Environmental Engineering Reference
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random motion of particles in shear that occurs even in the absence of concentration
gradient and leads to zero net drift of particles. While tracer diffusion does not affect
ˆ
, it governs how one particle species mixes with the other in bidensity suspensions,
resulting in the flux of individual species:
ˆ i
ˆ
d 2
4
=− ʳ
J tracer , i
D tr (ˆ)ˆ
,
(4.6)
where D tr (ˆ)
is the tracer diffusivity and dictates the extent of mixing in our model.
In the limit of dilute suspensions, [ 11 , 13 ] proposed the empirical expression D tr =
ˆ
2
2. For large concentrations, numerical simulations and experiments [ 23 ] suggest
that the tracer diffusivity becomes constant beyond a value
/
ˆ tr
0
.
4. Therefore, we
1
2
tr }
use the expression: D tr (ˆ) =
.
Combining Eqs. ( 4.4 )-( 4.6 ) yields the total flux of the i th species, J i ,
2 min
{ ˆ
J grav , i + ˆ i
ˆ
J i
=
J drift +
J tracer , i ,
(4.7)
=
J grav +
and the total flux J of both species simply corresponds to J
J drift . Notably,
tracer diffusion drops out of the total particle flux (i.e. J tracer , 1 +
0),
justifying its neglect in modelling monodisperse slurries [ 2 , 15 , 16 , 19 ]. In addition,
Brownian diffusion is not included in particle fluxes by assuming a large Péclet
number, or Pe
J tracer , 2
=
d 2
= ʳ
/
D
1, where D is the solvent diffusivity.
4.2.1 Thin Film Approximations and Equilibrium Theory
A thin film geometry [ 18 ] gives us the following dimensionless variables:
J x
ʴ
J z
u
H 2
d 2 U 0
1
H
1
U 0
w
ʴ
J
(
x
,
z
) =
x
,
z
) ,
u
=
,
,
=
,
,
H
μ l U 0
μ
μ l ,
= ˁ i ˁ l
ˁ l
p
=
p
,
μ =
ˁ s , i
,
where H and L are the characteristic film thickness and axial length scale, respec-
tively, and U 0
H 2 g sin
ʱ/ʽ l . Hats denoting the dimensionless quantities will be
subsequently dropped for brevity. In the thin film limit of
=
ʴ
H
/
L
1, the
momentum equation in the axial direction reduces to
˃ =− (
1
+ ˁ s , 1 ˆ 1 + ˁ s , 2 ˆ 2 ),
(4.8)
where
z is the dimensionless shear stress, and the prime denotes
the derivative with respect to z . In addition, we assume
˃ = μ(ˆ)∂
u
/∂
2
ʴ (
d
/
H
)
1, which
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