Fluxes of carbon dioxide and methane from swamp and impact factors in Sanjiang Plain, China

被引:49
作者
Song, CC [1 ]
Yan, BX
Wang, YS
Wang, YY
Lou, YJ
Zhao, ZC
机构
[1] Chinese Acad Sci, NE Inst Geog & Agr Ecol, Changchun 130012, Peoples R China
[2] Chinese Acad Sci, Inst Atmospher Phys, Beijing 100101, Peoples R China
来源
CHINESE SCIENCE BULLETIN | 2003年 / 48卷 / 24期
关键词
swamp; ecosystem respiration; CH4; flux; impact factor;
D O I
10.1360/03wd0250
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The fluxes Of CO2 and CH4 emission of the two types of primary swamp were measured in Sanjiang Plain using the opaque chamber and gas chromatogram technique. The mean value of ecosystem respiration flux in continuously inundated swamp ecosystem is 548.04 mg.m(-2).h(-1), lower than that of the seasonal inundated swamp (713.08 mg.m(-2).h(-1)). The peaks concentrated on July and August which are the growing period of the vegetation. CH4 emission was different from the respiration flux of ecosystem. The CH4 flux of continuously inundated swamp was 12.80 mg.m(-2.)h(-1), larger than that of the seasonal inundated swamp (8.56 mg.m(-2).h(-1)), and they were varied at different periods, the continuously inundated swamp emitted CH4 mainly from July to September, whereas from last August to middle September in the seasonal inundated swamp. The ecosystem respiration flux of the swamp has the significantly positive correlation with the soil temperature (0-10 cm depth) and the water temperature, but CH4 emission was associated with the soil temperature in a certain degree. The CH4 emission from swamp depends on the integral function of water table and soil temperature.
引用
收藏
页码:2749 / 2753
页数:5
相关论文
共 19 条
[1]  
Alm J, 1999, ECOLOGY, V80, P161, DOI 10.1890/0012-9658(1999)080[0161:CBOABB]2.0.CO
[2]  
2
[3]  
BARKLETT KB, 1993, CHEMOSPHERE, V26, P261
[4]   Sensitivity of a high-elevation Rocky Mountain watershed to altered climate and CO2 [J].
Baron, JS ;
Hartman, MD ;
Band, LE ;
Lammers, RB .
WATER RESOURCES RESEARCH, 2000, 36 (01) :89-99
[5]   Controls on CH4 emissions from a northern peatland [J].
Bellisario, LM ;
Bubier, JL ;
Moore, TR ;
Chanton, JP .
GLOBAL BIOGEOCHEMICAL CYCLES, 1999, 13 (01) :81-91
[6]   Are Phragmites-dominated wetlands a net source or net sink of greenhouse gases? [J].
Brix, H ;
Sorrell, BK ;
Lorenzen, B .
AQUATIC BOTANY, 2001, 69 (2-4) :313-324
[7]   Carbon dioxide and methane exchange of a subarctic heath in response to climate change related environmental manipulations [J].
Christensen, TR ;
Michelsen, A ;
Jonasson, S ;
Schmidt, IK .
OIKOS, 1997, 79 (01) :34-44
[8]   BIOGEOCHEMICAL ASPECTS OF ATMOSPHERIC METHANE [J].
Cicerone, R. ;
Oremland, R. .
GLOBAL BIOGEOCHEMICAL CYCLES, 1988, 2 (04) :299-327
[9]   METHANE EMISSION FROM MINNESOTA PEATLANDS - SPATIAL AND SEASONAL VARIABILITY [J].
DISE, NB .
GLOBAL BIOGEOCHEMICAL CYCLES, 1993, 7 (01) :123-142
[10]   CLIMATE CONTROLS ON TEMPORAL VARIABILITY OF METHANE FLUX FROM A POOR FEN IN SOUTHEASTERN NEW-HAMPSHIRE - MEASUREMENT AND MODELING [J].
FROLKING, S ;
CRILL, P .
GLOBAL BIOGEOCHEMICAL CYCLES, 1994, 8 (04) :385-397