Abstract

In this study, a semi-analytical solution to the dynamic responses of a multilayered transversely isotropic poroelastic seabed under combined wave and current loadings is proposed based on the dynamic stiffness matrix method. This solution is first analytically validated with a single-layered and a two-layered isotropic seabed and then verified against previous experimental results. After that, parametric studies are carried out to probe the effects of the soil’s anisotropic characteristics and the effects of ocean waves and currents on the dynamic responses and the maximum liquefaction depth. The results show that the dynamic responses of a transversely isotropic seabed are more sensitive to the ratio of the soil’s vertical Young’s modulus to horizontal Young’s modulus (Ev/Eh) and the ratio of the vertical shear modulus to Ev (Gv/Ev) than to the vertical-to-horizontal ratio of the permeability coefficient (Kv/Kh). A lower degree of quasi-saturation, higher porosity, a shorter wave period, and a following current all result in a greater maximum liquefaction depth. Moreover, it is revealed that the maximum liquefaction depth of a transversely isotropic seabed would be underestimated under the isotropic assumption. Furthermore, unlike the behavior of an isotropic seabed, the transversely isotropic seabed tends to liquefy when fully saturated in nonlinear waves. This result supplements and reinforces the conclusions determined in previous studies. This work affirms that it is necessary for offshore engineering to consider the transversely isotropic characteristics of the seabed for bottom-fixed and subsea offshore structures.

Highlights

  • With the rapid development of technologies, marine resources are being exploited on a large scale

  • As waves and/or currents propagate in seawater, a time-varying wave pressure will be generated on the surface of the seabed, increasing the excess pore water pressure and decreasing the effective stress of the soil skeleton

  • It is necessary to study the dynamic responses of the seabed under wave and/or current loading

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Summary

Introduction

With the rapid development of technologies, marine resources are being exploited on a large scale. Ye and Jeng [30] initiated the analysis of the dynamic responses of a single-layered isotropic poroelastic seabed under wave and current loadings in two dimensions based on the PD model and discussed the transient liquefaction depth of the seabed, respectively, under a following current and an opposing current. Their conclusions indicated that the current’s influence on the pore pressure should not be neglected, and the maximum liquefaction depth increases under the following current while decreasing under the opposing current. Maximum liquefaction depths of the single-layered TIP and the multilayered TIP seabed

Seawater-Seabed-Bedrock System
Governing Equations
Wave-Current Interaction
Boundary Conditions
General Solution to a TIP Layer
Dynamic Stiffness Matrix of TIP Multilayers
Verification of the Semi-Analytical Solution Based on Isotropic Layers
Comparisons
Semi-Analytical Solution Applied to TIP Layers and Parametric Study
Limits
Single-Layered
10. Maximum
12. Maximum
13. Vertical
14. Maximum
Effects of Permeability Coefficient
It has been explained by
Effects of Young’s Modulus
Pa v v all are relative to the typical value in
22. Distributions
Conclusions
Findings
Methods
Full Text
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