Systematic Analysis of Slope Disintegration Erosion Landform in South China

WU Zhifeng; LI Dingqiang; QIU Shijun

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Systematic Analysis of Slope Disintegration Erosion Landform in South China

- Systematic Analysis of Slope Disintegration Erosion Landform in South China
- Bulletin of Soiland Water Conservation Vol. 18, Issue 5, Pages: 24-26(1999)
- 作者机构：
  
  1. 广东省生态环境与土壤研究所,广东,广州,510650
  2. 华南师范大学地理系,广东,广州,510631
- 作者简介：
- 基金信息：
- DOI：
  CLC：
- Published：1999
- 稿件说明：
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WU Zhifeng, LI Dingqiang, QIU Shijun. Systematic Analysis of Slope Disintegration Erosion Landform in South China[J]. Bulletin of Soiland Water Conservation, 1999, 18(5): 24-26.
DOI：

WU Zhifeng, LI Dingqiang, QIU Shijun. Systematic Analysis of Slope Disintegration Erosion Landform in South China[J]. Bulletin of Soiland Water Conservation, 1999, 18(5): 24-26. DOI：

摘要

崩岗侵蚀是华南水土流失区最严重的一种水土流失类型。崩岗由崩壁、崩积堆和冲（洪）积扇3部分，组成三者在发生上具有相关性，并且通过物质的输送和能量的转化共同组成一个完整的侵蚀地貌系统。崩岗侵蚀地貌系统的发育规模通常首先表现出一个Logistic增长过程，随后系统的演化可分持续发展、波动、稳定平衡、消亡4种趋势

Abstract

Slope disintegration erosion is the most serious type of soil erosion in south China. Based on the field investigation

spatial structure of the erosion landform was analyzed. According to studies on the transmission and transformation of material and energy

and the feedback mechanism

the slope disintegration erosion landform system was built. The evolution tendency of the system included 4 directions such as sustained development

fluctuation

stable equilibrium and vanishment.

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