首页 | 本学科首页   官方微博 | 高级检索  
     检索      

三维地电断面激发极化法有限元数值模拟
引用本文:黄俊革,阮百尧,鲍光淑.三维地电断面激发极化法有限元数值模拟[J].地球科学,2003,28(3):323-326.
作者姓名:黄俊革  阮百尧  鲍光淑
作者单位:[1]中南大学信息物理学院,湖南长沙410083 [2]桂林工学院资源与环境工程系,广西桂林541004
基金项目:国家自然科学基金 (No .40 0 6 40 0 1),广西自然科学基金匹配项目,教育部优秀青年教师基金项目,广西培养新世纪学术和技术带头人专项基金 .
摘    要:用有限单元法求解三维地电断面激发极化法正演模拟算法.首先给出了三维构造中点源电场异常电位的边值问题与变分问题,简化无穷远边界上的边界条件以提高计算速度及计算精度.以此为基础计算视电阻率对模型电阻率的偏导数矩阵,并进行三维地电断面激发极化法正演模拟,与等效电阻率法相比节约了计算时间.对几例较典型的地电模型进行计算,结果表明本方法是正确可行的.

关 键 词:有限单元法  三维地电断面  激发极化法  正演  三维构造  电位  视电阻率  偏导数矩阵
文章编号:1000-2383(2003)03-0323-04

Finite Element Method for IP Modeling on 3-D Geoelectric Section
HUANG Jun-ge ,RUAN Bai-yao,BAO Guang-shu.Finite Element Method for IP Modeling on 3-D Geoelectric Section[J].Earth Science-Journal of China University of Geosciences,2003,28(3):323-326.
Authors:HUANG Jun-ge    RUAN Bai-yao  BAO Guang-shu
Institution:HUANG Jun-ge 1,2,RUAN Bai-yao2,BAO Guang-shu1
Abstract:FEM is used to modeling IP sounding on 3-D geoelectric section. First, this paper presents the 3-D boundary value and variation equation of point-source electrical field on a 3-D structure. Then, the boundary condition for the infinite boundary is simplified to improve calculation speed and precision. On this basis, the partial derivatives matrix for the ratio between the apparent resistivity and the model resistivity parameters is calculated, and at the same time, the IP on 3-D geoelectric section is positively simulated. Compared with equivalent resistivity method, this simulation saves much calculation time. The test of several relative typical geoelectric models shows that this modeling method is correct and feasible.
Keywords:D geoelectric section  IP  finite element method  partial derivatives
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号