A Study on Features and Formative Environment of Debris Flow in Fangdui Gully

Zhang Liping; Zhang Pingcang; Tang Keli

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A Study on Features and Formative Environment of Debris Flow in Fangdui Gully

- A Study on Features and Formative Environment of Debris Flow in Fangdui Gully
- Bulletin of Soiland Water Conservation Vol. 17, Issue 3, Pages: 39-41(1998)
- 作者机构：
  
  中国科学院水利部水土保持研究所,陕西杨陵,712100
- 作者简介：
- 基金信息：
- DOI：
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- Published：1998
- 稿件说明：
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Zhang Liping, Zhang Pingcang, Tang Keli. A Study on Features and Formative Environment of Debris Flow in Fangdui Gully[J]. Bulletin of Soiland Water Conservation, 1998, 17(3): 39-41.
DOI：

Zhang Liping, Zhang Pingcang, Tang Keli. A Study on Features and Formative Environment of Debris Flow in Fangdui Gully[J]. Bulletin of Soiland Water Conservation, 1998, 17(3): 39-41. DOI：

摘要

通过对山西省文水县北徐村房对沟1990年7月11日泥石流实地调查及访问

分析了该沟泥石流的形成环境

分析认为房对沟是一条由非泥石流沟演化而成的一条典型人为泥石流沟

没有明显的物源补给区及通过区之分

是由许多坡面型泥石流汇合而成的复合型沟谷泥石流。如果现在不进行治理

一旦暴雨突降

则泥石流爆发

后果不堪设想。

Abstract

The formative environment of debris flow is analysed by means of investigation in Fangduigully of Wenshui county.It is considered that Fangduigully is a typical complex debris flow gully affected by human actions.There is no clear distinction between areas of solid materials accumulation and passage way.At last

the debris flow of Fang duigully is predicted.The conclusion is that if there is no control engineering

the debris flow will become more serious when storm occurs.

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