Experimental and Numerical Investigation of 3D Dam-Break Wave Propagation in an Enclosed Domain with Dry and Wet Bottom

被引:17
|
作者
Kocaman, Selahattin [1 ]
Evangelista, Stefania [2 ]
Guzel, Hasan [1 ]
Dal, Kaan [1 ]
Yilmaz, Ada [1 ]
Viccione, Giacomo [3 ]
机构
[1] Iskenderun Tech Univ, Dept Civil Engn, TR-31200 Antakya, Turkey
[2] Univ Cassino & Southern Lazio, Dept Civil & Mech Engn, I-03043 Cassino, FR, Italy
[3] Univ Salerno, Dept Civil Engn, I-84084 Fisciano, SA, Italy
来源
APPLIED SCIENCES-BASEL | 2021年 / 11卷 / 12期
关键词
dam-break; laboratory experiments; CFD; unsteady flow; tailwater; wave front velocity; RANS simulations; SWEs; FLOW-3D; image analysis measurement; FINITE-VOLUME MODEL; INITIAL-STAGES; FLOW; SCHEME; SIMULATIONS; IMPACT; STAGE;
D O I
10.3390/app11125638
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Dam-break flood waves represent a severe threat to people and properties located in downstream regions. Although dam failure has been among the main subjects investigated in academia, little effort has been made toward investigating wave propagation under the influence of tailwater depth. This work presents three-dimensional (3D) numerical simulations of laboratory experiments of dam-breaks with tailwater performed at the Laboratory of Hydraulics of Iskenderun Technical University, Turkey. The dam-break wave was generated by the instantaneous removal of a sluice gate positioned at the center of a transversal wall forming the reservoir. Specifically, in order to understand the influence of tailwater level on wave propagation, three tests were conducted under the conditions of dry and wet downstream bottom with two different tailwater depths, respectively. The present research analyzes the propagation of the positive and negative wave originated by the dam-break, as well as the wave reflection against the channel's downstream closed boundary. Digital image processing was used to track water surface patterns, and ultrasonic sensors were positioned at five different locations along the channel in order to obtain water stage hydrographs. Laboratory measurements were compared against the numerical results obtained through FLOW-3D commercial software, solving the 3D Reynolds-Averaged Navier-Stokes (RANS) with the k-epsilon turbulence model for closure, and Shallow Water Equations (SWEs). The comparison achieved a reasonable agreement with both numerical models, although the RANS showed in general, as expected, a better performance.
引用
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页数:21
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