In general, in the electromagnetic surveying, frequency dispersion of conductivity is neglected. In contrast, in the common excited polarization method, current is indirectly supplied to the underground, so the secondary voltage originated by ramp turn off in the current flow is actually frequency dispersion of conductivity. Hence, electromagnetic (EM) effect and induced polarization (IP) effect come into being at the same time, which leads to distortion, in other words, sign reversal of EM response. For this reason, many researchers deeply studied the mechanism of the sign reversal and the forward modeling in consideration of this phenomenon.
Many researchers simulated the distorted transient response by conductivity related to frequency. Most of the research results concluded that Cole-Cole model is well suited to considering IP effect observed in TDEM.
Transient response of polarizable whole space is surely different from both polarizable half space response and non-polarizable whole space response.
Jon Kwang Bok, a researcher at the Faculty of Earth Science and Engineering, has approximated the whole space electromagnetic transient field originated by rectangular loop in the whole layered space which includes polarizable layers by using the Cole-Cole model and linear digital filtering method.
As a result, he has drawn two conclusions.
First, induced voltage measured has no relationship with whether the polarizable conductive layers are above or below the measurement spot. Second, polarization must be considered in the whole space inversion as in half space because the response computed by common whole space modeling method is a lot different from that by polarizable whole space modeling method.
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