A slight increase in the Reynolds number then induces a change in the velocities, also at the interface, Equation (
56), giving rise to a small change in the phase velocity of the neutrally-stable perturbations,
; a small change in voltage,
, is needed to counteract the change and bring the system to neutral stability to first order in
R. Note that only the normal stress condition, Equation (
60), is affected by (the change in) voltage.
The first-order-
R boundary and interface conditions are
In Equation (86) both
and
c were expanded. Since
differs from
c by a constant factor, Equation (
68g), we see from Equation (65) that
. Furthermore,
in Equations (86) and (88), since
at the neutral stability to zeroth-
R, Equation (
70a).
The overall solution of Equation (
81) or Equation (82) has the form
where
is a general solution of the homogeneous equation, and
is a particular solution of the inhomogeneous equation. We write the solutions of the two homogeneous equations
where coefficients
and
give the small changes to the corresponding zeroth-order coefficients in Equations (
69a) and (69b). Note that
, since we chose to normalize the entire solution
with respect to
, as it was done with
, Equation (
69a). However,
, since
in Equation (69b), in order to satisfy the boundary and interface conditions Equations (
83)–(88).
Inserting the complete solution
into Equations (
83)–(88) we obtain the system
where
-
are short labels. The system of Equations (
94)-(101) can finally be solved for the nontrivial eigenvalue
. The analytical expression for
and the expanded
-
(
contains
) are given in the
Appendix C.
5.1. Pure shear stress instability to first order in R
It follows from Equation (
A13)
where
is a very complicated real function of the flow parameters
k,
,
h,
,
and of voltage
. The phase velocity
is thus a purely imaginary number and the first-order-
R instability happens for
.
One can investigate the vast parameter space of Equation (
102), but we focus here on a handful of features. We first consider pure shear instability, i.e., the case without a voltage correction,
.
In
Figure 5(a) shown is
, the total change in the phase velocity
c per Equation (65), for two sets of parameters
, differing in
h:
and
. For
there is a critical wavenumber
for which the system is at the neutral stability to first order in
R, analogous to
of
Figure 3, but the trends in the two figures are opposite: in
Figure 5(a) the small wavenumbers,
, are stable and the large ones,
, unstable. For
, a configuration with a thinner bottom liquid, the system is unstable for all
k.
We further notice the orders-of-magnitude smaller values of the first-order corrections. We remember that typical values of
in microfluidics are on the order of 1 (
times smaller than those in
Figure 3, used to showcase the trends). Hence,
. It is perhaps surprising that the shear instability occurs at all. This is the famed Yih’s instability due to viscosity stratification first studied in the limit of small
k, [
14]. We have performed here the analysis for small
R, confirming Yih’s findings as a special case (re-visit
Section 4.1): by inspecting Equation (
A13), noticing the common factor
, and Equation (
70b) for
, we find the proportionality
where
is the pressure-gradient dependent factor in the zero-order-
flow, Equation (33b), and
is the viscosity ratio. It immediately follows from Equation (
103) that the condition
(two equal viscosities) is the neutral stability condition to first-order in
R, i.e.,
for all
k, and there is no instability; since Yih considered pure Couette flow (
) for which
, the instability
is indeed induced for a viscous stratification
.
However, in our more general Couette–Poiseuille flow, the neutral stability for all
k happens also when
, which occurs for a non-zero
forward pressure gradient
and the value
(e.g., for
and
,
yields the neutral stability for all
k). This is the case when the compounded zero-order-
velocity becomes the smooth (unbroken) parabola, Equation (
32). Hence, the viscosity stratification is not the sufficient condition - the generalized mechanism of the instability is the discontinuity in the slope (kink) of the zero-order-
velocity. The criterion does not pertain though to the single
that is independently neutrally stable to first order in
R, as determined by the complicated bracketed term in Equation (
A13).
We make a final remark. We have just seen that
is identically zero for all wavenumbers for
or
, on the account of
being then zero. At the same time we are already at the zeroth-order-
R neutral stability for which
. Hence,
, Equation (
70a), and the denominator of Equation (
57b) becomes zero making the disturbance infinite. In such cases we must employ second order expansion of the kinematic condition, as already noted. Nevertheless, a minute change from
and
brings forth the instability as discussed.
5.2. Onset of EHD Instability to First Order in R
As earlier mentioned, our main interest is the voltage correction
that brings the system to neutral stability to first-order in
R, i.e., how much the voltage
needs to change to compensate for the unstable growth of
due to the shear flow at small
R. The first-order change is found by solving
for
. The analytical solution for
is too complicated for display; we use the closed form of
, Equation (
A13), and work from there to obtain
.
To bring the system to first-order-R neutral EHD stability, we expect the stable regions of , i.e., those wavenumbers for which , to be destabilized by an increasing voltage (of normal E-field), whereas the unstable regions to be stabilized by a decreasing voltage.
This is indeed the case.
Figure 5(b) shows the first-order-
R voltage corrections
vs.
k, corresponding to the two cases of
Figure 5(a). For
, the voltage increases sharply for very stable small wavenumbers,
, to destabilize them, but decreases for
(the correction is negative), to dampen the growth of unstable ones. Note that
is the same in the two panels as it should be, since
. For
, the voltage correction is negative for all
k, in accordance with the all-positive growth rates of the
in panel (a).
Note that we depicted the overall change in the physical voltage,
, in Volts, in order to get the feel for the actual experimental change to first order in
R. Technically,
in the term
of Equation (88) has been expressed as
), where
is the impending voltage of Equation (
78). Like with
, the first-order-
R voltage corrections are six-seven orders of magnitude smaller compared to zeroth-order-
R values, making them challenging if not impossible to measure.
We emphasize that the first-order-
R corrections are found from the coupled EHD system of Equations (
94)-(101). The overall coupling of the first-order
E-field and the shear flow means that the phase velocities
of the pure shear relative to those of the coupled EHD cases will have different extremal points in general. The maximal voltage corrections
in the panel (b) thus do not coincide with the maximal
of (a).
Unlike the impending
voltages, the
corrections depend on the flow parameters
and
R. This is shown in
Figure 6(a), where three graphs are featured for different parameters of the EO pump of
Section 4.3. The pump drags a viscous oil by a thin layer of water:
;
.
Comparing
Figure 6(a) with
Figure 5(b) we first notice that the magnitudes of
are 100 times larger in
Figure 6(a) due to larger damping/growth rates around
, with more pronounced local minima. Second,
is shifted to the left enlarging the range of unstable wavenumbers (i.e., the area of negative voltage corrections). Stability is thus complicated function of parameters: the increase in
relatively destabilizes the system for
by shifting
to the left, and by making the negative voltage corrections for
larger; but at the same time it makes the positive voltage corrections for
also larger, the indication that already stable wavenumbers for
became even more stable for
.
From
Figure 6(a) alone, increase in
h stabilizes the system by shifting
to the right, but, like the increase in
, enhances the magnitudes of the voltage corrections from both sides of
. Increase in adverse pressure (
) shifts
to the right, but dampens the magnitude of the voltage corrections on the two sides.
The voltage corrections
for the largest wavenumber
allowed in the pump (
m,
Section 4.3), are
V,
V, and
V for the three cases
, respectively. Interestingly, if the driving velocity could be increased by a factor 10 to
cm/s (and correspondingly
), the voltage corrections
grow by another factor 100 and come into the experimentally feasible mV range: 69 mV, 1.2 mV and 1.1 mV, respectively.
Finally, the overall trends are best seen in the updated neutral stability diagram: in
Figure 6(b), the overall voltage
vs.
k is shown on log-log scale for a set of parameters for the EO pump. The actual small changes relative to those of
Figure 4 are too small to be seen (full line), and the magnification of
by a factor
(dotted line) and
(dashed line) is imposed to resolve the trends. The lines thus express the (magnified) neutral stability curves up to first order in
R, i.e. the curves for which
.
For and we see how stable regions, i.e., positive voltage corrections, increase with height, protruding into unstable domains for . For the voltage corrections are negative, and so the unstable domain bulges into the stable one.
For
the stable regions are overall diminished (the voltage correction is always negative), as the system is unstable for all
k, like
of
Figure 5. We finally remind that the neutral stability diagrams differ for different flow regimes.
This ends our comprehensive EHD stability analysis to first order in R.