Turbulent Dynamics and Heat Transfer in Transcritical Channel Flow

Kukjin Kim, C. Scalo, Jean-Pierre Hickey
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引用次数: 1

Abstract

We present direct numerical simulations (DNS) of turbulent channel flow to study turbulent dynamics and heat transfer effects at a transcritical temperature and supercritical pressure regime. The fully compressible Navier–Stokes equations in conservative form are closed with the Peng–Robinson (PR) equation of state and the Chung’s model for the thermophysical and transport properties. To quantify the turbulent heat transfer effect, the bottom and top walls of the channel are maintained at different isothermal temperatures, Ttop/bot = Tpb±∆T/2, where Tpb is the pseudoboiling temperature of working fluid and ∆T = 20 K. The bulk pressure and velocity are 1.1pc and 36 m/s, respectively, where pc is the critical pressure. The statistical mean profiles shows significant thermophysical variation in the regime having large thermodynamic gradient near the walls compared to the ideal gas case and the average pseudoboiling location is observed at y/h = 0.92. The root mean square (RMS) profiles of fluctuating velocity are attenuated in the pseudogas region, whereas the thermodynamic fluctuations are greater in that region than the pseudoliquid region. One-dimensional energy spectra fall off steeply at high wavenumber showing the adequacy of the DNS resolution. Instantaneous visualizations of near-wall turbulent structures reveal that the dense fluid ejection from the bottom wall reaches to the channel center region resulting in the large fluctuation in the thermodynamic properties across the channel.
跨临界通道流动中的湍流动力学和传热
我们提出了紊流通道流动的直接数值模拟(DNS)来研究跨临界温度和超临界压力下的紊流动力学和传热效应。完全可压缩的保守形式的Navier-Stokes方程被Peng-Robinson (PR)状态方程和Chung的热物理和输运性质模型所封闭。为了量化紊流换热效果,将通道底部和顶部壁面保持在不同的等温温度下,top/bot = Tpb±∆T/2,其中Tpb为工质拟沸腾温度,∆T = 20 K。体压力为1.1pc,速度为36 m/s,其中pc为临界压力。统计平均剖面显示,在壁面附近有较大热力学梯度的情况下,与理想气体情况相比,热物理变化显著,在y/h = 0.92时观察到平均伪沸腾位置。波动速度的均方根(RMS)分布在伪气体区有所衰减,而热力学波动在该区域比在伪液体区更大。一维能谱在高波数处急剧下降,显示了DNS分辨率的充分性。近壁湍流结构的瞬时可视化显示,从底壁喷出的致密流体到达通道中心区域,导致整个通道的热力学性质发生较大波动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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