Abstract
Characteristics and material transport of a bubble-driven plume in stably stratified water with uniform crossflow are studied using an Eulerian-Eulerian large-eddy simulation model. Four laboratory-scale plume conditions with different bubble rise velocities (, 6, 12, and ) are considered, and their characteristics under three weak crossflow conditions (, 1, and ) are studied. The interaction between the rising bubbles and the stratified water generates a double-plume structure, consisting of a rising plume of bubble/water mixture and a falling plume of dense water peeled from the rising plume due to the stratification effect. The presence of crossflow forces the rising plume to incline and causes the falling plume to form on the downstream side (with respect to the crossflow direction) of the rising plume, resulting in reduced contact area between the two plumes. Consequently, the turbulent mixing of the vertical momentum between the rising and falling plumes is reduced, causing the magnitude of the vertical velocity in both plumes to increase when the crossflow velocity is increased. The material transport from the plume to the horizontal intrusion layer (traced using dye) also exhibits strong dependence on the crossflow velocity. Faster crossflow results in narrower lateral extension and wider vertical extension of the intrusion layer due to the interaction between the peeling process and the crossflow. For cases with the two smaller (3 and ), the plume can form a distinct peeling event that dominates the material transport process. As a result, the mean intrusion layer height shows only small variation for these two plume conditions when is increased. In contrast, the plumes with and exhibit noticeable decrease of ( and , respectively) when is increased from to . Statistical analysis of the streamwise dye flux shows that the decrease of with increased for the cases with and is mainly due to the crossflow-enhanced mean flux of dye from the rising plume at the low elevation.
21 More- Received 8 March 2020
- Accepted 7 April 2021
DOI:https://doi.org/10.1103/PhysRevFluids.6.044613
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