分层流体中运动源生成的内波研究进展

针对两类密度分布模型------连续分层流体和间断分层流体, 综述了在运动潜体生成的Kelvin型和非Kelvin型内尾迹研究方面的现状, 内容侧重于运动源生成内波的解析理论和分层拖曳水槽中内尾迹实验方面的研究成果. 介绍了在连续分层流体中运动源生成的Kelvin型非线性内波的一般方程和在间断分层流体中Kelvin型内波的势流分析的一般方法; 概述了运动源诱生的先锋内孤立子、代数孤立子和平孤立波3类特殊非线性内波的研究进展, 其中运动潜体生成的平孤立内波被作者实验证实是一类极限孤立波, 并首次建立了共轭流动模型予以描述; 综合分析了在密度线性分布流体中潜体运动生成内波的动力学过程多样性特征, 其中包括内尾迹近场和远场的时空结构、不稳定结构、涡旋与湍流耦合结构以及湍流与内波相互作用结构等.      

分层流体中内波与半潜平台相互作用的模型试验

对密度分层流体中内波与半潜平台的相互作用问题进行了模型试验研究.采用摇板方法进行了内波造波试验,对内波波长、周期和波高进行了测量分析,获得了内波波高和波长与周期之间的相关关系.利用激光和倾角仪方法对半潜平台的纵荡和纵摇运动响应进行了测量分析,获得了平台纵荡运动及纵摇角幅值与内波周期之间的相关关系.结果表明,在半潜平台的设计与应用中,内波对其运动响应的影响是不可忽视的.特别地,发现了在内波周期的某个范围内,半潜平台的纵荡和纵摇都会出现倍频周期运动响应的现象.     

Experiments on the interaction of internal waves with the semi-submersible platform in a stratified fluid

对密度分层流体中内波与半潜平台的相互作用问题 进行了模型试验研究. 采用摇板方法进行了内波造波试验,对内波波长、周期和波高进行了 测量分析,获得了内波波高和波长与周期之间的相关关系. 利用激光和倾角仪方法对半潜平 台的纵荡和纵摇运动响应进行了测量分析,获得了平台纵荡运动及纵摇角幅值与内波周期之 间的相关关系. 结果表明,在半潜平台的设计与应用中,内波对其运动响应的影响是不可忽 视的. 特别地,发现了在内波周期的某个范围内, 半潜平台的纵荡和纵摇都会出现 倍频周期运动响应的现象.     

分层流中的瞬变波

本文用Laplace-Fourier变换方法研究两层流体中的瞬变波,分析了近似色散关系,讨论了不同模式波的主次关系,导出了由初始位移、大气扰动、水下爆炸,地震等因素所激励的表面波和内波的波形及其远场的渐近表达式。     

分层流体中混合流体团运动生成内波的研究现状

本文综述了分层流体中混合流体团运动生成内波的研究进展状况,系统地介绍了它的应用背景、实验和理论结果以及有待进一步研究的问题。      

考虑阻尼的无限长小垂度缆索弹性波的传播

缆索结构被广泛应用于电气、土木、海洋和航空工程等领域,随着缆索在工程中的应用长度越来越长,高阶振动越来越明显,研究时应该考虑扰动沿着缆索的传播.现有对缆索弹性波传播的研究中,通常不考虑阻尼项,然而阻尼对于波的传播有着重要影响.文章考虑阻尼的影响,发展了包含阻尼项的三维弹性缆索运动方程.通过求解上述含阻尼项的运动方程,分别考察了面内面外弹性波的频率关系、相速度和群速度等自由传播特性,进而通过计算无限长弹性缆索在初始余弦型脉冲作用下的位移响应,分析扰动沿着该缆索的传播规律,考察波的色散现象以及阻尼对于缆索弹性波传播的影响.结果表明,考虑阻尼后,面内波和面外波均为色散波,面内波在曲率的作用下,为高度色散波.此外,在阻尼的影响下,波的峰值在传播过程不断减小,且波的后缘端点响应总是高于前缘端点响应.     

连续分层流体中内波传播的李群分析法

对于密度连续分层海洋流体中的内波传播,从绝热Boussinesq近似方程组出发,得出了考虑变密度的非线性控制方程。应用李群分析方法,推导出了系统偏微分方程组的多组允许无穷小对称性、守恒矢量以及群不变解,对不变解的有关性质进行了说明,给出了系统精确解析解表达式。本文的李群分析解析解与已有文献中内波传播过程密度和垂向速度随时间变化的数值模拟计算结果基本一致,密度和垂向速度随时间呈正弦振荡,并且李群分析解析解也可推导出内波色散关系具有各向异性特征。     

分层流体中内孤立波数值造波方法及其应用

海洋内波是发生在密度分层海水中的波动，对潜艇航行的稳定性和悬停性都有重要影响。本文采用有限体积自适应半结构多重网格法求解Navier-Stokes方程，并用VOF(Volume of Fluid)方法追踪两层流体界面，应用双推板造波法进行内孤立波数值造波，对两层流体中的内孤立波数值造波方法进行研究和探讨。数值模拟结果证...     

具有内域的双层加筋圆柱壳动响应特性

采用外域双渐近法模拟外部流体域,内域双渐近法模拟内部流体域,采用非线性有限元软件ABAQUS 模拟结构,建立流固耦合数值模型并验证了其有效性. 利用建立的数值模型研究内部流体对双层加筋圆柱壳动响应的影响. 研究结果表明:一阶双渐近的解在中后期振荡周期变短、幅值变小,而二阶双渐近的解与解析解吻合良好;内部流体的存在减弱了双层加筋圆柱壳外壳的塑性变形,对其内壳塑性变形的影响较小;内部流体的存在减弱了双层加筋圆柱壳的速度响应.      

轴向应力波作用下圆柱壳塑性轴对称动力屈曲

运用有限元特征值分析方法对应力波作用下圆柱壳塑性轴对称动力失稳问题进行了研究。基于应力波理论和相邻平衡准则导出了圆柱壳轴对称动力失稳时的特征方程,在分析中同时考虑了应力波效应及横向惯性效应,把圆柱壳塑性动力失稳问题归结为特征值问题。通过引入圆柱壳动力失稳时的波前约束条件实现了此类问题的有限元特征值解法。计算结果揭示了圆柱壳塑性轴对称动力屈曲变形发展的机理,以及轴向应力波和屈曲变形的相互作用规律。     

Exact expressions for transient forced internal gravity waves and spatially-localized wave packets in a Boussinesq fluid

We re-examine a simple model describing the propagation of transient forced internal gravity waves in a Boussinesq fluid with constant horizontal mean velocity which was previously studied by Nadon and Campbell (Wave Motion, 2007). The waves are generated by a horizontally-periodic lower boundary condition and propagate upwards. We derive an alternative exact expression for the solution which more readily gives insight into the behaviour of the solution at high altitude. Some special cases of lower boundary conditions are considered to illustrate the features of the solution. This form of the solution allows us to use a Fourier transform to derive the solution for the more general situation where a wave packet is generated by a horizontally-localized lower boundary condition, comprising a continuous spectrum of horizontal wavenumbers or Fourier modes. This is a more realistic representation of internal gravity waves in the atmosphere and can be used as a starting point for investigating waves generated by an obstacle of finite horizontal extent such as an isolated mountain or a mountain range.     

Internal Waves Excited by a Moving Source in a Medium of Variable Buoyancy

The problem of the far field of internal gravity waves generated by an oscillating point perturbation source moving in a vertically infinite layer of a stratified medium of variable buoyancy is considered. The analytical solution of the problem is obtained by two ways for a model quadratic buoyancy frequency distribution. In the first case the solution is expressed in terms of the eigenfunctions of the vertical spectral problem and the Hermite polynomials. In the second case the solution in the form of the Green’s characteristic function is represented in terms of the functions of parabolic cylinder. The analytical solutions obtained make it possible to describe the amplitudephase characteristics of the far fields of internal gravity waves in a stratified medium with variable Brunt-Väisäläfrequency.     

An Exact Solution for Nonlinear Internal Equatorial Waves in the f-Plane Approximation

We present an exact solution of the nonlinear governing equations for internal geophysical water waves propagating westward in the f-plane approximation near the equator. We show that the mass transport velocity induced by this internal equatorial wave is eastward.     

On Time Reversible Description of the Process of Coagulation and Fragmentation

The process of coagulation is associated with scalar conservation laws, where the adhesion particle dynamics results from shock waves. Conversely, the fragmentation of a massive particle into a number of smaller ones, or into a continuous (dust) distribution, is associated with rarefaction waves. It is generally agreed that a reversible solution of a conservation law can include neither shock waves nor the spontaneous emergence of rarefaction waves. The present paper is an attempt to demonstrate that both coagulation and fragmentation may coexist for a reversible solution, under a natural generalization of the system of conservation law. This is done by introducing an action principle which includes, in addition to the inertial (kinetic energy) term, also an appropriately defined internal energy. The above generalization of the system of conservation law appears as the Euler–Lagrange equations for this action.     

Internal waves generated in an exponentially stratified fluid by an arbitrarily moving source

A theoretical investigation is made into the development of linear internal waves in an exponentially stratified flow of an ideal incompressible fluid in the Boussinesq approximation. The waves are generated by an arbitrarily moving point mass source. The obtained solution is used to investigate three special cases of motion: uniform motion at an angle to the horizontal, nonstationary motion during a finite interval of time, and uniform motion in a circular path. The method of solution of this problem is similar to that used by Wolfe and Lewis [1], who studied the generation of acoustic waves.Translated from Izvestiya Akademii Nauk SSSR, Mekhanika Zhidkosti i Gaza, No. 3, pp. 67–74, May–June, 1980.I thank V. V. Sazonov for assistance in the calculations.     

Rotationally symmetric internal gravity waves

Many mathematical models formulated in terms of non-linear differential equations can successfully be treated and solved by Lie group methods. Lie group analysis is especially valuable in investigating non-linear differential equations, for its algorithms act here as reliably as for linear cases. The aim of this article is to provide the group theoretical modeling of internal waves in the ocean. The approach is based on a new concept of conservation laws that is utilized to systematically derive the conservation laws of non-linear equations describing propagation of internal waves in the ocean. It was shown in our previous publication that uni-directional internal wave beams can be obtained as invariant solutions of non-linear equations of motion. The main goal of the present publication is to thoroughly analyze another physically significant exact solution, namely the rotationally symmetric solution and the energy carried by this solution. It is shown that the rotationally symmetric solution and its energy are presented by means of a bounded oscillating function.     

Behaviour of the acceleration and shock waves in materials with internal state variables

The explicit expressions for the change in the amplitudes of one-dimensional acceleration and shock waves propagating through arbitrary homogeneous materials described by the strain and internal state variables/parameters/are derived. The existence of a critical amplitude β for the acceleration wave and a critical strain gradient λ for the shock wave is established. For an infinitesimal shock wave the general form of the solution of the governing differential equation is furnished. The differential equations for the amplitudes of these two kind of waves are applied to an elastic-viscoplastic material.     

External shock loading on a submerged fluid-filled cylindrical shell

The interaction between a submerged fluid-filled elastic circular cylindrical shell and an external shock wave is considered. The study focuses on the internal acoustic field. A linear formulation of the problem is considered. A semi-analytical solution is obtained and used to simulate the interaction. A variety of phenomena are observed in the internal fluid, including the reflection and focusing of the internal acoustic wave as well as the radiation into the fluid of elastic waves propagating in the shell. Throughout the paper, the results of numerical simulations are compared with available experimental data, and a good agreement is observed. The solution developed appears to be suitable for use as a benchmark. Engineering relevance of the phenomena observed is discussed.     

The solitary waves in stratified shear flow

In this paper, the basic equation of internal long waves in stratified shear flow is derived under Boussinesq assumption, the first order approximation solution is given for solitary waves with the effects of slowly varying topograph at the sea bottom, weak stratification and basic shear flow. The Project Supported by the National Natural Science Foundation of China.     

Finite-amplitude solitary waves in a two-layer fluid

Second-mode nonlinear internal waves at a thin interface between homogeneous layers of immiscible fluids of different densities have been studied theoretically and experimentally. A mathematical model is proposed to describe the generation, interaction, and decay of solitary internal waves which arise during intrusion of a fluid with intermediate density into the interlayer. An exact solution which specifies the shape of solitary waves symmetric about the unperturbed interface is constructed, and the limiting transition for finite-amplitude waves at the interlayer thickness vanishing is substantiated. The fine structure of the flow in the vicinity of a solitary wave and its effect on horizontal mass transfer during propagation of short intrusions have been studied experimentally. It is shown that, with friction at the interfaces taken into account, the mathematical model adequately describes the variation in the phase and amplitude characteristics of solitary waves during their propagation.