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人工降雨条件下土壤结皮的形成以及与土壤溅蚀的关系
引用本文:胡霞 严平 李顺江 蔡强国 刘连友 蔡崇法 朱远达 张光远. 人工降雨条件下土壤结皮的形成以及与土壤溅蚀的关系[J]. 水土保持学报, 2005, 19(2): 13-16
作者姓名:胡霞 严平 李顺江 蔡强国 刘连友 蔡崇法 朱远达 张光远
作者单位:1. 北京师范大学,资源学院,北京,100875
2. 中国科学院,地理科学与资源研究所,北京,100101
3. 华中农业大学,资源环境学院,湖北,武汉,430070
基金项目:国家科技攻关项目(2002BA517A10)和中国科学院地理科学与资源研究所创新工程项目(CXIOG-A00-05-02)以及国家自然科学基金(30371191)资助
摘    要:通过人工模拟降雨溅蚀实验,测定土壤溅蚀速率,同时采样制作土壤切片,观察分析结皮的发育特征以及与土壤溅蚀的关系。结果表明,降雨过程中有两种类型结皮形成,即沉积结皮和结构结皮。土壤结皮随着土壤表面大团聚体或者大颗粒的分散而形成,并且伴随着下层大孔隙的出现。土表结皮的完善过程,也是土壤抗溅蚀能力增强的过程

关 键 词:人工模拟降雨  沉积结皮  结构结皮  溅蚀
文章编号:1009-2242(2005)02-0013-04

Development of Soil Crust Through Rainfall Simulating in Laboratory and Relationship Between Crust and Splash Erosion
HU Xia~,YAN Ping~,LI Shun-jiang~,CAI Qiang-guo~,HU Liang-you,CAI Chong-fa~,ZHU Yuan-da~,ZHANG Guang-yuan~. Development of Soil Crust Through Rainfall Simulating in Laboratory and Relationship Between Crust and Splash Erosion[J]. Journal of Soil and Water Conservation, 2005, 19(2): 13-16
Authors:HU Xia~  YAN Ping~  LI Shun-jiang~  CAI Qiang-guo~  HU Liang-you  CAI Chong-fa~  ZHU Yuan-da~  ZHANG Guang-yuan~
Affiliation:HU Xia~1,YAN Ping~1,LI Shun-jiang~2,CAI Qiang-guo~2,HU Liang-you,CAI Chong-fa~3,ZHU Yuan-da~2,ZHANG Guang-yuan~3
Abstract:Through rainfall simulating in laboratory, and observation on soil sample slices, this study intended to disclose crust development, and reveal the relationship between crust and splash erosion. Two kinds of crust, i.e., structural crust and depositional crust, were observed in the experiment. With the development of crust, bigger aggregates and grains were dispersed, and bigger pores formed beneath the crust. The development of crust was also the process of soil resisting splash erosion enhanced.
Keywords:rainfall simulating in laboratory  depositional crust  structural crust  splash erosion
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