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Numerical Analysis for Transient Two-Dimensional Coupled Heat and Mass Transfer in Soils by Considering the Effect of Seasonal Frost

机译:考虑季节霜效应的瞬态二维耦合热量和土壤传质的数值分析

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The aim of this paper is to provide a numerical solution for simultaneous heat and mass transfer within frozen soil surrounding building foundations. The soil freezing characteristic curve and therefore the ice content are obtained by combining a generalised form of the Clapeyron equation with the soil water retention curve (SWRC) and the thermodynamical equilibrium. The mass conservation is derived by considering the phase change and the water flux due to infiltration. Also, the heat conservation is derived considering phase change, conduction and convection of heat. This results in a system of coupled and highly non-linear differential equations. The numerical method used to solve the system of partial differential equations is based on a Galerkin finite element method with adaptive mesh refinement and dynamic time step control. The developed solution is validated by comparison with experimental data obtained from literature. An application is then presented to demonstrate the heat and mass transfer as a result of heat dissipation of a foundation. The distribution of temperature and ice water content are discussed and it is shown that in spring months (March, April and May), despite the temperature above 0°C at the ground surface, a frost zone still exists within the foundation soil. In the cold period, a high rate of heat transfer between the ground and the upper part of the basement wall causes a sudden change in temperature. Also, during the cold period, it is observed that the heat loss from basement walls is several times higher than the heat loss from the floor slab.
机译:本文的目的是提供一种数值溶液,用于在围绕建筑基础的冷冻土壤中的同时热量和传质。通过与土壤水保留曲线(SWRC)和热力学平衡组合,通过将甲素方程的普通形式与热力学平衡组合来获得土壤冷冻特性曲线,因此冰含量得到冰含量。通过考虑由于渗透引起的相变和水通量来得出质量保护。而且,考虑到热量的相变,传导和对流来推导热保守。这导致耦合和高度非线性微分方程的系统。用于解决部分微分方程系统的数值方法基于具有自适应网格细化和动态时间步长控制的Galerkin有限元方法。通过与从文献获得的实验数据进行比较验证开发的解决方案。然后提出了一种应用以证明由于基础的散热而导致的热量和质量传递。讨论了温度和冰水含量的分布,表明,在春季(3月,4月和5月)中,尽管在地面上高于0°C,霜区仍然存在于基础土壤中。在寒冷的时期,地面和基底壁的上部之间的高热传递速率导致温度突然变化。而且,在寒冷时期,观察到地下室壁的热量损失比从地板平板的热量损失高几倍。

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