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Q. Zhou et al. / Physica B 391 (2007) 206–211
207
layers by altering the size of the ferromagnetic grains,
making artificial boundaries or diluting with a nonmag-
netic insulator will significantly influence the transport
process [9–11]. In recent years, it was reported that
introduction of a second phase into the ferromagnetic
manganite matrix had resulted in an enhancement of MR
[12–14]. These secondary phases include insulating oxide
[11,12]; half-metallic ferromagnet [13] and polymer com-
posite [14], etc. It was further pointed out that the
conduction behavior and MR effect of the perovskite
manganites are significantly influenced by the grain
connectivity [15,16].
measurements were performed by standard four-probe
method in the temperature range from 380 to 20 K. The
MR was defined as MR ¼ (r0ꢀr3 T)/r0, where r3 T and r0
are the resistivities measured at 3 T magnetic field and zero
field, respectively.
3. Results and discussions
Fig. 1 shows a series of powder XRD patterns of
LSMO(1400 1C), Zr1h, Zr4h, Zr8h, Zr24h, and Zr48h,
recorded at room temperature. The XRD pattern for the
undoped sample shows a single-phase perovskite structure
¯
with R3c symmetry. But the impurity phases including
In this paper, we introduce ZrO2 as the second phase
into the manganite and investigate the effect of sintered
time on magnetotransport properties and MR in La2/3Sr1/
3MnO3 (LSMO)+0.1 (the mole fraction) ZrO2 granular
composites. Firstly, the LSMO manganite is nearly 100%
spin polarization [6], which may boost magnetoresistance
associated with spin-dependent tunneling; and LSMO has
high Curie temperature (TCE360 k) [2], being available to
attain a large MR at room temperature. Secondly, due to
the low solid solubility of Zr ions in La2/3Sr1/3MnO3, only a
small amount of Zr4+ ions go into the lattice of La2/3Sr1/3
MnO3 [17] and most Zr4+ ions segregate as secondary at
grain boundaries insulating compounds at higher Zr
content [17,18], which will influence the transport process.
Thirdly, the grain connectivity of samples can be improved
by high-temperature sintering with long time [15,16].
SrZrO3, La2Zr2O7 and ZrO2 occur in all Zr-doped samples
investigated here. These impurity phases are still retained
even after 48 h sintering at 1400 1C, indicating that only
limited amount of Zr can go into the lattice of La2/3Sr1/
3MnO3. Although these impurity phases appear in all our
doped samples, their contents are quite low (see the inset of
Fig. 1). The lattice parameters of these samples are shown
in Table 1. The lattice parameters of LaMnO3.15 in
˚
the JCPDSICDD (No. 32-0484) are a ¼ 5.523 A and
˚
c ¼ 13.324 A in a hexagonal system. The lattice parameters
of our sample for LSMO are close to these values. The
lattice parameters of LSMO+0.1(ZrO2) sets of samples
increase slightly with the sintered time. This can be
explained in terms of the different ionic radii of Zr4+
and Mn4+ ions (they are 0.72 and 0.53 A, respectively [19]),
˚
or in terms of the oxygen vacancies as reported by Rojas et
al. [20].
2. Experimental
Fig. 2 shows the typical SEM micrographs for several
samples. It can be seen that the size of grains gradually
increases and the connectivity between grains becomes
excellent with prolonging sintered time. One hour sintered
sample is very porous with a small grain size of about 5 mm
and contains a large number of weakly linked grain
boundaries. By contrast, the 48 h sintered sample appears
very dense with an excellent connectivity and melting
LSMO+0.1(ZrO2) samples were fabricated by three
steps. Firstly, the LSMO powders were prepared by sol–gel
method [17] and sintered at 1300 1C for 8 h. Secondly, the
ZrO2 particles were pre-prepared by a thermal decomposi-
tion method. Zr(NO3)4 ꢁ 5H2O was sintered in air at 650 1C
for 8 h. Thirdly, the above two pre-prepared powders in an
appropriate mole ratio were completely mixed, ground
carefully, and subsequently pressed into discs under
400 MPa. The final sintering process was carried out at
1400 1C in air for 1, 4, 8, 24, 48 h, respectively, and then
furnace cooled in air, to obtain a series of granular samples
(these samples are called Zr1h, Zr4h, Zr8h, Zr24h, Zr48h,
respectively), as well as LSMO was carried out at 1300 and
1400 1C for 8 h in air. X-ray diffraction (XRD) was used to
characterize the structure of the samples with Bruker D8-
ADVANCE. The morphology was probed by FEG SEM
Sirion. An X-ray photoelectron spectroscopy (XPS)
spectrum was obtained with Kratos XSAM800. Mg Ka
(1253.6 eV) X-ray source was used for excitation. The
resistivity r and saturated magnetization Ms measurements
were carried out by physical property measurement system
(PPMS). The DC magnetization measurements were carried
out with the vibrating sample magnetometer (VSM) of the
IDE Corporation in the temperature region of 150–400 K.
The paramagnetic–ferromagnetic transition temperature
(TC) was taken as the minimum dM/dT. The resistivity
Zr48h
Zr24h
Zr8h
Zr4h
Zr1h
26
27
28
29
2θ (deg.)
30
31
32
Zr48H
Zr24H
Zr8H
Zr4H
Zr1H
LSMO
20
30
40
50
60
70
80
2θ (deg.)
Fig. 1. X-ray powder diffraction patterns of LSMO(1400 1C), Zr1h, Zr4h,
Zr8h, Zr24h and Zr48h. The inset shows the relative enlarged diffraction
patterns.