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亚热带浅水池塘水-气界面甲烷通量特征
引用本文:龙丽,肖尚斌,张成,张文丽,谢恒,李迎晨,雷丹,穆晓辉,张军伟.亚热带浅水池塘水-气界面甲烷通量特征[J].环境科学,2016,37(12):4552-4559.
作者姓名:龙丽  肖尚斌  张成  张文丽  谢恒  李迎晨  雷丹  穆晓辉  张军伟
作者单位:三峡大学水利与环境学院, 宜昌 443002,三峡大学水利与环境学院, 宜昌 443002,三峡大学电气与新能源学院, 宜昌 443002;中国地质大学(武汉)资源学院, 武汉 430074,三峡大学(武汉)生物与制药学院, 宜昌 443002,三峡大学(武汉)生物与制药学院, 宜昌 443002,三峡大学水利与环境学院, 宜昌 443002,三峡大学水利与环境学院, 宜昌 443002,三峡大学水利与环境学院, 宜昌 443002,三峡大学水利与环境学院, 宜昌 443002
基金项目:国家自然科学基金项目(41273110);湖北省自然科学基金项目(2014CFB672);2015年三峡大学研究生科研创新基金项目(2015CX009);湖北省教育厅科研计划项目(Q20151209);湖北省自然基金指导性计划项目(2015CFC834)
摘    要:为研究亚热带富营养化浅水池塘水-气界面CH_4释放通量特征,以宜昌地区5个浅水池塘为对象,利用静态通量箱法进行了为期一年的水-气界面CH_4通量监测.结果表明,这5个池塘CH_4的年释放量分别为4.495、12.702、6.827、8.920、17.560 mg·(m~2·h)~(-1).其中扩散通量分别为0.075、0.087、0.118、0.086、0.151 mg·(m~2·h)~(-1),冒泡通量分别为4.420、12.616、6.709、8.834、17.409 mg·(m~2·h)~(-1),CH_4冒泡量占CH_4释放总量的98%以上,并且CH_4释放量明显高于其他水域生态系统(湖泊、水库).可见在富营养化浅水水域中,CH_4释放量较大,且冒泡排放是CH_4的主要排放方式,而只关注扩散排放而忽略冒泡排放则会大大低估CH_4释放量.

关 键 词:水-气界面  甲烷  扩散排放  冒泡排放  通量  浅水池塘
收稿时间:2016/5/13 0:00:00
修稿时间:2016/7/21 0:00:00

Characteristics of Methane Flux Across the Water-air Interface in Subtropical Shallow Ponds
LONG Li,XIAO Shang-bin,ZHANG Cheng,ZHANG Wen-li,XIE Heng,LI Ying-chen,LEI Dan,MU Xiao-hui and ZAHNG Jun-wei.Characteristics of Methane Flux Across the Water-air Interface in Subtropical Shallow Ponds[J].Chinese Journal of Environmental Science,2016,37(12):4552-4559.
Authors:LONG Li  XIAO Shang-bin  ZHANG Cheng  ZHANG Wen-li  XIE Heng  LI Ying-chen  LEI Dan  MU Xiao-hui and ZAHNG Jun-wei
Institution:College of Hydraulic & Environmental Engineering, China Three Gorges University, Yichang 443002, China,College of Hydraulic & Environmental Engineering, China Three Gorges University, Yichang 443002, China,College of Electrical Engineering & New Energy, China Three Gorges University, Yichang 443002, China;Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China,College of Biotechnology & Pharmaceutical Engineering, China Three Gorges University, Yichang 443002, China,College of Biotechnology & Pharmaceutical Engineering, China Three Gorges University, Yichang 443002, China,College of Hydraulic & Environmental Engineering, China Three Gorges University, Yichang 443002, China,College of Hydraulic & Environmental Engineering, China Three Gorges University, Yichang 443002, China,College of Hydraulic & Environmental Engineering, China Three Gorges University, Yichang 443002, China and College of Hydraulic & Environmental Engineering, China Three Gorges University, Yichang 443002, China
Abstract:Five shallow ponds of Yichang were selected to illustrate the characteristics of methane(CH4) in subtropical eutrophic shallow ponds. CH4 flux across the water-air interface was quantified with static floating chamber method for one year. Annual CH4 fluxes of the five ponds were 4.495, 12.702, 6.827, 8.920, 17.560 mg·(m2·h)-1 respectively. Diffusive CH4 fluxes were 0.075, 0.087, 0.118, 0.086, 0.151 mg·(m2·h)-1 respectively and bubble emissions were 4.420, 12.616, 6.709, 8.834, 17.409 mg·(m2·h)-1 respectively. Over 98% of total CH4 flux was bubble emission and CH4 flux was apparently higher than other aquatic ecosystems. So the CH4 flux of shallow waters was high and bubble emission was the dominant way. CH4 emission would be largely underestimated if the research only focus on the diffusion discharge and ignore the bubble emission.
Keywords:the water-air interface  methane  diffusion emission  bubble emission  flux  shallow ponds
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