2015
DOI: 10.1016/j.oceaneng.2015.06.029
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Laboratory study for pore pressures in sandy deposit under wave loading

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Cited by 84 publications
(72 citation statements)
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“…This analytical solution has been widely used for the validation of the waveinduced oscillatory pore pressure in a porous seabed without a structure in the literature [4]. Recently, Liu and Jeng [27] con ducted a series of ID laboratory experiments (similar to Ref. [7]) for the wave-induced oscillatory pore pressure in marine sedi ments.…”
Section: Validations Of the Present Modelmentioning
confidence: 96%
“…This analytical solution has been widely used for the validation of the waveinduced oscillatory pore pressure in a porous seabed without a structure in the literature [4]. Recently, Liu and Jeng [27] con ducted a series of ID laboratory experiments (similar to Ref. [7]) for the wave-induced oscillatory pore pressure in marine sedi ments.…”
Section: Validations Of the Present Modelmentioning
confidence: 96%
“…3. The comparison of vertical distribution of maximum wave-induced oscillatory pore pressure versus relative soil depth with the 1-D experimental results (symbols, [46]) and the analytical solution (dashed lines, [6]). t) into the mass conservation equation [42] is used in the present study.…”
Section: Boundary Conditionsmentioning
confidence: 99%
“…The numerical results of the maximum vertical oscillatory pore pressure (|p|/p 0 , p 0 is the amplitude of dynamic wave pressures at the seabed surface) versus relative soil depth (z/h) are compared with analytical solutions [6] and laboratory experiments [46]. Based on the poro-elastic theory developed by Biot [10], Hsu and Jeng [6] developed an analytical solution for an unsaturated, anisotropic soil of finite thickness.…”
Section: Verificationsmentioning
confidence: 99%
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