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Nitrogen Cycle
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Sources Lightning Inorganic fertilizers Nitrogen Fixation
Animal Residues Crop residues Organic fertilizers
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Forms of Nitrogen Urea CO(NH2)2 Ammonia NH3 (gaseous)
Ammonium NH4 Nitrate NO3 Nitrite NO2 Atmospheric Dinitrogen N2 Organic N
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Global Nitrogen Reservoirs
Metric tons nitrogen Actively cycled Atmosphere 3.9*1015 No Ocean soluble salts Biomass 6.9*1011 5.2*108 Yes Land organic matter Biota 1.1*1011 2.5*1010 Slow
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Roles of Nitrogen Plants 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 for
amino acids nucleic acids (purine, pyrimidine) cell wall components of bacteria (NAM).
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Nitrogen Cycles Ammonification/mineralization Immobilization
Nitrogen Fixation Nitrification Denitrification
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R-NH2 NH4 NO2 NO3 NO N2O N2
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Ammonification or Mineralization
NH4 NO2 R-NH2 NO NO2 NO3
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Mineralization or Ammonification
Decomposers: earthworms, termites, slugs, snails, bacteria, and fungi Uses extracellular enzymes initiate degradation of plant polymers Microorganisms 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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Immobilization The opposite of mineralization
Happens when nitrogen is limiting in the environment Nitrogen limitation is governed by C/N ratio C/N typical for soil microbial biomass is 20 C/N < 20 Mineralization C/N > 20 Immobilization
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Nitrogen Fixation N2 N2O NH4 NO2 R-NH2 NO NO2 NO3
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Nitrogen Fixation Energy intensive process :
N2 + 8H+ + 8e 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 fixing
Azobacter Beijerinckia Azospirillum Clostridium Cyanobacteria Require the enzyme nitrogenase Inhibited by oxygen Inhibited by ammonia (end product)
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Rates of Nitrogen Fixation
N2 fixing system Nitrogen Fixation (kg N/hect/year) Rhizobium-legume Cyanobacteria- moss 30-40 Rhizosphere associations 2-25 Free- living 1-2
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Applications to wetlands
Occur in overlying waters Aerobic soil Anaerobic soil Oxidized rhizosphere Leaf or stem surfaces of plants
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Bacterial Fixation Occurs mostly in salt marshes
Is absent from low pH peat of northern bogs Cyanobacteria found in waterlogged soils
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Nitrification N2 N2O NH4 NO2 R-NH2 NO NO2 NO3
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Nitrification Two step reactions that occur together :
1rst step catalyzed by Nitrosomonas 2 NH O2 2 NO2- +2 H2O+ 4 H+ 2nd step catalyzed by Nitrobacter 2 NO2- + O2 2 NO3-
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If pH < 6.0 rate is slowed If pH < 4.5 reaction is inhibited
Optimal pH is between 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 N2 N2O NH4 NO2 R-NH2 NO NO2 NO3
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Denitrification Removes a limiting nutrient from the environment
4NO3- + C6H12O6 2N2 + 6 H20 Inhibited by O2 Not inhibited by ammonia Microbial reaction Nitrate is the terminal electron acceptor
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Looking at the Nitrogen cycle through the eye of NH4
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Surface water Low [NH4] Oxidized layer Biodegradation Reduced soil layer Slow Diffusion C/N <20 C/N >20 [NH4] HIGH
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Surface water nitrification Low [NH4] Oxidized layer [NO3] high Reduced soil layer Slow Diffusion [NH4] HIGH
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N2 Surface water Oxidized layer [NO3] high Leaching Reduced soil layer [NO3] Low Denitrification
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QUESTIONS ?
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