摘要
本文依据泥石流灾害体形态确定的地貌发育程度构建了泥石流灾害的评价模型,并将熵理论综合应用于泥石流评价模型,应用该模型对兰州地区山谷泥石流趋势进行了分析,并指出了评价模型的不足。
Lanzhou urban has become a famous debris flow area in the upper reaches of Yellow River because of steep and frangible topographic, active geotectonic, soft and hard rock mass alternation, rainfall in a very short period and unreasonable development. This paper constructs an evaluation model on debris flow disaster by means of surface development degree of debris flow catastrophic body morphological, analyze valley debris flow development trend of Lanzhou urban areas applying entropy theory, and indicates the shortcomings of the debris flow evaluation model.
出处
《水文地质工程地质》
CAS
CSCD
北大核心
2006年第3期93-96,共4页
Hydrogeology & Engineering Geology
基金
西北师范大学科技与创新工程一期项目
西北师大青年基金资助
关键词
泥石流
系统熵模型
趋势分析
兰州
debris flow
system entropy model
trend analysis
Lanzhou