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dc.creatorĐorđević, Dejana
dc.date.accessioned2019-04-19T14:17:58Z
dc.date.available2019-04-19T14:17:58Z
dc.date.issued2012
dc.identifier.urihttps://grafar.grf.bg.ac.rs/handle/123456789/423
dc.description.abstractThis paper aims at studying the role of difference in bed elevations between the tributary and main canals (Delta z(T)) in 90 degrees confluence under different hydrologic/hydraulic conditions. To do this, 3D finite-volume model is used. Four Delta z(T)/ h(d) values in the range [0.0, 0.5] (where h(d) stands for the flow depth in the main canal at the confluence) and three values of the discharge ratio D-R = Q(MR)/Q(tot) ={0.250, 0.583, 0.750} are considered. It is found that the: 1) increase in Delta z(T) attenuates 3D flow at the confluence and enhances 3D flow in the post-confluence canal, 2) enhanced 3D flow affects the existence, size and position of the recirculation zone (RZ), 3) size of the RZ reduces as Delta z(T) increases, 4) maximal shear is attained in the upper layers when Delta z(T) gt 0 and 5) zone of tau(0,max) reduces and moves to the downstream junction corner as Delta z(T) increases.en
dc.rightsrestrictedAccess
dc.sourceRiver Flow 2012, Vols 1 and 2
dc.titleRole of bed elevation discordance at 90 degrees straight-channel confluencesen
dc.typeconferenceObject
dc.rights.licenseARR
dc.citation.epage1160
dc.citation.other: 1153-1160
dc.citation.spage1153
dc.identifier.rcubhttps://hdl.handle.net/21.15107/rcub_grafar_423
dc.identifier.wos000347871500154
dc.type.versionpublishedVersion


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