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Behavior of powder under weak perturbations: the concept of the effective surface. I.
E. Gurovich, S. Maruk
To cite this version:
E. Gurovich, S. Maruk. Behavior of powder under weak perturbations: the concept of the effective surface. I.. Journal de Physique II, EDP Sciences, 1991, 1 (10), pp.1147-1166. �10.1051/jp2:1991125�.
�jpa-00247581�
J. Phys. II France 1(1991) l147-l166 OCTOBRE1991, PAGE l147
Classificafion Physics Abstracts
05.40 05.60
Proofs not corrected by the authors
Behavior of powder under weak perturbations
:the concept of
the effective surface. 1.
E. V. Gurovich
(*)
and S. V. MarukDepartrrent of Theoretical Physics, Insfitute for lligh Pressure Physics, Moscow Region, Troisk, 142092, U-S-S-R-
(Received J3 May J99J, accepted in final form J7 June J99J)
Abswad. On the base of the semiphenomenological model one-panicle approach describing
the behavior of powder under weak perturbation is developed. The notion of the effective surface which restricts the possible shift of a grain due to the presence of surrounding ones is put forward.
The dynamics of swelling and packing down is considered as a synergetic self-organizing process through Poincare's maps. The equilibrium density for a given intensity of perturbations is
described. The origin of the convective motion in vibration and its threshold character are
investigated.
1. Inwoduction.
The
investigation
ofpowders (so-called granular
orfree-flowing materials)
is traced back to the studies ofFaraday (1831)
andReynold's (1885). They II,
2] describedunique
static anddynamic properties
of a mediumconsisting
of a great many ofgrains,
in interaction of which friction is of greatimportance.
Behavior ofpowder
was revealed todepend non-trivially
upon thedensity
and the manner ofgrains packing.
This leads to the existence of a number oforiginal phenomena breaking
up, as it seems, the fundamental laws of classical mechanics.So, under a rather
powerful
vibration ingranular
material a convective stream of massoccurs in the
opposite
direction to force ofgravity [I].
Another well known
phenomenon
is theresiding
ofpowder
atperturbations.
Underjostle, shaking
or vibration achange
of initial volume can reach themagnitude
of the order of 10 fb.This effect is
customarily
considered as a trivial one andexplained by
thetendency
of thedissipative
mechanical system to minimizepotential
energy. However, thestirring
can lead notonly
toresiding
but also toswelling
andexpanding.
Finally,
aninteresting phenomenon
such assegregation
ofpolydisperse powder
should be noted. Under chaotic disturbance a mixture ofgrains
of different sizes and masses can beseparated.
Thelarger (sometimes
evendenser) panicles
rise to the top,coming
to thesurface,
and smaller ones(though
lessdense)
filter downsinking
inspite
of » Archimed's law.l148 JOURNAL DE PHYSIQUE II N 10
Due to apparent industrial
applications
thesephenomena
have been thesubject
ofconsiderable
study.
At present there is a number oftechnological
andapplied
papers as a rule of adescriptive
character which can't be reviewed evenbriefly.
Some references to this type of papers can be found in references [3-27~ mentioned below. It is to be notedonly
thatthese
phenomena
have been usedlong
ago inpowder
industries.Nevertheless, as
paradoxical
as it is, themicroscopic grounds
andquantitative description
of these effects, in
spite
of their apparentsimplicity,
are absent until now(').
The reason for this is that the consistenttheory
ofpowder
stops at the verycomplicated problem
of classicalmechanics,
namely,
themany-body problem.
Inspite
of the number ofgrains
in the unit of volumebeing
in 106-108 times less than intypical problems
of the moleculardynamics
thisproblem
can't bedirectly
solved. As isusually
for this type ofproblems,
thefollowing questions
arise : how to connect the movement of any selectedparticle
with the others, how toconnect the local geometry of
packing
with theproperties
of medium as a whole ?There exist different ways to solve the
problem
concemed. The main part of the work is devoted to theanalysis
of randompacking [3, 17-24] usually
apacking
ofspheres
in the three-dimensional space or disks on theplane.
The commongeometrical probabilistic [23, 24]
methods,
data obtainedby
naturalII
8,21]
and numerical[17,
19,20] experiments
are used as the base of this work.The
regular packing
ofspheres
and disks havelong
ago been studied and classified incrystallography (Fig, I).
The share of the volumeoccupied by particles
inhexagonal
and cubicspatial packings
areequal
~
3~i~~~~
~~~~~~
~~~~The densities of
corresponding regular plane packings
are well known too.They
arerespectively,
The nature of random
packings
are to a great extent morecomplicated. Simulating
thestrucrue of monoatomic
liquid
Bemal[17]
discovered thedensity jump
between thehexagonal
and the random closedpackings.
Whileexperimenting
with the metallic balls [18]Scott showed the
density
ofpoured powder depending
on friction forces betweengrains.
The maximumdensity
that can be achievedby stirring
andpressing
isf 0.637
(1.3)
Finney following
Bemal and Skottreproduced [19]
their results and carried out thedeep
statisticprocessing
of three-dimensional random closedpacking by
computer simulation.Computer research of
plane
randompacking
of disks[20]
shows the maximumdensity
of it to beequal
tof 0.821
(1.4)
(~) There is a lack of studies and the origin of the convective motion is still unexplained » (Douady,
Fauve and Laroche, 1989), a basic phenomenological understanding of segregation mechanism has remained elusive (Rosato, Strandburg, Prinz, Swendsen, 1987), « the most elementary problems have not been fully addressed (Edwards, Oakenshott, 1989).
N 10 BEHAVIOR OF POWDER UNDER PERTURBATIONS l149
a) ~~,,
,
b)
,
dn
~2'~3
,_j , , ,_,
~Z,X3
Iii d)
~ic)
,,
, , , ,,,
~fi
,
~
xi ,
~
/
,
~
~~d~
,, ,
Xz>X3 ~ '~ i
W
Fig. I. a) Regular plane packing characterized by the angle p, b) the closed random plane and c) a
loose random plane packings, d) a local geometrical configuration in the regular three-dimensional packing characterized by the angle p, here loose two-dimensional layers have hexagonal synlmetry, e)
random packing in polydispersive powder. The particles having occupied one row (layer
4
in the more compact packings ~b) and occupiying after swelling (c) a number of rows (more thick layer d~) areshaded.Nowadays
there exist numerous papersconcerning
computer simulations of bothpoly-
andmono-disperse powders (see
references in[22-23]).
However, the values of maximum densities(1.3-4)
are stillintriguing
as is the notion of random closedpacking
itself.The random
packings
simulate arrangement ofpowder particles.
Nevertheless, in the papers devoted to the mathematicalanalysis
ofpackings
thephysical
results arepractically
absent. In these papersparticles
areregarded
aspurely geometric objects,
mass andgravity
field
being
absent whilegrain
arrangement fixed. To go over from thepacking
geometry toproperties
ofgranular
medium in thisapproach
isimpossible.
The second,
phenomenological approach,
tumed out to be more fruitful.Postulating
someproperties
ofpowder
as a continuous medium the authors of references[4,
5, 8,13-16] explain
some or other effects. In this
approach
the basic notiongoing
back toReynolds
[2] is concept of compact and friable(loose) packings
which reveal the solid andliquid phase properties
respectively.
So, when
describing
the convective motion[I,
I1,26]
under the vibration De Gennes[13]
has modernized this concept
using
the terms of active andpassive phases. During
the activephase
of vibration theparticle
acceleration is directedagainst
ofgravity force,
thepowder being
swollen.During
thepassive
oneparticles
fall whilepowder density increases,
and arrangement ofgrains being
fixed. It results in vibrationinstability
of the surface andarising
of the convective stream directed
upward.
II 50 JOURNAL DE PHYSIQUE II N 10'
The concept of fluidization of
powder
underperturbation
was earlier used[15,
16] toaccount for
shrinkage.
Outer disturbancedestroys
a metastable state, andpowder
shrinkstrying
to minimize [3,4]
itspotential gravity
energy. Thisexplanation,
however, is open to criticism.Really,
if beforestirring
thepowder
has closed randompacking, practically
anystirring
will lead to theswelling
of thepowder.
Thephenomenological
ideas of fluidization » and minimization ofpotential
energy cannot describe the effect ofswelling.
The
shrinkage
andswelling
ofpowder
were describedby
a unified way in the framework of anotherphenomenological
model [5], where theequilibrium
value ofdensity
reflects a balance between theamplitude
of theperturbations
andrestoring
force such asgravity.
In order to
explain
the effect of sizesegregation [3,
12, 14,25]
it is maintained in[15]
that the resistance to the motionupward
of alarge particle
is less then one to motion down. This results in «coming
to the surfacelarge grains
under the accidentalperturbation.
However thequestion
: how does the resistancedepend
on the relative size ofgrains
and their mass ?has no answer in the
phenomenological approach.
A brief survey of basic studies shows that the
phenomenological
waygives
afragmentary picture
in which numeroushypotheses
are introduced toexplain
various effects. It seems that this way doesn't allow themacroscopic properties
of freeflowing
medium to be united with thegeometric
characteristics ofpacking.
A third
microscopic approach
to thepowder
isnowadays developing.
The authors[10]
computer-simulated
thephenomenon
ofsegregation
in a mixture ofparticles
of two different(large
andsmall)
sizes inshaking
andexplained
it as follows : thelarge particle
is movedupward
as smallerparticles
fill voids beneath it. In order for alarge particle
to move back down alarge
void must open beneath it. Because several smallparticle
must movesimultaneously
in order to create suchlarge
void appearance of a suchlarge
void isrelatively unlikely,
and thus thelarger particle experience
a netupward
motion[10].
This
explanation
assumes theperturbation
to beenough powerful. Really,
for thelarge particle
to moveupward (to
theright,
to theleft)
under a weakperturbation
it is necessarythat several smaller
particles
should create alarge
void over it(to
theright,
to theleft),
that isunlikely
either. Moreover, the process ofsegregation depends
on the relative masses ofgrains [3,
12, 14,25].
Forexample
the Brazil nut »(in
the term of[10])
will be on the top but the steel ball of the same size will sink. In theprocedure [10]
«mass is notimportant
forsegregation
process »,The
original microscopic theory
wasdeveloped by
Edwards and coworkers[6-9],
who used the ideas and methods of statistical mechanics asapplied
topowder physics.
Thehypothesis
about
equal probability
of realization of the samedensity
states in the ensemble ofpowders
formed
by
the same extensivemanipulation
is taken as a basis (2) of theirtheory [6,
7] so to say thepowder analogy
of the microcanonical distribution[28].
This «powder ergodic»
hypothesis
is not trivial and,generally speaking,
demands someargumentation.
Numerousquestions
do arise : what constantplays
the role of the Boltzmann constant, what is it determinedby
anddependent
on ? How can oneintegrate
the states ofgranular
system overphase
space ofconfigurations
ofimpenetrable particles
to calculate the realphysical
parameters
through
distribution function ? The lastproblem
forpowder
as contrasted to the system ofpenetrable particles (ideal gas),
which are the mainapproach
for allproblems
of statisticalphysics
isunlikely
solveddirectly.
Theonly problem
solveddirectly
in framework of the method [6] is the one-dimensionalpowder.
In the morecomplicated
two- or three-dimensional cases, obtained results [6] became «intractable ».
(2) The similar hypothesis was put forth earlier in the work [24] devoted to mathematical analysis of random packings.
M 10 BEHAVIOR OF POWDER UNDER PERTURBATIONS list
In the
following splendid
papers[8-9]
Edwards and coworkersinvestigating
thebinary
mixture oflarge
and small sizegrains
used theanalogy
between the geometry of localpacking
and the well known
eight-vertex
model. Thisapproach
set forth somequestions
too. lvhatvertex model must
poly-granular
mediumgiven
infigure
I be describedby
?The
difficulty
of method of statisticalphysics
to describe thepowder
is due to thenonergodicity
[9] of the latter. In fact any state ofpowder
is metastable. In the lack of disturbance the distribution function ofgrain configurations
has no universal character but is determinedexclusively by
initial conditions. To put it in other way, it is not the initial state(that analysis
of randompacking)
butonly
behavior ofgranular
medium with certain initial conditions underperturbations
of certainintensity obeys physical law-govemed
nature. It isby
this way that thequestion
is put forward in the present paper.The first part of our work is built up as follows. In section 2 the basic for our
procedure
concept of the effective surface(one-particle approach)
isintroduced, equations
ofdynamics
are put in
paragraph
3 the mean-fieldapproach
for effective surface is stated and thesimple
models of effective surface are discussed ; sections 4, 5 and 6 are devoted to
description
ofswelling shrinkage
effects and toorigin
of convective motion under vibration. The size anddensity segregation
anddensity
of freepoured powder
will be discussed in second part.2. The effective surface
(one-particle approach).
Any
model ofpowder
is to reflect two obviousproperties
the dominant roles,first,
of theimpenetrability
ofgrains (the
effect of excluded volume which prevents from bothanalysis
ofrandom
packing
and direct realization of Edward'sapproach [6])
and,secondly,
the role of friction forces. The form ofgrains spheres, ellipsoids, polyhedrons
as well as concrete type ofperturbation, jostle, stirring, shaking,
vibration, as it was shownby experiments,
don't
change
thequalitative picture
of the effects discussed inparagraph
I. We'll considerspheres
and disks aspowder particles,
theirregular (I.1-2)
and random(1.3-4) packings being
commented on above.From the
microscopic point
of view an outsideperturbation (for example, banding
on the container walls in whichpowder is)
reveals in transmission of momentum fromunderlaying layers
to upper ones, which are free to move.Figure
2 shows(certain, schematic)
aninstantaneous
configuration
ofgrains
atstirring.
Because of mutualimpenetrability only
Zf
'~,~
,
~~$_
,
~___
,
~
'
~2 >~3
Fig. 2. An instantaneous state of powder under stirring. The « active » (or« liquid-like ») phase is the
particles 3, 4, 5, 6, 12 which are capable to move at the moment. The « passive » (or « solid-like ») phase is the grains1, 2, 7, 8-11, which haven't at the present moment any free space for moving. Local
geometric configurations, inside which a shift of shaded grain in respect with the surrounding ones can occur, are shown too. The tendency of shaded particle to emerge depends on the local geometry of packing : the more density (the less distance I between grains in a layer), the more tendency to swell (the more vertical component of the momentum obtained under stirring).
II 52 JOURNAL DE PHYSIQUE II N 10
particles
to becapable
tochange
theirposition
in respect with surrounding ones at this instantmoment are those, which have vacant voids for
moving
at the moment.So, having
obtained aknock from
particles
I or 2particle
3 iscapable
tochange
itsposition. Having
obtained a bit fromparticles
3 or 4grain
5changed
itsposition. Impulse
obtainedby particle
7 fromparticle
6(or by particle
it fromparticle 12)
Mill not result in anychange
ofposition
of the last but will pass toparticles
8 or 9(or
toparticle13).
Thesuggested picture
is similar toReynolds' [I]
and De Gennes's[13]
ideasalready
mentioned in the introduction. In ourdescription
active or«liquidlike» phase ~particles3-6, 12)
andpassive
«solidlike» one(particles
1,2,
7-9,11)
coexist in the bulksimultaneously
but arearranged
in differentpoints
of the volume.
Let us introduce a coordinate system x;, the axis xi
being
directedvertically upward.
Let us consider anarbitrary
selectedparticle (for example
one number3)
and follow itspositions
inthe coordinate system connected with the container after the each
n-th,
n+lst,n + 2d
perturbations. Figure
3 and comments to it show all thepossible
types of behavior : when testparticle
goesdown,
lifts or remainsapproximately
at itsplace.
Inprinciple
the sameprocedure
can be fulfilled for anygrain.
If whileaveraging
theprocedure
over allgrains
of medium one of these situations takeplace
it will mean that thepowder
settles and itsdensity rises,
swells or is in itsequilibrium
state under thegiven perturbations.
The
displacement
vector of somegrain
at the n-th disturbance is3u)~~
= r,l~~ r,l~ '
(2.1)
The full vector of
displacement
of thegrain
after n disturbances isequal
~(n)(~(0))
= ~in)
~lo)
~
( ~~(k)
(~
~)
' ' ' '
k =1 '
~
~+
l,n+/~~ ~+6~~j~+4
~~~4 ~$/
n+2n+3~~ ~~~ ~~7
n+6
~
~~ n+I
a)
~b) c)
Fig. 3. Behavior of an arbitrary selected grain a) sinking down, b) going to the surface, c) remaining
near its place under the n-th, n + lst, n + 2d knocks in container walls.
and
depends
upon the initialposition
of thegrain
r(°). In contrast to the continuous medium thedependence
u,l~) upon r1°~'strictly speaking,
isn't smooth and differentiable. It is due tograins
aren'tclamped together
and can intermix under chaoticperturbations. So,
there existsa random component of
displacement
vector causedby
the occasional momentum trans-mission in the random
packing
at the same time with theregular
component causedby
thegravity
force. Because of theregular
component of thedisplacement
vector directedperpendicular
to thegravity
force(along
the axes x~, x~)equals identically
to zero, the components 3u)~~,3u)~)
have amerely
accidental nature. Let thetypical
distance on whichgrains
are shifted at asingle
weakperturbation along
x~, x~equal
to 2ix (.
i 3"l~~i i
=
i 3"'~~
= 2
lx1
(2.3)M 10 BEHAVIOR OF POWDER UNDER PERTURBATIONS II 53
The value
ix depends
on thedensity
p~ ofpacking
and theintensity
of n-thperturbation.
It increases,certainly,
withdiminishing
of thedensity
and withrising
ofintensity.
To smooth the
dependence
ofdisplacement
vector3u)~)
upon theprior
coordinater;(~ ' of a
particle
let us average it over avolume,
which contains manygrains
and is muchmore then the
typical
occasionaldisplacement
x. For smoothedby
a such waydisplacement
vector
(3u,l~~)
one can introduce the strain tensor at the n-thperturbation
If at the n-th disturbance
powder density
doesn'tchange
p~= p~ j and convective streams
are absent one obtains
j~~jn)j
=
j~~jn)~
=j~~jn)j
= o
11
3"i~~ii
=
ii3Ui~~ii
= 2
(x(
and all the components of the deformation tensor are
equal
to zero. If the n-thperturbation
leads to the
swelling ~packing down)
ofpowder
p~ » p~_ j one has(3u)~~)
w0;(3u)~~)
=
(3u)~~)
= 0
i13"l~~ii
=
i18"l~~ii
=
2
(x(
and the
only
nonzero component of strain tensor is(3u)[~)
whatcorresponds
to the uniformtension
~pressing) along
axis xi.After the n-th perturbation which results in
swelling
orpacking
down ofpowder,
a distancedx)~~
'~ between twoarbitrary
selectedparticles
willequal
(dx)~~)
= l + 23u)/~ (dx)*'~)
=
ij
+ 23u))~ (dx)°))
k =1
Substituting
in theexpression
the definition of the deformation tensor(2.4)
one caneasily
make sure that
n a @~
lk)j
~ ~(n)j(dx)"~)
= l +
~
(~(dx)°~)
=
l + ~
(dx)°))
,
(2.5)
~ j 3Xj 3Xj
here u,(") is the full vector of
displacement (2.I).
An infinitesimal volume
(dV(°))
after nperturbations
will turn into the volume aj~)n)j
(dV~~~)
= + ~(dV~~~) (2.6)
3Xj The volume
dV(~)
contains not thesame
particles
which were contained indV(°)
beforeswelling (as
it were in continuousmedium)
butonly
the same number ofparticles.
The
applicability
of formulas(2.5-6)
is restrictedby
the finite size D of grains. Let usconsider a horizontal
layer
of the closed randompacking ~paragraph I)
thegrains,
whichare crossed
by arbitrary
drownedplane
xi= const. Over
(or under)
thesegrains
the nextlayer
is
disposecd-
thegrains,
whichdirectly
touch thegrain
of the firstlayer.
The distanceIN JOURNAL DE PHYSIQUE II M 10
d
between(mass center)
of the twolayers
isnaturally
toidentify
with thelayer
thickness of the random closedpacking.
Let k
perturbations
lead in a uniformloosing
of closedpacking (Fig, I). According
to the formula(2.5)
the thickness of aswelling layer
is3(u)~~) -3(u)~))
~~ ~
fi
~ ~ ~ ~k' ~k ~~~jo) ~~'~)
value u~ = u~_j characterizes
by
what averagemagnitude
the thickness of alayer
have increased after theswelling, by
what distance have raised on average agrain
with respect to thegrains
ofunderlaying
layer under the k-thshaking.
Thus,
under the k-th disturbance averagegrain
» free to move at the moment receives amomentum from one of the
surrounding grains
of theunderlaying layer (Fig. 3) along
thenormal to the tangent plane of
grains
and shifts in respect with thegrains
on tile distance u~ = u~ jalong
xi and on the distance 2 x~ in theperpendicular
direction(see (2.3)),
thepowder tuming
into a new metastablepacking.
It is worth to note that fulldisplacement
of agrain
at the k-thshaking
isgiven by (2,I).
But most part of thisdisplacement 3u)~~
agrain
moves as a whole withsurrounding
ones. Therefore,only
a part u~= u~_ j,
x~-x~_j of the
displacement 3u,l~)
connected with a relative movement in respect toneighboring grains
leads to a localrepacking and,
hence, to achange
of thedensity.
Let us introduce
(Fig. 4)
the effective surfaceu(x)
inside which the « average motion » of the averagegrain
inregard
to thesurrounding neighbors
occurs. Theturning
ofpowder
u(x)
~n-
f~n-
X~+
iU~+ U~
~kif"k+
U~
Xk-f"
Fig. 4. The effective surface inside which « the average motion » of « the average grain » in respect to its neighbors occurs under perturbations. The turning of powder from one rnetastable state pi _k into another state pk at the k-th perturbation corresponds to the vaulting over from one point of the effective surface to another. Compare with figure 3.
from one metastable state pk- i into another p~ at the k-th
perturbation corresponds
to thevaulting
over from onepoint (u~
j, x~ j
)
of the effective surface to another(u~, xk) Point.
It isimpossible
for averageparticle
to come out of theboundary
of effectivesurface,
itbeing
formed
by
thesurrounding impenetrable particles.
M lo BEHAVIOR OF POWDER UNDER PERTURBATIONS l155
Under a weak
stirring
orjostle
agrain
gets an momentum from one of theneighboring grains along
the normal to theplane
of their tangency. Because of the effective surface is createdby
thesurrounding grains
this momentum is directedalong
normal to it.Having
received a momentum a
particle
moves in thegravity
field. In the first collision with thesurrounding having repacked grains (with
a newpoint
of the effectivesurface)
thegrain
adheres to them
(to
the effectivesurface) losing
its kinetic energy. The last fact shows the dominant role of friction forces in theproperties
ofpowders.
The volume restrictedby
the effective surface is much less thengrain
volume(see paragraphs
3,4), and,
hence, under a weak oneperturbation
a shift of agrain
in respect toneighboring
ones is much less thengrain
size. In order to preventmisunderstanding
it should be noted that our concept does notassume any localization of real
grains
after numerous disturbances. The effective surface issituated in a
configuration (but
not thereal)
space. It determines the correlation of thepositions
ofneighboring grains
before and after aperturbation.
The form of the effective surface
being given,
it won't be difficult toinvestigate
thebehavior of the «average
grain».
Let theparticle,
which had been in theposition
x~, u~ before n-th
perturbation,
get thevelocity
v~along
the normal to the effective surfaceu(x).
Then it moves free in thegravity
fieldd~r/d~
= g
up to collision with the surface in the
point
x~~j, un~ j. Under the next n + lst
jolting
thegrain
gets thevelocity
vn~j and moves from the
position
x~~j, un~j to theposition
x~~~, u~~~ and adheres there and so on, and so on. The
points
x~, u~ and x~~i,u~~ j, x~~ i, u~
~ j and x~~~, u~~~ are connected due to the
folloming elementary
formula of motion in thegravity
fieldU(Xn+I)~U(Xn)
"
(Xn~Xn+1) (~(Xn)) ~) (i
+~
(Xn)) ~) (Xn~Xn+1)~
~
(2.8)
Here
..., n, n + I, n +
2,..,
are the numbers of disturbancesfioltings, stirrings).
In formula(2.8)
we moved on from theparticles
of finite size to thedescription
of their center ofgravity.
In accordance with
(2.6-7)
aposition
of theparticle
on the effective surface determines thedensity
ofpowder
:~
=
~~'~~(~
= l
+u~/d. (2.9)
Pn
(dV )
Here
d
is thelayer
thickness of random closedpacking,
f is thedensity
of the closedpacking (1.3-4).
The transition of apoint
to the bottom of effective surfacecorresponds
to aconsolidation of
powder
dp d~
dlxl
~°'S<°. (2,io)
The minimum
(the bottom)
of the surfacecorresponds
to the closed randompacking.
As to maxhnum value of u it is defined ratherby
a type of structures stable ingravity
field thanby geometric
considerations.The chain of
equations (2.8-9)
relates theposition
of «averagegrain»
x~, u~ on the effective surface and thedensity p~(x~)
ofpowder
before n-thjolting
to tile one ofl156 JOURNAL DE PHYSIQUE II M 10
x~~ j, u~
~ j and the
density
p~~ j(x~
~ j
)
after it. Theequations (2.8-9) formally
solve theproblem
of the weakperturbation
inone-particle approach.
3, The mean field
approach
for the effective surface.In this
paragraph
wedevelop
the mean(or self-consistent)
fieldtheory
for the effective surface.Any
state ofhomogeneous free-floving
medium is describedby
theposition
of theaverage
grain
» on the effective surface. A certainposition
u iscorresponded by
thegiven density
p of apowder
in accordance ~vith formula(2.9).
On the otherhand,
everydensity
iscorresponded by
thepacking
which possesses theperfectly
certain localgeometric
character- istics,specifically,
the certain averageangle
of momentum which is transmitted fromunderlayer
to agrain
free to move(Fig. 3).
Forexample,
thisangle
is markedby
p andequals
60° and 45° for theplane hexagonal
and cubicpackings (Fig. I) respectively.
It means, that everygiven density
p and,consequently,
every givenposition u(p )
of theparticle
on the effective surface are
corresponded by
certain value of theangle
of momentum transmission, and, hence, the certain tangentdu/dx
of the effective surface in thepoint x(p ). (Remind
that due to the definition of the effective surface the direction of momentumtransmission is
perpendicular
toit.) Putting
it another way, thedependence u(x)
= u
fl (x) (3.1)
is not
arbitrary
butstrictly
self-consistent.To obtain this
dependence
let us consider two randompackings
of different densities shownby figure
I and put theregular
ones(Fig. I)
of the samedensity
in accordance to these randompackings.
It isquite
natural to expect in thespirit
of meanfieldtheory,
that the localgeometrical
characteristics of the randompackings
and of thecorresponding regular
ones will coincide. In the framework of thissupposition
the form of the effective surface can be obtained as follows.In the
plane hexagonal packing (p
= 6
fl
the thicknessd
of alayer
or of a row(for example
dashed on inFig. I)
isequal
to D3/2,
where D is thegrain
diameter. Indecreasing density
theparticles
earlierbeing
in the same row(layer)
will occupy several rows (seeFig.
Iand comments to
it).
The thickness of alayer
of aregular plane packing
characterizedby
theangle
fl is D sin fl, and the number of rows which areoccupied by
theparticles
earlierbeing
in the same
layer
ofhexagonal packing
isequal
to 2 cos fl. So alayer
which in thehexagonal packing
had the thickness Dl12
has the thickness 2D sin flcos fl after
swelling
of thepowder.
The difference between these thicknesses isnaturally
to be identified with the ordinate u of the « average »grain
on the effective surface, the ordinatebeing
counted from the bottom of the effective surface whichcorresponds
to the most closedpacking. According
to the concept of the effective surface the
angle
flequals
3u/3x.Expressing
thetrigonometrical
functions flthrough
this derivative andsubstituting
them in the difference of the thicknesses of the closed and unclosedpackings layers
one can obtain thefollowing
differentialequation
describing
the effective surface for thepowder
of disks :an unessential constant
coming
to thedisplacement
of the coordinateorigin being
omitted in theright
hand of differentialequation (3.2).
The solution of theequation
is thefollowing
x/D
=
~
+ ln
(1 ~)
+ 0.053
(3.3)
M 10 BEHAVIOR OF POWDER UNDER PERTURBATIONS l157
0.83 0.637 ~
O.60
1 11
O.50
o88
O.OO 2.0O
1,oo 1.12
O.97 1.02
1 1
O.94 0.92
O.
a) b)
Fig. 5. The effective surface and dependence of the density on the point on it in the mean-field approach for the a) plane powder of disks, b) three-dimensional case, powder of spheres.
The
arbitrary
constant in theright
hand was chosen in such a way that the bottom of the effective surface shouldcorrespond
to the closed random two-dimensionalpacking (0.821).
The form of the effective surface for
powder
of a disks is shown in thefigure
5.In the
regular plane packing
characterizedby
theangle
fl the share of volumeoccupied by grains equals w/4
sin fl. Therefore coordinate x of theparticle
in the effective surface iscorresponded by
thefollowing density
of thepacking
p(x)=( (1+ ()
)~) (((
)~~ (3.4)
The values of these densities range
(Fig. 4)
within interval 0.79-0.821.The same considerations can be
applied
to the three-dimensional case, whereswelling
ofpowder
results in thethickening
of two-dimensionallayers
ofhexagonal
syrnrretry(Fig.
I).So in the closed
hexagonal
three-dimensionalpacking
(p = II/)
the thicknessd
ofa
layer
isequal
to D~fijj.
Inan unclosed
regular packing
theparticles,
which beforeswelling occupied
a one two-dimensionallayer
of the closedpacking (row
of thehexagonal packing
with thickness D
~fijj),
after theswelling
will takeup another more loose and thicker
layer (number 3Dcos~fl
ofrows
having
thickness D sin fleveryone).
The overall thickness d~ of the new layerconsisting
of theparticles
which weredisposed
in onelayer
of thehexagonal packing
may beeasily
shown toequal
3 D cos fl ~ sinfl. Identifying
thethickening
d~d
of thelayer
ofswelling packing
ascompared
with thelayer
of the closed(hexagonal)
one with the ordinate of the «average
particle
» on the effective surface u(see (2.7))
weobtain
(having expressed
theangle
flthrough
the tangent3u/3x)
thefollowing equation
for the form of the three-dimensional effective surface~
=
31~ l~li
+Ill
l~l~~~ (3.5)
l158 JOURNAL DE PHYSIQUE II N 10
The
arbitrary
constant connected Pith theoption
of the coordinateorigin
is omitted. Theparametric
solution of theequation (3.5)
isI
=
~
~
~ + 0.949 D
(I+t)/~
2 1/2 2
~=3(fi) (2-(fi)j (3.6)
D I+t I+t
and is shown in
figure
5. The numerical constant in theright
hand side of the firstequation (3.6)
was chosen so that the minimum of the effective surface shouldcorrespond
to the random closedpacking
ofspheres (0.637).
One can make sure that volume share
occupied by grains
in theregular
three-dimensionalpacking
characterizedby
theangle
fl isw/9 /cos~
fl sin fl~particularly,
for the closedhexagonal
onefl
=
I/ /
and the share of volume isequal
tow/3 /).
So, theposition
x(p
of the « averageparticle
» on the effective surfacecorresponds
to thedensity
ofpacking
~ d~ 2 3/2 d~ -2
~ ~~~
9i~
~ dX dX ' ~~ ~~the
density ranging
vithin 0.52-0.637.Formulas
(3.3-4)
or(3.6-7)
obtained above present theexamples
of a constructive realization of the idea of the effective surface set forth inparagraph
2.Comparing (3.5,
7~(or (3.2.4))
one finds that formulas(3.4, 7)
obtained from apurely geometric
considerationssatisfy
to and areonly particular
case of thegeneral
forrnula(2.9).
Let us consider the
following simple
models of the effective surfaces@
=a
(j(, (3.8)
~ =(j~j~ (3.9)
The
expression (3.8) approximates
the effective surface(3.3)
for theplane powder
of disks in the whole ange of densities, so doesexpression (3.9)
for the effective surface ofspheres (3.6)
except of the very narrowvicinity
of the surface bottomcorresponding
to the closed randompacking.
Note, that
according
to results(3.3, 6)
under a weakperturbation grains
ofpowder
move in respect withneighbor
ones on amagnitude
of order of10~'
-1 of their diameter. Thatcoincides with the results of natural
experiments.
Thus the parameter a introduced in(3.8, 9)
have to be assumeda l 10~ '
(3.10)
and
physically
allowable values of theposition
x range within 0.lD-lD.4. Swelling and subsiding ~packing down) of powder under perbwbation.
The nature of
subsiding (or swelling)
ofpowders
is illustratedby figure
3. There localgeometrical configurations (of
the type of theconfiguration
of thegrains1,
2, 3 and 11, 12, 14) inside which a relative rearrangement of aparticle
can occur are shown. The direction ofan momentum transmission is seen to
depend
upon the distanceI,
betweengrains
inpacking
and,
hence,
upon thedensity
of thepacking.
Thehigher
thedensity
is the more the vertical component of momentum obtained instirring
does and the more is « atendency
» forpowder
N lo BEHAVIOR OF POWDER UNDER PERTURBATIONS 1159
to swell. It means that the less
density (the higher
apoint
on the effectivesurface)
is the more vertical the walls of the effective surface are. It is this situation that takesplace
for the effective surfaces(3.9)
and(3.3, 6)
obtained in the mean fieldapproach.
That iswhy
under the same outward disturbance(under
the same averagemagnitude
of thehanding velocity
~ the behavior ofpowder depends
on its state, a friablepowder subsiding,
a compact oneswelling.
However both the last and the former are to arrive at theequilibrium
for the certainregime
ofperturbation density
p,regardless
of their initial state.The behavior of
free-flowing
medium is describedby
the behavior of the average »grain
on the effective surface. The behavior of the
grain
is determinedby
the chain ofequation (2.8),
whichgives
a scheme of one dimensional Puankare's mapsUn+I "
Un+I(Un),
Xn+I"Xn+I(Xn),
Pn+I"
Pn+I(Pn).
Here x~, u~ is a coordinate of the «average»
grain
on the effective surface andp~ is the
density
ofpowder corresponding
to thepoint
x~, u~.The method of Poincark's maps makes it
possible
toinvestigate complicated
manydimensional
dynamic
systems to which thepowders undoubtedly belong.
Tostudy qualitat- ively powder dynamics
weapply
the very illustrativetechnique
of a construction of Poincark'smap
diagrams [29].
For this purpose scheme of mapsgiven
in aimplicit
form should be rewritten in theexplicit
form.Analytically
it can be done for thesimple
forms of the effective surfaces(3.8, 9).
Having
substituted theexpressions (3.8, 9)
in the recursive correlations(2.8)
andsolving
the last in respect to +~~ j one can obtain for the first effective surface the
following explicit
forms of the maps
respectively
jx~~j>0, x~>0
x~~j =x~±
(a +a~')M~'
~ x~~j <0,x~<0
x~~j =x~±
(a -a~')(2M)~'± (41)
±~/(a-a~')~±8ax~M(2M)~'
jx~~j>0, x~<0
~~
x~~j <0,
x~>0,
whereA=
~~~),
M=~(l+a~~),
2V 2
and for the effective surface
(3.9)
as follows(A-a)x(+ (A-2a)a~~x~
x~~ j = ~ ~ ,
(4.2) (A+a)x~+Aa~
where
A=
~~~),
amA.2V
Here V is the average
velocity
obtainedby grains during repacking
which characterize theintensity
ofperturbation.
Typical diagrams corresponding
to the maps(4.1, 2)
are shown infigure
6. The sequence of thepoints
n, n + I, n + 2,(...,
k, k + I, k + 2, describes thepacking
downl160 JOURNAL DE PHYSIQUE II N lo
x
~i
x
Fig. 6. The typical diagrams of a packing down and a swelling of powder calculated for the effective surfaces a) 3.8, b) 3.9. The sequences of points n, n + I, n + 2, (... k, k + I, k + 2, describe a
packing down (swelling) of powder after n-th, n + lst, n + 2d, (k-th, k + lst, k + 2d, ...) stirring.
Both sequences converge to the fixed 2-cycle, which is corresponded by the density equilibrium for the certain intensity of a shaking.
p P
P
~
/~
n n n+I
I n-I n n+i I n-I n n+[
P P
~
/~ ~k+I
p ~k+[
~
~ k-I
~ ~
l. k-I k k+i i k-I k k+I
Fig. 7. A possible behavior of a density under perturbations of a given intensity which is described by the maps (4.1, 2).