sandbox/ecipriano/run/forcedbi.c
Isothermal Evaporation of a Binary Droplet in Forced Convection
A binary liquid droplet, made of two components with the same properties but with different volatilies evaporates in forced convective conditions. The droplet is initially placed on the left side of the domain. An inlet gas flowrate is imposed on the left boundary, such that Re=160 with the initial diameter of the droplet.
The animation shows the evaporation of the liquid droplet, plotting the mass fraction of the light component. The inlet velocity transports the mass fraction toward the right boundary. The Reynolds number selected for this simulation leads to the formation of Von-Karman streets that can be visualized from the transport of the chemical species mass fraction in gas phase.
Evolution of the mass fraction fields of the light component
Simulation Setup
We use the centered Navier–Stokes equations solver with volumetric
source in the projection step. The phase change is directly included
using the evaporation module, which sets the best (default)
configuration for evaporation problems. Many features of the phase
change (evaporation) model can be modified directly in this file without
changing the source code, using the phase change model object
pcm. Exploiting the balances module we can automatically
compute the mass balances for each chemical species involved.
#include "navier-stokes/low-mach.h"
#define FILTERED 1
#include "two-phase.h"
#include "tension.h"
#include "evaporation.h"
#include "balances/two-phase.h"
#include "view.h"Boundary conditions
Outflow boundary conditions are set at the top and right sides of the
domain. Boundary conditions for species must be set in the
init event since those fields are created in
defaults.
double vin = 1.424;
u.n[left] = dirichlet (vin);
u.t[left] = dirichlet (0.);
p[left] = neumann (0.);
u.n[right] = neumann (0.);
u.t[right] = neumann (0.);
p[right] = dirichlet (0.);Simulation Data
We declare the maximum and minimum levels of refinement, the initial radius and diameter, and the radius from the numerical simulation.
int maxlevel, minlevel = 5;
double D0 = 0.4e-3, R0, effective_radius0;
int main (void) {The number of gas and of liquid species are set in the
main() function.
NGS = 3, NLS = 2;We set the material properties of the two fluids. In addition to the
classic Basilisk setup for density and viscosity, we need to define
species properties such as the diffusivity. The default thermodynamic
pressure is the atmospheric value. To facilitate this setup we first set
those properties which are common to all the species, and then we can
refine the setup in the init event passing vectors to the
phase_set_properties() function.
rho1 = 800., rho2 = 5.;
mu1 = 1.138e-3, mu2 = 1.78e-5;
Dmix1 = 1.4e-7, Dmix2 = 1.25e-5;We solve two different sets of Navier–Stokes equations according with the double pressure velocity coupling approach. The system is isothermal, therefore, the solution of the temperature equation is skipped.
nv = 2;
pcm.isothermal = true;We change the dimension of the domain as a function of the initial diameter of the droplet.
R0 = 0.5*D0, L0 = 12.*(6.*R0);We change the surface tension coefficient.
f.sigma = 0.073;We run the simulation at different levels of refinement.
for (maxlevel = 9; maxlevel <= 9; maxlevel++) {
init_grid (1 << (maxlevel-3));
run();
}
}
#define circle(x, y, R) (sq(R) - sq(x - L0/6.) - sq(y - L0/2.))We initialize the volume fraction field and we compute the initial radius of the droplet. We don’t use the value D0 because for small errors of initialization the squared diameter decay would not start from 1.
event init (i = 0) {
refine (circle (x, y, 2.*R0) > 0. && level < maxlevel);
fraction (f, circle (x, y, R0));
effective_radius0 = sqrt (1./pi*statsf(f).sum);The initial thermodynamics states of the two phases (i.e. the
temperature, pressure, and composition) are defined and set. We force
setting the thermo state only if the simulation was not restored. The
composition is expressed in terms of mass fractions. The
YIntVals vector sets the thermodynamic VLE equilibrium
value for each chemical species.
ThermoState tsl, tsg;
tsl.T = TL0, tsl.P = Pref, tsl.x = (double[]){0.5,0.5};
tsg.T = TG0, tsg.P = Pref, tsg.x = (double[]){0.,0.,1};
phase_set_thermo_state (liq, &tsl, force = true);
phase_set_thermo_state (gas, &tsg, force = true);
YIntVals[0] = 0.8, YIntVals[1] = 0.4;
}We adapt the grid according to the mass fractions of the species A and B, the velocity and the interface position. The vector Y is the sum of the evaporating species mass fractions.
#if TREE
event adapt (i++) {
adapt_wavelet_leave_interface ({Y,u.x,u.y}, {f},
(double[]){1.e-3,1.e-3,1.e-3}, maxlevel, minlevel, 1);
}
#endifPost-Processing
The following lines of code are for post-processing purposes.
Output Files
We write on a file the squared diameter decay and the dimensionless time.
event output_data (t += 5e-5) {
char name[80];
sprintf (name, "OutputData-%d", maxlevel);
static FILE * fp = fopen (name, "w");
double tad = t*Dmix2/sq (2.*effective_radius0);
double effective_radius = sqrt (statsf(f).sum/pi);
double d_over_d0 = effective_radius/effective_radius0;
double d_over_d02 = sq (d_over_d0);
fprintf (fp, "%g %g %g %g\n", t, tad, d_over_d0, d_over_d02);
fflush (fp);
}Logger
We output the total liquid volume in time (for testing).
Movie
We write the animation with the evolution of the light chemical species mass fraction, and the interface position.
event movie (t += 0.000125; t <= 0.03) {
scalar A[], AL = liq->YList[0], AG = gas->YList[0];
foreach()
A[] = AL[] + AG[];
clear();
view (tx = -0.5, ty = -0.5);
draw_vof ("f");
squares ("A", min = 0., max = 0.5, linear = true);
save ("movie.mp4");
}Results
reset
set xlabel "t [s/mm^2]"
set ylabel "(D/D_0)^2 [-]"
set size square
set key top right
set grid
plot "OutputData-9" u 2:4 w l lw 2 t "LEVEL 9"reset
set xlabel "t [s]"
set ylabel "(m_L - m_L^0) [kg]"
set key bottom left
set size square
set grid
plot "balances-9" every 500 u 1:10 w p ps 1.2 lc 1 title "Evaporated Mass Species A", \
"balances-9" every 500 u 1:11 w p ps 1.2 lc 2 title "Evaporated Mass Species B", \
"balances-9" every 500 u 1:4 w p ps 1.2 lc 3 title "Evaporated Mass Total", \
"balances-9" u 1:(-$5) w l lw 2 lc 1 title "Variation Mass Species A", \
"balances-9" u 1:(-$6) w l lw 2 lc 2 title "Variation Mass Species B", \
"balances-9" u 1:(-$2) w l lw 2 lc 3 title "Variation Mass Total"