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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
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dcz
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pppp
dcx
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][
1
][
1
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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).
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