Ps. Routh et Dw. Oldenburg, Electromagnetic coupling in frequency-domain induced polarization data: a method for removal, GEOPHYS J I, 145(1), 2001, pp. 59-76
Electromagnetic (EM) coupling is generally considered to be noise in induce
d polarization (IP) data and interpretation is difficult when its contribut
ion is large compared to the IP signal. The effect is exacerbated by conduc
tive environments and large-array survey geometries designed to explore dee
per targets. In this paper we present a methodology to remove EM coupling f
rom frequency-domain TP data. We first investigate the effect of EM couplin
g on the IP data and derive the necessary equations to represent the IP eff
ect for both amplitude and phase responses of the signal. The separation of
the inductive response from the total response in the low-frequency regime
is derived using the electric field due to a horizontal electric dipole an
d it is assumed that at low frequencies the interaction of EM effects and I
P effects is negligible. The total electric field is then expressed as a pr
oduct of a scalar function, which is due to IP effects, and an electric fie
ld, which depends on the EM coupling response. It is this representation th
at enables us to obtain the IP response from EM-coupling-contaminated data.
To compute the EM coupling response we recognize that conductivity informa
tion is necessary. We illustrate this with a synthetic example. The removal
method developed in this work for the phase and the pur cent frequency eff
ect (PFE) data are applicable to 1-D, 2-D and 3-D structures. The practical
utility of the method is illustrated on a 2-D field example that is typica
l of mineral exploration problems.