首页> 外文期刊>Journal of Contaminant Hydrology >Macro-scale effective constitutive relationships for two-phase flow processes in heterogeneous porous media with emphasis on the relative permeability-saturation relationship
【24h】

Macro-scale effective constitutive relationships for two-phase flow processes in heterogeneous porous media with emphasis on the relative permeability-saturation relationship

机译:非均质多孔介质中两相流过程的宏观有效本构关系,重点是相对渗透率-饱和关系

获取原文
获取原文并翻译 | 示例
           

摘要

Macro-scale simulations often play an important role in the assessment and remediation of contamination by dense non-aqueous phase liquids (DNAPLs) in the subsurface. Effective parameters for the macro scale are required for these simulations in order to avoid a detailed discretisation of the geological structures. Starting from the observed influence of heterogeneities on multiphase flow processes at the macro scale, we present an upscaling procedure from the local to the macro scale for the derivation of constitutive relationships for multiphase flow processes. The approach is based on the assumption of an equilibrium of (capillary) forces, which allows the application of a percolation model. This results in saturation distributions for different capillary pressures. Averaging these distributions gives rise to a macroscopic capillary pressure-saturation relationship. For the saturation distribution, relative permeabilities and effective conductivities are computed depending on the structure and the flow direction. These are averaged with the help of the renormalisation method. The evolving relative permeability-saturation relationship for the macro scale shows a saturation-dependent anisotropy and pronounced residual saturations of the nonwetting phase (which were not assumed for the local scale). The anisotropy reflects the underlying structure of the considered system that needs not to be known in detail.
机译:宏观模拟通常在评估和补救地下稠密非水相液体(DNAPL)污染中起重要作用。这些模拟需要使用宏观尺度的有效参数,以避免地质结构的详细离散化。从宏观上观察到的非均质性对多相流动过程的影响出发,我们提出了从局部到宏观尺度的升阶过程,以推导多相流动过程的本构关系。该方法基于(毛细管)力平衡的假设,这允许应用渗流模型。这导致不同毛细管压力的饱和度分布。对这些分布求平均将产生宏观的毛细管压力-饱和关系。对于饱和度分布,根据结构和流动方向计算相对磁导率和有效电导率。在重新归一化方法的帮助下将它们平均。宏观尺度上不断变化的相对渗透率-饱和度关系显示出与饱和度有关的各向异性和非润湿相的显着残余饱和度(对于局部尺度未假定)。各向异性反映了不需要详细了解的所考虑系统的底层结构。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号