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首页> 外文期刊>International Journal of Thermal Sciences >Validation of a two-dimensional gas-kinetic scheme for compressible natural convection on structured and unstructured meshes
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Validation of a two-dimensional gas-kinetic scheme for compressible natural convection on structured and unstructured meshes

机译:结构化和非结构化网眼压缩自然对流二维气体动力学方案的验证

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摘要

Gas-kinetic schemes (GKS) have been developed as a kinetic Finite-Volume approach to computational fluid dynamics. The GKSa prioriallows to obtain approximate solutions of the fully compressible Navier-Stokes equations. In our contribution we show simulation results of compressible natural convection at large temperature differences and low Mach numbers beyond the applicable range of the Boussinesq approximation. The simulations were performed on non-uniform quadrilateral and unstructured triangular grids. The dependence of the critical Rayleigh number on the temperature difference for compressible Rayleigh-Bénard convection, predicted by theory, is accurately reproduced. Moreover, heat transfer in a buoyancy driven square cavity with differentially heated sides at large Rayleigh numbers and large temperature differences is investigated. Temperature and velocity profiles as well as Nusselt numbers show good agreement with benchmark results in literature. After validating the scheme for thermal compressible convection, we investigate unsteady natural convection at a Rayleigh number ofRa=5?109and at a large temperature difference ofTh/Tc=4. We find that compressibility has a leading influence on the stability of the boundary layers, such that the flow at the heated wall becomes unstable, whereas the flow at the cooled wall remains stable. This phenomenon has not yet received much attention.
机译:气体动力学方案(GKS)已被开发为计算流体动力学的动力学有限体积方法。 GKSA PROSIALLOWS获得完全可压缩Navier-Stokes方程的近似解。在我们的贡献中,我们显示了在大型温度差异和超出适用范围的近似范围内的可压缩自然对流的仿真结果。对非均匀四边形和非结构化三角网进行模拟。临界瑞利数对由理论预测的可压缩瑞利-Bénard对流的温差的依赖性,准确地再现。此外,研究了在大型瑞利数的差差侧的浮力驱动方腔中的热传递和大的温度差异。温度和速度概况以及纽带号显示与文学的基准结果良好。在验证热可压缩对流方案后,我们在瑞利= 5?109和DTH / TC = 4的大温差下调查不稳定的自然对流。我们发现压缩性具有对边界层的稳定性产生的主要影响,使得加热壁的流变得不稳定,而冷却壁的流量保持稳定。这种现象尚未受到很大的关注。

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