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首页> 外文期刊>International Journal for Numerical and Analytical Methods in Geomechanics >Coupled solution of heat and moisture flow in unsaturated clay barriers in a repository geometry
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Coupled solution of heat and moisture flow in unsaturated clay barriers in a repository geometry

机译:储层几何结构中非饱和黏土屏障中热湿流的耦合解

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摘要

An analytical solution in the Laplace transform domain is obtained for the transient heat and moisture transport in an unsaturated clay buffer with a geometry simulating repository conditions. A numerical inversion scheme based on Crump's method is used to obtain the time-domain solution. The coupled effect of thermally driven moisture transport is especially investigated because of its importance to alter the flow field in low-permeability buffers. The practical background is based on the case of an engineering bentonite barrier placed in a drift excavated in rock in the context of underground disposal of high-level radioactive waste. Parametric study has been performed to assess the effects of dimensionless geometry and material parameters on flow field. Despite the simplified assumptions required in order to obtain analytical expressions, the results incorporate the main mechanisms involved in the coupled thermo-hydraulic (T-H) problem, and they may be eventually used for validation purposes.
机译:获得了Laplace变换域中的解析解,用于在不饱和粘土缓冲区中进行瞬态热量和水分传输,并具有模拟库条件的几何形状。基于Crump方法的数值反演方案用于获得时域解。由于其对改变低渗透缓冲液中的流场的重要性,因此特别研究了热驱动水分传输的耦合效应。实际背景是基于在地下处置高放射性废物的背景下将工程膨润土屏障置于岩石开挖的巷道中的情况。已经进行了参数研究,以评估无量纲几何形状和材料参数对流场的影响。尽管为了获得解析表达式而需要简化的假设,但结果仍包含了耦合热液(T-H)问题中涉及的主要机理,并且最终可以将它们用于验证目的。

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