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Influence of arrangement of freezing tubes on the ground freezing process with flowing groundwater

机译:冻结管的布置对地下水渗流对地面冻结过程的影响

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Ground freezing process, while flow of the groundwater takes place is analysed in the paper. The considered process precedes drilling of the shafts. In particular, problem of arrangement of freezing tubes is discussed in the paper to obtain uniform frozen layer. It was demonstrated~8, that the flow of the groundwater can seriously influence the freezing process, and, if regular arrangement of freezing tubes is used, it can sometimes lead to formation of very unequal frozen layer. The appropriate numerical 2D calculations have been performed and their resutls are presented. Both the groundwater flow and the temperature field are calculated using FEM. The flow of the roundwater has been assumed to be incompressible. The velocity of the groundwater is then related to the velocity potential by Darcy's law and this potential is described by Laplace equation. The temperature distribution is determined by standard unsteady - state heat conduction equation with convective term in the unfrozen part of the domain and Stefan's boundary condition on the phase change interface. The original technique has been used, because of the unfrozen part of the domain, where the groundwater flows, changes it shape in time.
机译:本文分析了地面冻结过程,同时发生了地下水的流动。考虑的过程先于轴钻孔。特别地,在本文中讨论了冷冻管的布置问题以获得均匀的冷冻层。证明了〜8,地下水的流动会严重影响冷冻过程,如果定期使用冷冻管,有时会导致形成非常不均匀的冷冻层。适当的2D数值计算已经执行,并显示了其结果。地下水流量和温度场都是使用有限元法计算的。假定圆形水的流动不可压缩。然后,根据达西定律将地下水的速度与速度势相关,并用拉普拉斯方程描述该势。温度分布由标准的非稳态热传导方程确定,该方程在区域的未冻结部分具有对流项,并且在相变界面上具有Stefan边界条件。之所以使用原始技术,是因为该区域的未冻结部分(地下水流向该部分)会及时改变其形状。

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