The Elements of Agriculture: A Book for Young Farmers, with Questions Prepared for the Use of Schools — John Shaqi
The Elements of Agriculture: A Book for Young Farmers, with Questions Prepared for the Use of SchoolsWaring, George E. (George Edwin)
Science
The Elements of Agriculture: A Book for Young Farmers, with Questions Prepared for the Use of Schools
Waring, George E. (George Edwin)
Agriculture
What do we mean by the mechanical character of the soil?
Is its fertility indicated by its mechanical character?]
As a general rule, it may be stated that _all rocks are either
sandstones, limestones, or clays; or a mixture of two or more of these
ingredients_. Hence we find that all mineral soils are either _sandy_,
_calcareous_, (limey), or _clayey_; or consist of a mixture of these, in
which one or another usually predominates. Thus, we speak of a sandy
soil, a clay soil, etc. These distinctions (sandy, clayey, loamy, etc.)
are important in considering the _mechanical_ character of the soil, but
have little reference to its fertility.
By _mechanical_ character, we mean those qualities which affect the ease
of cultivation--excess or deficiency of water, ability to withstand
drought, etc. For instance, a heavy clay soil is difficult to
plow--retains water after rains, and bakes quite hard during drought;
while a light sandy soil is plowed with ease, often allows water to pass
through immediately after rains, and becomes dry and powdery during
drought. Notwithstanding those differences in their mechanical
character, both soils may be very fertile, or one more so than the
other, without reference to the clay and sand which they contain, and
which, to _our observation_, form their leading characteristics. The
same facts exist with regard to a loam, a calcareous (or limey) soil, or
a vegetable mould. Their mechanical texture is not essentially an index
to their fertility, nor to the manures required to enable them to
furnish food to plants. It is true, that each kind of soil appears to
have some general quality of fertility or barrenness which is well known
to practical men, yet this is not founded on the fact that the clay or
the sand, or the vegetable matter, enter more largely into the
constitution of plants than they do when they are not present in so
great quantities, but on certain other facts which will be hereafter
explained.
[What is a sandy soil? A clay soil? A loamy soil? A marl? A
calcareous soil? A peaty soil?]
As the following names are used to denote the character of soils, in
ordinary agricultural description, we will briefly explain their
application:
A _Sandy soil_ is, of course, one in which sand largely predominates.
_Clay soil_, one where _clay_ forms a large proportion of the soil.
_Loamy soil_, where sand and clay are about equally mixed.
_Marl_ contains from five to twenty per cent. of carbonate of lime.
_Calcareous soil_ more than twenty per cent.
_Peaty soils_, of course, contain large quantities of organic matter.[P]
[How large a part of the soil may be used as food by plants?
What do we learn from the analyses of barren and fertile soils?]
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