nitrogen cycle

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Nitrogen Cycle

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Page 1: Nitrogen cycle

Nitrogen Cycle

Page 2: Nitrogen cycle

Sources

• Lightning• Inorganic fertilizers• Nitrogen Fixation• Animal Residues• Crop residues• Organic fertilizers

Page 3: Nitrogen cycle
Page 4: Nitrogen cycle

Forms of Nitrogen

• Urea CO(NH2)2

• Ammonia NH3 (gaseous)• Ammonium NH4

• Nitrate NO3

• Nitrite NO2

• Atmospheric Dinitrogen N2

• Organic N

Page 5: Nitrogen cycle

Global Nitrogen ReservoirsNitrogen 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

Page 6: Nitrogen cycle

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.

Page 7: Nitrogen cycle

Nitrogen is a key element for

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

(NAM).

Page 8: Nitrogen cycle

Nitrogen Cycles

• Ammonification/mineralization• Immobilization• Nitrogen Fixation • Nitrification• Denitrification

Page 9: Nitrogen cycle

R-NH2

NH4 NO2

NO3NO2

NO

N2O

N2

Page 10: Nitrogen cycle

Ammonification or Mineralization

R-NH2

NH4 NO2

NO3NO2

NO

N2O

N2

Page 11: Nitrogen cycle

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

Page 12: Nitrogen cycle

• 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

Page 13: Nitrogen cycle

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

Page 14: Nitrogen cycle

Nitrogen Fixation

R-NH2

NH4 NO2

NO3NO2

NO

N2O

N2

Page 15: Nitrogen cycle

Nitrogen Fixation

• Energy 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)

Page 16: Nitrogen cycle

Microorganisms fixing

• Azobacter• Beijerinckia• Azospirillum• Clostridium• Cyanobacteria

• Require the enzyme nitrogenase

• Inhibited by oxygen

• Inhibited by ammonia (end product)

Page 17: Nitrogen cycle

Rates of Nitrogen Fixation

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

Page 19: Nitrogen cycle

Applications to wetlands

• Occur in overlying waters• Aerobic soil• Anaerobic soil• Oxidized rhizosphere• Leaf or stem surfaces of plants

Page 20: Nitrogen cycle

Bacterial Fixation

• Occurs mostly in salt marshes• Is absent from low pH peat of

northern bogs• Cyanobacteria found in

waterlogged soils

Page 21: Nitrogen cycle

Nitrification

R-NH2

NH4 NO2

NO3NO2

NO

N2O

N2

Page 22: Nitrogen cycle

Nitrification

Two step reactions that occur together :

• 1rst step catalyzed by Nitrosomonas2 NH4

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

• 2nd step catalyzed by Nitrobacter

• 2 NO2- + O2 2 NO3

-

Page 23: Nitrogen cycle

• 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?

Page 24: Nitrogen cycle

Denitrification

R-NH2

NH4 NO2

NO3NO2

NO

N2O

N2

Page 25: Nitrogen cycle

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

Page 26: Nitrogen cycle

Looking at the Nitrogen cycle through the eye

of NH4

Page 27: Nitrogen cycle
Page 28: Nitrogen cycle

Surface water

Oxidized layer

Reduced soil layer

[NH4] HIGH

Low [NH4]

Slow Diffusion

Biodegradation

C/N <20

C/N >20

Page 29: Nitrogen cycle

Surface water

Oxidized layer

Reduced soil layer

[NH4] HIGH

Low [NH4]

Slow Diffusion

nitrification

[NO3] high

Page 30: Nitrogen cycle

Surface water

Oxidized layer

Reduced soil layer

[NO3] high

Leaching

[NO3] Low

N2

Denitrification

Page 31: Nitrogen cycle