2. Nitrogen
โข 78% of the air is nitrogen (N2)
โข Nitrogen is essential for organisms
to make DNA, protein, amino
acids, etc.
โข Yet, N2 is useless to plants and
animals
3. How do organisms get nitrogen?
โข Two natural processes convert
nitrogen gas into usable
nitrogen:
โข Lightning
โข Nitrogen cycle
4. Nitrogen Cycle
โข 5 main processes cycle nitrogen through the atmosphere, biosphere,
and lithosphere:
1. Nitrogen fixation
2. Nitrification
3. Assimilation
4. Ammonification
5. Denitrification
5. 5
The Nitrogen Cycle
โข N2 gas is the most abundant gas in the atmosphere, 79% of air
volume.
โข Involves several types of microbes
โข 4 types of reactions:
โข nitrogen fixation โatmospheric N2 gas is converted to NH4
salts; nitrogen-fixing bacteria live free or in symbiotic
relationships with plants
โข ammonification โ bacteria decompose nitrogen-
containing organic compounds to ammonia
โข nitrification โ convert NH4
+ to NO2
- and NO3
-
โข denitrification โ microbial conversion of various nitrogen
salts back to atmospheric N2
9. The Nitrogen Cycle
N is cycled between: NH4
+ (-3 oxidation state) and NO3
- (+5 oxidation state)
10. Nitrogen Reservoir Metric tons nitrogen Actively cycled
Atmosphere
N2
Ocean
Biomass
Soluble salts (NO3, NO2
-, NH4
+)
Dissolved and particulate
organics
Dissolved N2
Land
Biota
Organic matter
Earthโs crust
3.9 x 1015
5.2 x 108
6.9 x 1011
3.0 x 1011
2.0 x 1013
2.5 x 1010
1.1 x 1011
7.7 x 1014
No
Yes
Yes
Yes
No
Yes
Slow
No
Global Nitrogen Reservoirs
12. Nitrogen Cycle
โข Nitrogen fixation
โข Bacteria (such as Rhizobium) convert gaseous nitrogen
into ammonia, which is taken up by plants
โข N2 + 3H2 ๏ 2NH3
Rhizobium
nodules
13. Biological inputs of nitrogen from N2 fixation
land - 135 million metric tons/yr (microbial)
marine - 40 million metric tons/yr (microbial)
fertilizers - 30 million metric tons/yr (anthropogenic)
Nitrogen must be fixed before it can be incorporated into biomass. This process
is called nitrogen fixation.
The enzyme that catalyzes
nitrogen fixation is nitrogenase.
N2 fixing system
Nitrogen fixation
(kg N/hectare/yr)
Rhizobium-legume
Anabaena-Azolla
Cyanobacteria-moss
Rhizosphere assoc.
Free-living bacteria
200-300
100-120
30-40
2-25
1-2
Rates of Nitrogen Fixation
1-2 kg N/hec/yr 2- 25 kg/N/hec/yr
14. Free-living bacteria must also protect nitrogenase from O2
complex is membrane associated
slime production
high levels of respiration
conformation change in nitrogenase when O2 is present
Azotobacter - aerobic
Beijerinckia - aerobic, likes acidic soils
Azospirillum - facultative
Clostridia - anaerobic
Examples of free-living bacteria:
15. Microorganisms fixing
โข Azobacter
โข Beijerinckia
โข Azospirillum
โข Clostridium
โข Cyanobacteria
โข Require the enzyme
nitrogenase
โข Inhibited by oxygen
โข Inhibited by ammonia (end
product)
16. Fate of ammonia (NH3) produced during nitrogen fixation
plant uptake
microbial uptake
adsorption to colloids (adds to CEC)
fixation within clay minerals
incorporation into humus
volatilization
nitrification
} assimilation and mineralization
19. Nitrification - Chemoautotrophic aerobic process
Nitrosomonas Nitrobacter
NH4
+ NO2
- NO3
-
Nitrosomonas:
34 moles NH4
+ to fix 1 mole CO2
Nitrobacter:
100 moles NH4
+ to fix 1 mole CO2
Nitrification is important in areas that are high in ammonia (septic tanks,
landfills, feedlots, dairy operations, over fertilization of crops). The nitrate
formed is highly mobile (does not sorb to soil). As a result, nitrate
contamination of groundwater is common. *Nitrate contamination can result in
methemoglobenemia (blue baby syndrome).
20. What is the fate of NO3
- following nitrification?
accumulation (disturbed vs. managed)
fixation within clay minerals
leaching (groundwater contamination)
dissimilatory nitrate reduction
โข nitrate ammonification
โข denitrification
plant uptake
microbial uptake
biological uptake (assimilatory nitrate
reduction)
}
Assimilatory nitrate reduction
many plants prefer nitrate which is reduced in the plant prior to use however,
nitrogen in fertilizer is added as ammonia or urea.
assimilatory nitrate reduction is inhibited by ammonium
nitrate is more mobile than ammonium leading to leaching loss
microorganisms prefer ammonia since uptake of nitrate requires a reduction
step
22. Nitrogen Cycle
โข Assimilation
โข Plants use ammonia (NH3),
ammonium ions (NH4
+), and
nitrate ions (NO3
-)
โข Make DNA, amino acids, and
protein
โข Animals get their nitrogen
from eating plants
23. NH3 is assimilated by cells into:
proteins
cell wall constituents
nucleic acids
Ammonia assimilation and ammonification
Release of assimilated NH3 is called ammonification. This process
can occur intracellularly or extracellularly
proteases
chitinases
nucleases
ureases
25. Nitrogen Cycle
โข Ammonification
โข Animals excrete excess nitrogen in their urine and feces
โข Additional nitrogen is added to the soil when organisms die
โข Decomposing bacteria and fungi convert the nitrogen in their waste into
usable ammonia (NH3) and ammonium ions (NH4
+)
26. - -
- -
+
+
H O
2
glutamate
dehydrogenase
NAD NADH
= O
glutamate ๏ก - ketoglutarate
+ NH3
NH3
A
At high N concentrations
-
-
-
-
-
-
+
+
+
= O
glutamate
glutamate
glutamine
๏ก - ketoglutarate
NH3
NH3
NH3
NH2
ATP
ADP + Pi
glutamine
synthetase
Ferredoxin
2H+
2e
-
glutamate-
synthase
(GOGAT)
Transamination
B
At low N concentrations
27. Fate of ammonia (NH3) produced during nitrogen fixation
plant uptake
microbial uptake
adsorption to colloids (adds to CEC)
fixation within clay minerals
incorporation into humus
volatilization
nitrification
29. Nitrogen Cycle
โข Denitrification
โข Bacteria in the soil convert usable ammonia (NH3) and ammonium ions (NH4
+)
back into nitrogen gas (N2) and nitrous oxide gas (N2O)
30. Denitrification
NO, N2O deplete the ozone layer
Reaction of N2O with ozone
O2 + UV light O + O
O + O2 O3 (ozone generation)
N2O + UV light N2 + O*
N2O + O* 2NO (nitric oxide)
NO + O3 NO2 + O2 (ozone depletion)
NO2 + O* NO + O2
returns fixed N to atmosphere:
get formation of NO (Nitric oxide), N2O (Nitrous oxide)
NO3 NO N2O N2
31. How are humans affecting the nitrogen cycle?
โข Burning fuels release nitric oxide
(NO) into the atmosphere
โข Creates acid rain
โข Harms vegetation
โข Harms aquatic ecosystems
โข Damages materials (metal, stone, etc.)
32. How are humans affecting the nitrogen cycle?
โข Excess livestock waste and
fertilizer adds nitrous oxide (N2O)
to the atmosphere
โข N2O is a greenhouse gas
โข May lead to global warming
33. Effects of Human Activities
on the Nitrogen Cycle
โข We alter the nitrogen cycle by:
โข Adding gases that contribute to acid rain.
โข Adding nitrous oxide to the atmosphere through farming
practices which can warm the atmosphere and deplete ozone.
โข Contaminating ground water from nitrate ions in inorganic
fertilizers.
โข Releasing nitrogen into the troposphere through deforestation.
34. How are humans affecting the nitrogen cycle?
โข Runoff from agricultural
lands and sewage
facilities adds nitrogen
to aquatic ecosystems
โข Results in algal blooms
โข Leads to โdead zonesโ
35. Nitrogen Cycle
โข Nitrogen cycle is the continuous sequence of natural processes by
which nitrogen in the atmosphere and nitrogenous compounds in
the soil are converted, as by nitrification and nitrogen fixation, into
substances that can be utilized by green plants and then returned to
the air and soil as a result of denitrification and plant decay.
36. Nitrogen Cycle
โข Nitrogen fixation:
The conversion of atmospheric nitrogen into nitrogenous
compounds by bacteria (Rhizobia) found in the root
nodules of legumes and certain other plants, and in the
soil.
โข Assimilation:
Plants take nitrogen from the soil, by absorption through
their roots in the form of their nitrate ions or ammonium
ions. All nitrogen obtained by animals can be traced back
to the eating of plants.
37. Nitrogen Cycle
โข Ammonification:
When a plant or animal dies, or an animal expels waste, the
initial form of nitrogen is organic. Bacteria, or fungi in some
cases, convert the organic nitrogen within the remains back
into ammonium (NH4
+).
โข Nitrification:
The oxidation of the ammonium compounds in dead organic
material into nitrites and nitrates by soil nitrobacteria,
making nitrogen available to plants.
Nitrosomonas species converts ammonia to nitrites (NO2
-).
Nitrobacter species are responsible for the oxidation of the
nitrites into nitrates (NO3
-).