题名滑坡危险度评价与预警方法研究——以三峡库区重庆市万州区为例
作者杨宗佶
学位类别博士
答辩日期2009
授予单位中国科学院水利部成都山地灾害与环境研究所
授予地点成都
导师乔建平
关键词滑坡 危险度评价 滑坡致滑概率 降雨 预警 万州区
学位专业自然地理学
中文摘要三峡库区位于长江上游,沿江两岸多为山地地形,滑坡灾害发生频繁,尤其是大、中型滑坡比较发育。这些滑坡灾害数量多、分布广、规模大,对当地的经济建设和生命财产造成了很大的危害,如何对滑坡进行便捷有效的评价和预警成为滑坡减灾防灾的关键。本研究是以万州区作为研究区,首先建立区域滑坡和单体滑坡危险度评价的指标体系,作为滑坡预警的本底环境因素,实现了对研究区区域和单体的滑坡危险度评价;由于降雨是三峡库区滑坡的重要外动力因素,结合降雨和滑坡的相关分析并建立滑坡降雨致滑模型,将滑坡本底环境因素与其诱发因素降雨进行耦合建立降雨型滑坡概率预警模型,从而实现对区域和单体滑坡进行点面结合的概率预警的目的。 全文共分九章:第一章,绪论;第二章,研究区环境概况;第三章,滑坡时空分布规律及形成机理;第四章,危险度评价客观权重的确定;第五章,区域滑坡危险度区划;第六章,单体滑坡危险度评价;第七章,滑坡与降雨关系;第八章,降雨型滑坡概率预警;第九章,结论和展望。 论文研究主要取得以下研究成果: (1)对万州区滑坡时空分布规律及形成机制进行了深入分析,滑坡时间分布是分别从滑坡的年际分布、年内分布和日分布来分析滑坡在时间上的规律特征。空间分布主要从滑坡与地层岩性、地形地貌、地质构造和坡形等多个地质环境因素的空间规律和分布特征统计来揭示其对滑坡的影响机制。最后分别从本底因子和触发因子两方面来论述了万州区滑坡的形成机理。 (2)建立万州区滑坡危险度区划体系,区划模型采用信息熵方法,根据历史滑坡资料求解各个因子的客观权重,因子赋值方式采用滑坡发生概率赋值;通过多因子叠加,得到万州区滑坡危险度区划结果。并分别从三种不同的分类方法对结果进行了检验,危险区滑坡发育密度上看,三种方法得到的结果都是高危险度区>中危险度区>低危险度区; (3)建立万州区单体滑坡危险度评价模型,通过对地层岩性、规模和变形迹象等8个致灾因子的滑坡发生概率进行因子赋值,采取滑坡发生概率赋值和信息熵计算因子熵权建立评价模型和指标体系,最后采用单体滑坡评价模型对万州区4个典型滑坡进行了评价和验证。并通过各个典型滑坡的深部位移监测数据和前人的研究成果来检验评价结果的正确性。 (4)在结合研究区1980~2005年逐日降雨资料和滑坡数据库的基础上,对研究区滑坡与当日降雨量、前10 d每日降雨量、滑坡与暴雨和连续性降雨的关系进行了统计分析,得到降雨对研究区滑坡的作用机理,确定了滑坡的前期有效降雨量模型,并建立了不同滑坡危险度区内滑坡发育的降雨临界值表达式。再通过对不同危险地区内降雨滑坡的频率分析和Binary logistic回归模型,得到了适合本研究区的区域和单体滑坡降雨致滑概率模型。 (5)结合降雨致滑概率模型,以及气象部门提供的前期有效降雨量和降雨概率为基础进行滑坡预警。建立了进行万州区降雨型滑坡预警的指标体系,并根据滑坡概率的不同进行了预警分级:黄色预警、橙色预警和红色预警,达到了对研究区进行降雨型滑坡预警的目的。并采取点面结合的方式和概率预警模型对万州区进行了预警的实例模拟。最后建立了万州区降雨型滑坡预警平台,对研究方法、成果及数据进行了整合和应用。
英文摘要

Three Gorges Reservoir lies in the upstream of Yangtze River, massive landslides
hazard is frequent and widespread because of the rough terrain and susceptible
geological environment, which is seriously threatened the local settlement and their
development. As a result the convenient hazard assessment and prediction in this area
is critical for disaster prevention and reduction. This research is exampled in Wanzhou
county, Chongqing city, and the assessment and prediction model’re established
according to the probability method. Landslide hazard assessment is the
environmental conditions of the landslides occurrences, combining with precipitation
and rainfall probability prediction of Meteorological Department as the triggering
factor, the prediction model are established, which can be used in both regional scale
and site-specific rainfall-induced landslide prediction in the study area.
This paper consists of nine chapters: (1) Introduction; (2) Background of the
study area; (3) Distribution and mechanism of landslides in the study area; (4)
Objective weight of factors in hazard assessment model ; (5) Zonation method of the
regional-scale landslide hazard degree; (6)The site-specific landslide hazard degree
assessment method; (7) Study on relation between the rainfall-induced landslides and
precipitation ; (8) Study on the prediction method of rainfall-induced landslide ; (9)
Summarization and prospect.
This paper consists of five main achievements as below:
(1) The regular pattern of distribution and mechanism of landslides in the study
area’re deeply Analyzed, temporal distribution is analyzed separately in interannual
scale, annual scale and day scale; statistics of spatial distribution is analyzed by the
influences of landslides and the environmental factors including lithology, stratum, terrain and slope shape and so on. Mechanism of landslides is dissertated by both
environmental factors and triggering factors.
(2) The model of regional scale landslide hazard zonation is established by the
landslide occurrence probability and information entropy to get objective weights of 6
bottom factors, which is applied in wanzhou county. The result is verified by 3
different classification methods and validity is proved for the consistence of different
classification methods.
(3) By combining the 8 factors of landslide influence and surface phenomena and
their information entropy weights, the site-specific landslide hazard assessment model
is established and applied in 4 typical landslides in Wanzhou County. The validity of
results is proved by the deep displacement monitoring data and the literatures.

(4) analyzing the relation between rainfall and landslide is carried out by
statistics of precipitation and landslides data in 2 decades, precipitation of 24 hours on
the day landslide occurring and precipitation 10 days before landslide occurring are
analyzed, and rain types of rainstorm and Continuous is also taking into account.
Then the expression of probability of rainfall-induced landslide is established after
calculation of 4 days rainfall related by SPSS with the Binary logistic method.
(5) Prediction model of rainfall-induced landslide is built by taking precipitation
and rainfall probability offered by Meteorological Department. The result of
prediction is classified into four grades which include green expressing with the first
grade, yellow with the second grade and orange red with the third grade, red with the
fourth grade. Prediction examples in study area is simulated by both regional scale
and site-specific scale by the model and prediction system platform is established by
software engineering and GIS development.

语种中文
学科主题灾害学
公开日期2010-10-13
分类号P64;TH1
内容类型学位论文
源URL[http://ir.imde.ac.cn/handle/131551/2149]  
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)
成都山地灾害与环境研究所_山地灾害与地表过程重点实验室
推荐引用方式
GB/T 7714
杨宗佶. 滑坡危险度评价与预警方法研究——以三峡库区重庆市万州区为例[D]. 成都. 中国科学院水利部成都山地灾害与环境研究所. 2009.
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