摘要
为了研究大气通过干湿沉降输入到农田土壤的氮通量,2007年6月至2008年5月在陕西榆林和洛川两地进行了为期一年的观测试验.结果表明:榆林和洛川地区大气总无机氮沉降通量分别为22.17和16.95kg.hm-2.a-1,湿沉降分别占95.1%和90.4%,干沉降分别占4.9%和9.6%,两个地区氮沉降均以湿沉降为主.总无机氮沉降中,NO3--N分别为12.22和9.24kg.hm-2.a-1,分别占总无机氮沉降量的55.1%和54.5%.由于污染水平、气象条件、下垫面特性等的差异,总无机氮沉降中,湿沉降量和NO3--N沉降量均是榆林地区大于洛川地区.
To investigate the farmland soil nitrogen input from atmospheric dry and wet deposition,a 1-year observation was conducted in the Yulin and Luochuan areas of North Shaanxi Province from June 2007 to May 2008.The total inorganic nitrogen （TIN） deposition in Yulin and Luochuan was 22.17 and 16.95 kg·hm-2·a^-1,among which,wet deposition accounted for 95.1% and 90.4%,while dry deposition accounted for 4.9% and 9.6%,respectively,illustrating that the nitrogen deposition in both Yulin and Luochuan was mainly come from wet deposition.In the TIN deposition,the amount of nitrate in Yulin and Luochuan was 12.22 and 9.24 kg·hm-2·a^-1,accounting for 55.1% and 54.5%,respectively.The amount of wet deposition and the percentage of nitrate in TIN deposition were higher in Yulin than in Luochuan,because of the differences in pollution level,weather condition,and underlying surface characteristics.
出处
《应用生态学报》
CAS
CSCD
北大核心
2010年第1期255-259,共5页
Chinese Journal of Applied Ecology
基金
国家自然科学基金项目(40675006)
教育部博士点基金项目资助
关键词
陕北
大气氮沉降
湿沉降
干沉降
North Shaanxi
atmospheric nitrogen deposition
wet deposition
dry deposition.
