贵州喀斯特山区土壤物理性质对土壤侵蚀的影响
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:

国家自然科学基金(40361004)和贵州省自然科学基金[2004(3049)]联合资助


Effect of Soil Physical Properties on Soil Erosion in Guizhou Karst Mountainous Region
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:

    对贵州喀斯特山区在不同土地利用方式下土壤主要物理性质对土壤侵蚀的影响进行了研究。结果表明:土壤物理性质是影响土壤侵蚀和土壤抗蚀性能的内在因素。贵州喀斯特山区土壤表现出明显的粗骨性土壤特征。不同土地利用方式下土壤物理性质具有明显的差异,林地、草地和台耕地的土壤物理性状良好,缓解了土壤侵蚀的发生发展,能有效地发挥保持水土的作用;大面积农耕坡地和裸坡地的土壤物理性状极差,促进了山区土壤侵蚀的发生发展,是引起土壤侵蚀的主要因素。喀斯特山区不同土地利用类型的土壤抗蚀能力依次为台耕地>林地、草地>坡耕地、裸坡地。

    Abstract:

    The effects on soil erosion by soil physical properties under different utilization types in Guizhou karst mountainous region were studied, the results showed that soil physical properties are internal factors on soil erosion and anti-erodibility, the karst mountainous soils are outstandingly characterized by sheleton soil in Guizhou province. The soil physical properties were greatly different under various land utilization types, the soil physical properties were very good in the wood lands, grasslands and cultivated-terrace lands, and reduced occurrence of soil erosion, but the soil physical properties were bad and difficiently favourable in agro-cultivated slope land and bare slope land. By comparison analysis, the main indexes of revaluating karst mountainous soil anti-erodibility were put forward. The soil anti-erodibility in various land utilization types was cultivated terrace land>wood land, grass land>cultivated slope land and bare slope land. The main site of soil and water loss was cultivated and bare slope lands in Guizhou karst mountainous region.

    参考文献
    相似文献
    引证文献
引用本文

徐燕 龙健.贵州喀斯特山区土壤物理性质对土壤侵蚀的影响[J].水土保持学报,2005,(1):157~159,175

复制
分享
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:
  • 录用日期:
  • 在线发布日期:
  • 出版日期:
文章二维码