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dc.contributor.author矢野, 勝正ja
dc.contributor.author大同, 淳之ja
dc.contributor.author角野, 稔ja
dc.contributor.alternativeYANO, Katsumasaen
dc.contributor.alternativeDAIDO, Atsuyukien
dc.contributor.alternativeSUMINO, Minoruen
dc.date.accessioned2009-01-30T04:54:16Z-
dc.date.available2009-01-30T04:54:16Z-
dc.date.issued1969-03-01-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/69683-
dc.description.abstractRecently, there are many disasters caused by abnormal heavy rains in Japan. Suchrams occur mud flow in a steep river in a mountaneous region. But we cannot fullyexplain these complex phenomena at present.In this paper, some experiments on the characteristics of movement of sand wereconducted in the steep slope channel (15 in in length, 40cm in width). It was concludedfrom the results of the experiments that seepage flow plays an important role for themovement of sand in the steep flume, and that the sediment begins to move as mudflow, when the slope of the bed sediment in the flume exceeds in angle of internalfriction of sediment. And some analytical model of characteristics of sand movement asmud flow was proposed.en
dc.format.mimetypeapplication/pdf-
dc.language.isojpn-
dc.publisher京都大学防災研究所ja
dc.publisher.alternativeDisaster Prevention Research Institute, Kyoto Universityen
dc.subject.ndc455.89-
dc.title土石流の発生限界に関する実験ja
dc.title.alternativeEXPERIMENTS ON THE CRITERION FOR OCCURRENCE OF MUD FLOWen
dc.typedepartmental bulletin paper-
dc.type.niitypeDepartmental Bulletin Paper-
dc.identifier.ncidAN00027784-
dc.identifier.jtitle京都大学防災研究所年報. Bja
dc.identifier.volume12-
dc.identifier.issueB-
dc.identifier.spage323-
dc.identifier.epage331-
dc.textversionpublisher-
dc.sortkey27-
dc.relation.urlhttp://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.html-
dcterms.accessRightsopen access-
dc.identifier.pissn0386-412X-
dc.identifier.jtitle-alternativeDisaster Prevention Research Institute Annuals. Ben
出現コレクション:No.12 B

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