globalchange  > 气候变化与战略
CSCD记录号: CSCD:5203896
论文题名:
长江口盐沼带湿地生态演替过程中甲烷排放研究
其他题名: Methane emission in the process of wetland vegetation succession in salt marsh of Yangtze River estuary
作者: 李杨杰1; 陈振楼1; 王东启1; 胡泓1; 王初2
刊名: 环境科学学报
ISSN: 0253-2468
出版年: 2014
卷: 34, 期:8, 页码:1037-1045
语种: 中文
中文关键词: 长江口盐沼带 ; 海三棱藨草 ; 互花米草入侵 ; CH_4排放通量
英文关键词: Yangtze estuary salt marsh ; Scirpus mariqueter ; invasion of Spartina alterniflora ; methane emissions
WOS学科分类: ENVIRONMENTAL SCIENCES
WOS研究方向: Environmental Sciences & Ecology
中文摘要: 甲烷(CH_4)作为河口湿地碳循环的重要中间产物,是大气中仅次于二氧化碳(CO_2)的第二大温室气体,其排放清单对于全球气候变暖趋势的预测具有重要意义.因此,本研究采用静态箱-气相色谱技术,针对长江口盐沼带湿地CH_4的排放通量展开了为期2年、每月1次的现场观测.研究结果表明,长江口盐沼带湿地持续表现为大气CH_4的净排放源,其中,2011年在海三棱藨草覆盖情况下,全年CH_4平均排放通量达到了1.00 mg·m~(-2)·h~(-1),2012年互花米草大规模入侵后,海三棱藨草生物量显著减小,全年CH_4排放通量减小为0.55 mg·m~(-2)·h~(-1).Pearson相关性分析表明,沉积物有机碳含量、光合有效辐射及含水率等均不是影响长江口盐沼带湿地CH_4排放的重要环境因子.在2011年,海三棱藨草生物量(p=0.001,r=0.928)、气温(p<0.01,r=0.432)均与CH_4排放通量呈现显著正相关,全年CH_4最大排放通量出现在生物量最大的夏季8月份; 2012年随着互花米草的入侵,CH_4排放通量在5月份达到了最大值,自5月份之后逐渐减小,互花米草的入侵使长江口中潮滩盐沼带湿地CH_4排放通量整体呈现出了下降的趋势.
英文摘要: As important intermediates in the process of carbon cycle in estuarine wetlands,methane (CH_4) is the important greenhouse gas that only seconds to carbon dioxide (CO_2) in the atmosphere. Accurate estimation of CH_4 emission inventory is important in predicting the global warming tendency. The static closed chamber-chromatograph method was used to investigate the monthly CH_4 fluxes from February 2011 to December 2012 in the salt marshes of Yangtze River estuary. The results indicated that salt marshes in Yangtze River estuary acted as a net source of atmospheric CH_4 and the annual average CH_4 fluxes was 1. 00 mg·m~(-2)·h~(-1) in 2011 when the Scirpus mariqueter was the dominant species. After the full-scale invasion of the alien Spartina alterniflora,biomass of Scirpus mariqueter decreased greatly in 2012,with the annual average CH_4 fluxes decreased to 0. 55 mg·m~(-2)·h~(-1). According to Pearson correlation analysis,sediment organic carbon,solar radiation and the water content were not the main factors of CH_4 fluxes. In addition,CH_4 fluxes were significantly positively correlated with both aboveground biomass of Scirpus mariqueter(p=0. 001,r=0. 928) and temperature (p<0. 01,r=0. 432) in 2011. Along with the invasion of Spartina alterniflora in 2012,CH_4 fluxes reached the highest value in May. The total CH_4 emissions also decreased significantly due to the invasion of Spartina alterniflora in 2012.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/147940
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作者单位: 1.华东师范大学资源与环境科学学院地理系, 上海 200241, 中国
2.上海师范大学旅游学院, 上海 200235, 中国

Recommended Citation:
李杨杰,陈振楼,王东启,等. 长江口盐沼带湿地生态演替过程中甲烷排放研究[J]. 环境科学学报,2014-01-01,34(8):1037-1045
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