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Olivier Bildstein

Researcher at Commissariat à l'énergie atomique et aux énergies alternatives

Publications -  49
Citations -  1542

Olivier Bildstein is an academic researcher from Commissariat à l'énergie atomique et aux énergies alternatives. The author has contributed to research in topics: Waste disposal & Corrosion. The author has an hindex of 22, co-authored 47 publications receiving 1340 citations. Previous affiliations of Olivier Bildstein include Institut Français & University of Montpellier.

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Hydration sequence of swelling clays: evolutions of specific surface area and hydration energy.

TL;DR: The results confirm experimentally that the hydration of Li- and Na-montmorillonite is mainly a cation-controlled process, in contrast with the Hydration of Cs samples in which the cation contribution to hydration is negligible, as it has been demonstrated using electrostatic calculations or conductivity measurements.
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Modelling iron–clay interactions in deep geological disposal conditions

TL;DR: In this paper, the reaction-transport code CRUNCH is used to investigate the iron-clay interactions at 50°C over a period of 10,000 years, which are the conditions considered here to represent the mean temperature value and the expected timescale for the corrosion stage.
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Coupled reaction-flow modeling of diagenetic changes in reservoir permeability, porosity and mineral compositions

TL;DR: DIAPHORE as mentioned in this paper is a two-phase, finite-volume, reaction-transport simulator, which couples kinetically-controlled dissolution and precipitation of minerals with equilibrium reactions of chemical species in the water phase.
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Experimental and modeling study of geochemical reactivity between clayey caprocks and CO2 in geological storage conditions

TL;DR: In this article, the authors present experimental and modeling results regarding the geochemical reactivity of two caprock samples under CO 2 storage conditions: a rock sample from the Chinle formation in Moab (Utah-USA) and a sample of the Comblanchie n formation in Charmotte (Paris Basin-France).
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On the cation dependence of interlamellar and interparticular water and swelling in smectite clays.

TL;DR: It is found that the interlayer space is never completely filled by water at the studied relative humidity values for all samples except for the Cs sample, which implies that the swelling observed in the mesopores for Li and Na samples is due to an osmotic swelling.