New spectral Lanczos decomposition method for induction modeling in arbitrary 3-D geometry

Author:

Druskin Vladimir L.1,Knizhnerman L. A.2,Lee Ping1

Affiliation:

1. Schlumberger‐Doll Research, Old Quarry Road, Ridgefield, Connecticut 06877-4108. Emails:

2. Central Geophysical Expedition, Moscow, Russia

Abstract

Traditional resistivity tools are designed to function in vertical wells. In horizontal well environments, the interpretation of resistivity logs becomes much more difficult because of the nature of 3-D effects such as highly deviated bed boundaries and invasion. The ability to model these 3-D effects numerically can greatly facilitate the understanding of tool response in different formation geometries. Three‐dimensional modeling of induction tools requires solving Maxwell’s equations in a discrete setting, either finite element or finite difference. The solutions of resulting discretized equations are computationally expensive, typically on the order of 30 to 60 minutes per log point on a workstation. This is unacceptable if the 3-D modeling code is to be used in interpreting induction logs. In this paper we propose a new approach for solutions to Maxwell’s equations. The new method is based on the spectral Lanczos decomposition method (SLDM) with Krylov subspaces generated from the inverse powers of the Maxwell operator. This new approach significantly speeds up the convergence of standard SLDM for the solution of Maxwell’s equations while retaining the advantages of standard SLDM such as the ability of solving for multiple frequencies and eliminate completely spurious modes. The cost of evaluating powers of the matrix inverse of the stiffness operator is effectively equivalent to the cost of solving a scalar Poisson’s equation. This is achieved by a decomposition of the stiffness operator into the curl‐free and divergence‐free projections. The solution of the projections can be computed by discrete Fourier transforms (DFT) and preconditioned conjugate gradient iterations. The convergence rate of the new method improves as frequency decreases, which makes it more attractive for low‐frequency applications. We apply the new solution technique to model induction logging in geophysical prospecting applications, giving rise to two orders of magnitude convergence improvement over the standard Krylov subspace approach and more than an order of magnitude speed‐up in terms of overall execution time. This makes it feasible to routinely use 3-D modeling for model‐based interpretation, a breakthrough in induction logging and interpretation.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference10 articles.

1. Alumbaugh, D., and Newman, G., 1995, Time efficient 3-D electromagnetic modeling on massively parallel computers: Internal Symposium on Three‐Dimensional Electromagnetics, Schlumberger‐Doll Research, Proceedings, 205–218.

2. Anderson, B., Barber, T., Druskin, V., Dussan, E., Lee, P., Knizhnerman, L., and Davydycheva, S., 1996, The response of multi-array induction tools in highly dipping formations with invasion and in arbitrary 3D geometry: Ann. Conf., SPWLA.

3. Boyce, W., Lynch, D., Paulsen, K., and Minerbo, G., 1992, Nodal based finite element modeling of Maxwell’s equations: Inst. Electr. Electron. Eng. Trans. Antennas Propagat.40, no. 6, 642–651.

4. Spectral approach to solving three-dimensional Maxwell's diffusion equations in the time and frequency domains

5. Spectral approach to solving three-dimensional Maxwell's diffusion equations in the time and frequency domains

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