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A semi-analytical solution for random wave-induced soil response and seabed liquefaction in marine sediments

机译:海洋沉积物中随机波浪引起的土壤响应和海床液化的半解析解

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摘要

In this study, unlike most previous investigations for wave-induced soil response, a simple semi-analytical model for the random wave-induced soil response is established for an unsaturated seabed of finite thickness. Two different wave spectra, the B-M and JONSWAP spectra, are considered in the new model. The influence of random wave loading on the soil response is investigated by comparing with the corresponding representative regular wave results through a parametric study, which includes the effect of the degree of saturation, soil permeability, wave height, wave period and seabed thickness. The maximum liquefaction depth under the random waves is also examined. The difference on the soil response under the two random wave types, B-M and JONSWAP frequency spectra, is also discussed in the present work.
机译:在这项研究中,与以往大多数对波浪引起的土体响应的研究不同,对于有限厚度的非饱和海床,建立了随机波浪引起的土体响应的简单半分析模型。新模型中考虑了两个不同的波谱,即B-M和JONSWAP谱。通过参数研究与相应的代表性规则波结果进行比较,研究了随机波载荷对土壤响应的影响,其中包括饱和度,土壤渗透率,波高,波周期和海床厚度的影响。还检查了随机波作用下的最大液化深度。本文还讨论了两种随机波类型B-M和JONSWAP频谱对土壤响应的差异。

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