advantage of MNPs, is typically more effective than filtration or
centrifugation as it prevents loss of the catalyst. The magnetic
separation of MNPs is simple, economical and promising for
industrial applications.3 Currently, much attention is focused on
the synthesis of magnetic core–shell structures by coating an
SiO2 shell around pre-formed NPs.4 Nanosized silica, which is
non-toxic and can be grafted with a variety of surface modifiers,
has great potential in many applications.5
The IR spectrum of the synthesized g-Fe2O3 NPs is shown in
Fig. 1. The absorption bands at 449.5, 588.7, 637.8, 799.5 and
900 cm-1 are in good agreement with the IR results reported for
pure maghemite (g-Fe2O3).10
Since Keggin-type heteropoly acids (HPAs) such as
H3PW12O40 (PW) were first commercialized in the industrial
research field, a large number of these catalysts have been
developed for a wide range of organic reactions in fundamen-
tal research.6,7 Several advantages to be highlighted of using
supported HPAs compared to homogeneous examples include
easier recovery and recycling after carrying out reactions, and
easier product separation.8 However, separation and recovery
of the immobilized HPAs are usually performed by filtration or
centrifugation, which are not eco-friendly processes.
The immobilization of PW on silica-coated g-Fe2O3 NPs
(designed as g-Fe2O3@SiO2-PW) can be employed to derive
a novel heterogeneous catalyst system that possesses both a
high separation efficiency and a relatively high surface area to
maximize catalyst loading and activity. Certainly, the use of envi-
ronmentally benign solvents has been another key research area
of green chemistry, with great advances being seen in aqueous
catalysis. Along this line, we synthesized g-Fe2O3@SiO2-PW as
a novel nanomagnetically-recoverable catalyst and assessed its
catalytic activity in Mannich-type reactions in water. Indeed,
the venerable Mannich reaction and its variants represent one
of the more powerful constructs for alkaloid synthesis.9 To the
best of our knowledge, this is the first report on the synthesis,
characterization and catalytic application of a g-Fe2O3@SiO2-
PW catalyst.
Fig. 1 IR spectrum of g-Fe2O3 NPs.
Sonication of the g-Fe2O3 NP suspension in an alka-
line ethanol–water solution of tetraethyl orthosilicate (TEOS)
caused the rapid coating of the magnetic cores with silica shells.
The outer shell of silica not only improves the dispersibility
but also provides suitable sites (Si–OH groups) for surface
functionalization with PW. Ultimately, mixing a suspension of
g-Fe2O3@SiO2 with a methanolic solution of PW lead to the
formation of g-Fe2O3@SiO2-PW NPs. Elemental analysis from
ICP showed that the W content was 23.7 wt%. Typically, a
loading at ca. 31 wt% PW (1.1 mmol g-1) was obtained.
Fig. 2(a) and (b) show the TEM image and size histogram
for the g-Fe2O3@SiO2-PW NPs, respectively. The particle size
distribution from the TEM image shows that 66% of NPs are
in the range 75–90 nm and that the mean diameter of the
observable NPs is 73.5 nm. The size distribution of the g-
Fe2O3@SiO2-PW NPs derived from a laser particle size analyzer,
illustrated in Fig. 2(c), indicates that the mean diameter of the
particles is 93.8 nm. As shown in the TEM image (Fig. 2(d)),
aggregation/coalescence of individual g-Fe2O3 NPs occurred,
and that they could have been in an aggregated state during the
coating process. Such aggregations form bigger structures with a
non-spherical morphology, which causes the difference between
the results derived from TEM analysis and the measurements
made by the laser particle size analyzer. A typically core–shell
structure of a g-Fe2O3@SiO2-PW NP is shown in Fig. 2(e). The
dark core of the g-Fe2O3 and the grey silica shell are clearly
observable. The typical silica shell thickness was estimated to
be around 10 nm. Due to the strong mass difference between
SiO2 and PW, it could be assumed that the outside darker
contrast indicates the shell of PW particles immobilized onto
the g-Fe2O3@SiO2 NPs.
Results and discussion
Scheme 1 presents the synthetic strategy for g-Fe2O3@SiO2-PW
NPs.
IR spectra of g-Fe2O3@SiO2, g-Fe2O3@SiO2-PW and PW
samples are shown in Fig. 3. All samples show broad bands
at around 1650 cm-1, which are attributed to adsorbed water.
The transmission spectrum of g-Fe2O3@SiO2 shows that the
absorption band at 589 cm-1 could be related to the vibration
of g-Fe–O.11 The other peaks at 627 and 895 cm-1 are pure g-
Fe2O3.10 The bands at 1100 cm-1, along with shoulder at 1200
and 461 cm-1, are presumably due to asymmetric stretching
and bending modes of Si–O–Si, respectively. The shoulder at
800 cm-1 may be assigned either to a symmetric stretching of Si–
O–Si or a stretching vibration of Fe–O bonds. The characteristic
band of Si–O–Fe appears at 686 cm-1 in this sample.12 The
Scheme 1 Schematic illustration of the general approach to the
synthesis of g-Fe2O3@SiO2-PW NPs.
Magnetic g-Fe2O3 NPs were prepared through the chemical
co-precipitation method. In aerated solutions, an aqueous
mixture of ferric and ferrous salts precipitate as an aqueous
dispersion of g-Fe2O3 via the addition of strong alkaline
solutions in the pH range 7.5–14. In this work, a solution of
NH4OH was used as the alkali source. The chemical reaction of
g-Fe2O3 precipitation is given by:
Fe2+ + Fe3+ + O2 + 2OH- → Fe2O3 + H2O
PW12O40 Keggin ion structure is well known and consists of
3-
This journal is
The Royal Society of Chemistry 2011
Green Chem., 2011, 13, 2116–2122 | 2117
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