Ma. Perez-flores et al., Imaging low-frequency and dc electromagnetic fields using a simple linear approximation, GEOPHYSICS, 66(4), 2001, pp. 1067-1081
We consider that all types of electromagnetic measurements represent weight
ed averages of the subsurface electrical conductivity distribution, and tha
t to each type of measurement there corresponds a different weighting funct
ion. We use this concept for the quantitative interpretation of dc resistiv
ity, magnetometric resistivity, and low-frequency electric and magnetic mea
surements at low induction numbers. In all three cases the corresponding in
verse problems are nonlinear because the weighting functions depend on the
unknown conductivity distribution. We use linear approximations that adapt
to the data and do not require reference resistivity values. The problem is
formulated numerically as a solution of a system of linear equations. The
unknown conductivity values are obtained by minimizing an objective functio
n that includes the quadratic norm of the residuals as well as the spatial
derivatives of the unknowns. We also apply constraints through the use of q
uadratic programming. The final product is the flattest model that is compa
tible with the data under the assumption of the given weighting functions.
This approximate inversion or imaging technique produces reasonably good re
sults for low and moderate conductivity contrasts. We present the results o
f inverting jointly and individually different data sets using synthetic an
d field data.