This article presents a specific experimental setup to study the hydration and dehydration of Callovo-Oxfordian (COx) argillite, which is considered as a possible host rock formation for radioactive nuclear waste at great depth in France. Argillite will swell during hydration and contract during dehydration, which is a key geotechnical process during the excavation and open-drift stages of a nuclear waste repository. Studies show that the partially saturated properties of argillite depend strongly on both water content and mechanical loading. In order to study the coupled hydro-mechanical behaviour of COx argillite, a specific experimental setup was developed. This new system can be used to carry out hydration and dehydration tests under controlled mechanical loading. The developed setup continuously records not only relative humidity, stress and deformation, but also the sample weight. Hydration and dehydration testing carried out on COx argillite confirms the performance of the specific setup.
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30 June 2014
Research Article|
June 09 2014
A specific setup to study hydration and dehydration of COx argillite at applied stresses
D. Yang;
D. Yang
*
State Key Laboratory of Geomechanics and Geotechnical Engineering, IRSM, Chinese Academy of Science, Wuhan, China
†
Laboratoire de Mécanique des Solides, Ecole Polytechnique, Palaiseau, France
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S. Chanchole;
S. Chanchole
†
Laboratoire de Mécanique des Solides, Ecole Polytechnique, Palaiseau, France
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H. Gharbi
H. Gharbi
†
Laboratoire de Mécanique des Solides, Ecole Polytechnique, Palaiseau, France
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Publisher: Emerald Publishing
Received:
March 10 2014
Revision Received:
April 14 2014
Accepted:
May 08 2014
Online ISSN: 2045-2543
ICE Publishing: all rights reserved
2014
Geotechnique Letters (2014) 4 (2): 94–97.
Article history
Received:
March 10 2014
Revision Received:
April 14 2014
Accepted:
May 08 2014
Citation
Yang D, Chanchole S, Gharbi H (2014), "A specific setup to study hydration and dehydration of COx argillite at applied stresses". Geotechnique Letters, Vol. 4 No. 2 pp. 94–97, doi: https://doi.org/10.1680/geolett.14.00017
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