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Solutions of an inverse laminar natural convection problem by subdomain and Galerkin methods

机译:子域和Galerkin方法求解逆层流自然对流问题

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摘要

Reconstruction of the velocity field, for a laminar free convection flow, from the knowledge of the temperature distribution, within the flow, is an inverse heat transfer problem. In this investigation, the velocity profile for a laminar convective flow along an isothermal vertical plate is reconstructed using known temperature distributions. The temperature distributions used in this inverse problem were generated numerically from the direct similarity solutions. To solve this inverse problem, continuity, momentum and energy equations are considered. To obtain the velocity solutions (profiles), the Galerkin and subdomain weighted residual methods are employed. The velocity solutions are represented by the sum of n-term weak functions satisfying the boundary conditions. The solutions considered in this study belong to a family of sine and polynomial functions. Comparison of the inverse solutions with the direct solutions confirms that velocity profiles can be reconstructed from the knowledge of temperature distribution with good accuracy.
机译:从层流内的温度分布的知识出发,对于层流自由对流而言,速度场的重建是一个逆向传热问题。在这项研究中,使用已知的温度分布重建了沿等温垂直板的层流对流的速度分布。反问题中使用的温度分布是从直接相似解中数值生成的。为了解决这个反问题,考虑了连续性,动量和能量方程。为了获得速度解(轮廓),采用了Galerkin和子域加权残差法。速度解由满足边界条件的n个项的弱函数之和表示。本研究中考虑的解决方案属于正弦函数和多项式函数。逆解与直接解的比较证实,可以从温度分布的知识中以良好的精度重建速度分布。

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