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Lever, D. A., Bradbury, M. H. (1985) Rock–matrix diffusion and its implications for radionuclide migration. Mineralogical Magazine, 49 (351) 245-254 doi:10.1180/minmag.1985.049.351.11

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Reference TypeJournal (article/letter/editorial)
TitleRock–matrix diffusion and its implications for radionuclide migration
JournalMineralogical MagazineISSN0026-461X
AuthorsLever, D. A.Author
Bradbury, M. H.Author
Year1985 (April)Volume49
Issue351
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_49/49-351-245.pdf+
DOIdoi:10.1180/minmag.1985.049.351.11Search in ResearchGate
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Mindat Ref. ID3729Long-form Identifiermindat:1:5:3729:1
GUID0
Full ReferenceLever, D. A., Bradbury, M. H. (1985) Rock–matrix diffusion and its implications for radionuclide migration. Mineralogical Magazine, 49 (351) 245-254 doi:10.1180/minmag.1985.049.351.11
Plain TextLever, D. A., Bradbury, M. H. (1985) Rock–matrix diffusion and its implications for radionuclide migration. Mineralogical Magazine, 49 (351) 245-254 doi:10.1180/minmag.1985.049.351.11
In(1985, April) Mineralogical Magazine Vol. 49 (351) Mineralogical Society
Abstract/NotesAbstractDiffusion into the rock matrix is potentially an important retardation mechanism for nuclides leached from an underground radioactive waste repository in a fractured hard rock. A technique for measuring the intrinsic diffusion coefficient and rock capacity factor is briefly described. Simple solutions to migration model equations are used, together with diffusion results and typical hydrogeological parameters, to estimate the impact of matrix diffusion on radionuclide migration. It is shown that retardation factors in excess of 100 and reductions in the peak concentration by 3–4 orders of magnitude are possible for non-sorbed ions, which would otherwise be carried by the flow and not retarded at all.


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