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Effect of rock discontinuities on certain rock strength and fracture energy parameters under uniaxial compression

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dc.contributor.author Tsoutrelis, CE en
dc.contributor.author Exadaktylos, GE en
dc.date.accessioned 2014-03-01T01:09:22Z
dc.date.available 2014-03-01T01:09:22Z
dc.date.issued 1993 en
dc.identifier.issn 09603182 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/10937
dc.subject fracture mechanics en
dc.subject Rock discontinuities en
dc.subject scale effect en
dc.subject stability en
dc.subject uniaxial compression en
dc.subject.other discontinuity en
dc.subject.other fracture energy en
dc.subject.other fracture mechanics en
dc.subject.other rock strength en
dc.subject.other stability en
dc.subject.other uniaxial compression en
dc.title Effect of rock discontinuities on certain rock strength and fracture energy parameters under uniaxial compression en
heal.type journalArticle en
heal.identifier.primary 10.1007/BF00423337 en
heal.identifier.secondary http://dx.doi.org/10.1007/BF00423337 en
heal.publicationDate 1993 en
heal.abstract Five series of test blocks of Pendeli marble with artificially created discontinuities of different crack densities (simulating three mutually orthogonal joint sets) were tested in uniaxial compression in order to study the effect of discontinuities on: (a) the compressive strength and the modulus of elasticity, and (b) certain fracture energy parameters expressed by the ratio WA/WV, where WA is the surface energy and WV the volume elastic strain energy. Mathematical relationships are derived similar to those suggested by other authors relating strength parameters to crack densities. Such relationships clearly show a reduction in strength with increased crack density. The experimental results obtained permit the extension of Persson's relation (which refers to ideal intact rock) to the more realistic case of discontinuous rock mass by introducing the appropriate term that takes into consideration the effect of rock mass discontinuities on the energy ratio WA/WV. A comparison between laboratory results and field observations was subsequently carried out assuming the rock mass to behave as a linearly elastic material, obeying the Hoek and Brown failure criterion. This comparison showed that laboratory results can be extended to larger scale. Furthermore, in order to predict the in situ strength and stability of a rock mass in uniaxial compression (which is of major importance in underground excavations) certain concepts are proposed based on laboratory tests, in situ investigations and first principles of linear elastic fracture mechanics. © 1993 Chapman & Hall. en
heal.publisher Kluwer Academic Publishers en
heal.journalName Geotechnical and Geological Engineering en
dc.identifier.doi 10.1007/BF00423337 en
dc.identifier.volume 11 en
dc.identifier.issue 2 en
dc.identifier.spage 81 en
dc.identifier.epage 105 en


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