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  • Nitrification

Denitrification

Denitrification

Nitrogen transformations in soil result in the loss of molecular nitrogen. The conversion of nitrate and nitrite into molecular nitrogen or nitrous oxide through microbial processes is known as denitrification. The escape of molecular nitrogen into the atmosphere, also known as volatilization of nitrogen is a drain on the availability of this vital element in soil for crop growth.

Denitrification of bound nitrogen to gaseous nitrogen is mediated by numerous species of bacteria which normally use oxygen of the air as hydrogen acceptor (aerobically) but also possess the ability to use nitrates and nitrites in the place of oxygen (anaerobically). Thus these bacteria have the faculty to grow aerobically in the absence of nitrate but anaerobically in the presence of nitrate. The anaerobically conversion of nitrate into molecular nitrogen is also known as nitrate respiration. In fact such or­ganisms capable of denitrification are isolated by enrichment cultures in anaerobic media containing excess of potassium nitrate.

The bacterial genera which bring about denitrification are Pseudomonas, Achromobacter, Bacillus and Micrococcus. Of these, Pseudomonas and Achromobacter are the predominant ones in soil. The biochemical reactions can be summed up as:

2NO3 - (nitrate) + 10H Denitrification N2 + 4H20 + 20H- or
2NO2- (nitrite) + 6HDenitrificationN2 + 2H20+ 20H- or
N2O (nitrous oxide) + 2 H DenitrificationN2 + H2O.
In short, the denitrification pathway can be depicted as NO2- (nitrate ® NO-2
(nitrate) ® NO (nitric oxide) ® N2O (nitrous oxide) ® N2 (dinitrogen)
Many soil bacteria like Thiobacillus denitrificans which are known to oxidize sulphur chemoautotrophically also reduce nitrate to nitrogen. The source of energy is sulphur or thiosulphate and this energy is used to convert nitrate into molecular nitrogen. The biochemical reactions can be summarised as:

5S + 6KNO3 + 2H20 Denitrification 3N2 + K2SO4 + 4KHSO4 or
5K2S203 + 8KNO3 + H2O Denitrification 4H2 + 9K2SO4 + H2SO4.

Fallow soils flooded with water are more congenial for denitrification than well drained and continuously cropped soils. In fact, the practice of continuous cropping which provides the much needed competition bet­ween plants and microorganisms for nitrate substrates minimizes the hazards of denitrification.

The denitrification process, besides depleting the fertility of soils, is also a cause for eutrophication of coastal waters because nitrate is a pollutant especially of drinking water. The process also influences the chemistry of the atmosphere by producing nitrous oxide a 'green house gas' that destroys the ozone (03) of the stratosphere.

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