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
On my own farm I use about one ton per acre of raw phosphate once
every six years, thus adding at least 250 pounds of phosphorus at a
cost of less than $8; whereas 200 pounds of the common "complete"
fertilizer per acre yearly would cost $12 every six years, and would
supply only 40 pounds of phosphorus. I do not use "complete"
fertilizers, because there is plenty of nitrogen in the air and
plenty of potassium in the soil; and because, by growing and plowing
under plenty of clover, I not only secure nitrogen from the air and
liberate potassium from the soil but also liberate the phosphorus
from the raw rock phosphate applied to the soil. In beginning the
use of raw phosphate where the supply of organic manures is limited,
I apply one ton of phosphate and 600 pounds of kainit in intimate
connection, turn them under, preferably with organic matter, then
add ground limestone if needed, and thus prepare to grow clover.
By far the most important agencies under the farmer's control for
the liberation of plant food are the decomposition products of
fermenting or decaying organic matter, such as green manures, crop
residues and ordinary farm manures. In the decomposition of these
organic materials sour or acid products are formed. Thus vinegar,
containing acetic acid, is formed from the fermentation of apple
juice, hard cider being an intermediate product. Sweet, chopped,
immature field corn becomes sour silage in the silo, lactic, acetic,
carbonic and other acids being formed. By a similar process cabbage
is turned into sauerkraut. Likewise sweet milk becomes sour, with
the formation of lactic acid. Oxalic, citric, tartaric, succinic,
malic, gallic and tannic are other well-known organic acids. Some of
these are contained in the sap or juice of certain plants, and these
or others are formed when crop residues are decomposed in the soil.
In the ultimate decomposition of organic matter the carbon appears
in the form of carbon dioxid which when combined with water forms
carbonic acid. Though this is a very weak acid, its solvent action
is very important.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account