Chemistry Reference
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X
x 2 p;j ¼
1
(29)
j
which is valid in each of the phases. Rearranging ( 28 ), summing up over all
polymer components, and using ( 29 ) one obtains:
X
I 2 j
x I 2
x I 2
x I 2 p;j '
1
¼
(30)
II
2 j
'
j
For given temperature, pressure, and polymer distribution in one phase ( x I 2 p;j ),
equations ( 27 ) and ( 30 ) can be used to determine the unknowns x I 1 and x I 1 .
Depending on the expressions for the fugacity coefficients
'
I 1 and
'
I 2 p;j , additional
unknowns, e.g., m I 2 ¼ P j x I 2 p;j m 2 p;j will have to be determined. The m 2 p,j are the
segment numbers of the various polymer species (which are of course the same in
the two phases). Additional equations can easily be obtained by multiplying ( 28 ),
e.g., with m 2 p,j , again rearranging, summing up over all polymer species, and using
( 29 ) to eliminate the unknown molecular weight distribution in the second phase:
X
I 2 j
x I 2
x I 2
x I 2 p;j m 2 p;j '
m I 2 ¼
(31)
II
2 j
'
1
Applying the approach given by ( 29 ) ( 31 ), rather than the classical approach of
considering only ( 27 ) and ( 28 ), has the advantage that the number of equations to be
solved numerically is independent of the number of considered polymer species.
After solving ( 27 ), ( 30 ), and ( 31 ), the missing concentrations of the single
polymer species (molecular weight distribution) in the second phase can easily be
obtained from rearranging ( 28 ):
I
2 j
x I 2 p;j '
x I 2
x I 2
x I 2 p;j ¼
(32)
II
2 j
'
A very elegant version of this approach is the so-called continuous thermody-
namics [ 56 59 ]. It can be considered as a reformulation of the classical thermody-
namic relationships that allows for using continuous molecular weight distribution
functions W ( M ) rather than the mole fractions of discrete polymer components.
Using this approach, e.g., ( 30 ) becomes:
ð
x I 2
x I 2
I
Þ '
2 ð
M
Þ
1
¼
W
ð
M
dM
(33)
II
'
2 ð
M
Þ
M
For certain combinations of analytical molecular weight distributions (e.g.,
Schulz Flory distribution) and fugacity-coefficient expressions, the integral in
( 33 ) can be solved analytically and no (time-consuming) summation is required.
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