论文标题
颗粒悬浮液中的传热状态
Regimes of heat transfer in particle suspensions
论文作者
论文摘要
我们介绍了在有限大小的中性型球形颗粒中进行传热的界面分辨模拟的结果,用于固体体积分数高达35%,而大量雷诺数从500到5600。流体方法的浸泡到液体含量的边界体积来求解流体和固体阶段的能量方程。我们将热传递与先前鉴定的粒子运动状态,即低体积分数处的粘性状态和较低的雷诺数,高雷诺克处的颗粒湍流以及中等体积的分数以及高体积分数下的颗粒状状态。我们表明,在粘性主导的状态下,热传递主要是由于热扩散并由于粒子诱导的波动而增强。在类似湍流的状态下,我们观察到由湍流通量主导的全球热传递的最大增强。然而,在颗粒剪切厚的状态下,随着粒子向通道核心的迁移而淬灭,传热增强降低。结果,紧凑的松散填充的核心区域形式以及热扩散对总热传递的贡献再次变得很重要。在这些流量的体积分数大于25%的情况下,全局传热变为低于单相湍流。
We present results of interface-resolved simulations of heat transfer in suspensions of finite-size neutrally-buoyant spherical particles for solid volume fractions up to 35% and bulk Reynolds numbers from 500 to 5600. An Immersed Boundary-Volume of Fluid method is used to solve the energy equation in the fluid and solid phase. We relate the heat transfer to the regimes of particle motion previously identified, i.e. a viscous regime at low volume fractions and low Reynolds number, particle-laden turbulence at high Reynolds and moderate volume fraction and particulate regime at high volume fractions. We show that in the viscous dominated regime, the heat transfer is mainly due to thermal diffusion with enhancement due to the particle-induced fluctuations. In the turbulent-like regime, we observe the largest enhancement of the global heat transfer, dominated by the turbulent heat flux. In the particulate shear-thickening regime, however, the heat transfer enhancement decreases as mixing is quenched by the particle migration towards the channel core. As a result, a compact loosely-packed core region forms and the contribution of thermal diffusion to the total heat transfer becomes significant once again. The global heat transfer becomes, in these flows at volume fractions larger than 25%, lower than in single-phase turbulence.