TALKS ON MANURES A SERIES OF FAMILIAR AND PRACTICAL TALKS BETWEEN THE AUTHOR AND THE DEACON, THE DOCTOR, AND OTHER NEIGHBORS, ON THE WHOLE SUBJECT
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growth of root brings the plant in contact with a larger feeding surface, and enables it to take up more nitric acid from its solution in the soil. Such is also the case during the w
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aith in good plowing, early sowing, and thorough cultivation. PREFACE TO FIRST EDITION. The Printers have got our “Talks on Manures” in type; and the publishers want a Preface.
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n as many months. Time is required for the chemical changes to take place in the soil. But watch the effect on the clover for the next two years, and when the land is plowed again, se
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is tillage.” CHAPTER VIII. SUMMER-FALLOWING. This is not the place to discuss the merits, or demerits, of fallowing. But an intelligent Ohio farmer writes me: --“I see that you
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eat will be produced by the slow combustion of a portion of the carbonaceous and nitrogenous matter, and the result will be a mass of material, which we should all recognize as “manur
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ny value in the table. For instance, there is a large amount of carbonaceous matter in the manure of animals, which, for some crops, is not without value, but which is not here taken
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s very considerable. The five tons (10,000 lbs.,) of fresh manure placed in a heap on the 3d of November, are reduced to 7,138 lbs. by the 30th of April. Of this 4,707 lbs. is water
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y manure deteriorates by being exposed to rain, spread out on the surface of the yard. The table merits careful study.” Table Showing Composition of Experimental Heap (No. III.). F
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plow in the manure at once, or to let it lie for some time on the surface, and to give the rain full opportunity to wash it into the soil. “It appears to me a matter of the greatest
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that he gets far more benefit from the manure when applied on the surface, and left exposed for several months, than if he plowed it under at once. I like to write and talk about Jo
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ht the farm thirteen years ago; and much of this increase has taken place during the last five or six years, and I expect to see still greater improvement year by year. “Never mind a
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e. 2d. When manure is allowed to lie scattered about over a large surface, it is liable to have much of its value washed out by the rain. In a compact heap of this kind, the rain or s
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ceive from ten to twenty times as much water as would fall on the surface of the heap.” “But you do recommend piling manure and fermenting it in the open air and keeping the top flat
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implements 65.00 Average repairs of place and buildings 175.00 Average depreciation and interest on stock 180.00 In
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practice. We must either plow under the clover, let it rot on the surface, or pasture it, or use it for soiling, or make it into hay, feed it out to stock, and return the manure to th
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to these crops, either by strengthening the straw, or stems of graminaceous plants, or otherwise benefiting them; but, after deducting the amount of silica from the total amount of m
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ction, a six-inch slice cut down at a depth of 12 inches from the surface, no distinct fibres could be found. The soil was almost completely saturated with rain when it was dug up on
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hed, when very nearly dry: Lbs. Surface, six inches 2,407,900 Next ” 2,444,200 Third ” 2,480,500 “
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nalyses of the soil show that in the first eighteen inches of the surface-soil, there was 6,550 lbs. of nitrogen per acre, on one part of the field, and 10,300 lbs. on the other part.
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about 5 per cent of nitrogen, and is also rich in minerals and _carbonaceous matter_. It gives an increase, but not as large in proportion to the nitrogen furnished, as the sulphate o
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t there is little danger of any loss from spreading manure on the surface, and I suppose you would have us conclude that we make a mistake in plowing it under, as the soil renders it
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nd it to his advantage to use it largely as a top-dressing on the surface. Exposing manure to the atmosphere, spread out on the land for several months, and harrowing it occasionally,
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and important results. I was there at the time. But this is not the place to discuss the question. I am often amused, however, at the remarks we often hear in regard to the inferior q
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njured by stagnant water _in the soil_, and standing water on the surface. I think we may safely say that one-third the wheat-crop of this county (Monroe Co., N.Y.), is lost for want
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potash, etc., was mixed with it, the ammonia, or potash, taking the place of the lime or soda. Prof. Way’s discovery, then, is not that soils have “absorptive properties”--that has b
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siderable extent. I have several times sown barley as soon as the surface-soil was thawed out five or six inches deep, but with a bed of solid frozen earth beneath. 3d. Two-rowed bar
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was applied in the spring. If the manure had been applied on the surface, instead of plowing it under, I believe the effect would have been still more in favor of the autumn-manuring
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h a little soil, and then the superphosphate or sulphate of ammonia placed on the top and covered with soil before the seed was planted. Notwithstanding this precaution, the rain wash
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ill not interfere with the drill. And the manure will be near the surface, where the young roots of the wheat can get hold of it. “You must recollect,” said the Doctor, “that the roo
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case; and yet there seem to be some facts that would incline us to place Indian corn with the leguminous plants, such as clover, peas, and beans, rather than with the cereals, wheat,
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to good food the refuse plant-food left in the soil. It is to the surface soil, what clover is to the subsoil. To the market gardener, or to a farmer who manures heavily common turnip
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e trouble is in the quality of the manure. It contains too much carbonaceous matter. In other words, it is so poor in nitrogen and phosphoric acid, that an excessive quantity has to b
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each load of this rotted manure costs at least $5.00. H. E. Hooker places the cost of manure equally high, but seems willing to use all he can get, and does not think we can profitab
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Some of it comes back to us in rains and dews. Of course, there are places where the sewage of our cities and villages can be used for irrigating purposes. But when water is used as f
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acid, and potash, are largely retained in the first few inches of surface soil, and the deeper roots get hold of only those portions which leach through the upper layer of earth. Nitr
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r thirty years’ experience in the use of these fertilizers, I would place far more confidence on a good and reliable analysis than on any actual trial I could make in the field. Testi
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and was very light, and that you might walk over the fresh plowed surface in the wettest weather without any clay sticking to your boots: still a portion of the soil was dark in color
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c acid by drainage. I was not at all surprised to find, that the surface soil of a wood on my farm, was poorer in nitrogen than the soil of an old permanent pasture, to which no manu
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o dispense with railroad transportation in bringing manure to their places and marketing crops. I have noticed that one of the shrewdest gardeners invariably composts horn-shavings an
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|948 | 1.6| 5.0| 2.2| 0.4| 0.3| 0.4| 1.0| 0.4| 0.2 Sugar-beet Pomace |700 | 2.9| 11.4| 3.9| 0.9| 2.6| 0.7| 1.1| 0.4| 0.9 Clarifying Refuse |948 | 0.8| 3.3| 0.3| 0.1| 1.1| 0.2|
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of roots) | 19 | 0.24| 1.15|0.336|0.108|0.132|0.144 Pomace (15 per cent | | | | | | | of roots) | 46 | 0.44| 1.71|0.5
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by Growing, 133-163 ” Letting it Rot on the Surface as Manure, 134 ” Nitrogen as a Manure for, 141 ” Pastu
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uperphosphate of Lime, When First Made in the United States, 324 Surface Application of Manure, 70-268 Swamp-muck,
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con,” said he _quotation marks as in original (same speaker)_ carbonaceous matter and water, of little or no value?” _text has question mark after close quote_ It would be a very
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99.59
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“The soil, it will be seen, in general character, resembles the
preceding sample; it contains a good deal of potash and phosphoric
acid, and may be presumed to be well suited to the growth of clover. It
contains more carbonate of lime, and is somewhat lighter than the sample
from the part of the field twice mown for hay, and may be termed heavy
calcareous clay.
“An acre of this land, 18 inches deep, weighed, when very nearly dry:
Lbs.
Surface, six inches 2,407,900
Next ” 2,444,200
Third ” 2,480,500
“Or in round numbers, every six inches of soil weighed per acre 2½
millions of pounds, which agrees tolerably well with the actual weight
per acre of the preceding soil.
“The amount of phosphoric acid and nitrogen in each six-inch layer was
determined separately, as before, when the following results were
obtained:
In Dried Soil.
First six Second Third six
inches. six inches. inches.
Percentage of phosphoric acid .159 .166 .140
Nitrogen .189 .134 .089
Equal to ammonia .229 .162 .108
“An acre, according to these determinations, contains in the three
separate sections:
First six Second Third six
inches. six inches. inches.
lbs. lbs. lbs.
Phosphoric acid 3,975 4,150 3,500
Nitrogen 4,725 3,350 2,225
Equal to ammonia 5,725 4,050 2,700
“Here, again, as might naturally be expected, the proportion of nitrogen
is largest in the surface, where all the decaying leaves dropped during
the growth of the clover for seed are found, and wherein root-fibres are
more abundant than in the lower strata. The first six inches of soil, it
will be seen, contained in round numbers, 2½ tons of nitrogen per acre,
that is, considerably more than was found in the same section of the
soil where the clover was mown twice for hay; showing plainly, that
during the ripening of the clover seed, the surface is much enriched by
the nitrogenous matter in the dropping leaves of the clover-plant.
“_Clover-roots_.--The roots from one square foot of this soil, freed as
much as possible from adhering soil, were dried at 212°, and when
weighed and reduced to a fine powder, gave, on analysis, the following
results:
Organic matter* 64.76
Mineral matter† 35.24
-------
100.00
=======
* Containing nitrogen 1.702
Equal to ammonia 2.066
† Including clay and sand
(insoluble silicious matter) 26.04
“A square foot of this soil produced 582 grains of dried clover-roots,
consequently an acre yielded 3,622 lbs. of roots, or more than twice the
weight of roots obtained from the soil of the same field where the
clover was twice mown for hay.
“In round numbers, the 3,622 lbs. of clover-roots from the land mown
once, and afterwards left for seed, contained 51½ lbs. of nitrogen.
“The roots from the soil after clover-seed, it will be noticed, were not
so clean as the preceding sample, nevertheless, they yielded more
nitrogen. In 64.76 of organic matter, we have here 1.702 of nitrogen,
whereas, in the case of the roots from the part of the field where the
clover was twice mown for hay, we have in 81.33 parts, that is, much
more organic matter, and 1.635, or rather less of nitrogen. It is
evident, therefore, that the organic matter in the soil after
clover-seed, occurs in a more advanced stage of decomposition, than
found in the clover-roots from the part of the field twice mown. In the
manure, in which the decay of such and similar organic remains proceeds,
much of the non-nitrogenous, or carbonaceous matters, of which these
remains chiefly, though not entirely, consist, is transformed into
gaseous carbonic acid, and what remains behind, becomes richer in
nitrogen and mineral matters. A parallel case, showing the dissipation
of carbonaceous matter, and the increase in the percentage of nitrogen
and mineral matter in what is left behind, is presented to us in fresh
and rotten dung; in long or fresh dung, the percentage of organic
matter, consisting chiefly of very imperfectly decomposed straw, being
larger, and that of nitrogen and mineral matter smaller, than in
well-rotted dung.
“The roots from the field after clover-seed, it will be borne in mind,
were dug up in November, whilst those obtained from the land twice mown,
were dug up in September; the former, therefore, may be expected to be
in a more advanced state of decay than the latter, and richer in
nitrogen.
“In an acre of soil, after clover-seed, we have:
Lbs.
Nitrogen in first six inches of soil 4,725
Nitrogen in roots 51½
Nitrogen in second six inches of soil 3,350
-------
Total amount of nitrogen, per acre, in
twelve inches of soil 8,126½
=======
“Equal to ammonia, 9,867 lbs.: or, in round numbers, 3 tons and 12½
cwts. of nitrogen per acre; equal to 4 tons 8 cwts. of ammonia.
“This is a very much larger amount of nitrogen than occurred in the
other soil, and shows plainly that the total amount of nitrogen
accumulates especially in the surface-soil, when clover is grown for
seed; thus explaining intelligibly, as it appears to me, why wheat, as
stated by many practical men, succeeds better on land where clover is
grown for seed, than where it is mown for hay.
“All the three layers of the soil, after clover-seed, are richer in
nitrogen than the same sections of the soil where the clover was twice
mown, as will be seen by the following comparative statement of results:
--------------+--------------------------+--------------------------
| I. | II.
| Clover-Soil twice | Clover-Soil once mown
| mown. | and then left for seed.
+--------+--------+--------+--------+--------+--------
| | | | | |
| Upper | Second | Third | Upper | Next | Lowest
|6 inches|6 inches|6 inches|6 inches|6 inches|6 inches
--------------+--------+--------+--------+--------+--------+--------
Percentage of | | | | | |
nitrogen in | .168 | .092 | .064 | .189 | .134 | .089
dried soil | | | | | |
Equal to | | | | | |
ammonia | .198 | .112 | .078 | .229 | .162 | .108
--------------+--------+--------+--------+--------+--------+--------
“This difference in the amount of accumulated nitrogen in clover-land,
appears still more strikingly on comparing the total amounts of nitrogen
per acre in the different sections of the two portions of the 11-acre
field.
Percentage of Nitrogen Per Acre.
First six Second Third six
inches. six inches. inches.
Lbs. Lbs. Lbs.
I. In soil, clover twice }
mown* } 3,350 1,875 1,325
II. In soil, clover once }
mown and seeded }
afterwards† } 4,725 3,350 2,225
===== ===== =====
Equal to ammonia:
* I. Clover twice mown } 4,050 2,275 1,600
† II. Clover seeded } 5,725 4,050 2,700
Lbs.
I. Nitrogen in roots of clover twice mown } 24½
II. Nitrogen in clover, once mown, and grown }
for seed afterwards } 51½
I. Weight of dry roots per acre from Soil I } 1,493½
II. Weight of dry roots per acre from Soil II } 3,622
Total amount of nitrogen in 1 acre, 12 inches }
deep of Soil I* } 5,249¼
Total amount of nitrogen in 1 acre, 12 inches }
deep of Soil II† } 8,126¼
Excess of nitrogen in an acre of soil 12 }
inches deep, calculated as ammonia in part }
of field, mown once and then seeded } 3,592½
---------
* Equal to ammonia } 6,374½
† Equal to ammonia } 9,867
“It will be seen that not only was the amount of large clover-roots
greater in the part where clover was grown for seed, but that likewise
the different layers of soil were in every instance richer in nitrogen
after clover-seed, than after clover mown twice for hay.
“Reasons are given in the beginning of this paper which it is hoped will
have convinced the reader, that the fertility of land is not so much
measured by the amount of ash constituents of plants which it contains,
as by the amount of nitrogen, which, together with an excess of such ash
constituents, it contains in an available form. It has been shown
likewise, that the removal from the soil of a large amount of mineral
matter in a good clover-crop, in conformity with many direct field
experiments, is not likely in any degree to affect the wheat-crop, and
that the yield of wheat on soils under ordinary cultivation, according
to the experience of many farmers, and the direct and numerous
experiments of Messrs. Lawes and Gilbert, rises or falls, other
circumstances being equal, with the supply of available nitrogenous food
which is given to the wheat. This being the case, we can not doubt that
the benefits arising from the growth of clover to the succeeding wheat,
are mainly due to the fact that an immense amount of nitrogenous food
accumulates in the soil during the growth of clover.
“This accumulation of nitrogenous plant-food, specially useful to cereal
crops, is, as shown in the preceding experiments, much greater when
clover is grown for seed, than when it is made into hay. This affords an
intelligible explanation of a fact long observed by good practical men,
although denied by others who decline to accept their experience as
resting upon trustworthy evidence, because, as they say, land cannot
become more fertile when a crop is grown upon it for seed, which is
carried off, than when that crop is cut down and the produce consumed on
the land. The chemical points brought forward in the course of this
inquiry, show plainly that mere speculation as to what can take place in
a soil, and what not, do not much advance the true theory of certain
agricultural practices. It is only by carefully investigating subjects
like the one under consideration, that positive proofs are given,
showing the correctness of intelligent observers in the fields. Many
years ago, I made a great many experiments relative to the chemistry of
farm-yard manure, and then showed, amongst other particulars, that
manure, spread at once on the land, need not there and then be plowed
in, inasmuch as neither a broiling sun, nor a sweeping and drying wind
will cause the slightest loss of ammonia; and that, therefore, the
old-fashioned farmer who carts his manure on the land as soon as he can,
and spreads it at once, but who plows it in at his convenience, acts in
perfect accordance with correct chemical principles involved in the
management of farm-yard manure. On the present occasion, my main object
has been to show, not merely by reasoning on the subject, but by actual
experiments, that the larger the amounts of nitrogen, potash, soda,
lime, phosphoric acid, etc., which are removed from the land in a
clover-crop, the better it is, nevertheless, made thereby for producing
in the succeeding year an abundant crop of wheat, other circumstances
being favorable to its growth.
“Indeed, no kind of manure can be compared in point of efficacy for
wheat, to the manuring which the land gets in a really good crop of
clover. The farmer who wishes to derive the full benefit from his
clover-lay, should plow it up for wheat as soon as possible in the
autumn, and leave it in a rough state as long as is admissible, in order
that the air may find free access into the land, and the organic remains
left in so much abundance in a good crop of clover be changed into
plant-food; more especially, in other words, in order that the crude
nitrogenous organic matter in the clover-roots and decaying leaves, may
have time to become transformed into ammoniacal compounds, and these, in
the course of time, into nitrates, which I am strongly inclined to think
is the form in which nitrogen is assimilated, par excellence by cereal
crops, and in which, at all events, it is more efficacious than in any
other state of combination wherein it may be used as a fertilizer.
“When the clover-lay is plowed up early, the decay of the clover is
sufficiently advanced by the time the young wheat-plant stands in need
of readily available nitrogenous food, and this being uniformly
distributed through the whole of the cultivated soil, is ready to
benefit every single plant. This equal and abundant distribution of
food, peculiarly valuable to cereals, is a great advantage, and speaks
strongly in favor of clover as a preparatory crop for wheat.
“Nitrate of soda, an excellent spring top-dressing for wheat and cereals
in general, in some seasons fails to produce as good an effect as in
others. In very dry springs, the rainfall is not sufficient to wash it
properly into the soil and to distribute it equally, and in very wet
seasons it is apt to be washed either into the drains or into a stratum
of the soil not accessible to the roots of the young wheat. As,
therefore, the character of the approaching season can not usually be
predicted, the application of nitrate of soda to wheat is always
attended with more or less uncertainty.
“The case is different, when a good crop of clover-hay has been obtained
from the land on which wheat is intended to be grown afterwards. An
enormous quantity of nitrogenous organic matter, as we have seen, is
left in the land after the removal of the clover-crop; and these remains
gradually decay and furnish ammonia, which at first and during the
colder months of the year, is retained by the well known absorbing
properties which all good wheat-soils possess. In spring, when warmer
weather sets in, and the wheat begins to make a push, these ammonia
compounds in the soil are by degrees oxidized into nitrates; and as this
change into food peculiarly favorable to young cereal plants, proceeds
slowly but steadily, we have in the soil itself, after clover, a source
from which nitrates are continuously produced; so that it does not much
affect the final yield of wheat, whether heavy rains remove some or all
of the nitrate present in the soil. The clover remains thus afford a
more continuous source from which nitrates are produced, and greater
certainty for a good crop of wheat than when recourse is had to
nitrogenous top-dressings in the spring.
SUMMARY.
“The following are some of the chief points of interest which I have
endeavored fully to develope in the preceding pages:
“1. A good crop of clover removes from the soil more potash, phosphoric
acid, lime, and other mineral matters, which enter into the composition
of the ashes of our cultivated crops, than any other crop usually grown
in this country.
“2. There is fully three times as much nitrogen in a crop of clover as
in the average produce of the grain and straw of wheat per acre.
“3. Notwithstanding the large amount of nitrogenous matter and of
ash-constituents of plants, in the produce of an acre, clover is an
excellent preparatory crop for wheat.
“4. During the growth of clover, a large amount of nitrogenous matter
accumulates in the soil.
“5. This accumulation, which is greatest in the surface soil, is due to
decaying leaves dropped during the growth of clover, and to an abundance
of roots, containing, when dry, from one and three-fourths to two per
cent of nitrogen.
“6. The clover-roots are stronger and more numerous, and more leaves
fall on the ground when clover is grown for seed, than when it is mown
for hay; in consequence, more nitrogen is left after clover-seed, than
after hay, which accounts for wheat yielding a better crop after
clover-seed than after hay.
“7. The development of roots being checked, when the produce, in a green
condition, is fed off by sheep, in all probability, leaves still less
nitrogenous matter in the soil than when clover is allowed to get riper
and is mown for hay; thus, no doubt, accounting for the observation made
by practical men, that, notwithstanding the return of the produce in the
sheep excrements, wheat is generally stronger, and yields better, after
clover mown for hay, than when the clover is fed off green by sheep.
“8. The nitrogenous matters in the clover remains, on their gradual
decay, are finally transformed into nitrates, thus affording a
continuous source of food on which cereal crops specially delight to
grow.
“9. There is strong presumptive evidence that the nitrogen which exists
in the air, in shape of ammonia and nitric acid, and descends, in these
combinations, with the rain which falls on the ground, satisfies, under
ordinary circumstances, the requirements of the clover-crop. This crop
causes a large accumulation of nitrogenous matters, which are gradually
changed in the soil into nitrates. The atmosphere thus furnishes
nitrogenous food to the succeeding wheat indirectly, and, so to say,
gratis.
“10. Clover not only provides abundance of nitrogenous food, but
delivers this food in a readily available form (as nitrates), more
gradually and continuously, and, consequently, with more certainty of a
good result, than such food can be applied to the land in the shape of
nitrogenous spring top-dressings.”
“Thank you Charley,” said the Doctor, “_that is the most remarkable
paper I ever listened to_. I do not quite know what to think of it. We
shall have to examine it carefully.”
“The first three propositions in the Summary,” said I, “are
unquestionably true. Proposition No. 4, is equally true, but we must be
careful what meaning we attach to the word ‘accumulate.’ The idea is,
that clover gathers up the nitrogen in the soil. It does not _increase_
the absolute amount of nitrogen. It accumulates it--brings it together.
“Proposition No. 5, will not be disputed; and I think we may accept No.
6, also, though we can not be sure that allowing clover to go to seed,
had anything to do with the increased quantity of clover-roots.
“Proposition No. 7, may or may not be true. We have no proof, only a
‘probability;’ and the same may be said in regard to propositions Nos.
8, 9, and 10.”
The Deacon seemed uneasy. He did not like these remarks. He had got the
impression, while Charley was reading, that much more was proved than
Dr. Vœlcker claims in his Summary.
“I thought,” said he, “that on the part of the field where the clover
was allowed to go to seed, Dr. Vœlcker found a great increase in the
amount of nitrogen.”
“That seems to be the general impression,” said the Doctor, “but in
point of fact, we have no proof that the growth of clover, either for
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Talks on Manures A Series of Familiar and Practical Talks Between the Author and the Deacon, the Doctor, and Other Neighbors, on the Whole Subject
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