Transport o
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particles i in fl fluid fl flows Transport o
- f p
Transport o of p particles i in fl fluid fl flows Transport o - - PowerPoint PPT Presentation
Transport o of p particles i in fl fluid fl flows Transport o of p particles i in fl fluid fl flows Mas Massimo mo Ce Cencini Ce Massimo Mas mo Cencini Istituto dei ei Sistemi emi Comp mples essi Istituto dei ei Sistemi
same density of the fluid
point-like
same velocity of the underlying fluid velocity fluid velocity
density different from that of the fluid
finite size
friction (Stokes) and other forces should be included
shape may be important (we assume spherical shape)
velocity mismatch with that of the fluid fluid
Rain droplets Rain droplets
Planetesimals Planetesimals
Dynamical and statistical properties of particles evolving in turbulence Dynamical and statistical properties of particles evolving in turbulence focus on clustering observed in experiments focus on clustering observed in experiments Clustering important for Clustering important for
(collisions, chemical reactions, etc...)
Wood, Hwang & Eaton (2005)
scales (!" = Kolmogorov length scale)
"<< << r << L << << r << L Many characteristic time scales
r < r r < " " Fast Fast evo evolvi ving scal scale: charact e: characteri erist stic t c time - e --->
Fast Fast evo evolvi ving scal scale: charact e: characteri erist stic t c time - e --->
Stokes time Fast fluid time scale
0#$ #$<1 <1 heavy heavy $ $=1 =1 neutral neutral 1< 1<$# $#3 3 light light
Stokes number Stokes number Density contrast Density contrast
Small particles a<< Small particles a<<" " Small local Re a|u-V|/ Small local Re a|u-V|/% %<<1 <<1 No feedback on the fluid (passive particles) No feedback on the fluid (passive particles) No collisions (dilute suspensions) No collisions (dilute suspensions)
Ve Very heavy particle Ve Very heavy particle $ $=0 =0 =0 =0 (e (e.g .g. . water r dro rople lets in air r (e (e.g .g. . water r dro rople lets in air r $ $=1 =10 =1 =10-3
)
hea eavy hea eavy lig light ht
neutr neutral al
Differentiable at Differentiable at small scales (r< small scales (r<" ") )
Particle in d-dimensional space Particle in d-dimensional space Well defined dissipative dynamical system in 2d-dimensional phase-space Well defined dissipative dynamical system in 2d-dimensional phase-space
Jacobian (stability matrix) Jacobian (stability matrix) Strain matrix Strain matrix
constant phase-space contraction rate, i.e. phase-space constant phase-space contraction rate, i.e. phase-space Volumes contract exponentially with rate -d/St Volumes contract exponentially with rate -d/St Motions evolve onto an attractor in phase space Motions evolve onto an attractor in phase space
$ $=0 St =0 St& &1 1 $ $=0 St=0 =0 St=0 $ $=3 St =3 St& &1 1
0. 0.16- 6->4 0- 0->3 65 65 12 1283 0. 0.16- 6->3. 3.5 10 105 256 2563 0. 0.16- 6->3. 3.5 65 65 12 1283 0. 0.16- 6->3. 3.5 18 185 51 5123 0. 0.16- 6->70 70 400 400 2048 20483 0. 0.16- 6->4 0- 0->3 18 185 51 5123
St $ Re'
N3
! Ejection/injection of heavy/light particles from/in vortices preferential concentration ! Dissipative dynamics in phase-space: volumes contraction & particles may arrive very close with very different velocities ! Finite response time to fluid fluctuations (filter of fast time scales)
(Maxey 1987; (Maxey 1987; Balkovsky, Falkovich, Fouxon Balkovsky, Falkovich, Fouxon 2001) 2001)
Strain rotation
Heavy particles like strain regions Heavy particles like strain regions Light particles like rotating regions Light particles like rotating regions
Bec et al (2006) Bec et al (2006)
1(
St) >
1(
St=0)
st stay l ay longer i er in st stay l ay longer i er in st strai rain-reg
st strai rain-reg
1(
St) <
1(
St=0)
st stayi aying aw away fro ay from st strai rain-reg regions st stayi aying aw away fro ay from st strai rain-reg regions
Calzavarini, MC, Lohse & Toschi 2008
Instantaneous p. distribution in a slice
Bec, Biferale, MC, Lanotte, Musacchio & Toschi (2007)
" &
' only
correlation dimension
1
10 St
Re'=400 Re'=185
0.1
Clustering & Preferential concentration are correlated !Maximum of clustering for St"&1 !D2 almost independent of Re', ! Dq) D2 multifractality
Re=75,185 Re=75,185
2&
Light particles: neglecting collisions might be a problem!
"?
Poisson ( (* *=0 =0) =0 =0)
Effective compressibility Effective compressibility
,=7.9 10-3 ,=2.1 10-3 ,=4.8 10-4
Inertial (heavy) particles Brownian motion in a Disordered media with Nontrivial spatio-temporal Correlation (turbulence) Simplified model: retaining only spatial correlations mimicking turbulent ones (Kraichnan model for the velocity)
e.g. separation between 2 particles R=X1-X2
Derevyanko, Falkovich, Turitsyn, Turitsyn JoT (2007) (1d) Horvai arXiv:nlin/0511023v1 [nlin.CD] (2d)
particles in turbulent flows”, PRL 86 2790-2793 (2001)
turbulent flow”, PoF 16, L47-L50 (2004)
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induced segregation of inertial particles”, PRL 101, 084504 (2008)
velocity distribution of heavy particles in turbulence”, JFM 646, 527 (2010)
PRE 68, 040101 (2003)
(2003)
flows” JFM 528, 255 (2005)
95, 240602 (2005)
particles in random smooth flows” PoF 17, 073301, 2005
driven by a telegraph noise”, PRE 76, 026313 (2007)
described by the telegraph model” PRE 76 026312, 2007
upper ocean turbylence” SIAM J App Math 62:777 (2002)
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the large Stokes number asymptotics” Physica D 226, 11-22, 2007; “Clustering
heavy particles Physica D 237, 2037-2050, 2008
particles in random flows” EPL 89 50002 (2010)
by random velocity fields” PRE 81, 016305 (2010)