Chemistry Reference
In-Depth Information
Fig. 2.8
Illustration to the
Popescu method (Eq. 2.26)
β
1
β
2
α
n
α
m
T
n,1
T
n,2
T
m,1
T
m,2
ture. For practical purposes, it can be approximated as the mean value of the interval
[
T
m
,
T
n
], i.e.,
T
ξ
= (
T
m
+
T
n
)/2. This approximation is accurate only for integration of
a linear function. For any other function, the accuracy of this approximation would
depend on the size of the interval [
T
m
,
T
n
] so that the smaller the interval, the better
the accuracy. Subject to Eq. 2.24, one can write Eq. 2.8 for two arbitrary conver-
sions
ʱ
m
and
ʱ
n
,
as follows:
A
TT
E
RT
−
g
()() (
α
−
g
α
=
−
) exp
,
(2.25)
n
m
n m
β
ξ
where
T
m
and
T
n
are the temperatures that correspond, respectively, to the conver-
sions
ʱ
m
and
ʱ
n
on the
ʱ
versus
T
curve at a given heating rate
ʲ
(Fig.
2.8
). Assum-
ing that the form of the reaction model does not change with the heating rate, the
left-hand side of Eq. 2.25 is constant for a set of different heating rates,
ʲ
i
. Then
Eq. 2.25 can be rearranged to:
β
E
RT
i
ln
=
Const
−
(2.26)
TT
−
ni mi
,
,
ξ
,
i
The activation energy can be determined from the slope of a linear plot of the left-
hand side of Eq. 2.26 against 1/
T
ξ,i
.
Although in the original publication [
39
] by Popescu, the intervals ∆
ʱ
=
ʱ
m
−
ʱ
n
used are relatively wide (0.3-0.8), the relative errors in the estimated
E
values re-
main within the tenths of percent. However, the primary advantage of the method is
in the flexibility to choose the integration limits by selecting any desired values of
ʱ
m
−
ʱ
n
. In particular, by making the ∆
ʱ
intervals smaller (e.g., 0.01-0.02), one can
practically eliminate the integration error that arises from the variability of
E
ʱ
with
ʱ
. This opportunity has been explored efficiently by Ortega [
42
], who applied the
mean-value theorem to derive isoconversional equations for the conditions when
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