of it, the following simple method is adopted : on the axle of the hinder wheels a crank is fixed, attached for greater simplicity to the pinion before mentioned. It is the same length as the crank of the hind wheels; when, therefore, the pinion is turned round, these wheels being by this crank raised, that is, the frame being lowered, say 2 inches, the extremity of this crank is lowered 4 inches.* From the crank a vertical rod rises, which is attached to one end of a lever rest- ing at the other end on the vertical rod at the front of the machine, and attached exactly at the middle by means of a rod of iron to the frame- work of the implement. When, therefore, the point of the crank is lowered 4 inches, the hindmost extremity of the lever is also lowered 4 inches, and, as it rests on the top of the vertical rod at the other end, it depresses the rod in the middle and the frame-work attached to it exactly 2 inches, the same as the hind part of it. The perfect parallelism of its motion is thus ensured, while the mode of lifting it requires but a small exertion of force. The implement is altogether about 6 cwt. in weight. It is supplied at Uley at prices varying according to the size, weight, &c. at which it is ordered, certain forms of the implement being intended for two horses and others for four. Before leaving this subject I wish to say a word which might perhaps have been more properly placed in the account of the plough. The looseness in which the use of this implement leaves the land is, in every case, except when dry weather is anticipated, the most advan- tageous for the germination of the seed or the growth of the plant. * Two inches by the action of the crank, and other^'2 inches by the lowering of the frame to which the crank is attached. On Agricultural Mechanics. 125 It has been customary to trample and roll, and by every means firm the land after wheat-sowing, to hinder the frost from throwing the young plants out. On this account, when my father stated his intention to a party of farmers who were walking over Whitfield Example farm, of sowing wheat on a field which had been subsoil-ploughed in the spring, and had borne an excellent crop of swedes, and which was then, after having been cultivated with Secular's implement, in as loose a state as possible, they tried to dissuade him, and foretold that the young plants would, on the first frost, be thrown out. The plants certainly sustained some severe frosts, but the result showed the fears expressed to have been unfounded. The Norfolk farmers, I believe, are very careful, in ploughing for wheat, to break the furrow-slice as little as possible, and to firm the land as much as possible, before sowing their wheat. They find that this tends to hinder the frost from throwing out the plant. May not this throwing out by the frost, upon wet land at least, be explained in this way ? The rain falls on such land, and sinks in till it comes to an impervious bot- tom, at no great depth, where the land has never been stirred by the plough or otherwise. It remains there, and, on freezing in winter, it of course forces open the land, and the plants are thrown out and killed. There are two ways of hindering this : one is to trample and roll the land, and make a hard surface, so that the rain, on falling, flows over the surface and is carried away by the open furrows. It thus does not sink in. This is the plan generally followed, but it often fails, as I be- lieve the experience of many would testify. Would not the better plan be to drain the land and put in the subsoil-plough and work it with the scarifier? The rain, on falling, will certainly sink in, but it will sink far beyond the reach of the frost, and will be carried away by the drains, the plants at the same time deriving all the advantages of a free and open soil. [To he continued.'] XI. — On the ^' Tchornoi Zem,^' or Black Earth of the Central Regions of Russia. By Roderick Impey Murchison, F.R.S., President of the Geological Society. [Since the accompanying sketch was read before the Geological Society of Londjn, I have added to it the valuable analysis of the black earth by M. Payen, and have willmgly acceded to the request of my friend Mr. Pusey to publish it in the volumes of the Agricultural Society.] In previous communications respecting the geological structure of Russia in Europe, M. de Verneuil and myself gave a sketch of the superficial accumulations which are apparent in the northern governments of that empire. In conjunction with our associate. Count Keyserling, we shall revert to this subject, both with the view of adding to our former stock of knowledge that which has resulted from recent researches, and also to show in one con- nected memoir the relations of all the varied superficial demtus 126 On the Tchornoi Zem, of Russia. The object, in the mean time, of this short notice is to call attention to a superficial deposit which occurs at intervals over enormous tracts in central and eastern Russia, and which, from the uniformity of its colour and composition, is without parallel in Europe. Though Pallas and the older writers upon Russia have briefly noticed the occurrence of a black vegetable mould, they have neither described the extent of ground occupied by it, nor its composition ; still less have they speculated upon its probable origin. The Baron A. Von Meyendorf, my com- panion in a part of my first journey, in a letter to M. Elie de -Beaumont, has indeed spoken of this material as being one of the chief sources of the agricultural wealth of the empire. Having recently, however, had the opportunity, in company with M. de Verneuil and Count A. Keyserling, of tracing the relations of this black earth over wider tracts than perhaps any modern observer, I have thrown together a few remarks which may serve to explain, 1st, the range and extent of the deposit, and its relations to the physical features of the land ; 2ndly, its agri- cultural properties; 3rdly, its chemical composition; 4thly, the theory of its origin. 1 . The black earth has its northernmost limit defined by a waving line which, passing from near Kief and Tchernigof, a little to the south of Lichwin, appears in the 54° of N. lat. in that tract, then advances in its course eastward to the 57° of N. lat. and occupies the left bank of the Volga west of Tcheboksar, between Nijny Novogorod and Kasan. In approaching the Ural chain, we saw no black earth to the north of Kasan, but we observed it plentifully on the Kama and around Ufa. Again, on the Asiatic or Siberian side of the Ural mountains we travelled through one large oasis of it near Kamensk, south of the Issetz river in latitude 56° N., and through another, between Miask and Sviask. Of its limits in the great Siberian plains we cannot speak from personal observation, but v/e were given to understand that it spreads over a considerable area in the eastern and central parts of that region. Nor can we exactly define its southern limits in these eastern longitudes, for although we met with it occasionally in the gorges of the chain and in the Baschkir country on both flanks of the southern Ural, and also in the steppes of the Kirghis, \Ye cannot pretend to say if it extends far to the south of Orenburg. We know, however, that it is not to be seen in the flat southern steppes between that place and the mouth of the Volga which were traversed by us ; for there the sur- face is strewed with fine submarine detritus containing nume- rous shells of the same species as those which now inhabit the adjacent Caspian. Nor have we seen any black earth to the south of Tzaritzin on the Volga, or on the steppes of the Kal- or Blade Earth of Russia . 127 mucks between that place and the mouth of the Don ; nor indeed anywhere except in very limited patches along the sea of Azof, or in other words on the southern face of the axis of elevation between the Dnieper and the Don, which is a pro- longation of the Carpathian chain, and constitutes what is com- monly called the granitic Steppe. It occurs, however, in great thickness on the slopes and plateaux on the northern side of that axis, where, as it really surmounts the carboniferous limestone with many seams of coal, a geologist who had not observed it in other places might at first sight be led to suppose that the black matter was due to the decomposition of the subjacent carbonaceous strata.'" It lies, however, upon rocks of all ages, and the great masses are included in the central region thus roughly defined. Geologically considered, therefore, the Tchornoi Zem occupies the centre of a great trough as large as an European empire, having the detritus of the crystalline and older rocks for its northern and the low granitic steppes for its southern limits. It is found at all levels, sometimes on plateaux, as on the right bank of the Volga, high above the adjacent plains, in various paral- lels, from 56J-° N. lat. to the high grounds extending to Saratof, and at heights of not less than 400 feet above the valleys ; in other places on slopes and undulations, and often in broad valleys, where the rivers, having cut through the deposit, expose its thickness on their banks. In the country where the southern limits of the northern drift are traceable, it is interesting to observe that its materials, reduced to small size, are overlapped by the black earth. I may here remark, that on the plateaux and their sides, the black earth, like all the other alluvia of Russia, is constantly cut into by the ravines, called '•' avrachs " or '" baltas " by the Russians, and which invariably show it to be the uppermost deposit. These ravines have been mentioned in a former communication ; but the attention of English geologists cannot be too frequently called to them, as the rapidity with which they are laid open after the ground has once begun to yawn, is something quite surprising to those who have been accustomed only to survey the trodden tracts of Europe and other parts of the world. Central Russia, indeed, may be described as consisting, to a very great extent, of a series of undulations, composed of incohe- rent materials, or, in other words, as a country so devoid of a visible skeleton or framework, that the vast increment of clay, sand, or mud, which occupies her surface, is easily denuded when * These coal-fields have since been described in the account of the gene- ral structure of central and southern Russia, communicated by myself and companions to th« Geological Society of London. 128 On the Tchonioi Zem, any adequate cause is brou^rht into play. The opening or fissuring of these masses, then, is due, in the first place, to an extreme climate, which subjects the surface to intense and long droughts, alternating with heavy debacles, arising from the melting of thick coverings of snow and ice. During the hot and parching summers the argillaceous grounds necessarily split into rents, and wherever these occur upon slopes, the thaw of the succeeding spring libe- rating vast bodies of snow and water, the smallest crack of the previous year is enlarged mto a gulley, which, widening as it descends, becomes in a few seasons a broad and deep ravine, through which the masses of melted snow, mud, sand, and clay are transported into the adjacent river. It is the conjunction, therefore, of the very incoherent nature of the upper deposits of Russia with the extremes of her climate which explains the form- ation of the innumerable ravines that fissure her surface. It would indeed be a curious problem to ascertain to what extent these ravines encroach annually upon the best arable and pasture grounds of the empire, and in what progression this waste takes place; as proved by the rapidly increasing deltas at the mouths of the Volga, Don, &c., and by the very perceptible silting up of the Sea of Azof. In no instance have I seen any means adopted to check this continual wear and tear, by which millions of tons of the richest soils are annually destroyed, and transported away by the great rivers. In the mean time, the geologist has to thank these *' avrachs " for most of his best sec- tions, for it is generally near their mouths, where the denudation has been deepest, that the parent- rock or true subsoil is laid bare. I may here also state, that it is owing to the ravined nature of the sides of the hills, and the wide mouths of these gullies, that the great roads of Russia pass almost invariably over the highest table-lands, where the "avrachs" are, comparatively speaking, absent. Instead of travelling along the banks of the great water- courses, as we might think would be the case by an inspection of a physical map, it has been found impossible to maintain roads along these lower levels, — first, from their being inundated during certain seasons ; and, secondly, by the innumerable mouths of the ravines, which defy all the efforts of bridge-makers, aud are for ever changing their courses and dimensions. Returning, however, from this allusion to a phenomenon which affects all the incoherent deposits of Russia, to our special subject, it must be clearly understood, that the black soil of which we are treating does not, by any means, occupy all the vast country in question. It occurs, indeed, in areas sometimes consisting of sev^eral large parishes, and is invariably the superior deposit, covering all other accumulations of clay, sand, 6cc. In thickness it \anes from a few feet to 15 or 1:0 feet. In travelling over or Black Earth of Russia. 129 these black tracts in the dry summer of last year, my companions and myself were often, during a whole day, more or less sur- rounded by a cloud of black dust arising from the dried up " Tchornoi Zem," which, even in rich grass countries, like those east of Odoyef, is of so subtle a nature as to rise up through the sod, under the stamp of the horse's feet, and form so dense a cloud, that on arriving at our station we were often amused at our chimney-sweep appearance.* '2. The " Tchornoi Zem" is unquestionably the finest soil in Russia, whether for the production of wheat or grass. It is so fertile as arable land, that the farmers never apply manure ; and, after taking many crops in succession, leave it fallow for a year or two, and then resume their scourging treatment. The natural productiveness of this soil has doubtless tended to confirm the prejudices of the peasants of Central Russia against the use of manure, enormous piles of which, the accumulation of ages, are seen behind most villages and towns, forming, between the houses and the river below them, hillocks of considerable magnitude, the export of which might really prove a very beneficial trade to those countries more advanced in agriculture, and whose poorer soils are worthless without repeated dressings of manure. In the mean time, however, it is right to state that well-educated Russian pro- prietors of such lands in Central Russia are now labouring hard to overcome the ignorance of their peasants, and have in some instances succeeded in inducing them to manure their fields; whilst in the northern governments, where the soil and climate are more adverse to the cultivator, improved agricultural habits are becoming prevalent, and in all the military and German colonies manure is regularly harrowed in, the culture being occa- sionally as clean as in some parts of Western Europe. In the central southern regions I may particularly cite M. Da- vidof, an extensive proprietor of black earth in the rich tract between Stavropol and Sysran, as one of the most spirited modern agriculturists. Educated in Scotland, where he acquired * Although it has been said that this black earth is unlike any superficial deposit in Europe, it is probable that the fine black earth of Hungary is merely a western limb of the great Russian accumulation. The " Tchornoi Zem " is indeed somewhat analogous in colour, uniformity of deposit, and fer- tilizing properties, to the " Regur " or cotton soil of the central (Deccan) and southern (Trichinopoly, &c.) districts of Hiudostan. In a memoir com- municated to the Royal Society, in 1837, by Lieut. Newbold, of the Madras Army, that otficer describes this Indian humus as being spread out in patches over wide tracts, and at all levels, and it is supposed by him to have been formed under water. In aspect, however, as well as in composition, the " Re- gur " differs from the " Tchornoi Zem " in not being so black, in containing much coarser grains of sand, and also calcareous (tufaceous) concretions, which are attributed by Mr. Newbold to springs rising from the subjacent rocks. VOL. III. K 130 On the Tchornoi Ztm, a taste for good farming, he is endeavouring, with the aid of his very intelligent agent, M. Brummer, and by the example of model farms, to lead the people to use manure and eat potatoes, a root generally al^horred by the Russian peasant. Turnips or other green rotation crops being also unknown in the interior of Russia, I have little doubt that, with an improved system like that proposed and put in practice by M. Davidof^ the agricul- tural products of Russia might be doubled. It is not in my power to give an exact return of the crop yielded by the black earth, nor can I refer my readers to Schnitzler's Statistics of Russia, without cautioning them against what I presume to be an error, when that author states, that in good seasons this black ground, in the government of Tambof, returns from 10 to 15 for 1, and in other years from 7 to 10 for 1.* With a knowledge of the treatment which this soil undergoes, such esti- mates must be overcharged, if viewed as average returns. More recentlv, indeed, the Baron A. von Meyendorf has prepared an useful statistical map, not yet published, in which the whole of Russia in Europe is divided into three regions — of forest, corn, and steppe. lie also states that the agricultural region affords 20,000,000 of hectares of wheat ; but I may observe, that the amount of this quantity which proceeds from the black earth cannot be known until its limits are defined. Nor would it have given a fair idea of the productiveness of this soil to have simply noted down the returns at this or that spot, where the plough had been long at work, and no manure used. The true test would be to show the amount of produce when the black earth is first changed from a state of steppe or grass to an arable condition. Eager as the Russian cultivator is to convert such lands, there are still very wide tracts of Southern and Eastern Russia, and on the flanks of the South Ural, where no plough has yet broken in upon this fine virgin soil, and where it still is loaded with the richest crops of grass. 3. Chemical composition. On fracturing a hardened lump * The mode of computing the fertility of a soil by the return from a given quantity of seed, which is commonly used by foreign writers, is very falla- cious, as it depends, in a great measure, on the quantity of seed sown on a given space. If a sack of wheat be sown broadcast on an acre of land, and the return be 5 quarters, this will be only 10 for 1 ; but if o pecks be dib- bled, and 5 quarters reaped, v.'hich is not uncommon, the return is no less than 32 for ] : yet the fertility of the soil is not in that proportion. In the rich black earth a smaller quantity of seed is required ; and, supposing 3 bushels sown per acre, an increase of 15 for 1 would only give 4 5 bushels — no very extraordinary crop for such land, in a climate peculiarly suited to the growth of wheat; and 10 for 1 would only be 30 bushels per acre — no very great average. There may, therefore, be no error in the statement of the return of the black soil of Tambof.— W, L. Rham. or Black Earth of Russia. 131 which I extracted six months ago from beneath 10 to 12 feet of subjacent similar earth, all jet black when moist, and which I had kneaded together to bring away, it offered in its dry state a slightly ferruginous brown tint ; and I further perceived that besides the black matrix, grains of lighter-coloured sand were interspersed. Having submitted a portion of this mass to Mr. R. Phillips, the Chemist of the Museum of Economic Geology, he has obligingly furnished me with this analysis: — Silica . . . .69-8 Alumina . . . .13*5 Lime . . . .1-6 Oxide of iron . . .7 Vegetable matter . . .6*4 Traces of humic acid, sulphuric acid, chlorine, &c. 1 '7 100 Dr. Daubeny, who has also interested himself in the examination of this black erirth, and has detected about the same proportion of organic matter as that noticed by Mr. Phillips, thus expresses himself: — '' The possession of a deep soil, easily penetrated by the roots of plants, and containing so large a per centage of mild humus, would alone impart great fertility." The celebrated French agricultural chemist, M. Payen, who analyzed a portion of this black earth at the request of M, de Verneuil, says : — ■ " The composition of this earth is remarkable for the propor- tion of azotised matter which it contains, and the volume of the azote. The connection between this earth and the organic sub- stance, when the latter is so rich in azote, appears to me to be essentially one of the surest indications of the fertility of soil, other conditions of chemical properties and mineral composition being favourable. In this respect, and according to my compared analyses, the earth in question approaches very near to two of the most fertile soils of France, that of the Limagne d' Auvergne (valley of the Upper Loire) and that of the neighbourhood of St. Denis, near Paris, notably in the farms of Marville and Stains. I have great pleasure in authorising Mr. Murchison to publish this analysis and the opinion I here express, and shall be much ho- noured if these details find a place in the Memoir of the Presi- dent of the Geological Society of London." ANALYSTS OF THE BLACK EARTH BY M. PAYEN. iro f f fi"05 Combustible organic matter rAlumine , P^I^ { 93 • 05 Incombustible j Soluble in ] Oxide of iron ot earth j matter = { boiling hydro- 13-755 1 Lime . . [ chloric acid J ] Magnesia . . Alkaline \ Chlorides) k2 5-04 5-62 • S2 0-98 1-21 132 On the Tchornoi Zt fSUica . . . 71-56 Insoluble in boil- ] I Alumina . . C"36 iiig hydrochloric >79' 30 j Lime (traces ofj acid J I Magnesia . . O'2-l or according to the quantities J Earth. Org. matter. Incombustible. 10*237 soluble. used in the analysis^ tl-724= 0- 119 -f 1-605 j 1-368 insoluble. After detailing the minute proportions of these soluble and insoluble contents, M. Payen adds, that the analysis of the combustible organic matter indicated the presence in 100 parts of the original earth, of . Water 4- 81 Azote 2-45 7-26 4- 140 grammes of the earth yielding 9* 498 cuhic centimetres of azotic gas. * In order to avoid error, not pretending myself to be acquainted with the method of analysis employed by M. Payen^ I here refer my readers to the original document, j * If we only consider the diemical elements of which this black earth, which is stated to be so fertile, is composed, the analysis does not afford us much information, without a knowledge of its mechanical texture. The same elementary substances may be so variously combined as to produce very different soils in respect to fertility. Thus, if 70 per cent, of silica were in the form of small crystals, such as we find in sea-sand, and the 13 per cent, of alumina combined with the 7 per cent, of iron and the sul- phuric acid were mechanically mixed with the sand, the result would be a soil not much superior to that of Bagshot Heath ; and although the 6 or 7 per cent, of organic matter, especially with a considerable portion of animal matter, would give it some fertility, it would never be fit for the growth of wheat, from a want of firmness. JBut if the alumina is combined with the silica, so as to form clay, and a portion of the silica only is in the form of fine sand, making with the clay a loamy soil, and the oxide of iron be a peroxide not hurtful to vegetation, then the organic matter intimately mixed with this soil will form the richest wheat-loam. This confirms an opinion I have ventured to express elsewhere — that, when the silica is in a very high state of division, and intimately blended with the alumina, it can no longer be considered as sand ; nor has it the porous quality by which sand is soon deprived of its moisture, and the organic matter is exhausted in it. This shows the necessity of a mechanical examination of a soil, which is so easily effected by sifting and washing alone, conjointly with an accurate chemical analysis, before we can form a correct opinion of the real fertility of a soil. — W. L. Rham. t Analyse de la Terre Noire de Russie, sur un C-chantillon transmis par M. Gourieff. Analyse. 6 • 95 mat. organique combustible. fAlumine . = 5-04 100 terre —I c< i 1 1 i t n i i Ox. de fer . = 5 '62 no A' 1 /Solubles dans lac. chloihvd. I ^, „ "^ 93-Ooceudres .{ , ;ii„.,^ _ lo.^n • < Chaux .= 0-82 Magnesie . = 0*98 Chls. alcals. = 1-21 rSilice . . = 71-56 [nsolubles dausTac. chlorhyd.j Alumine . = 0-36 bouillant = 79-o0 j Chaux (traces). iMagnesie . = 0-24 Ou d'apres les quantites employees pour I'analyse 1 -721 10- 237 soluble, terre = 0-119 mat. org. + 1-605 ceudre = . , j 1-308 insoluble. bouillant s= 13-79 or Black Earth of Russia. 133 Whilst the analyses of these able chemists afford us nearly the same results as to the proportions of solid materials, we learn from M. Pay en that the peculiar gaseous contents of the black earth may be the principal cause of its fertility. It would seem, indeed, that without a close attention to the proportion, not only of the soluble and insoluble constituents of soils, but also to their gaseous contents and their mechanical aggregation, it must be very difficult to estimate their fertilizing powers. Thus, in looking through the various British soils analyzed by Mr. R. Phillips, I find that a red, brick-coloured earth, already alluded to, from a property of Lord Calthorpe, (as dissimilar as possible in aspect and aggregation from the Tchornoi Zem of Russia, and differing also from it, I will venture to say, in produce,) has almost to minute quantities the same relative proportions of sand, clay, iron, and vegetable matter ; though the Russian earth is black, perme- able, and easily managed, and the English earth is red and tena- cious. Again, we see by the comparisons of M. Payen with what very different soils in France he compares the Tchornoi Zem of Russia. 4. When we speculate on the probable origin of the Tchornoi Zem, the first impression might be that which the Baron A. von Meyendorf adopted in a letter to M. Elie de Beaumont, and which is indeed the prevalent opinion in Russia, viz. that it is the humus arising from decayed forests or vegetables. But I am obliged to dissent from this opinion, seeing the uniform nature of the soil and its distribution at all levels without reference to the existing drainage ; and also from the fact, that in no part of the empire did my associates or myself ever perceive a trace of trees, roots, or vegetable fibre in the black mass. It is in vain to say Mat. soluble dans ac. chlorbyd, boitillaut = Alumine .... Ox. de fer . Sulfte. chx. = 0-036 1 = cbaux . . .j Magnesie .... Chlorures alcals. . 0-237 Per 100. 0-087 0-097 36-70 40-91 0-014 9-90 0-017 10-021 7-17 8-86 Mat. insoluble ac. chlorbyd. bouillaut = Sillce . Alumine Chaux Magnesie 1-368 Per 100. 1-232 90-24 0-110 8-03 traces. 0-008 I 0-90 DOSAGE DE L AZOTE. Donnees. Mat. employee = 4-110 Pression = Temperat. = 76-94 19<: c^^ 9<^« 9 Mis vide Perte 9- 190) eau per cent. 0-29Uf = 4-81 A incinerer = 1 - 724 1 cendre per cent. Cendres(rcuges)= 1-609J =93-09 Restcltais. Mat. normale employee = '4*140 „ seche = 3-940 ,, organique pure = 0-279 Vol. reel, de Fazote = 9c''498 Poids „ = 6i^ e 861 azote { Mat. normale = 1 • 66 „ seche = 1-74 „ pure = 24-99 pour 1000 134 On the Tclwrnoi Zcm, that such vegetables may have been entirely decomposed ; for in the deep denudations which expose 15 to 20 feet of this matter, surely some remains of the forests or bogs would be found in the lowest parts of the solid earth, just as we find roots and branches of oak, pine, birch, and hazel in our peat bogs. But if, for these reasons, it be impossible to adopt the hypothesis of simple terrestrial origin, and that we consider it a subaqueous deposit, with what known accumulation shall we compare the black earth? Having referred to some of the difficulties which are to be over- come before the practical farmer can avail himself of the lesson which is offered to him in the crucible of the chemist, I will (claiming the forbearance of agriculturists) say a few w^ords on the geological relations of this Russian earth, and conclude with an attempt to explain the cause of its colour. With what known superficial deposit, then, are we to compare it? Is it to be placed in parallel with the equally finely levigated silt which the Ger- mans call Loss, or with the upper diluvial mud which in Belgium, France, and Germany is said to bound the northern drift? Though this comparison is made by M. A. Erman, and has been alluded to by the eminent geologist M. E. de Beaumont, I do not conceive that it can be sustained. With the ordinary diluvial or drift clay the black earth has, indeed, nothing in common; for it does not contain a single transported pebble. Besides, it overlaps, and is never mixed with, that drift which occupies such large tracts of northern Russia. Again, the composition of the ''Tchornoi Zem" is most distinct from the Loss of Germany, which light-coloured, sandy, calcareous mass is abundantly filled with terrestrial and lacustrine shells in perfect preservation, clearly indicating that it was accumulated on the sides of an- cient, wide, lacustrine rivers, which were barred up so as to form lakes in the way described by Mr. Lyell, just before the present configuration of the land was completed. The fact, also, that the Loss has not yet been seen on high plateaux, but occu- pies the sides and bottoms of the great valleys in which rivers flow, is in itself sufficient to prove that, although it may have been accumulated at nearly the same epoch, it cannot be considered as the exact equivalent of the " Tchornoi Zem," which contains no terrestrial and fluviatile remains, and is found at all levels without any relation to the existing water-courses. Debarred, by the absence of any. portions of plants in its com- position, from referring it to the decay of ancient forests, and unable to compare it with any known deposit, from the absence of all organic remains, let us see whether the very peculiar nature of the physical, geographical, and geological conditions of Russia may not help us to a solution of the problem. or Black Earth of Russia. 135 Unlike all great regions hitherto examined^ central Russia is void of rocks of igneous origin or intrusive character^ and all her strata deviate from horizontality only by the slightest undulations. From this fact and from the incoherent texture of the rocks it is clear that her subsoil, which on account of its marine contents we know to have been formed under the sea, must have been raised and desiccated by very gradual and even movements. Judging from the evidences of geological succession also^, and seeing that, without the aid of great fractures or dislocations in the crust of the earth, some of the older rocks of Russia, such as the moun- tain limestone, are covered conformably by the inferior oolite, whilst the lias and, to a great extent, the new red sandstone are wanting, we see in these facts the proofs that either the former bottom of the sea was raised above the waters and remained dry for long periods, or that, in this very tranquil region of the earth's surface, the absence of all widely-spreading powerful currents ceased, at intervals, to extend from the neighbouring seas and rivers. Pursuing this mode of reasoning from the more ancient phenomena to those which immediately preceded our own era, we are led by positive evidence to conclude that the whole surface of central Russia (however parts of it may have had formerly di- viding barriers) was during that period again depressed beneath the level of the sea, in which the marine shells of the government of Archangel and the Southern Steppes were accumulated, and over which the sand, clavj, pebbles, and blocks of the north, as we have before described, were deposited. In all those parts where the strata show no signs of dislocation, the present physical features of the country, indeed, serve to explain the outline of the southern edge or extreme range of the northern drift ; for where high plateaux, like those on the left bank of the Volga between Nijny Novogorod and Kasan, stand out with their cliffs to the north, there we trace a well-defined limit beyond which that drift has not proceeded ; and where, on the contrary, longitudinal valleys, like that of the Okka, open to the south, there we perceive that northern blocks have advanced from 50 to 150 miles farther. In no part, however, of the great northern region occupied by the northern drift is there a trace of the " Tchornoi Zem," though yellow and white sands and stiff clays abound, the latter constantly charged with transported pebbles like our English drift or diluvium. Extending then as far southwards as currents, icebergs, and other causes, to which I have formerly referred, would transport them, and a submarine outline would permit the materials to advance, it is very natural to suppose that, where the northern drift ceased to advance, the bottom of the then sea, far removed from any currents, or unagitated by any disturbing force, would 136 On the Tchormi Zem. become covered with fine silt or mud, such as we know, from the soundincrs of hydrographers, is often found beneath mediterranean waters, far removed from the action of currents. The absence of any marine shells in this fine sediment is, it is true, a negative fact, which, if unaccompanied by some explana- tion, might indispose my readers to admit this hypothesis. We must, however, bear in mind that, after their emersion, the central parts of Russia, if but slowly and slightly elevated, may have long remained in an intermediate state of mire or slough with little egress for water ; so that the remains of deli- cate testacea (if they existed) may have been entirely decom- posed by the alternations of aqueous and atmospheric agency. But whether we adopt this view or not, we cannot, I repeat, look at the very great uniformity of its composition over such vast tracts, and its independence of existing drainage, without rejecting any theory Avhich would account for the production of the " Tchornoi Zem " by subaerial causes only, and on these grounds w^e must, I think, account for its origin by aqueous deposit and the subsequent modifications which it underwent in passing into a terrestrial condition. Lastly, 1 am borne out in this inference by the black colour of the soil ; for whilst the eminent chemists above cited ha\'e ascer- tained that soils of very different external appearance are nearly identical in their analysis with the black earth of Russia, the re- maining difference, or that of colour, may be due in the English and French examples to the vegetable matter being less decom- posed than in the case of the "Tchornoi Zem," an argument I beg leave to adduce as an additional proof of the materials having been originally deposited under water. XII. — Lecttire on the Application of Science to Agriculture. Delivered before the Members of the Royal Agricultural Society of England, on Thursday the 9th of December, 1841. By Charles Daubeny, M.D., F.R.S., Hon. Mem. of the R. E. Agricultural Society, Vice-President of the Geological Society, and Professor of Rural Economy in the University of Oxford. In acceding to the request made to me a few days ago on the part of the Council of the Royal Agricultural Society through their President, and attempting, in conformity with their wishes, to deliver before the farmers now assembled in the miCtropolis a lecture on some subject connected with the class of pursuits On the j^pjjlication of Science to Agriculture. 137 which this Institution is designed to foster, it may doubtless appear to many of you that I have undertaken a task, and am occupying a position, which neither my previous studies nor my present occupations justify me in assuming. For one indeed like myself, whose personal experience on matters of rural economy is nearly limited to the narrow precincts of a garden, to attempt instructing such an Assembly as the present on the conduct of operations with which many of those who constitute it have been familiar from their earliest years, and which in every case must form the subject of their daily thoughts and occupations, I should indeed regard as the extreme of presumption, were it not for the reflection, that the Society before which I now appear is expressly instituted for the purpose of connecting science with practice, and of summoning to the support of the agriculture of this country all the supplementary aid which either geology, botany, or chemistry may be capable of affording it. As, therefore, on the former evening, you listened with in- terest to a Professor of a sister University, when discoursing on subjects respecting which his own exact botanical knowledge, and his general acquaintance with the proper methods of experiment- ing, enabled him, though not a practical farmer, to speak with something Kke authority — so, on the present, it shall be my humble endeavour to bring under your consideration those de- partments of agricultural inquiry, upon which the science of chemistry either has thrown, or seems likely to throw important light. Proceeding, however, in that cautious spirit which ought to be our guide in matters of such great practical moment, a spirit too which is expressly inculcated by the Society whose members I now address, it is not my intention to prescribe to you any parti- cular modes of culture, even in cases where I may conceive that the present system runs counter to approved principles of science — but I would rather wish to suggest doubts, to pave the way to new lines of investigation, and to point out the manner in which those experiments which you are undertaking ought to be prose- cuted, so as to produce results most useful to the public and to yourselves. Few, indeed, who recollect the opposite systems of farming pursued in various parts of England, often without any corre- sponding variations in soil and climate to account for them, who consider the unequal amount of produce obtained from land of apparently similar quality in different situations, and are re- minded of the superiority in certain points of husbandry which must be conceded to nations inferior to our own in the scale of civilisation, will doubt that the agriculture of this country is far indeed removed from perfection ; and as no fault can be found 138 On the Aj^jdicatlon with the industry, the dihgent attention, the dnergy which per- vades the agricultural, no less than every other portion of the British people, the most promising direction in which we may hope to attain improvement is by arriving at more enlightened views with respect to the principles of husbandry, a more thorough understanding, of the nature of the soil we operate upon, and of the agents by which its condition is to be ameliorated. It must be admitted, indeed, that there Avas at no period of our history a greater disposition for making trial of new methods of culture ; and, moreover, that the experiments most popular at the present time are precisely those which have reference to the action of chemical agents upon the soil. But, judging from those cases which have fallen under my own personal observation, I should be led to apprehend, that the unscientific manner in which the investigations are oftentimes conducted, and the absence of any leading principle in the selection of these fertilising agents, or in their relative order of succession, have hitherto detracted much from the value of the results obtained. I may be permitted perhaps to illustrate my meaning by re- ference to another practical science, bearing some points of ana- logy to that which we are now considering. Let us suppose a physician, without being directed by any insight into the structure and functions of the human frame, or into the chemical nature of the drugs employed in medicine, to prescribe to his patients in- discriminately the various articles of the ' Materia Medica ' in succession, either singly or intermixed, noting down the results, and communicating from time to time to the world the cases in which he had fancied himself successful. Such a person, supposing his practice sufficiently extensive to enable him to ring all the changes of which the numerous medicinal agents at his command admitted, might no doubt in time discover some valuable remedies, provided only he were able to convey to others a correct idea of the nature of the ailments, and of the kind of constitutions, in which each particular mode of treatment had proved successful. But supposing that the nomenclature of disease at the period in which he lived was loose and uncertain, supposing that what was called fever in one place was known by some different appellation in another, I fear it would be difficult for him to render the in- formation he had acquired available, except perhaps to those wdthin the narrow limits of his own neighbourhood. His dis- coveries, therefore, must either die with himself, or, if adopted by others, must be expected to lead to many disappointments, from the mistakes that would occur as to the kinds of disorder they had been found calculated to remove. Now the present condition of agriculture does, I fear, in both these respects, resemble that which I have just been delineating ; of Science to Agriciiltitrc. 139 there is no lack, iudeed, of diligent and active prescribers, or of new recipes for improving the constitution and remedying the defects of the soil : but inasmuch as they have been tried, like the nostrums of the empiric, v/ithout any directing principle, we know not how to adapt them to the altered chxumstances of the land ; Avhilst, owing to the want of an exact nomenclature, cal- culated to serve as an universal language, wherewith to express the character of our soils, we are even disappointed in applying them where the circumstances are conceived to be the same. Professor Henslow has already, in his lecture of yesterday, remarked the vague sense in which many terms are used by husbandmen, no less than the difference in their acceptation amongst this class of persons from that which they are commonly understood to imply ; and it must be confessed that what he has pointed out as a defect in agricultural language in general, is applicable to the nomenclature of soils more particularly. Thus any loose clay is called marl in some parts of England, and loam in others ; whilst the latter term is interpreted by one person to mean a fat earth, and by another is defined to be a mixture of clay, calcareous earth, and sand, without the propor- tions being stated. " On referring to books on husbandry" (says Sir G. Sinclair), ''we are directed to a hazel-loam, a brown-loam, a clayey-loam, or to a humid sandy soil, garden mould, &c. ; but, owing to the perplexity arising out of the want of proper definitions, we find it utterly impracticable to determine what kind of soil is meant ; so that, of fifty different kinds I have myself examined in various parts of the kingdom, those under the same name appeared to differ greatly in their respective qualities." I will therefore proj)ose to the adoption of agriculturists, as a preliminary step, a system of classifying soils, founded expressly and entirely upon the relative proportion of their prevailing in- gredients — namely, that of the siliceous, the argillaceous, and calcareous earth present in them. In the arrangement now offered for your consideration,* we will begin with those soils which contain little or no calcareous matter — at the outside, not so much as 5 per cent, of the whole mass. These, supposing them to possess 50 per cent, of clay, are placed under the head of argillaceous soils, and are distinguished into two orders, the first wholly destitute of lime, the second con- taining less than 5 per cent, of that earth. Each of these orders are then subdivided into three species, distinguished as rich, poor, and intermediate, accordmg to the proportion of humus or * See Table I. 140 On the Application vegetable mould present in them. If the amount of this ingre- dient be not more than J per cent, the soils are called poor, as the fertility of a soil is in all cases greatly influenced by the proportion of this ingredient ; if it varies from 0*5 to 1*5 per cent., it is called intermediate; if from 1 • 5 to 5*0 per cent., it is distinguished as rich. The second class of soils comprehends those which contain from 30 to 50 per cent, of clay, and is denominated loamy. These likewise are divided into two orders, the one with, the other V, ithout lime ; and again into three species, according to the pro- portion of vegetable mould present in them. The third class embraces those soils which contain not more than 30 nor less than 20 per cent, of clay. They are called sandy loams, and are subdivided into orders and species, on the same principle as before. In the next, or fourth class, under the denomination of loamy lands, are ranged those soils which contain from 10 to 20 per cent, of clay : the remainder, with the exception of the small per centage of limestone and hum.us they may contain, consisting of sand. The fifth class, designated as sandy, includes all those soils in which the proportion of clay does not exceed 10 per cent.; and here again the same subdivisions are adopted. Hitherto, the amount of calcareous matter present is not sup- posed to exceed 5 per cent. ; but in the next class, that of marly soils, the above ingredient ranges in a proportion varying from 5 to 20 per cent, of the whole. Marly soils are to be distinguished into five orders, of which the first, called argillaceous, contains about 50 per cent, of clay ; the second, loamy, from 30 to 50 ; the third, sandy-loamy, from 20 to 30; the fourth, loamy-sandy, from 10 to 20 ; and the fifth is distinguished by the larger proportion of humus, which exceeds in quantity 5 per cent, of the whole, and is therefore denoted as humous marl ; which last is divided into three species — viz., argillaceous, which contains above 50 per cent, of clay ; loamy, which contains from 30 to 50 per cent. ; and sandy, possessing from 20 to 30 per cent, of the same ingredient. We next arrive at that class of soils which contains more than 20 per cent, of carbonate of lime, and which is therefore distin- guished as calcareous. These are subdivided according to the proportion of clay they may contain : when this earth exists in the proportion of more than 50 per cent., they are to be called argillaceous ; when it is from 30 to 50, loamy; when from 20 to SO, they are said to belong to the sandy loams of the calcareous class; when from 10 to 20, to the loamy sands; and when either destitute of clay altogether, or containing at most only 10 per cent, of it, they are called sandy. of Science to Agriculture. 141 Lastly, a calcareous soil which contains more than 5 per cent, of vegetable mould belongs to the sixth order, that of humous cal- careous soils, of which there are three species — namely, the argil- laceous, the loamy, and the sandy, characterised, as before, by the larger or smaller proportion of clay present in them. The last class, that of humous soils, is distinguished, in the first place, into three orders. The first consists of soluble mild humus — that is, of that description of vegetable mould which is in a fit condition to nourish the plants which grow in it ; the second, of acid humus, namely, containing a free acid, which by its presence is highly destructive to most kinds of vegetation. A third order consists of fibrous vegetable matter, such as peat, which, though not acid, is yet in a condition little fitted for imparting nourish- ment to plants. These orders are again subdivided into argil- laceous, loamy, and sandy, according to the proportion of clay present in them ; and lastly distinguished into two species, the one containing, the other destitute of calcareous matter. Such is the classification which has been proposed by a German writer,* and which appears to me to have the merit of embracing almost every variety of chemical composition found in nature amongst soils ; nor shall I make any apology for entering into this detailed explanation of it, as I conceive that, independently of its use in suggesting to us in what ingredients a given soil may be deficient, the advantage of being provided with a method of accurately defining the quality of any piece of land which has been made the subject of your experiments cannot but be appre- ciated by every practical farmer. But now the question occurs — in what manner is the requisite information to be obtained ? To a person altogether ignorant of chemistry the only method that presents itself is to depend upon the science of others, and to obtain an analysis of the soil from some competent authority; but as this, if adopted frequently, would prove both expensive and troublesome, it were very de- sirable if that limited amount of chemical knowledge could be diffused throughout the agricultural community which might enable each individual to determine for himself, in a rude way, the chemical constitution of the soils he cultivates. Certain easy directions for this purpose are given by the Rev. Mr. Rham, in the first Number of the Journal published by this Society ; and I am persuaded that by following his instructions every farmer would be enabled, if possessed of a slight elementary know- ledge of chemistry, to ascertain, after a little practice, the con- " Schlibler, in his work entitled " Grundsatze der Agricultur-Chemie." Leipsic, 1838. 142 On the Application stituents of his land, so far as to determine its proper place in our system of arrangement. Let me, however, remind you that such a rude analysis as I recommend tells you nothing respecting the presence or absence of many ingredients, which exist indeed in minute quantities in the soil, but which nevertheless occasion the most decided differences in its equalities as affecting vegetation. Such are the alkalies and the phosphoric acid, both of which necessarily escape detection whenever we examine such small quantities of the soil as usually are submitted to analysis. It is therefore no reflec- tion upon Sir H. Davy, in the last age, or on any chemist of the present, if, under such circumstances, he is silent as to the presence of these ingredients in the samples which he had under- taken to analyse.* If, therefore, information be sought on these points, larger portions of the soil must be sent, and a greater amount of chemical skill v^ill be called into requisition ; but where the object is merely to determine the sort of soil which exists on a given property, then a small quantity only need be examined, and a degree of science, such as would be easily attainable by most farmers, will suffice. Furnished, then, with this species of universal language, the agriculturist would be enabled to speak intelligibly, whenever he attempted to convey to others the results of his own experi- ments on the culture of land of a particular quality : he would then stand in the position occupied by a physician of a remote * Thus Sir C. Lemon last autumn expressed to me his surprise that a sample of the soil taken from the Serpentine of the Lizard was pronounced by Mr. R. Phillips, to whom it had been sent for examination, to be totally destitute of magnesia. I told him that I could myself state that no quan- tity of that earth considerable enough to be detected in a sample consisting of only a few hundred grains was present in it, having some time back executed a rough analysis of this soil. It would have been rash, however, to have concluded from this that magnesia was e7itirely absent, for ]\Ir. E. Solby has since informed me, that by operating on a much larger amount he has succeeded, not only in detecting ihe existence of the earth in ques- tion, but even of estimating the proportion it bears to the other ingredients. It has been remarked in the text, that phosphate of lime is another con- stituent of soils often overlooked, owing to the small quantity usually submitted to analysis. I may add, that several years ago I detected its presence in a great many specimens of secondary limestones in which Dr. Buckland had suspected the existence of coprolitic matter (one no doubt, but by no means the only source, from which it is derived). Within the last month I have been favoured by a letter from Mr. Schweitzer, the intelligent Director of the German Spa at Brighton, in which he states that he has discovered it in the proportion of one-thousandth part in the chalk of Brighton, and I have since found the phosphate in a somewhat larger quantity in the same formation, from the neighbourhood of Sudbury in Suffolk. of Science to Agriculture. 143 age, living at a period indeed at which the treatment of diseases was empirical, but at least possessing the means of conveying to others, by the aid of a precise system of nosology, a knowledge of the nature of the disorder for which a certain class of remedies had been found beneficial. But the adoption of a precise nomenclature, though an im- portant preliminary step, carries us after all but a small way towards that goal which the agriculturist should aim at attaining ; and he who is content with knowing what manures will suit his land, without troubling himself to ascertain the principle on which they act, is as far removed from a system of perfect hus- bandry, as the empiric of a former age is from the more enlightened practice of the present day. Why, for example, a method of culture, which has succeeded to admiration on one kind of land, appears inapplicable to another ; why a manure, which has pro- duced great crops the first year, seems to lose its effect on the next; or why the fertilising influence which it exerted when applied originally should be succeeded by the opposite effect at a later period ; w^hy a difference of season should cause an entire change in its effects upon the same land : these, and many other problems of the same description, we can only be said to be on the way to solve, when we have first settled amongst ourselves the principle upon which the substances applied to our land operate in improving it. At present the agricultural world seems divided on this point between two theories, both of them probably applicable to cer- tain cases, but nevertheless carefully to be distinguished as lead- ing to the greatest discrepancies in practice. The first of these considers manure as serving for food to plants : the latter regards them in some sense as stimulants to their vegetation. Here, however, as in the former instance, much confusion has arisen, in consequence of the term manure being applied to desig- nate two classes of agents essentially distinct. Thus some of the substances alluded to, such as quicklime, or its carbonate, act by improving the mechanical or chemical qualities of the soil and humus to which they are applied ; and to this operation the French term amendment of the soil would seem to be appropriate. Other manures, on the contrary, such as the dung of animals, exert a more direct influence upon the plants themselves ; and it is to these latter alone that either of the two theories alluded to can be considered applicable. Thus whilst the former class of manures communicates to the soil those qualities upon w^iich vigorous and active vegetation depends, the other may be supposed to supply the means for car- rying it on ; both of them conditions equally essential to the growth of plants, though each one perfectly distinct from the 144 On the Application ■ other — just as the nourishment of an animal depends both upon a healthy state of his organs of digestion and upon a due supply of nutritious aliment. There is, however^, a third description of manures every day coming more and more into vogue, which are by some considered to supply food, and by others regarded as acting in the capacity of stimulants to plants. To the latter class belong those various saline and earthy com- pounds, which a more extended acquaintance with chemistry, and an increased communication with foreign countries, have brought within the reach of the farmer : such, for example, as the nitrates of soda and of potass — the bone-earth, so extensively employed upon our turnip-fields — the gypsum, so useful on clover and grass land — and numerous other mineral substances, which will imme- diately occur to you. To ascertain in what manner these latter kinds of manure operate in fertilizing the soil is not, as some might suppose, a mere object of curiosity or of speculative interest, since its decision will afford us the means of determining the proper proportion in which to apply them, the kind of soils which will be most benefited by their addition, and many other points of an equally practical character. Whether these substances ever operate in any other manner, as, for example, as stimulants, may be afterwards discussed ; but that some of them at least are serviceable, by providing those con- stituents which the soil only contains, if at all, in limited quan- tities, cannot, I think, be disputed. With regard to bone-earth, which is now so extensively applied to the lands of this country, there can be no doubt that phosphate of lime, which constitutes its predominant ingredient, is secreted by the organs of a plant, and supplies the place of that which had been drawn from the soil by preceding crops. Its peculiar adaptation for turnips, which contain a larger per centage of phosphoric acid than any other of the ordinary crops of this country ; its usefulness on dairy-farms, where a great quantity of phosphate of lime is continually drawn from the soil in the form of butter and cheese sold off the estate ; and its serving to a certain extent as a substitute for farm-yard manure (the solid part of which consists in a great degree of this same substance), are circumstances all lending support to such an opinion. Now, with the view of taking advantage in our practice, as far as possible, of a theory which seems so plausible, as well as of testing its truth still further by the results of our experience, I conceive it would be a very useful exercise, if each agriculturist, besides entering in a book the amount per acre of the crops obtained, and of the different kinds of manure applied, were also to calculate the weight of Science to Agriculture. 145 of those solid ingredients contained in his crops, of which the soil possesses only a limited quantity ; as likewise the weight of the same which was present in the manure that had been added to them. But as an actual analysis of his crops, though by far the most accurate method of attaining such knowledge, would involve a degree of labour and science which few agriculturists could afford, it seems desirable that tables should be drawn up of the ingre- dients existing in all our ordinary crops, compiled from the best authorities that can be obtained. A specimen of such a table, which I have myself constructed for this purpose, stands now in the room under the title of " Agricultural Constants ;" * and on inspecting it you will immediately understand that it would be easy for the farmer to establish a system of scientific bookkeeping, by entering on the debtor side the materials that had been ab- stracted from the soil by his crops, and on the creditor side that restored to it by his manure : thus enabling him to ascertain whether his plan of farming has a tendency to enrich or to im- poverish his land. From this table it will appear that if an average crop of — Wheat be reckoned at 30 bushels, weighing 18001b will have abstracted from the soil Barley, 36 bushels = 1 ,900 lbs. Oats,' 30 do. 1,200 Potatoes, 6 tons 13,000 Turnips, 30 do. 33,000 C'--'{2::dX'"'"Td"'l= 2i at 1 ton per load Beans, 24 bushels, ' 1,200 lbs. Let us next illustrate this method of bookkeeping by reference to the Table now in the room, in which I have quoted the results given by Mr. Morton in his interesting work on soils, with re- spect to the system of husbandry pursued by him on Lord Ducie's example-farm at Tortworth. It will there be seen that, adopting his statements, there would have been abstracted per acre from the soil in six years — * See Table II., on the Constituents ofcertam crops, a title which I have adopted in preference to that given in the text, as the proportions of the ingredients are by no means cojistant, varying, within certain limits not yet defined, according to circumstances. , VOL. HI. ^ L Phosphoric Acid. lbs. oz. 7 3 4 13 5 3 24 6 3 3 8 146 On the Application 1st year, by mangel-wurzel, = 2nd do. wheat, 4 qrs. straw to do. 3rd do. 4th do. 5th do. 6th do. clover, oats, 7 qrs. straw to do. turnips, 25 tons wheat, 4 qrs. 30 tons 1900 lbs. . 3000 2600 3000 3000 1900 Total of phosphoric acid As 214—442—71—147, about = 147 lbs. of phosph losphonc A cid. lbs. oz. 11 1 7 9 1 12 3 10 2 1 12 36 5 7 9 71 10 1. lime. Added to ditto per acre during the same period 1st, The phosphate of lime present in the dung of cattle fed on the farm lbs. oz. 2ndly, Straw of the wheat . 1 12 , , oats . 112 quantity unknown. 3 8 3rdly, Fifteen bushels -of bone-dust at 56 lbs. pei bushel, consisting of — Animal matter Various salts, not phosphate Phosphate of lime 839 10 277 5 84 462 16 5 lbs. oz. 3 8 230 9 Total 242 8 Now it follows from this calculation, that Mr. Morton had added to his land, in the course of six years, more by 171 lbs. of phosphoric acid than had been taken off from it by the crops, even without reckoning that present in the dung of the sheep and cattle, the quantity of which is not ascertained : so that it would appear, either that a much smaller amount of bone earth would have answered as well, or that some other purpose besides that of supplying the crop with phosphoric acid is fulfilled by it. It must evidently be of the highest importance to determine which of these two be the true statement, since, if the former should turn out correct, then an unnecessary expenditure of an expensive material has been incurred; and if the latter be esta- blished, its recognition might lead us to discover some other material by wdiich this secondary object could be more effectually attained. Amongst many other suggestions that may occur to us from having such tables constantly before our eyes, there is one to which I shall advert, inasmuch as it bears relation to certain of Science to Agriculture. I4f points of theory recently introduced^ and pregnant with some most important applications to practice. Upon turning to the Table of Agricultural Constants you will perceive, that whilst an average crop of turnips, if estimated at 25 tons, contains 24 lbs. of phosphoric acid, one of wheat, con- sisting of 1800 lbs., will contain only 7 lbs. 3 ozs. of that ingre- dient ; and yet that, on examining the per centage of nitrogen, its proportion in either case will appear to approach nearly to an equality : that present in the crop of wheat being about 4J lbs. ; and in the crop of turnips, 5Jlbs. Now the interesting researches of Professor Liebig, with which I presume the agricultural world is by this time familiar, and upon which, moreover, I am unwilling here to dwell, as they have already formed the subject of one of my former lectures, reprinted in a late Number of this Society's Journal — these re- searches, I say, seem to have rendered it probable that nitrogen cannot be secreted by plants directly from the atmosphere. I am aware, indeed, that the French chemist, Boussingault, was led to the opposite conclusion, from experiments made by him upon the Jerusalem Artichoke ; but the nitrogen which this vegetable appeared to have drawn from the air may, I conceive, have been derived from the ammonia which rain-water always contains, and which vegetable mould holds in a condensed state within its pores. If this be admitted, it will then follow, that nitrogen, in order to furnish food to plants, must always have been previously combined with some other element, by which that tendency to assume an elastic state, which would prevent its assimilation, may be controlled. Hence the dependence of a productive wheat-crop upon an abundant supply of animal manure, which, by disengaging am- monia, affords it this necessary element in a fit condition to undergo absorption ; and hence the superior efficacy of liquid manure over every other kind, as it disengages a larger amount of the volatile alkali. By reference to the Table now standing in the room,* it will be * The Table is extracted from one given by Hermbstoedl, in the ' Annalen der Landwirthschaft,' vol. xxii., Part I., and is as follows : — 100 parts of wheat, in soil manured with — Human urine (dried) Bullock's blood (dried) . Human fgeces (dried) Sheep's dung . Pigeon's dung , . Cow's dung . Vegetable humus Same, but not manured . Contained of Gluten. Starch. 35-1 . 39-1 34-2 . 41-3 33-1 . 41-4 22-9 . 42-8 12-2 . 63-2 12-0 . 62-3 9-6 . 55-9 9.2 . G6'7 L 2 148 On the ylpjj/icatlon seen, that the proportion of g-luten to starch, as well as the aggre- gate amount of the crop itself, is augmented by manuring the soil with those materials which are richest in ammonia, such, for in- stance, as blood, pigeons' dung, &c. Now the practical inference I would deduce from this is, first, that it must be of the highest possible importance to preserve in tanks, or at least to detain, by the admixture of absorbent ma- terials, the liquid manure which is so often allowed to run to waste on your dunghills ; and, secondly, that it might be worth trying whether a better distribution of the manure at the disposal of the farmer might not be made, by adding the solid portion of his dung-heap, which is richest in the phosphates, to the turnip crop, and reserving the drainings, to be scattered, after the Bel- gian fashion^ in water-carts, over the ground intended for his wheat. May not this also serve to explain, why the nitrates of soda and of potass are in general found to be less serviceable to the turnip crop than to the cereal and other grasses ? Whatever other function these salts may discharge in agricul- ture, there is one at least which will probably not be denied to them, that, I mean, of furnishing an abundant supply of nitrogen to the crop. This arises from the decomposition of their nitric acid by the organs of the plant through the agency of light; and as it requnes a greater expenditure of chemical force to resolve into its elements a compound so stable as nitric acid than to effect the same with ammonia, we may understand why the influence of these manures should be so capricious in climates like our own, where the solar intensity is often interrupted ; and why Nature has provided that the products of animal decay should present themselves most commonly, in the form of nitric acid in hot countries, and in that of ammonia in cold ones. Now it appears from some recent researches of M. Pay en, in France,* that the rudiment of every vegetable tissue, the sub- stance ])rimarily produced in all instances during the development of the seed or bud, is a matter containing azote, and having some resemblance to the material which constitutes the muscular fibre of animals. Access, therefore, to a certahi amount of nitrogen is a necessary condition for incipient vegetation ; and a supply of animal manure, or of some substitute for it, such as the nitric salts, must clearly be indispensable for the rapid development of every kind of plant. But it is equally manifest, that if a manure rich in nitrogen merely " In the cambium, preceding the formation of the vegetable, appears first a granular contractile substance, containing azote. It fills the cells, the membranes of which are composed of carbon, oxvgen, and hydrogen only."— Comptes Rendu.s 1839, vol. ii., p. 3Q9. of Science to Agriculture. 149 be presented to a crop which, like the turnip, contains a large per centage of phosphoric acid, the growth of the latter may be checked, from its inability to obtain from the ground alone the requisite supply of this ingredient, whereas the grasses, which take up so much less of it, may find enough for their purpose in the soil, and therefore continue unarrested in their growth. And this I take to afford the true explanation of the fact ob- served, that certain manures act more efficiently when first applied than they are found to do subsequently, a result which matter- of-fact persons are contented to express by the phrase that the ground is tired of a certain kind of dressing ; and which those amongst them who indulge in theory account for by saying, that, like other stimulants, they lose their influence by repetition. Now I am ready to admit that these manures, besides supply- ing the plant v/ith nutriment, may exert an influence upon its development, of a description which it is, perhaps, necessary to denominate a stimulating one, until a more appropriate term shall have been proposed. This has been clearly explained by Professor Johnston of Dur- ham, in one of his recently published lectures,* where he shows, for example, by an appeal to actual experiment, that if two equal portions of the same grass or corn field in early spring be mea- sured off, and one of them be top-dressed with nitrate of soda, or v/ith saltpetre, the v/eight of nitrogen contained in the crop of hay or corn reaped from the latter v/ill generally be found to exceed that contained in the crop from the former, by a quantity much greater than that which was present in the nitrate with which the field had been dressed. It seems to me, therefore, probable, that the fuller and more rapid development of the organs of the plant, which was occasioned by the exuberant supply of nitrogen derived from the manure, had enabled the living tissue to draw, from the atmosphere, and from the rain-water in contact with its roots, a larger amount of nitrogen than it v/ould otherwise be ca- pable of deriving from the same sources : just as an animal, which, during its infancy, has thriven on a liberal supply of Avholesome and generous food, if it should afterwards be confined for a time to meagre diet, will extract more support from such materials than another would do, whose organs of digestion had been already enfeebled by a course of abstinence or depletion. But in whatever sense we choose to interpret the so-called stimulating influence of certain manures, it is obviously pursuing a mistaken analogy to consider the falling off of their efficacy after repetition as a case at all parallel to that insensibility to * See Johnston's Lectures on Agricultural Chemistry and Geology. 150 On the Apjylicatlon stimuli which animals acquire, from their continued use : for to imagine the soil, an inert mass, susceptible of such an influence, is obviously absurd ; and inasmuch as every successive crop grown upon the land consists of an assemblage of new individuals, it seems no less so to imagine that a given stimulus can in any respect operate less energetically upon it, in consequence merely of its having been applied to the crop of the year antecedent. In many of the cases in which, in the language of husband- men, the soil is said to tire of a particular species of manure, the phenomenon may, I think, be readily explained, from the ground being already surcharged with the material which the latter was calculated to afford, as under such circumstances no benefit can be expected to accrue from a more liberal supply of it. Thus, bone-dust, after producing great returns on its first ap- plication, seems frequently to lose all effect afterwards : in which case, however, it may be said that the ground remains benefited from the effect of the first year's dressing, and is only not further improved by the subsequent application of the same manure. But, in other instances, it has been asserted, that the land, after appearing to reap great immediate benefit from a certain kind of fertiliser — as, for example, from the nitrates — is left by it after- wards in even a worse condition than it was in previously. Now this effect may, I think, become intelligible, if we only recollect, that the different ingredients which each plant contains must be secreted in relative proportions one to the other, so that an in- creased absorption of any one will produce a larger demand for all the rest. Hence we may suppose, that the exuberant supply of nitrogen furnished by these salts had caused the organs of the plant to secrete so much larger an amount of the earthy phosphates, of the alkalies, &c., of which there is only a limited proportion present, that the crop of the succeeding year became stunted by reason of the soil being no longer able to afford to it, in adequate quan- tities, these essential elements of its constitution. And if this be the true account of the matter, the practical inference would seem to be that, instead of abandoning the use of the nitrates altoge- ther, as the theory I have been combatting would suggest, it should be our endeavour to supply those other ingredients which are deficient, by the addition, at intermediate periods, of bone- earth or of wood-ashes, in proportions adequate to the demand for them, occasioned by the expected increase of crop. FortunateU^ we are provided, in the dung of animals, with a species of manure of which the land never can be said to tire ; and for this snnple reason, that it contains within itself not one alone, but all the ingredients which plants require for their nutrition. of Science to Agriculture. 151 ancl^ what is perhaps of equal importance, existing too in that precise condition in which they are most readily taken in and assimilated. Where this material is sufficiently cheap and abundant, other kinds of manure may for the most part be dispensed with ; but as in certain stages of society the amount of animal life increases throughout a given region in a greater ratio than the fixation of gaseous matters which takes place through the instru- mentality of vegetables can proceed, and as the existence of large cities tends to disturb the balance which nature seems to aim at establishing between the quantities of food produced and con- sumed, by attracting into their vortices a large proportion of the corn and cattle that has been reared in the country, it is well that we have at our command, in the various mineral manures which science has brought to light, the means of supplying the defi- ciency. But, assuredly, the most effectual, as well as the most eco- nomical method of restoring the balance between the town and country would be to avail ourselves of that enormous accumu- lation of animal exuviee which the existence of a crowded city ne- cessarily occasions, and to convert that which is now n pabulum of disease into a source of life and abundance. As indeed the geologists of the present day cite as a proof of the ignorance or neglect of their predecessors, that the stone re- quired for the fortifications at Gibraltar was brought out from England, when it might have been obtained upon the very spot ; so I conceive our descendants will marvel at the inattention to chemical science evinced by the present generation of farmers, in exporting from distant regions, such as South America, substitutes, and those, perhaps, but imperfect ones, for that fertilizing material, of which the greater part is allowed to deposit itself unprofitably in the beds of our rivers. Not that I would by any means be supposed to discourage, under present circumstances, the importation of fertilizing ma- terials from abroad. Some of these, such as the Guano, lately introduced into this country from the islands of the Pacific, contain ammoniacal salts in a more concentrated form than any other known species of manure ; whilst others, such as bone-earth, comprise within a given compass a larger amount of phosphoric acid — hence their portability may give them advantages, by secur- ing greater economy of transport, in spite of the distance from whence they are brought : nor must we forget, that the measures for carrying off filth adopted in large cities are of a nature which would preclude us from obtaining it in sufficient quantity, in case that any great increase in the demand for it^ as a manure, should hereafter be created. 152 On the Application It is only, therefore, to the neglect of this material in places where it can be obtained cheaply and abundantly, that my obser- vations apply ; but they may at least serve to suggest to us the advantages of making all the use of it we can, and of endeavour- ing to reduce what we have in excess to a condition in which it may be conveniently transported to a distance. The means of preserving and rendering portable the night-soil and other impurities of a great metropolis, as well as the various expedients by which farm-yard manure may be applied to the best advantage, and its volatile parts either retained or slowly dis- engaged, as occasion may require, would alone afford us materials for another lecture — in the present I only allude to these topics as additional proofs of the advantages that would accrue, from having some amount of chemical knowledge diffused generally throughout the agricultural community. But how is this important point to be secured ? The present generation of farmers, living, as they often do, at a distance from the great emporiums of science, and being in all cases engrossed by the daily routine of practical avocations, can hardly find much time to devote to the acquisition of theoretical knowledge ; and of them all perhaps that can be .expected is, that they should arrive at a sense of its value, coupled with a desire, that those who follow their footsteps may possess that information in which they feel their own deficiency. It is to the rising generation that we must principally look for improving the practice of husbandry by a due attention to its jyrincijjles ; and this can only be brought about by instilling into the minds of those at least amongst their number who look for- ward to the management of large estates, either of their own or of others, the elements of physical science, at a period of life when the attention is most awake, and the thoughts unoccupied by more imperious duties. It is remarkable that, of all the nations of civilised Europe, England is perhaps the only one which is destitute of any public establishment for the instruction of those designed for agriculture, although two centuries ago the poet Cowley was alive to its im- portance, as, in one of his prose essays, he strongly recommends the erection of a College in each of our Universities, for the express purpose of educating those who were to be trained to husbandry in the several arts of aration, pasturage, gardening, and rural economy. In France the establishment of Grignon, near Paris, supplies means of instruction for more than a hundred pupils in the elements of physics, in chemistry, in botany, in other branches of natural history, and in the veterinary art. In the kingdom of Wirtemburg, that of Hohenheim near Stuttgard, to which is of Science to Acjricidhire, 153 assigned one of the royal palaces, provides a still more complete course of education of a similar kind. In Bavaria^ in Prussia, in Lombardy, and in the Tuscan territory, the respective govern- ments have evinced an equal solicitude for the same end ; and even Ireland has in this respect taken the start of ourselves by the foundation of a school of agriculture. In these and similar institutions theory goes hand in hand with experience, and the practical management of a farm alternates with, and illustrates the lectures of the professors. It is there- fore the more a matter for surprise, as well as of regret, that in this country, where the demands of a rapidly increasing popu- lation ou2fht to tax to the utmost the skill and invention of hus- bandmen, the student in agriculture finds himself often com- pelled, from the want of similar provisions of a public nature, to serve his apprenticeship in the art in parts of the country offering no facilities whatsoever for the acquisition of scientific knowledge. Should, however, as it may be hoped will happen, this glaring deficiency in our provisions for national instruction be hereafter sup- plied, we must not flatter ourselves that by its ineans the great body of those actively engaged in agriculture will acquire the leisure and science necessary for solving those many intricate problems that lie on the very threshold of agricultural chemistry. To determine, for example, in what precise manner the several artificial manures operate upon the crops ; by what agency and under what cir- cumstances the latter are enabled to decompose them, and how far one of them admits of being substituted for another, are tasks, each of which demands, not only a profound acquaintance with modern chemistry, but likewise a devotion of time and of attention not often compatible with active occupations. And whilst the wealthier agriculturist would be discouraged from the prosecution of such experiments by the above considerations, men of moderate means may also be precluded from undertaking them by the pecuniary sacrifices with which they would be necessarily attended. Considering, therefore, the great national importance of many of these inquiries; the immense increase in the produce of the country that would accrue from any discover}, however incon- siderable, in the principles of husbandry; and the difficulty of meeting in any one individual with that union of science, perse- verance, capital, and devotion, both of time and money, which such experiments involve ; the supplying means for carrying them into effect would seem to be precisely one of those objects, which should engage the attention of societies of men combined together with a view to the advancement of agriculture. It is on these grounds that I think much advantage would be 154 On the Aj^ipUcatmi derived from the establishment, under proper management, of an Experimental Farm — not that I would discourage the great body of farmers from making such experiments as they may feel them- selves equal to, or deny the necessity of repeating the same ope- rations on various kinds of land before their advantage can be regarded as sufficiently tested; but that I conceive there are many trains of research which will never be attempted, or, if attempted, will never be successfully carried out, without such an auxiliary. The foundation indeed of an experimental farm, under the auspices of this Society, or of more than one, if the zeal of the leading agriculturists could be sufficiently awakened to raise the requisite funds, has been long and anxiously desired by many persons of great practical experience in agricultural matters ;"^' and I cannot but think that if each of them were conducted by an ex- perienced supervisor, who should be expected to carry into effect the views and suggestions of such men of science as may have directed their attention to the theory of agriculture, those deficient links would shortly be supplied, which, even if considered in themselves unimportant, are nevertheless necessary parts of the chain which serves to connect our theory with our practice. If in juxtaposition with each of these establishments on which new methods of culture were tried, and the precise operation of the various manures worked out, there was founded a model or example farm for exhibiting the most approved system of hus- bandry now in use, every discovery that should be announced as having been brought to light at the former might undergo the further test of being repeated at the latter, before it received the iinal impress of the Society's sanction. And let it not be supposed that either the model-farms which are already instituted, or which may hereafter be set on foot under the auspices of any public Body, such, for instance, as the Society I am now addressing, could supersede or take the place of one designed for agricultural experiments. Since a model-farm, in order to serve as an example to the neighbourhood, must be conducted with a view to profit, all new schemes of cultivation which do not carry with them on their very face a reasonable probability of advantage must be necessarily rejected ; and yet, where the object is one of national and not of individual gain, the discovery of a single new fact would compen- sate for a hundred unsuccessful trials. If experiments are divided into those which produce fruit, and those which elicit light, it is * I may instance, in particular, Sir Francis Mackenzie of Gairloch, Bart., who has been urgent in his solicitations, first to the Highland Society, and since, as I understand, to the Royal Agricultnral Society of England, to establish Experimental Farms in both countries. of Science to Agriculture. 155 evident that the former only can be expected to meet with atten- tion on farms which are either in the hands of individuals, or which are intended as examples for their imitation ; but as the distinction made by Lord Bacon by no means implies that the latter class of experiments is barren, but only that the fruit they bear is of tardier growth, this Society could not be accused of losing sight of those practical ends for which it was instituted, if, in the spirit of the instructions of the great Restorer of Learning, it sought for experiments which afford light, even in preference to those which promise immediate profit. A Society like this, indeed, may be said to bear the same rela- tion to an individual Proprietor which the latter does to the Tenant at will ; and as the prospect of a remote and contingent advantage often stimulates the landlord to embark his capital and labour on improvements which the yearly occupant would reasonably shrink from engaging in ; so a still more far-sighted view of future benefit to the community, and a more enduring interest in the welfare of this mighty empire, may justify a Body of men like that to v/hich I now appeal in instituting experiments of a description such as few individuals could be induced to undertake. 15G Gu. thr ApplicaivM Agricultural Designations and general Relations with reference to their Produce.* /,a«rf ./ijr JFIieat and Spelt. The calcareous kinds not too rich in clay, and not too poor in sand and humus, give good returns. ^Mieat, spelt, barley, rape, beans, flax, and clover floiiri.sh in it especially. Those poor in humus are still suited for oats. lAindfor Barley. The soils which are rich in iiumus, and contain lime, are well suited even for wlieat and spelt, and often approach lu'arly to the foreiroing kinds. They are, moreover, suited lor Triticum dicoecnm? (Em- mer), one-grained wheat (Einkorn), rye, oats, rape (Keps), flax, and clover. Zanri /(;r 5a)7 L-j in coo o o o o o o o o o BBS >p O ip coo BBB c c c o U-: ..-5 3 coo o tn o < BBB BBS coo :-: ^; c: o' o c iii o o o :7 :t :■■> BBB coo coo coo BBB o o o coo BBB ceo 0- to 10 0- to 10 0- to 10 5 Sag = c s COO t c .2 .£■ c 1 o t i. 6 i |l| s t "5 o Poor . . . With Lime. < Intermediate Rich . . . s 1 i ■^3 1 Poor . . . Without Lime. < Intermediate 1 Rich . . . Poor . . . With Lime. J Intermediate Rich . . . III 12 3 "i ' • £ • III £ > 5 1 r: 1 [Poor . . . Argillaceous. < Intermediate iUich. . . III £ J 1. AuaiLLACKOrs Soils. Above 50 per cent, of Clay. More than 5 per cent. of Lime. 2. Loamy Soils. Not more than 50 nor less than 30 per cent, of Clay. Not more than 5 of Lime. o. Sanpy Loams. Not more than 30 nor less than 20 per cent. of Clay: Not more than 5 of Lime. 4. Loamy Sands. Not more than 20 nor less than 10 per cent, of Clay. Less than 5 per cent, of Lime. 5. Sani>y Soils. Not more than 10 per ^ cent, of Clay. Less than 5 per cent. of Lime. xri < of Science to AgncuUitre. 157 1 i 1 1 s a o i ri il a J The argillaceous soils often approacli in value to the argillace(ms m:irls ; the remaining orders of both | these classes eijually correspond one with the other : | to the most valuable belongs, as in the former case, the | liumous. Those wanting in humus require much i manure. Those rich iu clay are well suited for spelt and wheat; oats, Triticum dicoccum, lucern, and sainfoin thrive ia them. Their value is mucli decreased by containing an excess of lime. The value of these soils is greatly augmented by admixture with lime. Those which contain lime and clay are suited for wheat, spelt, barley, and oleaginous plants; the loamy and sandy are espe- cially adapted for oats, and in most places for wheat. The peaty and acid humous may be made fruitful by admixture with lime, sand, and clay. 1 1 1 1 1 ! 1 1 i I I I I [ I 111 1 I 1 a ^ .Sec o o o 1 1 1 1 1 1 1 1 1 1" - o o c o I^ o O O rH coo 0,^0 i = .- <1 O iCl o O A^ O 22S o o o 6 Ai o 222 O in o O Ah O 222 o in lO O O O Ah O 222 O lO O O Ah O 222 lO >o o O Ah o o o_o O O cp O lO o 1 ' ' <1 o o o o - - < o o o o o o o o O O rH O o rH a <=> ^ O O ,-1 O O rH O O rH O O rH o o o c« ■:-! c-j m o lo o lO m o o o W W CV) 222 o o o < o o o CM Ol W o o o (M W M ggg o o o §ss sss 2ls III OS/ 20 to 30. 20 to 30 20 to 30 o o o U2 2 o o o O »fS lO 222 222 o o o 222 o o o o o o 222 o o o o o o o o o ^22 2oo U 3 O tB2 !J ..2 n It 1^ 2 2 .2 >, Hi o ' a • be a *2 ■ i- • a • •^ Ul " il ° 2 '2 * n p •I- ill f m i III a S 2 ^ 2 in Insoluble carbon- ( Clayey . . ized or acid < Loamy . . Humus. 1 Sandy 1 ii Si ill 7. Calcareous Soils. Containing mor(! than\ 20 per cent, of Lime. 8. Husious Soils. Containing more thnn^ 5 percent, of Lime. 158 Oa the Application I H Z 5 < •siuaipoiSuj •otiuonio •pioy Duoiidsoqj •uoji JO apixQ •Buiraniv Ol CO W O O 00 «o o o — o •ppy o 1^ S2 ^?^ r- O 05 O ;s S ■^ M o 0^ CO CM .n CO o S ■^3U!S 1 i 00 .o — CD 11 CO o il" S §! 00 o O 1 CM => o o o JO apiXQ s '• O N o M : : : o o 00 1- : : t^ O Ci O O 00 lO «2 ■* 50 O O ^ CM •Bpos •ssc^oa {i O O S>1 O! OT o ^ o cv- o CO o o CM o o 1- c> 00 -o ^ C'X 1 ^ o •iiisouSej^ * ! 00 CO iO ^ o O 00 o ^ ^ •oraiq o CM '"' i'^< •uoqjBQ r?^ f2 fg O O O) C» O". o 1} JO • • a • • • s ic • -^ • . , o 3 •n > a • 2 • S • >.-' -s c 1 • S • o • &■ , • . • , . , , . . f-^-^ • • a • t"r>. r.^ « . . . . 2 " rt o ' * • s g . '% ?rll £ .d a II ^ >■ Ti rt c^ ^ to M r- f" M m P* ►Jo*' JO suoj OG ;noqB of Science to Agriculture. 159 O «D to (M O 1 00 M i t- o fi ■n rv. •am,ioiqo § IS to s CO 00 o ^ i o to to 'go •ppv oi.ioiidsoqj s ^g C5 .? ■* i o> 00 o O) i- o s ■ppV oi.inqdius ^ gg i o ■* 1^ s 2 i 2 O! 00 •li^UTS 1 o § o t- : : to : ^ : ; JO opiXQ 1 2 g o r, o C5 o i 1 00 1 1 •noil JO apixo CO **§ o - o 00 o - ^ o s - o •T3ixiumxv o CO CO 00 i OJ s s s 00 J^ C5 •BTsauSiJH 00 ii to CO 01 *- s 1 i CO o % o5 •auiti •sjuaipaiKiii paxi J jo pjox •SSTJ^OJ \i7 Ji ( == ■a^ozy •uoqjB3 puv ia^tJAi inB:^uo3 c • • • •2| o 'c3 as- een ied & • Ii -9 il) -3 eS "^ o-S p- S '^ 11 .§8 8 43 ^ V iJ fi.w S. S .2 s ^ 5 2-3-3 C.2 SJSO Sll s^ •^ rtiS Sell g-i§„ .S a S3 a > P S Q S o S .§5 2 2 r^S >» o 3 P5 S P^ JO '•sqtOOO'OOT ( 161 ) MISCELLANEOUS COMMUNICATIONS AND NOTICES. I. — Application of Blue Shale to the Surface of Land. To the Secretary. Sir, — Every one who has travelled through the coal districts must have observed immense accumulations near the pits of a blue clay-like substance brought up from the mines, called in the West Riding of Yorkshire ^^ Blue ShcUe.^' The rapidity with which this accumulates, in most instances, makes it inconvenient, and in time it becomes a great incumbrance. It is often burnt, and in that state is found useful for the growth of turnips drilled along with crushed bones ; but as the whole of the mass is to turn over before it will burn thoroughly, the burning of it becomes tedious and expensive. Having a farm, of which many parts are hilly and very thin of soil, without any bed of clay or marl near it, has compelled me to try many experiments to find a substitute for them, and having now some years' experience of the utility of applying this blue shale to the gravelly parts of my farm, I am induced by the success which has attended its appli- cation to submit my observations of one experiment (amongst many I have tried) to your Society to show that even this article, which is gene- rally considered not only useless but absolutely a nuisance, may become of value if applied to soils of a gravelly and sandy nature. The soil upon which I have tried it is that lying upon the magnesian limestone near Ferrybridge, proverbial for its natural poverty and in- ability to resist drought. Amongst the experiments I above mentioned I found a great advan- tage in applying the " Blue Shale " on my pastured seeds in autumn previous to ploughing them up for wheat to the extent of 12 two-horse cart-loads per acre. I invariably found it of great use, its effects being visible in the wheat crop, not only from the straw being stronger and longer, but the ear was much better filled and the grain plumper than in those parts of the field where it had not been applied, and its effects were very visible for several years afterwards.* That it wasof greatuse to my land, being thus ascertained, caused me to apply it more liberally ; and the result of one experiment of this liberal application I now lay before you. One of the fields of my farm had been considered for many years of so little value as not to be worth the trouble of cultivating it, and, from the grass-roots dying away in summer on the hilly parts, it was of no value when laid in grass. My predecessor in the farm had suffered this field to lie (once ploughed out of stubble) for several years, until it was * An instance is now visible where applied in 1 833 ; the field is now wheat, and where the shale was applied appears much more luxuriant. — May, 1842. VOL. III. M 162 Application of Blue Shale to the Surface of Land. overgrown with weeds, twitch, and thistles, which had shed their seeds for years unmolested. This field is 7 acres, exclusive of the fences, and consists of the sides, or rather the ends, of two steep hills facing east and west, with a valley between them. The hills take up about 5i acres, the valley the re- mainder. A great portion of the soil has been washed from the top and sides of the hills, and little has been left more than a mass of small gravel-like stones about 2 inches thick, on the top of about 4 inches of sandy soil. The substratum is yellowish calcareous sand,* called here marl, but a more inappropriate name could not be given to it — it is very porous ; the sides and tops of these hills in a dry season not supporting any vege- tation whatever to maturity excepting poppies. I entered to the occupation of this field in January, 1833, and, the spring being favourable, I was enabled to sow it with white Norfolk turnips in June, giving it 9 three-horse cart-loads of rotten manure per acre, and drilling in with the turnips a compost, made some weeks before, of 14 qrs. of crushed bones, half-inch, and their dust, 10 qrs. of kiln-dust, and 28 qrs. of fine ashes from weeds burnt. These turnips were a complete failure in every part except the valley (swealing away, to use a provincial term, both on the tops and sides of the hills), in which the crop was good, and eaten off with sheep. In 1834 sowed it with barley and small seeds for pasturing, giving it 12 bushels of rape- dust per acre — produce of the whole field, 11 qrs. 3 bushels of barley, or 13 bushels per acre. On the hills a great portion did not shoot into ear. In 1835 and 1836 pastured with sheep ; in October, 1836, solved it with wheat and rye (called here maslin) and 16 bushels of rape-dust per acre; 1837, wheat and rye — produce of the whole field, 9 qrs. 1 bushel, or 7| bushels per acre. Again the corn badly fed, and the rye scarcely having half-a-dozen grains in an ear. Being satisfied that giving this field the tillage I was doing, without its producing me some better crops, would not pay me, I determined to cover the hills with "blue shale," which in other parts of my farm I had found of use ; and commenced immediately after harvest, when the carting was good. I had to lead it about one-third of a mile ; and in the whole laid upon the hills 287 three-horse cart-loads, at a cost of 11/. 11j,, viz. — * I have attempted to improve my farm by an admixture of soils, and have found it by far the most certain way of making ferm.anent im-provenients. The calcareous sand here mentioned, which m the neighbourhood has been considered perfectly poisonous to plants, by mixing it liberally with the soil, I have found to contribute to a considerable increase of my crop. — C. C. This experiment is interesting, and may lead to others of a similar nature. The great advantage of a mixture of different earths, even of those which are barren in their nature, in improving the fertility of a soil, is as yet but little known. It is of no use to manure highly, until the texture of the soil and its power of absorbing and retain- ing moisture be ascertained ; and the earths which are the cause of the l)arrenuess of one soil, may greatly improve another of an opposite quality, when mixed with it. We know this to be the case with chalk and marl ; but much remains yet to be done by a mixture of gravel, sand, peat, clay, and decomposed rocks, and experiments on a moderate scale will throw much light on this subject. — W. L. Rham. £. s. d. y 2 8 6 12 8 5 £11 11 Application of Blue Shale to the Surface of Land. 163 4 men, filling and spreading, 6 days, at 2-9. Od. per day 1 do. do. do. 3 days, at 2s. Od. , , 2 lads, driving, &c. . 6 days, at 1^. Od. , , 1 1 horses . . .6 days, at 2s. 6d. , , I immediately ploughed it in ; and about Christmas I cross-ploughed it. With repeated workings I mixed it intimately with the soil ; and after cleaning it I sowed it in June, 1838, with hybrid turnips, giving it 8 three-horse loads of rotten manure per acre, and drilling on the whole field a compost of 14 qrs. of half-inch bones, with their dust, and 14 qrs. of vegetable ashes, made from weeds, &c., burnt. The crop of turnips was really good. It was eaten off with sheep ; and 250 shearlings were eight weeks upon them, besides the scraps which were eaten by ewes. 1839, barley and small seeds; produce, 35 qrs. 3 bushels, or40f- bushels of marketable* barley per acre, weighing 16 st. 3 lbs. per sack of 4 bushels. 1840, pastured with sheep; in autumn sowed with golden- drop wheat. 1841, wheat; produce 21 qrs. 6 bushels marketable corn, weighing 63^ lbs. per bushel : thus making an increase in my barley crop of 27f- bushels, and of my wheat 17|- bushels per acre, besides saving the expense of from 12 to 16 bushels of rape-dust per acre in each crop. I am Yours respectfully, Holmefield House, Ferrybridge^ Chas. Charnock. January 15, 1842, Last year I tried an experiment on a dry grass-field, laying on one acre 1 cwt. of nitrate of soda, cost 22^., and on another acre 4 qrs. of soot, cost 16^. ; the result was very much in favour of the soot. IT. — Improved Dibbling -Wheel. To the Secretary. Sir, — Having seen, in the Report of the Council Meeting on the 9th of March, a description of a dibbling-wheel for mangel-wurzel, by William Miles, Esq., M.P., and which consists of only "one'* wheel, I send you a drawing of a machine which we have used for seven years, with the greatest success, "never having lost our plant" since we used it. It appears that the only difference between it and Mr. Miles's consists in our using two wheels, which are placed on an axle at any distance apart under 34 inches. Now, if only one wheel is used, and the han- dles are fixed like a barrow, the man who uses it must of course follow the machine and walk on the ridge, or else by the side of the wheel. * i. e. without the small or light soilings. 164 Improved Dibbling- Wheel. Ours having two wheels working upon two ridges (21 inches apart), the man naturally walks in the furrow between them ; and, with a very little practice, can use two wheels as easily as one, and of course work two ridges at the same time. We sow from 3 to 4 lbs. of seed per acre, which enables us to deposit from two to four seeds in each hole, and which of course gives a better chance of a plant than only one. I can only add our entire concurrence in this mode of sowing that very useful root above any other we have yet seen tried. I am, Sir, Your obedient servant, William Adams, Jun. Great Barton., Bury St. Edmunds, April 15, 1842. [It might be an improvement in this implement to set the dib of one wheel opposite to the centre of the interval in the other wheel.] [The Dibs are 2 inches long by \\ inch wide at the base, and tapering to a point ; and can be set 14i in., 16^ in., and 18^ in. apart.] III. — On the Application of different Manures as a Substitute for Bones in the Growth of Turnips. To Henry Hand ley., Esq. Sir, — The very high and increasing price of bones having induced me to endeavour to discover a substitute, I send you the result of some ex- periments made under my own superintendance this season. Soil, a sandy loam, varying from 9 to 12 inches deep, recumbent on a lime- stone bottom. Manures for the Growth of Turnips. 165 The land was fallowed in the usual manner, and ploughed, on the 3rd of June, into ridges 27 inches asunder, and the whole manured with 6 cart-loads per acre of good yard manure, made by bullocks eating oil- cake and straw during the last winter. The ridges were then split, rolled, and drilled with a common one-horse ridge drill, at the rate of 3 lbs. per acre, of purple-top swede and green-top yellow turnips. The first part of them, with 6 bushels of half-inch bones and dust, at 2^. 9d. ; 4 gallons of whale-oil, at 2s. Ad. ; and about 40 bushels of ashes, pared from the hedge-sides and burnt. The second part, with 20 bushels of scutch, at 1.^. 6(i., and 40 of ashes. The third, with a mixture of night-soil and cinder-ashes, worked toge- ther till sufficiently dry to drill, 20 bushels per acre, with 40 of ashes. The fourth, with 12 bushels of crushed oyster-shells and 6 gallons of whale-oil, mixed, and 40 of ashes. The fifth, with 6 gallons of oil and 40 of ashes. The sixth, with burnt ashes only. The first and third are decidedly the best, with no perceptible differ- ence between them ; the fourth and fifth are equally good ; the second and sixth are very much the worst, and very insufficient for the pur- pose required. I last year used 2000 bushels of bones ; upon the same number of acres I have this year used 200 ; and, by the substitution of other manures in lieu of bones, I have saved in the first year 125/.; and I have, in every respect, to all appearance, as good a crop of turnips. If I have a preference, it is in favour of the night-soil compost ; which costs, when made thoroughly ready for use, about 5^. per ton, of 25 bushels. I remain, Sir, Your obedient servant, John Marshall. Riseholme, near Lincoln^ Oct, 29, 1841. IV. — On the Drainage of Land. To H. Handleij, Esq. Sir, — In a recent article " On the Drainage of Land " published in your Journal, no mention whatever is made of sod-draining, or of dram - age with the mole-plough ; and thorn-draining is mentioned only inci- dentally. These drains, though not always so permanent as tile or stone drains, are nevertheless so much cheaper as to deserve further notice. Of mole-draining I have seen but little; I have never practised it myself. I shall therefore confine my observations to thorn and sod drains: the former of these are applicable chiefly to arable, and the latter to grass lands. I ought to observe that my experience in draining has been confined almost entirely to clay lands — the kind of soil to which these drains are best suited. 166 On I he Drainage of Land, Thorn-drains are so general!)'' known as not to need any particular description. They are preferable to tile-drains in this respect, that, being open on all sides to the surrounding earth, they admit the water more freely than tiles do. Where tiles are laid in a tenacious clay, the clay in a wet sea?on becomes so " puddled " round the tiles, as scarcely to allow the percolation of the surrounding water. I have tile-drained seventy acres of land, of which the subsoil was a chalkstone clay. Stubble was laid upon the tiles. During the late wet season the water stood in many of the furrows : the drainage was by no means good. Wherever the furrow had in the course of successive ploughings been carried a foot or more from the line of drain, there the water stood. The drains were not above a foot deep, yet the water could not pene- trate ; even where an opening was cut from the furrow to the tiles, the water could scarcely gain admission through the intervals of the tiles, so tightly was each interval stopped wdth clay. Very different was the drainage of about fifty acres of much more tenacious clay w?iich had been drained with thorns. The drainage there was perfect. Thorn-draining has an advantage over tile-draining in point of cheap- ness also. The comparative expense of draining an acre of land with each kind of drain may be seen from the following estimate. The prices of labour and of tiles are such as are usually given in this neigh- bourhood. The quantity of stubble to be laid on the drains, and the number of tiles required for the main drain, would be the same in each case, and are therefore omitted : — £. s. d. £. s. d. 1500 tiles at 305. per 1000 . . 2 5 Carriage of do., say 5^. per 1000 . 7 6 Laying and filling 20 running acres (the running acre is 24 yards) of drains at 6rf. per acre . . . . 10 Total expense of draining an acre with tiles 3 2 6 One load of thorns, and carriage of do. 10 Laying and filling 20 acres of thorn- drain, at \0d. per running acre . 16 8 Additional expense of deeper main-drain 4 Total expense of drainmg an acre with thorns 1 17 Balance in favour of thorn-drains . . . 15 6 The disadvantages of thorn-drains are, that they are not permanent ; and that, being deeper, it is more difficult to obtain a good outfall for them. The duration of a good thorn-drain depends greatly on the firmness of the soil in which it is laid. When the thorns have perished, the superincumbent clay still forms an arch for the drain. Perhaps fifteen years may be taken as the average duration of a thorn-drain. On the Drainage of Land. 167 The best materials for such drains are gorse and white-thorn.* The common hawthorn, willow tops, and other materials, are also used. The thorns ought not to be cut till the leaf is fallen, else the dead leaves will encumber the drain. Sod-draining requires a more explicit description ; for, though not unknown elsewhere, it is not, I believe, very generally practised. One mode of sod-draining is by digging a drain about a foot wide, and then doubling the sod into the shape of an inverted V, with the grass inwards. The sods are then laid in the drain, resting on their edges, with the bent middle upwards. I have known drains of this kind to last very many years. The more common and more effectual way of sod-draining is, how- ever, as follows. The turf along the intended line of drain is cut with a turfing spade into a quadrangular shape c h b' c' (fig. 1), 9 inches c a a t O c c' = 9 inches. a a^ = 3 inches. h b' = Q inches. a m — \ foot. e c" = 18 inches. € a" = Q inches. Earth So/ds Drain Section of a sod-drain. Longitudinal view of a sod- drain. wide at top and 6 inches wide at bottom. Narrow wedges, acb^a' c' b', are next cut off on each side, and thrown aside, leaving the sod about 3 inches wide on the grass side and 6 inches wide underneath. The sods are then raised with a spade, each sod being about a foot long and 6 inches deep. The ends a b (fig. 2), &c. slanting off, so that each sod overlaps its neighbour. The sod having been thus removed, a "spit " of earth is taken out, and the crumbs are removed with a common draining- scoop. Another spit is then taken out with a narrow spade, and the loose earth is again removed with a narrow scoop, such as is used in making thorn-drains. The drain thus formed is wedge-shaped (see fig. 3), being about 18 inches deep, about 9 inches wide at top, and scarcely an inch wide at bottom. The depth and width of course vary a little, if the level of the surface requires it. In this respect sod-drains have an advantage over mole-drains, which must be parallel to the level of the surface. They may therefore be carried over ridges and other inequalities where the mole-plough would be unavailable. The sod is next placed in the drain with the grass-side downwards, Alder is very durable ; heath and black -thorn probably the most durable of all. 168 On the Drainage of Land. each sod lapping over the end of its neighbour (see fig. 4), and the drain is filled up with earth. The sod, if carefully cut, fits closely into the drain. It will bear a great weight: indeed the greater the weight upon it the more closely it is wedged down against the sloping sides of the drain. In this respect our drains seem to be superior to those made with ledges or shoulders to support the sod ; for in such drains the weight rests chiefly upon two points, whereas in our wedge-shaped drains the whole of each side shares in the pressure. Where the soil is tender, the drain is made a little larger, and a larger sod is filled in ; or a few thorns are placed in the drain to support the tender earth. In sand or gravel-beds, or other very bad places, it is well to lay tiles as far as the soft soil extends. In very wet furrows it is well to cut the drain a little on one side of the furrow, for both the soil and the sod are generally sounder there. Drains of this kind, if carefully made, last many years. In the only case in which I have known well-made sod-drains require to be renewed, they had lasted about twenty years. In cutting ditches, sewers, &c., I have lately fallen in with sod-drains considerably more than twenty years old, which were as sound as when they were first made. The usual price per acre (of 24 running yards) for making sod-drains is 10c/., and \s. per running acre for the main-drains. Where the soil is stony I have given as much as 1,?. per acre for the sod -drains, and 1^. 6d. for the main-drains. In counties where labour is cheap the expense would pro- bably be less. The expense of draining an acre of land with sods may be estimated as follows : — 20 running acres of sod-drain, at 10c?. per acre Tiles for main drain, say ..... Laying do. at 1.^. per 24 yards, say Total expense of sod-draining an acre of land . 18 6 No stubble or other material is required to lay upon the drains. Ac- cording to this estimate the expense of draining with sods is less than a third of the expense of draining with tiles. Supposing sod-drains to last twenty years, the interest of the money saved by substituting sod-drains for tile-drains will more than pay the expense of renewing the sod-drains ad wfiniium. I have drained between sixty and seventy acres with sod-drains, and so well am I satisfied with them, that I intend to drain about as much more in the same way. I am, Sir, Your obedient servant, H. H. Brown. Heckington, Feb. 23, 1842. Note — I drained some clay land in the year 1814 in this way, and very little of it has required to be renewed. — Spencer. s. d. 16 8 1 4 6 THE JOURNAL OF THE ROYAL AGRICULTURAL SOCIETY OF ENGLAND, VOLUME THE THIRD. 1842. PARTS n,— HI.: COMPLETING THE V O L U Jil E. PRACTICE WITH SCIENCE. LONDON: JOHN MURRAY, ALBEMARLE STREET. MDCCCXLir. TBEUE experiments, it is true, are not easy ; STILL THEY ARE IN THE POWER OF EVERY THINKING HUSBANDMAN. HE V.TIO ACCOMPLISHES BUT ONE, OF HOWEVER LIMITED APPLICATION, AND TAKES CARE TO REIORT IT FAITHFULLY, ADVANCES THE SCIENCE, AND, CONSEQUENTLY, THE PRACTICE OF AGRICULTURE, AND ACQUIRES THEREnV A RIGHT TO THE GRATITUDE OF HIS FELLOWS, AND OF THOSE WHO COME AFTER. TO MAKE MANY SUCH IS BEYOND THE POWER OF MOST INDIVIDUALS, AND CANNOT BE EXPECTED. THE FIRST CARE OF ALL SOCIETIES FORMED FOR THE IMPROVEMENT OF OUR SCIENCE SHOULD BE TO PREPARE THE FORMS OF SUCH EXPERIMENTS, AND TO DISTRIBUTE THE EXECUTION OF THESE AMONG THEIR MEMBERS. Von Thaer, Principles of /Igriculture. London: Friuti-d by ^VIELIAM Ci.owrs aiui Sons, Statufjid Stii-et. CONTENTS OF PARTS II.— III., VOLUME III. ARTICLE ^^«^ XIII.— On the Progress of Agricultural Knowledge during the last Four Years. By Ph. Pusey, M.P., F.R. and G.S. 169 XIV.— Account of the Meeting of German Landowners in 1841. By Henry Handley 217 XV.— On the Marling of a Light Sandy Soil on the Duke of Bedford's Farm at Woburn. By Charles Burness . 233 XVI.— On Claying or Marling Land. By F. W. Overman . 234 XVII.— Early Vetches. By William Jones Williams . . 230 XVIII.— On the Cultivation of Lucerne. By Joshua Rodwell . 238 XIX.— Agriculture of the Netherlands. Part II. By the Rev. W. L. Rham 240 XX.— On the Planting and Management of Forest- Trees. By Charles Falkner 2^3 XXL— On Wheat. By C. Hillyard, of Thorpelands, near Northampton . . . • • • .297 XXII.—Observations on the Natural History and Economy of various Insects affecting the Turnip Crops, mcludmg the White Cabbage-Butterllies, the Turnip-seed Weevil, &c. By John Curtis, F.L.S., Corresponding Member of the Imperial and Royal Georgofili Society of Florence, &c. 306 XXIIL— On the Use of Burnt Clay as a Manure for Heavy Clay Soils. By Francis Pym 323 XXIV.— On the Failure of the Red Clover. By the Rev. W. Thorp 326 XXV.—On Measuring Cattle. By C. Hillyard, of Thorpelands, near Northampton . . . . • • .337 XXVI.— Report on the Exhibition of Implements at the Bristol Meeting in 1842 338 XXVIL— On the Public Institutions for the Advancement of Agri- cultural Science which exist in other Countries, and on the Plans which have been set on foot by Individuals with a similar intent in our own. By Charles Daubeny, M.D., F.R.S., Professor of Rural Economy in the Uni- versity of Oxford 364 XXVIIL— On the Dyock Oat. By the Rev. R. W. Fisher . .387 XXIX.— Report on the Wheats selected for Trial at Cambridge, and on other Wheats. By W. Miles, M.P. . . 391 XXX.— Report on Prize-Wheats. By G. Kimberley . . . 395 XXXI.— Report on Prize-Wheats. By H. Handley . . . o^^^l IV CONTENTS. XXXII —Account of Mr. Irving's New Machine for Constructing Tiles. By W. Ford 398 XXXIII. — Agricultural Tour in Denmark, Sweden, and Russia. By James F. W. Johnston, F.R.S 400 Miscellaneous Communications and Notices : — v.— Account of Experiments on the Growth of Swedes ' . 423 VI.— On the Application of Clay to Moor-Land . . .427 VII. — Simple and Effectual Method of destroying Rats and Mice 428 VIII.— On the Use of Lime 429 IX. -On the Feeding of Stock 430 X.— On the Chemical Constituents of Crops . . . 433 XL— On the Quantity of Minute Ingredients of Soil contained in an Acre of Land 434 XII. — Experiments with Guano 437 XUL— New and Economical Oil-Cake 439 APPENDIX : Council and Officers of the Royal Agricultural Society of England Honorary Members Report of the Council to the Anniversary Meeting . , General Meetings of 1842-3 Statement of Accounts from July to December, 1841 Award of Prizes at the Meeting at Bristol .... Prizes for the Meeting at Derby Prizes and Conditions for Essays and Reports on various subjects XV xvi xvii xxiii xxiv XXV xxxii XXXV i LIST OF PLATES. Plate I. to face page II. „ 321 322 Title-page and general Contents of Vol. III. ERRATA. ■ Part I. Ill Mr. Murcliisou's paper, p. 130, line 21, for "hectares"' read "hectolitres." Parts II.— III. lu Mr. Pusey's paper, p. 185, line 10,/o/' " 36*." read " 51s.'' ( 169 ) XIII. — 0)1 the Progress of Agricultural Knowledge durhig the last Four Years. By Ph. Pusey, M.P., F.R. and G.S. As four years have passed since our Society was founded for extending the knowledge and improving the practice of hus- bandry, it may not be useless now to inquire how far, if at all, its working has hitherto carried out the views of our founders. Though we could not be fairly required to have done much in so short a time, we certainly ought to have done something, strengthened as we have been by the hearty aid of the English farmers. We should be encouraged, I think, by knowing what we have done, if, indeed, we have succeeded in anything; we shall be more likely to advance farther, if we look at the diffi- culties we still have to deal with ; and the best encouragement, perhaps, for active men, is the knowledge that they have yet a great deal to do. The extension of science may, however, mean two different things, either the spread of existing knowledge among a wider number of persons — and this is a most important object in our department ; for if the best practice of each different district could become general in the country, a very great im- provement in farming would at once be effected — or it may mean the discovery of principles hitherto entirely unknown. In examining how far we have advanced in either way the know- ledge of farming, it may be convenient to begin with the soil itself, proceeding afterwards from tillage and seed-time to har- vest; and as no soil, however good, can yield what it ought while it is drenched with water, we must first consider drainage. It is only seven years since we heard in England, chiefly through the present Speaker of the House of Commons, that a ma- nufacturer in Scotland, now well known as Mr. Smith of Deanston, had found the means of making all land, however wet and poor it might be, warm, sound, and fertile, and that this change was brought about by two processes, thorough-draining and subsoil- ploughing. PI is rule of draining was this : that we are not to endea- vour merely to find out hidden springs, and to cut them through by a single drain, which in some of our books appeared to be re- garded as all that was necessary; but that, as the whole surface of retentive soils is rendered wet, not by accidental springs, but by the rain, the whole surface of the field must be made thoroughly dry by under-drains, running throughout at equal distances ; any field, he said, however wet, might be so dried, provided these under- drains were cut sufficiently near to each other. This was the prin- ciple of Thorough or Frequent Draining asserted by Mr. Smith of Deanston in 1 835 ; and this principle, which was then new and startling, may now be regarded as firmly established. But though it was then so novels I have discovered accidentally that it has been long practised to its fullest extent in one part of VOL. III. N 170 Progress of Agricnltvrnl Kvowlechjp England. I do not speak of furrow-draining, which was well known in many districts, for the drains were not generally so deep nor so numerous as they are on the Deanston system. But an old drill-man from Suffolk having observed to me, that if he were the tenant of a strong clay farm in this neighbourhood, he should drain the whole of it with drains cut 12 feet apart and 3 feet in depth, I was struck with this remark of an old man who had never read the new system of drainage, yet described it as carried to its utmost extent, for drains could scarcely be cut nearer or deeper. He told me, on being further questioned, that it was the method which he had seen as a boy at his native place. Mr. Allan Ransome, at my request, inquired into the matter, and informs me that forty years ago three properties, one of them Lord Huntingfield's, near Yoxford, in Suffolk, were drained in this manner. I have reason to believe that the same effectual mode of draining has long been practised in Essex, so much so as" to be called the Essex system even in Scotland. Now, in proving that Mr. Smith's system is not new, I do not lower his claims to our thanks, for he probably invented it also, and at all events carried it out with an energy which made it new in his hands; but I think the fact of its previous practice in Suffolk and Essex worth notice for two reasons : one, that any new method, however highly recommended, must be received with doubt as long as it continues new, and that consequently the best praise by which any method can be recommended to practical farmers is, not that it is new, but on the contrary that it is old and tried ; the other reason is this, that here was a plan of drain- age which was regarded as novel, yet had been employed and esta- blished for half a century at no great distance from London ; and this is by no means a singular proof how little the farmers in one part of England knew, until lately, what the others were doing. All, however, who are at all acquainted with improved husbandry are now agreed that on wet land thorough-drain- ing is to a farm what a foundation is to a house. There is no doubt now what ought to be done ; the difficulty is to find means for doing it, since one-third of England, I believe, re- quires to be drained. It would be easy to bring forward in- stances of great profit resulting from drainage ; and I may refer to the accounts of Sir James Graham's operations at Netherby,'"^' and of Lord Hatherton'sf at Teddesley, where the water which gushes out of the underground drains is thrown over a water-wheel, threshes the corn, and does the other work of the barn ; still great returns cannot be held out in all cases, yet every wet farm ought to be drained. But the advantage of draining is not to be measured * Journal, vol. i. p. 32. t Ibid., vol. ii. p. 273, on the Drainage of Land : by J. F. Burke. during the last Foitr Years. 171 merely by the additional bushels of corn that may be grown on an acre ; though I believe five or six bushels of wheat per acre would be a fair estimate of the increase ; for such land is usually thrown up into very narrow ridges, perhaps 10 feet wide, and no corn grows in the bare furrow ; so that one-tenth of the land is lost altogether ; the lower half of the ridge, too, on each side of the furrow bears often only straggling ears ; long tracts of such fields must have been seen between Birmingham and Liverpool last year by many of our members ; and it may be useful for landowners to know that every arable field which is laid up in ridges probably requires more or less to be drained; in fact these deep furrows were devised by our ancestors for drying the ridges piled up between them. An intrinsic advantage, however, of draining is this, that the character of the farm is changed. It is difiicult to obtain a good tenant for a cold clay farm ; and I am inclined to think that some of these farms have gone backwards in the last fifty years. On two such farms, now in wretched condition, I found it was in the memory of living persons that they had once borne far better crops. No long time ago it was the clay lands that fed the country; but since the great change effected in light-land farming by turnip husbandry, every farmer wishes to occupy what is called a stock- farm, a farm where he can fold his sheep on the land at all seasons, consequently the clay-farms have become less and less popular; and, in some cases, have fallen into inferior hands."'' Nor can we be surprised at the unpopularity of a wet farm_, for its discomforts are endless, as well as its losses. The acts of hus- bandry are at all times liable to interruption by excess of rain. The farm.er does not know when he can plough or sow ; often his teams cannot go on the land ; so that the work to be done * A main reason why clay-farms have, to a considerable extent, fallen into *' inferior hands" is the circumstance that they are the only farms which, from the moderate outlay required to enter, come within the reach of a cer- tain class. If, for instance, a farming servant or cottager, either by mar- riage, bequest, or a long course of industry, shall have become possessed of a few hundred pounds, and desire to be himself an occupier, he is debarred from entering upon a grazing, a mixed, or a con-vertible farm, by the capital necessary to purchase stock or artificial manures ; but for a small clay-farm a team of horses and a few implements are alone essential. He ploughs, sows, and reaps, and converts his straw into what he calls manure by the mouths and feet of a few starved calves or yearlings, mainly aided by the winter rains, and then carts it on his land, little better than rotted straw. No wonder the condition of small clay-farms should be low. Yet, however disagreeable the enumerated drawbacks to a clay-farm, and I admit they are many, there is none more gratefid for capital expended, either in drain- ing or manure. Once drained, the art of clay-farming consists in the art of ploughing, and the art of making manure. If, on the one hand, the clays could advantageously spare their superfluous moisture to the thirsty, gra- velly, or sandy soils, on the other hand, they do not burn, like these, under a summer sun, and at all events carefully retain, until required by the crop, whatever manure is put into them.— H. Handley, n2 172 Progress of Agricultural Knowledge accumulates ; yet when the favourable moment arrives, in which all the work must be done at once, he requires more horses for each plough than the light-land farmer, while he has less time for doing that work. In a wet autumn he must sow his wheat too late ; perhaps not sow it at all. If he does sow wheat, and the rain continues, the seed sometimes rots in the ground ; or if it has come up well, winter soaks the hollows thoroughly, if it does not fill them with standing water ; and in spring, on each side of the furrow, large blanks are seen in the crop.* In fact a perpetual struggle is going on between the plough- man with his horses on one side, who endeavours to reduce this stubborn clay into mould, and the rains which render it solid again. There are some such farms, so hard in dry weather, so tough in their best state of moderate moisture, so deep and impassable in wet winters, so cold and backward in spring — I have one such farm myself — that farmers who are accustomed to warm, sound land, fit at all times for stock and for labour, say they would not occupy such ground free of rent. No one who knows the effect of thorough-draining can see without regret such farms, and the starveling crops which they bear. If the occupier be a bad farmer, his own circumstances are probably in proportion to the poverty of his land ; if a good one, half his exertions are lost, and he does not obtain the fair reward of his industry and enterprise. If I were a working- farmer, nothing would induce me to enter on a cold wet farm, unless there were a fair prospect of its being drained, either with my own money under a long lease, or with the aid of my landlord. Our Society has wisely abstained from entering into questions between landlords and tenants ; and I will therefore merely mention that sometimes in Scotland, on a lease for nineteen years, the tenant pays for the draining himself; some- times the landlord finds materials, and the tenant the labour, or the landlord pays for the whole, receiving interest for his outlay. The landlord, however, may not find it convenient to make heavy advances over a large property ; but, as Lord Stanley recom- mended, he may borrow the money for such a purpose. In dis- tricts, indeed, where under-draining is still unknown, the tenant may not be aware of its advantage, and therefore may not meet his views. In that case a few fields may be drained at first, in order to prove the advantage ; or if a poor wet farm should fall in, it may be taken in hand and reclaimed, which is mora useful and * I have also heard from a farmer on a very stiff clay that the wetter the winter the more rain is required on such land by the wheat in the following summer, the more consequently it suffers in a season of drought. The rea- son, I think, must be this, that the water lodged in winter condenses the soil, destroying the looseness which the plough had produced in it, and thus rendering it when dry once more a close clay, through which the roots of the plant cannot make their way, and which moderate summer rains cannot penetrate ; but this is not generally applicable to clay lands. durm