Prediction of particles deposition in a dilute quasi-steady gravity current by Lagrangian markers: effect of shear-induced lift force
Autor: | Ali Koohandaz, Ehsan Khavasi, Arameh Eyvazian, Hamid Yousefi |
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Jazyk: | angličtina |
Rok vydání: | 2020 |
Předmět: |
Physics
Multidisciplinary Velocity gradient 0208 environmental biotechnology Flow (psychology) lcsh:R lcsh:Medicine 02 engineering and technology Mechanics Sedimentation 01 natural sciences Article 010305 fluids & plasmas 020801 environmental engineering Vortex Gravity current Environmental sciences Shear (sheet metal) Physics::Fluid Dynamics Obstacle 0103 physical sciences lcsh:Q Civil engineering lcsh:Science Particle deposition |
Zdroj: | Scientific Reports, Vol 10, Iss 1, Pp 1-17 (2020) Scientific Reports |
ISSN: | 2045-2322 |
Popis: | A gravity current in a channel at the presence of a triangular obstacle was investigated using LES simulation and the Eulerian approach. The Saffman–Mei equation was also applied to examine the effect of shear-induced lift force on particle deposition. To this end, particles were considered as Lagrangian markers and injected into gravity current. It is important to keep in mind that the interaction between the gravity current and particles was treated as a one-way coupling. The results show that shear-induced lift force prevents particles to deposit at the entrance of channel, where the velocity gradient is high. Furthermore, a reduction in the rate of sediment deposition can be seen again in the vicinity of obstacle due to high velocity gradient. The important result is that the shear-induced lift force has an important role in the cases with considerable velocity gradient in quasi-steady flows and this force can affect the pattern of sedimentation over time. Q criterion is utilized to depict the vortical structures of flow. Vortical structures with larger diameter, that indicate stronger vortexes, has been seen in various sections of channel, especially in the region near the obstacle due to the presence of obstacle. |
Databáze: | OpenAIRE |
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