globalchange  > 气候变化与战略
CSCD记录号: CSCD:5453920
论文题名:
不同水分条件下巴音布鲁克天鹅湖高寒湿地夏季N_2O日排放特征
其他题名: Daily Characteristics of Summer N_2O Emission under Different Water Conditions at Bayinbuluke Swan Lake Alpine Wetland
作者: 胡保安1; 贾宏涛2; 朱新萍2; 蒋平安2; 杨磊1; 胡毅1; 王宁宁1
刊名: 生态环境学报
ISSN: 1674-5906
出版年: 2015
卷: 24, 期:5, 页码:1556-1565
语种: 中文
中文关键词: 高寒湿地 ; 土壤
英文关键词: N_2O ; alpine wetland ; soil ; N_2O
WOS学科分类: ENVIRONMENTAL SCIENCES
WOS研究方向: Environmental Sciences & Ecology
中文摘要: 在气候变暖背景下温室气体排放特征的研究已成为全球变化的研究热点之一,而湿地生态系统与温室气体排放有着密切的关系。湿地N_2O排放对水分变化的响应机制研究对干旱区高寒湿地的科学管理具有重要意义。以新疆天山中部巴音布鲁克天鹅湖高寒湿地为研究区,采用静态箱-气相色谱法,对处于不同水分条件下高寒湿地生态系统N_2O排放特征进行研究。结果表明:(1)常年积水区、季节性积水区、常年干燥区生态系统N_2O的日平均排放通量分别为1.27、0.99、0.98 mug·m~(-2)·h~(-1)。生态系统日N_2O累积排放量分别为常年积水区30.61 mug·m~(-2)、季节性积水区23.97 mug·m~(-2)、常年干燥区23.08 mug·m~(-2)。(2)季节性积水区生态系统N_2O排放日变化表现为3峰曲线,其峰值分别出现在2:00(1.30 mug·m~(-2)·h~(-1))、11:00(1.28 mug·m~(-2)·h~(-1))和21:00(1.66 mug·m~(-2)·h~(-1)),而常年干燥区生态系统N_2O排放日变化表现为双峰曲线,峰值分别出现在9:00(1.40 mug·m~(-2)·h~(-1))和17:00(1.42 mug·m~(-2)·h~(-1))。(3)环境因素显著影响着湿地生态系统N_2O排放,地表植被活体生物量与生态系统N_2O累积排放量呈现显著正相关性,在常年积水区地下10 cm土壤温度与生态系统N_2O排放通量相关性达到显著水平(F=8.326,P=0.018),在季节性积水区土壤含水量与生态系统N_2O排放通量有显著相关性(F=4.787,P=0.043)。
英文摘要: Characteristics of greenhouse gas emission had became the focus of global change study under the background of climate warming, and the wetland ecosystem and greenhouse gas emissions are closely related. Understanding the effect of water change on the dynamics of wetland N_2O emissions is important for the scientific management of alpine wetland in arid area.Taking the alpine wetland at Swan Lake of Bayinbuluke in the middle Tianshan Mountain as a study area, the emission characteristics of N_2O was measured under different water conditions at alpine wetland ecosystems using the method of static steel chambers and gas chromatography. Results showed that: (1) The average daily emissions of N_2O at perennial seeper area, seasonal water area and perennial dry area were 1.27, 0.99, and 0.98 mug·m~(-2)·h~(-1), respectively, while the cumulative daily emissions of N_2O at perennial seeper area, seasonal water area and perennial dry area were 30.61, 23.97 and 23.08 mug·m~(-2), respectively. (2) The curve of N_2O daily emissions in seasonal water area had three peaks, which occurred at 2:00 (1.30 mug·m~(-2)·h~(-1)), 11:00 (1.28 mug·m~(-2)·h~(-1)), and 21:00 (1.66 mug·m~(-2)·h~(-1)), while the curve of N_2O daily emissions in perennial dry area peaked at 9:00 (1.40 mug·m~(-2)·h~(-1)) and 17:00 (1.42 mug·m~(-2)·h~(-1)). (3) Environmental factors had significant effect on N_2O emissions in wetland ecosystems. There is a significant positive correlation between the soil N_2O cumulative emissions and vegetation living biomass at all areas. The significant correlation between N_2O emissions and soil temperature of underground 10 cm was only found at perennial seeper area (P=0.018), while the correlation between N_2O emissions and soil water content was significant (P=0.043) only at seasonal water area.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/149730
Appears in Collections:气候变化与战略

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作者单位: 1.新疆农业大学草业与环境科学学院, 乌鲁木齐, 新疆 830052, 中国
2.新疆农业大学草业与环境科学学院, 新疆土壤与植物生态过程实验室, 乌鲁木齐, 新疆 830052, 中国

Recommended Citation:
胡保安,贾宏涛,朱新萍,等. 不同水分条件下巴音布鲁克天鹅湖高寒湿地夏季N_2O日排放特征[J]. 生态环境学报,2015-01-01,24(5):1556-1565
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