Carbon exchange in a freshwater marsh in the Sanjiang Plain, northeastern China

被引:44
作者
Song, Changchun [1 ]
Sun, Li [1 ]
Huang, Yao [2 ]
Wang, Yuesi [2 ]
Wan, Zhongmei [3 ]
机构
[1] Chinese Acad Sci, NE Inst Geog & Agroecol, Key Lab Wetland Ecol & Environm, Changchun 130012, Peoples R China
[2] Chinese Acad Sci, Inst Atmospher Phys, Beijing 100029, Peoples R China
[3] Jilin Univ, Coll Earth Sci, Changchun 130061, Peoples R China
关键词
Net ecosystem CO2 exchange; Methane; Environmental control; Eddy covariance; Static chamber; Marsh; ECOSYSTEM CO2 EXCHANGE; METHANE EMISSIONS; DIOXIDE EXCHANGE; FLUX MEASUREMENTS; NATURAL WETLANDS; CH4; EMISSION; TABLE; VEGETATION; BALANCE; N2O;
D O I
10.1016/j.agrformet.2011.04.001
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Northern wetlands are critically important to global change because of their role in modulating atmospheric concentrations of greenhouse gases, especially CO2 and CH4. At present, continuous observations for CO2 and CH4 fluxes from northern wetlands in Asia are still very limited. In this paper, two growing season measurements for CO2 flux by eddy covariance technique and CH4 flux by static chamber technique were conducted in 2004 and 2005, at a permanently inundated marsh in the Sanjiang Plain, northeastern China. The seasonal variations of CO2 exchange and CH4 flux and the environmental controls on them were investigated. During the growing seasons, large variations in net ecosystem CO2 exchange (NEE) and gross ecosystem productivity (GEP) were observed with the range of -4.0 to 2.2 (where negative exchange is a gain of carbon from the atmosphere) and 0-7.6 g C m(-2) d(-1), respectively. Ecosystem respiration (RE) displayed relatively smooth seasonal pattern with the range of 0.8-4.2 g C m(-2) d(-1). More than 70% of the total GEP was consumed by respiration, which resulted in a net CO2 uptake of 143 +/- 9.8 and 100 +/- 9.2 g C m(-2) for the marsh over the growing seasons of 2004 and 2005, respectively. A significant portion of the accumulated NEE-C was lost by CH4 emission during the growing seasons, indicating the great potential of CH4 emission from the inundated marsh. Air temperature and leaf area index jointly affected the seasonal variation of GEP and the seasonal dynamic of RE was mainly controlled by soil temperature and leaf area index. Soil temperature also exerted the dominant influence over variation of CH4 flux while no significant relationship was found between CH4 emission and water table level. The close relationships between carbon fluxes and temperature can provide insights into the response of marsh carbon exchange to a changing climate. Future long term flux measurements over the freshwater marsh ecosystems are undoubtedly necessary. (C) 2011 Elsevier B.V. All rights reserved.
引用
收藏
页码:1131 / 1138
页数:8
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