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基于~(137)Cs示踪法的太湖流域典型山地土壤侵蚀规律分析
引用本文:陕永杰,濮励杰,张健,朱明,王海燕,赵艳,彭补拙.基于~(137)Cs示踪法的太湖流域典型山地土壤侵蚀规律分析[J].水土保持学报,2011,25(2):29-32,38.
作者姓名:陕永杰  濮励杰  张健  朱明  王海燕  赵艳  彭补拙
作者单位:1. 南京大学地理与海洋科学学院,江苏,南京,210093;山西师范大学城市与环境科学学院,山西,临汾,041004
2. 南京大学地理与海洋科学学院,江苏,南京,210093;国土资源部土地利用重点实验室,北京,100029
3. 南京大学地理与海洋科学学院,江苏,南京,210093
基金项目:国家自然科学基金委“基础科学与人才培养基金”(J0630535); 南京大学“科研创新基金”(2007CL10)
摘    要:在生态环境敏感区—太湖周边选择两个地质构造不同的山体,运用137Cs示踪法分析了137Cs分布和土壤侵蚀规律。结果表明:沉积岩山体黄棕壤的137Cs含量表层大于底层,岩浆岩山体黄红壤137Cs含量中部高,表层和底层低。岩浆岩山体坡面的土壤侵蚀变化情况为:坡顶>坡上部>坡中部>坡底;沉积岩山体坡面土壤侵蚀变化为:坡中部>坡下部>破上部。研究区土壤侵蚀整体而言为微度或轻度侵蚀,在太湖周边区域未经人为扰动的山体表土移动运输程度很小,不会对山前平原和太湖水体造成明显影响,土壤流失不显著。

关 键 词:137Cs示踪法  太湖流域  土壤侵蚀

Analysis of Soil Erosion Rules of Typical Mountain along Taihu Lake Basin Using ~(137)Cs-based Tracer Method
SHAN Yong-jie,PU Li-jie,ZHANG Jian,ZHU Ming,WANG Hai-yan,ZHAO Yan,PENG Bu-zhuo.Analysis of Soil Erosion Rules of Typical Mountain along Taihu Lake Basin Using ~(137)Cs-based Tracer Method[J].Journal of Soil and Water Conservation,2011,25(2):29-32,38.
Authors:SHAN Yong-jie  PU Li-jie  ZHANG Jian  ZHU Ming  WANG Hai-yan  ZHAO Yan  PENG Bu-zhuo
Institution:SHAN Yong-jie1,2,PU Li-jie1,3,ZHANG Jian1,ZHU Ming1,WANG Hai-yan1,ZHAO Yan1,PENG Bu-zhuo1(1.School of Geographic and Oceanographic Sciences,Nanjing University,Nanjing,Jiangsu 210093,2.College of Urban and Environment Sciences,Shanxi Normal University,Linfen,Shanxi 041004,3.Key Laboratory of Land Use Ministry of Land and Resources,Beijing 100029)
Abstract:Two different geological formations of mountains of ecological sensitive areas around Taihu lake were selected,and 137Cs tracer method was used to analyze the137Cs distribution and soil erosion rules.The results showed that: The137Cs content on the surface of yellow brown soil of sedimentary rocks was more than at the bottom,while the137Cs content in central of rocky body yellow red lava was higher than on the surface and at bottom.Soil erosion variances along body of magma rocky slope were: top of the hill...
Keywords:137Cs-based tracer method  Taihu lake basin  soil erosion  
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