首页> 外文期刊>Eurasian Journal of Soil Science >An experimental investigation of rill erosion processes in lateritic upland region: A pilot study
【24h】

An experimental investigation of rill erosion processes in lateritic upland region: A pilot study

机译:红土高地地区小溪侵蚀过程的实验研究:一项试点研究

获取原文
       

摘要

The present paper is based on field investigation and measurement of rill erosion processes at Rangamati Experimental Station (Medinipur, West Bengal in India). In rill experiments, three different natural rills were studies in field for understanding of the dynamics of soil erosion processes of a rill catchment area. Geometric and morphological characteristics of each rill catchment area were analyzed. Results showed the widening, deepening and extended of rills because of sidewall sloughing, knick-points and head-ward erosion during surface runoff process. Progressive increases of rill volume were observed in the upper, middle and lower catchment with the change of time. Rill area has increased by runoff processes of 4.2 % and 6.8 % for Rill-A and Rill-B respectively. These processes are depends on surface coverage, soil texture, slope gradients and runoff velocity.
机译:本文基于在Rangamati实验站(印度西孟加拉邦梅迪尼布尔)的钻探侵蚀过程的现场调查和测量。在小溪实验中,在野外研究了三种不同的自然小溪,以了解小溪集水区土壤侵蚀过程的动态。分析了每个小溪集水区的几何和形态特征。结果表明,由于地表径流过程中的侧壁塌陷,拐点和头朝前的侵蚀,小溪的扩大,加深和扩展。随着时间的变化,上,中,下流域的小溪体积逐渐增加。 Rill-A和Rill-B的径流面积分别增加了4.2%和6.8%。这些过程取决于地表覆盖率,土壤质地,坡度和径流速度。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号