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Corn
& The Environment
Corn,
Soil Structure & Erosion
Good
soil structure is important in allowing crop plants to yield well, and
in helping resist erosion caused by the action of rainfall, melting snow
in early spring, and wind.
Corn
has strengths and weaknesses as a "soil building crop."
The
strengths include the high photosynthetic rate and high dry matter yields
produced by corn plants. More organic matter is returned annually to the
soil with corn than with any other Canadian farm crop.
The
large amount of soil tillage traditionally associated with seed-bed preparation
and weed control meant high rates of soil organic matter oxidation (breakdown).
However, as discussed in an earlier section, newer conservation tillage
methods have reduced this loss, resulting in soil organic matter build-up
with corn production.
Corn
provides good "canopy" protection of soil surface during midsummer
months, thereby reducing the potential for erosion caused by rainfall.
A
negative with corn, however, is the relative slow rate at which ground
cover is established in springtime, compared to crops such as perennial
forages and winter cereals. This "flaw" can be countered, in
large part, by the use of conservation tillage methods which leave the
residues of previous crops on the soil surface for over-winter and early-spring
protection.
High
levels of soil erosion can also result in the loss of nutrients attached
to soil particles. This is especially important for phosphate which has
been a water pollutant in the Great Lakes. The control of soil erosion
and the use of soil tests which ensure that excessive phosphate fertilizer
is not applied are means of reducing water contamination by phosphates.
One
weakness with corn as a soil building crop involves the fact that its
roots are coarse and deeply penetrating. While this helps to improve the
structure of deeper soil layers, it is less effective in stabilizing surface
soil than are the fine, shallow roots of crops such as perennial grass
species and winter cereals.
In
practice, corn is now almost always grown in a crop rotation. Rotations
with soybeans, winter wheat, spring-seeded small grain cereals, and/or
perennial forages are most common. Each species has its own unique strengths
and weaknesses as a soil-building crop, and the different rotational crop
species tend to complement each other.
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