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Radionuclide migration into natural fracture surfaces of granitic rock

Conference · · Mater. Res. Soc. Symp. Proc.; (United States)
OSTI ID:5875431
The update of cesium on natural fracture surfaces taken from granitic bedrock has been studied as well as the depth penetration into the underlying rock. The fracture minerals usually exhibit good sorptive properties with respect to cesium (with the exception of calcite). The surface coatings do not act as physical diffusion barriers and do not prevent a migration into the underlying rock. A considerable depth penetration into the rock (several mm over a period of three months) was observed. The dominating pathways into the rock matrix were the high-capacity minerals in grains or in microfissures. The calculated diffusivity in the rock matrix was of the order of 10/sup -13/ m/sup 2//s.
Research Organization:
Chalmers Univ. of Technology, Goeteborg, Sweden
OSTI ID:
5875431
Report Number(s):
CONF-821107-Pt.1
Conference Information:
Journal Name: Mater. Res. Soc. Symp. Proc.; (United States) Journal Volume: 15
Country of Publication:
United States
Language:
English

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