Published 2005 | Version v1
Miscellaneous

HTO and 36CI- diffusion in Callovo-Oxfordian argilites and Oxfordian limestones

  • 1. CEA Saclay, Lab. de Mesure et Modelisation de la Migration des Radionucleides (L3MR), (DEN/DPC/SECR), 91 - Gif-sur-Yvette (France)
  • 2. Agence Nationale pour la Gestion des Dechets Radioactifs (ANDRA), Service Transfert, Direction Scientifique (DS/TR), 92 - Chatenay Malabry (France)

Description

The Callovo-Oxfordian argillite formation is under investigation as a potential host rock for a high-level radioactive waste repository at the Andra Underground Research Laboratory in Meuse/Haute-Marne (France). The Oxfordian limestone formation (160 m - 417 m) located above the Callovo-Oxfordian formation (417 m - 508 m) may be a potential medium for radionuclides migration. Diffusion is assumed to be the main transport mechanism governing radionuclide migration through argillite and the basis of Oxfordian limestone. The purpose of this study is to quantify their diffusive properties. (authors)

Part of:
Clays in natural and engineered barriers for radioactive waste confinement

Additional details

Publishing Information

Imprint Title
Clays in natural and engineered barriers for radioactive waste confinement
Imprint Pagination
723 p.
Journal Page Range
p. 106-107
Report number
INIS-FR--3949

Conference

Title
2. international meeting clays in natural and engineered barriers for radioactive waste confinement
Dates
14-18 Mar 2005
Place
Tours (France)

Optional Information