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Migration in a Single Fracture in Granitic Rock

Published online by Cambridge University Press:  25 February 2011

Harald Abelin ,
Jard Gidlund ,
Luis Moreno  and
Ivars Neretnieks
Harald Abelin
Affiliation:
Department of Chemical Engineering Royal Institute of TechnologyS-100 44 Stockholm, Sweden
Jard Gidlund
Affiliation:
Department of Chemical Engineering Royal Institute of TechnologyS-100 44 Stockholm, Sweden
Luis Moreno
Affiliation:
Department of Chemical Engineering Royal Institute of TechnologyS-100 44 Stockholm, Sweden
Ivars Neretnieks
Affiliation:
Department of Chemical Engineering Royal Institute of TechnologyS-100 44 Stockholm, Sweden
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Abstract

An in situ experiment to study migration in a single fracture in granitic rock has been performed. Both sorbing and nonsorbing tracers have been used. Results from a tracer run with a nonsorbing tracer (Uranine) are presented. The breakthrough curves have been explored with a model which takes into account hydrodynamic dispersion as well as diffusion into the rock matrix. Diffusivities and porosities of the rock matrix measured in the laboratory are used to interpret the field data. A short description of the experimental design is given. This investigation is a part of the STRIPA PROJECT phase I.

Type
Research Article
Information
MRS Online Proceedings Library (OPL) , Volume 26: Symposium D – Scientific Basis for Nuclear Waste Management VII , 1983 , 239
Copyright
Copyright © Materials Research Society 1984

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References

REFERENCES

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5. Moreno, L., Neretnieks, I.: Evaluation of some tracer tests in the granitic rock at Finnsjön, KBS Technical Report 83-38 (1983).Google Scholar