两种流体力学中的“不确定性”原理

S. Gavrilyuk
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引用次数: 3

摘要

Hamilton原理是有限自由度力学中最基本的建模工具之一。它指出机械系统的可逆运动完全由相应的拉格朗日量决定,拉格朗日量是系统的动能和势能之差。控制方程是哈密尔顿作用的欧拉-拉格朗日方程。汉密尔顿原理可以自然地推广到单速度和多速度连续体力学(无限自由度系统)。特别是,多速度连续体的运动是用“牛顿定律”(欧拉-拉格朗日方程)的耦合系统来描述的。耗散项的引入与热力学第二定律和对势能行为(凸性)的自然限制相一致,使我们能够推导出物理上合理和数学上良好的控制方程。我将考虑一个最简单的双速流体的例子,其中一个相是不可压缩的(例如,含尘空气的流动,或不可压缩流体中可压缩气泡的流动)。一个非常令人惊讶的事实是人们可以从同一个拉格朗日量中得到不同的控制方程。不同类型的控制方程是由于自变量的选择和相应的虚运动。即使总动量和总能量方程是相同的,单个分量的方程也会因存在或不存在陀螺力(也称为“升力”)而彼此不同。这些力对控制方程的双曲性没有影响,但可以极大地改变密度和分量速度的分布。据我所知,这种多相流控制方程的不确定性在“多流体”界中从未被讨论过。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
‘Uncertainty’ principle in two fluid–mechanics
Hamilton’s principle (or principle of stationary action) is one of the basic modelling tools in finite-degree-of-freedom mechanics. It states that the reversible motion of mechanical systems is completely determined by the corresponding Lagrangian which is the difference between kinetic and potential energy of our system. The governing equations are the Euler-Lagrange equations for Hamil- ton’s action. Hamilton’s principle can be naturally extended to both one-velocity and multi-velocity continuum mechanics (infinite-degree-of-freedom systems). In particular, the motion of multi–velocity continuum is described by a coupled system of ‘Newton’s laws’ (Euler-Lagrange equations) for each component. The introduction of dissipative terms compatible with the second law of thermodynamics and a natural restriction on the behaviour of potential energy (convexity) allows us to derive physically reasonable and mathematically well posed governing equations. I will consider a simplest example of two-velocity fluids where one of the phases is incompressible (for example, flow of dusty air, or flow of compressible bubbles in an incompressible fluid). A very surprising fact is that one can obtain different governing equations from the same Lagrangian. Different types of the governing equations are due to the choice of independent variables and the corresponding virtual motions. Even if the total momentum and total energy equations are the same, the equations for individual components differ from each other by the presence or absence of gyroscopic forces (also called ‘lift’ forces). These forces have no influence on the hyperbolicity of the governing equations, but can drastically change the distribution of density and velocity of components. To the best of my knowledge, such an uncertainty in obtaining the governing equations of multi- phase flows has never been the subject of discussion in a ‘multi-fluid’ community.
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