Transport in Porous Media最新文献_第8页

Pore-Scale and Upscaled Investigations of Release and Transport of Lithium in Organic-Rich Shales 富有机页岩中锂的释放和迁移的孔隙尺度和放大研究

IF 2.7 3区工程技术

Transport in Porous Media Pub Date : 2024-03-08 DOI: 10.1007/s11242-024-02071-2

Jiahui You, Kyung Jae Lee

{"title":"Pore-Scale and Upscaled Investigations of Release and Transport of Lithium in Organic-Rich Shales","authors":"Jiahui You, Kyung Jae Lee","doi":"10.1007/s11242-024-02071-2","DOIUrl":"10.1007/s11242-024-02071-2","url":null,"abstract":"<div><p>To meet the extensive demand for lithium (Li) for rechargeable batteries, it is crucial to enhance Li production by diversifying its resources. Recent studies have found that produced water from shale reservoirs contains various organic and inorganic components, including a significant amount of Li. In this study, findings from hydrothermal reaction experiments were analyzed to fully understand the release of Li from organic-rich shale rock. Subsequently, numerical algorithms were developed for both pore-scale and continuum-scale models to simulate the long-term behavior of Li in shale brines. The experimental conditions considered four different hydrothermal solutions, including the solutions of KCl, MgCl<sub>2</sub>, CaCl<sub>2</sub>, and NaCl with various concentrations under the temperature of 130 °C, 165 °C, and 200 °C. The release of Li from shale rock into fluid was regarded as a chemical interaction of cation exchange between rock and fluid. The reactive transport pore-scale and upscaled continuum-scale models were developed by coupling the chemical reaction model of Li interaction between rock and fluid. The model was first implemented to investigate the release and transport of Li in the pore scale. Continuum-scale properties, such as effective diffusivity coefficients and Li release rate, were obtained as the field-averaged pore-scale modeling results. These properties were used as the input data for the upscaled continuum-scale simulation. The findings of this study are expected to provide new insight into the production of Li from shale brines by elucidating the release, fate, and transport of Li in subsurface formations.</p></div>","PeriodicalId":804,"journal":{"name":"Transport in Porous Media","volume":"151 4","pages":"813 - 830"},"PeriodicalIF":2.7,"publicationDate":"2024-03-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"140075479","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

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

引用次数: 0

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

引用次数: 0

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}

引用次数: 0

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

引用次数: 0

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

引用次数: 0

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

引用次数: 0

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