Chemistry Reference
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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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