A Living from the LandDuryee, William B. (William Budington)
History
A Living from the Land
Duryee, William B. (William Budington)
Agriculture
Don't install electrical service without full attention to principles of
convenience, safety and economy involved.
_Chapter_ VI
MAKING THE SOIL PRODUCE CROPS
There are many treatises available that deal with the soil, its
composition and its treatment. No attempt will be made here to go
exhaustively into that subject. There are a few fundamental factors,
however, which the potential owner should know regarding soil treatment,
for that is the base upon which he will build his income-producing
operations.
The particles of soil have had their genesis in rock. The rock has become
disintegrated and decomposed through natural processes. The action of the
weather is the most important factor in creating soil. Water falling on
rock not only wears it away mechanically, but through certain mild acid
elements which it acquires, disintegrates the binding materials that hold
rock segments together. In addition, there is the action of frost and
freezing, too, making the moisture in rock expand and contract and thereby
causing the breaking down of the segments. With this action is coupled
that of hot suns which cause expansion and breaking up of the rock as it
becomes heated and cooled under atmospheric influence.
A great deal of the soil surface in many sections of the country is the
result of glacial action. These glaciers not only eroded the surface,
thereby creating millions of rock particles, but they also carried large
deposits of the rock particles to more distant areas and deposited them
over a subsoil that may be totally different in character from the surface
soil thus deposited.
_How Tillable Soil Is Made._--The action of plants themselves has a great
effect in adding to our supply of tillable soil. Seeds of plants or seeds
of trees become established in some slightly weathered rock areas and
begin to grow. The roots penetrate wherever there is any loose soil, and
partly by their pressure and partly through the acidity accompanying
decomposing plant tissue, complete a further breaking down of the rock.
There is a continuous process of destruction of rocks and leveling off of
mountains and hills to fill the valleys below.
Many groups of deep-rooted plants tend to increase the depth of the
surface soil by growth of the roots in the subsoil and by creating therein
a condition approaching that which already exists on the surface. The
action of earth worms and similar forms of life in bringing subsoil to
the top and in opening channels through which water and surface air can
penetrate constitutes another continually operating force in the creation
of a productive soil. A deeper layer of productive soil can also be
created through a plan of consistently deeper plowing, bringing up with
each annual plowing operation a small portion of subsoil which, when mixed
with the surface soil, tends to become like it.
[Illustration: (_Courtesy New Jersey Department of Conservation and
Development_)
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