SSSAJ Journal of Natural Resources and Life Sciences Education
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Fig. 2. Temperature and moisture responses of the mineralization rate constants of the active (ka) and slow (ks) organic N pools. ka and ks were estimated by the double exponential model with fixed pool sizes that were obtained with the data at 35°C and 55% WHC using standard ka (0.693) and ks (o.054). The equations for insignificant moisture responses were not shown.





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