scholarly journals Residual streaming flows in buoyancy-driven cross-shore exchange

2021 ◽  
Vol 920 ◽  
Author(s):  
W. Coenen ◽  
A.L. Sánchez ◽  
R. Félez ◽  
K.A. Davis ◽  
G. Pawlak
Keyword(s):  

Abstract

Physics ◽  
2021 ◽  
Vol 3 (4) ◽  
pp. 1046-1050
Author(s):  
Yuri E. Litvinenko

Electromagnetic expulsion acts on a body suspended in a conducting fluid or plasma, which is subject to the influence of electric and magnetic fields. Physically, the effect is a magnetohydrodynamic analogue of the buoyancy (Archimedean) force, which is caused by the nonequal electric conductivities inside and outside the body. It is suggested that electromagnetic expulsion can drive the observed plasma counter-streaming flows in solar filaments. Exact analytical solutions and scaling arguments for a characteristic plasma flow speed are reviewed, and their applicability in the limit of large magnetic Reynolds numbers, relevant in the solar corona, is discussed.


Author(s):  
Kouki Onitsuka ◽  
Juichiro Akiyama ◽  
Yohei Iiguni ◽  
Daisuke Kiuchi ◽  
Noriaki Kawara

In Japanese rivers, there are many river constructions, i.e., dams, weirs, drops, for the purpose of flood control. Fishways are river constructions which facilitate migration of fish past dams and weirs. There are a lot of fishway types such as pool-and-weir type, stream type, operation type and so on (see Nakamura, 1995). The pool-and-weir fishway is typical type in Japanese rivers. There are three types of flow regimes in pool-and-weir fishways such as a plunging flow, streaming flow and intermixed flow of plunging and streaming flows. Rajaratnam et al. (1988) proposed a prediction formula of these flow regimes. However, this formula has no physical meaning. Further the accuracy of formula is not high. In this study, the criterion formula, which can predict the flow regime in the pool-and-weir fishway, is suggested semi-theoretically. The experiments were conducted with changing the aspect ratio and discharge in the pool-and-weir fishway. The water surface profiles were measured with a point gauge and also two components velocities were measured with a 2-D electromagnetic current meter. A new criterion formula, which is able to predict the flow formation, is proposed.


PLoS ONE ◽  
2013 ◽  
Vol 8 (5) ◽  
pp. e65089 ◽  
Author(s):  
Paulo Branco ◽  
José M. Santos ◽  
Christos Katopodis ◽  
António Pinheiro ◽  
Maria T. Ferreira

2007 ◽  
Vol 122 (5) ◽  
pp. 3004
Author(s):  
Charlotte W. Kotas ◽  
Peter H. Rogers ◽  
Minami Yoda

2004 ◽  
Vol 9 (6) ◽  
pp. 517-532 ◽  
Author(s):  
Luigi A. Grieco ◽  
Saverio Mascolo

2017 ◽  
Vol 819 ◽  
pp. 285-310 ◽  
Author(s):  
Nicolas Périnet ◽  
Pablo Gutiérrez ◽  
Héctor Urra ◽  
Nicolás Mujica ◽  
Leonardo Gordillo

Wave patterns in the Faraday instability have been studied for decades. Besides the rich wave dynamics observed at the interface, Faraday waves hide elusive flow patterns in the bulk – streaming patterns – which have not been studied experimentally. The streaming patterns are responsible for a net circulation in the flow, which is reminiscent of the circulation in convection cells. In this article, we analyse these streaming flows by conducting experiments in a Faraday-wave set-up using particle image velocimetry. To visualise the flows, we perform stroboscopic measurements to both generate trajectory maps and probe the streaming velocity field. We identify three types of patterns and experimentally show that identical Faraday waves can mask streaming patterns that are qualitatively very different. Next, we consider a three-dimensional model for streaming flows in quasi-inviscid fluids, whose key is the complex coupling occurring at all of the viscous boundary layers. This coupling yields modified boundary conditions in a three-dimensional Navier–Stokes formulation of the streaming flow. Numerical simulations based on this framework show reasonably good agreement, both qualitative and quantitative, with the velocity fields of our experiments. The model highlights the relevance of three-dimensional effects in the streaming patterns. Our simulations also reveal that the variety of streaming patterns is deeply linked to the boundary condition at the top interface, which may be strongly affected by the presence of contaminants.


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