Trotwood's Monthly, Vol. II, No. 2, May, 1906Various
History
Trotwood's Monthly, Vol. II, No. 2, May, 1906
Various
Agriculture -- Southern States -- Periodicals; Horses -- Periodicals; Southern States -- Periodicals
If a post-hole dug three feet deep in the field where it is desired to
sow alfalfa shows water standing in it for more than a few days in the
year, that soil needs under-draining before being sown to alfalfa.
In general, the depth to the water level should be about forty feet. If
there is a greater depth it is generally better.
Now, we will consider the matter of fertility. Alfalfa feeds deep in the
soil after it gets established and it secures a part of its nitrogen
through the aid of the bacteria from the air.
Nevertheless, it is a gross feeder upon phosphorus and potash and cannot
secure these from the air. Nor will it at first secure all its needed
nitrogen from the air.
Therefore, land destined to be sown to alfalfa should be rich when sown.
If it is not rich it should be made rich before seed is consigned to it.
Next, comes the need of humus in the soil. Now “humus” is simply decayed
vegetable matter, and is best supplied through turning under vegetable
growths such as cowpeas, or through the use of stable manures. Humus in
the soil does several very needed things.
First, it supplies a direct plant food through the nitrogen, phosphorus
and potash that it contains, being especially rich in nitrogen.
Next, in decaying it forms compounds that attack the locked-up mineral
elements of the soil and sets them free to be absorbed by the plants.
Then it absorbs moisture and makes the soil more slow in drying, besides
preventing the close packing that comes with puddling in clay soils
deficient in humus.
And as important as anything, perhaps most important of all, it puts
“life” into the soil. Soils with humus in them are really alive, for the
decaying vegetable matter attracts bacteria of many sorts that in their
life and death and decay form many compounds that the plants can absorb
and thus directly increase fertility and make plants grow.
Good soils are truly “live” soils, filled with legions of microscopic
forms of life, most of it beneficial to the higher orders of growing
plants useful to men.
Poor soils, deficient in humus, cold, puddled clays, are literally “dead”
soils and speak sadly of a dying civilization and decaying people.
Alfalfa, then, revels in a deep, rich, sweet soil. How are we to provide
it in the South?
First, there are many river bottoms that are admirably adapted to
alfalfa, being made up of rich alluvial loams, pervious to air and
moisture, and not holding a surplus of moisture. On these soils alfalfa
usually thrives splendidly.
Next, there are new lands freshly cleared where robber crops have not yet
had time to take out the fertility. Often these newer soils will respond
wonderfully with alfalfa. Some very steep mountain sides are growing
alfalfa finely when sown on freshly-cleared surfaces.
Some lands are naturally fertile enough so that they will, with little
aid, grow alfalfa very well. Nevertheless, even the best of the old
cleared parts need manure before being sown to alfalfa.
Public-domain text, read in full here on John Shaqi.
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