What is it about?
This study employs COMSOL software to simulate the upward motion of a single bubble in quiescent water, considering various container dimensions and air bubble sizes. The research reveals a strong agreement between empirical formulas and numerical simulations, emphasizing the precision of COMSOL. Findings include the impact of drag forces on bubble shapes, the formation of vortices during ascent, and the concentration of vorticity within the bubble. The study explores how larger aspect ratios enhance ascent velocities, the influence of container diameter on rising speed, and the effects of gravitational forces. Overall, the research provides valuable insights into bubble dynamics in multiphase flows, benefiting diverse industrial applications and highlighting the utility of computational tools like COMSOL for studying complex phenomena.
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Why is it important?
This study holds significance for industrial applications by providing a thorough examination of bubble dynamics in multiphase flows using COMSOL simulations. The research's validation of computational tools and comprehensive coverage of diverse container dimensions and bubble sizes offer versatile insights applicable across various industrial settings. The findings contribute to a deeper understanding of forces influencing bubble behavior, such as drag forces and gravitational effects, offering potential for process optimization and resource utilization improvements. Seeing vortices and unevenness during bubble ascent also helps us learn more about how fluids move. And the fact that numerical simulations and empirical formulas agree so well with each other backs up theoretical approaches, making it easier to trust established models that predict bubble dynamics in multiphase systems.
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This page is a summary of: Dynamics of single bubble ascension in stagnant liquid: An investigation into multiphase flow effects on hydrodynamic characteristics using computational simulation, Physics of Fluids, December 2023, American Institute of Physics,
DOI: 10.1063/5.0174622.
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