描述流体等压单向垂直涡旋流动的Navier-Stokes方程的精确解

N. Burmasheva, E. Prosviryakov
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引用次数: 2

摘要

本文提出了描述等压非均匀单向流体运动的Navier-Stokes方程的一组精确解。由于不可压缩性方程,非均匀库埃特流的速度依赖于两个坐标和时间。速度场的表达式具有广泛的泛函任意性。采用分离变量的方法得到了精确解,并利用可加性和可乘性两种代数运算证明了修正经典库埃特流的重要性。这篇文章包含了广泛的参考书目信息,使它有可能跟踪在精确的库埃特解决方案的变化,为流体力学的各个领域的牛顿不可压缩流体。流体流动由依赖于一个变量(水平坐标)的多项式来描述。多项式的系数在函数上依赖于第二(垂直)坐标和时间;它们由一系列最简单的齐次和非齐次偏微分抛物型方程确定。将精确解代入Navier-Stokes方程后,用待定系数法得到了方程链。提出了一种研究粘性流体稳态运动的常微分方程组的积分算法。在这种情况下,所有定义速度的函数都是多项式。结果表明,即使没有对流混合(蠕变流),涡度矢量和剪应力的拓扑结构也具有复杂的结构。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Exact solutions of the Navier–Stokes equations for describing an isobaric one-directional vertical vortex flow of a fluid
The article proposes a family of exact solutions to the Navier–Stokes equations for describing isobaric inhomogeneous unidirectional fluid motions. Due to the incompressibility equation, the velocity of the inhomogeneous Couette flow depends on two coordinates and time. The expression for the velocity field has a wide functional arbitrariness. This exact solution is obtained by the method of separation of variables, and both algebraic operations (additivity and multiplicativity) are used to substantiate the importance of modifying the classical Couette flow. The article contains extensive bibliographic information that makes it possible to trace a change in the exact Couette solution for various areas of the hydrodynamics of a Newtonian incompressible fluid. The fluid flow is described by a polynomial depending on one variable (horizontal coordinate). The coefficients of the polynomial functionally depend on the second (vertical) coordinate and time; they are determined by a chain of the simplest homogeneous and inhomogeneous partial differential parabolic-type equations. The chain of equations is obtained by the method of undetermined coefficients after substituting the exact solution into the Navier–Stokes equation. An algorithm for integrating a system of ordinary differential equations for studying the steady motion of a viscous fluid is presented. In this case, all the functions defining velocity are polynomials. It is shown that the topology of the vorticity vector and shear stresses has a complex structure even without convective mixing (creeping flow).
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