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Cite this: CrystEngComm, 2012, 14, 3355
www.rsc.org/crystengcomm COMMUNICATION
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View Online / Journal Homepage / Table of Contents for this issue
Controlled growth and magnetic properties of a-Fe2O3 nanocrystals:Octahedra, cuboctahedra and truncated cubes†
Liang Bing Wang,a Le Xin Song,*ab Zheng Dang,a Jie Chen,a Jun Yanga and Jie Zengc
Received 12th December 2011, Accepted 7th March 2012
DOI: 10.1039/c2ce06661k
A series of a-Fe2O3 crystalline materials with fascinating poly-
hedral morphologies, such as octahedral, cuboctahedral and trun-
cated cubic structures, were prepared through a novel solid-phase
sintering process. Our results demonstrated that the structural
transformations among the polyhedra were easily controlled by the
sintering times. This suggested that the Wulff polyhedra trans-
formation could occur in a hexagonal crystal system. Furthermore,
we found that the magnetic properties of the a-Fe2O3 crystals were
associated with their size and shape.
With the prosperity of nanotechnology in the past two decades,
polyhedral theory has largely been developed through experiments.1,2
Polyhedral structures, such as octahedral, cuboctahedral, truncated
cubic and cubic structures, have attracted much attention and have
found wide applications as electrical and optical devices due to their
interesting properties, such as high symmetry, nano-sized dimension
and the existence of critical edges, etc.3 One example is that noble
metal nanocrystals, such as gold, silver and platinum nanopolyhedra,
can be obtained in very small grain sizes (often only below 20 nm),
which exhibit excellent physical and chemical properties.4–6 A great
achievement by Xia and co-workers has been to controllably
synthesize silver nanostructures.7 Furthermore, a controlled struc-
tural transformation between polyhedra is an essential goal of crystal
engineering strategies. Recently, Castleman and co-workers reported
that the morphology of titanium carbide nanoparticles could be
changed from cubic to cuboctahedral by using different methane
concentrations.8 Chen and colleagues revealed a controllable growth
for FePt cuboctahedral, octapodal, truncated cubic, and cubic
nanostructures by means of adjusting the reaction parameters.9
However, although a variety of fascinating features of these structural
transformations may exist, the studies were mostly focused on the
solution-mediated synthesis.10–13 It was necessary, therefore, to
aDepartment of Chemistry, University of Science and Technology of China,Jin Zhai Road 96, Hefei 230026, China. E-mail: [email protected]; Fax:+86-551-3601592; Tel: +86-551-3492002bState Key Laboratory of Coordination Chemistry, Nanjing University,Nanjing 210093, ChinacDepartment of Biomedical Engineering, Washington University, St. Louis,Missouri 63130, USA
† Electronic supplementary information (ESI) available: Experimentalsection, SEM, and SQUID. See DOI: 10.1039/c2ce06661k
This journal is ª The Royal Society of Chemistry 2012
develop a novel strategy to construct polyhedral structures upon
solid-phase treatment and to especially address such structural issues.
Hematite (a-Fe2O3) has wide applications in many fields, such as
chemical filters, catalysis aids, and electrode materials in lithium
batteries, owing to its low cost, good performance and high
stability.14–17 Different structures including spheres, rods, wires,
arrays, tubes, belts, disks, rings, dendrites, propellers and flowers have
been elucidated.18–25 Although a-Fe2O3 has been prepared as nano-
crystals with octahedral and cubic shapes,26,27 to the best of our
knowledge, there is no precedent in the literature for the formation of
cuboctahedral and truncated cubic structures of a-Fe2O3. Hence, this
represents the first evidence of these morphologies in a hexagonal
system. It is therefore of great interest to find a way of constructing
such structures and thus to understand the formation mechanisms.
Herein, we conducted a series of critical experiments on this
subject. Typically, an aqueous solution of FeCl3 and b-cyclodextrin
(b-CD)28 was introduced to obtain an aggregate, followed by sin-
tering of the product at specific temperatures for different periods of
time. Samples 1–3, which were determined to be a-Fe2O3, were
obtainedwith sintering at 723K in air for 8 h (sample 1); 16 h (sample
2) and 24 h (sample 3), respectively. It was found that with the
increase in sintering times, the highly ordered crystal structures of the
a-Fe2O3 samples experienced a continuous transformation from
octahedral to cuboctahedral and truncated cubic structures. We have
also proposed a possible mechanism for such a structural trans-
formation. We believe that the present work provides a striking
Fig. 1 XRD patterns of samples 1–3 (A, curves a–c) and FE-SEM
images of samples 1 (B), 2 (C), and 3 (D).
CrystEngComm, 2012, 14, 3355–3358 | 3355
Fig. 2 TEM images and SAED patterns of the octahedral (a, b),
cuboctahedral (c, d) and truncated cube structures (e, f).
Fig. 3 Schematic illustration of the formation of octahedral, cubocta-
hedral and truncated cubic structures.
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example of the close relationship between the sintering conditions and
crystallographies.
Fig. 1A shows theX-ray diffraction (XRD) patterns of the samples
1–3 indicating the formation of a unique a-Fe2O3 structure, since all
the XRD diffraction peak positions and intensities are in good
accordance with the JCPDS reference (89–0596).29 The cell is
hexagonal (space group R�3c) with constants: a ¼ 0.504 nm and
c ¼ 1.377 nm.
Fig. 1B–D shows typical field-emission scanning electron micros-
copy (FE-SEM) images of these three samples. As seen in Fig. 1B,
sample 1 exhibits an octahedral shapewith good uniformity. A higher
magnification (see Fig. S1, ESI†) displays more detail about the
octahedral units consisting of 8 equilateral triangular surfaces and 12
identical edges (with a mean edge length of 250 � 30 nm).
Interestingly, after further sintering for 8 more hours, the size of
these octahedral crystals became bigger (sample 2, with a mean edge
length of 700 � 70 nm), as shown in Fig. 1C. The increase in sizes
implies that sintering times could be applied to control the growth
process of the a-Fe2O3 octahedral particles. In addition, a few well-
ordered cuboctahedral particles were also observed in the same
sample (Fig. S2, ESI†). The mean edge length was determined to be
around 1.2 mm. Note that there are several truncated cubic particles
with an edge length of ca. 350 nm in the bottom left of Figure S2.† It
seems that sintering a-Fe2O3 at 723K for 16 h produced amixture of
polyhedra with different shapes. Although the products were domi-
nated by the bigger octahedra, the structural transformations from
octahedron to cuboctahedron and truncated cube should be
involved.
For sample 3, we found that the major products were truncated
cubes (with a mean edge length of about 500–800 nm, see Fig. 1D)
accompanied by some cuboctahedra (see Figure S3, ESI†). No
octahedral structures were observed. Moreover, it was found in
Figure S3 (ESI†) that the cuboctahedral particles were covered by
small pieces of other particles.We also noticed that the cuboctahedral
structures in sample 3 aremuch bigger andmore equiaxed in shape in
comparison with those in sample 2.
Together, these results not only provide the first example of
cuboctahedral a-Fe2O3 crystals, but also strongly demonstrate that
the crystal structure of the a-Fe2O3 particles has undergone
a continuous transformation from small octahedra to big octahedra,
cuboctahedra and truncated cubes with the increase in sintering
times. Therefore, the sintering time is an essential condition in
controlling the morphologies of the a-Fe2O3 crystals in this
approach.
Studies presented so far on the continuous transformations among
octahedral, cuboctahedral and truncated cubic structures have been
limited to a cubic crystal system.30–35 However, all the a-Fe2O3
crystals reported in this work and elsewhere belong to a hexagonal
crystal system.35 Considering the a-Fe2O3 crystals obtained here
exhibit a typical polyhedron transformation, 36,37 it would be inter-
esting to reveal themechanism of this structural transformation in the
developed polyhedral system.
Fig. 2a, c and e show the transmission electron microscopy (TEM)
images of an octahedral structure (sample 1), a cuboctahedral
structure (sample 2), and a truncated cubic structure (sample 3),
respectively. Further structural characterization of the polyhedra was
carried out by selected-area electron diffraction (SAED) patterns
(Fig. 2b, d and f). These patterns not only reveal that the a-Fe2O3
particles have a single-crystalline structure, but also present
3356 | CrystEngComm, 2012, 14, 3355–3358
[0001] and [2�1�10] zone axis in a hexagonal structure, as shown in
Fig. 2b, d and f. The view directions of the polyhedra are illustrated in
this figure.
A possible formation and transformation mechanism for the
a-Fe2O3 particles was proposed as follows. Some of the b-CD
molecules decomposed under oxygen to form carbon dioxide and
water (eqn (1)), while others were carbonized to produce carbon
particles (eqn (2)).38 The generation and growth of a-Fe2O3 crystal
seeds (eqn (3) and (4)) might to be affected by the in situ carbon
particles produced during synthesis. We used Raman spectra to
investigate the generation of carbon particles during the formation of
the a-Fe2O3 polyhedra. Based on the Raman spectra (Figure S4,
ESI†), we found that the carbon particles are only detectable in a very
early stage (0.5 h) of the sintering process. After sintering for 8 h
(sample 1) or longer (samples 2 and 3), no carbon signals were found.
These observations suggest that the adsorption of the carbon particles
and its capping effect did not play a key role in the generation of
cuboctahedral and truncated cubic a-Fe2O3 crystals. Thanks to the
theoretical studies from other groups on the surface energies of a-
Fe2O3,14,15 the {10�1 2} planes of a-Fe2O3 crystals were found to have
the lowest surface energy. Since the truncated cube of a-Fe2O3 was
mostly encased by such planes, it should be the lowest energy
morphology compared to the octahedron and cuboctahedron struc-
tures. As such, it is not hard to understand the mechanism for the
transformation from octahedra to cuboctahedra and truncated cubes
at an elevated temperature (723 K) due to the thermodynamic
consideration, as shown in Fig. 3. It is also worth noting that, in the
early stage of the reaction, the synthesis is often known as
This journal is ª The Royal Society of Chemistry 2012
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a kinetically controlled process39 and the nanocrystals will take shapes
deviating from the thermodynamically favored one. In this case,
octahedra enclosed by {0001} facets are formed.
C42H70O35 þ 42O2 �����!D42CO2 þ 35H2O (1)
C42H70O35 �����!D42Cþ 35H2O (2)
FeCl3 þ 3H2O �����!DFeðOHÞ3 þ 3HCl (3)
2FeðOHÞ3 �����!D
Fe2O3 þ 3H2O (4)
The effect of the sintering temperatures on the construction of the
a-Fe2O3 crystal structures was also investigated by controlled
experiments. As shown in Figure S5 (ESI†), the a-Fe2O3 particles
obtained at 673 K for 24 h (sample 4) are much smaller (about 200–
300 nm in size) andmore irregular, when compared with sample 3. In
addition, no cuboctahedral and truncated cubic structures were
found, though several octahedral structures appeared. This result
suggests that a lower temperature (50 K) is beneficial for the gener-
ation of small particles, but is highly disadvantageous to the forma-
tion of symmetrical polyhedral structures. In another set of
experiments, we noticed that the a-Fe2O3 crystal obtained at 773 K
for 24 h (sample 5) is composed of a large number of incomplete
polyhedra with a mean edge length of about 1.5–2.0 mm, as shown in
Figure S6, ESI.†
We also investigated the dependence of the magnetic properties of
the five a-Fe2O3 samples on their sizes and shapes using a super-
conducting quantum interference device (SQUID). Fig. 4 shows the
hysteresis loops of samples 1–3, indicating weak ferromagnetic
properties at 300K for this set of samples, which is in agreement with
the observations previously reported.40
The hysteresis loops of samples 4 and 5 (Figure S7, ESI†) nearly
coincide, and they exhibit a lower saturation magnetization (Ms <
0.22 emu g�1) and a lower remanence (Mr < 0.06 emu g�1) compared
to sample 3 (Ms, 0.32 emu g�1 andMr, 0.11 emu g�1). Although all of
the samples have a similar coercivity (Hc, 517Oe), there is a difference
in the shape of the hysteresis loops near the coercive field. This
difference is a reflection of the difference in the rotation of the
magnetic domains in the crystals with different sizes and morphol-
ogies. However, in the cases of samples 1 and 2, there is no saturation
of the magnetization at 300 K in fields up to the maximum applied
magnetic field (30 kOe), and their magnetizations at 30 kOe are 0.83
and 1.35 emu g�1, respectively. The higher magnetizations are
ascribed to a uniform intensity of themagnetization in a thicker crust.
At the same time, the two samples present a small hysteresis loopwith
Fig. 4 Field dependencies of themagnetizations of samples 1–3 at 300K.
This journal is ª The Royal Society of Chemistry 2012
the same coercive forces of 3.7 kOe but different remnant magneti-
zations of 0.23 and 0.35 emu g�1. These results reveal that the size and
shape are two important factors in tuning the magnetic properties of
the a-Fe2O3 crystal materials. This may be related to different
magneto-crystalline anisotropies in different microstructural
phases.41,42
In conclusion, a series of a-Fe2O3 crystalline materials with
different fascinating polyhedral morphologies, such as octahedral,
cuboctahedral and truncated cubic structures, were prepared through
a novel solid-phase sintering process. A mechanism was proposed to
explain the formation and transformation of the polyhedral struc-
tures. Our result suggests that the Wulff’s polyhedral transformation
given in a cubic crystal system can be extended to a hexagonal crystal
system. It also demonstrates that such a structural transformation
between the polyhedral crystals of a-Fe2O3 can be easily controlled
by the sintering times.We believe that these findings will contribute to
the understanding of controlled structural and physical characteris-
tics in nanocrystals.
This project was supported by NSFB (No. J1030412) and NSFC
(No. 21071139).
Notes and references
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