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首页> 外文期刊>Ocean Engineering >An integrated three-dimensional model of wave-induced pore pressure and effective stresses in a porous seabed: Ⅱ. Breaking waves
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An integrated three-dimensional model of wave-induced pore pressure and effective stresses in a porous seabed: Ⅱ. Breaking waves

机译:多孔海底波浪引起的孔隙压力与有效应力的三维综合模型:Ⅱ。碎波

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The evaluation of the wave-induced liquefaction potential is particularly important for coastal engineers involved in the design of marine structures. Most previous investigations of the wave-induced liquefaction have been limited to two-dimensional non-breaking waves. In this paper, the integrated three-dimensional poro-elastic model for the wave-seabed interaction proposed by [Zhang, H., Jeng, D.-S., 2005. An integrated three-dimensional model of wave-induced pore pressure and effective stresses in a porous seabed: I. A sloping seabed. Ocean Engineering 32(5/6), 701-729.] is further extended to simulate the seabed liquefaction potential with breaking wave loading. Based on the parametric study, we conclude: (1) the liquefaction depth due to breaking waves is smaller than that of due to non-breaking waves; (2) the degree of saturation significantly affects the wave-induced liquefaction depth, and no liquefaction occurs in full saturated seabed, and (3) soil permeability does not only significantly affect the pore pressure, but also the shear stresses distribution.
机译:波浪引起的液化潜力的评估对于参与海洋结构设计的沿海工程师而言尤其重要。以前大多数关于波浪引起的液化的研究都局限于二维非破坏性波浪。本文中,[Zhang,H.,Jeng,D.-S.,2005]提出了波浪-海床相互作用的三维三维弹性模型。多孔海底的有效应力:I.倾斜的海底。海洋工程32(5/6),701-729。]进一步扩展为模拟具有破波载荷的海底液化潜力。在参数研究的基础上,我们得出以下结论:(1)破碎波引起的液化深度小于非破碎波引起的液化深度。 (2)饱和度显着影响波浪引起的液化深度,在完全饱和的海床中不发生液化;(3)渗透性不仅显着影响孔隙压力,而且还剪切应力分布。

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