湍流热对流中稀微粒子的输运和沉积

A. Xu, Shi Tao, Leping Shi, H. Xi
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引用次数: 15

摘要

本文分析了稀颗粒在湍流瑞利-贝纳德对流中的输运和沉积行为。对瑞利数($Ra$)为$10^{8}$和普朗特数($Pr$)为0.71(对应于空气的工质)进行了二维直接数值模拟。采用拉格朗日点粒子模型来描述微粒子在湍流中的运动。结果表明:在Stokes数($St$)小于$10^{-3}$时,悬浮粒子在湍流中均匀分布,在$10^{-3}\lesssim St \lesssim 10^{-2}$时,悬浮粒子倾向于聚集成带。在更大的St下,微粒会在对流中迅速沉积。我们还计算了粒子轨迹的均方位移(MSD)。在较短的时间间隔内,MSD呈弹道分布,在垂直方向和横向方向上各向同性;在较长的时间间隔内,MSD反映了粒子的受限运动,并且在不同方向上具有各向异性。我们进一步得到了颗粒在壁上沉积位置的相图,并根据颗粒的密度和直径确定了三种沉积状态。一个有趣的发现是,分散的颗粒倾向于沉积在热羽流产生的垂直壁上,这可以通过倾斜电池和改变大尺度环流的旋转方向来验证。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Transport and deposition of dilute microparticles in turbulent thermal convection
We analyze the transport and deposition behavior of dilute microparticles in turbulent Rayleigh-Benard convection. Two-dimensional direct numerical simulations were carried out for the Rayleigh number ($Ra$) of $10^{8}$ and the Prandtl number ($Pr$) of 0.71 (corresponding to the working fluids of air). The Lagrangian point particle model was used to describe the motion of microparticles in the turbulence. Our results show that the suspended particles are homogeneously distributed in the turbulence for the Stokes number ($St$) less than $10^{-3}$, and they tend to cluster into bands for $10^{-3} \lesssim St \lesssim 10^{-2}$. At even larger $St$, the microparticles will quickly sediment in the convection. We also calculate the mean-square displacement (MSD) of the particle's trajectories. At short time intervals, the MSD exhibits a ballistic regime, and it is isotropic in vertical and lateral directions; at longer time intervals, the MSD reflects a confined motion for the particles, and it is anisotropic in different directions. We further obtained a phase diagram of the particle deposition positions on the wall, and we identified three deposition states depending on the particle's density and diameter. An interesting finding is that the dispersed particles preferred to deposit on the vertical wall where the hot plumes arise, which is verified by tilting the cell and altering the rotation direction of the large-scale circulation.
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