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) Soil C and N dynamics are differently affected by the identity and specific structure of chemical substrates entering soil (Links between (coutney). Nave et al. (2009) suggested that the N inputs increased the primary production and soil C storage, which was accompanied by an increase in the mineral N content and a decrease in the C/N ratio. The authors considered that the mineral N input might exceed its binding capacity in biological biomass, including the microbiological biomass in SOM, especially with carbon deficiency, which caused nitrogen leaching to the ground and surface water.
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