The propagation of a solitary wave over seabed mud of the Voigt model

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在浅水里,海床泥能有效地浪费表面严肃波浪的体力。在这份报纸,海床泥导致的独居的波浪变细基于一个二分层的系统,水在被假定是 inviscid 被学习,泥层被 Voigt 模型描述。对在 Voigt 模型的泥上的独居的波浪合适的一套 Boussinesq 类型方程被建立,由联合不安分析和 Laplace 转变。堕落进牛顿的模型,的盒子我们的 Boussinesq 类型方程刘和禅宗(2007 ) 等价于那些,当显示泥影响的条款极大地被简化时。基于方程,独居的波浪的变细被学习。波浪振幅的一个进化方程被获得,泥速度
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