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A.O. de Souza et al. / Journal of Alloys and Compounds 680 (2016) 701e710
refinement).
Fig. 5 shows the volume of primitive unitary cell (VC) as a
function of the iron concentration (x). The cell volume decreases
almost linearly with the iron concentration, at a rate of dVC/
dx ~ ꢁ0.06 Å3 and ꢁ0.01 Å3, for the tetragonal and cubic structures,
respectively.
This decrease may be explained based on the Fe3þ cation radius,
smaller than that of the Zr4þ cation, and confirms that iron enters
substitutional to zirconium in either the t-ZrO2 matrix, or the c-
ZrO2 matrix, forming Zr1-xFexO2 solid solutions. Vacancies gener-
ated by the doping (as shown below) may contribute to the volume
decrease as well.
Compared to the data reported in Ref. [39], the present values
for the volume of the tetragonal lattice differ only about 1%, but
present the same rate of change under the dopant concentration
variation. On the other hand, the results obtained by Ref. [40] differ
from the ours not only in magnitude (~3%) but also regarding the
range of stability of the c-Zr1-xFexO2 (mono)phase.
3.3. Magnetization characterization
Fig. 6 shows the curves of magnetization and the respective
reciprocal susceptibility as a function of temperature, for the
x ¼ 0.05, 0.07 and 0.09 samples.
Fig. 3. X-ray experimental diffractograms for the x ¼ 0 (a), 0.09 (b), 0.15 (c) 0.25 (d),
0.30 (e) and 0.40 (f) samples. Miller indexes in (a) and (c) are respective to the
tetragonal and cubic zirconia structures, respectively. The red arrows in (f) indicate the
peaks of the Fe2O3 phase. (For interpretation of the references to color in this figure
legend, the reader is referred to the web version of this article.)
For these concentrations, the magnetization grows mono-
tonically with decreasing temperature. FC and ZFC curves overlap
without evidence of magnetic irreversibility (i.e., a temperature,
Tirr, which indicates the separation of ZFC and FC curves). Therefore,
these samples show a feature typical of paramagnetic (PM) sys-
tems. However, the temperature dependence of reciprocal sus-
ceptibility curves reveals the possible existence of two Curie-Weiss
(C-W) regimes, one at higher temperatures and another at lower
temperatures.
the fact that the ionic radius of Fe3þ (the valence will be given by
€
the Mossbauer results presented later in this paper) (0.92 Å) is
smaller than that of Zr4þ (0.98 Å) in an eight-coordinated neigh-
borhood [38]. Hematite was pointed out as the phase formed from
the exceeding iron, also in samples prepared by other methods
[26,29].
In this sense, the cꢁ1 vs. T curves were fitted, using the
c
¼
c0 þ (T ꢁ
q)/C equation (i.e., a modified Langevin function),
considering different temperature ranges. The temperature-
independent signal c0 was added to the Langevin fitting pro-
cedures in order to allow for magnetic contributions other than the
specific Zr1-xFexO2 solid solution phase, composing the specimen to
be characterized (e.g., the sample holder). The parameters fitted
specifically taking into account separately the T ꢃ 100 K and
T ꢂ 100 K ranges are listed in Table 2 (which also includes data for
the x ¼ 015 and 0.25 samples). For the lowest temperature range, all
Fig. 4 shows refined diffractograms for the x ¼ 0.05 (Fig. 4a) and
x ¼ 0.20 (Fig. 4b) samples. All the refinements were performed
considering only one phase (i.e., tetragonal for 0 ꢂ x ꢂ 0.09 and
cubic for 0.15 ꢂ x ꢂ 0.25) and resulted in lattice parameters (see
Table 1) which are in good agreement with those previously ob-
tained, either for undoped ZrO2 or for iron doped zirconia [39e41].
Small differences observed between these and the present values
may be attributed to different methods of refining the X-ray profiles
(i.e., refinement programs used and parameters fixed initially in the
the C-W coefficients (q
0s) are small and negative, whereas for the
highest temperature range they totalize some tens of negative
Kelvin degrees. All these coefficients reflect AFM fluctuations,
although a change in the magnetic regime is effectively revealed in
going from RT to 10 K, for the three concentrations. This may be
attributed to a variation with temperature of the molecular field
constant,
g
(¼
q/r C) [42], which would weaken with decreasing
temperature, until an “almost ideal” paramagnet. However, in
every case the interactions between the magnetic moments are
weak and are overcame by thermal fluctuations, even at low
temperatures.
On the other hand, c0 presents typical values for frustrated
oxide systems [43e45], increasing slightly with x and the T range,
whereas the specific constant, C, does not show any noteworthy
trend, as the concentration or the T range vary.
In principle, the AFM fluctuations should involve only iron
magnetic moments, stabilized in trivalent state, as revealed by
€
Mossbauer spectroscopy. Considering the concentrations used and
a good dilution of the dopant in the ZrO2 matrix, the nearest ferric
cations are apart by two or three lattice parameters. Therefore, not
close enough for an effective exchange interaction. In other words,
a percolation threshold was not reached by the cations, somehow
Fig. 4. Refined X-ray diffractograms, for the x ¼ 0.05 (a) and x ¼ 0.20 (b) samples.