Chemistry Reference
In-Depth Information
-
Η
RT
p
(7)
p
=
p
exp
o
with H
p
= 43 kJ.mol
-1
.
The combination of equations (5), (6) and (7) gives:
Η
RT
-
c
C
=
C
exp
(8)
o
with C
o
= S
o
p
o
and H
c
= (H
s
+ H
p
).
All the experimental results can be explained if H
s
is negative and close to H
P
in absolute value. Thus, C will increase or decrease with temperature depending
on whether H
s
is lower or higher than H
P
in absolute value, as previously estab-
lished in recently published works [10, 11, 13].
3.2.2. Diffusion
Diffusivity is analyzed assuming a Fickian mechanism. The coefficient of diffu-
sion D was determined from the classical relationship:
2
π
16
m
m
e
t
2
D
=
for m
t
≤
0.6 m
∞
(9)
∞
where e is the sample thickness.
The Arrhenius plot for diffusion coefficient (Fig. 5) displays a non-linear shape
suggesting two possible ways of interpretation. The first explanation considers
Figure 5. Variation of water diffusivity in PEI with temperature.
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