An Integral Equation and its Solution for some Two‐and Three‐Dimensional Problems in Resistivity and Induced Polarization

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Abstract

Summary. The potential, U, about a point electrode, at the surface of a layered ground in which there is an heterogeneity embedded, satisfies the integral equation: (Formula Presented.) Here, U* and σ* are the corresponding quantities for the potential and conductivity without the heterogeneity. The integral is taken over the surface of the heterogeneity, ∂U/∂n is the normal derivative (in the direction of the outward normal) of U, and G is a Green's function. Solutions to this equation can readily be found by using the Galerkin method of solving integral equations. The solutions of this equation when the heterogeneity is a sphere or a cylinder in a uniform ground or beneath a conductive overburden are the most readily found. When the solution of the integral has been found for the potential it is a simple matter to calculate the apparent resistivity or chargeability for any electrode configuration. Copyright © 1975, Wiley Blackwell. All rights reserved

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Lee, T. (1975). An Integral Equation and its Solution for some Two‐and Three‐Dimensional Problems in Resistivity and Induced Polarization. Geophysical Journal of the Royal Astronomical Society, 42(1), 81–95. https://doi.org/10.1111/j.1365-246X.1975.tb05851.x

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