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dc.creatorDavis, R. O.
dc.creatorBerrill, J. B.
dc.date1998-03-31
dc.identifierhttps://bulletin.nzsee.org.nz/index.php/bnzsee/article/view/553
dc.identifier10.5459/bnzsee.31.1.33-50
dc.descriptionThe Port Island, Kobe downhole records from the Hyogo-ken Nanbu earthquake are analysed to obtain approximate histories of shear stress, shear strain and dissipated energy at a range of depths. Our calculation method relies on measured accelerations in the horizontal plane to produce horizontal components of shear stress and strain using instantaneous modal superposition. A simple dissipated energy-dynamic pore pressure relationship is used to model the development of pore pressure leading to liquefaction. The results show a rapidly developing zone of liquefaction which initiates at a depth of roughly 15 metres in the Port Island reclaimed soils.en-US
dc.formatapplication/pdf
dc.languageeng
dc.publisherNew Zealand Society for Earthquake Engineeringen-US
dc.relationhttps://bulletin.nzsee.org.nz/index.php/bnzsee/article/view/553/530
dc.rightsCopyright (c) 1998 R. O. Davis, J. B. Berrillen-US
dc.rightshttps://creativecommons.org/licenses/by/4.0en-US
dc.sourceBulletin of the New Zealand Society for Earthquake Engineering; Vol 31 No 1 (1998); 33-50en-US
dc.source2324-1543
dc.source1174-9857
dc.titleEnergy dissipation and liquefaction at Port Island, Kobeen-US
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typeArticleen-US


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