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2. 5-D RESISTIVITY TOMOGRAPHY USINGBOUNDARY INTEGRAL EQUATIONS
作者姓名:Mao Xianjin  Bao Guangshu
作者单位:College of Resource,Environment and Civil Engineering,Central South University of Technology,Changsha 410083,China
摘    要:ResistivityTomography(RT)isakindofnewgeophysicsmethodandtechnique.UsingitonecangetmuchhigherresolutionofsubsurfacethanthatoftraditionalDCelectricalmethods.Sofar,themethodsofRTaremainlybasedonthefinite--elementmethodandalphacentersmethodll~3j.ItiswellknownthatRTisanon--linearinversionproblem.TheinversionmethodbasedonthefiniteelementmethodislineariziedonlyusingthelineartermofTaylorseries,soitisunavoidabletocalculateJacobimatrix.Thiscomputationnotonlycostsalotoftime,butalsotakesupmuchmemoryo…

收稿时间:19 May 1997

2.5-D Resistivity Tomography using boundary integral equations
Mao Xianjin, Bao Guangshu.2. 5-D RESISTIVITY TOMOGRAPHY USINGBOUNDARY INTEGRAL EQUATIONS[J].Journal of Central South University of Technology,1997,4(2):104-107.
Authors:Mao Xianjin  and Bao Guangshu
Affiliation:(1) College of Resource, Environment and Civil Engineering, Central South University of Technology, 410083 Changsha, China
Abstract:DC Resistivity Tomography is a non-linear inversion problem. So far there are mainly two kinds of inversion methods, based on the finite-element method and alpha centers method. In this paper, the disadvantages of these two kinds of methods were analysed,and a new method of forward modeling and inversion (Tomography) based on boundary integral equations was proposed. This scheme successfuly overcomes the difficulties of the two formarly methods. It isn't necessary to use the linearization approximation and calculate the Jacobi matrix. Numerical modeling results given in this paper showed that the computation speed of our method is fast, and there is not any special requirement for initial model, and satisfying results of tomography can be obtained in the case of great contrast of conductivity. So it has wide applications.
Keywords:2  5-D problem  boundary integral equations  resistivity tomography
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