Exact(18)
The interactive model, which represents priming by a power function of old C decomposition rate with the amount of the new C, is the most parsimonious.
Based on vial results, partitioning was significantly related to C decomposition.
Based on model results, partitioning between DNRA and N2 production was positively linearly related to the ratio of C decomposition to NO3− reduction rates (C/NO3−) but not C decomposition alone.
Oxygen partial pressure enables to control the degree of C decomposition.
Organic C decomposition rates were inferred based on modeled rates as well as stoichiometric conversions of NH4+ production in pre-incubated vials.
However, land-use management influences the quantity and quality of carbon (C) inputs which may, in turn, affect microbial activity and soil C decomposition rates.
Similar(42)
However, these hypotheses of soil property-C decomposition relationships have not been explicitly tested at large spatial scales.
Our results show inverse soil property-C decomposition relationships and quantitatively evaluate the essential roles of soil texture (clay content) in controlling decomposition of SOC at a large spatial scale.
Protection is not considered to equate to a permanent and complete removal of organic C from decomposition, but rather to a reduced decomposition rate relative to similar unprotected materials.
The susceptibility of this C to decomposition is largely controlled by the potential of microorganisms to degrade it with long-term implications for C dynamics in agroecosystems.
Cellulose contributed the most C during decomposition, and fungal phospholipid fatty acids incorporated the highest level of 13C from labeled litter.
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