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Integral equation for nonequilibrium chemical potential
and the Kirkwood diffusion equation: derivation from
the generalized Boltzmann equation
Byung Chan Eu
To cite this version:
Integral equation
for
nonequilibrium
chemical
potential
and
the Kirkwood diffusion
equation:
derivation from the
generalized
Boltzmann
equation
Byung
Chan Eu(*)
Department
ofChemistry
andDepartment
ofPhysics,
McGillUniversity, Montreal,
PQ, Canada H3A 2K6(Reçu
le 13 avril 1989,accepté
le 8septembre 1989)
Résumé. 2014 Dans cet
article,
l’équation cinétique
des fluidessimples
denses estgénéralisée
etappliquée
à l’établissement d’uneéquation intégrale
pour lepotentiel
chimique
horséquilibre
etde
l’équation
de diffusion de Kirkwood des fluidespolyatomiques
denses(polymères,
parexemple).
La déduction demande lagénéralisation
del’équation intégrale
de Kirkwood à des fonctions de distribution deconfiguration, l’équation intégrale
dupotentiel chimique
local au casdes fluides
polyatomiques
horséquilibre,
et un ensembled’ équations
d’ évolution des variablesmacroscopiques.
Leséquations
d’évolution des variablesmacroscopiques
et lathermodynamique
des processus irréversibles ont les mêmes structures
mathématiques
que dans le cas des fluidessimples
denses. Lesliquides plus
ou moinssimples
sont traitésséparément
dans cette théorie, par différentesintégrales
de collisionqui
interviennent dans leséquations
d’évolution(équations
constitutives)
pour divers flux tels que les tenseurs de contraintes, les flux de chaleur et lesflux
diffusifs.L’équation
de diffusion de Kirkwood est obtenue pour la fonction de distribution deconfigurations
d’une moléculepolyatomique,
en utilisant un ensembled’approximations
sur leséquations
des fonctions de distribution et de diffusion du flux de masse. Commeexemple
d’application
deséquations
d’évolution aux variablesmacroscopiques,
on considère la viscosité d’une solution binaire de fluidepolyatomique
etmonoatomique
et on obtient une formule pour laviscosité
intrinsèque
en termesd’intégrales
de collision. Cette formule foumit uneexpression
demécanique statistique
pour la viscositéintrinsèque.
Abstract. 2014 In
this paper the kinetic
equation
for densesimple
fluidsreported previously
isgeneralized
andapplied
to derive anintegral equation
fornonequilibrium
chemicalpotential
and the Kirkwood diffusionequation
for densepolyatomic
fluids(e.g., polymers).
The derivationrequires
ageneralization
of the Kirkwoodintegral equation
forconfiguration
distributionfunction, the
integral equation
for local chemicalpotential
to the case ofnonequilibrium
polyatomic
fluids, and a set of evolutionequations
formacroscopic
variables. The evolutionequations
formacroscopic
variables and irreversiblethermodynamics
are found to have the samemathematical structures as for dense
simple
fluids. Thesimple
andnonsimple
fluids aredistinguished
in the presenttheory by
the different collision bracketintegrals appearing
in the evolutionequations
(constitutive equations)
for various fluxes such as stress tensors, heat fluxes ClassificationPhysics
Abstracts 05.00 - 51.00 - 66.00(*)
Mailing
address :Department
ofChemistry,
McGillUniversity,
801 Sherbrook Street West, Montreal, Quebec, Canada H3A 2K6.and diffusion fluxes. The Kirkwood diffusion
equation
is obtained for theconfiguration
distribution function of a
polyatomic
moleculeby using
a set ofapproximations
on the distribution function and the mass flux diffusionequations.
As an illustration ofapplication
of the evolutionequations
formacroscopic
variables, theviscosity
of abinary
solution ofpolyatomic
and monatomic fluids is considered and an intrinsicviscosity
formula is obtained for it in terms of collision bracketintegrals.
This formulaprovides
a statistical mechanical formula for intrinsicviscosity.
1. Introduction.
Statistical mechanical theories
[1-5]
of dense fluidsconsisting
ofcomplex
molecules(e.g.,
polymers
andhydrocarbons)
oftenproceed
on the basis of intuitive models andapproxi-mations that
produce
tractable butonly qualitatively
correct results. In such theories[1-5]
and also inequilibrium
theories[6-8]
of densesimple
fluidsapproximations
of various kinds are made in essence for chemicalpotentials
for the fluids of interest on the basis of models. As often shown inequilibrium theory
[6-8]
of densesimple
fluids,
chemicalpotentials play
animportant
role incalculating thermodynamic
functions,
and there is agreat
deal ofinsight
one cangain by studying approximation
methods for chemicalpotentials.
The same would be truefor
nonequilibrium polyatomic
fluids. In this paper wedevelop
a formaltheory
fornonequilibrium
chemicalpotentials
and derive the Kirkwood diffusionequation
forconfigur-ation distribution function
closely
related to theformer,
which would alsohelp
usdevelop
someapproximate
kinetic theories ofcomplex
molecular fluids.Kinetic
theory
oftransport
processes in dense monatomic fluids and the attendanttheory
of irreversiblethermodynamics
have been studied in recent papers[9-11]
in which we have made use of thegeneralized
Boltzmannequation
for densesimple
fluids. The formalismsdeveloped
therein have beensuccessfully applied
torheological problems
[10,
llb, c]
andgeneralized
hydrodynamics
of non-Newtonian fluids[llb-d].
They
are alsosuggestive
ofgeneralization
tononsimple
fluids and condensed matter ingeneral.
For the stated aims in this paper we firstpresent
a formalgeneralization
of thetheory
to a fluid mixtureconsisting
ofpolyatomic
molecules or a mixture of monatomic andpolyatomic
molecules. We will show that the evolutionequations
for variousmacroscopic
variables such as thedensity, velocity,
internal energy, massfluxes,
heatfluxes,
stress tensors, etc. remainformally
similar to those obtained for densesimple
fluidsexcept
for the necessarychanges arising
from the appearance of the internaldegrees
of freedom absent in the case ofsimple
(monatomic)
fluids. Thesimilarity
we observe between themacroscopic equations
fornonsimple
andsimple
fluids is notsurprising
since
nonsimple
andsimple
fluids are, from the continuumtheory
standpoint,
distinguishable
only
in terms oftransport
coefficients and related molecularparameters.
The situation is therefore similar to the one in theequilibrium
thermodynamics
where,
forexample,
the virialequations
of state are similar for bothsimple
andnonsimple
fluidsexcept
for the details of the virial coefficients which reflect the nature of interactions and themolecularity
of the fluid inquestion.
By
using
the formalismdeveloped,
we show that whenpolyatomic
molecules areinterpreted
to includepolymers,
thepresent
kinetictheory
contains in it the well knowntheory
of Kirkwood[12]
onpolymer
solutions,
since the Kirkwood diffusionequation
forconfiguration
distribution function can be obtained for apolymer
solution if a set ofapproximations
is made. We will list theapproximations
in the text. The Kirkwood diffusionequation
holds for dilutepolymer
solutions,
but its extension into thehigher
concentrationconcentrated solutions if
pair
correlation functions forpolymers
were included in the calculation of conditional diffusion fluxesappearing
in thegeneral theory.
(Here
we meanby
a conditional diffusion flux the mass flux of aparticle, given
a constrainedconfiguration
of otherparticles).
It appears thatalthough
this kind ofgeneralization
is feasibleby
proceeding
onestep
further than the Kirkwoodtheory requires
incalculating
the effects ofpair
correlations,
theresulting theory
would becomeunwieldy
and cumbersome. We find itsimpler
to use the stress tensor and other evolutionequations
to calculateviscosity
and othertransport
properties
of apolyatomic
fluid. The formalism forcalculating viscosity presented
in this paperprovides
an alternative route distinctive from the Kirkwood line of attack.With the evolution
equations developed,
we theninvestigate
transport
processes of abinary
densemixture,
with aparticular
attentionpaid
to viscousphenomena
for their obviousutility
in connection withrheology
ofpolyatomic,
e.g.,polymeric, liquids.
In section 2 the kinetic
equation
and the evolutionequations
arepresented
forpolyatomic
fluids. The latterequations
are to becompared
with those forsimple
dense fluids with theemphasis placed
on thepoints
ofdifference,
if there is any.By using
themacroscopic
evolutionequations,
wedevelop theory
of irreversiblethermodynamics
whose structure also remains the same as that forsimple
dense fluids. In section 3 wepresent
a « derivation » ofthe Kirkwood diffusion
equation
forconfiguration
distribution function which wasoriginally
obtained with the Brownian motion model for motion ofparticles
in apolyatomic
orpolymer
molecule. Theequation
can be obtained without a Brownian motion model.Moreover,
statistical mechanical formulas forparameters
in theoriginal
Kirkwood diffusionequation
are identified. We alsopresent
the Kirkwoodintegral equation
for correlationfunctions,
e.g.,configuration
distribution functions andpair
correlationfunctions,
fornonequilibrium,
and anintegral equation
fornonequilibrium
chemicalpotentials.
These twoequations
would facilitatestudy
ofnonequilibrium
effects on correlation functions andthermodynamic
quantities
ingeneral.
In section 4 formulas fortransport
coefficients areobtained
in terms of collision bracketintegrals
for densepolyatomic
fluids. These results reduce to theChapman-Enskog
firstapproximation
fortransport
coefficients for a dilute fluid as thedensity
of the fluid decreases.Specializing
to abinary polymeric
solution,
we obtain the intrinsicviscosity
formula in terms of the collision bracketintegrals.
This formulaprovides
an alternative method of calculation for intrinsicviscosity
which isbasically
different from theexisting
methods. Section 5 is for discussion and conclusion.2. Kinetic
equation
andmacroscopic
evolutionequations.
2.1 PRELIMINARY. - In view of the
complexity
of notation necessary fordescription
ofpolyatomic
molecularsystems
it is useful tosystematize
thesymbols
and their usage. We will reservesubscripts a,
b,
c, ... forspecies, subscripts i, j,
k, f,
... formolecules,
subscripts q, s, t,
... for atoms or groups in a molecule. Thesesubscripts
will often appearconsecutively.
Forexample,
maq
means the mass ofparticle
or group q in molecularspecies
a, andraiq
means the coordinate vector ofparticle q
in the i-th molecule ofspecies
a. With this code for usage of thesubscripts pertaining
toparticles
in a molecule of aspecies,
we now definesymbols :
Maq =
mass of theq-th particle
(or group)
inspecies
a.raiq =
position
vector, relative to a fixed coordinateorigin,
of theq-th particle
in the i-thcomposite particle
(molecule)
ofspecies
a.Rai =
center of mass vector of the i-thparticle
ofspecies
a.aiq
= distance of theq-th particle
inspecies a
from its center of mass located at=
velocity
vector of theq-th particle
in molecule i ofspecies
a.= center of mass
velocity
vector of molecule i ofspecies a
relative to the coordinateorigin.
=
maq
Valq
= momentumconjugate
toraiq.
=
ma
V ai
= momentumconjugate
toRai .
- E
Maq,
the total mass of molecularspecies
a.qEa
-
maq
gaiq,
the momentumconjugate
totaiq-The dot over a
symbol
means the time derivative :e.g., g
=de/dt.
In the above
system
of coordinates thereclearly
holds the relationfor every
position
vectorsof q
E i andconsequently
This
identity
is easy toverify
if the definition of the center of mass of a molecule is usedalong
with(2.1).
Thisimplies,
of course, the relationIf the
system
consists of rspecies
which may bepolyatomic
or monatomicmolecules,
the Hamiltonian may be writtenor, with the center of mass kinetic energy and the internal energy of the molecules made
explict,
Here
where
Vai
is thepotential
energy of an isolated molecule i E a. Thepotential
energywhere
For dense
polyatomic
fluids in which we areinterested,
expressing
the Hamiltonian in thecenter of mass energy, the energy for internal
degrees
of freedom and the intermolecular interaction energy is notparticularly advantageous
mode ofrepresentation
for energy from the mathematicalstandpoint.
The
phase
ofNa, Nb,
...particles
will be abbreviated withX(N)=X(Na,Nb’’’.):
where {Paiq}
and{raiq}
respectively
stand for the momenta and coordinates of a set ofparticles
in N molecules ofspecies
a, etc., and2.2 KINETIC EQUATION AND MACROSCOPIC EQUATIONS. - We consider
an
r-component
fluid mixturecontaining Na, Nb, N c’
... molecules forspecies a,
b,
c, ... that may bepolyatomic,
diatomic or monatomic. The mixture contains at least onepolyatomic species.
The volume of thesystem
is V. The evolution of thesystem
isstatistically
describedby
the distribution functionobeying
a suitable kineticequation.
In the case of monatomicfluids,
either of a
single
component
or ofmultiple
components,
we have shown that the kineticequation
may be assumed to follow ageneralized
Boltzmannequation
[9].
Thisgeneralized
Boltzmannequation
has been deducedby using
thesimilarity principle
[9e]
which may be stated as follows : there is a setof
equations
of
motionfor
distributionfunctions
atdifferent
levelsof
correlation which are similar in their basic mathematical structures andproperties
andparticularly
in their broken time-reversal symmetry. Theseequations
arestructurally
similar tothe Boltzmann
equation
for dilute gases. Thisprinciple together
with the Boltzmannequation
for dilute gases has led us to a kineticequation
for distribution function¡(s) (x (s) ;
t )
for clustera
consisting
of s monatomicparticles
where
Ls
is the Liouvilleoperator,
TSI S2 ... SN
(z )
is the collisionoperator
for N clusters each of which consists of sparticles (thus
sl, s2, etc.meaning
thefirst,
second,
etc. clusters of sparticles),
ctl is the renormalized(i. e. ,
scaledup)
volume of thesystem
lu = NV with Nstanding
for the number ofclusters,
and X is the number ofparticles,
X = sN. This mannerof renormalization leaves the bulk
density
invariant : n =lim s /V
= limX 1 crI .
In(2.8)
thelimit z - + 0 must be understood. This
parameter
z i e (e :::. 0)
gives
a measure of duration of molecular collisions which take thesystem
of molecules from an initial to a final state. This collision time is assumed to be much shorter than the time span(kinetic
timescale)
over which the distribution functions evolve.Therefore,
the kineticequation (2.8)
must beregarded
as atime-coarse-grained
equation
for distribution functions that are averages offine-grained
distribution functions over the duration of collision. The collision time span is difficult to
The distribution functions
i,,(’)
are normalized as follows :and if there is a molecular
quantity
A (x (’) ;
t )
such thatwhere Aj
aresingle-particle
variables andAk
aretwo-particle
variables,
then the average for A at r isgiven by
We will henceforth use
angular
brackets to denote the average of mechanicalquantity
A(x(’»
over thephase
space with the statisticalweight
In
(2.10)
the second line follows from the firstby
virtue of the normalization condition(2.9),
and the third line from the secondby
theidentity
andsymmetry
of the clusters(subsystems).
The last line issimply
the definition ofF (X)(x (X) ;
t ),
but it may be also construed as the usual definition of A which iscommonly
encountered in the dense fluid kinetictheory
based on the Liouvilleequation :
seeIrving
and Kirkwood[13].
The kinetic
equation (2.8)
with the rule ofaveraging
(2.10)
provides
a means to calculate necessarymacroscopic
variables tostudy
irreversible processes in densesimple
fluids. Theargument
[9e]
used to obtain the kineticequation
(2.8)
and the rule ofaveraging
(2.10)
aregeneral
since no reference is made to themolecularity
of the substanceinvolved,
and hence can be sogeneralized
as to describe irreversible processes in densepolyatomic
fluids.r
We
imagine
N clusters of s= L sa
particles
where Sa
stands for the number of molecules ofa = 1
species
a. Then with themeaning
of thephase
forparticles
extended as in(2.7)
we canThe collision
operator
TS(l),
s(2), ...,
s(N)(z) = TS1,
S2, ..., SN(z)
for Xparticles
broken up into Nclusters of s molecules is determined
by
the classicalLippmann-Schwinger equation
[9a]
where
c(N)== {s(l),
s (2 ),
..., s(N)}
stands for N clusters of sparticles,
£C’(N)
denotes theintercluster interaction Liouville
operator
andR(O ) (z)
is the resolventoperator
for Nindependent
correlated clustersHere
Ls(a)
is the Liouvilleoperator
for the o’-th cluster and has the form asgiven
in(2.11).
Thenby using
the Boltzmannequation
for apolyatomic
gas mixture and thesimilarity
principle
it ispossible
to arrive at the kineticequation
where
Here
sa ( a )
stands for the number ofparticles
ofspecies a
in cluster a. The kineticequation
isa
postulate
for thepolyatomic
fluid inquestion.
Itclearly
remainsstructurally
the same as the densesimple
fluid kineticequation
(2.8)
except
for the increased dimension of thephase
space to accommodate the internaldegrees
of freedom forpolyatomic
molecules. Thesignificance
of theparameter
z in(2.12a), (2.12b)
and(2.13)
is the same as discussed in connection with(2.8).
In(2.13)
the limit £ -. + 0 must be understood as taken. We thus mustregard
the distribution functions in(2.13)
ascoarse-grained
ones which evolve on a kinetictime scale much
longer
than the collision time scale on which the collisionoperator
TS(l), s(2), ..., s(N)
is defined.Appearance
of the collisionoperator
in the kineticequation
presumes that there are wellseparated
time scales of molecular collisions and kineticevolution of distribution functions. Existence of such time scales is
generally
assumed in modern works[14]
on kinetictheory
and dense fluids inparticular.
As a matter offact,
abinary
collisionoperator,
aparticular example
of such collisionoperator,
can be used to write the Boltzmann collisionoperator
as is often done in the derivation of the Boltzmannequation ;
see references[9a]
and[15].
In this case it ispossible
to showunambiguously
that£-1
1coarse-grained
in space so thatthey
do notchange
over the collision volume. We remark that theLaplace
transform[9a]
associated with the definition of collisionoperators
must beinterpreted
as a time coarsegraining
over the collisional time scale.Because of the
similarity
of the kineticequation
(2.13)
to(2.8)
we obtainmacroscopic
equations
which are alsostructurally
similar to those derived from(2.8).
Sincethey
may be derived from(2.13)
in the same manner as from(2.8)
wesimply
list theequations
below. We will useangular
brackets to denote theaveraging
over thephase
space of apolyatomic
system :
It is
important
to recall the rule ofaveraging
described in(2.10)
when we derive the evolutionequations given
below. We first define various statistical formulas formacroscopic
observablesappearing
in thepresent
theory.
To this end it is necessary to define thefollowing
molecularexpressions
for various moments :where with the notation
It is useful to note that the definitions of
haB)
given
above are correct to theapproximation
in which the terms of0(À )
orhigher
in theexpansion
of theoperator
exp (-
’k raiq ;
bksV r)
areneglected.
This latteroperator
appears in the termscontaining
theforces gaiq;
bles. Inclusion of theneglected
terms would bemathematically
correct, but very difficult to handle inpractice.
Moreover,
they
appear to benonphysical
sincethey
arise from the delta functions which mayhave too
sharp
a distribution. Forp a, ha
and pa
see(2.17), (2.33)
and(2.49b)
below. With the definitions ofh (’)
we now calculate variousmacroscopic
variables as follows :We construct an
antisymmetric
tensor S =p5
withangular
momentum vector S as follows :These
macroscopic
variablesobey
thefollowing
conservation laws and evolutionequations :
In the evolution
equations
above,
i.e.,
theenthalpy
per unit massof a, ta
is the internal energydensity
of a, p,, is thehydrostatic
pressure andwhere
/ïJ
are the molecular formulas for the stress tensor, heatfluxes,
massfluxes,
etc.defined in table I. We call
A«)
dissipative
terms sincethey
areintimately
related to theentropy
production
due todissipative
processes such as viscousflow,
heat conduction andmass diffusions
occurring
in thesystem.
The conservation
equations
and the evolutionequations
listedabove,
with theexception
of theangular
momentum conservationequation,
have the same structure as thoseappearing
in the densesimple
fluid kinetictheory
[9b-g]
except
for the fact that themacroscopic
variables consist of the center of mass and internal contributions and thedissipative
terms must reflectthe involvement of the internal
degrees
of freedom in the molecular collision processes in thesystem.
Whatever the molecular collisionaldetails,
thedissipative
terms may beexpressed
in terms of stress tensors, heatfluxes,
massfluxes,
etc. whichincidentally
are henceforth calledsimply
fluxes,
and the fluxdependence
of thedissipative
terms is similar to thesimple
fluidcounterpart except
that the coefficients reflect themolecularity
of the fluid inquestion.
Thesecoefficients consists of collision bracket
integrals
which indicates the details of collisions between theparticles
in thesystem.
Thereforethey
are the source of information on molecularproperties
of thesystem
in thepresent
theory.
It isimportant
to note that the evolutionequations
(2.29)-(2.32)
are in a fixedframe,
butthey
can be converted to thecorotating
frame versionby using
the rulesreported
in reference[9g].
(*)
These definitions off/Ja)
andya)
are correct to theapproximation neglecting
the terms ofo (À)
orhigher
in the operatorexp (- À r aiq ; bks . V r )
which also appears in the definitions ofTable 1
(continued).
{ABC}
= sum of nonreduntantsymmetrized products
of the vectors or tensors.2.3 ENTROPY AND THE EQUILIBRIUM SOLUTION TO THE KINETIC EQUATION. - The kinetic
equation
(2.13)
satisfies the H-theorem if thesolutions,
distributionfunctions,
belong
to the zero class functions[9a]
for which the totaleigenvalue
of the Liouvilleoperator
N
£0
= Y
Ls(a)
equals
zero. Theequilibrium
distributionfunction,
forexample,
has thisa = 1
property.
Thenonequilibrium
distribution function must be chosen in such a way that the H-theorem issatisfied,
and the modified moment method[16]
we make use of in this series of work ensures that therequirement
be met.The
entropy
of thesystem
is definedby
the formulaand for zero class functions
[9a, e]
there holds theinequality
equilibrium
distribution function in fact isuniquely given by
thevanishing
collisionintegral
of(2.13) :
We note here
again
that the limit s -. + 0 should be understood in(2.42).
Equation
(2.42)
means that the
operand
is a collisional invariant. It can beshown,
by
following
theprocedure
described elsewhere
[9a],
that the solution toequation
(2.42)
subject
to the conservation of energy and momentum is the canonical distribution functionwhere
Hs)
is the Hamiltonian of sparticles
and is
proportional
to thereciprocal
temperature.
Therefore we obtainwith q
denoting
the normalization factor. the number of internal
degrees
offreedom ,
and h is the Planck constant. It is
put
into theintegral
to make the latter dimensionless. The factor N! is alsoput
in there tocompensate
for theovercounting
of thefrequency
of states.The
nonequilibrium
distribution function is now looked for in a form to conform to the H-theoremby taking
anexponential
formand the normalization factor
.ae (X)
is definedby
theexpression
with
/3
=1 IkB
T. Thetemperature
T is definedby
the statistical formulaThat
is,
thetemperature
is definedby
the average kinetic energy. It is consistent with the notion oftemperature
being
a measure of motions ofparticles
in thesystem
and also with the definition of T in the case of densesimple
fluids. The reader is referred to reference[9e]
for a more detailed discussion ontemperature.
The factors N! andh f in
(2.48)
appear for the same reason as for theequilibrium
normalization factor(2.45).
The pressure of thesystem
is defined in a manner similar to that in the densesimple
fluidtheory :
where
It is to be noted that the
temperature
is taken not with theequilibrium
temperature,
but with thetemperature
as defined in(2.49a).
ThereforeFI(Z)
is different fromF(x)
by
thetemperature
factor. Often in kinetictheory,
thehydrostatic
pressure is definedby
[18]
thetrace of stress tensor : pa = Tr
Pa/3.
Since the stress tensor isgenerally
timedependent
for anonequilibrium
system,
this definition makeshydrostatic
pressure anonequilibrium
quantity.
Moreover,
it leads to the conclusion thatda
=pâ,,
in(2.36)
vanishes and as a consequencethe dilatational
part
of theentropy
production accompanying
theexpansion
orcompression
of the fluid vanishestogether
with the bulkviscosity.
Therefore,
the author believes that it is notappropriate
for dense fluids to definehydrostatic
pressure with the trace of stress tensor as mentioned earlier. The definition in(2.49b)
does not have thedifficulty
mentioned andeasily
reduces to theequilibrium
statistical mechanical formula forhydrostatic
pressuregiven
interms of the virial tensor.
If
H{N’)
isdecomposed
intocomponents
related to various fluxes in thesystem
which is
positive
for all values ofxJa}:
Theentropy
fluxJ,
isgiven by
the formulawhere
la
is the chemicalpotential
of a per unit massand
The unknown
xJa}
are determinedby
theconsistency
conditionwhich may be looked upon as a differential
equation
for theentropy
density
sinceHère
and
Z
are defined in(2.29)-(2.32).
Attendant to(2.56),
there holds the extended Gibbs relationEquation
(2.57)
is a consequence of(2.58).
Theentropy
density,
entropy
flux andentropy
production
form a balanceequation
where
This
inequality
isequivalent
to the second law ofthermodynamics
as was shown elsewhereThe
macroscopic
evolutionequations
(2.24)-(2.32), (2.58)
and(2.59)
have the same form as thoseappearing
in the densesimple
fluidtheory
[9]
except
for the statistical definitions ofmacroscopic
variables and the details of thedissipative
terms which reflect themolecularity
of thesystem
inquestion.
This isquite
understandable since thesemacroscopic
equations
aremeant for gross
description
of behavioruniversally
exhibitedby macroscopic
systems
and,
in thisparticular
case,by
apolyatomic
fluid.3. The Kirkwood diffusion
equation.
Kirkwood
[12]
proposed
a Brownian motion model forpolymeric
solutions which has beenextensively
usedby
Kirkwood himself and later workers[19-22]
forstudy
ofviscoelasticity
ofpolymeric
solutions. In the model a diffusionequation
is obtained for theconfiguration
distribution function of apolymer
when a set ofapproximations
andassumptions
is made. The Brownian motion of beadsmaking
up apolymer
chain is one of theassumptions.
In this section we show that the Kirkwood diffusionequation
can be obtained within the framework of thepresent
polyatomic
fluid kinetictheory.
The result itself is not new, but its derivation from thegeneralized
Boltzmannequation
demonstrates the power of the latter for kineticphenomena.
Furthermore,
there are acouple
of intermediate results necessary for the derivation which turn out to be new fornonequilibrium polyatomic
fluids but also can be useful forcalculating
some of theirnonequilibrium
properties.
The intermediate results inquestion
are thegeneralized
Kirkwoodintegral equation
for correlation functions and chemicalpotentials
when there existnonequilibrium
fluxes in thesystem.
Theseequations,
whenappropriately
solved,
wouldyield
themagnitude
of the effects on correlation functions ofnonequilibrium
processes, e.g., shear-induced distortion ofpair
correlationfunctions,
etc.They
have, therefore,
apotential
forapplication
to studies ofnonequilibrium
fluidproperties.
3.1 GENERALIZED KIRKWOOD INTEGRAL EQUATION. - To carry out this
part
of discussion we assume that the interaction energy of thesystem
consists ofpairwise
additivepotentials.
We therefore may writeNow
following
Kirkwood[23],
we introducecharging
parameters
[6]
which indicate thestrengths
of interactions betweenparticles
in thesystem.
It is sufficient for our purpose todesignate
aparticular
molecule,
say, al and consider its correlation with the rest of thesystem.
Thusdenoting
thecharging
parameter
by e,
we may write thepotential
V for thesystem
in the formHere the
charging parameter e
rangesfrom e
= 0to e
= 1. Thusat e
= 0 theparticle
al is
completely decoupled
from the rest of thesystem
andat e
= 1 it isfully coupled
with allThe
potential
energypart
h (’)
of the molecular formulas for fluxesh,,q
can be also writtensimilarly :
These
decompositions
(3.2)
and(3.3)
will bepresently
used in the derivation of thegeneralized
Kirkwoodintegral equation.
,We now define the
configuration
distribution function1JI’a(lR, t)
where R stands for the setof coordinates for
particles
in apolyatomic
(e.g., polymer)
molecule,
IIB ={Raiq} :
This distribution function
gives
theprobability
offinding particles q
E a atRaq
for all q E a at time t. If thecharging
parameter e
is notequal
tounity,
thenfor the
configuration
distribution function atarbitrary
Theconfiguration
distribution function1/’ a
is amass-weighted
reduced distribution functiondescribing
the evolution of theconfiguration
of asingle polyatomic
moleculeinteracting
with the rest of thesystem.
In(3.5)
we have inserted theparameter e
in F (oN’) to indicate thatparticle
al ispartially
«charged
».We may write
It is also useful to define
pair
correlation functionsand the
symbol
where
The reduced distribution function
V(2)
describes the correlation between a molecule ofspecies a
andparticle s
ofspecies
c. This is thecounterpart
of thepair
correlation function for asimple
fluid.Differentiation of
(3.5)
withrespect to e
and use of(3.6)
together
with theappropriate
definitions ofH(N)(e), H1(x)(e)
andA (x)(e)
yield,
after somealgebraic manipulations,
thefor which we made use of the
identity
and the definition
Equation
(3.9)
is thegeneralized
Kirkwoodintegral equation
for1/’a(lR, t ).
If(3.7)
is differentiatedwith e
and a similar calculation ismade,
there followintegral equations
forâ 2 cs
and
so on, thatis,
essentially
anonequilibrium
Bogoliubov-Born-Green-Kirkwood-Yvon(BBGKY)
hierarchy
for correlation functions. It is ofnonequilibrium
since there arenonequilibrium
fluxesappearing
in theequations.
Theseequations
reduce to those in theequilibrium
BBGKYhierarchy
[14a-d]
as the fluxes orxJa)
vanish for all a and a The termscontaining
xJa)
are the new features in thegeneralized
Kirkwoodintegral equation. They
should inprinciple
be able to account fornonequilibrium
effects on theconfiguration
distribution of
polyatomic
(e.g., polymer)
molecules innonequilibrium
flux fields. Since(3.9)
is sufficient for the purpose of thepresent
work we will not work out theequation
for1/’ Js
here. It isstraightforward
to derive theintegral equation
forP (2 )
and thesubsequent
members of thehierarchy.
3.2 LOCAL CHEMICAL POTENTIALS. - The
equation
for a local chemicalpotential
can beobtained
by following
the sameprocedure
as for dense monoatomic fluids when(3.2)
and(3.3)
are usedalong
with the definition of A(e).
Since it will berepetitive
if we gothrough
thederivation in
detail,
we willsimply
present
the result below. When the volume and thetemperature
arekept
constant the chemicalpotential
1£a may be written as[6, 23]
The
one-particle
chemicalpotentiel
F£o a
is definedby
the formulafor
particle a1, na
=X a/CU’,
andxi(n’ ’)
collectively
stands for thephase
of the internaldegrees
of freedom for molecule al. With this definition of
.°
we may writeand thus
By using
thisidentity
we findin
the formEliminating
the second term on theright
hand side of(3.15)
by using
(3.9),
we obtain theequation
for local chemicalpotential
J.L a :where qa is such that
If the
nonequilibrium
contribution to qa isneglected,
then we findwhere
qâint )
is the internal molecularpartition
function for thepolyatomic
molecule in hand. In the last term in(3.16)
the sum over s is restricted to those of s = q if c = a. Thatis,
P 121
is the «pair
correlation function » for a molecule ofspecies a
andparticle s
in anotherspecies
if c =/= a or anotherpolyatomic
molecules of the samespecies
if c = a.Let us assume that a stands for a
polyatomic species
and the concentrations ofpolyatomics
aresufficiently
low. Then since the «pair
correlation function »IP 121
may beneglected,
we mayapproximate
ILa to the lowest order as follows :This is the
approximate
local chemicalpotential
which we will use in the derivation of Kirkwood’s diffusionequation.
Thisapproximation
limits the Kirkwood diffusionequation
tothe
regime
ofsufficiently
dilute solutions.3.3 KIRKWOOD DIFFUSION EQUATION. - With the
preparation
above,
we are nowready
topartition
function qa with(3.17’)
we findwhere
and thus
F .
is the force onparticle y
in alby
otherparticles
in the molecule- 1. e. ,
it is the so-calledspring
force if we borrow thecommonly
usedterminology
inpolymer
solution theories.In the case of uniform pressure the
thermodynamic
forceX y4
may
then be written asThe evolution
equation
for diffusion fluxJaq
may be obtained from(2.30)
by
decomposing
the latterinto q
components
where
To the lowest order
approximation
taking
a linear term in thethermodynamic
force or the fluxes and also to a linearapproximation
forLBz >,
where Àaq; bs
are collision bracketintegrals
for diffusion fluxes which aregiven by
the formulawhere
with m,
standing
for a mass(e.g.,
reducedmass)
and d for a sizeparameter
of a molecule(or
amonomer unit in the case of a
polymer),
andfaster time scale than conserved
hydrodynamic
variables.Therefore,
it is reasonable to setThat
is,
Substituting
(3.21)
and(3.22)
into(3.23),
we findInverting
thisrelation,
wefinally
obtain the linearflux-thermodynamic
force relationsIt is now convenient to define the
transport
coefficientsThese are diffusion coefficients. Substitution of
(3.19)
into(3.25)
yields
the diffusion flux in the formWe have shown that
1JI’a
obeys
thegeneralized
Kirkwoodintegral equation.
The same function alsoobeys
thefollowing
differentialequation
which can be derived from the definition for1JI’a,
(3.4),
and the kineticequation
(2.13) :
where
This flux factorizes
approximately
to the formThis can be shown
by following
theprocedure
described in aprevious
paper[9f]
onelectrolyte
solutions. Thisapproximation
is valid if the heat fluxpart
of thenonequilibrium
contributionto the distribution function is assumed to consist of the kinetic energy
part
depending
on thewhere
the self-diffusion coefficient. This is related to the friction coefficient
appearing
in the Brownian motion model. WhenAJj
isneglected
and theapproximate
Jaq
so obtained is substituted into(3.28),
there follows theequation
which is the Kirkwood diffusion
equation
forconfiguration
distribution functionqf,, (R, t )
for asingle polyatomic
(e.g., polymer)
molecule in a flow field u.Neglect
ofOJâq
isjustifiable
if the diffusion of a bead is uninfluencedby
other beads since theapproximation
amounts to theassumption
thatCùaq; as
= 0if q
s. Therefore theapproximation
shouldyield
reasonable results if the chain is nottangled by
itself and others. This fact and the manner in which(3.32)
is derived indicateclearly
that it is anequation holding
for a dilute solution.It is useful to collect the
assumptions
andapproximations
made to obtain the Kirkwood diffusionequation
in thepresent
kinetictheory.
1. Factorization
ofj(2)
This is due to theassumption
on the heat flux termappearing
in the distribution functionby
which thepotential
energy contribution to the heat flux isneglected.
If the processes do not include heat flows in thesystem
thisassumption
is notrequired
and the factorization ofJâq
becomes exact within the thirteen momentapproximation
which isgenerally satisfactory
for the usualhydrodynamic description
of afluid ;
cf. reference[9f].
2.Neglect of
« pair
correlationfunction »
ll,(2)
- Thisapproximation
holds if the solute concentration issufficiently
low,
andpermits
anapproximate
calculation of local chemicalpotentials
for solutes andcorresponding thermodynamic
forces.3.
Steady
stateÎaq
in the substantialframe of reference.
- Thisassumption
isjustifiable
since diffusion fluxes should relax faster than conserved variables. Since the evolutionequation
(3.20)
forJaq
is the average of Newton’sequation
of motion forparticle q
e a, thisassumption
isequivalent
toneglecting
the inertia term in theLangevin equation
forparticle
q e a in the Brownian motion modeland,
inaddition,
alsoassuming
thehomogeneity
of diffusion fluxes in space,i. e. ,
If the diffusion occurs in a flow
field,
thisassumption
isgenerally
violated,
and one must take the effect of flow into account. This may be done if anapproximate
formula for u isemployed.
Forexample,
if the shear is notlarge,
then we may takewhere y is the shear rate tensor assumed to be constant.
(It
is useful to note here that theeven further and take the Oseen tensor
approximation generally
taken inpolymer
solutiontheories
[12, 19-22].
To be morerigorous,
it is necessary to solve the diffusion flux evolutionequation
together
with the momentum balanceequation
and the stress tensor evolutionequation.
Thisapproach,
however,
is rather difficult toimplement
inpractice.
Neither is it themost convenient of the methods for
obtaining
transport
properties
ofpolyatomic
(e.g.,
polymer)
solutions.4.
Neglect
of
àj (2)
Thisassumption
isjustifiable
if theconfiguration
of the chain isrelatively simple,
i.e.,
untangled,
and if the concentration ofpolymers
is low. Therefore the retention of this termprobably
wouldimprove
the accuracy for1JI’a
when the solute concentration is notsufficiently
low.Finally,
a note on the flux evolutionequation
(3.20).
As mentionedbefore,
it isequivalent
to the
Langevin equation
for motion of aparticle
immersed in the medium of otherparticles.
However,
there are someimportant
differences which endow(3.20)
with a morepowerful
capability.
First ofall,
it can deal with nonlinear situations since thedissipative
termllaq
isgenerally
nonlinear for processes removed far fromequilibrium.
Thedissipative
termscan be
explicitly
calculated in terms of molecularproperties
if thepresent
molecularapproach
ispursued
to its ultimate end.Equation
(3.20)
does notrequire
anassumption
on diluteness of the solution.Therefore,
it can handle concentrated solutions as well. All these features are vested in thedissipative
terms in thepresent
theory.
4.
Viscosity
of abinary
mixture.The kinetic
equation
used in this workprovides
a formalism with which to calculate varioustransport
coefficients forpolyatomic
fluids and we take thisopportunity
to show some formal results for shearviscosity.
Theprocedure
toemploy
for the purpose isbasically
the same as the one used forsimple
dense fluid mixturesreported previously
[9e, 24].
Therefore we shallnot go into the
subject
indepth
here.Instead,
we shall pay a close attention toviscosity only,
since it is better studied
experimentally especially
in connection withpolymer
solutions which are relevant to thepresent
kinetictheory
and also related to the friction coefficientsÀ aq ; bs
presented
in section 3.4.1 STEADY STATE SOLUTION OF STRESS EVOLUTION EQUATIONS. - To be more
specific,
in ourinvestigation
we shall confine the discussion to abinary
mixture in which apolyatomic
fluid is dissolved in a solventconsisting
of aspherical
molecular(simple)
fluid. If there is nooscillatory
shearacting
on thesystem
the stress relaxesgenerally
on a faster time scale than the fluidvelocity
of thedensity.
It is then sufficient to consider thesteady
state stressevolution
equation.
Furthermore we will assume that the stress ishomogeneous
so that it doesnot
depend
onposition.
We also assume that the shear rate issufficiently
small so that it is sufficient to consider the linear shear ratedependence
of the stress tensor. Thatis,
we assumethat the flow is Newtonian. We will later
develop
atheory
for non-Newtonian flowalong
the line taken in theprevious
paper[9]
on densesimple
fluids.Under these
assumptions
the stress tensor evolutionequations
become linearalgebraic
equations
forRc,
(c = a, b ; a
=solute,
b =solvent) :
term
A a (1)
for
the solutespecies
as follows :and
similarly
for the solventcomponent
b. In(4.1a, b)
the coefficientsRaa,
Rab,
etc. are the collision bracketintegrals
related to the stress tensors. Theirexplicit
forms aregiven by
the formulawhere the
subscripts
c and d are eithera (solute )
or b(solvent ).
These coefficients are relatedto the Newtonian viscosities of the solvent and solute
species.
The linearalgebraic
set
(4.1a, b)
can be solved foree=
p P c,
(c
= a,b )
toyield
where
These solutions can be used to calculate the viscosities of the solvent and the solute.
4.2 INTRINSIC VISCOSITY OF THE SOLUTION. - Since the viscosities
are defined
by
the relationswe
identify
71 g
andq§,
respectively,
with the coefficients in(4.3a, b) :
The formulas in
(4.6a, b)
give
the Newtonian viscosities in terms of statistical formulaswhich,
Since in
practice
theviscosity
of a mixture is measured in thelaboratory,
the actual observable is the totalviscosity 17 0 :
where
The intrinsic
viscosity
of a solution is definedby
thelimiting
formulawhere c stands for the concentration of the solute in the units of the
weight
per volume(e.g.,
g/deciliter).
Therefore the intrinsicviscosity
is the relativeviscosity
of the solute in the infinite dilution limit and has the dimension of volume/mass. It is of interest to us here.In order to have a better idea of the intrinsic
viscosity
we use(4.4a-d)
and(4.6a, b)
and examine their mass fractiondependence
astep
beyond
the formal structure. For this purposewe introduce a
parameter
Te of dimension time definedby
the formulawhere mr is a mean mass and d is a mean size
parameter
of the moleculesmaking
up thesystem.
Thisparameter
rc isroughly
a measure of collision time between twoparticles.
We then scale the collision bracketintegrals Raa,
etc. in thefollowing
manner :These