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Redox window with minimum global warming potential contribution from rice soils

Eight different rice (Oryza sativa L.) soils were incubated using a microcosm technique to study CO 2 , CH 4 , and N 2 O contribution to global warming potential (GWP) at different redox potential (E H ) conditions. Cumulative GWP from these three greenhouse gases reached a minimum at a redox window of +180 to -150 mV. Within the redox window, CO 2 production accounted for 86% of the cumulative GWP, because both N 2 O and CH 4 production were low. When E H was higher than +180 mV, both CO 2 and N 2 O production made a significant contribution to the cumulative GWP, whereas CH 4 production was a dominant contributor when E H was lower than -150 mV. During the incubation, each soil exhibited a unique signature of developing such an optimum redox window with a minimum GWP. Multiple regressions showed that initial soil organic matter (OM) and S content might have a significant control (P = 0.02) on the time required for the soils to reach the redox window when the incubation started from aerobic conditions. The results of this integrated study on productions of the three greenhouse gases provide a theoretical base for abating soil GWP loading into the atmosphere by regulating soil E H conditions.