Nitrogen Fixation

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Nitrogen Fixation

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Nitrogen fixation refers to the chemical conversion of nitrogen gas (dinitrogen, N2) to an oxidized form (a form with fewer electrons), usually nitric oxide (NO) or ammonia (NH3). Nitrogen fixation can occur through inorganic reactions that do not involve living organisms 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.

Land–based ecosystems fix about 135 million metric tons of nitrogen each year. Marine ecosystems fix about 40 million metric tons annually. Atmospheric dinitrogen can be fixed by inorganic reactions occurring in combustion, lightning strikes, and other circumstances involving high temperatures. Overall, naturally occurring non-biological fixation has been estimated to be equivalent to 10–20% of biological fixation of dinitrogen.

Nitrogen fixation is also associated with certain human activities. The internal combustion engines of automobiles burn fuels under conditions of very high temperature and pressure which favors the oxidation of nitrogen gas to nitric oxide, an important air pollutant and source of fixed nitrogen. The combustion of coal and other organic fuels also results in the formation of nitric oxide through both the fixation of nitrogen gas and the oxidation of the organic nitrogen of the fuel. Also, nitrogen gas is fixed industrially in enormous amounts to provide agricultural fertilizers.

Biological nitrogen fixation is accomplished through the action of an enzyme known as nitrogenase. Nitrogenase consists of two distinct proteins which contain molybdenum, iron, and sulfur. Because the nitrogenase proteins are denatured by exposure to oxygen (O2), they can only operate in an anaerobic environment.

The nitrogenase enzyme can cleave other triple bonds in addition to that of dinitrogen gas. One example is the triple bond that exists in acetylene. Most assays of nitrogen fixation rates take advantage of this fact, measuring nitrogenase activity through the rate at which ethylene is generated by the reaction of acetylene with nitrogenase.

Only certain microorganisms can synthesize the nitrogenase enzyme. Some of these microbes are free–living in soils and water, while others occur in mutualisms with fungi or plants.

A large number of free–living bacteria of anaerobic environments have the ability to fix nitrogen, including the genus Clostridium. Fewer genera of aerobic bacteria have this ability. Free–living nitrogen fixation occurs most vigorously in habitats containing large quantities of carbon–rich organic debris such as rotting logs, heaps of sawdust, and compost piles.

Blue-green bacteria are free-living, photosynthetic microbes that fix nitrogen in aquatic habitats and moist soil, including the genera Anabaena, Nostoc, and Calothrix. Strains of these microbes also live in mutualisms with certain fungi in a symbiosis known as lichens which have an ability to fix nitrogen. Anabaena and Nostoc also occur in a mutualism with the floating aquatic fern Azolla which can be cultivated on the surface of rice paddies to fix nitrogen at a rate as great as 100–150 kg N/ha.yr, saving on the use of synthetic fertilizer.

Nitrogen-fixing bacteria can also occur in mutualisms with certain vascular plants. The best known of these associations are with species of legumes (order Leguminosae). About one–half of the world’s 10,000 species of legumes occur in a nitrogen–fixing mutualism with bacteria in the genus Rhizobium. About 50 of these species are utilized in agriculture, for example, the food crops garden pea (Pisum sativum ), broad bean (Vicia faba ), and soybean (Glycine max ), and the soil conditioners red clover (Trifolium pratense ) and alfalfa (Medicago sativa ). The strain of Rhizobium is specific to each legume species.

Rhizobium occurs in specialized nodules on the roots of the legumes. These are developed when the soil–dwelling Rhizobium invades a root hair, stimulating the plant to form a nodule. Nodule development is inhibited in acidic soils and if the concentrations of nitrate in soil are large. To protect the nitrogenase enzyme, the interior of the nodules is anaerobic. This is due in part to the presence of an oxygen–binding pigment known as leghaemoglobin which colors the nodule interior a dark red. The leghaemoglobin also serves as an oxygen carrier important for other aspects of bacterial metabolism, in this way performing a similar function as the haemoglobin of animals.

Several hundred species in other plant families also develop root nodules that can fix nitrogen. The best known of these are the woody plants known as alders (Alnus spp. ), which develop nodules containing actinomycetes in the genus Frankia. that are known to fix nitrogen include the genera Casuarina, Ceanothus, Myrica, Dryas, and Shepherdia, variously associated with fungi, actinomycetes, or bacteria.

Some species of grasses occur in a relatively loose, non-obligate mutualism with nitrogen–fixing microorganisms. These associative symbioses include those of the crabgrass Digitaria with the bacterium Spirillum and that of another weedy grass, Paspalum, with Azotobacter. Although these nitrogen–fixing symbioses do not involve agriculturally important species of plants, they may nevertheless prove to be significant. Research is being conducted into the possibility of transferring the associative ability of nitrogen fixation of these species into grasses that are important in agriculture, such as corn (Zea mays ) and wheat (Triticum aestivum ). If this feat of bioengineering could be accomplished, it could lead to significant savings of nitrogen fertilizer which must be manufactured using non-renewable resources.

One last example of a nitrogen–fixing mutualism involves termites. These insects have a bacterium, Enterobacter agglomerans, in their gut that fixes nitrogen. This is important to termites because their diet of cellulose is highly deficient in nitrogen.

Resources

BOOKS

Freedman, Jeri. Climate Change: Human Effects On The Nitrogen Cycle. New York: Rosen Publishing Group, 2006.

Leigh, G.J. The World’s Greatest Fix: A History of Nitrogen and Agriculture. Oxford: Oxford University Press, 2004.

Lovelock, James. The Revenge of Gaia: Earth’s Climate Crisis and the Fate of Humanity. New York: Basic Books, 2006.

Bill Freedman

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