Emma Ollivier-Triquet , Benjamin Braconnier , Véronique Gervais-Couplet , Souhail Youssef , Laurent Talon , Daniela Bauer
{"title":"粘滞带的流动和传输:部分饱和度和佩克莱特数对非费克式、渐近前分散的影响","authors":"Emma Ollivier-Triquet , Benjamin Braconnier , Véronique Gervais-Couplet , Souhail Youssef , Laurent Talon , Daniela Bauer","doi":"10.1016/j.advwatres.2024.104774","DOIUrl":null,"url":null,"abstract":"<div><p>Transport phenomena in unsaturated porous media still present an important research topic. In particular, in the context of recent environmental concerns, further understanding of contaminant transport in the partially saturated vadose zone is necessary. However, there is currently a lack of understanding of the relationship between water saturation, in particular the two-phase distribution, and dispersion. This is due to the intricate interactions between the two-phase flow and the porous structure, as well as the complexity of the experimental techniques, which prevents a significant number of configurations from being analysed.</p><p>We explore passive tracer transport in two-dimensional unsaturated porous media via experimental and numerical methods. To this goal, we conduct co-injection experiments to produce two-phase distributions (air/water) at different saturations in a transparent micromodel that mimics the topology of the Bentheimer sandstone. From these experiments, we generate images using multi-scale multiple-point statistics modelling (MPS). Employing the Lattice Boltzmann method, we calculate velocity and concentration fields for both experimental and generated images under saturated and unsaturated conditions. Our results show strong similarities in velocity distributions, good agreement in concentration profiles, and a matching of dispersion characteristics between experimental and MPS-generated images. MPS enables us to create a variety of unsaturated porous media structures with different topologies but similar transport properties. From these images, we analyse transport over a large range of saturations and Peclet numbers. We observe pre-asymptotic non-Fickian transport regimes characterized by a variance increasing with time according to a power law with exponent <span><math><mrow><mi>α</mi><mo>></mo><mn>1</mn></mrow></math></span>. We find that <span><math><mi>α</mi></math></span> increases as saturation decreases, due to enhanced flow heterogeneity, and with higher Peclet numbers. This behaviour is confirmed through large-scale simulations.</p></div>","PeriodicalId":7614,"journal":{"name":"Advances in Water Resources","volume":"191 ","pages":"Article 104774"},"PeriodicalIF":4.0000,"publicationDate":"2024-07-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Flow and transport in the vadose zone: On the impact of partial saturation and Peclet number on non-Fickian, pre-asymptotic dispersion\",\"authors\":\"Emma Ollivier-Triquet , Benjamin Braconnier , Véronique Gervais-Couplet , Souhail Youssef , Laurent Talon , Daniela Bauer\",\"doi\":\"10.1016/j.advwatres.2024.104774\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Transport phenomena in unsaturated porous media still present an important research topic. In particular, in the context of recent environmental concerns, further understanding of contaminant transport in the partially saturated vadose zone is necessary. However, there is currently a lack of understanding of the relationship between water saturation, in particular the two-phase distribution, and dispersion. This is due to the intricate interactions between the two-phase flow and the porous structure, as well as the complexity of the experimental techniques, which prevents a significant number of configurations from being analysed.</p><p>We explore passive tracer transport in two-dimensional unsaturated porous media via experimental and numerical methods. To this goal, we conduct co-injection experiments to produce two-phase distributions (air/water) at different saturations in a transparent micromodel that mimics the topology of the Bentheimer sandstone. From these experiments, we generate images using multi-scale multiple-point statistics modelling (MPS). Employing the Lattice Boltzmann method, we calculate velocity and concentration fields for both experimental and generated images under saturated and unsaturated conditions. Our results show strong similarities in velocity distributions, good agreement in concentration profiles, and a matching of dispersion characteristics between experimental and MPS-generated images. MPS enables us to create a variety of unsaturated porous media structures with different topologies but similar transport properties. From these images, we analyse transport over a large range of saturations and Peclet numbers. We observe pre-asymptotic non-Fickian transport regimes characterized by a variance increasing with time according to a power law with exponent <span><math><mrow><mi>α</mi><mo>></mo><mn>1</mn></mrow></math></span>. We find that <span><math><mi>α</mi></math></span> increases as saturation decreases, due to enhanced flow heterogeneity, and with higher Peclet numbers. 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Flow and transport in the vadose zone: On the impact of partial saturation and Peclet number on non-Fickian, pre-asymptotic dispersion
Transport phenomena in unsaturated porous media still present an important research topic. In particular, in the context of recent environmental concerns, further understanding of contaminant transport in the partially saturated vadose zone is necessary. However, there is currently a lack of understanding of the relationship between water saturation, in particular the two-phase distribution, and dispersion. This is due to the intricate interactions between the two-phase flow and the porous structure, as well as the complexity of the experimental techniques, which prevents a significant number of configurations from being analysed.
We explore passive tracer transport in two-dimensional unsaturated porous media via experimental and numerical methods. To this goal, we conduct co-injection experiments to produce two-phase distributions (air/water) at different saturations in a transparent micromodel that mimics the topology of the Bentheimer sandstone. From these experiments, we generate images using multi-scale multiple-point statistics modelling (MPS). Employing the Lattice Boltzmann method, we calculate velocity and concentration fields for both experimental and generated images under saturated and unsaturated conditions. Our results show strong similarities in velocity distributions, good agreement in concentration profiles, and a matching of dispersion characteristics between experimental and MPS-generated images. MPS enables us to create a variety of unsaturated porous media structures with different topologies but similar transport properties. From these images, we analyse transport over a large range of saturations and Peclet numbers. We observe pre-asymptotic non-Fickian transport regimes characterized by a variance increasing with time according to a power law with exponent . We find that increases as saturation decreases, due to enhanced flow heterogeneity, and with higher Peclet numbers. This behaviour is confirmed through large-scale simulations.
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