Analysis of 2D homogeneous space solutions of the seismoelectric P-SV-TM mode for interferometric purposes

Seismic and electromagnetic imaging methods both provide the geophysicist with different types of medium parameters. Seismic methods are sensitive to the elastic properties of the medium, while electromagnetic methods are sensitive to the electric properties. In porous-saturated media, these two wave fields occur as a coupled system, which is known as 'seismoelectrics'. This coupling is caused by physical interactions at the grain surface boundary and is a function of several medium parameters, such as dynamic permeability. This medium parameter is valuable to the oil and gas industry, as well to the field of hydrology. By conducting a seismoelectric survey it would theoretically be possible to provide an extra control on this medium parameter. However, both practice and theory have shown that this coupling mechanism also results in a low signal-to-noise ratio. A possible solution to this problem would be to apply interferometric Green's retrieval, which is a technique based on stacking of cross-correlated data. This approach has been proved successful for the SH-TE mode in 1D. The SH-TE mode forms together with the P-SV-TM mode, the total seismoelectric system. In this thesis the first steps are taken towards the proof that this technique could also work for the P-SV-TM mode of the system. This is supported by a modelling experiment of 2D homogeneous space solutions of the seismoelectric P-SV-TM mode for different configurations. This analysis turned out that the unwanted artefacts observed in the interferometric retrieval are generated by cross-correlations between P-waves and SV-waves.

Subject

seismoelectrics
interferometry
cross-correlation

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Student theses

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master thesis

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IHartstra_MscThesis_final.pdf

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