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Thermo-hydraulic modeling of artificial ground freezing: Application to an underground mine in fractured sandstone

机译:人工地面冻结的热工水力模拟:在裂缝性砂岩地下矿中的应用

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The difficult geological conditions of underground mines in permeable and fractured rocks require the use of ground support and inflow management methods. Artificial ground freezing offers the opportunity to reduce the permeability of the ground and to consolidate it. However, the establishment of this technique can be made complicated by two phenomenas: the strong ground heterogeneity, which renders delicate an overall freezing prediction, and the potential presence of high seepage-flow velocities, which may have a negative impact on freezing progress. The present article presents a coupled use of the thermo-hydraulic model and the freeze-pipe ground model presented in Vitel et al. (2016, 2015) with an application to the Cigar Lake underground mine in Northern Saskatchewan, Canada. The first model allows the estimation of the temperature and pressure distribution in the ground during freezing while the second model simulates the heat transfer between a freeze pipe and the surrounding ground, which is useful to determine the boundary conditions of the thermo-hydraulic model. First, the article restates the governing equations of both models. Then, after the validation of the numerical results with respect to field measurements, a joint use of the models is proposed, in particular to (i) predict the ground temperature evolution, (ii) study the impacts of the geological conditions on the freezing progress and (iii) optimize the freezing system design. (C) 2016 Elsevier Ltd. All rights reserved.
机译:地下矿井在渗透性和破碎性岩石中的艰难地质条件要求使用地面支撑和流入管理方法。人工冻结地面提供了降低地面渗透性并加以巩固的机会。但是,此技术的建立可能会因以下两种现象而变得复杂:强烈的地面异质性(使整体冻结预测变得微妙)和高渗流速度的潜在存在(可能对冻结进度产生负面影响)。本文介绍了Vitel等人提出的热工水力模型和冻结管地面模型的结合使用。 (2016年,2015年)应用于加拿大北萨斯喀彻温省的雪茄湖地下矿山。第一个模型可以估算冻结过程中地面的温度和压力分布,而第二个模型可以模拟冻结管与周围地面之间的热传递,这对于确定热工水力模型的边界条件很有用。首先,本文重申了两个模型的控制方程。然后,在对有关野外测量的数值结果进行验证之后,提出了模型的联合使用,特别是(i)预测地温变化,(ii)研究地质条件对冻结过程的影响(iii)优化冷冻系统的设计。 (C)2016 Elsevier Ltd.保留所有权利。

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