Nitrogen is another important property in the soil. It is one of the primary nutrients that is essential to living, grow and reproduce for plants. Nitrogen in soil has two forms as organic nitrogen and inorganic nitrogen.
Most of the nitrogen in the soil is found in organic
material in the soil. The organism in the soil like plants, animals, and microorganism
has lots of compounds that are rich in organic matter. Their wastes and dead
bodies are accumulated in the soil. Organic nitrogen can be found in amino acid
(20-50%), hexamine (5-10%) and amino sugar (1%) in their cells. This nitrogen is
available for plants only after decomposition by soil microorganisms.
Inorganic
nitrogen is accumulated in soil by fixation of atmospheric nitrogen by soil
microorganisms in the soil. The small amount of inorganic nitrogen is produced during
thunderstorms by lighting as NO-3.These
NO-3 are reached to the soil by dissolving in
precipitation as nitric acid.
The soil nitrogen cycle
Degradation of the organic matter
will result in the release of ammonium and nitrate nitrogen, a process called mineralization.
Inorganic nitrogen is added to soil after fixation of atmospheric nitrogen and
organic nitrogen by soil microorganisms.
Mineralization
of nitrogen can be divided into two chemical reactions. They are ammonification
and ammonium hydrolysis. Ammonification
is a transformation of organic nitrogen to ammonia.
R−NH2+H2O→NH3+R−OH+energy
Ammonium hydrolysis is a transformation
of ammonia to ammonium by reacting with water molecules.
NH3+H2O→NH4++OH−
Ammonium is
rapidly converted into nitrate at a high concentration of oxygen called nitrification.
Ammonium is unstable under
aerobic conditions. Nitrification is also divided into two chemical reactions.
Ammonium is transformed into
nitrite in the first step. Nitrosomonas are one of the transforming bacteria of
ammonium to nitrate under aerobic conditions.
2NH4++3O2
→2NO-2 +2H2O+4H+
Oxidation of nitrite is transformed
into nitrate by Nitrobacter under the aerobic condition at the second step.
2NO2− +O2 →2NO3
NO-3 is relatively highly soluble in
water that can be absorbed by roots of plants more easily.NO-3 can be easily
leached through the soil due to the solubility.
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