Quantum-mechanical calculations25 show that reduced
binuclear species with protons localized on the bridging oxy-
gens (Tables 3 and 4) or with vacancies of the bridging oxygens
(Table 3) give blue shifted charge transfer bands relative
to those arising from intact ones; a proton on the terminal
oxygen leads to a red shift. The Vis part of the spectra
in heteropoly acids and Cs-salts is revealed to be formed by
course of constitutional water release is approximately two
times smaller than in HPA. The propene atmosphere leads to
the same effects in the Vis part of HPA and Cs2A spectra.
However, propene is more efficient in the extraction of water
than He, due to the additional reaction leading to the product
isopropanol. Therefore, for propene–HPA the Vis band shift is
larger, and in Cs2A the Vis peak position stabilizes at lower
temperatures.
Under action of O2 the band in the Vis part of the HPA
spectrum disappears after the crystal water loss.At the same
time under O2 flux in Cs2A salt the Vis peak can be observed
from RT to 663 K, and this is due to the presence of Cs+ ions
which prevent oxidation.
d–d and IVCT transitions V4+–O–Mo6+ ! V5+–O–Mo5+
,
Mo5+–O–Mo6+ ! Mo6+–O–Mo5+ (Table 3). Depending on
temperature, the IVCT transitions arise from species
(OtOp(Ob)3Hb1)V4+–Ob–Mo6+(OtOp (Ob)3)with a proton loca-
lized on the bridging oxygen or reduced species of the type of
VMoO10 , VMoO9 , Mo2O10 , Mo2O9 with one or two oxygen
vacancies25 (Table 3).
The spectroscopic changes in the UV/Vis range at the high-
est temperature (607 K, 663 K) are shown in Figs. 4 and 5. HPA
treated in He develops a clear absorption band at 665 nm
(directly observed in the spectra, deconvoluted on two bands
at 660 and 740 nm, see section 3). For Cs2A treated in He as
well a broader absorption band at 715 nm (directly observed
in the spectra deconvoluted on two bands at 680 nm and 770
nm, see section 3) is detected (not shown). At 663 K the Vis
peak position for Cs2A treated in He (Table 2 ) is close to that
of HPA, permitting the conclusion that MoO3 and Cs3A salt
are formed from Cs2A in good agreement with a Raman shift
of the main Keggin band from 988 cmꢀ1 for Cs2A to 992
cmꢀ1 for Cs3A.13 This spectroscopic feature indicates an expul-
sion of vanadyl species based on the calculated peak maximum
at 660/740 nm for HPA and 680/770 nm for Cs2A. These con-
clusions can also be drawn on the basis of observed absorption
bands of VOSO4ꢄ5H2O at 625 and 766 nm.36 However, corre-
sponding Raman bands indicating vanadyl species could not
be observed for these catalysts treated in He.13 The absorption
band at 665 nm that is observed in the presence of He disap-
pears in the presence of O2 for HPA (Fig. 4). It also suffers a
red shift and is weaker for Cs2A treated in O2 . As for the Vis
peak position in Cs2A, it can be recognized that this position
regains its RT2 value at higher temperatures. Hence, the pre-
sence of molecular O2 could stabilize the Cs2A structure. In
HPA, He/H2O effects an even stronger Vis absorption band
at ca. 665 nm than pure He. In this case the expulsion of vana-
dium species seems to be clearer, still in contrast to the Raman
observation (no corresponding bands). For Cs2A treated in
He/H2O a weaker Vis band, which is red shifted, could indicate
a smaller number of expelled vanadyl species. HPA treated in
propene shows a very broad weak absorption band with an
observed peak maximum at ca. 635 nm and 2 deconvoluted
spectra whose peak maxima are around 520 and 650 nm (not
shown). In contrast, for Cs2A treated in propene as for HPA
At RT after a certain time on gas flux (for example, He (Fig.
2)) in HPA the loss of crystal water begins. At this initial stage
there is no reduction, the HPA is partly in the hydrated phase,
the protons are not localized and reside on the bridging water
moieties H5O2+. However, the quantitative determination of
the V4+ content by EPR10 shows that even at this stage vana-
dium is present as V4+, its amount is about 0.5–2 mol%. At the
same time a small amount of Mo5+ is also detected. Thus initi-
ally, the Vis part of the spectra originates mainly from the d–d
transitions in the contained V4+ and Mo5+ ions.28 The total
spectrum intensity increases due to the increase in the intensity
of the charge transfer band arising from the V4+–Mo6+ inter-
valent transition in intact species VMoO11 28 which contributes
to the first near-IR band (Table 4 and section 4.5.). At tem-
peratures 326–422 K the removal of crystal water (see thermo-
gravimetric (TG) data in Table 1) is accompanied by the
localization of acidic protons, the most energetically favour-
able sites of which have been shown to be the bridging oxy-
gens34,35 All reduced species with protons residing on the
bridging oxygens listed in Tables 3 and 4 give rise to new
d–d transitions blue shifted in comparison with those arising
from intact VMoO11 clusters (Table 3). Besides this, at tem-
peratures 326–422 K on the border of the Vis and near-IR
range a new charge transfer band originating from the
(OtOp(Ob)3Hb1)V4+–Ob–Mo6+(OtOp(Ob)3) species appears
(Table 3). On the other hand, with temperature rise in the
region of crystal water loss the concentration of reduced pro-
tonated species increases as fast as the protons localize on
the oxygens of the reduced intact species. Both mentioned fac-
tors lead to the observed gradual blue shift of the Vis peak
position in HPA and Cs2A (Table 2). At the same time, the
spectrum intensity increases due to increase in the transfer
parameter with water loss. However, in spite of the smaller
number of localized protons for Cs2A in the region of crystal
water loss, the blue shift of the Vis band is of the same order
for HPA and Cs2A. This can be explained by the stronger crys-
tal field and electron–vibrational coupling in Cs2A.
As the temperature continues to rise, constitutional water
evolves (see TG data in Table 1). This water is formed by
the extraction of an oxygen by two protons and leads to the
formation of defective clusters in which bridging oxygens are
removed. However, the constitutional water evolution itself
is not accompanied by the appearance of new reduced clusters.
Therefore, at this stage the transformations of the spectra may
occur due to the reduced species of the type of VMoO10
,
VMoO9 , Mo2O10 , Mo2O9 enumerated in Table 3 and formed
from reduced protonated species. Meanwhile, the evolution of
molecular oxygen may lead to the formation of the same
clusters VMoO10 , VMoO9 , Mo2O10 , Mo2O9 from intact
non-reduced VMo11 , Mo2O11 ones. The indicated ill-defined
species promote a further blue shift of the Vis band.Their con-
centration increases with temperature rise, and the total inten-
sity of the Vis part of the spectra grows. After crystal water
removal for Cs2A the position of the Vis band remains nearly
unchanged insofar as, due to the structure of this compound,
the number of species with oxygen vacancies formed in the
Fig. 4 Influence of gas atmospheres on the in situ UV/Vis spectra of
H4PVMo11O40 at 607 and 663 K. a,b: He; c,d: He/H2O; e,f: O2 ; g,h:
propene; i,k: O2/propene. For better visualization the spectra were ver-
tically shifted.
2404
Phys. Chem. Chem. Phys., 2002, 4, 2398–2408