Electromagnetic/Acoustic Coupling in Partially Saturated Porous Rocks: An Extension of Pride’s Theory
Author:
Funder
FONCYT
Publisher
Springer Science and Business Media LLC
Subject
General Chemical Engineering,Catalysis
Link
https://link.springer.com/content/pdf/10.1007/s11242-023-01983-9.pdf
Reference50 articles.
1. Albers, B.: Analysis of the propagation of sound waves in partially saturated soils by means of a macroscopic linear poroelastic model. Transp. Porous. Med. 80(B06209), 173–192 (2009). https://doi.org/10.1007/s11242-009-9360-y
2. Allègre, V., Lehmann, F., Ackerer, P., et al.: Modelling the streaming potential dependence on water content during drainage: 1. A 1D modelling of SP using finite element method. Geophys. J. Int. 189, 285–295 (2012). https://doi.org/10.1111/j.1365-246X.2012.05371.x
3. Allègre, V., Maineult, A., Lehmann, F., et al.: Self-potential response to drainage-imbibition cycles. Geophys. J. Int. 197(3), 1410–1424 (2014). https://doi.org/10.1093/gji/ggu055
4. Allégre, V., Jouniaux, L., Lehmann, F., et al.: Influence of water pressure dynamics and fluid flow on the streaming-potential response for unsaturated conditions. Geophys. Prospect. 63, 694–712 (2015). https://doi.org/10.1111/1365-2478.12206
5. Bear, J.: Dynamics of fluids in porous media. Dover Civil and Mechanical Engineering Series, Dover, (1988). https://books.google.com.ar/books?id=picSrNsgY8oC
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