Chemistry Reference
In-Depth Information
Ni(I)
g
= 2.0027
g
= 2.09
2800
3000
3200
3400
3600
Magnetic field (gauss)
FIGURE 9.11
9 GHz EPR spectrum at 77 K of β-carotene in Ni-MCM-41 after 350 nm irradiation. (From
Konovalova, T.A.,
J. Phys. Chem. B
, 105, 7549, 2001. With permission.)
(Hartmann et al. 1996). The
g
||
component is often too weak to observe. The Ni(I) EPR signals were
not detected upon 350 nm irradiation of Ni-MCM-41 samples before adsorption of carotenoids.
Detected at 9 GHz, EPR signals of an isolated Ni(I) species with
g
=
2.09 provide direct evidence for
the reduction of Ni(II) ions by carotenoids.
9.14.2 C
AROTENOIDS
IN
F
E
-MCM-41
Multifrequency EPR spectroscopy was applied to study Fe(III)-MCM-41 mesoporous molecular
sieves with incorporated carotenoids (Konovalova et al. 2003).
EPR spectroscopy is a useful technique for characterizing the iron sites in both the low-spin
5/2) electronic coni gurations. The spin Hamiltonian for high-spin iron
is given by the following equation (Dowsing and Gibson 1969, Sweeney et al. 1973):
(
S
=
1/2) and high-spin (
S
=
1
⎛
⎞
2
2
2
2
Hg
=β
BS
+
DS
−
S
+
E
(
SS
−
)
(9.24)
⎜
⎟
S
Z
X
Y
⎝
⎠
3
In this case the
g
-tensor exhibits extremely small anisotropy, and the spectral characteristics are
determined by the ZFS parameters
D
(axial) and
E
(rhombic). When the symmetry is axial,
D
≠
0
and
E
1/3. Most high-spin d
5
systems do not belong to
one of these special cases. Several different symmetries of Fe
3+
contribute to multicomponent EPR
spectra with overlapping signals. Such complex spectra arising from more than one center can be
analyzed at different microwave frequencies. For high-spin Fe
3+
in proteins, zeolites, and MCM-41
molecular sieves, the electron Zeeman interaction (
gbB
0
S
) is much smaller at the X-band frequency
than the ZFS interaction. This makes interpretation of the 9 GHz EPR spectra difi cult due to inho-
mogeneous broadening arising from the ZFS and overlapping signals. Use of higher microwave
frequency is particularly advantageous in this case.
Studies with 9-287 GHz EPR (Konovalova et al. 2003) were carried out to characterize the Fe
3+
sites in Fe-MCM-41 molecular sieves. Multifrequency EPR measurements were also performed to
elucidate the types of iron sites which are responsible for carotenoid oxidation, their stability, and
accessibility. The X-band EPR spectrum of Fe-MCM-41 activated at 260°C and recorded at 77 K
consists of a strong sharp peak at
g
=
0. In the case of rhombic symmetry,
E/D
=
9.0 (Figure 9.12a). The presence of
these signals originating from the middle Kramers doublet and the lowest Kramers doublet, respec-
tively, is characteristic of high-spin Fe
3+
when
E/D
=
4.3 with a shoulder at
g
=
=
1/3 (Abragam and Bleaney 1970, Pilbrow
1990). The observation of a
g
4.3 signal in zeolites and aluminophosphate molecular sieves is usu-
ally considered as evidence for the presence of framework Fe
3+
ions (Goldfarb et al. 1994, Kosslick
=
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