Effects of Rainfall on the Characteristics of Soil Greenhouse Gas Emissions in the Wetland of Qinghai Lake

被引:9
|
作者
Yang, Ziwei [1 ,2 ,3 ]
Chen, Kelong [2 ,3 ]
Liu, Fumei [1 ,2 ,3 ]
Che, Zihan [2 ,3 ]
机构
[1] Qinghai Normal Univ, Sch Geog Sci, Xining 810008, Peoples R China
[2] Qinghai Normal Univ, Key Lab Nat Geog & Environm Proc Qinghai Prov, Xining 810008, Peoples R China
[3] Qinghai Normal Univ, Minist Educ, Key Lab Qinghai Tibet Plateau Surface Proc & Ecol, Xining 810008, Peoples R China
基金
中国国家自然科学基金;
关键词
lakeside wetland; greenhouse gas fluxes; static chamber-gas chromatography; rainfall changes; METHANE EMISSIONS; CARBON-DIOXIDE; DENITRIFICATION; RESPIRATION; FLUX;
D O I
10.3390/atmos13010129
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Niaodao, a lakeside wetland, was used as the focus of this study to investigate the effect of rainfall changes on the greenhouse gas fluxes of wetland ecosystems. Wetland plots with different moisture characteristics (+25%, -25%, +75%, and -75% rainfall treatments and the control treatment (CK)) were constructed to observe in situ field greenhouse gas emissions at 11:00 and 15:00 (when the daily mean values were similar) in the growing season from May to August 2020 by static chamber-gas chromatography and to investigate the responses of wetland greenhouse gases to different rainfall treatments. The results showed the following: (1) The carbon dioxide (CO2) flux ranged from -49.409 to 374.548 mg center dot m(-2)center dot h(-1). The mean CO2 emission flux was greater at 11:00 than at 15:00, and the +25% and +75% treatments exhibited substantially higher CO2 emissions. In addition, the CO2 flux showed a small peak at the beginning of the growing season when the temperature first started to rise. All treatments showed the effect of the CO2 source, and their effects were significantly different. (2) The methane (CH4) flux ranged from -213.839 to 330.976 mu g center dot m(-2)center dot h(-1) and exhibited an absorption state at 11:00 and an emission state at 15:00. The CH4 emission flux in August (the peak growing season) differed greatly between treatments and was significantly negatively correlated with the rainfall amount (p < 0.05). (3) The nitrous oxide (N2O) flux ranged from -10.457 to 16.878 mu g center dot m(-2)center dot h(-1) and exhibited a weak source effect throughout the growing season, but it was not significantly correlated with soil moisture; it was, however, negatively correlated with soil temperature. (4) The different treatments resulted in significant differences in soil physical and chemical properties (electrical conductivity, pH, total soil carbon, and total soil nitrogen). The rainfall enhancement treatments significantly improved soil physical and chemical properties.
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页数:15
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