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首页> 外文期刊>Vadose Zone Journal >Numerical Evaluation of Effective Unsaturated Hydraulic Properties of Fractured Rocks using a Stochastic Continuum Approach
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Numerical Evaluation of Effective Unsaturated Hydraulic Properties of Fractured Rocks using a Stochastic Continuum Approach

机译:随机连续谱法数值模拟裂隙岩的有效非饱和水力特性

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摘要

This study builds on past studies that have investigated the effective properties of unsaturated porous media and merges stochastic continuum concepts to develop a numerical procedure for estimating the effective flow parameters that are independent of pressure head or saturation. The procedure involves the development of a numerical permeameter based on randomly generated, spatially correlated fields of fundamental fracture properties such as spacing and aperture. Local values of hydraulic conductivity, and the van Genuchten fitting parameters α and n in this random field are computed from local values of mechanical aperture and spacing based on the cubic law and relationships established from pore-scale fracture simulations. By considering multiple realizations of these spatially correlated fields and by running the numerical permeameter over a range of effective saturations and flow rates, outputs are generated that can be fit with the standard van Genuchten model to estimate block effective values of saturated hydraulic conductivity and the van Genuchten unsaturated hydraulic parameters of a fracture continuum at the field scale. These parameters can then be incorporated to conventional numerical simulators originally developed for porous media. The study shows that reasonable approximations to the results obtained through computationally demanding stochastic simulations can be developed based on estimates of the mean fracture spacing and aperture. Although the example application assumes the presence of an impermeable rock matrix, the hydraulic properties estimated for the fracture continuum with this methodology can be combined with those measured or similarly estimated for a matrix continuum in dual-permeability continuum models.
机译:这项研究是在以往研究的基础上进行的,这些研究调查了不饱和多孔介质的有效特性,并合并了随机连续体的概念,以开发一种数值程序来估算独立于压头或饱和度的有效流量参数。该程序涉及基于基本断裂特性(例如间距和孔径)的随机生成的,与空间相关的场的基础上的数值渗透仪的开发。根据立方定律和从孔隙尺度裂缝模拟建立的关系,根据机械孔径和间距的局部值,计算出该水力传导率的局部值以及该随机字段中的van Genuchten拟合参数α和n。通过考虑这些空间相关字段的多种实现,并通过在一定的有效饱和度和流速范围内运行数值渗透仪,可以生成可与标准van Genuchten模型拟合的输出,以估算饱和水力传导率和van的块有效值。现场尺度上裂缝连续体的Genuchten非饱和水力参数。然后可以将这些参数合并到最初为多孔介质开发的常规数值模拟器中。研究表明,可以基于平均裂缝间距和孔径的估算值,对通过计算要求较高的随机模拟获得的结果进行合理近似。尽管示例应用程序假定存在不渗透的岩石基质,但是可以使用这种方法将对裂缝连续体估算的水力特性与在双渗透连续体模型中针对矩阵连续体测得或类似估算的那些相结合。

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  • 来源
    《Vadose Zone Journal》 |2012年第4期|p.1-10|共10页
  • 作者单位

    aComputational Earth Sciences Group (EES-16), MS T003, Los Alamos National Labora-tory, Los Alamos, NM 87545, USA;

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  • 正文语种 eng
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