Flow structure of unconfined turbidity currents interacting with an obstacle

被引:19
|
作者
Wilson, Richard I. [1 ]
Friedrich, Heide [2 ]
Stevens, Craig [3 ,4 ]
机构
[1] Tonkin & Taylor Ltd, Water Engn, Auckland, New Zealand
[2] Univ Auckland, Dept Civil & Environm Engn, Auckland, New Zealand
[3] Natl Inst Water & Atmospher Res, Wellington, New Zealand
[4] Univ Auckland, Dept Phys, Auckland, New Zealand
关键词
Unconfinement; Obstacle; Turbidity current; Turbulence; Mixing; GRAVITY-CURRENT FLOWS; TURBULENCE STRUCTURE; VELOCITY; ENTRAINMENT; DEPOSITS; EARTHQUAKE; CHANNEL; BREAKS; SALINE;
D O I
10.1007/s10652-018-9631-7
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Driven by a growing importance to engineered structures, investigating the flow characteristics of turbidity currents interacting with a basal obstruction has become popular over the last three decades. However, research has focused on confined studies or numerical simulations, whereas in situ turbidity currents are typically unconfined. The present study investigates experimentally the velocity and turbulence structure of an unconfined turbidity current, in the immediate regions surrounding a rectangular obstacle. Initial density of the current, and substrate condition is varied. Through a novel technique of installing ultrasonic probes within the obstacle, the presence of a velocity recirculation region immediately upstream and downstream of the obstacle is revealed and confirmed with high-resolution imagery. This was found to be comparable to previous confined studies, suggesting that stream-wise velocity profile structure is somewhat independent of confinement. The obstacle was found to reduce velocity and turbulence intensity maxima downstream of the obstacle when compared with unobstructed tests.
引用
收藏
页码:1571 / 1594
页数:24
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