Apart from
the special roles of organic matter in the soil formation and fertility,
weathering and decomposition of soil mineral, formation of soil structure,
source of carbon and mineral nutrients as well as growth and development of
plants. The following are the functions of organic matter in soil generally;
The more or
less stable end product of composition and synthesis of organic matter is a
store house for the exchangeable and available cation. This humus helps to
reduce nutrient loss through leaching.
Organic matter
increases the buffer capacity of soil. It also helps to buffer the soil against
rapid chemical changes which may occur.
It reduces
the impact of rain drops on soil surfaces thereby reducing the susceptibility
of the soil to erosion.
Acids
produce during decomposition help in release of nutrients. More so, some acids
produce during decomposition help in the dissolving of minerals thus making it
more available to plants for their growth and development.
Organic matter
increases the amount of available water in sandy and loaming soil. The granular
structure got from organic matter supply more water than sticky and impervous
soils.
Roots of
death plants and decayed ones. When roots die and decay, they provide channels
through which new plant root grows more luxuriantly.
Organic matter
is a source of food/energy to both macro and micro organisms living in the
soil.
Organic matter
in the soil makes phosphorus more available to acid soils. As organic matter
decomposes it releases lactates, oxalates, citrate acids which combine with
phosphorus easily and makes phosphorus easily available.
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