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where for simplicity the equality 18
η
=
ζ
is used to relate translational (
η
) and
) viscosities [see, e.g., Eq. (2.30) of Rey (2010)]. Figure 2.16a shows
the computed scalar order parameter
S
and the alignment angle as a function
of De for steady shear of an isotropic solution, for
rotational (
ζ
0.95 and several
U
values; the shapes of
S
curves are consistent with experiments (Gobeaux
et al., 2007; Rey, 2010). Flow-induced birefringence is due to increasing
S
and decreasing
β
=
θ
al
as shear rate increases.
From Figure 2.16a it is seen that the limits of a shear rate (Deborah number)
scan then are
1
50
40
0.8
θ
@U = 2.6
30
0.6
θ
@U = 2
θ
@U = 1
S@U = 1
S@U = 2
S@U = 2.6
20
0.4
10
0.2
0
0
0
5
Deborah number, De
(a)
10
16
50
θ
@
β
= 0.5
S @
β
= 0.5
θ
@
β
= 0.7
S @
β
= 0.7
θ
@
β
= 0.95
S @
β
= 0.95
40
30
20
10
0
01 234 5 67 89 0
Deborah number, De
(b)
Figure 2.16
/4) as a function of De of a
sheared isotropic solution of rods: (a) different concentration of rods (
U
) and
Flow - induced birefringence (
S
>
0, 0
<
θ
al
<
π
β
=
0.95;
increasing
U
increases the initial slope
dS
/
d
De. (b) Same but for
U
=
2 and different
β
values; increasing
β
increases the plateau value of
S
. [Adapted from Rey (2010) .]
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