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Naji, M. |
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Motta, Antonella |
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Aletan, Dirar |
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Mohamed, Tarek |
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Ertürk, Emre |
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Taccardi, Nicola |
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Kononenko, Denys |
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Petrov, R. H. | Madrid |
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Alshaaer, Mazen | Brussels |
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Bih, L. |
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Casati, R. |
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Muller, Hermance |
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Kočí, Jan | Prague |
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Šuljagić, Marija |
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Kalteremidou, Kalliopi-Artemi | Brussels |
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Azam, Siraj |
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Ospanova, Alyiya |
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Blanpain, Bart |
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Ali, M. A. |
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Popa, V. |
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Rančić, M. |
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Ollier, Nadège |
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Azevedo, Nuno Monteiro |
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Landes, Michael |
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Rignanese, Gian-Marco |
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Siitari-Kauppi, Marja
University of Helsinki
in Cooperation with on an Cooperation-Score of 37%
Topics
Publications (5/5 displayed)
- 2022Comparison of the chemo-mechanical behavior of low-pH cement exposed to calcareous water and to argillite pore watercitations
- 2019Mineralogical and microstructural evolution of Portland cement paste/argillite interfaces at 70 degrees C - Considerations for diffusion and porosity propertiescitations
- 2018Imaging connected porosity of crystalline rock by contrast agent-aided X-ray microtomography and scanning electron microscopycitations
- 2016Behavior of Cs in Grimsel granodioritecitations
- 2007Direct simulation of heterogeneous diffusion and inversion procedure applied to an out-diffusion experimentcitations
Places of action
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article
Mineralogical and microstructural evolution of Portland cement paste/argillite interfaces at 70 degrees C - Considerations for diffusion and porosity properties
Abstract
<p>A Portland cement (CEM I) paste was poured onto an argillite disk in diffusion cells with reservoirs filled by alkaline water and argillite pore water. The system evolution was followed over the course of 415 days. The imposed temperature of 70 degrees C affected the mineralogy (precipitation of crystallized C-S-H) and mechanical strength of the interface that became brittle over time. The interface consisted of a calcite/tobermorite/C-A-S-H layer, whose thickness increased at a growth rate of 0.3 mu m/d. Contrary to calcite crusts that formed in immersion tests or when hardened cement was placed in contact with argillite, this layer had no significant effect on the diffusion properties during the one-year duration of the experiment due to its microporous structure and rather small thickness (100 mu m). The argillite mineralogy was altered over 100 mu m. In the cement paste, the total porosity decreased because carbonation was enhanced with temperature, which counterbalanced the effect of decalcification over 400 mu m.</p>