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

机译:在热带稻田中,植物排之间的水汽对甲烷和二氧化碳排放的贡献

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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.
机译:尽管稻田中通过水引起的气泡沸腾占主导,从稻田土壤向热带地区的大气直接排放甲烷(CH4),但人们对这种沸腾的时间变化和调控因素知之甚少。淹没的稻田土壤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,CO2沸腾也可能发生。我们使用安装在水稻植株之间的自动密闭室调查了热带稻田中CH4和CO2沸腾的动力学。气泡沸腾会导致CH4浓度突然增加。同时,室内空气中的CO2浓度突然增加,这表明还发生了CO2沸腾。气泡沸腾产生的CH4和CO2排放与大气压力下降和土壤表面温度升高相关。 CH4和CO2沸腾对每日总排放量的相对贡献分别为95–97%和13–35%。

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