TY - GEN
T1 - Submerged-flow dynamics of granular media in a rotating drum
AU - King, Hubert
AU - Chaikin, Paul
AU - Ertas, Deniz
AU - Kushnick, Arnold
AU - Meier, Steven W.
AU - Zhou, Fuping
PY - 2009
Y1 - 2009
N2 - The dynamics of granular flows are often influenced by viscous interstitial fluids such as water. The majority of granular flow experiments address dry granular flow. However, we now extend such studies to include fluids having viscosities from 1 to 4 mPa s, allowing a direct comparison to the dry case. Using direct grain imaging and particle image velocimetry techniques, we show that varying fluid properties such as density and viscosity changes the dynamics of the flowing layer. At a fixed rotation rate, the dynamic tilt angle and the flow depth increases with fluid viscosity; the most dramatic incremental change occurring between the dry case and the liquid case with 1 mPa s fluid. To better understand the inter-grain interactions governing this behavior, we have performed DEM simulations of the rotatingdrum system, using an inter-grain squeeze force to approximate the fluid effects. While dry flow profiles and trends in the macro-flow behavior as a function of viscosity are reproduced well by these simulations, the magnitude of the incremental fluid effects are somewhat smaller than observed experimentally. The discrepancy may be due to neglected fluid-drag effects and/or improper scaling of grain and drum size between experiments and the model.
AB - The dynamics of granular flows are often influenced by viscous interstitial fluids such as water. The majority of granular flow experiments address dry granular flow. However, we now extend such studies to include fluids having viscosities from 1 to 4 mPa s, allowing a direct comparison to the dry case. Using direct grain imaging and particle image velocimetry techniques, we show that varying fluid properties such as density and viscosity changes the dynamics of the flowing layer. At a fixed rotation rate, the dynamic tilt angle and the flow depth increases with fluid viscosity; the most dramatic incremental change occurring between the dry case and the liquid case with 1 mPa s fluid. To better understand the inter-grain interactions governing this behavior, we have performed DEM simulations of the rotatingdrum system, using an inter-grain squeeze force to approximate the fluid effects. While dry flow profiles and trends in the macro-flow behavior as a function of viscosity are reproduced well by these simulations, the magnitude of the incremental fluid effects are somewhat smaller than observed experimentally. The discrepancy may be due to neglected fluid-drag effects and/or improper scaling of grain and drum size between experiments and the model.
KW - Discrete element modeling
KW - Granular flow
KW - Particle tracking velocimetry
KW - Submerged granular flow
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U2 - 10.1063/1.3179819
DO - 10.1063/1.3179819
M3 - Conference contribution
AN - SCOPUS:70450199050
SN - 9780735406827
T3 - AIP Conference Proceedings
SP - 1031
EP - 1034
BT - Powders and Grains 2009 - Proceedings of the 6th International Conference on Micromechanics of Granular Media
T2 - 6th International Conference on Micromechanics of Granular Media, Powders and Grains 2009
Y2 - 13 July 2009 through 17 July 2009
ER -