2022
DOI: 10.1016/j.compgeo.2021.104522
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On propagation characteristics of Rayleigh wave in saturated porous media based on the strain gradient nonlocal Biot theory

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Cited by 9 publications
(2 citation statements)
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“…This theory considers the dynamic coupling effect and dissipation mechanism between the fluid and solid phases in the porous media (Biot, 1954). Later, Berryman (1980) verified the theory of Biot by comparing the measured elastic wave velocity in porous structures with the prediction of Biot theory (Johnson, 1980;Berryman, 1999;Ding et al, 2022). According to the measured P-wave velocity and the porosity of saturated sediments, Lee (2002) calculated the Biot coefficient suitable for S-wave velocity.…”
Section: Introductionmentioning
confidence: 90%
“…This theory considers the dynamic coupling effect and dissipation mechanism between the fluid and solid phases in the porous media (Biot, 1954). Later, Berryman (1980) verified the theory of Biot by comparing the measured elastic wave velocity in porous structures with the prediction of Biot theory (Johnson, 1980;Berryman, 1999;Ding et al, 2022). According to the measured P-wave velocity and the porosity of saturated sediments, Lee (2002) calculated the Biot coefficient suitable for S-wave velocity.…”
Section: Introductionmentioning
confidence: 90%
“…These theories fall roughly into two categories: highorder gradient theories [2][3][4][5][6] and Eringen's nonlocal theories [7]. Based on these theories, the problems of one-dimensional consolidation of a porous layer [3,8] and wave propagation in porous media [9][10][11] have been examined. Besides, the high-order theories have been also applied to the study of the response of bone tissues (e.g., Giorgio et al [5]).…”
Section: Introductionmentioning
confidence: 99%