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Nitrogen Cycle

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Encyclopedia of Soil Science

Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

As a constituent of cell proteins nitrogen is an indispensable nutrient for all living organisms, and although approximately three quarters of the atmosphere (about 386 Ă— 10 13 t) is made up of dinitrogen gas (N 2) the element is always a limiting factor in the growth of plants and animals since it cannot be assimilated by most organisms in elemental form. Animals derive their nitrogen from plant sources, and plants manufacture their protein mostly from soil nitrogen. The latter is present in complex organic combinations, which, like nitrogen gas, cannot be used directly by plants. Only one to two percent of the total nitrogen in the soil is present in inorganic forms (mostly as ammonium or nitrate, occasionally as nitrite) and it is this that can be assimilated by plants. Nitrite, which at high levels is toxic to plants, has only a transitory existence in aerated soils, being readily oxidized to nitrate.

The path of nitrogen in the biosphere can be viewed as a cycle of reactions...

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Arbestain, M.C., MacĂ­as, F., Chesworth, W., Chesworth, W., Spaargaren, O., Semoka, J. (2008). Nitrogen Cycle. In: Chesworth, W. (eds) Encyclopedia of Soil Science. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3995-9_381

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