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Effect of grain shape and angularity on the undrained response of fine sands

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dc.contributor.author Tsomokos, A en
dc.contributor.author Georgiannou, VN en
dc.date.accessioned 2014-03-01T01:33:18Z
dc.date.available 2014-03-01T01:33:18Z
dc.date.issued 2010 en
dc.identifier.issn 0008-3674 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/20366
dc.subject Angularity en
dc.subject Laboratory tests en
dc.subject Sands en
dc.subject Stiffness en
dc.subject Torsional shear en
dc.subject Triaxial compression en
dc.subject.classification Engineering, Geological en
dc.subject.classification Geosciences, Multidisciplinary en
dc.subject.other Angularity en
dc.subject.other Laboratory test en
dc.subject.other Laboratory tests en
dc.subject.other Torsional shear en
dc.subject.other Triaxial compression en
dc.subject.other Compression testing en
dc.subject.other Stiffness en
dc.subject.other Sand en
dc.subject.other compression en
dc.subject.other cylinder en
dc.subject.other fine grained sediment en
dc.subject.other grain size en
dc.subject.other laboratory method en
dc.subject.other sand en
dc.subject.other scanning electron microscopy en
dc.subject.other shear stress en
dc.subject.other stiffness en
dc.subject.other torsion en
dc.subject.other triaxial test en
dc.subject.other void ratio en
dc.title Effect of grain shape and angularity on the undrained response of fine sands en
heal.type journalArticle en
heal.identifier.primary 10.1139/T09-121 en
heal.identifier.secondary http://dx.doi.org/10.1139/T09-121 en
heal.language English en
heal.publicationDate 2010 en
heal.abstract The objective of this paper is to discuss the effect of grain shape and angularity on the undrained behaviour of sands. Four fine to medium (D50 = 0.15-0.29 mm) and uniform sands were examined. These sands have similar and (or) identical grading curves, but differ with respect to the angularity of their grains. Under the electron scanning microscope two sands have rounded grains and the other two have subangular to angular grains. For sands with rounded grains, evidence of undrained behaviour undergoing systematic weakening (shear stress reduction after a transient peak deviator stress) is provided by torsional hollow cylinder tests. However, sands with the same grading curve and void ratio, but angular grains, show stable response with a continuous increase in strength after a transient peak. A small variation in the sand gradation, i.e., D50 = 0.22 ± 0.07 mm, does not appear to alter the pattern of undrained response described earlier, with the angular sand (D50 = 0.15) exhibiting stable response to shear and the rounded sands (D50 = 0.22 and 0.29) having unstable response to shear. The stiffness characteristics of the sands are also presented. Triaxial compression tests were performed to confirm the pattern of response observed under torsional testing. en
heal.publisher NATL RESEARCH COUNCIL CANADA-N R C RESEARCH PRESS en
heal.journalName Canadian Geotechnical Journal en
dc.identifier.doi 10.1139/T09-121 en
dc.identifier.isi ISI:000277476300004 en
dc.identifier.volume 47 en
dc.identifier.issue 5 en
dc.identifier.spage 539 en
dc.identifier.epage 551 en


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