Rheology of granular flows: Role of the interstitial fluid
Transcript of Rheology of granular flows: Role of the interstitial fluid
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Rheology of granular flows:
Role of the interstitial fluid
Olivier Pouliquen,
IUSTI, CNRS, Aix-Marseille University
Marseille, France
Colorado 2003, USGS
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Motivations : debris flows, landslides, avalanches, silo
Not Fault!!!
Low level of pressure: 10-100 kPa in natural events0.1-1 kPa in the experiments
=> Rigid and non breakable particles
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Particles of different sizes + liquid (non newtonian) + complex topography+ unsteady flows …
In this talk :
1) rheology of dry granularflows ?…
2) What happen whencoupling with the interstitialfluid matters …?
? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ?
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Dry granular material:Collection of grains
No cohesionNo brownian motionNo fluid interaction
… Only contact interactions
But not so easy…
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Dry granular flowsDifferent flow regimes
Solid
Liquid
Gas
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Dry granular flowsDifferent flow regimes
Solid
Liquid
Gas
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Quasi-static deformations :Soil mechanics and plasticity
Focus on initial deformation
What happens :
! at large deformations ?
! for fast deformations ?
«!solid!»
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Dry granular flowsDifferent flow regimes
Solid
Liquid
Gas
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Kinetic theory for rapidgranular gases
! constitutive equations couplingDensity, velocity and granular temperature
Binary collisions+inelastic collisions
a) b)
But if not enough energy is injected: ! finite duration contact, ! multiple contact,
«!gas!»
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Dry granular flowsDifferent flow regimes
Solid
Liquid
Gas
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Different flow configurations studiedboth experimentally and numerically
GDR Midi, Eur. Phys. J 04
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Lois et al 2005Da Cruz et al, PRE 05GdR Midi, Eur. Phys. J 04
plane shear under controlled normal stress
P
U
h
P
One imposes P and
Shear stress "?Volume fraction #?
A single dimensionless number (inertial number)
(Savage 84, Ancey et al 99)
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Inertial number
* ratio between 2 times :
: time scale of the mean shear
: microscopic time for rearrangement
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«!quasi-static!» « liquid » «!gas!»
!
I =˙ " dP /#
10
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Da Cruz et al, PRE 05GdR Midi Eur. Phys. J 04
P
U
h
P
One imposes P and
Shear stress "?Volume fraction #?
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!
I =˙ " d
P /#
!
" /P
P
!
" = µ I( )P
!
" = " I( )
!
"
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remark: No velocity weakening
Dacruz et al PRE 05
Peyneau & Roux PRE 08
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Data from
Inclined plane exp. (Pouliquen 99)Inclined plane simulations (Baran et al 2006)Annular shear cell exp. (Sayed, Savage JFM, 84)
For spheres
Forterre, Pouliquen ARFM 08
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!
I =˙ " d
P /#
!
" = µ(I)P
!
µ(I) = µs+
µ2"µ
s
I0I +1
An empirical friction law:
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And shear at constant volume fraction ??
$
f1
#
#
Bagnold Proc. R. Soc 54Lois et al PRE 07Lemaitre PRE 05Da Cruz et al PRE 05
Constant pressure
µ
I
#
f2
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allows to describe (not perfectly) velocity profileson inclined plane,
Let’s go further…
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Predicted velocity and volume fraction profiles
Gdr Midi et al, 2004,Da cruz et al 2002,Silbert et al 2001
Rheology µ(I) predicts - V % h1.5- (h-z)1.5
and &=cte
-Pb with thin flows and close to free surfaceGdr Midi et al, 2004,Da cruz et al 2002,Rajchenbach 2003
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allows to describe (not perfectly) velocity profileson inclined plane, on pile,…
Let’s go further…
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3D generalisation: a visco-plastic model (Jop et al Nature 06)
assumptions : 1) P isotropic
2) and are colinear
Effectiveviscosity
(Savage 83, Goddard 86, Schaeffer 87,…)
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3D generalisation of the friction law :granular flows as a viscoplastic fluid
(Jop et al Nature 06)
Pressure dependent viscosity
assumptions: 1) P isotropic2) and are co-linear
(Savage 83, Goddard 86, Schaeffer 87,…)
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flows on a heap : a full 3D problem
L = 1.5 m
W
Q
(P. Jop et al Nature 06)
y/d
V(y,z)
z/d
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0
1
2
3
4
5
6
7
-0,2 0 0,2 0,4 0,6 0,8 1 1,2
0
1
2
3
4
5
6
7
-0,2 0 0,2 0,4 0,6 0,8 1 1,2
-10
0
10
20
30
40
500 0,2 0,4 0,6 0,8 1
-10
0
10
20
30
40
500 0,2 0,4 0,6 0,8 1
Flow between rough lateral walls:
y/W y/W
h/d
!
Vsurf
gd
Jop et al , Nature 2006
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Jop et al, Phys. Fluids 2007 Initiation of the flow?
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Long wave instability in granular flows
(Y. Forterre, JFM 06 )
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Experimental Setup : forcing of the instability
Forterre and Pouliquen JFM 02
Loudspeakers
Power supply Function generator
Nozzle
Slides projector
Stabilized
alimentationf, AGBF
!
h
x
y
z
Photodiodes
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Dispersion relation
Forterre, JFM 06
Instability threshold
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Granular slumping(Lacaze and Kerswell 08)
Lajeunesse et al Phys. Fluids 2004,2005Lube et al JFM 2004,Larrieu et al JFM 2006,Staron & Hinch JFM 2005,Lacaze et al Phys. Fluids 2008…
Lajeunesse et al 05
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Lacaze and Kerswell(preprint 08)
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Relative Success of the visco-plastic description.
A starting point to adress other configurations…(simulating the pressure dependent visco-plastic rheology is non trivial…)
But there are problems when approaching the solid…
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Limits of the viscoplastic approach:
1) Quasistatic flows (shear band, finite size effect….)A need for non local approach…
2) Transient flows when preparation plays a crucial role
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Exponential tailNot predicted..
Velocity profile
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Shear bands in quasi-static flow
(Forterre & Pouliquen ARFM 08, Jop PRE 08)
Howell et al PRL 99Mueth et al Nature 00Bocquet et al PRE 02…
Not captured by the viscoplastic approach
1.0
0.8
0.6
0.4
0.2
0.0121086420
V/Vw
y/d
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Limit of a local rheology ?
Not captured by the viscoplastic approach
Flow threshold
Finite size effects
hysteresis
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to go further?
Role of the fluctuations ?
Role of the correlations ?
Link with plasticity of other amorphous and glassy systems
Aranson and Tsimring PRE,01,
Louge Phys. Fluids 03,
Josserand et al 06
Mills et al 08
Jenkins and Chevoir 01,
Pouliquen et al 01, Ertas and Halsey 03,
Lemaitre 02Bazant 07Nott 08Behringer 08…
Jenkins Phys. Fluids 06,…
Radjai and Roux PRL 02
5 10 15 20 25 30
5
10
15
20
25
30
Pouliquen PRL 04
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!!
F
Evidence for non local effects:Microrheology experiments
0
20
40
60
80
100
0 100 200 300 400 500 600
Deflection angle
(mRad)
time (s)
'=0
'!0
M. Van Hecke 2008
Pouliquen, Forterre, Nott
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Pouliquen & Forterre, Phil. Trans, 2009
Self activated process
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Limits of the viscoplastic approach:
1) Quasistatic flows (shear band, finite size effect….)A need for non local approach…
2) Transient flows when preparation plays a crucial role
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Daerr & Douady 99
Influence of the initialVolume fraction on the Collapse of a pile.
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#
(
#c
CouplingFriction- dilatancy
"
(
"c
Quasi-static case : critical statetheory
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Reynolds Dilatancy
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(Radjai and Roux 98)
P
(
dX
dY
#
(
#c
assumption: critical volume fraction
!
" #c
Dilatancy angle
Simple critical state theory
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critical state theory :
dilatancy but no shear rate dependence
Visco plastic theory :
shear rate dependence but no dilatancy
Shear rate dependent critical state theory
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Shear rate dependent critical state theory :
!
I =˙ " dP /#
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3D generalisation :. . .
.
.
.
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Initiation of flow on an inclined plane:
)
different
z
Application to a dry flow:
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Initiallydense
Initially loose
z
z
z
z
Comparison with DEM simulations with N. Taberlet…
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Changing time scales…by putting the granular material in water
(Cassar et al, Phys. Fluids 06)
Laser
P.C
DV
recorder
!P
d=112 µm
glass beads
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Dry
Immersed
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A naive idea :
fluid only plays a role by changing the time scale of rearrangements
I = ( tmicro" = P µ(I) with
viscous :
dry :
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µ=tg)
Idry Ivisc
Cassar et al. Phys. Fluids 05
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Submarine flows on heap
Doppler et al, JFM 07
Flow rate
Velocity profile
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And dilatancy ???
And Pore pressure ??
Cf In Faults Rice JGR 75, Rudnicki JGR 84, …
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Large scale experiments in the USGS facility
Iverson et al , (2000) Science
How to explain the variety of landslides observed in nature ?
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Dense preparation Courtesy of Dick Iverson
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Loose preparation Courtesy of Dick Iverson
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Pore Pressure feedback argument(Iverson Rev. Geo. 97, JGR 05)
&!
! Fluid expelled! Pfluid !! Peff "
! Friction "! Less frictionbetween grains
Loose case Dense case
&"
! Fluid sucked! Pfluid "
! Peff !
! Friction !
! higher frictionbetween grains
In faults: rice JGR 75, Rudnicki JGR 84, …
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A simple experiment:
Loose sampleDense sample
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Experimental setup(Pailha et al 08)
1m
20cm
7cm
Glass beads : 160µm Liquid: mixture of water and Ucon oil:*=9.8 10-3 kg/m.s
*=96 10-3 kg/m.s
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Experimental procedure
Compaction by taps0.60
0.59
0.58
0.57
0.56
0.55
!
20151050
# tap
Result of sedimentation
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Velocity of theFree surface
Pressure underThe avalanche
+=25ºh=5mm*=96 10-3 Pa.s
0.6
0.5
0.4
0.3
0.2
0.1
Su
rfa
ce
ve
locity (
mm
/s)
-4
-2
0
2
4
Pore
pre
ssure
(P
a)
5004003002001000Time (s)
Typicalresults
,&i=0.562
,&i=0.568
,&i=0.592&i=0.588&i=0.584
&i=0.578&i=0.571
(Pailha et al Pof 08)
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Velocity of theFree surface
Pressure underThe avalanche
+=25ºh=5mm*=96 10-3 Pa.s
0.6
0.5
0.4
0.3
0.2
0.1
Su
rfa
ce
ve
locity (
mm
/s)
-4
-2
0
2
4
Pore
pre
ssure
(P
a)
5004003002001000Time (s)
Typicalresults
,&i=0.562
,&i=0.568
,&i=0.592&i=0.588&i=0.584
&i=0.578&i=0.571
(Pailha et al Pof 08)
Dense
&i>&c
Loose &i<&c
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Triggering time
in the dense case
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Triggering time
60
50
40
30
20
10
Tim
e (
s)
0.6050.6000.5950.5900.5850.580
Phi
+ =25°
+ =26.4°
+ = 28°
+ = 30°
h=3.7 mmh=6.1 mm
*=9.8 10-3 kg/m.s
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Deformation
For
12
10
8
6
4
2
0
Su
rfa
ce
ve
locity (
mm
.s-1
)
403020100Time (s)
initial preparation erased
1.6
1.4
1.2
1.0
0.8
0.6
0.4
0.2
0.0
Surf
ace
vel
oci
ty (
mm
.s-1
)
0.80.60.40.20.0Deformation
!i=0.588
!i=0.584
!i=0.582
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Two phase flow model
Rheology of thegranular phase
Granular matter
2Dilatancy
Soil mechanics
3
Coupling with the liquid:Two phase equations
Fluids mechanics
1
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Depth averaged approach (Pitman and Le 05) :
submarine avalanches :
)
z
h
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Submarine granular avalanches:
Relative weight Viscous drag due to the Vertical displacement
(Cassar et al 05,Doppler et al 07 )
Shear rate critical state theory
Particle-fluidcoupling
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Calibration of the model looking at the steady state
0.55
0.50
0.45
0.40
!start
0.590.580.570.56
"
!
µ Iv( )
!
"eq Iv( )
!
K
A single freeParameterK2
0.62
0.60
0.58
0.56
0.54
0.52
0.50
!
4x10-3
3210
I
0.58
0.56
0.54
0.52
0.50
0.48
0.46
0.44
µ
2.5x10-3
2.01.51.00.50.0I
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Predictions :Velocity Pressure
0.7
0.6
0.5
0.4
0.3
0.2
0.1
0.0
u (
mm
.s-1
)
4003002001000
t (s)
-4
-2
0
2
4
Po
re p
ressu
re (
Pa
)
5004003002001000t (s)
-4
-2
0
2
4
Po
re p
ressu
re (
Pa
)
5004003002001000t (s)
0.7
0.6
0.5
0.4
0.3
0.2
0.1
0.0
u (
mm
.s-1
)
4003002001000
t (s)
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Different hDifferent viscosities
Scaling of the triggering time
t/t0
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Pore Pressure Maximum acceleration
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Conclusions for submarineavalanches
A simple critical state approach+ a viscoplastic rheology+ two phase flow equations
!Semi quantitative predictions in the complexdynamics of the flow initiation of submarine avalanches
Beyond the depth averaged approach ?Question of the numerical implementation of such models?
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Index matchingmethod
Mickael Pailhaunpublished
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Conclusions for constitutive modeling of granular flows
Visco-plastic approach gives the order zero of viscousbehavior of granular flows
It can serve as a base for further developments:-irregular particles?-cohesive particles?-polydispersed materials?-breakable particles?(dilatancy, underwater granular flows, cohesive flows…)
-link with the microscopic physics? -how to capture non local effects (role of fluctuations, link with glassy systems,….) ?
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Towards more complex granular media:
Polydispersed : Felix et Thomas PRE 04 Rognon et al 06…
Cohesive granular matter:
granular matter with fluid interactions
Rognon et al 08Halsey et al 06Richefeu et al 06 …
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Merci à
Mickael Pailha Pierre Jop, Cyril Cassar Yoël Forterre Pascale Aussillous Maxime Nicolas Prabhu Nott Jeff Morris Neil Balmforth Bruno Andreotti Olivier Dauchot…