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Soil Nitrogen (Components (Inorganic N <2% (Adsorbed inorganic N…
Soil Nitrogen
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Concerns
Eutrophication, algal blooms and anoxia
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Biodiversity loss, change to less nitrogen efficient species
Losses
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Volatilisation
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NH3 volatilisation losses usually decrease with time due to increase in acidity (as a result of nitrification)
Up to 25% of added urea may be lost as NH3 gas. Don't apply urea in dry, windy conditions
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Measurement
Kjeldahl Method
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Hg, Se or Cu catalyst - Cu safest
Does not break N-N or N-O bonds so samples containing these require pre-treatment (can make up to 10% of plant N, much less in soil)
Otherwise TKN calculated, not TN
LECO
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All soil N converted to N2 and detected using a thermal conductivity detector. Generally expressed as a %
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Inputs
N fixation
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Rhizobia gives mineral N to host plant in return for energy (carbohydrates) and a managed habitat in plant roots
The rhizobia nitrogenase enzyme is sensitive to oxygen concentration which the plant manages using leghaemogloebin which carries O2 away to respiration sites
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When clover dies and is decomposed, or when eaten by animals and is returned in excreta, N becomes available to non-legume plants (e.g. ryegrass)
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N2 fixation decreases in the presence of NH4+ or NO3- in solution - e.g. fertiliser has been applied
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Transformations
Most nitrogen is not immediately available to plants and requires mineralisation by microbes to release
Mineralisation and Immobilization are the conversions between organically-bound nitrogen and inorganic nitrogen (NO3- and NH4+)
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