Table 5 Comparison of data for the interrelation of E , E , n and j
app true
O2
E
/kJ mol~1
app
Method of estimation
La0.7Ce0.3FeO
La0.7Sr0.3FeO
La0.7Sr0.1Ce0.2FeO
3
3
3
Slopes of ln R \ f (1000/T ) from ref. 12
90.2
93.6a
88.9
92.7b
83.9
82.0c
Eqn. (15) using n values found from Fig. 1, eqn. (2)
and the j and E
values found from Fig. 5, eqn. (5)
O2
true
Plots in Fig. 6
92.3
65.3
68.4
a E (kJ mol~1) \ E ] nj : 93.9 \ 75.5 ] (0.35 ] 52.6). b 94.15 \ 63.2 ] (0.14 ] 221.1). c 82.0 \ 66.1 ] (0.13 ] 122.3).
app true O2
shown. This table contains the E values found by three dif-
A simulation of the kinetic results using a suitable computer
program20 enables the direct estimation of kinetic and equi-
librium constants as well as the determination of true activa-
app
ferent ways for the three tested catalysts: First E
as found
app
from the slopes of the Arrhenius-type lines in ref. 12. Second
the E values as found from eqn. (15) after substituting the
tion energies E and the heats of adsorption of oxygen j
.
app
true
O2
relevant values of E , the mean value of the reaction rate
The exponent n used in the empirical rate equation R \
true
order n and j calculated previously in this work. Third the
k@(P )n(P )m can be related to the extent of contribution of
O2
O2
CH4
E
values calculated from the Arrhenius-type plots in Fig. 6.
the heat of adsorption j to the apparent activation energy
app
O2
The agreement between these values is excellent for the LaÈ
CeÈFeÈO catalysts for the three cases. In the other two cases
catalysts LaÈSrÈFeÈO and LaÈSrÈCeÈFeÈO) the plots in Fig.
give lower values as compared to the other two methods of
according to the relationship E \ E ] nj . This is
applied more precisely in cases where the K
the same order of magnitude as unity, while some discrep-
app
true
O2
P
term is of
O2 O2
(
6
ancies develop as soon as K P becomes larger and larger.
O2 O2
calculation. These discrepancies can be traced to the less satis-
factory matching of the lines in Fig. 1 with the actual RidealÈ
Eley curves in Fig. 3.
Large values of K and j for the above solids were
O2
O2
related to the existence of a SrFeO
phase, which is able to uptake large amounts of oxygen as
perovskite crystal
3Bx
In other words when the reaction rate R, as described by
the RidealÈEley scheme, increases in a smooth way as a func-
established by TPD/O experiments in previous work.18
2
tion of P , as observed in the case of LaÈCeÈFeÈO (Fig. 3),
O2
then the matching between the three cases is perfect. On the
References
other hand if the values of R, as a function of P , quickly
reach steady values, as in the case of LaÈSrÈFeÈO and LaÈSrÈ
CeÈFeÈO solids, an appreciable mismatching is developed
between the calculated values of E , because the exponential
eqn. (9) expresses the situation in a less satisfactory way. In
those cases the values of E
should be nearer to the actual value.
Therefore eqn. (9) is more applicable and useful in cases
where KP values in the denominator of the RidealÈEley
relationship are of the same order of magnitude as unity. In
other words, when KP is relatively small but not too small.
When KP is getting larger and larger, eventually the model
ceases to express the kinetics.
What might be the physicochemical reasons for the stronger
adsorption of oxygen on the LaÈSrÈFeÈO and LaÈSrÈCeÈFeÈ
O solids, which lead to larger values of the K P term in the
RidealÈEley relationship and to the fast approach of steady
values of reaction rate R as a function of P in Fig. 3? We
think that this is related to the existence of a SrFeO
phase in the two solids. This crystal phase was determined
previously17,18 very precisely with Mossbauer spectroscopy at
0 K and the results are listed in Table 1. We observe in this
table that LaÈSrÈFeÈO contains 33% of SrFeO while LaÈ
O2
1
2
3
M. F. M. Zwinkels, S. G. Jaras and P. G. Menon, Catal. Rev.-Sci.
Eng., 1993, 35, 319.
Advanced Materials in Catalysis, ed. R. J. H. Voorhoeve, J. P.
Remeika and L. E. Trimble, New York, 1977, p. 129.
L. G. Tejuka, J. L. G. Fierro and J. M. D. Tascon, Adv. Catal.,
1989, 36, 237.
app
from the other two methods
app
4
5
6
J. G. McCarty and H. Wise, Catal. T oday, 1990, 8, 231.
T. Seiyama, Catal. Rev.-Sci. Eng., 1992, 34, 281.
H. Arai, T. Yamada, K. Eguchi and T. Seiyama, Appl. Catal.,
1
986, 26, 265.
7
M. Stojanovic, C. M. Mims, H. Moudallal, Y. L. Yang and A. J.
Jacobson, J. Catal., 1997, 166, 324.
8
9
L. Marchetti and L. Forni, Appl. Catal. B, 1998, 15, 179.
H. M. Zhang, Y. Shimizu, Y. Teraoka, N. Miura and N.
Yamazoe, J. Catal., 1990, 121, 432.
1
0
1
D. Klvana, J. Vaillancourt, J. Kirchnerova and J. Chauki, Appl.
Catal. A, 1994, 109, 181.
1
Y. Teraoka, H. M. Zhang and N. Yamazoe, Chem. L ett., 1985,
O2 O2
1
367.
12 V. C. Belessi, A. K. Ladavos and P. J. Pomonis, Appl. Catal. B:
O2
crystal
Environmental, 2001, 31, 183.
3Bx
1
3
A. K. Ladavos and P. J. Pomonis, J. Chem. Soc., Faraday T rans.,
1
992, 88, 2557.
14
15
16
Y. Yao, Ind. Eng. Chem., Prod. Res. Dev., 1980, 19, 293.
K. Otto, J. M. Andino and C. L. Parks, J. Catal., 1991, 131, 243.
G. Saracco, F. Geobaldo and G. Baldi, Appl. Catal. B, 1999, 20,
277.
2
3Bx
SrÈCeÈFeÈO contains 12% of this phase. Furthermore the
phase SrFeO3Bx was found to be directly related to the exten-
17 V. C. Belessi, C. N. Costa, T. V. Bakas, T. Anastasiadou, P. J.
Pomonis and A. M. Efstathiou, Catal. T oday, 2000, 59, 347.
18 V. C. Belessi, T. V. Bakas, C. N. Costa, A. M. Efstathiou and P. J.
Pomonis, Appl. Catal. B, 2000, 28, 13.
sive oxygen uptake as determined by O -TPD experiments.18
2
This strong and extensive adsorption of oxygen on the
SrFeO3Bx crystal phase of those two solids LaÈSrÈFeÈO and
1
9
G. Longworth, in Mossbauer Spectroscopy Applied to Inorganic
LaÈSrÈCeÈFeÈO, justiÐes the large K P values and their
O2 O2
Chemistry, ed. E. J. Long, Plenum Press, New York, 1984, vol. I,
di†erent behaviour compared to the LaÈCeÈFeÈO sample.
p. 43.
20
21
22
The relevant computer program is available on request from
ppomonis=cc.uoi.gr
Conclusions
The following conclusions can be drawn from this work.
The kinetics of the deep oxidation of CH on oxidic solids
LaÈCeÈFeÈO, LaÈSrÈFeÈO and LaÈSrÈCeÈFeÈO, having
mixed oxidic and perovskitic components, follow the Rideal-
Eley model.
Y. Bard, in Non L inear Parameter Estimation, Academic Press,
New York, 1973, p. 83.
D. Cuthbent, F. Wood and J. Gorman, in Fitting Equations to
Data: Computer Analysis of Multifactor Data, John Wiley &
Sons, New York, 2nd edn., 1999.
4
2
3
G. K. Boreskov, V. V. Popovski and V. A. Sazonov, Proceedings
of the 4th International Congress Catalysis, Moscow, 1968, p. 439.
3862
Phys. Chem. Chem. Phys., 2001, 3, 3856È3862