The Farm That Won't Wear OutHopkins, Cyril G. (Cyril George)
Science
The Farm That Won't Wear Out
Hopkins, Cyril G. (Cyril George)
Agriculture; Fertilizers; Soils
Probably there has never been a greater waste of time and effort in
the name of science than in the endeavor to determine the
"available" plant food in soils. The almost universal assumption has
been that the plant food in the soil exists in two distinct
conditions, "available" and "unavailable," and that the
determination of the "available" plant food would reveal both the
crop-producing power of the soil and the fundamental fertilizer
requirements for the improvement of the soil for crop production.
After ascertaining the total stock of plant food in the plowed soil,
the next important question is not how much is "available," but
rather how much can be made available during the crop season, year
after year. In other words we must make plant food available by
practical methods of liberation, by converting it from insoluble
compounds into soluble and usable forms; for plant food must be in
solution before the plant can take it from the soil. For the
present, space is taken only to emphasize the value of decaying
organic manures in the important matter of making plant food
available; and attention is also called to the fact that the
decomposition of the organic matter of the soil--including both
fresh materials and old humus--is hastened by tillage and by
underdrainage, which permit the oxygen of the air to enter the soil
more freely, oxygen being a most active agent in nitrification and
other decomposition processes of organic matter, as well as in the
more common combustion of wood, coal, and so forth.
The Renewal of Fertility
In rational systems of general farming the supply of any element
which is normally very abundant may be renewed from the subsoil by
even the very slight erosion which occurs on all ordinary lands in
humid sections. This statement applies to iron and potassium, and
often to magnesium.
If two million pounds of normal surface soil contain 30,000 pounds
of potassium, one inch an acre would contain 4500 pounds of that
element; and if a third of this--1500 pounds--were removed by
cropping and leaching before its removal by surface washing, then
two-thirds of a century could be allowed for the erosion of one inch
of soil, with crop yields of 50 bushels of wheat, 100 bushels of
corn and oats, and 4 bushels of clover seed to the acre, provided
the stalks, straw and clover hay were returned to the land, either
directly or in farm manure. This amount of surface washing is likely
to occur on land sufficiently undulating for good surface drainage,
provided the land is plowed and cultivated as frequently as would be
required for a four-year rotation as suggested above. Where hay,
straw, potatoes, root crops or common market garden crops are sold,
very much larger amounts of potassium leave the farm than in grain
farming or live-stock farming, and in such cases potassium must
ultimately be purchased and returned to the soil, either in
commercial form or in animal manures from the cities.
Thirty Bushels for Potassium
Public-domain text, read in full here on John Shaqi.
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