Fluxes and pools of methane in wetland rice soils with varying organic inputs

Measurements of methane emission rates and concentrations in the soil were made during four growing seasons at the International Rice Research Institute in the Philippines, on plots receiving different levels of organic input. Fluxes were measured using the automated closed chambers system (total emission) and small chambers installed between plants (water surface flux). Concentrations of methane in the soil were measured by collecting soil cores including the gas phase (soil-entrapped methane) and by sampling soil solution in situ (dissolved methane). There was much variability between seasons, but total fluxes from plots receiving high organic inputs (16–24 g CH₄ m^–2) always exceeded those from the low input plots (3–9 g CH₄ m^–2). The fraction of the total emission emerging from the surface water (presumably dominated by ebullition) was greater during the first part of the season, and greater from the high organic input plots (35–62%) than from the low input plots (15–23%). Concentrations of dissolved and entrapped methane in the low organic input plots increased gradually throughout the season; in the high input plots there was an early-season peak which was also seen in emissions. On both treatments, periods of high methane concentrations in the soil coincided with high rates of water surface flux whereas low concentrations of methane were generally associated with low flux rates.     

种植杂交稻对甲烷排放的影响及评价

早、中、晚稻三季24h稻田甲烷监测结果表明,种植杂交稻没有明显增进福田甲烷排放的作用．甲烷释放总量在3个种植季节中,除连作晚稻的杂交稻田比常规稻田高11．6％外,早稻、单季稻杂交稻田分别低于常规稻田6．4％和8．9％．稻田甲烷每周日平均释放量在水稻生长前期（移栽后5～7周）杂交稻高于常规稻,孕穗至收获期杂交稻低于常规稻．温度对甲烷释放影响十分明显．在不同水稻种植季节,稻田甲烷释放模式各不相同．经测定,杂交稻田的土壤产甲烷细菌数量及土壤产甲烷潜力明显高于常规稻田,其中产甲烷细菌数可相差数倍至2个数量级．试验结果还表明,种植水稻明显增加了稻田甲烷排放量,与侵水稻田相比．植稻田甲烷排放量增加了41．4％．     

Sulfate-containing amendments to reduce methane emissions from rice fields: mechanisms,effectiveness and costs

Application of sulfate-containing amendments is oftensuggested as a mitigation option to reduce methane (CH₄) emissionsfrom rice (Oryza) fields. This paper discusses the mechanism andpotential of this mitigation option, reviews the relevant experimental data,and presents first, indicative costs of application. CH₄ emission datafor rice fields with sulfate-containing amendments are compiled toreinterpret the resulting reduction in CH₄ emission and find a generalrelationship between emission reduction and amount of sulfate applied. Thereduction in CH₄ emission depends on the amount of sulfate applied.However, absolute emission reduction is location specific and cannot bederived from the amount of sulfate (SO^2- ₄) applied only. We established alogarithmic relationship, across locations, between SO^2- ₄ application andfractional emission reduction relative to the emission of the non-amendedcontrol field. Recycling of SO^2- ₄ in the rhizosphere was essential to explainthe observed reductions in CH₄ emission for a number of theexperiments. The cost of applying SO^2- _{_4}-containing fertilizers varies acrosscountries and depends on local fertilizer prices. Since a fractional reductionis obtained, the cost-efficiency in terms of CH₄ mitigation per unitof SO^2- ₄ applied will be highest in high-emitting rice production systems.Provided the proper target areas are selected, the cost of SO^2- ₄-containingfertilizer as a mitigation option to reduce CH₄ emissions in rice fieldsis estimated at 5–10 US dollar per Mg CO₂-equivalent.