首页> 外文会议>International conference on cold regions engineering >Numerical Analysis for Transient Two-Dimensional Coupled Heat and Mass Transfer in Soils by Considering the Effect of Seasonal Frost
【24h】

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

机译:考虑季节冻害的土壤瞬态二维传热传质数值分析

获取原文

摘要

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:本文的目的是为建筑物基础周围的冻土内部同时传热和传质提供数值解决方案。通过将Clapeyron方程的广义形式与土壤保水曲线(SWRC)和热力学平衡相结合,可以获得土壤的冻结特性曲线以及冰含量。质量守恒是通过考虑相变和渗透引起的水通量得出的。同样,在考虑相变,热传导和对流的情况下得出热量守恒。这导致了一个耦合的,高度非线性的微分方程系统。用于求解偏微分方程组的数值方法是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。通过与从文献中获得的实验数据进行比较,可以验证所开发的解决方案。然后介绍了一个应用程序,以演示由于地基散热而产生的热量和质量传递。讨论了温度和冰水含量的分布,结果表明,在春季月份(3月,4月和5月),尽管地表温度高于0°C,但在基础土壤中仍存在霜冻区。在寒冷时期,地面与地下室壁上部之间的高传热率会引起温度的突然变化。另外,在寒冷时期,观察到地下室壁的热损失比楼板的热损失高几倍。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号