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dc.creatorKeramaris E., Prinos P.en
dc.date.accessioned2023-01-31T08:43:13Z
dc.date.available2023-01-31T08:43:13Z
dc.date.issued2016
dc.identifier10.18869/acadpub.jafm.68.228.24147
dc.identifier.issn17353572
dc.identifier.urihttp://hdl.handle.net/11615/74851
dc.description.abstractIn this study lock-exchange experiments are performed in a tank of rectangular upper cross section and a lower vegetated valley of trapezoidal shape to study the effect of drag resistance, due to vegetation, on gravity currents. Many natural and man-made channels are approximately trapezoidal. For the simulation of the vegetation the bed is covered by flexible grass vegetation (height of vegetation, hv=2.0cm) of different submergence ratio hv/H (hv=height of vegetation, H=water depth). The motion of the gravity current is monitored with a digital video of high definition, the front velocity is measured and the height of the front is captured. Twenty four experiments are performed, twelve inside the trapezoidal section (H/Htr=0.4, 0.6 or 0.8) and twelve over the trapezoidal section (H/Htr=1.2, 1.4 or 1.6). The initial Reynolds number, based on the height of the valley and the reduced gravity, is greater than 10000 for all cases indicating that the gravity currents are turbulent. Results are compared with those of similar experiments without vegetation (Keramaris and Prinos, 2010) and hence the effect of the vegetation drag resistance on the motion of the current is investigated. The main conclusion of this study is that the shape of the tank plays a significant role in the propagation of gravity currents. The presence of trapezoidal increases the velocity of gravity currents in comparison with triangular or orthogonal shape.en
dc.language.isoenen
dc.sourceJournal of Applied Fluid Mechanicsen
dc.source.urihttps://www.scopus.com/inward/record.uri?eid=2-s2.0-84964562194&doi=10.18869%2facadpub.jafm.68.228.24147&partnerID=40&md5=4a7148171e896ea204f4aee820d606a3
dc.subjectIsfahan University of Technologyen
dc.titleGravity currents in a vegetated valley of trapezoidal shapeen
dc.typejournalArticleen


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