Pseudo‐seismic wavelet transformation of transient electromagnetic response in engineering geology exploration

This paper presents some new theoretical analysis and numerical simulations of that transient electromagnetic diffusion‐field response is transformed into a pseudo‐seismic wavelet in engineering geology exploration. It can clearly reveal the electric interface under ground. To simplify the integral equation used in the transformation, the integral range is separated into seven windows, and each window is compiled into a group of integral coefficients. Then, the accuracy of the coefficients is tested, and the calculated coefficients are used to derive the pseudo‐seismic wavelet by optimization method. Finally, several geo‐electric models are designed, so that model responses are transformed into the pseudo‐seismic wavelet. The transformed imaginary wave shows that some reflection and refraction phenomena appear when the wave meets the electric interface. This result supports the introduction of the seismic interpretation in data processing of transient electromagnetic method.