金沙江干热河谷元谋强侵蚀区土壤裂隙形成与侵蚀机制
DOI:
CSTR:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

S157.1

基金项目:

国家支撑计划课题


Mechanism of Formation of Soil Crevice and Soil Erosion in Intensively-eroded Area in Yuanmou Dry and Hot Valley of Jinshajiang River
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    根据金沙江干热河谷元谋地区红土层非常发育的裂隙现象,对该地区典型区土壤裂隙形成的环境和土壤剖面进行了调查,并采样进行相关土壤理化性质测定、粘土矿物X-射线衍射分析以及土壤微形态研究。结果表明:(1)该区旱季丰富的土壤裂隙形成与该区主要分布的第四系古红土层(QS)和第四系元谋组的黄棕色土层(QY)等红土母质特性有密切关系;(2)由于土壤裂隙非常发育,成为了边坡崩塌和直接产生重力侵蚀的成因,加剧了土壤侵蚀过程,导致了土柱和土林等强侵蚀景观形成。研究表明,土壤裂隙是金沙江干热河谷元谋地区强烈侵蚀和水土流失所特有的成因。

    Abstract:

    The Yuanmou dry and hot valley of the Jinshajiang river is one of the fragmental environment areas in China,where the soil and water loss was very serious.It is difficult to interpret the peculiar soil erosion phenomenon using the traditional opinion.This study based on the observation in the environment and soil profiles which related with developed soil crevice,and using such means as chemical analysis,X-ray diffraction pattern and micromorphology.Results showed that:(1) In this area,the developed soil crevice was significant correlated with the parent material of the quaternary system old red horizon(QS) and yellow brown horizon(QY).(2) The developed soil crevice was the main reason for soil fall and gravity erosion,as the result,the soil erosion increased obviously.Finally this paper advanced a new viewpoint that soil crevice was the most important reason of the seriously soil and water loss formation.

    参考文献
    相似文献
    引证文献
引用本文

何毓蓉,沈南,王艳强,唐家良,高庭艳,杨艳鲜,范月清.金沙江干热河谷元谋强侵蚀区土壤裂隙形成与侵蚀机制[J].水土保持学报,2008,(1):33~36

复制
分享
相关视频

文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:
  • 最后修改日期:2007-09-30
  • 录用日期:
  • 在线发布日期:
  • 出版日期:
文章二维码
关闭