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
HISTORICAL REVIEW OF SOIL INVESTIGATION.
While the obvious importance of the physical soil-conditions has long
ago rendered them subjects of close study by Schübler[106] Boussingault
and others, the chemistry of soils was very generally neglected for a
considerable period, after the hopes at first entertained by Liebig
that chemical analysis would furnish a direct indication and measure
of soil fertility, had been sorely disappointed in respect to the only
soils then investigated, viz., the long-cultivated ones of Europe. The
results of chemical analysis sometimes agreed, but as often pointedly
disagreed, with cultural experiences; so that after the middle of the
nineteenth century, but few thought it worth while to occupy their time
in chemical soil analysis.
[106] The early work of Schübler on soil physics, published at Leipzig
in 1838 under the title of “Grundsätze der Agrikulturchemie” and now
almost inaccessible outside of old libraries, is remarkable as having
anticipated very definitely much that has since been brought forward
and elaborated anew. He is really the father of agricultural physics.
_Popular Forecasts of Soil Values._—In newly-settled countries, and
still more in those yet to be settled, the questions of the immediate
productive capacity, and the future durability of the virgin land are
the burning ones, since they determine the future of thousands for
weal or woe. This need has long ago led to approximate estimates made
on the part of the settler, by the _observation of the native growth,
especially the tree growth_; and where this consists of familiar
species, normally developed, such estimates on the part of experienced
men, based on previous cultural experience, are generally very
accurate; so much so that in many of the newer states they have been
adopted in determining not only the market value, but also the tax rate
upon such lands, their productiveness, and probable durability being a
matter of common note.
Thus in the long-leaf pine uplands of the Cotton States, the
scattered settlements have fully demonstrated that after
two or three years cropping with corn, ranging from as much
as 25 bushels per acre the first year to ten and less the
third, fertilization is absolutely necessary to farther
paying cultivation. Should the short-leaved pine mingle with
the long-leaved, production may hold out for from five to
seven years. If oaks and hickory are superadded, as many
as twelve years of good production without fertilization
may be looked for by the farmer; and should the long-leaved
pine disappear altogether, the mingled growth of oaks and
short-leaved pine will encourage him to hope for from twelve
to fifteen years of fair production without fertilization.
Public-domain text, read in full here on John Shaqi.
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