Transient-pressure modelling in fractured porous media with a new embedded finite element approach

IF 4 2区 环境科学与生态学 Q1 WATER RESOURCES
Behnam V. Damirchi , Pouria Behnoudfar , Luís A.G. Bitencourt Jr. , Osvaldo L. Manzoli , Daniel Dias-da-Costa
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Abstract

This paper presents a unified, embedded finite element formulation for simulating transient fluid flow in fractured porous media while accounting for transverse and longitudinal directions. The transverse flow arises due to pressure variations on both sides of fractures, as these typically exhibit lower permeability in the perpendicular direction. A simple coupling framework is introduced to connect independent sets of finite element meshes, one for the bulk porous media and the other for natural discontinuities. Importantly, the proposed coupling technique does not introduce additional degrees of freedom, and discontinuities can arbitrarily intersect the background elements of the continuum domain. Additionally, standard quadrature rules for integration can be used without modifications, thus avoiding additional remediation steps found with nodal enrichment strategies. These advantageous features make our method a robust technique capable of modelling transient fluid flow as an integral part of a coupled hydro-mechanical formulation. The performance is assessed using several numerical examples. These encompass various cases of fracture orientation relative to the background elements. The results demonstrate a good agreement with reference solutions. The effects of the coupling parameter, as well as the transverse and longitudinal permeabilities, in the temporal domain, are also investigated. The results demonstrated that the proposed method is capable of handling any values of transverse or longitudinal permeability compared to the surrounding porous domain. Moreover, the findings confirmed that, as a rule of thumb, a coupling parameter should be selected 10 times larger than the highest permeability used in the model.

用新的嵌入式有限元方法建立断裂多孔介质中的瞬态压力模型
本文提出了一种统一的嵌入式有限元公式,用于模拟断裂多孔介质中的瞬态流体流动,同时考虑横向和纵向方向。横向流动是由于裂缝两侧的压力变化引起的,因为这些裂缝通常在垂直方向表现出较低的渗透性。本文引入了一个简单的耦合框架,用于连接独立的有限元网格集,其中一个用于连接大体积多孔介质,另一个用于连接天然不连续面。重要的是,所提出的耦合技术不会引入额外的自由度,非连续性可以任意地与连续域的背景元素相交。此外,标准正交积分规则无需修改即可使用,从而避免了节点富集策略中的额外补救步骤。这些优势使我们的方法成为一种强大的技术,能够将瞬态流体流动建模作为水力机械耦合计算的一个组成部分。我们通过几个数值实例对该方法的性能进行了评估。这些例子包括相对于背景元素的断裂方向的各种情况。结果表明与参考解具有良好的一致性。此外,还研究了耦合参数以及横向和纵向渗透率在时域中的影响。结果表明,与周围多孔域相比,所提出的方法能够处理任何横向或纵向渗透率值。此外,研究结果还证实,作为经验法则,耦合参数的选择应比模型中使用的最高渗透率大 10 倍。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Advances in Water Resources
Advances in Water Resources 环境科学-水资源
CiteScore
9.40
自引率
6.40%
发文量
171
审稿时长
36 days
期刊介绍: Advances in Water Resources provides a forum for the presentation of fundamental scientific advances in the understanding of water resources systems. The scope of Advances in Water Resources includes any combination of theoretical, computational, and experimental approaches used to advance fundamental understanding of surface or subsurface water resources systems or the interaction of these systems with the atmosphere, geosphere, biosphere, and human societies. Manuscripts involving case studies that do not attempt to reach broader conclusions, research on engineering design, applied hydraulics, or water quality and treatment, as well as applications of existing knowledge that do not advance fundamental understanding of hydrological processes, are not appropriate for Advances in Water Resources. Examples of appropriate topical areas that will be considered include the following: • Surface and subsurface hydrology • Hydrometeorology • Environmental fluid dynamics • Ecohydrology and ecohydrodynamics • Multiphase transport phenomena in porous media • Fluid flow and species transport and reaction processes
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