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Nitrification and denitrification are the main contributors to soil N2O production and emission, and distinguishing their contributions to N2O emission under natural conditions is vital to deciphering nitrogen biogeochemistry. Stable isotopes have provided insight to resolve this problem, of which δ15N2Obulk (15N abundance in N2O), dual isotopes (δ15N, δ18O) and site preference (SP) are the most effective...
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