Fundamentals of Nitrogen Cycle

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    FUNDAMENTALS OFNITROGEN CYCLE

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    The nitrogen cycle is the set ofbiogeochemical processes by whichnitrogen undergoeschemical reactions, changes form,and moves

    Nitrogen is required for all organisms

    to live and grow because it is theessential component ofDNA, RNA,and protein. However, most

    organisms cannot use atmosphericnitro en, the lar est reservoir.

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    The five processes in the nitrogencycle -- fixation, uptake,mineralization, nitrification, anddenitrification -- are all driven bymicroorganisms.

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    NITROGEN

    CYCLE

    Nitrogen (N) is

    an essentialcomponent of

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    The inert nature of N2 means thatbiologically available nitrogen is often

    in short supply in natural ecosystems,limiting plant growth and biomassaccumulation.

    Nitrogen is an incredibly versatileelement, existing in both inorganicand organic forms as well as manydifferent oxidation states. The

    movement of nitrogen between theatmosphere, biosphere, andgeosphere in different forms is

    described by the nitrogen cycle(Fi ure 1), one of the ma or

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    Nitrogen Cycle:

    Figure 1:Thenitrogen

    cycle.Yellowarrowsindicate

    humansourcesofnitrogento the

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    Five mainprocesses cycle

    nitrogen throughthe biosphere,atmosphere, andgeosphere:

    nitrogen fixation,nitrogen uptake(organismalgrowth), nitrogen

    mineralization

    As microbiallymediated

    processes, thesenitrogentransformationstend to occur

    faster thangeologicalprocesses likeplate motion, a

    very slow, purely

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    Figure 2:

    Part of aclover rootsystembearingnaturallyoccurringnodules ofRhizobium,bacteria thatcan fixatmospheric

    nitrogen.Each noduleis about 2-3mm long.

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    Nitrogen fixationN2 NH4+ Nitrogen fixation is the

    process wherein N2 is converted toammonium, essential because it is the

    only way that organisms can attainnitrogen directly from the atmosphere.Certain bacteria, for example thoseamong the genusRhizobium, are the

    only organisms that fix nitrogen throughmetabolic processes. Nitrogen fixingbacteria often form symbiotic

    relationships with host plants. Thiss mbiosis is well-known to occur in the

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    In addition to nitrogen fixing bacteria, high-energynatural events such as lightning, forest fires, and

    even hot lava flows can cause the fixation ofsmaller, but significant amounts of nitrogen(Figure 3). The high energy of these naturalphenomena can break the triple bonds of N2molecules, thereby making individual N atoms

    available for chemical transformation.

    Within the last century, humans have become asimportant a source of fixed nitrogen as all naturalsources combined. Burning fossil fuels, using

    synthetic nitrogen fertilizers, and cultivation oflegumes all fix nitrogen. Through these activities,humans have more than doubled the amount offixed nitrogen that is pumped into the biosphereevery year (Figure 3), the consequences of whichare discussed below.

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    Figure 3: Recent

    increases inanthropogenic Nfixation in relationto natural Nfixation. Modified

    from Vitousek, P. M.and P. A. Matson(1993). Agriculture,the global nitrogencycle, and trace gasflux. TheBiogeochemistry ofGlobal Change:Radiative TraceGases. R. S.Oremland. New

    York, Chapman andHall: 193-208.

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    Nitrogen uptake

    NH4+ Organic N The ammoniaproduced by nitrogen fixing bacteriais usually quickly incorporated into

    protein and other organic nitrogencompounds, either by a host plant,the bacteria itself, or another soil

    organism. When organisms nearerthe top of the food chain (like us!)eat, we are using nitrogen that hasbeen fixed initially by nitrogen fixing

    bacteria.

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    Nitrogen mineralization

    Organic N NH4+ After nitrogen isincorporated into organic matter, it isoften converted back into inorganic

    nitrogen by a process called nitrogenmineralization, otherwise known asdecay. When organisms die,

    decomposers (such as bacteria andfungi) consume the organic matter andlead to the process of decomposition.During this process, a significant

    amount of the nitrogen contained

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    Nitrification

    NH4+ NO3- Some of the ammoniumproduced by decomposition isconverted to nitrate via a process

    called nitrification. The bacteria thatcarry out this reaction gain energy fromit. Nitrification requires the presence ofoxygen, so nitrification can happen

    only in oxygen-rich environments likecirculating or flowing waters and thevery surface layers of soils andsediments. The process of nitrificationhas some im ortant conse uences.

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    Denitrification

    NO3- N2+ N2O Through denitrification,oxidized forms of nitrogen such asnitrate and nitrite (NO2-) are converted

    to dinitrogen (N2) and, to a lesserextent, nitrous oxide gas.Denitrification is an anaerobic process

    that is carried out by denitrifyingbacteria, which convert nitrate todinitrogen in the following sequence:NO3- NO2- NO N2O N2.

    Nitric oxide and nitrous oxide are both

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    Human alteration of the N cycle andits environmental consequences:

    Early in the 20th century, a Germanscientist named Fritz Haber figured outhow to short circuit the nitrogen cycle

    by fixing nitrogen chemically at hightemperatures and pressures, creatingfertilizers that could be added directly

    to soil. This technology has spreadrapidly over the past century, and,along with the advent of new cropvarieties, the use of synthetic nitrogen

    fertilizers has led to an enormous boom

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    Not all of the nitrogen fertilizer appliedto agricultural fields stays to nourish

    crops. Some is washed off ofagricultural fields by rain or irrigationwater, where it leaches into surface orground water and can accumulate. Ingroundwater that is used as a drinkingwater source, excess nitrogen can leadto cancer in humans and respiratory

    distress in infants. The U.S.Environmental Protection Agency hasestablished a standard for nitrogen indrinking water of 10 mg per liter

    nitrate-N. Unfortunately, many systems

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    Reactive nitrogen (like NO3- and NH4+)present in surface waters and soils, can

    also enter the atmosphere as thesmog-component nitric oxide (NO) andthe greenhouse gas nitrous oxide(N2O). Eventually, this atmosphericnitrogen can be blown into nitrogen-sensitive terrestrial environments,causing long-term changes. For

    example, nitrogen oxides comprise asignificant portion of the acidity inacid rain which has been blamed forforest death and decline in parts of

    Europe and the Northeast United

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    Currently, much research is devoted to

    understanding the effects of nitrogenenrichment in the air, groundwater, andsurface water. Scientists are also

    exploring alternative agriculturalpractices that will sustain highproductivity while decreasing thenegative impacts caused by fertilizer

    use. These studies not only help usquantify how humans have altered thenatural world, but increase ourunderstanding of the processesinvolved in the nitro en c cle as a

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