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dc.contributor.author | 今本, 博健 | ja |
dc.contributor.author | 大年, 邦雄 | ja |
dc.contributor.alternative | IMAMOTO, Hirotake | en |
dc.contributor.alternative | OHTOSHI, Kunio | en |
dc.date.accessioned | 2009-02-10T01:49:57Z | - |
dc.date.available | 2009-02-10T01:49:57Z | - |
dc.date.issued | 1979-04-01 | - |
dc.identifier.issn | 0386-412X | - |
dc.identifier.uri | http://hdl.handle.net/2433/70283 | - |
dc.description.abstract | This 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.mimetype | application/pdf | - |
dc.language.iso | jpn | - |
dc.publisher | 京都大学防災研究所 | ja |
dc.publisher.alternative | Disaster Prevention Research Institute, Kyoto University | en |
dc.subject.ndc | 517.1 | - |
dc.subject.ndc | 501.23 | - |
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.alternative | STUDY ON THE CHARACTERISTICS OF OPEN CHANNEL FLOW WITH SUSPENDED LOAD (1) | en |
dc.type | departmental bulletin paper | - |
dc.type.niitype | Departmental Bulletin Paper | - |
dc.identifier.ncid | AN00027784 | - |
dc.identifier.jtitle | 京都大学防災研究所年報. B | ja |
dc.identifier.volume | 22 | - |
dc.identifier.issue | B-2 | - |
dc.identifier.spage | 453 | - |
dc.identifier.epage | 468 | - |
dc.textversion | publisher | - |
dc.sortkey | 28 | - |
dc.relation.url | http://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.html | - |
dcterms.accessRights | open access | - |
dc.identifier.pissn | 0386-412X | - |
dc.identifier.jtitle-alternative | Disaster Prevention Research Institute Annuals. B | en |
出現コレクション: | No.22 B-2 |

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