...
首页> 外文期刊>Reviews of Geophysics >MODELING AND SIMULATION OF PORE-SCALEMULTIPHASE FLUID FLOW AND REACTIVETRANSPORT IN FRACTURED AND POROUS MEDIA
【24h】

MODELING AND SIMULATION OF PORE-SCALEMULTIPHASE FLUID FLOW AND REACTIVETRANSPORT IN FRACTURED AND POROUS MEDIA

机译:裂隙和多孔介质中孔隙尺度多相流体流动和反应性输运的建模与模拟

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

In the subsurface, fluids play a critical role bytransporting dissolved minerals, colloids, and contaminants(sometimes over long distances); by mediating dissolutionand precipitation processes; and by enabling chemicaltransformations in solution and at mineral surfaces.Although the complex geometries of fracture apertures,fracture networks, and pore spaces may make it difficult toaccurately predict fluid flow in saturated (single-phase)subsurface systems, well-developed methods are available.The simulation of multiphase fluid flow in the subsurface ismuch more challenging because of the large density and/orviscosity ratios found in important applications (water/airin the vadose zone; water/oil, water/gas, gas/oil, and water/oil/gas in hydrocarbon reservoirs; water/aironaqueousphase liquids (nonaqueous phase liquids/dense nonaqueousphase liquids) in contaminated vadose zone systems; andgas/molten rock in volcanic systems, for example). Inaddition, the complex behavior of fluid-fluid-solid contactlines and their impact on dynamic contact angles must also be taken into account and coupled with the fluid flow. Herewe review the methods that are currently being used tosimulate pore-scale multiphase fluid flow and reactivetransport in fractured and porous media. After theintroduction, the review begins with an overview of thefundamental physics of multiphase fluids flow followed bya more detailed discussion of the complex dynamicbehavior of contact lines and contact angles, an importantbarrier to accurate pore-scale modeling and simulation. Themain part of the review focuses on five differentapproaches: pore network models, lattice gas and latticeBoltzmann methods, Monte Carlo methods, particlemethods (molecular dynamics, dissipative particledynamics, and smoothed particle hydrodynamics), andtraditional grid-based computational fluid dynamicscoupled with interface tracking and a contact anglemodel. Finally, the review closes with a discussion offuture trends and challenges.
机译:在地下,流体通过输送溶解的矿物质,胶体和污染物(有时是长距离的)而起着至关重要的作用。通过介导溶解和沉淀过程;尽管裂缝孔,裂缝网络和孔隙空间的复杂几何形状可能使难以准确地预测饱和(单相)地下系统中的流体流动,但可以使用完善的方法。由于在重要应用(渗流区内的水/空气;水/油,水/气,气/油和水/油/气)中发现了大的密度和/或粘度比,因此在地下进行多相流体流动的模拟更具挑战性。碳氢化合物储层中的气体;受污染的渗流带系统中的水/空气/非水相液体(非水相液体/致密非水相液体);以及火山系统中的气体/熔岩。此外,还必须考虑流体-固体-接触线的复杂行为及其对动态接触角的影响,并将其与流体流动相结合。在此,我们回顾了目前用于模拟裂隙和多孔介质中的孔尺度多相流体流动和反应输运的方法。在介绍之后,本综述首先概述了多相流体流动的基本物理原理,然后更详细地讨论了接触线和接触角的复杂动态行为,这是精确进行孔尺度建模和模拟的重要障碍。这篇综述的主要部分集中在五个不同的方法上:孔隙网络模型,晶格气体和格子玻尔兹曼方法,蒙特卡洛方法,粒子方法(分子动力学,耗散粒子动力学和平滑粒子流体动力学),基于传统网格的计算流体动力学,界面跟踪和a接触角模型。最后,回顾以对未来趋势和挑战的讨论结束。

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