Ram A. Pawara,
Sunil M. Patangeb and
Sagar E. Shirsath*c
aDepartment of Physics, Arts, Commerce and Science College, Satral 413711, MS, India
bMaterials Science Research Laboratory, SKM, Gunjoti, Osmanabad 413613, MS, India
cDepartment of Physics, Vivekanand College, Aurangabad 431001, MS, India. E-mail: shirsathsagar@hotmail.com; Tel: +91 9421666605
First published on 9th August 2016
Nanoparticles of Ho3+ substituted in Co–Zn ferrites were synthesised by sol–gel method. The phase formation of these samples has been confirmed by X-ray powder diffraction technique. XRD Rietveld refinement carried out using the FULLPROF program shows that the Co–Zn ferrite retains its single phase cubic structure with space group Fd3m for x ≤ 0.05. Occupancy of the cations is explained on the basis of site preference, size and valance of the substitution cations. The nanostructure and morphology of prepared samples were investigated by field emission scanning electron microscopy and transmission electron microscopy. The elemental percentage of the constituent ions was determined using energy dispersive spectroscopy. The magnetic interactions among the nanoparticles were analyzed by employing a temperature dependent vibration sample magnetometer, field cooled (FC)/zero field cooled (ZFC) measurements. The ZFC and FC curves diverge below the blocking temperature exhibiting a ZFC cusp at 195–225 K. The saturation magnetization of Co–Zn ferrite increased linearly with Ho3+ substitution for x ≤ 0.05 and almost remains constant thereafter. The frequency dependence of the AC susceptibility measurements was performed on the sample. It shows a peak at around spin freezing temperature, with the peak position shifting as a function of driving frequency, indicating a spin-glass-like transition of the sample.
Special attention has been given to cobalt containing spinel ferrites due to their large magneto-crystalline anisotropy and high saturation magnetization which is promising for magnetic materials in recording media. CoFe2O4 is an inverse spinel oxide having structural formula (Fe3+)A[Co2+Fe3+]BO4. All the Co2+ ions normally occupy the octahedral [B] sites due to its favorable atomic radius and charge distribution in an octahedral crystal field and the Fe3+ ions are equally distributed between the (A) and the [B] sites.12 The FeA–O–FeB interaction is very strong and CoFe2O4 is ferrimagnetic below 790 K (TN, Neel temperature). On the other hand, ZnFe2O4 is a normal spinel with structural formula (Zn2+)A[Fe23+]BO4. The FeA–O–FeB interaction is not effective in ZnFe2O4 due to the absence of the magnetic ion at the tetrahedral (A) site and the TN is only ∼9 K. In the case of Co–Zn ferrites the general distribution of cations among (A) and [B] sites is given by (Zn1−xFex)A[CoxFe2−x]BO4. On substitution of Zn2+ in Co ferrite the Fe3+ ions migrate from (A) to [B] site and consequently the FeA–O–FeB interaction becomes feeble.13 The magnetic measurements have revealed that the TN of bulk Co0.2Zn0.8Fe2O4 is ∼200 K, which is much smaller than TN of the CoFe2O4, but considerably higher than that of ZnFe2O4.14 Marked improvement in the saturation magnetization of Co ferrite has also been observed with the substitution of proper amount of Zn ions.15–17 However the coercivity, remanent magnetization and resistivity found to decrease for these samples.
Rare earth lanthanides (Ln3+) substituted ferrites are nowadays under extensive investigations in order to enhance the saturation magnetization, permittivity and permeability. Experimental and theoretical investigations of the exchange interactions in the rare earth-transition metal (4f–3d) elements containing spinel oxides have received more attention in the recent years.18–20 At the same time rare earth ions expected to affect spin-glass behavior.21 Large magneto-crystalline anisotropy in CoFe2O4 arises due to a strong spin (S)–orbit (L) coupling in Co2+ ions and similar strong spin–orbit (L–S) coupling has been noted in 4f grouped rare-earth (RE3+) ions. By introducing RE3+ Co–Zn, RE3+ ions are stabilized in B-sites of the spinel structure. Hence, one would expect a significant change of magnetic moment, ferromagnetic ordering temperature and anisotropy energy constant in the spinel structure of Co–Zn ferrite upon RE doping. RE3+ ions have a variety of magnetic properties, their magnetic moment vary from 0 to 10.6 μB, among them Ho3+ ions posses the highest magnetic moment of 10.6 μB.
One of the challenging issues for physics, chemistry and material science researchers with these compounds is their synthesis in single phase and understanding of their complex magnetism such as spin glass behavior at low temperature. Our aim is to probe the complex magnetic nature of Ho3+ ions in Co–Zn (Co0.7Zn0.3HoxFe2−xO4) compound using the probe of temperature, frequency and magnetic field dependent magnetic properties. We concentrated on some aspects, which we feel are important to unearth the complex magnetism of these systems.
The phase formation identification of the prepared samples was characterized by X-ray diffraction (XRD, Philips X'Pert instrument) with Cu-Kα radiation (wavelength λ = 1.54056 Å) at room temperature. The grain morphology and particle size was investigated by field emission scanning electron microscopy (FE-SEM) (FEI NOVA NANOSEM 600) and transmission electron microscopy (TEM) (JEOL 3010) respectively. Magnetic hysteresis was measured at 10 and 300 K using vibrating sample magnetometer. Field cooled (FC) and zero field cooled (ZFC) measurements with an external applied magnetic field of 100 Oe were carried out in the temperature range of 50–350 K. AC susceptibility measurements were carried out with varying temperature from 50 to 350 K at three different frequencies; 100, 500 and 1000 Hz with an applied magnetic field of 10 Oe (with a commercial superconducting quantum interference device, Quantum Design, USA). 57Fe Mossbauer measurements were carried out in transmission mode with 57Co radioactive source in constant acceleration mode using standard PC-based Mossbauer spectrometer equipped with Wissel velocity drive. Velocity calibration of the spectrometer is done with natural iron absorber at room temperature. The spectra were analyzed with NORMOS program considering the distribution of hyperfine fields.
The obtained values of weight percent of spinel phase and second phase are listed in Table 1, that shows spinel phase for x > 0.05 slightly decreased with Ho substitution. Therefore, the small amount of Ho3+ ions in Co0.7Zn0.3Fe2O4 can affect not only the phase composition but also the size of the spinel matrix, which is due to orthoferrite (HoFeO3) phase.24,25 It has been reported that phase formation is affected by the concentration of rare earth element, Ho3+, in substituted samples of CoFe2O4.26 The most important reason for the phase formation in the Ho3+ substituted Co–Zn ferrites is the electronic configuration, larger ionic radii of the Ho3+ rare earth element and diffusion of Ho3+ ions at the grain boundaries. K. Bharathi et al.27 relate such distortion in the lattice to the changes in the O–Fe and O–Co bond lengths at octahedral B site. It is worth to mention here that, upto x = 0.05, Ho3+ is highly soluble in Co–Zn ferrite. This level of Ho3+ solubility is quite better as compared to previous reports (ref. 22–26) related to rare earth doping. This could be mainly related to the synthesis condition of the prepared samples. The lattice constant (a) increased from 8.401 to 8.419 Å with increase Ho ions. The increase in a is linear up to x = 0.05, whereas it almost remain constant for x > 0.05. The increase in a with Ho3+ substitution can be explained on the basis of difference in ionic radii between Ho (1.04 Å) and Fe (0.67 Å) ions, where smaller Fe ions at octahedral B site are replaced by the larger Ho ions. The rare earth Ho ions may induce root mean square (rms) lattice strain in Co–Zn ferrite due to its larger ionic radii. Therefore, using the XRD data; Williamson–Hall (W–H) extrapolations as a Lorentzian function were utilized to determine the lattice strain in all the samples (Fig. 4). The Williamson–Hall plots show that the slopes of all plots are negative. This negative slope indicates that strain could be very small. The negative slope of the plots of all samples also indicates compressive strain experienced in smaller grain size samples. As the Ho3+ substitution is increased up to x ≤ 0.5, slop is changing its sign from negative to positive which is an indication of increase in strain. Further, for x ≥ 0.075 the W–H plot almost remains flat confirming that Ho3+ ions have the limit to enter into Co–Zn spinel lattice. The average crystallite size (tXRD) of the synthesized powders is calculated from the XRD line broadening of the (311) peak using Scherer's equation28 value crystalline size are display in Table 1 crystalline size in order to few nanometer.
Comp. x | x = 0.0 | x = 0.025 | x = 0.05 | x = 0.075 | x = 0.1 |
---|---|---|---|---|---|
W% of spinel phase | 100 | 100 | 98.9 | 98.3 | 97.8 |
W% of secondary phase | 0 | 0 | 1.1 | 1.7 | 2.2 |
tXRD (nm) | 45 | 42 | 44 | 40 | 38 |
In spinel ferrites, metal ions occupy tetrahedral (A) and octahedral [B] site. In the present system, occupancy of atom is calculated using the FULLPROF program. The values of atomic coordinates, occupancy and inversion parameter are given in ESI Table 2.† It is observed from Table 2 that Zn ions preferred tetrahedral A site, the Ho3+ ions show a preference for octahedral B sites. It is to explain that the radius of the octahedral site is larger than that of tetrahedral site in the spinel lattice. As the ionic radius of the Ho3+ ion is 1.04 Å which could be large for tetrahedral A site and therefore these larger Ho3+ ions occupy octahedral site. The small amount of Ho3+ cations substituted for Fe3+ cations which enter into the octahedral sites by rearrangement of cations between the tetrahedral and octahedral sites to minimize the free energy of the system. It is also observed that Co2+ ion initially occupy only octahedral sites, but as the Ho3+ concentration increased Co2+ ions occupied both sites. Partial migration of Co2+ ions from B to A sites has been observed by increasing the Ho3+ concentration.
Ions | x = 0.0 | x = 0.025 | x = 0.05 | x = 0.075 | x = 0.1 |
---|---|---|---|---|---|
Zn | 0.2998(2) | 0.2998(3) | 0.2997(3) | 0.2998(2) | 0.2997(3) |
Fe | 0.6998(2) | 0.6999(1) | 0.6998(2) | 0.6998(2) | 0.6999(1) |
Co | 0.6998(2) | 0.7000(1) | 0.6998(2) | 0.6999(1) | 0.6998(2) |
Fe | 1.2999(2) | 1.2751(1) | 1.2503(2) | 1.2252(2) | 1.2000(1) |
Ho | 0.0000 | 0.0249(1) | 0.0498(2) | 0.0749(1) | 0.0999(1) |
O | 3.998(2) | 3.997(4) | 3.996(4) | 3.999(2) | 3.998(3) |
Energy dispersive spectroscopy (EDS) was carried out to determine the elemental composition of the prepared samples. Fig. 5 display the EDS pattern of a typical sample of Co0.7Zn0.3Fe2O4 (x = 0.0) and the results obtained on the elemental analysis are presented in ESI Table 3.† It is observed that the theoretical and observed elemental compositions are in good agreement with each other. The surface morphology and grain size were observed using FE-SEM (Fig. 6). It is evident that the grain sizes are uniformly distributed, however, there are some abnormal grain growth is also observed. The presence of smooth grain boundaries can also be seen in the FE-SEM images.
TEM images of typical samples (x = 0.0 and 0.1) are represented in Fig. 6. The TEM image for pure Co–Zn ferrite reveal that the nanoparticles are almost regular in shape, cubic in nature, partially agglomerated with uniform particle size. On the other side particle size is not uniform for Ho3+ substituted Co–Zn ferrite (x = 0.1). Some of the Ho3+ ions segregated on the grain boundaries of Co–Zn ferrite thereby minimizing the possibility of increasing the grain size by the process of agglomeration. Ho3+ with its larger ionic radii required greater energy to replace Fe3+ and to form the Ho–O bond. Energy is utilized for this process at the expense of crystallization and therefore the decrease in crystalline nature with smaller particle size is observed. Similar decrease in crystallinity is reported by L. Zhao et al.29 with the inclusion of Nd3+ in cobalt.
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Fig. 7 Variation of magnetization (M) with applied magnetic field (H) of Co0.7Zn0.3HoxFe2−xO4, measured at 300 K and 10 K. |
The increase in Ms at 10 K is attributed to frozen spin-glass-like state on the surfaces of the nano-particles where the decrease in thermal energy and magnetic moments get aligned along the external magnetic field direction. Since at high temperatures, the surface spins can experience many disorder states with similar energies in a short time, which weakens their response to the applied magnetic field and thus lowers the magnetization as compare to their bulk counterpart. However, below the freezing temperature, the surface spins may freeze to a certain state, which increases the projection of the moments in the direction of applied magnetic field. Magnetic hardness, associated with the sharp increase of coercivity is observed for Ho3+ substituted Co–Zn ferrite at 10 K. This may correspond to the appearance of the exchange anisotropy field (HE). The observation of this exchange anisotropy field is a clear indication of the existence of a magnetically disordered surface layer that becomes frozen at low temperature.30 Therefore, the observed increase of the coercivity can be attributed to the extra energy required for the switching of the core spins that are pinned by the exchange interactions with the frozen spin glass-like surface layer. The direct competition of exchange interactions between surface spins lies at the origin of the observed high field irreversibility and accounts for the large experimental values of the coercive fields.31
To inspect the existence of magnetic ordering in pure Co–Zn and Ho3+ substituted Co–Zn ferrite nanoparticles, these samples were subjected to FC-ZFC measurements with an applied magnetic field of 100 Oe (Fig. 8). The typical spin-glass cusp-like maximum in the ZFC curve is observed which is corresponding to the blocking temperature (TB). To determine the TB; the differentiate analysis is carried out and the temperature corresponding to the maximum temperature is determined as dM/dT becomes zero. It is observed that TB shifts from 195 K (x = 0.0) to 225 K (x = 0.1). Below TB, with decreasing temperature the B site antiferromagnetic (JBB) interactions become stronger which compete with the (JAB) ferrimagnetic interactions. The competition between the exchange interactions results in strong spin frustration and decrease of magnetization at low temperature. At temperatures above TB, the thermal energy (i.e., kBT) is higher than the magnetic energy barrier and thus the materials become superparamagnetic following the Curie–Weiss law. Tirr is the temperature, at which FC and ZFC curve bifurcate, also undergo changes with Ho3+ substitution. It is observed that Tirr for x = 0.0 is 229 K whereas it is 270 K for x = 0.1. In ZFC, the domain structure at low temperature state differs from the high temperature state and the domain structure gets adjusted as the temperature is increased. In FC, the domain structure retains its state at high temperature configuration from 50 K to 300 K. It is to be noted that bifurcation temperature, Tirr, is higher than that of the TB, such behavior in FC-ZFC indicates the existence of strong dipole–dipole interaction among spins.32
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Fig. 8 Variation of magnetization (M) with temperature (T) measured in field cooled (FC) and zero field cooled (ZFC) mode at 100 Oe. |
The large difference between the magnetizations in ZFC and FC indicate that Ho3+ substituted Co–Zn ferrite possess higher coercivity at lower temperature. This coercivity can be related to the anisotropy constant in Ho3+ substituted Co–Zn ferrite cubic spinel system. In this system Co2+ ion induces this anisotropy as the Fe3+ has no orbital momentum and Co2+ in the low symmetry coordination has an orbital contribution caused by the relevant spin–orbit coupling that gives rise to single ion anisotropy. The anisotropy constant was obtained from the fitted ZFC curve:33
It is observed from FC curves that magnetization continuously decreased with the increase in temperature. The temperature dependence of the Ms can be well fitted to Bloch's spin wave theory. Bloch's law describes the temperature-dependence of the Ms of ferri/ferromagnetic materials where Ms(T) is dominated by the excitation of long wavelength spin-wave fluctuations, called magnons. In case of contiguous distribution of spin-wave states as in the bulk, the temperature dependence of magnetization given by the Bloch law as:34
AC susceptibility measurements are useful to understand the dynamics of freezing of the spin-glass systems in which the temperature associated with the maxima of χ′ corresponding to spin freezing temperature (Tf), varies with the Ho3+ substitution. Fig. 9 shows the variation of χ′ vs. T at selected frequencies of 100, 500 and 1000 Hz for the end samples (x = 0.0 and x = 0.1) of the present study where the magnitude of ac magnetic field is kept constant at Hac = 10 Oe. It is found that a small shift of the peak position of χ′ to higher temperature for higher driving frequency. The peak shift per frequency decade is quantified in the phenomenological parameter K = ΔTf/Tf(Δlogf), where ΔTf is the difference between Tf measure in Δlog
f frequency interval.36 The value of K represents the strength of inter-particle interaction among magnetic nanoparticles. This parameter lies in the range of 0.005 to 0.06 for interacting nanoparticles of spin glass systems.37 In the present system it is 0.0097 for x = 0.0 and 0.011 for x = 0.1, supporting the claim of spin glass behavior. The intensity of the peak increases for lower measuring frequencies. Furthermore χ′(T) curves for different measuring frequencies overlap for temperatures higher than the peak temperature. This behavior is observed in many spin-glass and disordered magnetic system,38,39 that confirmed the transition from paramagnetic to spin glass phase in pure Co–Zn (x = 0.0) and Ho3+ substituted Co–Zn (x = 0.1) ferrite. The spin freezing temperature Tf can be accurately determined by the position of the cusp of the real part of AC susceptibility, χ′, and it is observed for both the samples. In other words, the maximum relaxation time (τ) of the system is equal to 1/f at Tf. A shift in the Tf from 234 K to 251 K for f = 100 Hz, 241 K to 260 K for f = 500 Hz and 246 K to 268 for f = 1000 Hz is observed as Ho3+ substitution in Co–Zn ferrite changed from x = 0.0 to 0.1.
In order to gain clear insight into the spin glass behavior by considering the interaction nano-particles. The data is fitted to Vogel–Fulcher equation: τ = τ0exp[−Ea/kB(Tf − T0)], where τ0 is characteristic relaxation time, Ea is activation energy, kB is the Boltzmann constant and T0 a characteristic temperature which is the measure interparticle interaction energy.40 Fig. 9 shows the experimental and fitted curve for x = 0.0 and 0.1. The obtained parameters T0 and τ0 for Ea/kB = 811 K are listed in Table 3. The obtained τ0 from the fitted line of f = 100 Hz is 9.1 × 10−12 s for Co–Zn ferrite (x = 0.0), whereas it is decreased to 4.5 × 10−13 s for Ho3+ substituted Co–Zn ferrite (x = 0.1). Values of τ0 are in close proximity to spin glass system; the value of τ0 ∼10−13 s is identical in magnitude with that for atomic spin-glasses, for which τ0 denotes a spin flip time of individual magnetic moments belonging to atoms or ions. The decrease in τ0 of Co–Zn ferrite with increase in Ho3+ substitution could be attributed to the exchange coupling strength between nanoparticles. Interparticle interaction energy, T0, decreased from 195 to 217 K for Ho3+ substation and is in good agreement with the TB obtained from the ZFC curve.
Comp. | f (Hz) | Tf (K) | Vogel–Fulcher model | Spin glass power-law | ||
---|---|---|---|---|---|---|
T0 (K) | τ0 (s) | Tg (K) | τ0 (s) | |||
x = 0.0 | 100 | 234 | 195 | 9.1 × 10−12 | 203 | 5.3 × 10−12 |
500 | 240 | 198 | 8.2 × 10−12 | 207 | 4.3 × 10−12 | |
1000 | 246 | 208 | 5.2 × 10−13 | 210 | 4.9 × 10−13 | |
x = 0.1 | 100 | 251 | 217 | 4.5 × 10−13 | 220 | 4.4 × 10−13 |
500 | 260 | 224 | 3.2 × 10−13 | 229 | 2.2 × 10−13 | |
1000 | 268 | 232 | 1.7 × 10−13 | 238 | 1.2 × 10−13 |
To determine if the dynamics of a magnetic system exhibit critical slowing down, the ac susceptibility data can be compared to the predictions of dynamic scaling theory, which states that the relaxation time in a spin glass, related to the correlation length ξ as τ ∝ (Tf/Tg − 1)−v as glass transition as Tg is approached. Fitting the data with spin glass power-law could provide concrete information about the spin glass state:41
Fig. 10 shows the Mössbauer spectra of three typical samples x = 0.0, 0.05 and 0.1 recorded at room temperature. The data is analyzed with distribution of hyperfine fields. The observed sextet confirms the magnetic ordering in all the samples at room temperature. However, broadened nature six-line pattern may have arisen from the random distribution of magnetic (Fe, Co and Ho) and nonmagnetic (Zn) ions in the sublattices. It may also be due to the existence of magnetically ordered regions that are not coupled to each other by intersublattice, i.e. A–B superexchange interactions. Further, the center of the Zeeman pattern does not show any significant change for all the studied samples and could be related to the zero quadrupole splitting resulted from the presence of chemical disorder. The chemical disorder produces a distribution of electric field gradient (EFG) of varying magnitude, direction sign, and symmetry, that can be represented by the equation:43
|ΔEQ| = 1/2|ΔEQ0|(3![]() ![]() |
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Fig. 10 Room temperature Mossbauer spectra and their corresponding variation of hyperfine field distribution for the typical samples (x = 0.0, 0.05 and 0.1) of Co0.7Zn0.3HoxFe2−xO4. |
The obtained average isomer shift is consistent with Fe3+ state. The variation of hyperfine field distribution P(Bhf) as a function of field Bhf is also shown in Fig. 10. The shape of P(Bhf) shows a broad low field tail down to Bhf = 0 and a high field maximum. The hyperfine field distributions at high filed are broad for x = 0.0 and it becomes narrower as the substitution of Ho3+ increased to x = 0.1. This is connected with different local surroundings of the Fe atom in investigated compounds. The values of internal magnetic field Bhf depend upon the nearest neighbour distribution around Fe atoms, which increased as more Ho3+ atoms surround Fe atoms. The average hyperfine field of Co–Zn ferrite is increased from 45.55 T (x = 0.0) to 46.33 T (x = 0.1) with the substitution of Ho3+ substitution. According to Neel,44 contribution to hyperfine magnetic field is due to the strongest A–B superexchange interactions and contributions from to A–A/B–B exchange interactions may be neglected. As the ratio of Fe(B)3+/Fe(A)3+ should be decreased with the incorporation of the Ho3+ ions at octahedral B-site that expected to decrease in hyperfine field. However, with the increase in Ho3+ substitution it seems to be that A–B interaction increased as evident by increase in hyperfine field. This also supports the increase in saturation magnetization as observed by M–H loops measured at room temperature and at 300 K.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/c6ra12541g |
This journal is © The Royal Society of Chemistry 2016 |