Publications des scientifiques de l'IRD

Laine M., Balan Etienne, Allard T., Paineau E., Jeunesse P., Mostafavi M., Robert J. L., Le Caer S. (2017). Reaction mechanisms in swelling clays under ionizing radiation : influence of the water amount and of the nature of the clay mineral. RSC Advances, 7 (1), p. 526-534. ISSN 2046-2069.

Titre du document
Reaction mechanisms in swelling clays under ionizing radiation : influence of the water amount and of the nature of the clay mineral
Année de publication
2017
Type de document
Article référencé dans le Web of Science WOS:000393741900069
Auteurs
Laine M., Balan Etienne, Allard T., Paineau E., Jeunesse P., Mostafavi M., Robert J. L., Le Caer S.
Source
RSC Advances, 2017, 7 (1), p. 526-534 ISSN 2046-2069
We have studied the H-2 production under ionizing radiation of water confined in synthetic saponite and montmorillonite as a function of the relative humidity. The H-2 radiolytic yields in the dry systems are very similar to that measured in a non-swelling clay mineral. They are 2-3 times higher with one water layer in the interlayer space, evidencing very efficient energy transfers and efficient recombination reactions due to a high confinement. With two water layers, the H-2 yields decrease as compared to the previous case, but remain higher than in bulk water, proving that recombination reactions of hydrogen atoms are less efficient. Electron paramagnetic resonance measurements evidence that reactivity changes significantly with the number of water layers. Saponite and montmorillonite give similar results, showing that reactivity is driven by the amount of water and that the details of the clay structure play a less important role. Lastly, the behavior of natural vs. synthetic swelling clays is discussed. The presence of impurities, even in small quantities, significantly alters energy transfers and has a positive implication for the geological nuclear waste management.
Plan de classement
Sciences fondamentales / Techniques d'analyse et de recherche [020] ; Sciences du milieu [021] ; Géologie et formations superficielles [064] ; Economie : secteurs d'activité [096]
Localisation
Fonds IRD [F B010069245]
Identifiant IRD
fdi:010069245
Contact