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- W2413856382 abstract "Dispersion and attenuation of elastic waves have been observed in crustal rocks. Existing theories and experimental measurements evidenced the existence of different energy-loss mechanisms. In rocks fully saturated by a Newtonian fluid, one major candidate is fluid flow at different scales, separating three regimes: the drained, undrained, and unrelaxed regimes. Here, two elastic transitions, between these three regimes, are investigated. Both the cause and the consequence of the drained/undrained transition are evidenced. Because the second transition measured occurs at higher frequency, where no global fluid flow occurs, it in turn is associated to the undrained/unrelaxed transition (or squirt flow). For both transitions, the amount of open microcracks seems to be the major contributor to the magnitudes of attenuation." @default.
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- W2413856382 date "2016-06-01" @default.
- W2413856382 modified "2023-09-24" @default.
- W2413856382 title "Dispersions and attenuations in a fully saturated sandstone: Experimental evidence for fluid flows at different scales" @default.
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- W2413856382 doi "https://doi.org/10.1190/tle35060495.1" @default.
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