Anales AFA - XVI Meeting on Recent Advances of Physics of Fluids and its Applications 52-56
EFECTOS GRAVITATORIOS EN LA RETRACCIÓN DE FILAMENTOS LÍQUIDOS
APOYADOS SOBRE UN PLANO INCLINADO
GRAVITY EFFECTS IN THE RETRACTION OF LIQUID FILAMENTS RESTING ON AN
INCLINED PLANE
P. D. Ravazzoli*1, A. G. González1y J. A. Diez1
1Instituto de Física Arroyo Seco, Universidad Nacional del Centro de la Provincia de Buenos Aires, and
CIFICEN-CONICET-CICPBA, Pinto 399, 7000, Tandil, Argentina.
Recibido: 06/09/2021; Aceptado: 16/11/2021
En este trabajo estudiamos la retracción de filamentos líquidos apoyados sobre sustratos sólidos inclinados en condi-
ciones de mojabilidad parcial. Debido a esto, cada extremo del filamento retrae longitudinalmente dando lugar a la
formación de una región de acumulación de masa (cabeza) cerca del extremo, donde subsecuentemente se desarrolla
un cuello en su parte posterior. Luego, este cuello se rompe formando una gota separada, mientras que el resto del
filamento reinicia la secuencia de formación de cabeza con cuello y su posterior ruptura. En el caso horizontal, este
proceso es simétrico y conduce a un arreglo regular de gotas equiespaciadas. Cuando el sustrato se encuentra inclinado,
la gravedad actúa de manera diferente en cada extremo, modificando la distancia retraída por cada extremo hasta el mo-
mento de la ruptura, como así también la velocidad de retracción y la distancia final entre gotas la cual, además, deja de
ser uniforme. Encontramos que, en el caso del plano inclinado, la distancia máxima que retrae el extremo que recede en
contra (a favor) de la gravedad disminuye (aumenta) respecto del caso horizontal. Este efecto resulta ser un mecanismo
útil para el auto–posicionamiento de las gotas resultantes al final del proceso. Nuestros resultados experimentales, tales
como posiciones de los extremos, perfiles del espesor en el corte longitudinal, etc., son contrastados con simulaciones
numéricas de las ecuaciones de Navier–Stokes, obteniéndose un buen acuerdo. Éste se ha logrado empleando como
condición de contorno en la línea de contacto la relación de Cox–Voinov–Blake (CVB), la cual incluye tanto los efectos
de la hidrodinámica macroscópica como así también de la dinámica molecular.
Palabras Claves: mojabilidad, filamentos, ángulo de contacto.
We study the retraction of liquid filaments resting on inclined solid substrates under partially wetting condition. This
one causes each extreme of the filament to retract and form a region of mass accumulation (head) that subsequently
develops a neck at its rear part. This neck then breaks up into a separate drop, while the rest of the filament restarts the
sequence. In the horizontal case, this process is symmetric and leads to a regular arrangement of evenly spaced drops.
When the substrate is inclined, gravity acts differently at each end, thus modifying the distance retracted by each end,
the retraction speed and the final distance between drops, which also ceases to be uniform. We find that, in the case
of the inclined plane, the maximum distance retracted by the end that recedes against (in favor of) gravity decreases
(increases) with respect to the horizontal case. This effect turns out to be a useful mechanism for the self–positioning
of the resulting drops at the end of the process. Our experimental results, such as end positions, thickness profiles in the
longitudinal section, etc., are contrasted with numerical simulations of the Navier–Stokes equations, obtaining a good
agreement. This is achieved by using in the contact line the boundary condition known as Cox–Voinov–Blake (CVB)
relationship, which includes both the effects of macroscopic hydrodynamics as well as molecular dynamics.
Keywords: wettability, filaments, contact angle.
https://doi.org/10.31527/analesafa.2022.fluidos.52 ISSN 1850-1168 (online)
I. INTRODUCTION
In this work, we are concerned with the retraction and
fragmentation of a long liquid filament sitting on an incli-
ned substrate under partial wetting conditions. As schema-
tically presented in Fig. 1(a), we focus our attention on the
evolution of both extremes of the filament when the subs-
trate inclination angle with respect to the horizontal is α.
Once the liquid thread is placed on the incline, with its axis
along the gravity component parallel to the plane, its ends
start to recede along the longitudinal direction and advance
in the transverse one. This process leads to the formation of
a bulged region, here referred to as head. As a consequen-
* pravazzoli@ifas.exa.unicen.edu.ar
ce of these combined motions a thinner region, called neck,
is developed in the connecting region between the head and
the rest of the filament that rapidly breaks up thus leading to
a sessile drop that separates from the rest of the filament [1].
While the original head becomes a sessile drop, the rest
of the filament repeats this process till a final arrangement
of aligned drops is reached. A main feature of these drops
is that the shape of their footprints is noncircular [2]. For
the horizontal case, these drops are equally distanced [3],
but this is not the case when the substrate is inclined (see
Fig. 1(b)).
The physical mechanisms involved in the evolution of the
head and its retraction in the horizontal case have been pre-
©2022 Anales AFA 52
FIG. 1: (a) Scheme of the liquid filament placed on an inclined
substrate with the axis of the filament along the gravity compo-
nent parallel to the plane. (b) Final drop arrangement after the
complete breakup of a filament of length L =3.36 cm and width
w=0.6mm on a substrate inclined α=12.5. The segments na-
med as Li(i =1,...,7) are the retraction distances travelled by
the contact line to form the drop separated from the remaining fi-
lament: L1, L2and L3(L4, L5, L6and L7) correspond to the uphill
(downhill) extreme.
viously reported [4]. Here, the main goal is to determine the
effects of the component of gravity along the incline and
parallel to the axis of the filament on its dynamic evolution
and the final drops arrangement. We measure the evolution
of the height profiles of the filament in the xz–plane (lon-
gitudinal direction) and from that information we are able
to determine the contact angle at the filament tips, θx, and
their velocities, vcl . When the breakup processes have come
to an end, we measure the distance between drops for both
uphill and downhill extremes.
Our results are contrasted with numerical simulations,
which solve the Navier–Stokes equations with appropria-
te boundary conditions at the contact line. To do so, we
employ a combination between the hydrodynamic model
proposed by Cox [5] and Voinov [6] (CV model) and a
molecular–kinetics one from Blake [7]. This combined mo-
del was first proposed by Petrov [8,9] and more recently
adjusted to the liquid–solid combination used here [4] and
named as CVB model.
II. EXPERIMENTAL RESULTS
We place a liquid filament on an inclined substrate with
the axis of the filament along the gravity component pa-
rallel to the plane. The liquid partially wets the substrate
(glass microscope slide) that was coated with a fluorinated
solution (EGC-1700 of 3M). We focus our interest on the
axial dewetting of the tips of the filament, which is made
of a silicone oil (polydimethylsiloxane, PDMS), with den-
sity ρ=0.97 g/cm3, viscosity µ=21.7 Poise and surface
tension γ=21.0 dyn/cm. The filaments are generated from
a controlled impact of the substrate against a vertical jet
of PDMS, thus obtaining a liquid thread on the substrate
with uniform width and parallel straight contact lines [4].
The whole system is placed on a base inclined α=12.5
and the experiments where perform at room temperature
(a)
(b)
(c)
FIG. 2: Height profiles at the filament extremes for α=0(both
extremes are identical) and α=12.5(uphill and downhill extre-
mes) at different times: (a) t =0s, (b) t =50 s and (c) t =100 s.
(T20C).
The evolution of an inclined filament is similar to that of
a horizontal one. While in that case, the dewetting and brea-
kup mechanism repeats itself until a regular arrangement of
drops is formed, in the inclined plane case, the retraction
distances of the tips of the filament, xf, are different becau-
se of gravity effects (xf(t)0 for t0). Consequently, the
space between the resulting drops also differs. It should be
mentioned that the inclination angle, α, needs to be small
enough so that the formed drops remain static and do not
slide over the substrate leading to drop coalescence [10].
From the lateral observation of the filament evolution (si-
de view) we are able to obtain the height profiles of the head
region at any time. In Fig. 2we show these profiles for both
the horizontal and inclined cases at some selected times. We
firstly observe that the downhill (uphill) tip recedes slower
(faster) for α=12.5than for α=0. From these profiles
we measure the position of the tip, xf, as a function of time,
whose results are shown in Fig. 3. At early times (t<20 s),
the gravity effects are not yet important. For later times, the
case with inclined plane shows that the downhill (uphill) tip
recedes slower (faster) than the horizontal case. This im-
plies that the maximum retraction distance (achieved when
the receding processes stop) becomes smaller (larger) for
the downhill (uphill) extreme.
Ravazzoli et al. / Anales AFA - XVI Meeting on Recent Advances of Physics of Fluids and its Applications 52-56 53
α=0Exp
α=12.5(uphill)Exp
α=12.5(downhill)Exp
α=0Num
α=12.5(uphill)Num
α=12.5(downhill)Num
xf(cm)
0
0,1
0,2
0,3
0,4
0,5
t(s)
0 25 50 75 100 125 150
FIG. 3: Time evolution of the filament tips. The symbols corres-
pond to the experimental data: black circles to α=0, while red
squares and blue triangles to uphill and downhill tips, respectivley,
for α=12.5. The lines correspond to the results of the numerical
simulation: black solid line to α=0, while red and blue dashed
lines to uphill and downhill tips, respectively, for α=12.5.
TABLE 1: Retraction lengths: Distances travelled by the filament
tip up to neck breakup and separated drop formation.
α=12.5
Uphill
L10.412 cm
L20.398 cm
L30.405 cm
Downhill
L40.216 cm
L50.211 cm
L60.208 cm
L70.210 cm
After the complete evolution of the filament, a configu-
ration of separated drops is reached (Fig. 1(b)), so that we
measure the distance, Li, between them. These results are
presented in Table 1. As expected, the distances between
drops at the uphill extreme are larger than the ones for the
horizontal case (0.295 cm), while they are shorter at the
downhill extreme. For a given inclination angle, each extre-
me shows a typical separation distance, within the experi-
mental error. Therefore, the variation of αcan be used as a
method to control the distance between final drops.
III. NUMERICAL SIMULATIONS
Wettability model
In order to perform the numerical simulations we need to
use a suitable boundary condition to describe the contact li-
ne dynamics. As mentioned above, we use a combined mo-
del first proposed by Petrov [8], that includes both the hy-
drodynamic and molecular aspects of the local fluid–solid
interaction (CVB model). The model yields the following
relationship between the contact angle, θ, and the velocity
of the contact line, vcl ,
θ3=arccos3cosθ01
Γsinh1vcl
v0
+9µvcl
γlnac
,(1)
where θ0is the microscopic equilibrium contact angle, ac=
pγ/(ρg)is the capilary length (macroscopic length scale),
and gis gravity. The microscopic length scale, , the cha-
racteristic velocity, v0and the dimensionless parameter, Γ,
are of molecular origin and depend on both the frequency of
molecular displacements at equilibrium and the average dis-
tance between adsortion sites. These parameters were mea-
sured and reported elsewhere [4] for the PDMS and glass
previously coated with the fluorinated solution EGC-1700,
which is the same liquid–substrate configuration used here.
Their values are:
θ0=50.57,v0=6.212 ×107cm/s,
=8.302 ×104ac,Γ=95.455.(2)
In Fig. 4we compare the experimental results of the con-
tact angle at the tip, θx, as function of the contact line velo-
city, vcl with the CVB model. The dots represent the ex-
perimental results for α=0 and α=12.5(uphill and
downhill tips), while the solid line corresponds to Eq. (1)
with the parameters in Eq. (2). The experimental error in θ
is θ=±1, and in vcl it is vcl =±1.1×103cm/s. This
agreement between experiments over an inclined substrate
and the CVB model, confirms that the relationship in Eq. (1)
effectively represents a local phenomenon, non affected by
the presence of gravity.
t
α=0
α=12.5(uphill)
α=12.5(downhill)
Model:CVB
θx()
20
25
30
35
40
45
50
vcl×10-3(cm/s)
−6 −5 −4 −3 −2 −1 0
FIG. 4: Tip contact angle, θx, as function of the contact line velo-
city, vcl . The symbols correspond to the experimental cases, α=0
(black) and α=12.5(red squares for uphill and blue triangles
for downhill). The solid line shows the theoretical model (Eq. 1)
and the arrow indicates the time evolution direction.
Time evolution
We obtain the time evolution of a liquid filament by nu-
merically solving the dimensionless Navier–Stokes equa-
tion,
Rev
t+ (v·
)v=
p+2vzsinα,(3)
where Re =ρacγ/µ2is the Reynolds number. In our ca-
se, we have Re =0.14, so that some slight inertial effects
are considered in the simulations. Besides, we impose the
boundary condition at the contact line as given by Eq. (1)
by using the specific parameters for our liquid–solid confi-
guration (see Eq. (2)). Since we have chosen acas the cha-
racteristic length of the problem, the corresponding Bond
number is Bo =sinα.
The initial shape of the filament is represented by a cylin-
Ravazzoli et al. / Anales AFA - XVI Meeting on Recent Advances of Physics of Fluids and its Applications 52-56 54
FIG. 5: Contour lines of the filament for t =0130 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=0case. 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
technological interest to produce an arrange of self positio-
ning drops with varying spacings.
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