A BOUNDARY-ELEMENT METHOD FOR 2-D DC RESISTIVITY MODELING WITH A POINT CURRENT SOURCE

Authors
Citation
Sz. Xu et al., A BOUNDARY-ELEMENT METHOD FOR 2-D DC RESISTIVITY MODELING WITH A POINT CURRENT SOURCE, Geophysics, 63(2), 1998, pp. 399-404
Citations number
17
Categorie Soggetti
Geochemitry & Geophysics
Journal title
ISSN journal
00168033
Volume
63
Issue
2
Year of publication
1998
Pages
399 - 404
Database
ISI
SICI code
0016-8033(1998)63:2<399:ABMF2D>2.0.ZU;2-W
Abstract
A new boundary element method (BEM) is presented for 2-D de resistivit y modeling with a point source. When compared with previously publishe d techniques, the new method has two main features: (1) The normal der ivative of potential has been eliminated from the integral equation. T he formulation of the present method is simpler and requires less memo ry and time than the previous published methods. (2) Multiple subsurfa ce inhomogeneous bodies can be modeled. For a simple testing model, th e maximum relative error of reciprocity test is 0.24% and the average relative error is 0.05%. For the same model, the maximum relative diff erence between the BEM solution and the finite-element method solution is 1.14% and the average relative difference is 0.73%. For a field ge oelectrical profile, the responses of the constructed model agree with the observed data quite well.