Contribution of Ebullition to Methane and Carbon Dioxide Emission from Water between Plant Rows in a Tropical Rice Paddy Field.

International Scholarly Research Notices Pub Date : 2015-12-29 eCollection Date: 2015-01-01 DOI:10.1155/2015/623901
Shujiro Komiya, Kosuke Noborio, Kentaro Katano, Tiwa Pakoktom, Meechai Siangliw, Theerayut Toojinda
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引用次数: 19

Abstract

Although bubble ebullition through water in rice paddy fields dominates direct methane (CH4) emissions from paddy soil to the atmosphere in tropical regions, the temporal changes and regulating factors of this ebullition are poorly understood. Bubbles in a submerged paddy soil also contain high concentrations of carbon dioxide (CO2), implying that CO2 ebullition may occur in addition to CH4 ebullition. We investigated the dynamics of CH4 and CO2 ebullition in tropical rice paddy fields using an automated closed chamber installed between rice plants. Abrupt increases in CH4 concentrations occurred by bubble ebullition. The CO2 concentration in the chamber air suddenly increased at the same time, which indicated that CO2 ebullition was also occurring. The CH4 and CO2 emissions by bubble ebullition were correlated with falling atmospheric pressure and increasing soil surface temperature. The relative contribution of CH4 and CO2 ebullitions to the daily total emissions was 95-97% and 13-35%, respectively.

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热带稻田植物行间水的沸腾对甲烷和二氧化碳排放的贡献。
在热带地区,水稻土向大气直接排放的甲烷(CH4)主要以水田泡泡沸腾为主,但目前对这种泡泡沸腾的时间变化及其调控因子了解甚少。浸没水稻土中的气泡也含有高浓度的二氧化碳(CO2),这意味着除了CH4沸腾外,还可能发生CO2沸腾。利用安装在水稻植株之间的自动封闭室,研究了热带稻田中CH4和CO2的沸腾动态。CH4浓度的突然增加是由气泡沸腾引起的。同时,腔室空气中的CO2浓度突然升高,表明CO2沸腾也在发生。气泡沸腾的CH4和CO2排放量与大气压力下降和土壤表面温度升高有关。CH4和CO2泡腾对日总排放量的相对贡献分别为95-97%和13-35%。
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