Hostname: page-component-586b7cd67f-gb8f7 Total loading time: 0 Render date: 2024-11-25T17:51:49.110Z Has data issue: false hasContentIssue false

Factors Influencing Mass Diffusion in Bentonite and Mixtures of Bentonite and Sand

Published online by Cambridge University Press:  25 February 2011

S.C.H. Cheung
Affiliation:
Atomic Energy of Canada Limited, Whiteshell Nuclear Research Establishment, Pinawa, Manitoba, ROE ILO, Canada
D.W. Oscarson
Affiliation:
Atomic Energy of Canada Limited, Whiteshell Nuclear Research Establishment, Pinawa, Manitoba, ROE ILO, Canada
R.S. Lopez
Affiliation:
Atomic Energy of Canada Limited, Whiteshell Nuclear Research Establishment, Pinawa, Manitoba, ROE ILO, Canada
Get access

Abstract

A model, based on the relative volumes of surface and interstitial water in soil, has been developed to study the effective mass diffusion coefficient in bentonite and mixtures of bentonite and sand. The results show that, when the surface water layer is fully developed to a thickness of 0.25 nm, the theoretical effective mass diffusion coefficient decreases with increasing dry density andbentonite content in a mixture of bentonite and sand. The development of surface water depends on the initial water content, the conversion of interstitial water to surface water, and the dry density. When the surface water layer is not fully developed, the effective mass diffusion coefficientdoes not necessarily decrease as the dry density increases.

Considering the magnitude of measured mass diffusion coefficients in bentonite compacted to a dry density of 1.75 Mg/m], the model indicates that in this system there is significant conversion of interstitial to surface water. This suggests that mass diffusion coefficients in compacted bentonite are mainly influenced by the relative volumes of interstitial and surface water.

Type
Research Article
Copyright
Copyright © Materials Research Society 1984

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

1. Boulton, J. (Ed.), Management of Radioactive Fuel Wastes: The Canadian Disposal Program, Atomic Energy of Canada Limited Report, AECL-6314 (1978).Google Scholar
2. Bird, G.W. and Cameron, D.J., Vault Sealing Research for the Canadian Nuclear Fuel Waste Management Program, Atomic Energy of Canada Limited Technical Record*, TR-145 (1982).Google Scholar
3. Lai, T.M. and Mortland, M.M., “Cationic-Diffusion in Clay Minerals I. Homogeneous and Heterogeneous Systems,” Soil Sci. Soc. Amer. Proc. 32 (1), 5661 (1968).CrossRefGoogle Scholar
4. Yong, R.N. and Warkentin, B.P., Introduction to Soil Behaviour (Macmillan, New York 1966).Google Scholar
5. Frape, S.K. and Fritz, P., A Preliminary Report on the Occurrence and Geochemistry of Saline Groundwaters on the Canadian Shield, Atomic Energy of Canada Limited Technical Record*, TR-136 (1981).Google Scholar
6. Neretnieks, I., Transport of Oxidants and Radionuclides through a Clay Barrier, KBS Teknisk Rapport, KBD-YT-79, Karnbranslesakerhet, Stockholm (1978).Google Scholar
7. Manheim, F.T., “The Diffusion of Ions in Unconsolidated Sediments,” Earth Planet. Sci. Lett. 9, 307309 (1970).CrossRefGoogle Scholar
8. Eriksen, T., Jacobsson, A. and Pusch, R., Ion Diffusion through Highly Compacted Bentonite, KBS Teknisk Rapport, KBS-TR-81-06, karnbranslesakrhet, Stockholm (1981).Google Scholar