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Fig. 2. Global warming potential (GWP) contribution of N2O, CH4, and CO2 as a function of soil EH. All eight soils showed the same pattern of (i) N2O, (ii) CH4, and (iii) CO2 dynamics with soil EH change from high to low. The figure was plotted in a logarithmic scale to cover a wide range of values. Global warming potential contributions below 1 mg CO2 equivalent kg–1 h–1 were considered insignificant and not illustrated in the figure for clarity.