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Volumes 72-83 (2023)
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Volume 83
Pages 1-258 (December 2023)
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Volume 82
Pages 1-204 (November 2023)
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Volume 81
Pages 1-188 (October 2023)
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Volume 80
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Volume 79
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Volume 78
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Volume 77
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Volume 76
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Volume 75
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Volume 74
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Volume 73
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Volume 72
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Volume 83
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Volumes 60-71 (2022)
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Volume 71
Pages 1-108 (December 2022)
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Volume 70
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Volume 69
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Volume 68
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Volume 67
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Volume 66
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Volume 65
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Volume 64
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Volume 63
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Volume 62
Pages 1-104 (March 2022)
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Volume 61
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Volume 60
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Volume 71
- Volumes 54-59 (2021)
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- Volume 1 (2003)
• Effect of particle density on clustering is studied using simulations.
• Very dilute suspension is allowed to settle at Reynolds number more than 250.
• In mixture, larger density particles dominated the settling characteristics.
• Physics behind the studied anomalies is explained using the vortical structures.
Dilute suspension of particles with same density and size develops clusters when settle at high Reynolds number ( 250). It is due to particles entrapment in the wakes produced by upstream particles. In this work, this phenomenon is studied for suspension having particles with different densities by numerical simulations. The particle-fluid interactions are modelled using immersed boundary method and inter-particle collisions are modelled using discrete element method. In simulations, settling Reynolds number is always kept above 250 and the suspension solid volume fraction is nearly 0.1 percent. Two particle density ratios (i.e. density of heavy particles to lighter particles) equal to 4:1 and 2:1 and particles with same density are studied. For each density ratio, the percentage volume fraction of each particle density is nearly varied from 0.8 to 0.2. Settling characteristics such as microstructures of settling particle, average settling velocity and velocity fluctuations of settling particles are studied. Simulations show that for different density particles settling characteristics of suspension is largely dominated by heavy particles. At the end of paper, the underlying physics is explained for the anomalies observed in simulation.