scholarly journals 3-D DC resistivity modeling and inversion using multi-resolution framework

2019 ◽  
Vol 2019 (1) ◽  
pp. 1-3
Author(s):  
Jingyu Gao ◽  
Maxim Smirnov ◽  
Maria Smirnova ◽  
Gary Egbert
Geophysics ◽  
2002 ◽  
Vol 67 (2) ◽  
pp. 610-617 ◽  
Author(s):  
Qinzhong Ma

The integral equation for dc resistivity modeling of 3‐D inhomogeneous bodies buried in a layered earth is derived by using Green's theorem. The main features of this method are (1) the layers above and below the 3‐D object can be included, (2) multiple subsurface inhomogeneous bodies can be embedded in the different layers, and (3) the boundary element method (BEM) is used to solve the integral equation using triangular surface elements. Linear variation of the electrical properties is assumed within each element. The potential on the ground surface is obtained by solving the linear equation system with Gaussian elimination. Model calculations demonstrate that the results obtained by this method compare well with the analytical solution of a sphere in a uniform half‐space and the asymptotic behavior for the solution of a buried body beneath a surficial layer as the layer resistivity approaches that of the half‐space. A comparison of responses over elongate 3‐D bodies with responses over 2‐D bodies of identical cross‐section also shows satisfactory agreement.


Geophysics ◽  
1996 ◽  
Vol 61 (5) ◽  
pp. 1301-1307 ◽  
Author(s):  
Shengkai Zhao ◽  
Matthew J. Yedlin

Two basic refinements of the finite‐difference method for 3-D dc resistivity modeling are presented. The first is a more accurate formula for the source singularity removal. The second is the analytic computation of the source terms that arise from the decomposition of the potential into the primary potential because of the source current and the secondary potential caused by changes in the electrical conductivity. Three examples are presented: a simple two‐layered model, a vertical contact, and a buried sphere. Both accurate and approximate Dirichlet boundary conditions are used to compute the secondary potential. Numerical results show that for all three models, the average percentage error of the apparent resistivity obtained by the modified finite‐difference method with accurate boundary conditions is less than 0.5%. For the vertical contact and the buried sphere models, the error caused by the approximate boundary condition is less than 0.01%.


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