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Lattice Boltzmann simulation of heat transfer with phase change in saturated soil during freezing process

机译:冻结过程中饱和土相变的晶格Boltzmann仿真

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A lattice Boltzmann model is presented for simulating heat transfer with phase change in saturated soil. The model includes a quartet structure generation set for creating soil structure, double distribution functions for simulating temperature field evolution of soil particles and water, respectively, and an enthalpy-based method for tracing phase interface. The model is validated by two cases with analytical solutions. Then, we investigate the influence of porosity on freezing process in saturated sandy loam soil. The results demonstrate that porosity is the predominant factor when the location is far from the cold source; otherwise, thermal gradient is more important.
机译:提出了一种晶格Boltzmann模型,用于模拟饱和土中相变的热传递。 该模型包括用于产生土壤结构,分别用于模拟土壤颗粒和水的温度场演变的双分布函数的四重奏结构,以及用于跟踪相界面的焓的方法。 该模型由两个分析解决方案的两种情况进行验证。 然后,我们研究了孔隙率对饱和砂土土壤中冷冻过程的影响。 结果表明,当位置远离冷源时,孔隙率是主要因素; 否则,热梯度更为重要。

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