Yang Wenyan, Song Changchun, Zhang Jinbo
Northeast Institute of Geography and Agroecology, Chinese Academic Science, Changchun Jilin, 130012, China.
Sci Total Environ. 2006 Dec 1;371(1-3):286-92. doi: 10.1016/j.scitotenv.2006.08.034. Epub 2006 Oct 4.
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.
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。