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Nitrogen Cycle02

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Page 1: Nitrogen Cycle02
Page 2: Nitrogen Cycle02

SourcesSourcesLightningInorganic fertilizersNitrogen FixationAnimal ResiduesCrop residuesOrganic fertilizers

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FORMS OF NITROGENFORMS OF NITROGENUrea CO(NH2)2

Ammonia NH3 (gaseous)Ammonium NH4

Nitrate NO3

Nitrite NO2

Atmospheric Dinitrogen N2

Organic N

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Global Nitrogen Reservoirs

Nitrogen Reservoir

Metric tons nitrogen

Actively cycled

Atmosphere 3.9*1015 No

Ocean soluble salts

Biomass6.9*1011

5.2*108

YesYes

Land organic matter Biota

1.1*1011

2.5*1010

SlowYes

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ROLES OF NITROGENROLES OF NITROGENPlants and bacteria use nitrogen in the form

of NH4+ or NO3

-

It serves as an electron acceptor in anaerobic environment

Nitrogen is often the most limiting nutrient in soil and water.

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NITROGEN IS A KEY ELEMENT NITROGEN IS A KEY ELEMENT FORFOR

amino acids nucleic acids (purine, pyrimidine) cell wall components of bacteria (NAM).

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NITROGEN CYCLESAmmonification/mineralizationImmobilizationNitrogen Fixation NitrificationDenitrification

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R-NH2

NH4 NO2

NO3NO2

NO

N2O

N2

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R-NH2

NH4 NO2

NO3NO2

NO

N2O

N2

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Mineralization or AmmonificationDecomposers: earthworms, termites,

slugs, snails, bacteria, and fungiUses extracellular enzymes initiate

degradation of plant polymersMicroorganisms uses:Proteases, lysozymes, nucleases to

degrade nitrogen containing molecules

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Plants die or bacterial cells lyse release of organic nitrogen

Organic nitrogen is converted to inorganic nitrogen (NH3)

When pH<7.5, converted rapidly to NH4

Example:

Urea NH3 + 2 CO2

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ImmobilizationmmobilizationThe opposite of mineralizationHappens when nitrogen is limiting in the

environmentNitrogen limitation is governed by C/N

ratioC/N typical for soil microbial biomass is 20C/N < 20 MineralizationC/N > 20 Immobilization

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Nitrogen Fixation

R-NH2

NH4 NO2

NO3NO2

NO

N2O

N2

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Nitrogen FixationNitrogen FixationEnergy intensive process :

N2 + 8H+ + 8e- + 16 ATP = 2NH3 + H2 + 16ADP + 16 Pi

Performed only by selected bacteria and actinomycetes

Performed in nitrogen fixing crops (ex: soybeans)

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Microorganisms fixingMicroorganisms fixingAzobacterBeijerinckiaAzospirillumClostridiumCyanobacteria

Require the enzyme nitrogenase

Inhibited by oxygenInhibited by

ammonia (end product)

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Rates of Nitrogen Rates of Nitrogen FixationFixation

N2 fixing system Nitrogen Fixation (kg N/hect/year)

Rhizobium-legume 200-300

Cyanobacteria- moss

30-40

Rhizosphere associations

2-25

Free- living 1-2

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Applications to Applications to wetlandswetlandsOccur in overlying watersAerobic soilAnaerobic soilOxidized rhizosphereLeaf or stem surfaces of plants

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Bacterial FixationBacterial FixationOccurs mostly in salt marshesIs absent from low pH peat of northern bogsCyanobacteria found in waterlogged soils

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NitrificationNitrification

R-NH2

NH4 NO2

NO3NO2

NO

N2O

N2

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NitrificationTwo step reactions that occur together :

1rst step catalyzed by Nitrosomonas2 NH4

+ + 3 O2 2 NO2- +2 H2O+ 4 H+

2nd step catalyzed by Nitrobacter2 NO2

- + O2 2 NO3-

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Optimal pH is between 6.6-8.0

If pH < 6.0 rate is slowed

If pH < 4.5 reaction is inhibited

In which type of wetlands do you thing Nitrification occurs?

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Denitrification

R-NH2

NH4 NO2

NO3NO2

NO

N2O

N2

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DenitrificationRemoves a limiting nutrient from the

environment4NO3

- + C6H12O6 2N2 + 6 H20

Inhibited by O2

Not inhibited by ammoniaMicrobial reactionNitrate is the terminal electron acceptor

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Surface water

Oxidized layer

Reduced soil layer

[NH4] HIGH

Low [NH4]

Slow Diffusion

Biodegradation

C/N <20

C/N >20

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Surface water

Oxidized layer

Reduced soil layer

[NH4] HIGH

Low [NH4]

Slow Diffusion

nitrification

[NO3] high

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Surface water

Oxidized layer

Reduced soil layer

[NO3] high

Leaching

[NO3] Low

N2

Denitrification

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