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考虑渗流和地震时的砂土边坡稳定性计算
引用本文:卢玉林,薄景山,陈晓冉,王丽.考虑渗流和地震时的砂土边坡稳定性计算[J].重庆大学学报(自然科学版),2017,40(1):65-75.
作者姓名:卢玉林  薄景山  陈晓冉  王丽
作者单位:1. 防灾科技学院 防灾工程系,北京 101601; 中国地震局工程力学研究所,哈尔滨 150080;2. 中国兵器工业北方勘察设计研究院有限公司,石家庄,050011;3. 中国地震局工程力学研究所,哈尔滨,150080
基金项目:河北省教育厅高等学校科学技术研究项目(ZC2016150);中国地震局教师科研基金(20120103);中央高校基本科研业务费专项资金(ZY20150203)。
摘    要:基于极限平衡理论,以砂土边坡为研究对象,推导了渗流和地震存在时拟静力法和拟动力法边坡安全系数的计算表达式。通过程序求解,与已有算例对比表明,计算结果基本一致,验证了2种方法解析式的合理性。参数分析表明,水位越高,边坡失稳越严重,水力梯度与安全系数基本为线性关系。渗流方向向下时,稳定性随水力梯度的增加而增大;渗流方向向上时,变化规律相反。水平地震加速度系数对稳定性的影响剧烈,竖向地震加速度系数对稳定性影响较小,简化计算可以忽略不计。最终得出拟静力法的解析式,简单、实用,而拟动力法则可以更为全面地考察砂土边坡稳定性随时间变化的特点。

关 键 词:砂土边坡  渗流  拟静力法  拟动力法  稳定性计算
收稿时间:2016/9/2 0:00:00

Calculation of sand slope stability with considering seepage and earthquake
LU Yulin,BO Jingshan,CHEN Xiaoran and WANG Li.Calculation of sand slope stability with considering seepage and earthquake[J].Journal of Chongqing University(Natural Science Edition),2017,40(1):65-75.
Authors:LU Yulin  BO Jingshan  CHEN Xiaoran and WANG Li
Institution:Department of Disaster Prevention Engineering, Institute of Disaster Prevention, Beijing 101601, P. R. China;Institute of Engineering Mechanics, China Earthquake Administration, Harbin 150080, P. R. China,Department of Disaster Prevention Engineering, Institute of Disaster Prevention, Beijing 101601, P. R. China;Institute of Engineering Mechanics, China Earthquake Administration, Harbin 150080, P. R. China,China North Industries Norengeo Ltd., Shijiazhuang 050011, P. R. China and Institute of Engineering Mechanics, China Earthquake Administration, Harbin 150080, P. R. China
Abstract:On the basis of the limit equilibrium theory, we took a sand slope as research object and deduced the expressions of the slope safety factor with quasi-static method and pseudo-dynamic method when steady seepage and earthquake were present. The results of computer programs agree well with those of exiting methods, which verifies the validity of the two analytic methods. Parameter analysis shows that there is a linear relationship between hydraulic gradient and safety factor, and the higher the water level, the easier the slope is to lose stability. When the seepage direction is downward, the slope stability increases with the increase of hydraulic gradient, and when the seepage direction is upward, the change rule is opposite. The slope stability increases significantly with the increase of horizontal seismic acceleration factor, and the effect of vertical seismic acceleration factor on the slope stability is relatively small, which can be ignored in simplified calculation. Generally, the analytic formula of pseudo-static method is simple and practical, and the formula of the pseudo-dynamic method can more comprehensively investigate the characteristics of the slope stability changing with time.
Keywords:sand slope  seepage  pseudo-static method  pseudo-dynamic method  stability calculation
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