Materials Science and Engineering B 190 (2014) 52–58
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Materials Science and Engineering B
jo ur nal home p age: www.elsevier.com/locate/mseb
Structural and magnetic properties of CoFe
2-x
Mo
x
O
4
nanocrystalline ferrites
Mohamed Bakr Mohamed
a
, Adel Maher Wahba
b,∗
, M. Yehia
c
a
Ain Shams University, Faculty of Science, Physics Department, Cairo, Egypt
b
Tanta University, Faculty of Engineering, Department of Engineering Physics and Mathematics, Tanta, Egypt
c
Reactor Physics Department, Nuclear Research Center, Atomic Energy Authority, PO Box 13759 Cairo, Egypt
a r t i c l e i n f o
Article history:
Received 4 May 2014
Received in revised form 10 August 2014
Accepted 2 September 2014
Available online 16 September 2014
Keywords:
Cobalt ferrite
Magnetic properties
Cation distribution
Mössbauer spectroscopy
a b s t r a c t
Structural and magnetic properties of CoFe
2-x
Mo
x
O
4
(x — 0, 0.04, 0.08, 0.12, 0.16, 0.2, and 0.3) nano fer-
rites synthesized by autocombustion method were investigated. X-ray powder diffraction patterns have
confirmed the pure cubic crystalline phase of the synthesized nanoparticles. Magnetic properties were
explored using vibrating sample magnetometry and Mössbauer spectroscopy. Both the crystallite size
(D) and the saturation magnetization (M
s
) decreased continuously with increasing Mo content. Bertaut
method based on X-ray diffraction, infrared spectroscopy (IR) data, saturation magnetization and Möss-
bauer spectroscopy were used to suggest the cation distribution in tetrahedral (A) and octahedral [B]
sites for the whole samples.
© 2014 Elsevier B.V. All rights reserved.
1. Introduction
The nano-size CoFe
2
O
4
is an important magnetic material
for its wide range of applications including electronic and
microwave devices [1], ferro-fluids [2], and high-density infor-
mation storage [3]. Its excellent properties include high cubic
magnetocrystalline anisotropy [4], high coercivity [5], reasonable
saturation magnetization [6], and high Curie temperature T
c
[7].
Molybdenum-substituted ferrites have been investigated as an
attempt to understand the correlation of the cation distribution
with both electric and magnetic properties [8–10]. The cation
distribution of such ferrites is characterized by the existence of
mixed-valence states of Fe, Mo, and/or Co cations [11]. Dwivedi
et al. [9] recorded a coexistence of both ferroelectricity and mag-
netic ordering around room temperature in Mo-substituted cobalt
ferrite. They suggested that Mo enters into the tetrahedral site
where it transforms Fe
3+
into Fe
2+
cations to maintain the charge
neutrality. They also argued that the observed giant dielectric-
constant values are attributed to the Maxwell-Wagner relaxation
process and that the origin of ferroelectricity is the presence of
d
0
-ness of Mo
6+
ion. Well known is that nanoferrites can be easily
oxidized between 100 and 500
◦
C, while keeping its original struc-
ture. This provides the possibility of the metal cations to appear in
∗
Corresponding author. Tel.: +020 1281138450; fax: +020 226842123.
E-mail address: a m wahba@yahoo.co.uk (A.M. Wahba).
more than single valence state; the fact that allows both electric
and magnetic properties to be tailored for several applications, e.g.
sensors and multiferroics [9,11–13].
In the present work, citrate-precursor autocombustion method
was used to prepare Mo-substituted CoFe
2-x
Mo
x
O
4
nanoferrites
(x
—
—
—
—
0, 0.04, 0.08, 0.12, 0.16, 0.2 and 0.3), in which Fe
3+
was partially
substituted by Mo
6+
. The latter is characterized by its high valence
state and its d
0
electronic configuration. The effect of Mo substi-
tution on the structural and magnetic properties of nano CoFe
2
O
4
was investigated using XRD, IR, Mössbauer spectroscopy and VSM
magnetometery. The cation distribution suggested based on those
measurements was compared to that obtained for the bulk Mo-
substituted cobalt ferrites.
2. Experimental
Nanocrystalline CoFe
2-x
Mo
x
O
4
(x
—
—
—
—
0, 0.04, 0.08, 0.12, 0.16,
0.2, and 0.3) were prepared using citrate-precursor autocom-
bustion method [14]. Analytical grade stoichiometric amounts of
Co(NO
3
)
2
·6H
2
O, Fe(NO
3
)
3
·9H
2
O, (NH
4
)
6
Mo
7
O
24
and dehydrated
citric acid C
6
H
8
O
7
were used as starting materials. Metal com-
pounds and citric acid were dissolved in minimum amounts of
doubly distilled water. The citric to the all-metal molar ratio was
chosen as 1:1. Metal solutions were mixed together and then the
citric solution was added, followed by one-hour stirring using a
magnetic stirrer. Ammonia solution (NH
4
OH) was then added drop
by drop to the nitrate-citrate solution to adjust the pH value at 6.0;
http://dx.doi.org/10.1016/j.mseb.2014.09.010
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