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level: Level 1

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level questions: Level 1

QuestionAnswer
What percentage of the atmosphere is N2?78%
Nitrogen Cycle DefinitionThe Nitrogen Cycle describes the process by which N is gained or lost by the soil; absorbed by plants and returned to the soil as organic matter.
2 Forms of N available to plantsNitrate-N (NO3)- Ammonium-N (NH4)+ (Ammonium-N is rapidly converted to Nitrate-N via Nitrification.)
NitrificationThe process by which Ammonium-N (NH4)+ is rapidly nitrified into Nitrate-N (NO3)- for crop uptake. Nitrification is a bacterial process and takes place at soil temperatures above 4ºC.
DenitrificationThe process by which Nitrate-N (NO3)- is reduced to Nitrous oxide (N2O) and Nitrogen gas (N2). This normally occurs in warm, anaerobic soils (typically due to compaction and water-logging).
VolatilisationThe process by which Ammonia gas (NH3) is lost from the soil when the concentration of Ammonium-N (NH4)+ exceeds the adsorptive capacity of the soil.
Conditions of volatilisationLight, warm, drying alkaline soils are prone to volatilisation. Most ammonia emissions come from livestock manures during storage and spreading, and some come from the application of urea fertiliser.
How to minimise Nitrous Oxide (N2O) emissionsMatch N inputs to crop requirements.
Soil Nitrogen Supply (SNS) definitionThe amount of nitrogen (kg/ha N) in the soil that becomes available for uptake by the crop from establishment to the end of the growing season, taking into account nitrogen losses.
SNS EquationSNS = SMN + estimate of total crop N + estimate of mineralisable N
What percentage of the atmosphere is N2?78%
LeachingThe loss of Nitrate-N (NO3)- via water.
FixationThe process by which atmospheric Nitrogen gas (N2) is converted to organic-N (R-NH2). This is primarily achieved either by rhizobial bacteria in legume nodules or by industrial fertiliser production.
MineralisationThe process by which microbes convert Organic-N (R-NH2) to Ammonium-N (NH4)+. This occurs in warm, moist, well-aerated soils.
ImmobilisationThe process by which soil organisms consume Nitrate-N (NO3)- or Ammonium-N (NH4)+, converting it to Organic-N (R-NH2), locking it up within their cells until they die and decompose.