Temporal Variation of N Isotopic Composition of Decomposing Legume Roots and Its Implications to N Cycling Estimates in Tracer Studies in Agroforestry Systems
Simulated evolution of the N pools in (a) the residue application experiment (RA), and (b) the full interaction experiment (FI). Note that inorganic N from the residue (NSR) remains close to zero for most of the time in both experiments as it is quickly absorbed by plant or microbial biomass.
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