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Numerical Simulation of the Evolution of Viscous Rotating Drops

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Rotating Drops

Marco A. Fontelos1, Víctor García-Garrido1and Ultano Kindelán2

1Instituto de Ciencias Matemáticas (ICMAT, CSIC-UAM-UC3M-UCM), Madrid, Spain. 2Dept. de Matemática Aplicada y Métodos Informáticos, UPM, Madrid, Spain.

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1 Introduction

2 Numerical Method (BEM)

3 Numerical results

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Introduction

Background

Studies concerning the evolution of rotating drops date back to the original experiments of J. Plateau in 1843.

Computation of equilibrium shapes for this problem was initiated by Poincaré in 1885. Two families of solutions, axisymmetric shapes and 2-fold shapes, could be obtained.

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Brown & Scriven (1980) determined branches of solutions where the axial symmetry of the drop is broken and drops present a 2-fold, 3-fold or in general n-fold symmetry.

The drops with 2-fold symmetry can be observed, for instance, when a drop that is rolling over an inclined plane leaves the plane, undergoes free falling (Aussillous & Quéré) (2008).

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The branches of solutions with n-fold symmetry contain also solutions such that each lobe consists of a chain of small droplets connected by thin filaments as demonstrated by Heine (2006).

Besides equilibrium shapes with the topology of the sphere, there are also equilibrium shapes with the form of a torus Gulliver (1984).

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Although there is a huge wealth of equilibrium shapes, one cannot expect that all of them come up to be stable.

Once a rotating drop in equilibrium destabilizes, there are essentially two possibilities:

1 Transition towards another equilibrium shape.

2 Evolution in such a way that its surface becomes non-smooth at

some time and a singularity develops.

In this work we implement a boundary element method to compute theevolution of drops rotating around a fixed axis, determine the stability/instability of equilibrium shapes and study the formation ofsingularities that give rise to topological changes in the drop.

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Equations

Two viscous incompressible fluids: drop & surrounding media. Fluid drop: µ1, ρ1,u(1), p(1).

Outer fluid: µ2, ρ2,u(2), p(2).

Both fluids are rotating around a common axis with angular velocity ω.

Non-inertial frame

ρi 

u(i)t +u(i)· ∇u(i)=

−∇p(i)+ µi∆u(i)− 2ρiω ×u(i)− ρiω × (ω ×r) in Di(t) , ∇ · u(i)=0 in Di(t) .

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Boundary conditions

Balance of stresses across the interface of both fluids: 

T(2)− T(1)n = 2γκn on ∂D (t) , (1) T(k )is the stress tensor inside (k = 1) and outside (k = 2) the drop, given by: Tij(k )= −p(k )δij+ µk   ∂ui(k ) ∂xj +∂u (k ) j ∂xi   , k = 1, 2 . (2) Kinematic condition: vN =u · n ≡ u(1)· n = u(2)· n on ∂D (t) , (3) vN: normal velocity of the free boundary ∂D(t).

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Scaling

If the axis of rotation is fixed:

ω×(ω ×r) = −ω2rer⇒ ρiω2rer= ∇  1 2ρiω 2r2  , Π(i)=p(i)−1 2ρiω 2r2.

Characteristic length l, typical velocity U (ωl) and a characteristic time scale τ = l/U: u(i)= u (i) U ,r = r l,t = t τ, Π (i) = l µUΠ (i), ω = ωbz , µ i = µi µ, ρi = ρi ρ. (Re = ρUlµ ,Ek = ρωlµ2) ρiRe 

u(i)t +u(i)· ∇u(i) = −∇Π(i)+ µi∆u(i)− 2 Ekbz × u

(i) in D i(t) ,

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Stokes system  T(2)− T(1)n = 1 Ca  2κ −Bo 2 r 2  n on ∂D (t) . (5) Ca = µU γ , Bo = (ρ1− ρ2) ω2l3 γ .

Dealing with the limit in which Re  1 and Ek  1, so that viscous forces dominate over inertial and Coriolis forces, we can approximate Navier-Stokes equations by the Stokes system:

−∇Π(i)+ µi∆u(i) = 0 in Di(t) , (6)

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Numerical Method (BEM)

Boundary integral formulation of the Stok. syst (6) with b.c. (5)

uj(rp) = − 1 4π 1 µ1+ µ2 Z ∂D(t) fi(r)Gij(r, rp)dS(r) − 1 4π µ2− µ1 µ2+ µ1 Z ∂D(t) ui(r)Tijk(r, rp)nk(r)dS(r) (8) Gij(r, rp) = δij |r − rp| +(ri− rp,i)(rj− rp,j) |r − rp|3 , i, j, k = 1, 2, 3, (9) Tijk(r, rp) = −6 (ri− rp,i)(rj− rp,j)(rk − rp,k) |r − rp|5 , i, j, k = 1, 2, 3,(10) fi(r) =  2κ(r) −1 2Ω 2r2  ni(r), i = 1, 2, 3. (11)

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Procedure for solving the integral equation

1 Calculate the curvature κ in each node of the mesh.

2 Calculate the velocity by obtaining the balance force termf from

the centrifugal force and κ, replacing it in (8) and solving the resulting integral equation.

3 Given the velocityu, we move the points of the surface using the

explicit Euler scheme.

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Numerical results

Initial configuration

Mesh

Elements ≈ 1000 - 20000, Nodes ≈ 500 - 10000

Two families of numerical tests

1 Ω =cte. (Ω =

√ Bo).

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Table 1: 3D evolution

Constant L

L < L2Axisymmetric equilibrium L2<L < L∗2stable peanut shape L∗2<L < L∗3Breakup (2-fold) L > L∗3Breakup (3-fold) L2∈ (0.65, 0.66)

L∗2∈ (1.06, 1.10) L∗3∈ (1.74, 1.78)

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Evolution of the rotating drop at constant L for L = 1.41, µ1=1 and µ2=0.01. -1 -0.5 0 0.5 1 -0.8 0 0.8 0.4 0.4 -0.4 -0.3 -0.2 -0.10 0.1 0.2 0.3 0.4 x y z (a) t = 2.36 -1 -0.5 0 0.5 1 -0.8 0 0.8 0.4 0.4 -0.4 -0.3 -0.2 -0.10 0.1 0.2 0.3 0.4 x y z (b) t = 8.11 -0.4 0 0.4 -1.5 -1 -0.5 0 0.5 1 1.5 -0.4 -0.3 -0.2 -0.10 0.1 0.2 0.3 0.4 x y z (c) t = 12.36 -0.40 0.4 -2 -1.5 -1 -0.5 0 0.5 1 1.5 2 -0.4 -0.2 0 0.2 0.4 x y z (d) t = 14.16

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Shape of the rotating drop at constant L near the breakup point (t = 14.55) for L = 1.41, µ1=1 and µ2=0.01.

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Shape of the rotating drop at constant L near the breakup point for L = 3.54 and µ1= µ2=0.5. Observe that for L > L∗3the dominant mode driving the symmetry-breaking instability is 3-fold.

-2 -1.5 -1 -0.5 0 0.5 1 1.5 2 -2 -1.5 -1 -0.5 0 0.5 1 -0.4 -0.2 0 0.2 0.4

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Different equilibrium or breakup configuration starting from a torus. 0.4 0 -0.4 0.8 -0.8 -0.4 0 0.4 0.8 -0.8 -0.4 -0.2 0 0.2 0.4 x y z

(e) Toroidal initial configuration

-0.4 0 0.4 0.8 -0.8 0.3 0 -0.3 -0.6 0.6 -0.3 -0.2 -0.10 0.1 0.2 0.3 x y z (f) Equilibrium shape (L = 0.85) 0 0.4 -0.4 -0.4 0 0.4 0.8 -0.8 -1.2 1.2 1.6 -1.6 -0.4 -0.2 0 0.2 0.4 x y z (g) Near break-up (L = 1.7) -1 -0.5 0 0.5 1 -1.5 -1 -0.5 0 0.5 1 1.5 2 -0.20 0.2 x y z (h) Near break-up (L = 2.83)

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Conclusions

In this contribution we have studied the evolution of rotating viscous drops.

We have developed a numerical algorithm based on the boundary integral formulation of Stokes system.

The numerical algorithm is adaptive and introduces automatically local refinement in the critical regions such as necks, where the drop is going to break up.

Based on the numerical results and the analysis of the equations, we have described the evolution at constant angular momentum L. The different regimes found were summarized in table I.

Figure

Table 1: 3D evolution

References

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