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Coupled Simulation Model for Ice Migration

机译:冰迁移耦合模拟模型

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摘要

Detection of exterrestrial ice or water is among the most important tasks for space exploration. The resources are invaluable to build permanent base on the Moon or on the Mars. There are different processes governing the migration, formation and accumulation of ice under exterrestrial environment. Especially, this involves coupling of multiple fields such as thermal, hydraulic and mechanical fields. This paper describes the development and implementation of a coupled thermo-hydro-mechanical model for unsaturated porous materials. The coupling integrates the Fourier's laws for heat transfer, Richard's equation for fluid transfer, and linear constitutive relationship. Coupled parameters were utilized to transfer information within or between field variables. Additional relationships, such as the similarity between drying and freezing processes, Clapeyron equation for ice balance were incorporated to consider the effects of frost action. Numerical simulations were implemented in multiphysical platform to solve the coupled nonlinear partial differential equations. A simulation case was carried out on a relatively simple geometry, using accepted models for thermal, hydraulic and mechanical properties. Results of multiphysical simulations, (such as the freezing induced moisture redistribution, the thermal stresses, etc) are consistent with the basic laws and experience. The results indicate under terrestrial environment, ground freezing will cause moisture to migrate toward ground surface. By incorporating the unique phase transition mechanism under exterrestrial environment, the simulation model can potentially be used to guide the exploration of water resources under exterrestrial environment.
机译:探测外星冰或水是太空探索最重要的任务之一。资源是建立月球或火星永久基地的宝贵资源。在外部环境下,有不同的过程控制着冰的迁移,形成和积聚。特别地,这涉及多个领域的耦合,例如热,液压和机械领域。本文描述了不饱和多孔材料热-水-力学耦合模型的开发和实现。联轴器集成了热传递的傅立叶定律,流体传递的理查德方程和线性本构关系。利用耦合参数在字段变量之内或之间传递信息。还考虑了其​​他关系,例如干燥和冷冻过程之间的相似性,用于冰平衡的Clapeyron方程来考虑霜冻作用的影响。在多物理平台上进行了数值模拟,以求解耦合的非线性偏微分方程。使用公认的热,水力和机械特性模型,在相对简单的几何体上进行了仿真。多物理场模拟的结果(例如冻结引起的水分重新分布,热应力等)与基本定律和经验一致。结果表明,在地面环境下,地面冻结将导致水分向地面迁移。通过结合地球环境下独特的相变机制,该模拟模型可以潜在地用于指导地球环境下的水资源开发。

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