中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
第七章 中国泥石流灾害区划

文献类型:专著章节/文集论文

作者刘琼招 ; 唐川
专著(文集)名中国自然灾害区划 灾害区划、影响评价、减灾对策
其他责任者王劲峰 等 著
出版日期1995
出版者中国科学技术出版社 ; 中国科学技术出版社
出版地北京 ; 北京
出处页码131-166
关键词泥石流 孕育环境 分类分级 危险评价指标 泥石流 孕育环境 分类分级 危险评价指标
出版者中国科学技术出版社 ; 中国科学技术出版社
出版地北京 ; 北京
关键词泥石流 孕育环境 分类分级 危险评价指标 泥石流 孕育环境 分类分级 危险评价指标
其他题名CHAPTER 7 THE REGIONALIZATION OF DEBRIS FLOW HAZARD IN CHINA
中文摘要

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。

英文摘要

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.

语种中文
源URL[http://ir.imde.ac.cn/handle/131551/7810]  
专题成都山地灾害与环境研究所_成都山地所知识仓储(2009年以前)
推荐引用方式
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, 北京:中国科学技术出版社, 中国科学技术出版社,1995:131-166.

入库方式: OAI收割

来源:成都山地灾害与环境研究所

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