2009
DOI: 10.3107/jesss.3.41
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Evolution of a Generic Clay/Cement Interface: First Reactive Transport Calculations Utilizing a Gibbs Energy Minimization Based Approach for Geochemical Calculations

Abstract: The long-term evolution of deep geological repositories for nuclear waste is governed by geochemical processes in conjunction with mass and energy transport. A key role for the design of the multi-barrier system is the knowledge of long term changes at the interfaces between different materials. We investigate the porosity evolution at a generic interface between clay and cement containing materials. We use novel reactive transport codes that couple a Gibbs Energy Minimization (GEM) chemical equilibrium thermo… Show more

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Cited by 8 publications
(3 citation statements)
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“…However, the application of this relationship depends upon specific calibration to the system under study and thus cannot be applied a priori (e.g. Kosakowski et al, 2009). Moreover, it is important for predictive modelling (especially in fractured rocks) to have a better understanding of how porosity/fractures may be occluded due to the precipitation of neoformed minerals.…”
Section: Porosity-permeability Modif|cationmentioning
confidence: 99%
“…However, the application of this relationship depends upon specific calibration to the system under study and thus cannot be applied a priori (e.g. Kosakowski et al, 2009). Moreover, it is important for predictive modelling (especially in fractured rocks) to have a better understanding of how porosity/fractures may be occluded due to the precipitation of neoformed minerals.…”
Section: Porosity-permeability Modif|cationmentioning
confidence: 99%
“…To simplify the model, boric acid interaction with the aggregate was assumed to be negligible and the aggregate in the model was represented by the relatively insoluble mineral rutile (TiO 2 ). Kosakowski, et al (2009) [5] employed a similar approach and used SnO 2 to represent inert components in their cement model. Values of concrete porosity and pore diffusion coefficient were set equal to 0.07 and 1  10 6 cm 2 /s, respectively [4].…”
Section: Reactive Transport Modelingmentioning
confidence: 99%
“…Particularly challenging from the computational point of view are the simulations of systems in which precipitation and/or dissolution reactions led to significant changes of porosity in the media. Strong porosity changes typically observed at interfaces of engineered technical barriers and natural rock formations with different geochemical characteristics, e.g., clay and cement interfaces [ Marty et al , 2009; Kosakowski et al , 2009; De Windt et al , 2004]. Mineral precipitation in aquifers and reservoirs change their transport properties significantly and may lead eventually to complete clogging of the pore space [ Saripalli et al , 2001].…”
Section: Introductionmentioning
confidence: 99%