IMHE OpenIR  > 成都山地所知识仓储(2009年以前)
第七章 中国泥石流灾害区划
Alternative TitleCHAPTER 7 THE REGIONALIZATION OF DEBRIS FLOW HAZARD IN CHINA
Language中文
刘琼招; 唐川
Source Publication中国自然灾害区划 灾害区划、影响评价、减灾对策
Editor王劲峰 等 著
Pages131-166
1995
Publisher中国科学技术出版社
Publication Place北京
Keyword泥石流 孕育环境 分类分级 危险评价指标
Abstract

分析泥石流的孕育环境,根据分类分级与危险评价指标,作出自然过程层面的全国泥石流强度频度图、人文过程层面的全国泥石流损失危险图。

Other Abstract

The regionalization boundary lines are mainly in light of the boundary of watershed. Because the occurrence and development ofdebris flow are all under the control of the range of watershed, which namely the synthetcal circulating system including many factors such as geology, landferm, hydrology, climate, ect, the rang of debris flow disaster is also under the control of the range of watershed. the whole country can be divided into four maijor are as according to the ocean where big river draft in and the extent of debris flow disater. The dangerous extent in whole major area and whole year or many years (namely in time and space) are not even, being of the characteristics of phaseand fluctuation. Because the dangerous extent in the same major area is different yet, it can be further divided into four degrees on the basis of debris flow characterstics. The dangerous extent in the debris flow distributed flow distributed area or active regions are not even too. The dangerous area of debris flow mainly locte at accumlative area and transporting area.
The active belt of debris flow has closely relation to gelogical structure, earthquake Debirs flows are mainly distributed on the sounthern slope with an elevation between 800-2500 meter and gradient between 25°~33°,the gully-type debris flows are mainly distributed in the ravines with a longitudinal 100‰~400‰. On the geology,debris flow distribution is under the control of active fault zone and the lithogy (soft statum or soft and hard altemated statum favour the occurence of debris flow). In the climate, debris flow distribution is under the control of rainfall and temperature, especially, the beavy rain in parts of an area, in a process of rainfall, serveral debris flow gullies are generated at the same time, beside, in the dry-hot river valley regions, debris flows frequent too. The unrasonble hiam economic activities as minings, bulding roads, denudation of forests and steep land cultivation are all the causes of debris flow generation.

Document Type专著章节文集论文
Identifierhttp://ir.imde.ac.cn/handle/131551/7810
Collection成都山地所知识仓储(2009年以前)
Recommended Citation
GB/T 7714
刘琼招,唐川. 第七章 中国泥石流灾害区划. 中国自然灾害区划 灾害区划、影响评价、减灾对策. 北京:中国科学技术出版社,1995:131-166.
Files in This Item:
File Name/Size DocType Version Access License
第七章 中国泥石流灾害区划.pdf(3298KB) 开放获取CC BY-NC-SAView Application Full Text
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[刘琼招]'s Articles
[唐川]'s Articles
Baidu academic
Similar articles in Baidu academic
[刘琼招]'s Articles
[唐川]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[刘琼招]'s Articles
[唐川]'s Articles
Terms of Use
No data!
Social Bookmark/Share
File name: 第七章 中国泥石流灾害区划.pdf
Format: Adobe PDF
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.