dc.creator | Davis, R. O. | |
dc.creator | Berrill, J. B. | |
dc.date | 1998-03-31 | |
dc.identifier | https://bulletin.nzsee.org.nz/index.php/bnzsee/article/view/553 | |
dc.identifier | 10.5459/bnzsee.31.1.33-50 | |
dc.description | The 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.format | application/pdf | |
dc.language | eng | |
dc.publisher | New Zealand Society for Earthquake Engineering | en-US |
dc.relation | https://bulletin.nzsee.org.nz/index.php/bnzsee/article/view/553/530 | |
dc.rights | Copyright (c) 1998 R. O. Davis, J. B. Berrill | en-US |
dc.rights | https://creativecommons.org/licenses/by/4.0 | en-US |
dc.source | Bulletin of the New Zealand Society for Earthquake Engineering; Vol 31 No 1 (1998); 33-50 | en-US |
dc.source | 2324-1543 | |
dc.source | 1174-9857 | |
dc.title | Energy dissipation and liquefaction at Port Island, Kobe | en-US |
dc.type | info:eu-repo/semantics/article | |
dc.type | info:eu-repo/semantics/publishedVersion | |
dc.type | Article | en-US |