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
CITATION STYLE
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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