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Nitrogen Fixation - Inorganic Nitrogen Fixation, Biological Nitrogen Fixation

tons ecosystems estimated terrestrial

Nitrogen fixation refers to the chemical conversion of nitrogen gas (dinitrogen, N2) to some oxidized form, usually nitric oxide (NO) or ammonia (NH3). Nitrogen fixation can occur through inorganic reactions or as a result of biological processes. Because the nitrogen atoms in dinitrogen are bound by a very strong triple bond, this gas is very stable and cannot be utilized as a source of nutrition by any but a few highly specialized microorganisms. These nitrogen-fixing microbes are critically important ecologically because nitrogen fixation is the ultimate source of the capital of available organic nitrogen in ecosystems.

It has been estimated that terrestrial ecosystems fix about 135 million metric tons of nitrogen/year (106 tons N/yr), and marine ecosystems 40 × 106 tons N/yr. The terrestrial fixation most commonly occurs in agroecosystems in which legumes are cultivated which fix an estimated 44 × 106 tons N/yr, while grasslands fix 45 × 106 tons N/yr, forests 40 × 106 tons N/yr, and all other terrestrial ecosystems 10 × 106 tons N/yr. Industrial fixation of nitrogen for the manufacturing of synthetic fertilizers contributed another 30 × 106 tons N/yr in the early 1980s, while fixation during combustion accounts for 19 × 106 tons N/yr. Because of increasing demands for nitrogen fertilizers for agriculture, it has been estimated that industrial fixation could increase to 100 × 106 tons N/yr by the year 2000.


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