3-D resistivity inversion using the finite-element method

With the increased availability of faster computers, it is now practical to employ numerical modeling techniques to invert resistivity data for 3-D structure. Full and approximate 3-D inversion methods using the finite-element solution for the forward problem have been developed. Both methods use reciprocity for efficient evaluations of the partial derivatives of apparent resistivity with respect to model resistivities. In the approximate method, the partial derivatives are approximated by those for a homogeneous half-space, and thus the computation time and memory requirement are further reduced. The methods are applied to synthetic data sets from 3-D models to illustrate their effectiveness. They give a good approximation of the actual 3-D structure after several iterations in practical situations where the effects of model inadequacy and topography exist. Comparisons of numerical examples show that the full inversion method gives a better resolution, particularly for the near-surface features, than does the approximate method. Since the full derivatives are more sensitive to local features of resistivity variations than are the approximate derivatives, the resolution of the full method may be further improved when the finite-element solutions are performed more accurately and more efficiently.

[1]  S. Treitel,et al.  A REVIEW OF LEAST-SQUARES INVERSION AND ITS APPLICATION TO GEOPHYSICAL PROBLEMS* , 1984 .

[2]  R. Parker,et al.  Occam's inversion; a practical algorithm for generating smooth models from electromagnetic sounding data , 1987 .

[3]  Gerald W. Hohmann,et al.  Topographic effects in resistivity and induced-polarization surveys , 1980 .

[4]  R. Jeffrey Lytle,et al.  Iterative Ray Tracing between Boreholes for Underground Image Reconstruction , 1980, IEEE Transactions on Geoscience and Remote Sensing.

[5]  Stanley H. Ward,et al.  Three-dimensional resistivity inversion using alpha centers , 1981 .

[6]  G. W. Hohmann,et al.  An investigation of finite-element modeling for electrical and electromagnetic data in three dimensions , 1981 .

[7]  Yutaka Sasaki,et al.  Two‐dimensional joint inversion of magnetotelluric and dipole‐dipole resistivity data , 1989 .

[8]  Douglas W. Oldenburg,et al.  Approximate inverse mappings in DC resistivity problems , 1992 .

[9]  G. L. Oppliger Three-dimensional terrain corrections for mise-a-la-masse and magnetometric resistivity surveys , 1984 .

[10]  Stephen K. Park,et al.  Inversion of pole-pole data for 3-D resistivity structure beneath arrays of electrodes , 1991 .

[11]  G. W. Hohmann,et al.  Two-dimensional resistivity inversion , 1984 .

[12]  David E. Boerner,et al.  Approximate Frechet derivatives in inductive electromagnetic soundings , 1990 .

[13]  O. Zienkiewicz The Finite Element Method In Engineering Science , 1971 .

[14]  Hiromasa Shima,et al.  2-D and 3-D resistivity image reconstruction using crosshole data , 1992 .