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SrI2 Diffusion Experiment in Granite From Underground Research Laboratory in Manitoba, Canada

Published online by Cambridge University Press:  10 February 2011

T. Yamaguchi ,
S. Nakayama  and
T.T. Vandergraaf
T. Yamaguchi
Affiliation:
Japan Atomic Energy Research Institute, Tokai, Ibaraki, 319-11Japan
S. Nakayama
Affiliation:
Japan Atomic Energy Research Institute, Tokai, Ibaraki, 319-11Japan
T.T. Vandergraaf
Affiliation:
Whiteshell Laboratories, AECL, Pinawa Manitoba, Canada, ROE ILO
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Extract

It is important to quantify the diffusion of radionuclides into pores in rock and to understand the diffusion mechanism to evaluate the migration of radionuclides in deep geological formations. The diffusivity of ions into the rock matrix is usually estimated using a theory for the diffusion in porous material, in which a proportional relationship exists between the effective diffusivity in rock and the diffusivity in the bulk of the solution. In this study, diffision of nonsorbing Γ and sorbing Sr2+ was observed simultaneously and the results were compared.

Type
Research Article
Information
MRS Online Proceedings Library (OPL) , Volume 506: Symposium – Scientific Basis for Nuclear Waste Management XXI , 1997 , 1091
Copyright
Copyright © Materials Research Society 1998

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References

REFERENCES

[1] Nishiyama, K. et al. , Mining. Geol. 40, 323 (1990).Google Scholar
[2] Crank, J.: The Mathematics of Diffusion, 2d ed., p.342, Oxford Univ. Press, New York (1975).Google Scholar
[3] Ohlsson, Y. and Neretnieks, I.: SKB-TR 95-12 (1995 ).Google Scholar