{"title":"高非均质多孔介质中CCAR网格的混合有限元方法","authors":"Davood Khoozan , Bahar Firoozabadi","doi":"10.1016/j.advwatres.2025.105089","DOIUrl":null,"url":null,"abstract":"<div><div>Upscaling is critical in computational simulations of flow and transport in porous media, bridging fine-scale geological details with coarse-scale computational models, particularly in groundwater modeling and subsurface hydrology. Cartesian cell-based anisotropic refinement (CCAR) grids facilitate this process by adaptively refining grid cells in regions of significant heterogeneity or complex flow dynamics. This study proposes a novel mixed hybrid finite element (MHFE) method for solving flow equations on CCAR grids. The method employs hypothetical triangulation, subdividing each CCAR grid element based on the number of surrounding faces. This enables the elimination of internal face unknowns through flux conservation and pressure continuity rules, enhancing computational efficiency without increasing the degrees of freedom. The proposed method was validated using four models, including synthetic and highly heterogeneous domains with various boundary conditions. The accuracy of the proposed method is evaluated against a fine-grid reference solution and a standard finite volume (FV) method applied to uniformly coarsened grids. Across all test cases, the MHFE method demonstrates significantly improved velocity accuracy. Grid convergence analysis revealed consistent monotonic convergence with rates of α ≈ 0.38 for pressure error and α ≈ 0.32 for velocity error. Computational efficiency analysis demonstrated speedup factors of 30–40 x compared to fine-grid simulations while maintaining superior accuracy relative to conventional coarse-grid approaches. Results also demonstrated the ability of the proposed method to accurately compute velocity and pressure fields, as well as streamlines, without distortions or discontinuities, even in complex configurations. By assigning permeability at the hypothetical triangulation level, the method preserved fine-scale heterogeneity and produced a more accurate equivalent permeability field compared to conventional approaches. Additionally, the method imposes no restrictions on the number of neighbors per element, addressing challenges inherent to CCAR grids. These features establish the proposed MHFE method as a robust and efficient tool for advanced upscaling applications in porous media, offering accurate and reliable solutions for complex groundwater systems and geological formations.</div></div>","PeriodicalId":7614,"journal":{"name":"Advances in Water Resources","volume":"205 ","pages":"Article 105089"},"PeriodicalIF":4.2000,"publicationDate":"2025-08-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Mixed hybrid finite element method on CCAR grids in highly heterogeneous porous media\",\"authors\":\"Davood Khoozan , Bahar Firoozabadi\",\"doi\":\"10.1016/j.advwatres.2025.105089\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Upscaling is critical in computational simulations of flow and transport in porous media, bridging fine-scale geological details with coarse-scale computational models, particularly in groundwater modeling and subsurface hydrology. Cartesian cell-based anisotropic refinement (CCAR) grids facilitate this process by adaptively refining grid cells in regions of significant heterogeneity or complex flow dynamics. This study proposes a novel mixed hybrid finite element (MHFE) method for solving flow equations on CCAR grids. The method employs hypothetical triangulation, subdividing each CCAR grid element based on the number of surrounding faces. This enables the elimination of internal face unknowns through flux conservation and pressure continuity rules, enhancing computational efficiency without increasing the degrees of freedom. The proposed method was validated using four models, including synthetic and highly heterogeneous domains with various boundary conditions. The accuracy of the proposed method is evaluated against a fine-grid reference solution and a standard finite volume (FV) method applied to uniformly coarsened grids. Across all test cases, the MHFE method demonstrates significantly improved velocity accuracy. Grid convergence analysis revealed consistent monotonic convergence with rates of α ≈ 0.38 for pressure error and α ≈ 0.32 for velocity error. Computational efficiency analysis demonstrated speedup factors of 30–40 x compared to fine-grid simulations while maintaining superior accuracy relative to conventional coarse-grid approaches. Results also demonstrated the ability of the proposed method to accurately compute velocity and pressure fields, as well as streamlines, without distortions or discontinuities, even in complex configurations. By assigning permeability at the hypothetical triangulation level, the method preserved fine-scale heterogeneity and produced a more accurate equivalent permeability field compared to conventional approaches. Additionally, the method imposes no restrictions on the number of neighbors per element, addressing challenges inherent to CCAR grids. These features establish the proposed MHFE method as a robust and efficient tool for advanced upscaling applications in porous media, offering accurate and reliable solutions for complex groundwater systems and geological formations.</div></div>\",\"PeriodicalId\":7614,\"journal\":{\"name\":\"Advances in Water Resources\",\"volume\":\"205 \",\"pages\":\"Article 105089\"},\"PeriodicalIF\":4.2000,\"publicationDate\":\"2025-08-20\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Advances in Water Resources\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0309170825002039\",\"RegionNum\":2,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"WATER RESOURCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Advances in Water Resources","FirstCategoryId":"93","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0309170825002039","RegionNum":2,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"WATER RESOURCES","Score":null,"Total":0}
Mixed hybrid finite element method on CCAR grids in highly heterogeneous porous media
Upscaling is critical in computational simulations of flow and transport in porous media, bridging fine-scale geological details with coarse-scale computational models, particularly in groundwater modeling and subsurface hydrology. Cartesian cell-based anisotropic refinement (CCAR) grids facilitate this process by adaptively refining grid cells in regions of significant heterogeneity or complex flow dynamics. This study proposes a novel mixed hybrid finite element (MHFE) method for solving flow equations on CCAR grids. The method employs hypothetical triangulation, subdividing each CCAR grid element based on the number of surrounding faces. This enables the elimination of internal face unknowns through flux conservation and pressure continuity rules, enhancing computational efficiency without increasing the degrees of freedom. The proposed method was validated using four models, including synthetic and highly heterogeneous domains with various boundary conditions. The accuracy of the proposed method is evaluated against a fine-grid reference solution and a standard finite volume (FV) method applied to uniformly coarsened grids. Across all test cases, the MHFE method demonstrates significantly improved velocity accuracy. Grid convergence analysis revealed consistent monotonic convergence with rates of α ≈ 0.38 for pressure error and α ≈ 0.32 for velocity error. Computational efficiency analysis demonstrated speedup factors of 30–40 x compared to fine-grid simulations while maintaining superior accuracy relative to conventional coarse-grid approaches. Results also demonstrated the ability of the proposed method to accurately compute velocity and pressure fields, as well as streamlines, without distortions or discontinuities, even in complex configurations. By assigning permeability at the hypothetical triangulation level, the method preserved fine-scale heterogeneity and produced a more accurate equivalent permeability field compared to conventional approaches. Additionally, the method imposes no restrictions on the number of neighbors per element, addressing challenges inherent to CCAR grids. These features establish the proposed MHFE method as a robust and efficient tool for advanced upscaling applications in porous media, offering accurate and reliable solutions for complex groundwater systems and geological formations.
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