Transport in Porous Media最新文献_第10页

Correction: Effects of Intra-REV Pore Distribution Modeling in the Flow of Non-Newtonian Fluids in Porous Media 更正：非牛顿流体在多孔介质中流动时 REV 内孔隙分布模型的影响

IF 2.7 3区工程技术

Transport in Porous Media Pub Date : 2024-03-08 DOI: 10.1007/s11242-024-02063-2

Allan B. G. Motta, Roney L. Thompson, Mateus P. Schwalbert, Luiz F. L. R. Silva, Jovani L. Favero, Rodrigo A. C. Dias, Raphael J. Leitão

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Correction: Water Upconing in Underground Hydrogen Storage: Sensitivity Analysis to Inform Design of Withdrawal 更正：地下储氢中的水上升：敏感性分析为取水设计提供依据

IF 2.7 3区工程技术

Transport in Porous Media Pub Date : 2024-03-08 DOI: 10.1007/s11242-024-02066-z

Curtis M. Oldenburg, Stefan Finsterle, Robert C. Trautz

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Effects of Hyporheic Exchange and Settlement on the Particle Size Distribution of Colloids 孔隙水交换和沉降对胶体粒径分布的影响

IF 2.7 3区工程技术

Transport in Porous Media Pub Date : 2024-03-06 DOI: 10.1007/s11242-024-02061-4

Zhongtian Zhang, Guangqiu Jin, Hongwu Tang, Wenhui Shao, Qihao Jiang, Xiaorong Zhou, Haiyu Yuan, David Andrew Barry

{"title":"Effects of Hyporheic Exchange and Settlement on the Particle Size Distribution of Colloids","authors":"Zhongtian Zhang, Guangqiu Jin, Hongwu Tang, Wenhui Shao, Qihao Jiang, Xiaorong Zhou, Haiyu Yuan, David Andrew Barry","doi":"10.1007/s11242-024-02061-4","DOIUrl":"10.1007/s11242-024-02061-4","url":null,"abstract":"<div><p>Colloid particle size plays an important role in contaminant adsorption and clogging in the hyporheic zone, but it remains unclear how the particle size changes during the transport of colloids. This study investigated the variation of the particle size of colloids in the overlying water and the effects of settlement and hyporheic exchange via laboratory experiments and numerical simulations with two main factors settlement and hyporheic exchange being considered. The results show that the particle size distribution varies when colloids transport in hyporheic zone, and both settlement and hyporheic exchange are involved in the exchange of colloids between stream and streambed. Large-sized particles are mainly controlled by settlement and advection and thus their concentration in the overlying water decreases more quickly; but small-sized particles are mainly controlled by hyporheic exchange and thus their concentration decreases more slowly, and some particles can be resuspended. The increase of retention coefficient and settling velocity will accelerate the transfer of colloids into the streambed. This study may provide important insights into the variation of the particle size of colloids in the overlying water and the effects of settlement and hyporheic exchange.</p></div>","PeriodicalId":804,"journal":{"name":"Transport in Porous Media","volume":"151 4","pages":"719 - 741"},"PeriodicalIF":2.7,"publicationDate":"2024-03-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140054488","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

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Acknowledgement of Reviewers for 2023 鸣谢 2023 年审查员

IF 2.7 3区工程技术

Transport in Porous Media Pub Date : 2024-03-04 DOI: 10.1007/s11242-024-02057-0

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Pore-Scale Modeling of CO2 Injection Using Density Functional Hydrodynamics 利用密度函数流体力学建立二氧化碳注入的孔隙尺度模型

IF 2.7 3区工程技术

Transport in Porous Media Pub Date : 2024-02-27 DOI: 10.1007/s11242-024-02064-1

Oleg Dinariev, Nikolay Evseev, Alexander Sidorenkov, Leonid Dovgilovich, Mikhail Stukan, Maxim Fedorov

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Correction: A History Matching Study for the FluidFlower Benchmark Project 更正：流体花基准项目历史匹配研究

IF 2.7 3区工程技术

Transport in Porous Media Pub Date : 2024-02-25 DOI: 10.1007/s11242-024-02065-0

Xiaoming Tian, Michiel Wapperom, James Gunning, Samuel Jackson, Andy Wilkins, Chris Green, Jonathan Ennis-King, Denis Voskov

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Estimation of Fracture Permeability from Aperture Distributions for Rough and Partially Cemented Fractures 根据粗糙和部分胶结断裂的孔径分布估算断裂渗透率

IF 2.7 3区工程技术

Transport in Porous Media Pub Date : 2024-02-25 DOI: 10.1007/s11242-024-02059-y

Christopher J. Landry, Maša Prodanović, Zuleima Karpyn, Peter Eichhubl

{"title":"Estimation of Fracture Permeability from Aperture Distributions for Rough and Partially Cemented Fractures","authors":"Christopher J. Landry, Maša Prodanović, Zuleima Karpyn, Peter Eichhubl","doi":"10.1007/s11242-024-02059-y","DOIUrl":"10.1007/s11242-024-02059-y","url":null,"abstract":"<div><p>Natural fractures in subsurface reservoirs are frequently partially cemented with mineral precipitates, and it is unclear if fracture permeability models developed for rough barren fractures are applicable for fractures where roughness originates from cement linings. Here, we use a digital rock physics workflow to quantify the error in fracture permeability predicted by these models for five digitally synthesized rough fractures and four fractures imaged using three-dimensional X-ray computed microtomography. Samples include a rough, artificially-induced barren fracture in sandstone, a cement-lined natural fracture in limestone sampled from outcrop, and two cement-bridged natural fractures in tight-gas sandstones sampled from reservoir core. The images are then processed, segmented, characterized to determine statistical moments of the aperture distribution, and used in lattice Boltzmann model flow simulations. We address complications in measuring aperture distributions from images when the fracture pore space morphology deviates from the typical theoretical description of rough fractures and evaluate three different methods of measuring local aperture. The alternative cubic law using the nominal mean aperture is found to overestimate fracture permeability by upwards of one to two orders of magnitude, while the fracture permeability models using statistical moments of the aperture distribution are far more accurate for both rough barren and partially cemented fractures. We also define an empirical description of the upper and lower bounds of fracture permeability estimates as a function of relative roughness that is applicable to both rough barren and partially cemented fractures.</p></div>","PeriodicalId":804,"journal":{"name":"Transport in Porous Media","volume":"151 4","pages":"689 - 717"},"PeriodicalIF":2.7,"publicationDate":"2024-02-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139969290","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Capillarity-Driven Hydrate Film Formation in Geologic Carbon Storage 地质碳封存中毛细管驱动的水合物薄膜形成

IF 2.7 3区工程技术

Transport in Porous Media Pub Date : 2024-02-21 DOI: 10.1007/s11242-024-02062-3

David E. Fukuyama, Hugh C. Daigle, Wen Song

{"title":"Capillarity-Driven Hydrate Film Formation in Geologic Carbon Storage","authors":"David E. Fukuyama, Hugh C. Daigle, Wen Song","doi":"10.1007/s11242-024-02062-3","DOIUrl":"10.1007/s11242-024-02062-3","url":null,"abstract":"<div><p>Much of the continental margins in the world oceans provide the necessary thermodynamic conditions to store CO<span>(_2)</span> as ice-like hydrates (CO<span>(_2cdot)</span>6 H<span>(_2)</span>O). While resistant to buoyant migration and leakage, the fundamental growth mechanisms that control the injection, capacity, and security of CO<span>(_2)</span> hydrates stored in the seafloor remain unresolved. Extensive field and laboratory testing give rise to conflicting views on the kinetics and growth configurations of hydrates, where mechanistic models reconciling the formation of hydrates observed in nature remain missing. This work elucidates a fundamental pore-scale reactive transport mechanism that underpins the rate and morphology of hydrate formation. We reveal a previously unrecognized mode of hydrate formation in porous seafloor sediments, hydrate film growth via reaction-imbibition, where superhydrophilic hydrate crystallites (<span>(theta sim 0^circ)</span>) formed at water–CO<span>(_2)</span> interfaces create a secondary microporous medium (<span>(sim)</span> 10 to 100 nm pores) within lithologic sediment pores (<span>(sim)</span> 10 to 100 <span>(mu)</span>m pores) to promote further hydrate growth. Unlike past diffusion-controlled models, we show that spontaneous water imbibition into the hydrate micropores establishes rapidly new water–CO<span>(_2)</span> interfaces (i.e., hydrate formation surfaces) via capillary-driven convection and is the dominant mechanism for supplying water to the hydrate formation interface.</p></div>","PeriodicalId":804,"journal":{"name":"Transport in Porous Media","volume":"151 4","pages":"743 - 752"},"PeriodicalIF":2.7,"publicationDate":"2024-02-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139925584","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Semi-analytical Model to Predict Dynamic Capillary Pressure–Saturation Relationship for Flows in Heterogeneous Porous Media 预测异质多孔介质中流动的动态毛细管压力-饱和度关系的半分析模型

IF 2.7 3区工程技术

Transport in Porous Media Pub Date : 2024-02-20 DOI: 10.1007/s11242-024-02058-z

Harris Sajjad Rabbani, Saideep Pavuluri

{"title":"Semi-analytical Model to Predict Dynamic Capillary Pressure–Saturation Relationship for Flows in Heterogeneous Porous Media","authors":"Harris Sajjad Rabbani, Saideep Pavuluri","doi":"10.1007/s11242-024-02058-z","DOIUrl":"10.1007/s11242-024-02058-z","url":null,"abstract":"<div><p>The capillary pressure defines pressure difference between non-wetting and wetting fluids. The capillary pressure is part of the flow governing equations, and its definition can have a profound impact on the nature of fluids displacement in a multiphase flow environment. Conventionally, capillary pressure–saturation relationships are determined under equilibrium conditions which signify that all the fluid–fluid interfaces that exist at the pore scale maintain a static configuration at a certain instant in time. However, there exist experimental and numerical evidences that state that the dynamic nature of fluid flows indeed plays a prominent role in defining the trends of the capillary pressure–saturation relationships. In this paper, we develop a first of a kind semi-analytical model to predict the capillary pressure–saturation curves during drainage displacement by integrating the dynamics of fluid flow based on fundamental laws of fluid mechanics. The proposed semi-analytical model can potentially be incorporated into existing multiphase flow simulators to rapidly compute the capillary pressure at various saturations of the flow medium under dynamic flow conditions. The presented semi-analytical model has been validated against experimental and numerical data sets available in the literature at various flow conditions and considering different sets of fluid properties. We noticed a satisfactory match of the results predicted by the proposed semi-analytical model against the literature data. After performing a holistic sensitivity analysis, we notice that the properties of the porous medium, and the fluid–solid interactions play a significant role in defining the trends of the capillary pressure–saturation curves.</p></div>","PeriodicalId":804,"journal":{"name":"Transport in Porous Media","volume":"151 4","pages":"665 - 687"},"PeriodicalIF":2.7,"publicationDate":"2024-02-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s11242-024-02058-z.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139925247","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Complementary Mass Transport Investigations in Open-Cell Foams: Full-Field Computational Fluid Dynamics Simulation with Random-Walk Microscopic Particle Tracking and Methane Nuclear Magnetic Resonance Displacement Measurements 开孔泡沫中的互补质量传输研究：全场计算流体力学模拟与随机漫步微观粒子跟踪和甲烷核磁共振位移测量

IF 2.7 3区工程技术

Transport in Porous Media Pub Date : 2024-02-16 DOI: 10.1007/s11242-023-02045-w

Mehrdad Sadeghi, Andreas Brix, Sebastian Trunk, Georg R. Pesch, Hannsjörg Freund, Jorg Thöming

{"title":"Complementary Mass Transport Investigations in Open-Cell Foams: Full-Field Computational Fluid Dynamics Simulation with Random-Walk Microscopic Particle Tracking and Methane Nuclear Magnetic Resonance Displacement Measurements","authors":"Mehrdad Sadeghi, Andreas Brix, Sebastian Trunk, Georg R. Pesch, Hannsjörg Freund, Jorg Thöming","doi":"10.1007/s11242-023-02045-w","DOIUrl":"10.1007/s11242-023-02045-w","url":null,"abstract":"<div><p>Numerical simulation can provide detailed understanding of mass transport within complex structures. For this purpose, numerical tools are required that can resolve the complex morphology and consider the contribution of both convection and diffusion. Solving the Navier–Stokes equations alone, however, neglects self<b>-</b>diffusion. This influences the simulated displacement distribution of flow especially in porous media at low Péclet numbers (Pe < 16) and in near-wall regions where diffusion is the dominant mechanism. To address this problem, this study uses μCT-based computational fluid dynamics (CFD) simulations in OpenFOAM coupled with the random-walk particle tracking (PT) module <i>disTrackFoam</i> and cross-validated experimentally using pulsed-field gradient (PFG) nuclear magnetic resonance (NMR) measurements of gas flow within open-cell foams (OCFs). The results of the multi-scale simulations—with a resolution of 130–190 µm—and experimental PFG NMR data are compared in terms of diffusion propagators, which are microscopic displacement distributions of gas flows in OCFs during certain observation times. Four different flow rates with Péclet numbers in the range of 0.7–16 are studied in the laminar flow regime within 10 and 20 PPI OCFs, and axial dispersion coefficients were calculated. Cross-validation of PFG NMR measurements and CFD-PT simulations revealed a very good matching with integral differences below 0.04%, underpinning the capability of both complementary methods for multi-scale transport analysis.</p></div>","PeriodicalId":804,"journal":{"name":"Transport in Porous Media","volume":"151 4","pages":"645 - 664"},"PeriodicalIF":2.7,"publicationDate":"2024-02-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s11242-023-02045-w.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139772669","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0