Fig. 4. Carbon dioxide evolution for individual soil cores drained to the potentials to the dry side of the detected optima for net nitrification. The CO2 evolution is related to (a) volumetric water content or (b) the relative solute diffusivity.
Fig. 4. Carbon dioxide evolution for individual soil cores drained to the potentials to the dry side of the detected optima for net nitrification. The CO2 evolution is related to (a) volumetric water content or (b) the relative solute diffusivity.