with K+. This corresponds to the inhibition of the allylic oxidation
and is consistent with the consensus that the nucleophilic lattice
oxygen species generally attack the allylic hydrogen and induce
allylic oxidation. In other words, one role of K+ is to inhibit the
reactivity of lattice oxygen and thus to suppress the allylic
oxidation.
Because not only PO selectivity but C3H6 conversion also
increased remarkably after the addition of K+, the presence of K+
must also accelerate the activation of N2O for C3H6 epoxidation.
Our investigations have suggested that the change in the coordina-
tion structure of iron brought by K+ may account for such an
accelerating effect. A distinct Raman band at ca. 1000 cm21 was
observed after the modification of the FeOx/SBA-15 with an alkali
metal salt in UV-Raman studies, which have been shown to be
useful in determining the coordination structure of iron.9 In Fig. 2B,
the FeOx/SBA-15 showed Raman bands at 981, 1074 and 1138
cm21 in the region of 900–1200 cm21. The latter two bands
probably arise from the tetrahedral iron site in the framework of
SBA-15. A part of iron may be incorporated into the framework of
SBA-15 in the FeOx/SBA-15. After the modification with K+, these
bands became unnoticeable, and a band at 1000 cm21 appeared
distinctly. Another band at 808 cm21 also appeared after the
modification with K+, but this band could also be observed for a K+/
SBA-15 without iron (curve g of Fig. 2B). Thus, the band at 808
cm21 may not be related to iron sites. The intensity of the band at
1000 cm21 increased with an increase in K/Fe ratio from 0 to 5.0,
and slightly decreased with a further increase in K/Fe ratio. Since
this band shifts slightly to a lower wavenumber as compared with
those assigned to the framework Fe–O–Si, we tentatively speculate
that it arises from the tetrahedral FeO4 on the surface, which is
probably stabilized by alkali ions. Such an iron structure should be
effective for the activation of N2O for the epoxidation of C3H6.
In conclusion, we have found a dramatic shift of reaction route
from allylic oxidation to epoxidation during the oxidation of
propylene with N2O by modifying the FeOx/SBA-15 with K+. The
roles of K+ are to suppress the allylic oxidation by decreasing the
reactivity of lattice oxygen and to induce a coordination structure of
iron effective for epoxidation.
Fig. 1 Changes of catalytic performances with a change in K/Fe atomic ratio
in the modified 1 wt% FeOx/SBA-15. Symbols of selectivity: (5) propylene
oxide, (8) allyl alcohol, (:) acrolein, (2) COx.
Further investigations revealed that, similar shift of allylic
oxidation to epoxidation likewise occurred when other potassium
salts such as KNO3, KAc or KBr were used as the modifier instead
of KCl. Thus, it was K+ but not Cl2 played an important role. Other
alkali metal salt such as LiCl, NaCl, RbCl or CsCl also worked as
useful modifiers for PO formation. PO selectivity and yield
decreased with the following sequence, KCl > NaCl > RbCl >
CsCl > LiCl. By changing reaction conditions, PO selectivity of
80% can be obtained at 4% C3H6 conversion over a K+–FeOx/SBA-
15 catalyst, higher than that reported over the Na+–Fe2O3/SiO2
catalyst (70% PO selectivity at 2.5% C3H6 conversion).7c The
turnover frequency for PO formation over our catalyst was 5.2 mol
(mol-Fe)21 h21. Similar to many catalysts reported so far,3,4,7c the
activity of our catalyst also decreased with time on stream (TOS) as
shown in Table 1. It has been clarified that the decrease in C3H6
conversion with TOS is caused by the carbon deposition, and the
activity can almost be recovered by regenerating the catalyst with a
gas flow containing He and O2 at 823 K.
We have clarified that the redox property is an important factor
in determining the reaction route. The H2–TPR studies indicated
that the reactivity of the lattice oxygen of FeOx in the FeOx/SBA-15
was remarkably inhibited by the modification with K+ (Fig. 2A). A
reduction peak corresponding to the reduction of Fe3+ to Fe2+ was
observed at 682 K for the sample without modification. The main
reduction peak was shifted to 888–918 K after the modification
This work was supported by the NSF of China (Nos. 20273054
and 20021002) and the National Basic Research Program of China
(No. 2003CB615803).
Notes and references
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Fig. 2 TPR profiles (A) and UV-Raman spectra (B). (a) 1 wt% FeOx/SBA-
15, (b) K+–1 wt% FeOx/SBA-15 (K/Fe = 2.5), (c) K+–1 wt% FeOx/SBA-15
(K/Fe = 5), (d) K+–1 wt% FeOx/SBA-15 (K/Fe = 10), (e) K+–1 wt% FeOx/
SBA-15 (K/Fe = 15), (f) SBA-15, (g) K+/SBA-15 (K/Si = 0.04).
C h e m . C o m m u n . , 2 0 0 4 , 1 3 9 6 – 1 3 9 7
1397