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Estimation of Heat Transfer Coefficients for Biomass Particles by Direct Numerical Simulation Using Microstructured Particle Models in the Laminar Regime

机译:利用层压制度中微结构粒子模型的直接数值模拟估计生物质颗粒的热传递系数

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Direct numerical simulation of convective heat transfer from hot gas to isolated biomass particle models with realistic morphology and explicit microstructure was performed over a range of conditions in the laminar regime. Steady-state results demonstrated that convective interfacial heat transfer is dependent on the wood species. The computed heat transfer coefficients were shown to vary between the pine and aspen models by nearly 20%. These differences are attributed to the species-specific variations in the exterior surface morphology of the biomass particles. We also quantify variations in heat transfer experienced by the particle when positioned in different orientations with respect to the direction of Fluid flow. These results are compared to previously reported heat transfer coefficient correlations in the range of 0.1 < Pr < 1.5 and 10 < Re < 500. Comparison of these simulation results to correlations commonly used in the literature (Gunn, Ranz-Marshall, and Bird-Stewart-Lightfoot) shows that the Ranz-Marshall (sphere) correlation gave the closest h values to our steady-state simulations for both wood species, though no existing correlation was within 20% of both species at all conditions studied. In general, this work exemplifies the fact that all biomass feedstocks are not created equal, and that their species-specific characteristics must be appreciated in order to facilitate accurate simulations of conversion processes.
机译:在层流制度的一系列条件下,在一系列条件下在具有现实形态和显式微观结构的热气体与分离的生物质粒子模型的直接数值模拟。稳态结果表明,对流界面传热依赖于木材物种。所计算的传热系数显示在松树和白杨模型之间变化近20%。这些差异归因于生物质颗粒的外表面形态的特异性变化。当在不同取向相对于流体流动方向上定位不同取向时,我们还量化了粒子所经历的传热变化。将这些结果与先前报告的传热系数相关性与0.1

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