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广义Bayes法在裂隙岩体渗透系数随机反演中的应用
引用本文:郑桂兰,王媛,王飞. 广义Bayes法在裂隙岩体渗透系数随机反演中的应用[J]. 水利学报, 2008, 39(4): 419-425
作者姓名:郑桂兰  王媛  王飞
作者单位:1. 河海大学,交通学院,南京,210098
2. 河海大学,土木学院,南京,210098
基金项目:国家自然科学基金 , 科技部科技支撑计划 , 高等学校博士学科点专项科研项目
摘    要:工程中由于存在各种随机因素,采用确定性的渗流分析方法进行渗透系数的反演必然会导致结果的不确定性.本文基于渗流场的随机有限元分析方法,结合变尺度优化算法和广义Bayes法,建立了一种渗透系数的随机反演方法,推导了详细的计算公式.该方法不仅考虑量测水头、渗透系数的随机性,还考虑了边界水头的随机性,不仅可以获得渗透系数的均值反演结果,还可以得到标准差的反演结果.最后将该法应用于重力坝坝基渗流算例分析中,以渗流有限元正分析计算结果作为"假想"的实测点水头值,通过随机反演,同时获得渗透系数均值与标准差的反演结果,将输入信息与反演结果对比分析,验证了渗透系数和标准差反演结果的正确性.

关 键 词:渗透系数  随机反演  广义Bayes法  变尺度法  Bayesian method  裂隙  岩体渗透系数  随机反演方法  应用  permeability coefficient  rock  stochastic analysis  generalized  验证  结果对比分析  输入信息  水头值  实测点  分析计算结果  渗流有限元  算例分析  坝基  重力坝  标准差
文章编号:0559-9350(2008)04-0419-07
修稿时间:2007-05-29

Application of generalized Bayesian method to stochastic analysis of fissured rock permeability coefficient
ZHENG Gui lan. Application of generalized Bayesian method to stochastic analysis of fissured rock permeability coefficient[J]. Journal of Hydraulic Engineering, 2008, 39(4): 419-425
Authors:ZHENG Gui lan
Affiliation:Hohai University, Nanjing 210098, China
Abstract:The random factors in engineering practice, such as randomness of water head on boundary, error of monitored water head and other random factors always result in the uncertainty of permeability obtained from reverse analysis using deterministic seepage analysis method. In this paper, a method for stochastic inverse analysis of permeability coefficient based on the stochastic finite element analysis method and applying variable metric algorithm and generalized Bayesian method is developed. By using this method not only the randomness of the monitored water head and permeability but also the randomness of boundary water head can be considered. The inversion results include the mean permeability coefficient and standard deviation of permeability coefficient. The validity of the proposed method is verified by the seepage analysis result of a gravity dam foundation. The results obtained from stochastic finite element analysis of seepage field are regarded as the assumed measured water head. The mean permeability coefficient and standard deviation are obtained from inverse analysis according to this assumed water head. The inversion results are in good agreement with the input data.
Keywords:permeability   stochastic inverse analysis   generalized Bayesian method   variable metric algorithm
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