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Non-Self-Conjugate Model Formulation of the Pekeris Boundary Problem

机译:Pekeris边界问题的非自共轭模型表示

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摘要

The theory of wave processes in layered media developed in classical works [1-3] is based on the solution of the key boundary problem of hydroacous-tic science formulated and solved by Pekeris in [1] for the system: homogeneous fluid layer-homogeneous fluid half-space. A characteristic peculiarity of the model formulation suggested in [1-3] is the fact that boundary conditions at the interface waveguide-half-space are formulated as identical conditions of continuity by pressure and normal components of the oscillation velocity with respect to the horizontal coordinate (local conditions of (p, v_z) continuity), while the model formulation appears self-conjugate.
机译:经典著作[1-3]中发展的层状介质中波过程理论是基于Pekeris在[1]中提出并解决的系统的水声科学关键边界问题的解决方案:均质流体层-均质流体半空间。在[1-3]中提出的模型公式的一个特点是,在界面波导半空间处的边界条件由压力和相对于水平坐标的振荡速度的法线分量公式化为相同的连续性条件。 ((p,v_z)连续性的局部条件),而模型公式显示为自共轭的。

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  • 来源
    《Doklady Earth Sciences》 |2010年第2期|p.1342-1345|共4页
  • 作者

    B.A.Kasatkin; N.V.Zlobina;

  • 作者单位

    Institute of Problems of Marine Technology, Far East Division, Russian Academy of Sciences, ul. Sukhanova 5a, Vladivostok, 690950 Russia;

    rnInstitute of Problems of Marine Technology, Far East Division, Russian Academy of Sciences, ul. Sukhanova 5a, Vladivostok, 690950 Russia;

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