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中国东北淡水沼泽甲烷排放动态

Dynamics of methane emissions from a freshwater marsh of northeast China.

作者信息

Yang Wenyan, Song Changchun, Zhang Jinbo

机构信息

Northeast Institute of Geography and Agroecology, Chinese Academic Science, Changchun Jilin, 130012, China.

出版信息

Sci Total Environ. 2006 Dec 1;371(1-3):286-92. doi: 10.1016/j.scitotenv.2006.08.034. Epub 2006 Oct 4.

Abstract

In this paper, CH(4) flux was measured from Nov. 2002 to Oct. 2005, to estimate CH(4) emissions in winter and during freeze-thaw period, and interannual variation in CH(4) emissions in freshwater marsh in northeast China. The results showed that there was an obvious CH(4) emission (0.1-2.3 mg m(-2) h(-1)) in the freshwater marsh in winter. Flux of CH(4) in winter (November to March the next year) was about 3.8%, 5.5%, and 2.2% of the whole year in 2003, 2004, and 2005, respectively. Emission of CH(4) significantly increased during the freeze-thaw period (April-June), and was about 30.8%, 20.9%, and 20.6% of the whole year in 2003, 2004, and 2005, respectively. Standing water depth greatly governed interannual variation of CH(4) emissions from marshes during the thaw-freeze period. Interannual variation of CH(4) emissions was significant during the growing season (p<0.05). Standing water depth during April to June was a primary factor, which affected the interannual variation of CH(4) flux during the growing season. Precipitation during the preceding non-growing season affected CH(4) emission indirectly via standing water depth.

摘要

本文于2002年11月至2005年10月测量了CH(4)通量,以估算中国东北淡水沼泽冬季和冻融期的CH(4)排放以及CH(4)排放的年际变化。结果表明,冬季淡水沼泽存在明显的CH(4)排放(0.1 - 2.3毫克·米(-2)·小时(-1))。2003年、2004年和2005年冬季(11月至次年3月)的CH(4)通量分别约占全年的3.8%、5.5%和2.2%。在冻融期(4 - 6月)CH(4)排放显著增加,2003年、2004年和2005年分别约占全年的30.8%、20.9%和20.6%。积水深度极大地影响了沼泽在冻融期CH(4)排放的年际变化。生长季CH(4)排放的年际变化显著(p<0.05)。4 - 6月的积水深度是影响生长季CH(4)通量年际变化的主要因素。前一个非生长季的降水量通过积水深度间接影响CH(4)排放。

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