4.7 Article

Particle-resolved simulations of local liquid spreading in packed beds: Effect of wettability at varying particle size

Journal

PHYSICS OF FLUIDS
Volume 34, Issue 6, Pages -

Publisher

AIP Publishing
DOI: 10.1063/5.0096157

Keywords

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Funding

  1. University Grants Commission (UGC), New Delhi, India
  2. Deutscher Akademischer Austauschdienst German (DAAD), Bonn, Germany

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This study investigates the dynamics of liquid spreading in a randomly packed three-dimensional bed using simulations and numerical values. Inertial force plays a significant role in promoting lateral liquid spreading at the beginning, while capillary force dominates as the inertial force diminishes. A regime map is proposed to show the relationship between different forces and the resultant liquid spreading.
Packed beds are widely used to perform solid-catalyzed gas-liquid reactions, e.g., hydrodesulfurization, oxidation, and hydrogenation. The overall performance of packed beds is often governed by local liquid spreading. In the present work, the dynamics of liquid spreading through a randomly packed three-dimensional bed is investigated using particle-resolved volume-of-fluid simulations. The effect of particle surface-wettability ( theta) at varying particle diameter ( d(p)) on the relative contributions of forces governing the dynamics of liquid spreading is analyzed using the Ohnesorge (Oh(I)), Weber ( We(I)), and AB(I) (proposed in the present work) numbers. With the help of simulated liquid spreading and these numbers, we show that the contribution of inertial force is significant at the beginning of liquid spreading irrespective of theta as well as d(p) and promotes lateral liquid spreading (AB(I) > 1, We(I) > 1). Once the dominance of inertial force diminishes, the capillary force leads to a substantial increase in the lateral spreading (AB(I) > 1, We(I) < 1). In the final stages, the gravitational force dominates restricting the lateral liquid spreading (AB(I) < 1). Furthermore, we have proposed a regime map constructed using AB(I) and We(I), which provides a relationship between different forces and the resultant liquid spreading at breakthrough. We also show that the dominance of capillary force (AB(I) > 1, We(I )< 1) results in the highest lateral spreading, whereas the flow dominated by inertial (AB(I) > 1, We(I) > 1) and gravitational force ( AB(I) (sic) 1) leads to intermediate and least lateral liquid spreading, respectively.

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