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dc.creatorStephenson, W. R.
dc.date1975-12-31
dc.identifierhttps://bulletin.nzsee.org.nz/index.php/bnzsee/article/view/1195
dc.identifier10.5459/bnzsee.8.4.245-254
dc.descriptionThe concept of directed resonance is put forward, and its occurrence in New Zealand and overseas is documented. It is observed mainly on water-saturated recent alluvium. Analytical procedures for detecting directed resonance effects in earthquake records are outlined. The resonance parameters are shown to be independent of the particular earthquake, and highly dependent on local boundaries of the alluvium. Cellular mode resonant response is suggested to be the mechanism generating directed resonance at individual sites, and is shown to occur for scale models of alluvial deposits. Experimental apparatus which would be needed to unequivocally confirm the earthquake excitation of cellular resonant modes is described in an appendix.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/1195/1162
dc.rightsCopyright (c) 1975 W. R. Stephensonen-US
dc.rightshttps://creativecommons.org/licenses/by/4.0en-US
dc.sourceBulletin of the New Zealand Society for Earthquake Engineering; Vol 8 No 4 (1975); 245-254en-US
dc.source2324-1543
dc.source1174-9857
dc.titleCellular normal modes of alluvium responseen-US
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typeArticleen-US


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