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An energy-based approach to estimate seismic attenuation due to wave-induced fluid flow in heterogeneous poroelastic media
(Wiley Blackwell Publishing, Inc, 2016-11)
Wave-induced fluid flow (WIFF) due to the presence of mesoscopic heterogeneities is considered as one of the main seismic attenuation mechanisms in the shallower parts of the Earth's crust. For this reason, several models ...
Modeling Forced Imbibition Processes and the Associated Seismic Attenuation in Heterogeneous Porous Rocks
(Blackwell Publishing, 2017-11)
Quantifying seismic attenuation during laboratory imbibition experiments can provide useful information toward the use of seismic waves for monitoring injection and extraction of fluids in the Earth's crust. However, a ...