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雅鲁藏布江河水中CH4和N2O气体浓度及释放特征

叶润成1,2,吴起鑫1,赵志琦2,胡健2,崔丽峰2,丁虎2,3*   

  1. (1贵州大学国土资源部喀斯特环境与地质灾害重点实验室, 贵阳 550025;2中国科学院地球化学研究所环境地球化学国家重点实验室, 贵阳 550081;3University of Glasgow, Glasgow G12 8QQ, Scotland, UK)
  • 出版日期:2019-03-10 发布日期:2019-03-10

Concentrations and emissions of dissolved CH4 and N2O in the Yarlung Tsangpo River.

YE Run-cheng1,2, WU Qi-xin1, ZHAO Zhi-qi2, HU Jian2, CUI Li-feng2, DING Hu2,3*   

  1. (1Key Laboratory of Karst Environment and Geohazard, Ministry of Land and Resources, Guizhou University, Guiyang 550025, China; 2State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China; 3University of Glasgow, Glasgow G12 8QQ, Scotland, UK).
  • Online:2019-03-10 Published:2019-03-10

摘要: 河流向大气释放大量温室气体,是陆地生态系统物质循环和能量流动的重要环节。山地河流是温室气体排放的热点区域,但迄今山地河流CH4和N2O释放方面的研究较少。为探究高原中大型河流CH4和N2O浓度的时空分布特征及其影响因素,对雅鲁藏布江(雅江)干流和主要支流河水中CH4和N2O气体进行了季节性采样分析。结果表明,雅江河水中CH4含量为2.3~864.9 nmol·L-1,N2O含量为8.2~23.7 nmol·L-1,枯水期CH4含量和丰水期无显著差异(P=0.112),但枯水期N2O含量显著高于丰水期(P=0.017),流量和水温可能分别是影响CH4和N2O变化的主要因子。雅江河水CH4和N2O的释放速率分别为4.3~11.1 mg C·m-2·d-1和0.16~0.37 mg N·m-2·d-1,排放量分别为1.88~4.59 Gg C·a-1和0.07~0.16 Gg N·a-1,分别约占全球河流CH4和N2O释放量的1.25‰~3.06‰和2.17‰~4.96‰。山地河流CH4和N2O的排放需要引起重视,全球河流温室气体释放可能需要进行重新评估。  

关键词: 草地早熟禾, 聚类分析, 种子产量, 产量性状

Abstract: Rivers release large quantities of greenhouse gases into the atmosphere, which is an important link in the material cycling and energy flow of terrestrial ecosystems. Mountainous rivers are ‘hotspots’ for greenhouse gas emission, but the release of CH4 and N2O from those rivers has been less documented. To explore the spatiotemporal distributions and related controls of CH4 and N2O in middle-large plateau rivers, the seasonal variations of CH4 and N2O in tributary and main stream of the Yarlung Tsangpo River were examined. The results showed that the ranges of CH4 and N2O concentrations in the Yarlung Tsangpo were 2.3-864.9 and 8.2-23.7 nmol·L-1, respectively. There was no significant difference in CH4 concentrations between low-flow and high-flow periods (P=0.112), but the N2O contents were higher in low-flow months than in high-flow months (P=0.017). River water discharge and water temperature were the major factors controlling the dynamics of CH4 and N2O emission, respectively. The release rates of CH4 and N2O in the Yarlung Tsangpo River ranged 4.3-11.1 mg C·m-2·d-1 and 0.16-0.37 mg N·m-2·d-1, respectively. The emission amounts of CH4 and N2O in Yarlung Tsangpo River system were 1.88-4.59 Gg C·a-1 and 0.07-0.16 Gg N·a-1, accounting for 1.25‰-3.06‰ and 2.17‰-4.96‰ of global river estimations, respectively. The evasion of CH4 and N2O in mountainous rivers need further detailed studies, which may revise the global estimation of greenhouse gas emission.

Key words: Poa pratensis, Cluster analysis, Seed yield, Yielding characteristics