4.7 Article

Regimes of heat transfer in finite-size particle suspensions

Journal

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.ijheatmasstransfer.2021.121514

Keywords

Direct simulation; Heat transfer; Multiphase flow; Particle suspension

Funding

  1. European Research Council [ERC-2013-CoG-616186]
  2. TRITOS
  3. Swedish Research Council [VR 2014-5001]
  4. National Infrastructure for High Performance Computing and Data Storage in Norway [NN9561K]

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This study presents the heat transfer characteristics of particle suspensions under different particle concentrations and Reynolds numbers through interface-resolved simulations. The variation of heat transfer mechanisms is discussed from the perspective of particle motion regimes, showing that heat transfer in the viscous regime is mainly influenced by thermal diffusion, while the largest enhancement occurs in the particle-laden turbulence regime, and heat transfer enhancement in the particulate shear-thickening regime is influenced by mixing effects.
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 turbu-lence 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. (c) 2021 The Author(s). Published by Elsevier Ltd. This is an open access article under the CC BY license ( http://creativecommons.org/licenses/by/4.0/ )

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