Numerical simulation of reactive processes in an experiment with partially saturated bentonite
Bentonites are preferred materials for use as engineered barriers for high-level nuclear waste repositories. Simulation of geochemical processes in bentonite is therefore important for long-term safety assessment of those repositories. In this work, the porewater chemistry of a bentonite sample subj...
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Published in | Journal of contaminant hydrology Vol. 83; no. 1; pp. 122 - 147 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
Amsterdam
Elsevier B.V
01.02.2006
Elsevier Science |
Subjects | |
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Abstract | Bentonites are preferred materials for use as engineered barriers for high-level nuclear waste repositories. Simulation of geochemical processes in bentonite is therefore important for long-term safety assessment of those repositories. In this work, the porewater chemistry of a bentonite sample subject to simultaneous heating and hydration, as studied by Cuevas et al. [Cuevas, J., Villar, M., Fernández, A., Gómez, P., Martín, P., 1997. Porewaters extracted from compacted bentonite subjected to simultaneous heating and hydration. Applied Geochemistry 12, 473–481.], was assessed with a non-isothermal reactive transport model by coupling the geochemical software PHREEQC2 with the object-oriented FEM simulator GeoSys/RockFlow. Reactive transport modelling includes heat transport, two-phase flow, multicomponent transport and geochemical reactions in the liquid phase, i.e. ion exchange, mineral dissolution/precipitation and equilibrium reactions. Simulations show that the easily soluble minerals in bentonite determine the porewater chemistry. Temperature affects both two-phase flow and geochemical reactions. Porosity change due to dissolution/precipitation is low during the experiment. However, changes of the effective porosity caused by bentonite swelling can be very large. The simulated results agree well with the experimental data. |
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AbstractList | Bentonites are preferred materials for use as engineered barriers for high-level nuclear waste repositories. Simulation of geochemical processes in bentonite is therefore important for long-term safety assessment of those repositories. In this work, the porewater chemistry of a bentonite sample subject to simultaneous heating and hydration, as studied by Cuevas et al. [Cuevas, J., Villar, M., Fernández, A., Gómez, P., Martín, P., 1997. Porewaters extracted from compacted bentonite subjected to simultaneous heating and hydration. Applied Geochemistry 12, 473-481.], was assessed with a non-isothermal reactive transport model by coupling the geochemical software PHREEQC2 with the object-oriented FEM simulator GeoSys/RockFlow. Reactive transport modelling includes heat transport, two-phase flow, multicomponent transport and geochemical reactions in the liquid phase, i.e. ion exchange, mineral dissolution/precipitation and equilibrium reactions. Simulations show that the easily soluble minerals in bentonite determine the porewater chemistry. Temperature affects both two-phase flow and geochemical reactions. Porosity change due to dissolution/precipitation is low during the experiment. However, changes of the effective porosity caused by bentonite swelling can be very large. The simulated results agree well with the experimental data. Bentonites are preferred materials for use as engineered barriers for high-level nuclear waste repositories. Simulation of geochemical processes in bentonite is therefore important for long-term safety assessment of those repositories. In this work, the porewater chemistry of a bentonite sample subject to simultaneous heating and hydration, as studied by Cuevas et al. [Cuevas, J., Villar, M., Fernández, A., Gómez, P., Martín, P., 1997. Porewaters extracted from compacted bentonite subjected to simultaneous heating and hydration. Applied Geochemistry 12, 473-481.], was assessed with a non-isothermal reactive transport model by coupling the geochemical software PHREEQC2 with the object-oriented FEM simulator GeoSys/RockFlow. Reactive transport modelling includes heat transport, two-phase flow, multicomponent transport and geochemical reactions in the liquid phase, i.e. ion exchange, mineral dissolution/precipitation and equilibrium reactions. Simulations show that the easily soluble minerals in bentonite determine the porewater chemistry. Temperature affects both two-phase flow and geochemical reactions. Porosity change due to dissolution/precipitation is low during the experiment. However, changes of the effective porosity caused by bentonite swelling can be very large. The simulated results agree well with the experimental data.Bentonites are preferred materials for use as engineered barriers for high-level nuclear waste repositories. Simulation of geochemical processes in bentonite is therefore important for long-term safety assessment of those repositories. In this work, the porewater chemistry of a bentonite sample subject to simultaneous heating and hydration, as studied by Cuevas et al. [Cuevas, J., Villar, M., Fernández, A., Gómez, P., Martín, P., 1997. Porewaters extracted from compacted bentonite subjected to simultaneous heating and hydration. Applied Geochemistry 12, 473-481.], was assessed with a non-isothermal reactive transport model by coupling the geochemical software PHREEQC2 with the object-oriented FEM simulator GeoSys/RockFlow. Reactive transport modelling includes heat transport, two-phase flow, multicomponent transport and geochemical reactions in the liquid phase, i.e. ion exchange, mineral dissolution/precipitation and equilibrium reactions. Simulations show that the easily soluble minerals in bentonite determine the porewater chemistry. Temperature affects both two-phase flow and geochemical reactions. Porosity change due to dissolution/precipitation is low during the experiment. However, changes of the effective porosity caused by bentonite swelling can be very large. The simulated results agree well with the experimental data. Bentonites are preferred materials for use as engineered barriers for high- level nuclear waste repositories. Simulation of geochemical processes in bentonite is therefore important for long-term safety assessment of those repositories. In this work, the porewater chemistry of a bentonite sample subject to simultaneous heating and hydration, as studied by Cuevas et al. [Cuevas, J., Villar, M., Fernandez, A., Gomez, P., Martin, P., 1997. Porewaters extracted from compacted bentonite subjected to simultaneous heating and hydration. Applied Geochemistry 12, 473-481.], was assessed with a non- isothermal reactive transport model by coupling the geochemical software PHREEQC2 with the object-oriented FEM simulator GeoSys/RockFlow. Reactive transport modelling includes heat transport, two-phase flow, multicomponent transport and geochemical reactions in the liquid phase, i.e. ion exchange, mineral dissolution/precipitation and equilibrium reactions. Simulations show that the easily soluble minerals in bentonite determine the porewater chemistry. Temperature affects both two-phase flow and geochemical reactions. Porosity change due to dissolution/precipitation is low during the experiment. However, changes of the effective porosity caused by bentonite swelling can be very large. The simulated results agree well with the experimental data. |
Author | Shao, Hua Xie, Mingliang Kolditz, Olaf Bauer, Sebastian Nowak, Thomas |
Author_xml | – sequence: 1 givenname: Mingliang surname: Xie fullname: Xie, Mingliang email: mingliang.xie@uni-tuebingen.de organization: Center for Applied Geoscience, Chair of GeoSystemsResearch, University of Tübingen, Sigwartstr. 10. D-72076 Tübingen, Germany – sequence: 2 givenname: Sebastian surname: Bauer fullname: Bauer, Sebastian organization: Center for Applied Geoscience, Chair of GeoSystemsResearch, University of Tübingen, Sigwartstr. 10. D-72076 Tübingen, Germany – sequence: 3 givenname: Olaf surname: Kolditz fullname: Kolditz, Olaf organization: Center for Applied Geoscience, Chair of GeoSystemsResearch, University of Tübingen, Sigwartstr. 10. D-72076 Tübingen, Germany – sequence: 4 givenname: Thomas surname: Nowak fullname: Nowak, Thomas organization: Federal Institute for Geosciences and Natural Resources, Stilleweg 2, D-30655, Hannover, Germany – sequence: 5 givenname: Hua surname: Shao fullname: Shao, Hua organization: Federal Institute for Geosciences and Natural Resources, Stilleweg 2, D-30655, Hannover, Germany |
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Keywords | Bentonite Non-isothermal reactive transport Two-phase flow Numerical modelling Geochemical reaction experimental studies waste disposal ion exchange ground water bentonite pollution radioactive waste precipitation safety pore water temperature clastic rocks models liquid phase porosity dissolution bicarbonate ion swelling transport high-level waste sedimentary rocks sodium two-phase models hydration numerical models porous media |
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Snippet | Bentonites are preferred materials for use as engineered barriers for high-level nuclear waste repositories. Simulation of geochemical processes in bentonite... Bentonites are preferred materials for use as engineered barriers for high- level nuclear waste repositories. Simulation of geochemical processes in bentonite... |
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SubjectTerms | Bentonite Bentonite - chemistry Buffers Chemical Precipitation chemical reactions Computer Simulation Earth sciences Earth, ocean, space Engineering and environment geology. Geothermics Exact sciences and technology Geochemical reaction geochemistry hazardous waste high-level radioactive waste repository Hot Temperature Hydrogeology Hydrology. Hydrogeology Ion Exchange mathematical models Models, Theoretical Non-isothermal reactive transport non-thermal reactive transport Numerical modelling Permeability Pollution, environment geology Porosity Radioactive Waste radionuclides Solubility Two-phase flow waste disposal Waste Management - methods Water Movements |
Title | Numerical simulation of reactive processes in an experiment with partially saturated bentonite |
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