FIG. 5: Contour lines of the filament for t =0−130 s every
∆t=10 s as given by the numerical simulation. At t =130 s the
downhill neck is formed and it is close to its breakup. At t =0the
filament height is h0=0.02 cm, its width is w =0.6cm, and its
length is L =3cm.
drical cap with contact angle θ0along its sides. The extre-
mes of the filament are shaped as halves of ellipsoidal caps
with a contact angle at the tip, θx=20◦. The ellipsoidal
and cylindrical caps are matched with smooth continuity of
thickness and contact angle.
Top views of the time evolution of the filament are shown
in Fig. 5. As observed in the experiments, the simulations
also yield that the downhill extreme recedes a shorter dis-
tance than the uphill one, till they break up and form the co-
rresponding drops. Since the numerical method used here
(moving mesh) does not allow for separations of the fluid
into several domains, the code is unable to describe the
complete breakup flow at the necks. Nevertheless, it is able
to simulate the flow up to moments near the breakup, and its
results remain useful for the purposes of the present work.
However, the retraction distances and the retraction velo-
cities are smaller than those measured in the experiments.
As shown in Fig. 3, the numerical simulation underestima-
tes the displacement of the tip in the α=0◦case. This dif-
ference changes when the substrate is inclined. It becomes
larger for the uphill extreme and smaller for the downhill
one. In the latter case, the differences are practically negli-
gible.
In Fig. 6we compare the experimental and numerical
height profiles for an inclined filament. In order to point
out the shape differences, the experimental data have been
shifted till the position of the experimental and numerical
contact lines are coincident. It can be seen that for t=50 s
(Fig. 6(a)) the main differences are behind the heads of both
extremes, in the neck regions, where the experimental profi-
les are a bit lower than the numerical ones. This departure is
more pronounced for t=100 s in the downhill neck, while
the numerical head height is smaller than the experimental
one at the uphill head. We believe that the differences at the
uphill head and neck are related with the slower retraction
of the tip as observed in Fig. 3.
IV. CONCLUSION
The experiments on the retraction of liquid filaments over
an inclined substrate show that the presence of a longitudi-
nal component of gravity produces an increase (decrease) of
0.0 0.5 1.0 1.5 2.0 2.5 3.0
0.00
0.01
0.02
0.03
0.04
x
zExperiment
Numerical Solution
0.0 0.5 1.0 1.5 2.0 2.5 3.0
0.00
0.01
0.02
0.03
0.04
x
zExperiment
Numerical Solution
FIG. 6: Comparison between experimental and numerical height
profiles. The gray dashed line corresponds to the initial numerical
state, the solid blue line to the numerical solution and the red dots
to the experimental profile. In order to compare the shape of the
profile, the experimental data have been shifted so that the position
of the tip is the same as in the numerical case. (a) t =50 s and (b)
t=100 s.
the retraction distance for the uphill (downhill) extreme ne-
cessary to produce each separated droplet. Moreover, as the
breakup process repeats itself at each new filament extre-
me, we find that these retraction distances remain constant
for all drops formed in both the uphill and downill portions
of the initial filament (see Table 1).
It is interesting to point out that we confirmed the lo-
cal behavior of the CVB wettability model. As we show
in Fig. 4the relationship vcl (θ)measured for the uphill and
downhill extremes of the filament is in good agreement with
the model parametrized for the spreading of a circular drop
over a horizontal substrate.
By using the CVB model in the simulations we found
a good agreement with the experiments for early times res-
pect to the breakup time (say t<30 s, see Fig. 3). For α=0
and later times we observe that the simulation predicts lo-
wer retraction velocities of the extremes. This is due to the
fact that the numerical method is unable to model comple-
te breakups (or fluid domain separation), and thus it leaves
a very thin filament connecting the almost separated drop
from the remaining filament. The inclusion of a longitudi-
nal volume force (gravity component parallel to the incline)
for α>0 generates an additional downslope flow inside
the filament such that it decreases (increases) the volume of
the uphill (downhill) head due to the flow along the neck,
which remains spuriously not broken for longer times due
to the numerical flaw. This effect explains the even lower
retraction velocity of the uphill extreme, and the compensa-
tion of this velocity at the downhill extreme, which is now
increased respect to the α=0 case.
We consider that a complete understanding of the who-
le phenomenology still requires a more detailed physical
model which, to our knowledge, is still unavailable in the
literature. This type of flows constitute a simple method of
Ravazzoli et al. / Anales AFA - XVI Meeting on Recent Advances of Physics of Fluids and its Applications 52-56 55