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天山中部巴音布鲁克高寒草原大气无机氮沉降

岳平1,2,宋韦1,2,李凯辉1**,贺桂香1,2,王晓丽1,2,刘学军1,3   

  1. (1中国科学院新疆生态与地理研究所干旱区生物地理与生物资源重点实验室, 乌鲁木齐 830011; 2中国科学院大学, 北京 100049; 3中国农业大学资源与环境学院, 北京 100193)
  • 出版日期:2014-06-18 发布日期:2014-06-18

Inorganic N deposition in the Bayinbuluk alpine grassland of the central Tianshan mountains.

YUE ping1,2, SONG Wei1,2, LI Kai-hui1, HE Gui-xiang1,2, WANG Xiao-li1,2, LIU Xue-jun1,3   

  1. (1Key Laboratory of Biogeography and Bioresource in Arid Land, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China; 2University of Chinese Academy of Sciences, Beijing 100049, China; 3College of Resources and Environmental Sciences, China Agricultural University, Beijing 100193, China)
  • Online:2014-06-18 Published:2014-06-18

摘要:

随着我国经济的不断发展,人为活动导致的大气氮沉降显著升高,并已影响到偏远地区的生态系统.为了系统评价天山中部巴音布鲁克高寒草原的大气氮沉降现状, 2010年5月至2011年12月对研究区域的氮素干、湿沉降进行观测分析.结果表明: 研究区气态HNO3、NH3和NO2的年沉降通量分别为1.47、0.68和0.13 kg N·hm-2,颗粒物中铵态氮(NH4+)和硝态氮(NO3-)的年通量分别为0.23、0.25 kg N·hm-2;降水中NH4+-N和NO3--N的年沉降通量分别为2.47和1.59 kg N·hm-2.巴音布鲁克高寒草原的大气氮沉降通量为6.82  kg N·hm-2.其中,湿沉降为4.06 kg N·hm-2·a-1,干沉降为2.76 kg N·hm-2·a-1.研究区氮沉降具有明显的季节变化特征:干沉降主要集中在春、夏季,占干沉降总量的72.1%;湿沉降主要集中在夏、秋季,占湿沉降总量的78.3%.

 

Abstract: N deposition has increased significantly with economic development and intensive human activities in China and has affected natural ecosystems in remote areas. To evaluate the atmospheric N deposition of the Bayinbuluk alpine grassland of the central Tianshan Mountains, the dry and wet N depositions were monitored from May 2010 to December 2011. Fluxes of HNO3, NH3, NO2, particulate ammonium and nitrate (pNH4+ and pNO3-) averaged at 1.47, 0.68, 0.13, 0.23 and 0.25 kg N·hm-2·a-1, respectively. Wet depositions of NH4+-N and NO3--N were 2.47 and 1.59 kg N·hm-2·a-1, respectively. Total atmospheric inorganic N deposition fluxes averaged at 6.82 kg N·h-2·a-1, and the wet and dry depositions were 4.06 and 2.76 kg N·hm-2·a-1, respectively. Nitrogen deposition fluxes showed a significant seasonal change, with 72.1% of dry N deposition occurring in spring and summer, and 78.3% of wet N deposition concentrating in summer and autumn.