Upload
lindsay-ross
View
214
Download
0
Tags:
Embed Size (px)
Citation preview
Lorentz Centre, 19 Sep. 2006
Particle transport and flow modification in planar temporally evolving mixing layers
Djamel Lakehal, Chidambaram Narayanan(G. Yadigaroglu, ETH Zurich)
Adjunct Lecturer at ETH & Manager of ASCOMP GmbH(www.ascomp.ch)
Outline
Motivations: environmental concerns
Mixing layer basic flow features
Transport under 1-way coupling
Transport under 2-way coupling
Summary
Transport & dispersion of sandVolcanic ash dispersion
CO2
H20
Environmental flows with particles and droplets
Simulation: Eulerian-Lagrangian formulation
fpi
j
Fx
u
x
p
x
uu
t
u
x
u
j
j
j
j
j
j
j
2
21
0
Re
FLUID
PARTICLE
3/2
2
Re15.01
)(2
9
pd
pippp
dp
f
txuud
fdt
dvi
i
Details
Re=400, 64 X 129 Fourier Chebyshev collocation; Lx=4/Km
Tangent-hyperbolic U velocity fieldAmplitude of Fund. & Sub. modes Ef = 10-2; Es = 10-4
Rep < 1; Np = 2-4.105 particles; St= 0.3 - 5; M = 0.1-0.52nd order Runge-Kutta for Particle Equation
4th order Lagrangian ploynomial velocity interpolation
2D particle-laden mixing layer under 1- and 2-way Coupling: What is new ?
The analysis is Eulerian-Eulerian based
The controlling mechanisms
The mean vertical particle-phase velocity induced by KH
The correlation between particle-phase and fluid-phase modal (KH induced) stress
The effect of particle-phase modal velocity on the growth of the particle-phase mixing layer
Basic Flow Features:
1. flow evolution
2. Kinetic energy balances
Particle Transport under One-way
1. centrifuging effect
2. statistics
3. momentum balance
I- Outline: Particle Transport under 1-way Coupling
Saturation of fund. mode at t=48
initiation of pairing at t=72
end of pairing at t=96
single vortex at t=120
Analysis: Continuum formulation
cdz
pppp
dcz
dpppp
pppp
dcx
dpppp
p
Fz
pww
z
wwwwnz
nFwwnz
wnt
wuuwnz
nFuwnz
unt
wnzt
n
''
][
1
][
1
0
CONTINUM
FIELD
FLUID
W
II- Outline: Particle Transport under 2-way Coupling
Computational parameters
Particle accumulation patterns
Fundamental mode saturation & pairing
Particle Statistics
1. Generation of small scales
2. Evolution of average modal stress
3. Mean kinetic energy balance
St=2M=0.2
No new instability forms for low M and uniformly distributed particles: rather drag effect
t=72 t=96
Summary
Particle transport in turbulent mixing layers was analyzed using DNS + Lagrangian particle tracking.
Particles modify the flow evolution dramatically even at mass loadings of 0.5; generation of small scales.
Intricate undulating patterns are formed.
Effect of preferential concentration on particle statistics was emphasized.
Related publications
Narayanan C., Lakehal, D.: DNS of particle-laden mixing-layers. Part I: One-way coupled flow and dispersed-phase features. Phys. Fluids, 18(9), pp. 15, 2006.
Narayanan C., Lakehal, D.: DNS of particle-laden mixing-layers. Part II: Two-way coupled induced generation of small-scale vorticity, Phys. Fluids, 18(9), 2006.
Botto L., Narayanan C., Fulgosi M., Lakehal D.: Effect of near-wall turbulence enhancement on the mechanism of particle deposition, Int. J. Multiphase Flow, 31(8), 2005.
Lakehal D., Narayanan C.: Numerical Analysis of the continuum formulation for the Initial Evolution of Mixing Layers with Particles, Int. J. Multiphase Flow, 29(6), 2003.
Narayanan C., Lakehal D., Botto L., Soldati A.: Mechanisms of particle deposition in a fully-developed turbulent open channel flow, Phys. of Fluids, 15(3), pp. 763, (2003).
Narayanan C., Lakehal D.: Temporal instabilities of a mixing-layer with uniform and non-uniform particle loadings, Physics of Fluids, 14(11), pp. 3775, (2002).
Narayanan C., Lakehal D.: Linear Stabilities Analysis of Particle-Laden Mixing Layers using Lagrangian Particle Tracking, Powder Technology, 125, pp. 122, (2002).