Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regionsHilgard, Eugene W. (Eugene Woldemar)
Science
Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regions
Hilgard, Eugene W. (Eugene Woldemar)
Soils
It is now well understood that its efficacy is largely due to the
important physical effects it produces in the soil. It helps directly
to render heavy clay soils more loose and readily tillable. If well
“rotted” or cured it also serves to render sandy, leachy soils more
retentive of moisture; and the humus formed in its progressive decay
imparts to all soils the highly important qualities discussed later on
(chapt. 8). More than this, the later researches have shown that stable
manure acts perhaps most immediately upon the bacterial activity in the
soil, greatly increasing it not only directly by the vast numbers of
these organisms it brings with it, but also in supplying appropriate
food for those normally existing in the soil (see chapt. 9). In
so doing it serves indirectly to render the soil ingredients more
available, and to impart to the soil the loose condition required in a
good seed-bed—a “tilth” which cannot be brought about by the operations
of tillage alone.
The only possible substitute for the use of stable manure is found
in green-manuring with leguminous crops conjointly with the use of
commercial or mineral fertilizers. Unless this is done the use of the
latter, alone, ultimately leads to a depletion of humus substances,
which renders the acquisition of proper tilth by the seed-bed
impossible, and causes a compacting of the surface soil which no
tillage can remedy.
_Proper method of using stable manure in humid and arid climates._—In
the humid region it is a common practice to spread the stable manure
on the surface of the fields and leave it there without any special
operation to put it into the soil; trusting to the rains, earthworms
and subsequent tillage for its being brought into adequate contact
with the roots; it is rarely plowed in. In the arid region this
mode of using it is impracticable; it would remain on the surface
indefinitely without advancing in its decay because of the dryness, and
unless plowed in very deep the ordinary, strawy manure would ruin the
seed-bed by rendering it too pervious to the dry air, thus preventing
germination. Much of this valuable material has therefore been, and to
some extent is still being burnt, thus causing a severe depletion of
the land, both of humus and of mineral plant-food. The best way to deal
with stable manure in the arid regions is to thoroughly rot or cure it
before putting it on the land, and then plowing it in. To do this of
course it must be put in piles and wetted regularly; a procedure which
at the high prices of labor is thought to be too expensive, but which
in the end would be found eminently profitable, unless green-manuring
is regularly done. The very small proportion of humus generally present
in arid soils renders this precaution indispensable, if production and
proper tilth is to be maintained. The saving of stable manure and of
all composting material, even if less needful as a means of supplying
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