Large-eddy simulation of bubble plume in stratified crossflow

Shuolin Xiao, Chen Peng, and Di Yang
Phys. Rev. Fluids 6, 044613 – Published 29 April 2021

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 (wr=3, 6, 12, and 20cm/s) are considered, and their characteristics under three weak crossflow conditions (Uc=0.5, 1, and 2cm/s) 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 wr (3 and 6cm/s), the plume can form a distinct peeling event that dominates the material transport process. As a result, the mean intrusion layer height ht shows only small variation for these two plume conditions when Uc is increased. In contrast, the plumes with wr=12 and 20cm/s exhibit noticeable decrease of ht (9% and 24%, respectively) when Uc is increased from 0.5 to 2cm/s. Statistical analysis of the streamwise dye flux shows that the decrease of ht with increased Uc for the cases with wr=12 and 20cm/s is mainly due to the crossflow-enhanced mean flux of dye from the rising plume at the low elevation.

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  • Received 8 March 2020
  • Accepted 7 April 2021

DOI:https://doi.org/10.1103/PhysRevFluids.6.044613

©2021 American Physical Society

Physics Subject Headings (PhySH)

Fluid Dynamics

Authors & Affiliations

Shuolin Xiao, Chen Peng, and Di Yang*

  • Department of Mechanical Engineering, University of Houston, Houston, Texas 77204, USA

  • *diyang@uh.edu

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Vol. 6, Iss. 4 — April 2021

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