Onset of motion of a partly hidden cylinder in a laminar shear flow

被引:26
|
作者
Martino, R. [1 ]
Paterson, A. [2 ]
Piva, M. [1 ]
机构
[1] Univ Buenos Aires, Fac Ingn, Grp Medios Porosos, RA-1063 Buenos Aires, DF, Argentina
[2] Univ Buenos Aires, Fac Ingn, Dept Hidraul, RA-1127 Buenos Aires, DF, Argentina
来源
PHYSICAL REVIEW E | 2009年 / 79卷 / 03期
关键词
channel flow; external flows; laminar flow; mechanical contact; shear flow; SEDIMENT TRANSPORT; INCIPIENT MOTION; BED; PARTICLES; VELOCITY; EROSION; WAVES;
D O I
10.1103/PhysRevE.79.036315
中图分类号
O35 [流体力学]; O53 [等离子体物理学];
学科分类号
070204 ; 080103 ; 080704 ;
摘要
In this paper, the onset of motion of an isolated cylinder partially exposed to a shear flow is experimentally investigated. The experiments are performed in a small narrow channel which provides a vertical shear layer flow whose sizes correspond with the channel width. The bottom of the channel is smooth except in the test zone, at long distance from the inlet, where the cylinder is placed with its principal axis perpendicularly directed to the main flow. The geometry of the channel bottom at the test zone is such that the cylinder is partially buried and presents different expositions to the incident flow. In this way, the geometrical constraints imposed by the sediment bed on a single particle in a natural sediment transport situation are reproduced in an idealized context. The results are interpreted in terms of the relation between the particle mobility parameter at the critical condition and the here defined particle burial degree with respect to the bed geometrical constraints beta. We emphasize the role played by this burial degree that is dependent on the particle exposure to the incident flow E and the resistance to the motion by mechanical contacts with its surroundings given by the so-called static pivot angle phi.
引用
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页数:9
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