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Investigation on the natural convection in horizontal concentric annulus using the variable property-based lattice Boltzmann flux solver

机译:基于可变属性的格子玻尔兹曼通量求解器研究水平同心环空中的自然对流

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The natural convection in horizontal concentric annulus with isothermal walls is studied numerically by using the recently-proposed variable property-based lattice Boltzmann flux solver (VPLBFS). The widely-concerned constant property solution (CPS) and the real solution (VPS) in which the total variation in fluid properties is considered, are obtained by using the simplified version and the standard version of the VPLBFS, respectively. The integral effect of the total variation in fluid properties on flow patterns and heat transfer rates is discussed, and the deviation of the CPS from the real solution is quantified in a wide range of temperature difference ratio. Then, several commonly-reported solutions with partial variation in fluid properties (P-VPSs) are obtained by using various simplified versions of the VPLBFS. The individual effects of partial variation in fluid properties are discussed through the comparison between the P-VPSs and the CPS. It is found that the individual effects depend on individuals, but none of which can be regarded as a good approximation to the integral effect of the total variation in fluid properties as a large temperature difference ratio is imposed. The present work gives the real solution for the natural convection heat transfer in horizontal concentric annulus and demonstrates the necessity of considering the total variation in fluid properties in the study about thermal flow problems in which the Boussinesq approximation is invalid.
机译:通过使用最近提出的基于可变属性的点阵玻尔兹曼通量求解器(VPLBFS),对具有等温壁的水平同心环空中的自然对流进行了数值研究。分别使用简化版本和标准版本的VPLBFS获得了广泛关注的恒定特性解决方案(CPS)和考虑了流体特性总变化的实际解决方案(VPS)。讨论了流体性质的总变化对流型和传热速率的整体影响,并在较宽的温差比范围内量化了CPS与实际溶液的偏差。然后,通过使用VPLBFS的各种简化版本,可以获得几种流体特性(P-VPSs)有部分变化的常用报告解决方案。通过比较P-VPS和CPS,讨论了流体特性局部变化的个体影响。发现个体效应取决于个体,但是当施加大的温差比时,没有一个可以被认为是流体特性总变化的积分效应的良好近似。目前的工作为水平同心环空自然对流换热提供了真正的解决方案,并证明了在研究Boussinesq近似无效的热流问题时,必须考虑流体性质的总变化。

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