Aaron Peche, Tuong Vi Tran, Theresa Hennig, Vinay Kumar, Robert Kringel, Sven Altfelder
{"title":"低渗透多孔介质中放射性核素扩散输运的时间尺度和溶质突破距离","authors":"Aaron Peche, Tuong Vi Tran, Theresa Hennig, Vinay Kumar, Robert Kringel, Sven Altfelder","doi":"10.1007/s12665-025-12182-8","DOIUrl":null,"url":null,"abstract":"<div><p>The calculation of radionuclide transport in the subsurface is an important part of analyses to evaluate safety of nuclear waste disposal sites. Such calculations often emphasize on the solute breakthrough in space and time. In this context, unfractured low-permeability porous media represent effective radionuclide retention because diffusion becomes the dominant mode of transport. Under such conditions and for safe containment, diffusion is desired to be smallest, optimally in combination with large retardation by e.g. sorption. The present study investigates timescales and solute breakthrough distances for selected radionuclides in low-permeability porous media. The used mathematical model is the solute transport equation incorporating the processes of diffusion, sorption, and decay. Firstly, published physical through-diffusion experiments are recalculated in order to validate the transport parameters using a numerical simulator. Secondly, timescales and distances of radionuclide breakthrough are calculated using an analytical model. The simulation results indicate that solute breakthrough converges at a certain distance as decay becomes the dominant process limiting transport. For example, the migration of <span>\\(^{36}\\)</span>Cl in Opalinus Clay converges at a solute breakthrough distance of approximately 162 m for timescales beyond 10 Mio years. Based on the results, an expression based on the <span>\\(2{\\text {nd}}\\)</span> Damköhler number is introduced and its accuracy is demonstrated. With this simple equation, maximum solute breakthrough distances can be calculated based solely on the input of a dimensionsless number, the effective diffusion coefficient, the effective porosity or capacity factor, and the physical half-life. That expression is accurate (<span>\\(R^2=1.00\\)</span>) for non-sorbing radionuclides acting as inert tracers. For sorbing radionuclides, that equation deviates more from simulation results (<span>\\(R^2=0.77\\)</span>). Results of the present study contribute to long term safety analyses of nuclear waste disposal sites.</p></div>","PeriodicalId":542,"journal":{"name":"Environmental Earth Sciences","volume":"84 10","pages":""},"PeriodicalIF":2.8000,"publicationDate":"2025-05-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s12665-025-12182-8.pdf","citationCount":"0","resultStr":"{\"title\":\"Timescales and solute breakthrough distances of diffusive radionuclide transport in low-permeability porous media\",\"authors\":\"Aaron Peche, Tuong Vi Tran, Theresa Hennig, Vinay Kumar, Robert Kringel, Sven Altfelder\",\"doi\":\"10.1007/s12665-025-12182-8\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>The calculation of radionuclide transport in the subsurface is an important part of analyses to evaluate safety of nuclear waste disposal sites. Such calculations often emphasize on the solute breakthrough in space and time. In this context, unfractured low-permeability porous media represent effective radionuclide retention because diffusion becomes the dominant mode of transport. Under such conditions and for safe containment, diffusion is desired to be smallest, optimally in combination with large retardation by e.g. sorption. The present study investigates timescales and solute breakthrough distances for selected radionuclides in low-permeability porous media. The used mathematical model is the solute transport equation incorporating the processes of diffusion, sorption, and decay. Firstly, published physical through-diffusion experiments are recalculated in order to validate the transport parameters using a numerical simulator. Secondly, timescales and distances of radionuclide breakthrough are calculated using an analytical model. The simulation results indicate that solute breakthrough converges at a certain distance as decay becomes the dominant process limiting transport. For example, the migration of <span>\\\\(^{36}\\\\)</span>Cl in Opalinus Clay converges at a solute breakthrough distance of approximately 162 m for timescales beyond 10 Mio years. Based on the results, an expression based on the <span>\\\\(2{\\\\text {nd}}\\\\)</span> Damköhler number is introduced and its accuracy is demonstrated. With this simple equation, maximum solute breakthrough distances can be calculated based solely on the input of a dimensionsless number, the effective diffusion coefficient, the effective porosity or capacity factor, and the physical half-life. That expression is accurate (<span>\\\\(R^2=1.00\\\\)</span>) for non-sorbing radionuclides acting as inert tracers. For sorbing radionuclides, that equation deviates more from simulation results (<span>\\\\(R^2=0.77\\\\)</span>). 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Timescales and solute breakthrough distances of diffusive radionuclide transport in low-permeability porous media
The calculation of radionuclide transport in the subsurface is an important part of analyses to evaluate safety of nuclear waste disposal sites. Such calculations often emphasize on the solute breakthrough in space and time. In this context, unfractured low-permeability porous media represent effective radionuclide retention because diffusion becomes the dominant mode of transport. Under such conditions and for safe containment, diffusion is desired to be smallest, optimally in combination with large retardation by e.g. sorption. The present study investigates timescales and solute breakthrough distances for selected radionuclides in low-permeability porous media. The used mathematical model is the solute transport equation incorporating the processes of diffusion, sorption, and decay. Firstly, published physical through-diffusion experiments are recalculated in order to validate the transport parameters using a numerical simulator. Secondly, timescales and distances of radionuclide breakthrough are calculated using an analytical model. The simulation results indicate that solute breakthrough converges at a certain distance as decay becomes the dominant process limiting transport. For example, the migration of \(^{36}\)Cl in Opalinus Clay converges at a solute breakthrough distance of approximately 162 m for timescales beyond 10 Mio years. Based on the results, an expression based on the \(2{\text {nd}}\) Damköhler number is introduced and its accuracy is demonstrated. With this simple equation, maximum solute breakthrough distances can be calculated based solely on the input of a dimensionsless number, the effective diffusion coefficient, the effective porosity or capacity factor, and the physical half-life. That expression is accurate (\(R^2=1.00\)) for non-sorbing radionuclides acting as inert tracers. For sorbing radionuclides, that equation deviates more from simulation results (\(R^2=0.77\)). Results of the present study contribute to long term safety analyses of nuclear waste disposal sites.
期刊介绍:
Environmental Earth Sciences is an international multidisciplinary journal concerned with all aspects of interaction between humans, natural resources, ecosystems, special climates or unique geographic zones, and the earth:
Water and soil contamination caused by waste management and disposal practices
Environmental problems associated with transportation by land, air, or water
Geological processes that may impact biosystems or humans
Man-made or naturally occurring geological or hydrological hazards
Environmental problems associated with the recovery of materials from the earth
Environmental problems caused by extraction of minerals, coal, and ores, as well as oil and gas, water and alternative energy sources
Environmental impacts of exploration and recultivation – Environmental impacts of hazardous materials
Management of environmental data and information in data banks and information systems
Dissemination of knowledge on techniques, methods, approaches and experiences to improve and remediate the environment
In pursuit of these topics, the geoscientific disciplines are invited to contribute their knowledge and experience. Major disciplines include: hydrogeology, hydrochemistry, geochemistry, geophysics, engineering geology, remediation science, natural resources management, environmental climatology and biota, environmental geography, soil science and geomicrobiology.