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THE TIME‐DOMAIN ELECTROMAGNETIC RESPONSE OF POLARIZABLE BODIES: AN APPROXIMATE CONVOLUTION ALGORITHM 1
Author(s) -
SMITH R. S.,
WALKER P. W.,
POLZER B. D.,
WEST G. F.
Publication year - 1988
Publication title -
geophysical prospecting
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.735
H-Index - 79
eISSN - 1365-2478
pISSN - 0016-8025
DOI - 10.1111/j.1365-2478.1988.tb02192.x
Subject(s) - polarizability , impulse response , time domain , transient response , laplace transform , frequency domain , frequency response , convolution (computer science) , step response , fourier transform , polarization (electrochemistry) , physics , mathematical analysis , response time , optics , mathematics , computer science , chemistry , quantum mechanics , computer graphics (images) , control engineering , machine learning , molecule , artificial neural network , electrical engineering , computer vision , engineering
It is now believed that the negative transients observed in coincident‐loop transient electromagnetic (TEM) measurements are caused by polarizable bodies (bodies whose conductivity increases as a function of frequency). Ordinarily the TEM response of polarizable bodies is obtained by calculating the frequency‐domain response at many frequencies and transforming it to the time domain via Fourier, Laplace or Hankel transforms. This is normally a computationally laborious task. However, for some simple non‐polarizable bodies the time‐domain response is analytical and can be computed easily. When these simple bodies are weakly polarizable an approximate response can be obtained by convolving the easily‐calculated, non‐polarizable response with the impulse response of the polarization. The approximate response is found to be very similar to the exact response for the polarizabilities normally seen in geological materials.