Abstract
AbstractMacroscopic properties of sedimenting suspensions have been studied extensively and can be characterized using the Galileo number (Ga), solid-to-fluid density ratio ($$\pi _p$$
π
p
) and mean solid volume concentration ($${\bar{\phi }}$$
ϕ
¯
). However, the particle–particle and particle–fluid interactions that dictate these macroscopic trends have been challenging to study. We examine the effect of concentration on the structure and dynamics of sedimenting suspensions by performing direct numerical simulation based on an Immersed Boundary Method of monodisperse sedimenting suspensions of spherical particles at fixed $$Ga=144$$
G
a
=
144
, $$\pi _p=1.5$$
π
p
=
1.5
, and concentrations ranging from $${\bar{\phi }}=0.5$$
ϕ
¯
=
0.5
to $${\bar{\phi }}=30\%$$
ϕ
¯
=
30
%
. The corresponding particle terminal Reynolds number for a single settling particle is $$Re_T = 186$$
R
e
T
=
186
. Our simulations reproduce the macroscopic trends observed in experiments and are in good agreement with semi-empirical correlations in literature. From our studies, we observe, first, a change in trend in the mean settling velocities, the dispersive time scales and the structural arrangement of particles in the sedimenting suspension at different concentrations, indicating a gradual transition from a dilute regime ($${\bar{\phi }} \lesssim 2\%$$
ϕ
¯
≲
2
%
) to a dense regime ($${\bar{\phi }} \gtrsim 10\%$$
ϕ
¯
≳
10
%
). Second, we observe the vertical propagation of kinematic waves as fluctuations in the local horizontally-averaged concentration of the sedimenting suspension in the dense regime.
Publisher
Springer Science and Business Media LLC
Subject
Physical and Theoretical Chemistry,General Physics and Astronomy,General Chemical Engineering
Cited by
18 articles.
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