Chemistry Reference
In-Depth Information
in E ʱ when the difference between the maximum and minimum values of E ʱ is more
than 20-30 % of the average E ʱ value. In the case of calcium oxalate monohydrate,
this difference is close to 100 % of the average value.
Needless to say that performing integration over small temperature segments in
accord with Eq. 2.21:
T
E
RT
a
α
IE T
(,
)
=
exp
d
T
(2.21)
αα
T
a
α
would also eliminate the error associated with the variability of E ʱ in the isocon-
versional method based on Eq. 2.17. Consistency of the resulting E ʱ dependence
with the dependence produced by the Friedman method has been demonstrated by
Budrugeac [ 38 ], who also proposed a new nonlinear differential isoconversional
method that makes use of a numerical algorithm similar to that represented by
Eqs. 2.15 and 2.16.
In addition to the methods proposed by Vyazovkin, there are several other flex-
ible integral isoconversional methods [ 39 - 46 ]. Among them, a method proposed by
Popescu [ 39 ] deserves a special attention because it combines the flexibility with
computational simplicity. The method makes use of the so-called mean value theo-
rem to approximate the temperature integral. The theorem states that a definite inte-
gral of a continuous function f (  x ) on the closed interval [ a, b ] can be presented as:
b
(2.22)
f
( )
x dx
=−
(
b
a f c
)
( ),
a
where f (  c ) is the mean value of f (  x ) over the interval [ a,b ]. The equality is exact
because the mean value is defined as:
b
1
f c
()
=
f
() .
x dx
(2.23)
(
ba
)
a
The theorem does not say where the point c is located, it only proves that it is lo-
cated within the interval [ a, b ]. The application of the theorem to the temperature
integral defined on the temperature interval [ T m ,T n ] allows one to arrive at the fol-
lowing equation [ 39 ]:
T
n
E
E
=−
exp
dT
(
T
T
) exp
.
(2.24)
n
m
RT
RT ξ
T
m
The equation is exact only when the value of T ξ is such that the respective value
of the exponential function equals the mean value of the function in the interval
[ T m ,T n ]. Unfortunately, there is no simple practical way to determine such tempera-
 
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