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Ecological Importance of Denitrification

Ecological Importance of Denitrification
Denitrification plays an important role in soil ecology. Soil is depleted of essential nutrients for plants by denitrification. The rate of denitrification is controlled by the amount of oxygen.

Denitrification can occur only when the oxygen tension is very low. Even 1 % oxygen depresses nitrification to about 12%. The gaseous products of denitrification appear in the order nitric oxide, nitrous oxide and molecular nitrogen.

Molecular nitrogen accounts for 83-95% of the nitrate present in the soil, and nitric oxide for 5%. Appreciable reduction of nitrate to nitrite occurs only in the presence of good concentrations of organic matter and low oxygen levels (7%). Denitrification decreases the fertility of the soil, and consequently agricultural productivity.

The highly soluble nitrate ion may be leached from soils into fresh waters. High concentrations of nitrate are toxic, and therefore denitrification maintains the potability of fresh waters. Nitrate ions leached from the soil are eventually carried to the oceans. If denitrification did not take place, the earth’s supply of nitrogen, including atmospheric nitrogen, would and up in the oceans. Life would not be possible on land masses, except near the shores of oceans.

Loss of nitrogen by denitrification occurs during seasonal flooding of the land, or as a result of over irrigation of poorly drained land. Constantly wet soils have low concentrations of oxygen. This promotes the growth of nitrate reducing anaerobic species and denitrification, resulting in poor fertility of the soil.

 

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