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论文摘要

基于BSTEM模型的二元结构河岸崩塌过程模拟

Modeling of the Composite Bank Failure Process Using BSTEM

作者:宗全利(武汉大学 水资源与水电工程科学国家重点实验室;石河子大学 水利建筑工程学院);夏军强(武汉大学 水资源与水电工程科学国家重点实验室);邓春艳(武汉大学 水资源与水电工程科学国家重点实验室);许全喜(长江水利委员会 水文局)

Author:Zong Quanli(State Key Lab. of Water Resources and Hydropower Eng. Sci.,Wuhan Univ.;College of Water Conservancy and Architectural Eng.,Shihezi Univ.);Xia Junqiang(State Key Lab. of Water Resources and Hydropower Eng. Sci.,Wuhan Univ.);Deng Chunyan(State Key Lab. of Water Resources and Hydropower Eng. Sci.,Wuhan Univ.);Xu Quanxi(Bureau of Hydrology,Changjiang Water Resources Commission)

收稿日期:2012-11-11          年卷(期)页码:2013,45(3):69-78

期刊名称:工程科学与技术

Journal Name:Advanced Engineering Sciences

关键字:崩岸模拟;BSTEM模型;上荆江;坡脚冲刷;潜水位

Key words:modeling of bank failure;BSTEM;Upper Jingjiang Reach;toe erosion;water table

基金项目:国家自然科学基金资助项目(51079103);国家“973”重点基础研究发展规划资助项目(2012CB417001)

中文摘要

针对上荆江典型二元结构河岸的崩塌问题,综合考虑近岸水流冲刷作用与河岸土体组成及力学特性,采用BSTEM模型分析了上荆江不同时期的岸坡稳定性,并对二元结构河岸的崩塌过程进行了模拟。结果表明:枯水期和汛前涨水期河岸稳定性较高,为崩岸较弱阶段;洪水期和落水期河岸稳定性较低,并伴随持续崩塌,属崩岸强烈阶段。此外分析还表明坡脚冲刷和潜水位变化对河岸稳定性有重要影响,两者分别是引起洪水期和落水期崩岸强度较大的重要原因。最后在综合考虑坡脚冲刷、潜水位变化和崩塌后土体在坡脚堆积等因素基础上,模拟了2009—2010年荆34断面右侧河岸的崩塌过程,河岸崩塌总宽度与崩塌后岸坡形态等模拟结果与实测结果符合较好。因此在模拟上荆江二元结构河岸崩塌过程时,必须同时考虑坡脚冲刷、潜水位变化和坡脚堆积等因素的影响。

英文摘要

Considering the near-bank fluvial erosion,the soil composition and mechanical properties,the degrees of riverbank stability for composite bank in the Upper Jingjiang Reach (UJR) were analyzed during different water level periods using BSTEM,and the process of bank failure was simulated.The results indicated that the degrees of riverbank stability are high during the periods of low water level and water-level rising before the flood season,which leads to the stage of weak bank failure,and they are low during the periods of high water level and water-level recession with the continuous bank collapse occurring,which belongs to the stage of intensive bank failure.In addition,the effects of bank toe erosion and water table variation on the degree of bank stability were investigated.This analysis indicated that these two factors have an important influence on the process of bank failure,and they can cause respectively intensive bank failure during the high water and recession periods.Finally,with the bank toe erosion,water table variation and deposition form of the collapsed bank soil being considered in the calculation,the process of bank failure of the right riverbank at Jing34 section was simulated over the period from Nov.2008 to Oct.2010.The model-predicted results were in well agreement with the measured data of the total bank retreat width and the collapsed bank shape.Therefore,these influencing factors should be included when simulating the process of composite riverbank failure.

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