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dc.contributor.authorPervukhina, M.
dc.contributor.authorEsteban, L.
dc.contributor.authorLebedev, Maxim
dc.contributor.authorMallants, D.
dc.contributor.authorSchoning, G.
dc.contributor.authorClennell, M.
dc.date.accessioned2017-06-23T02:59:09Z
dc.date.available2017-06-23T02:59:09Z
dc.date.created2017-06-19T03:39:33Z
dc.date.issued2016
dc.identifier.citationPervukhina, M. and Esteban, L. and Lebedev, M. and Mallants, D. and Schoning, G. and Clennell, M. 2016. Permeability of dried and re-saturated shaly samples and accompanying microstructural changes, pp. 3143-3147.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/53252
dc.identifier.doi10.1190/segam2016-13855648.1
dc.description.abstract

© 2016 SEG.Permeability that is of practical importance for both reservoir rocks and seals is often measured in laboratory as in situ borehole measurements are expensive and timeconsuming. A practice of permeability measurements on dry samples, which is common in oil and gas industry, frequently gives results that strongly overestimate permeability measured on water-saturated samples. In this study permeability to gas and to brine were measured on shaly samples with high fraction of swelling clays. Microstructural changes, which accompanying the resaturation process, were photographed using micro computed tomography. We found that significant difference in gas and brine permeability is caused by shrinkage of swelling clay that results in crack opening. As this process is irreversible, any efforts to resolve the true permeability depend on avoiding desiccation of the core samples with swelling clays.

dc.titlePermeability of dried and re-saturated shaly samples and accompanying microstructural changes
dc.typeConference Paper
dcterms.source.volume35
dcterms.source.startPage3143
dcterms.source.endPage3147
dcterms.source.issn1052-3812
dcterms.source.titleSEG Technical Program Expanded Abstracts
dcterms.source.seriesSEG Technical Program Expanded Abstracts
curtin.departmentDepartment of Exploration Geophysics
curtin.accessStatusFulltext not available


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