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

• Published in: Biogeochemistry Vol. 47; no. 3; pp. 269 - 295
• Main Authors: Yao, H, Conrad, R, Wassmann, R, Neue, H.U
• Format: Journal Article
• Language: English
• Published: Heidelberg Kluwer Academic Publishers 01.12.1999; Springer; Springer Nature B.V
• Subjects: Acid soils; Agricultural soils; Carbon; Carbon dioxide; Earth sciences; Earth, ocean, space; Electrons; Exact sciences and technology; Geochemistry; Iron; Methane; Methane production; Nitrogen; Organic carbon; Organic soils; Redox potential; Rice fields; Rice soils; Soil and rock geochemistry; soil bacteria; soil chemistry; Soil organic carbon; Soils; Sulfates; Surficial geology; Southern Europe; Italy; Far East; Philippine Islands; China; carbon dioxide; Eh; accumulation; production; Europe; nitrogen; ferrous iron; regression analysis; hydrogen; sulfates; nitrates; acetate; agriculture; chemical reduction; Asia; methane; pH; iron; statistical analysis; soils; organic carbon
• ISSN: 0168-2563; 1573-515X
• DOI: 10.1007/bf00992910

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-,SO42-, pH, Eh, H2 and acetate were monitored during anaerobic incubation at 30 °C 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 μmol d-1 g-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 0.01 and 3.08 μmol d-1 g-1. During steady state the constant CH4 and CO2 production rates varied from 0.07 to 0.30 μmol d-1 g-1 and 0.02 and 0.28 μmol d-1 g-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 <5% nonmethane hydrocarbons. Associated with the reduction of available Fe(III) most of the CO2 was produced during the reduction phase. The electron transfer was balanced between total CO2 produced and both CH4 formed and Fe(III), sulfate and nitrate reduced. Maximum CH4 production rate (r = 0.891) and total CH4 produced (r = 0.775) correlated best with the ratio of soil nitrogen to electron acceptors. Total nitrogen content was a better indicator for "available" organic substrates than the total organic carbon content. The redox potential was not a good predictor of potential CH4 production. These observations indicate that the availability of degradable organic substrates mainly controls the CH4 production in the absence of inorganic electron acceptors.