1887

Abstract

Understanding the seismoelectric interface response is important for the development of seismoelectric exploration methods. Comparisons between the theory and measurements are scarce. We present a full-waveform seismoelectric model based on the complete set of electrokinetic equations. The numerical predictions are compared with seismoelectric interface response measurements using an artifical porous sample and a natural rock. Good agreement is found in terms of travel time and polarity of the waveforms. The agreement is shown to hold for sample thicknesses smaller than the dominant wavelength.

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/content/papers/10.3997/2214-4609.20149491
2011-05-23
2024-04-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20149491
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