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dc.contributor.author今本, 博健ja
dc.contributor.author大年, 邦雄ja
dc.contributor.alternativeIMAMOTO, Hirotakeen
dc.contributor.alternativeOHTOSHI, Kunioen
dc.date.accessioned2009-02-10T01:49:57Z-
dc.date.available2009-02-10T01:49:57Z-
dc.date.issued1979-04-01-
dc.identifier.issn0386-412X-
dc.identifier.urihttp://hdl.handle.net/2433/70283-
dc.description.abstractThis paper deals with characteristics of the resistance coefficient and the vertical distributionsof velocity and concentration of free surface shear flows with suspended sand particles, as a firststage of research program for hydraulics of multi-phase flows.Main results obtained through the experimental investigation are as follows; 1) The resis-tance coefficient of a sediment-laden flow over smooth bed increases with, while that of a flow overrough bed decreases, with increasing of sediment concentration. 2) The vertical distribution ofmean velocity in the outer region is confirmed to be logarithmic for a sediment-laden flow as sameas a clear water flow. 3) It should be noticed that, in a sediment-laden flow over smooth bed, decreasing of velocity near the bed results larger velocity gradient compared to a clear water flow, and that, in a sediment-laden flow over rough bed, increasing of velocity near the free surfaceresults larger velocity gradient. 4) The Karman constant of sediment-laden flow over bothsmooth and rough beds becomes larger than that of a clear water flow. The integral constant of alogarithmic velocity distribution for a flow over smooth bed decreases with increasing of sedimentconcentration, but that for a flow over rough bed increases with increasing of sediment concentra-tion. 5) The characteristics of turbulence of a sediment-laden flow is also changed from thatof a clear water flow, especially in the region near the bed, where the turbulence intensity andthe energy dissipation rate become larger. 6) Non-uniform lateral distribution of sedimentconcentration may be described by the connection with large-scale turbulent motion such as asecondary flow. That is, high and/or low speed streaks are seemed to correspond with low and/orhigh sediment concentration, and these characteristics should be more investigated in details.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.ndc517.1-
dc.subject.ndc501.23-
dc.title固液混相開水路流れの水理特性に関する研究 (1)ja
dc.title.alternativeSTUDY ON THE CHARACTERISTICS OF OPEN CHANNEL FLOW WITH SUSPENDED LOAD (1)en
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.volume22-
dc.identifier.issueB-2-
dc.identifier.spage453-
dc.identifier.epage468-
dc.textversionpublisher-
dc.sortkey28-
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.22 B-2

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