Short-term dynamics of abiotic and biotic soil (CO2)-C-13 effluxes after in situ (CO2)-C-13 pulse labelling of a boreal pine forest
P>Physical diffusion of isotopic tracers into and out of soil pores causes considerable uncertainty for the timing and magnitude of plant belowground allocation in pulse-labelling experiments. Here, we partitioned soil CO2 isotopic fluxes into abiotic tracer flux (physical return), heterotrophic flux, and autotrophic flux contributions following (CO2)-C-13 labelling of a Swedish Pinus sylvestris f