人工降雨条件下土壤结皮的形成以及与土壤溅蚀的关系

您当前的位置：

首页 >

文章列表页 >

更新时间：2024-11-07

- 人工降雨条件下土壤结皮的形成以及与土壤溅蚀的关系
- Development of Soil Crust Through Rainfall Simulating in Laboratory and Relationship Between Crust and Splash Erosion
- 水土保持学报 2005年第2期页码：13-16
- 作者机构：
- 作者简介：
- 基金信息：
  
  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
- DOI：
  中图分类号：
- 纸质出版：2005
- 稿件说明：
移动端阅览
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,(2):13-16.

Development of Soil Crust Through Rainfall Simulating in Laboratory and Relationship Between Crust and Splash Erosion[J]. 2005, (2): 13-16.
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,(2):13-16. DOI：

Development of Soil Crust Through Rainfall Simulating in Laboratory and Relationship Between Crust and Splash Erosion[J]. 2005, (2): 13-16. DOI：

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

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.

浏览量

下载量

CSCD

文章被引用时，请邮件提醒。

提交

工具集

关联资源

人工降雨条件下土壤结皮的形成以及与土壤溅蚀的关系