Effects of Excavation Damage on the Physical Properties of Rock Matrix

dc.contributorAalto-yliopistofi
dc.contributorAalto Universityen
dc.contributor.authorKiuru, R.en_US
dc.contributor.authorJacobsson, L.en_US
dc.contributor.authorKirály, D.en_US
dc.contributor.authorSuikkanen, J.en_US
dc.contributor.departmentDepartment of Civil Engineeringen
dc.contributor.groupauthorMineral Based Materials and Mechanicsen
dc.contributor.organizationRISE Bioeconomyen_US
dc.contributor.organizationSom System Kft.en_US
dc.contributor.organizationPosiva Oyen_US
dc.date.accessioned2021-09-29T10:00:29Z
dc.date.available2021-09-29T10:00:29Z
dc.date.issued2021-09-06en_US
dc.descriptionFunding Information: The views expressed are those of the authors and do not necessarily reflect those of Posiva Oy. This research is based on work funded by Posiva Oy. This research was funded by the Academy of Finland, grant number 319798. Publisher Copyright: © Published under licence by IOP Publishing Ltd.
dc.description.abstractPosiva Oy has conducted investigations into excavation damage, including comprehensive laboratory testing of physical properties of rock specimens from excavation damaged rock mass. Laboratory testing was conducted on drill core specimens extracted from the excavated surface of a tunnel located at approximately 345 m depth in Olkiluoto, Finland. A total of 141 drill core specimens of three main rock types, a structurally isotropic coarse-grained pegmatoid (PGR) and structurally anisotropic veined gneiss (VGN) and diatexitic gneiss (DGN), were subjected to petrophysical testing, rock mechanics testing and petrographic analyses. Results from the various tests were subjected to rigorous statistical analysis in order to reveal the effects excavation damage has on the physical properties of the rock mass. Results of the study revealed changes that are credited to excavation damage in resistivity, S-wave velocity and various elastic properties of the rock specimens. Effects of excavation damage and the depth of the excavation damaged zone seem to be different to gneiss compared to pegmatoid. On microscopic level, the extent of excavation damaged zone appears to be 0.2 - 0.4 m depending on the measured property. This means that the deeper excavation damaged layer observed by geophysical surveys may be caused by larger scale fractures.en
dc.description.versionPeer revieweden
dc.format.extent7
dc.format.mimetypeapplication/pdfen_US
dc.identifier.citationKiuru, R, Jacobsson, L, Király, D & Suikkanen, J 2021, 'Effects of Excavation Damage on the Physical Properties of Rock Matrix', IOP Conference Series: Earth and Environmental Science, vol. 833, no. 1, 012020. https://doi.org/10.1088/1755-1315/833/1/012020en
dc.identifier.doi10.1088/1755-1315/833/1/012020en_US
dc.identifier.issn1755-1307
dc.identifier.issn1755-1315
dc.identifier.otherPURE UUID: db361261-bc1d-4d7e-bf5b-d0bd2d89a839en_US
dc.identifier.otherPURE ITEMURL: https://research.aalto.fi/en/publications/db361261-bc1d-4d7e-bf5b-d0bd2d89a839en_US
dc.identifier.otherPURE FILEURL: https://research.aalto.fi/files/67744312/Kiuru_2021_IOP_Conf._Ser._Earth_Environ._Sci._833_012020.pdf
dc.identifier.urihttps://aaltodoc.aalto.fi/handle/123456789/110199
dc.identifier.urnURN:NBN:fi:aalto-202109299399
dc.language.isoenen
dc.publisherInstitute of Physics Publishing
dc.relation.fundinginfoThe views expressed are those of the authors and do not necessarily reflect those of Posiva Oy. This research is based on work funded by Posiva Oy. This research was funded by the Academy of Finland, grant number 319798.
dc.relation.ispartofseriesIOP Conference Series: Earth and Environmental Scienceen
dc.relation.ispartofseriesVolume 833, issue 1en
dc.rightsopenAccessen
dc.titleEffects of Excavation Damage on the Physical Properties of Rock Matrixen
dc.typeA4 Artikkeli konferenssijulkaisussafi
dc.type.versionpublishedVersion

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