Prashant
Kumar
*abc,
Saurabh
Pathak
abde,
Arjun
Singh
abf,
H.
Khanduri
a,
G. A.
Basheed
ab,
Lan
Wang
c and
R. P.
Pant
*ab
aCSIR-National Physical Laboratory, New Delhi, India-110012. E-mail: rppant@nplindia.org; prashantkhichi92@gmail.com
bAcademy of Scientific and Innovative Research, CSIR-NPL Campus, New Delhi, India-110012
cSchool of Science, RMIT University, Melbourne, VIC 3000, Australia
dSchool of Engineering, RMIT University, VIC 3000, Australia
eDepartment of Mechanical Engineering, University of Melbourne, Parkville, VIC, 3010 Australia
fDepartment of Physics, Indian Institution of Technology, Jammu-181221, India
First published on 6th April 2020
A novel investigation on the finite-size effects on the spin resonance properties of cobalt ferrite (CoFe2O4) nanoparticles has been performed using a room temperature ferromagnetic resonance (FMR) technique. A single broad spectrum was obtained for the CoFe2O4 nanoparticle samples, which indicated that all the samples were showing ferromagnetic characteristics. An asymmetric FMR line shape with a hefty trailing section was obtained due to the high magneto-crystalline anisotropy in CoFe2O4 nanoparticles, which changed with the size distribution. The resonance field for the samples shifted to a higher value due to the increase in the magneto-crystalline anisotropy in the CoFe2O4 nanoparticles with an increase in size. A systematic change in the resonance field and line width was observed with the change in the size distribution of the particles. Initially, it decreased with an increase in the size of the particles and increased after the critical size range. The critical size range is the imprint of the shift of the magnetic domain from a single domain to multi domain. The line width increased at higher annealing temperatures due to the enhancement in the dipole–dipole interaction, which led to a higher spin concentration as well as magneto-crystalline anisotropy. Furthermore, the saturation magnetization (Ms) as well as ‘Mr/Ms’ increased from 37.7 to 71.4 emu g−1 and 0.06 to 0.31, respectively. The highest coercivity (750.9 Oe) and anisotropy constant (4.62 × 104 erg cm−3) were found for the sample annealed at 700 °C, which can be corroborated by the literature as the critical annealing temperature at which CoFe2O4 nanoparticles shift from single domain nanoparticles to multi-domain nanoparticles. Post-processing annealing is critical in advanced processing techniques and spin dynamics plays a vital role in various interdisciplinary areas of applications.
Ferrites belonging to the AB2O4 group (family) are mainly controlled by divalent cations, which occupy the tetrahedral ‘A’ sites, and trivalent cations, which have a high degree of affinity for the octahedral ‘B’ sites.11,12 Therefore, the whole range of distribution of cations possible in spinel ferrites can be shown by the general formula (M1−α2+ Feα3+) [Mα2+ Fe2−α3+], where cations inside the round and square brackets occupy the tetrahedral and octahedral sites, respectively. Alpha (α) represents the degree of inversion and shows the fraction of the tetrahedral site occupied by Fe3+ cations, which depends on the synthesis method and post-annealing. If α = 0, the spinel ferrite is normal; when α = 1, it is an inverse spinel ferrite. However, if 0 < α < 1, the spinel ferrites are mixed.7 The presence of two transition metal ions at the crystallographic site leads to a unique type of hopping conductivity and magnetic coupling. CoFe2O4 is an interesting material because of its high magneto-crystalline anisotropy, coercivity, chemical stability, good electrical insulation, mechanical hardness and moderate magnetization at room temperature.12,13 Apart from this, CoFe2O4 has excellent physical and chemical stability, which makes it suitable for magnetic recording applications as high-density digital recording disks. A recent investigation has shown that the cobalt ferrite nanoparticles have photo-induced magnetic properties.14 Magneto-crystalline anisotropy is a very important parameter in connection with the characterization of the materials utilized in technical applications, particularly magnetic recording media. Magneto-crystalline anisotropy strongly depends on the interaction of cations in the A and B sites, which can also be altered by changing the lattice-occupancy state, crystallite size, bond angle and bond length.7
Pure and doped CoFe2O4 show a variety of novel properties that vary with the nature of the cations, their charge and site occupancy distribution between tetrahedral and octahedral sites.7,11,15,16 Different experimental methods have been used in the preparation of ferrite nanoparticles such as sol–gel techniques,13 co-precipitation,1,17 hydrothermal,18 microemulsion19 and combustion methods,20etc. Among all of these, the co-precipitation method has been widely used as the prepared sample exhibits high crystallinity, homogeneity and good textural properties of the obtained material.1,7,17 Also, this technique offers an advantage due to its low cost, high-quality production and less time consumption.
Also, the magnetic properties of the CoFe2O4 nanocrystals depend on the different sizes, shapes and synthesis methods.20,21 C. H. Chia et al. prepared a series of CoFe2O4 nanocrystalline powders with varying synthesis temperatures and further annealing was done at different temperatures to optimize the structural and magnetic properties using the chemical co-precipitation method.17 They reported a significant increase in the saturation magnetization (Ms) from 43.2 to 60.7 emu g−1, with the annealing temperature from 300 to 1200 °C. A similar trend was also found in the coercive field (Hc), which increased from 376 Oe at 300 °C to 1201 Oe at 1200 °C. However, the coercive field Hc reached its maximum of 1373 Oe at 400 °C and then decreased to 870 Oe at 600 °C.22 The drastic change in Hc for high-temperature annealed samples (900 °C) might originate from the transition of a single magnetic domain to a multi-domain within a particle. Further, K. Rana et al.12 synthesized CoFe2O4 magnetic nanoparticles using the citrate precursor method and post-processing by annealing was done in the temperature range 700–1100 °C. They suggested that the increase in the crystallite size and magnetization was due to the increase in the annealing temperature. Also, the Ms and coercive field increased from 53.69 to 74.46 emu g−1 and 257.40 to 304.99 Oe, respectively. A linear increase in the saturation magnetization (Ms) with the annealing temperature was observed in CoFe2O4 MNPs, although the Ms values of the samples were significantly lower than the bulk value of 90 emu g−1.12
Even though numerous methods have been reported extensively for the CoFe2O4 preparation, the precise control of the size and morphology to achieve desired properties is still in progress. The investigation of spin dynamics plays a key role in the EMI shielding operation and has been reported for the CoFe2O4 by many researchers. However, most of the research reports limit their discussion to the resonance field and g-value, which are major imprints of the material characteristics.7,15,23 Other key spin resonance parameters that can provide a more detailed understanding of the properties of materials required to enhance the performance of the device have rarely been reported in the literature.7
In the present work, CoFe2O4 MNPs were synthesized by a wet chemical co-precipitation method and post-processing was carried out by annealing the as-prepared CoFe2O4 powder at different temperatures (300–900 °C). A detailed investigation of the microwave resonance behaviour was carried out by a ferromagnetic resonance (FMR) study and the spin resonance parameters were calculated by fitting the FMR spectra. The present study emphasizes the modification of the structural, morphological, static and dynamic magnetic properties of the single-phase cobalt nanoferrites by post-process annealing.
Fig. 2 Le Bail Rietveld refinement of CoFe2O4 nanoparticles annealed at (a) 300 °C, (b) 500 °C, (c) 700 °C, and (d) 900 °C. |
Sample | Crystallite size (nm) (Sherrer method) | Crystallite size (nm) (W–H method) | Strain | Average particle size (nm) | Lattice parameter (Å) | X-ray density (dx) g cm−2 | Specific surface area “S” (m2 g−1) |
---|---|---|---|---|---|---|---|
a | 8.4 | 5.9 | 0.0074 | 10.1 | 8.338 | 5.38 | 110.41 |
b | 10.6 | 9 | 0.0051 | 13.3 | 8.341 | 5.35 | 84.32 |
c | 17.9 | 14.2 | 0.0032 | 20.4 | 8.356 | 5.33 | 55.18 |
d | 39.5 | 39 | 0.0024 | 40.8 | 8.376 | 5.30 | 27.74 |
At higher annealing temperatures, the lattice parameter and crystallite size increased, and a similar trend has also been observed in another study after annealing.1 The growth of the crystallite size at higher annealing temperature could be because the solid–vapour surface of the crystal was replaced by a solid–solid interface via diffusion, which reduced the overall surface energy during the thermal annealing and caused the expansion of the crystallite volume.20,27 However, the strain, X-ray density and specific surface area were decreased with the increase in annealing temperature (Table 1), which could be related to the modification of the crystal structure and particle growth.11 The calculated crystallite sizes of the annealed samples from both methods (Debye–Scherrer and Williamson–Hall plot), suggested the systematic increase in the crystallite size with the increase in annealing temperature, which is similar to an earlier report.12 We calculated the specific surface area as per the following relation:
Specific surface area – S = 6/dx × D, where dx = X-ray density, D = crystalline size. |
Also, the X-ray density, ρ of the samples was calculated from the XRD patterns using the relation, ρ = 8M/NV, where M is the molecular weight, N is Avogadro's number, and V is the cell volume.7Fig. 1-(ii) shows the variation in the lattice parameter and crystallite size with the increase in the annealing temperature. The variation in the specific surface area and particle size with annealing temperature is shown in Fig. 1-(iii). It can be seen clearly in Fig. 2 that the peaks became sharper for the sample with elevated annealing temperature, reflecting the increased crystallite size.
The Le Bail refinement of all the powder samples was performed using the pseudo-Voigt profile function. The values of all the refinement parameters such as the “goodness of fit” χ2, the R factors (RP = profile factor, RB = Bragg factor, and RF = crystallographic factor), lattice constant parameters (a, b, c), and the cell volumes (V) for all the samples were calculated, and the structural parameters obtained from profile refinement are listed in Table 2.
Sample | χ2 | R B | R F | R WP | R exp | R P | V (Å3) | a = b = c (Å) |
---|---|---|---|---|---|---|---|---|
a | 1.08 | 0.189 | 0.124 | 46.5 | 44.72 | 48.4 | 577.748 (±0.392) | 8.328 |
b | 1.48 | 3.925 | 2.483 | 45.0 | 37.02 | 34.6 | 581.657 (±0.000) | 8.347 |
c | 1.79 | 5.660 | 3.696 | 52.0 | 38.87 | 40.0 | 585.413 (±0.193) | 8.365 |
d | 1.90 | 5.538 | 4.016 | 54.2 | 39.31 | 41.8 | 586.475 (±0.077) | 8.370 |
The refined spectrum of each sample displayed a single-phase cubic spinel structure of CoFe2O4 and the goodness of fit was in the range of 1.08–1.90. The refinement was carried out by assuming the Fdm symmetry (space group – 227). Further, the refinement was performed by fixing the octahedral sites (16d (1/8, 1/8, 1/8)), tetrahedral sites (8a (1/2, 1/2, 1/2)) and free oxygen (32e (x, x, x)) sites.7,11 The Rietveld refinement depicts that the Le Bail fit is optimum for extrinsic site transposal (γ′) equal 10% of the maxima. Moreover, the low γ′ value recommends the control of the size distribution of the CoFe2O4 nanoparticle samples with no or very little intrinsic variations. The lattice parameters calculated by the refinement and the position of oxygen atoms for each sample are plotted in Fig. 2(a–d). The complete process adopted for the Le Bail refinement has been described in detail in our previous work.7
Fig. 3 FTIR spectra of CoFe2O4 nanoparticles annealed at (a) 300 °C, (b) 500 °C, (c) 700 °C, and (d) 900 °C. |
In this study, we observed the low-frequency band v2 at around 412 cm−1 and the higher frequency band ν1 at around 554 cm−1. The characteristic bands at 1368 cm−1 and 1550 cm−1 are due to the O–H bending peak, similar to the values obtained by Rana et al.12 Also, the O–H stretching peak was observed at 3560 cm−1 as shown in Fig. 3. The reduction of the O–H diffraction peak with the increase in the annealing temperature is due to the loss of residual water molecules; we have observed that with the increase in the annealing temperature to 900 °C, the peaks for water molecules were also diminished, and similar behaviour was also reported in literature.12 As the annealing temperature increases, the intensities of the bands corresponding to O–H stretching vibrations decrease drastically, and this might be due to the loss of residual water molecules in all of the samples.12,16 These band positions were found to be in agreement with the characteristic infrared absorption bands of cobalt ferrite nanocrystals because CoFe2O4 is an inverse spinel in which Co2+ ions occupy the octahedral sites and Fe3+ ions occupy the tetrahedral sites. The absorption band ν1 is caused by the stretching vibrations of the tetrahedral metal (Fe3+)–oxygen bond, and the absorption band ν2 is caused by the octahedral metal (Fe3+/Co2+)–oxygen vibrations in octahedral sites.21
Fig. 4 TEM images of CoFe2O4 nanoparticles annealed at (a) 300 °C, (b) 500 °C, (c) 700 °C, (d) 900 °C. |
The size distribution was also measured by Small Angle X-ray Scattering (SAXS). Fig. 5 shows the plot between the distribution function and the particle size for all the samples. The size distributions of all the samples were obtained by fitting the energy plot of the SAXS, assuming log-normal distribution and mean diameter. Fig. 5 depicts that sample ‘a’ has a narrow particle size distribution between 5–10 nm, which increased for sample ‘b’ to 5–20 nm, for sample ‘c’ to 2–35 nm and for sample ‘d’ to 10–70 nm; these are complementary to the TEM results. Sample ‘a’ depicts the left-skewed plot, which suggests that the particles in the sample are not spherical but are elongated along the X-axis. The SAXS plot obtained for samples ‘b’, ‘c’ and ‘d’ showed no skewness, confirming that the particles are spherical in nature.25
Fig. 5 Small Angle X-ray Scattering (SAXS) shows the particle size distribution of CoFe2O4 nanoparticles annealed at (a) 300 °C, (b) 500 °C, (c) 700 °C, and (d) 900 °C. |
Fig. 6 Room temperature hysteresis loops of CoFe2O4 nanoparticles annealed at (a) 300 °C, (b) 500 °C, (c) 700 °C, and (d) 900 °C. |
Sample | M s (emu g−1) | H C (Oe) | M r (emu g−1) | M r/MS | Anisotropy constant (k) (erg cm−3) |
---|---|---|---|---|---|
a | 37.7 | 82.9 | 2.4 | 0.06 | 0.32 × 104 |
b | 45.5 | 233.4 | 6.2 | 0.13 | 1.08 × 104 |
c | 60.3 | 750.9 | 19.2 | 0.31 | 4.62 × 104 |
d | 71.4 | 459.6 | 19.3 | 0.27 | 3.35 × 104 |
The M–H loops revealed the transition from the single domain to the multi-domain nature with the increase in the annealing temperature from 700 to 900 °C, which led to an increase in the coercivity of sample ‘c’ and a decrease in the coercivity of sample ‘d’.21 The saturation magnetization (Ms) increased significantly from 37.7 emu g−1 to 71.4 emu g−1 (Table 3) with the increase in annealing temperature from 300 to 900 °C, showing the enhancement of ferromagnetism at a higher annealing temperature. The increase in the Ms value for larger particle size was found at a higher annealing temperature, showing the dependence of Ms on the particle size.12 However, the coercivity increased gradually for the samples annealed at temperatures from 300 to 700 °C and decreased on further increase in the annealing temperature to 900 °C. This trend of change in the coercivity indicates the presence of the single domain nature in samples ‘a’, ‘b’ and ‘c’, and the multi-domain nature in sample ‘d’. At 700 °C the particle exhibited the single domain nature with the maximum value of coercivity among all the annealed samples because of the coherent rotation of spins, which is consistent with the literature.17 The critical average particle size for the single domain was observed around 20 nm (sample c). The increase in coercivity from sample ‘a’ to sample ‘c’ (Table 3) could be attributed to the increase in the magnetic anisotropy for sample ‘c’.21,22 The magnetic anisotropy and coercivity decreased on increasing the annealing temperature to 900 °C, due to the formation of the multi-domain region within the particles of sample ‘d’.1,28 The variation in the saturation magnetization and coercivity with particle size could also be explained on the basis of the magnetic domain structure, super-exchange interaction, particle diameter, magneto-crystalline anisotropy and shape anisotropy.20
Combining all the magnetic properties of the annealed CoFe2O4 nanoparticles, we can conclude that the saturation magnetization (Ms) value of the annealed samples increased up to 71.4 emu g−1 on increasing the annealing temperature up to 900 °C, which is significantly lower than the bulk CoFe2O4 value of 90 emu g−1.12 Our results for Ms are better at the nano-level and are higher than reported by Sajjia et al. (62 emu g−1).13 The lower value of Ms for nanoparticles could be attributed to the finite size effect. The finite-size effect shows a non-collinearity (spin canting) in the spinel structure (tetrahedral, A site, SA and octahedral, B site SB) that results in a decrease in the net magnetic moment.7,27,29 This is in accordance with the two-sublattice Néel model, defined as the difference between the moments of the A sublattice and B sublattice. The increase in the particle size favoured the increase in the collinearity of spins (SA and SB) in the ferrimagnetic structure, which enhanced the saturation magnetization at higher annealing temperatures. The squareness ratio (R = Mr/Ms) was between 0.06–0.27, which decreased with an increase in the annealing temperature due to the decrease in the energy loss per unit cycle and its value was less than 0.5, so there was a uniaxial anisotropy according to the Stoner Wohlfarth model.7,12 Also, for nano-sized ferrite particles, the surface area is larger and thus the surface energy and surface tension are higher as compared to the bulk.
Generally, in the collinear ferromagnetic (FiM) structure, the value of the magnetic moment per formula unit is calculated by considering the collinear two-sublattice Néel model of ferrimagnetism. In the present investigation, the calculated moment for each of the samples from the theory does not match the experimental values obtained from VSM. This discrepancy may be due to the spin canting at the B site; thus, we considered the three-sublattice Yafet–Kittel model to calculate the spin canting (basically a lack of full alignment of spins), which was already discussed in detail in our recent publication.7 The canting angle ϕ was calculated using the following assumption: M = MBcosϕ − MA. The calculated values of the canting angles were 39.81, 32.44, 33.63 and 33.29 for the samples a, b, c and d respectively.
The schematic representation of the annealing effects on the domain structure of the CoFe2O4 nanostructure is shown in Fig. 7. The schematic indicates that the increase in the particle size from 5–100 nm has two different domain wall structures. The annealed nanoparticles (300–700 °C) were ferromagnetic with a single-domain nature, which converted to multi-domain particles upon annealing at 900 °C.
Fig. 8 Room temperature ferromagnetic resonance spectra (FMR) of CoFe2O4 nanoparticles annealed at (a) 300 °C, (b) 500 °C, (c) 700 °C, and (d) 900 °C. |
Sample Name | H r (G) | ΔHpp (G) | ΔH1/2 (G) | g-value | N S (spin per g) |
---|---|---|---|---|---|
a | 1057.72 | 3229.69 | 5593.98 | 1.8 | 7.6471 × 1022 |
b | 721.54 | 2256.25 | 3907.93 | 2.0 | 4.8080 × 1022 |
c | 1902.37 | 2995.08 | 5198.63 | 1.4 | 9.1177 × 1022 |
d | 1925.08 | 3041.98 | 5268.86 | 1.2 | 10.8039 × 1022 |
The values of the spin resonance parameters are shown in Table 4. The spin concentration (NS), as well as the peak to peak line width (ΔHPP), significantly depends on the annealing temperature. The dipole–dipole interactions and linewidth increased at higher annealing temperatures, resulting in higher NS.30 The presence of the Co2+ ions in CoFe2O4 caused the high magneto-crystalline anisotropy of the material and broadened the FMR spectra.10 Generally, NS is calculated by the comparison method with a standard DPPH, in which the area under the curve of DPPH (contains 1.52718 × 1018 spins per g) is compared with the area under the curve of the samples, provided all the conditions such as modulation amplitude, time constant and gain are the same. However, this method is not very reliable, so we calculated NS by statistical theory, which predicts that when the line shape is Lorentzian or between Lorentzian and Gaussian. The spin concentration can be calculated by the following equation:7,31
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