二氧化碳
温室气体
甲烷
环境科学
焊剂(冶金)
环境化学
水槽(地理)
大气科学
碳循环
水文学(农业)
生态系统
外推法
化学
生态学
海洋学
地质学
地理
生物
数学分析
地图学
有机化学
岩土工程
数学
作者
Balathandayuthabani Panneer Selvam,Sivakiruthika Natchimuthu,Lakshmanan Arunachalam,David Bastviken
摘要
Abstract Inland waters were recently recognized to be important sources of methane ( CH 4 ) and carbon dioxide ( CO 2 ) to the atmosphere, and including inland water emissions in large scale greenhouse gas ( GHG ) budgets may potentially offset the estimated carbon sink in many areas. However, the lack of GHG flux measurements and well‐defined inland water areas for extrapolation, make the magnitude of the potential offset unclear. This study presents coordinated flux measurements of CH 4 and CO 2 in multiple lakes, ponds, rivers, open wells, reservoirs, springs, and canals in India. All these inland water types, representative of common aquatic ecosystems in India, emitted substantial amounts of CH 4 and a major fraction also emitted CO 2 . The total CH 4 flux (including ebullition and diffusion) from all the 45 systems ranged from 0.01 to 52.1 mmol m −2 d −1 , with a mean of 7.8 ± 12.7 (mean ± 1 SD) mmol m −2 d −1 . The mean surface water CH 4 concentration was 3.8 ± 14.5 μ m (range 0.03–92.1 μ m ). The CO 2 fluxes ranged from −28.2 to 262.4 mmol m −2 d −1 and the mean flux was 51.9 ± 71.1 mmol m −2 d −1 . The mean partial pressure of CO 2 was 2927 ± 3269 μatm (range: 400–11 467 μatm). Conservative extrapolation to whole I ndia, considering the specific area of the different water types studied, yielded average emissions of 2.1 Tg CH 4 yr −1 and 22.0 Tg CO 2 yr −1 from India's inland waters. When expressed as CO 2 equivalents, this amounts to 75 Tg CO 2 equivalents yr −1 (53–98 Tg CO 2 equivalents yr −1 ; ± 1 SD) , with CH 4 contributing 71%. Hence, average inland water GHG emissions, which were not previously considered, correspond to 42% (30–55%) of the estimated land carbon sink of I ndia. Thereby this study illustrates the importance of considering inland water GHG exchange in large scale assessments.
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