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论文摘要

沟道松散物质起动形成泥石流实验研究

Research on debris flow initiation due to bed failure after Wenchuan earthquake

作者:庄建琦(中国科学院成都山地灾害与环境研究所);崔鹏(中国科学院成都山地灾害与环境研究所);胡凯衡(中国科学院成都山地灾害与环境研究所);陈晓清(中国科学院成都山地灾害与环境研究所);葛永刚(中国科学院成都山地灾害与环境研究所)

Author:zhuangjianqi();();();();()

收稿日期:2010-04-14          年卷(期)页码:2010,42(5):230-236

期刊名称:工程科学与技术

Journal Name:Advanced Engineering Sciences

关键字:沟道松散物质起动;泥石流;起动模式;起动机理;汶川地震

Key words:debris flow due to channel failure; initiation model; initiation mechanism; Wenchuan earthquake

基金项目:国家973计划资助项目(2008CB425802); 中科院知识创新项目(KZCX2–YW–Q03–5)

中文摘要

为研究震后泥石流形成模式和机理,开展震后泥石流防治和预测,根据震后泥石流形成环境特点,设计泥石流起动装置,开展震后泥石流形成模式和机理试验。本研究共进行了25组试验,主要研究可泥石流在不同坡度情况下的泥石流形成模式和机理,主要认识:1、在坡度8°-12°情况下,泥石流的形成模式是冲蚀→冲沟→崩塌→堵塞→溃决→泥石流的模式;2、在坡度13°-17°情况下,泥石流的形成模式是逐渐侵蚀加剧(朔源侵蚀、下切侵蚀和侧蚀),容重逐渐增加形成泥石流的模式;3、在坡度18°-25°情况下,泥石流的形成模式是坡面流水→入渗→失稳→下滑→流态化的模式;4、根据孔隙水压力变化特征,不同的起动模式下的土体内部孔隙水压力变化特征不同,孔隙水压力的变化可以解释不同泥石流起动模式的机理特征。根据研究结果,可以对不同起动下的泥石流模式进行不同的防治规划,同时结合泥石流起动过程中孔隙水压力的变化,可以解释泥石流起动的模式,对开展震后泥石流预报提供了参考。

英文摘要

In order to understand the initiation model and mechanism and forecast and prevent the debris flow after earthquake, designing the facilities of debris flow initiation according to the environment post-earthquake to study the debris flow initiation mechanism. In this study, the 25 groups test were carried out at different slopes using the same soil material to study the debris flow initiation of debris flow at varies slopes, the results show that: 1. The initiation model of debris flow is erosion → gully → collapse → block → failure and transformed into debris flow between 8°-12° as initiation due to dam-failure; 2. The initiation model of debris flow is increased erosion gradually (down cutting erosion, back word cutting and lateral erosion) with the bulk density increasing and transformed into debris flow between 13°-17° as initiation due to erosion; 3. The initiation model of debris flow is surface flow → infiltration → failure → fluidization and transformed into debris flow between 18°-25° as initiation due to slope failure; 4. The change character of water pore-pressure is different at different slope experiments; the water pore-pressure inner soil reveals the initiation mechanism of debris flow at different slope. The prevention programmer could reference for the results of initiation model at different at varies slopes and carry out the different plan; the change characters of water pore-pressure revealed the initiation process of debris flow could be used forecast debris flow initiation for post-earthquake reconstruction projects.

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