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Published byAdonis Leppert Modified over 10 years ago
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Nitrogen Cycle
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The nitrogen cycle represents one of the most important nutrient cycles found in terrestrial ecosystems (Figure 9s-1). Nitrogen is used by living organisms to produce a number of complex organic molecules like amino acids, proteins, and nucleic acids. The store of nitrogen found in the atmosphere, where it exists as a gas (mainly N2), plays an important role for life.
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Although we are surrounded by nitrogen gas, and organisms need nitrogen to live, most organisms cannot use the nitrogen gas (N2) found in the air. Nitrogen must be combined with other elements, such as Hydrogen, to be usable by organisms. The process of nitrogen combining with other elements is called nitrogen fixation. The process can be performed by a special type of bacteria that grows on the roots of certain plants, or a lightning bolt can split the two nitrogen atoms, allowing the "free" nitrogen atoms to react with oxygen and hydrogen atoms. These two natural processes produce limited amounts of nitrogen in the environment.
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Animals receive the required nitrogen they need for metabolism, growth, and reproduction by the consumption of living or dead organic matter containing molecules composed partially of nitrogen.
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In most ecosystems nitrogen is primarily stored in living and dead organic matter. This organic nitrogen is converted into inorganic forms when it re-enters the biogeochemical cycle via decomposition. Decomposers, found in the upper soil layer, chemically modify the nitrogen found in organic matter from ammonia (NH3 ) to ammonium salts (NH4+). This process is known as mineralization and it is carried out by a variety of bacteria and fungi.
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