Kim Y, Park S - J, Lee B - Y, Risk D (2016) Continuous measurement of soil
carbon efflux with Forced Diffusion (FD) chambers in a tundra ecosystem of Alaska.
Not exact matches
The steady state [CO2] level is a function of two rates, the influx (conversion of plant material into CO2, burning fossil fuels and vulcanism) and
efflux (fixation of
carbon, mineralization of
carbon).
The
efflux rate, or true sink rate, is the rate of mineralization or inorganic and organic, biotic,
carbon; mostly due aquatic organisms.
After the hurricane had passed, soil
carbon - dioxide
efflux — due to microbial and plant respiration — increased while gross primary productivity decreased.