A microstructure insight into the water retention properties of the Callovo-Oxfordian claystone

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Abstract

The effect of changes in suction on the microstructure of the Callovo-Oxfordian claystone along wetting and drying paths was investigated by using mercury intrusion porosimetry. Based on a simplified brick model, the changes of the average thickness of the platelets that constitute the clay matrix (50%) are interpreted as the consequence of the successive adsorption of ordered layers of water molecules along the smectite surfaces, as demonstrated on pure smectites for a long time. This shows the predominant role played by the smectite phase in the overall response of the Callovo-Oxfordian claystone when submitted to suction changes under no stress.

Original languageEnglish
Article number06006
JournalE3S Web of Conferences
Volume9
DOIs
Publication statusPublished - 12 Sept 2016
Externally publishedYes
Event3rd European Conference on Unsaturated Soils, E-UNSAT 2016 - Paris, France
Duration: 12 Sept 201614 Sept 2016

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