Effect of soil characteristics on sequential reduction and methane production in sixteen rice paddy soils from China, the Philippines, and Italy

The potentials for sequential reduction of inorganic electron acceptors and production of methane have been examined in sixteen rice soils obtained from China, the Philippines, and Italy. Methane, CO2, Fe(II), NO3(-), SO4(2-), pH, Eh, H2 and acetate were monitored during anaerob incubation at 30 øC for 120 days. Based on the accumulation patterns of CO2 and CH4, the reduction process was divided into three distinct phases: (1) an initial reduction phase during which most of the inorganic electron acceptors were depleted and CO2 production was at its maximum, (2) a methanogenic phase during which CH4 production was initiated and reached its highest rate, and (3) a steady state phase with constant production rates of CH4 and CO2). The reduction phases lasted for 19 to 75 days with maximum CO2 production of 2.3 to 10.9 mu mol d(exp -1) g(exp -1) dry soil. Methane production started after 2 to 87 days and became constant after about 38-68 days (one soil > 120 days). The maximum CH4 production rates ranged between 0.0 1 and 3.08 mu mol d(exp -1) g(exp -1). During steady state the constant CH4 and CO2 production rates varied from 0.07 to 0.30 mu mol d(exp -1) g(exp -1) and 0.02 and 0.28 mu mol d(exp -1) g(exp - 1) respectively. Within the 120 d of anaerobic incubation only 6-17% of the total soil organic carbon was released into the gas phase. The gaseous carbon released consisted of 61-100% CO2 <0.1-35% CH4, and