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Changing fire regimes and additional unburnt biomass may alter soil N2O dynamics through changes in the microbial processes of nitrification and de-nitrification.
Among these losses is the soil emission of the potent greenhouse gas nitrous oxide (N2O) which is mainly produced by the soil microbial processes of nitrification and denitrification.
Biologically available nitrogen is removed from ecosystems through the microbial processes of anaerobic ammonium oxidation (anammox) or denitrification, while dissimilatory nitrate reduction to ammonium (DNRA) retains it.
Nitrous oxide is a potent greenhouse gas and its production is mediated by the soil microbial processes of denitrification and nitrification.
Nitrous oxide (N2O) is produced naturally in the soil during the microbial processes of nitrification and denitrification.
Metabolism involves gut microbial processes of the demethylation of dimethylbutanoic acid, hydroxylation/dehydroxylation and β-oxidation, resulting in the production of 2-hydroxyisovaleric acid (3-methyl-2-hydroxybutanoic acid), 3-hydroxybutanoic acid and lactic acid (2-hydroxypropanoic acid), and finally re-cyclization of heptanoic acid to produce cyclohexanecarboxylic acid [ 64].
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The importance of temperature sensitivity soil microbial processes on global dynamics of soil C pools has been reported by many authors (Anderson 1992; Zogg et al. 1997).
Specifically, MICP utilizes the microbial process of hydrolysis of urea to induce pH increase leading to calcite precipitation.
We examined predictors of NO3− removal via the microbial process of denitrification in an urban wetland system in New Jersey, USA with highly heterogeneous soils.
The removal of NO3− and nitrite (NO2−) in cold climates through the microbial process of denitrification was evaluated using a pilot-scale fixed-bed bioreactor (27 m3).
Typically the microbial process of denitrification is viewed as simply a function of environmental factors (e.g. C, N, and redox status) in the biogeochemical model of denitrification [45].
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