Effects of Al3+ Substitution on Structural and Magnetic Behavior of CoFe₂O₄ Ferrite Nanomaterials.

A sol-gel autocombustion method was used to synthesize Al3+ ion-substituted cobalt ferrite CoAlxFe2-xO₄ (x = 0⁻1.5). According to X-ray diffraction analysis (XRD), cobalt ferrite was in a single cubic phase after being calcined at 1000 °C for 3 h. Moreover, the lattice constant decreased with increase in aluminum substituents. When the sample was analyzed by Scanning Electron Microscopy (SEM), we found that uniformly sized, well-crystallized grains were distributed in the sample. Furthermore, we confirmed that Al3+ ion-substituted cobalt ferrite underwent a transition from ferrimagnetic to superparamagnetic behavior; the superparamagnetic behavior was completely correlated with the increase in Al3+ ion concentration at room temperature. All these findings were observed in Mössbauer spectra. For the cobalt ferrite CoAlxFe2-xO₄, the coercivity and saturation magnetization decrease with an increase in aluminum content. When the annealing temperature of CoAl0.1Fe1.9O₄ was steadily increased, the coercivity and saturation magnetization initially increased and then decreased.

1. Introduction

Ferrite is an important magnetic material. Cobalt ferrite is a hard ferromagnetic material, and its characteristic properties are as follows: moderate saturation magnetization (80 emu/g), high coercivity (5000 Oe), high Curie temperature TC (520 °C), large anisotropy constant (2.65 × 105–5.1 × 105 J/m3) [1,2]. Cobalt ferrite has the following properties: high electromagnetic performance, large magneto-optic effect, excellent chemical stability, and excellent mechanical hardness [1,2,3]. Because cobalt ferrite is a hard ferromagnetic material, it is used as a high-density recording medium [4]. Cobalt ferrite substituted nonmagnetic Al3+ ions; such material has low magnetic coercivity and large resistivity. Soft ferrite is the core material in power transformers that are used in the field of electronics and telecommunication. Singhal et al. [5] used the aerosol route for substituting Fe3+ ions in cobalt ferrite with Al3+ ions. The magnetic hyperfine field decreases; the ratio of Fe3+(oct.)/Fe3+(tet.) ions increases with an increase in Al3+ ions. Chae et al. [6] synthesized AlCoFe2−O4 ferrite powders, and they determined magnetic properties of the sample. In AlCoFe2−O4 ferrite powders, saturation magnetization and coercive force decrease with increasing concentration of Al. In a study conducted by Kumar et al. [7], it was found that crystallite size of cobalt ferrite increased when they were doped with Al3+ ions. Consequently, saturation magnetization, coercive force, remnant magnetization, and magnetic anisotropy constant decreased in these doped structures. Raghavender et al. [8] investigated the dielectric properties of cobalt ferrite by doping with Al3+ ions. These ferrite materials exhibit low dielectric character, so they are extensively used in high-frequency applications. In this study, ferrite CoAlFe2−O4 (x = 0–1.5) materials were synthesized with a sol-gel autocombustion process. The aim of this study was to determine the variation in the magnetic performance of cobalt ferrite powders, which were partially doped with nonmagnetic aluminum cations.

2. Experimentation

2.1. Sample Preparation

Cobalt ferrite powders CoAlFe2−O4 (x = 0–1.5) were synthesized with a sol-gel autocombustion process. The raw materials of the sample were of analytical grade: Co(NO3)2·6H2O, Al(NO3)3·9H2O, Fe(NO3)3·9H2O, C6H8O7·H2O (citric acid), and NH3·H2O (ammonia). The molar of metal nitrates Al(NO3)3·9H2O was 0–0.15 mol. The molar ratio of metal nitrates to citric acid was maintained at 1:1. After weighing metal nitrates and citric acid, they were dissolved in deionized water to prepare solutions. Ammonia was added to increase the pH of the metal nitrate solution from 7 to 9. A dried gel was obtained by stirring the metal nitrate mixture in a thermostat water bath at 80 °C. Citric acid was added continuously to the dried gel. The resultant gel was dried in an oven at 120 for 2 h. The resultant powder was then burnt by igniting it in air. The dried powders were ground and sintered at specific temperatures.

2.2. Characterization

The structure and crystallite sizes of CoAlFe2−O4 (x = 0–1.5) were determined by X-ray diffraction (D/max-2500V/PC, Rigaku Corporation, Tokyo, Japan) in the 2θ range of 20–70°. Micrographs were observed by scanning electron microscopy (NoVaTM Nano SEM 430, FEI Corporation, Hillsboro, OR, USA). Saturation magnetization was determined by Quantum Design MPMS series XL-7 (Quantum Design Corporation, San Diego, CA, USA). To obtain the Mössbauer spectrum, a Mössbauer spectroscope was operated in constant acceleration mode with a 57Co source (Fast Tec PC-mossII, FAST Corporation, Oberhaching, Bavaria, Germany).

3. Results and Discussion

3.1. X-ray Diffraction Analysis (XRD)

Figure 1 illustrates XRD patterns for CoAlFe2−O4 (x = 0–1.5) ferrites, which were calcined at 1000 °C. The XRD spectrum shows that all the samples have a single-phase structure. An impurity peak was not observed in these samples. Table 1 and Figure 2 prove that the lattice constant can be decreased by increasing the concentration of Al3+ ions. The decrease in lattice parameter is probably attributed to the radius of Al3+ ions (0.50 Å), which is smaller than Fe3+ ions (0.64 Å) [5,6]. X-ray density was determined from the following equation [5,8]: where a is the lattice constant; M is the relative molecular weight; and N is the Avogadro number. Table 1 and Figure 2 show that density decreases with an increase in Al3+ ion content. Because the atomic weight of Fe is greater than that of Al, the relative density constant decreases with increasing Al3+ ion substitution. X-ray density decreases under the following condition: the relative decrease in molecular mass is greater than the negligible decline in the lattice parameter. The average crystallite size decreases with an increase in the concentration of Al3+ ions. This phenomenon has been attributed to the size mismatch of Al3+ and Fe3+ ions, increasing strain and stress in the sample [7].

Figure 1

X-ray diffraction (XRD) patterns of CoAlFe2−O4 calcined at 1000 °C.

Table 1

The XRD data of CoAlFe2−O4 calcined at 1000 °C.

Content (x)	Lattice Parameter (Å)	Average Crystallite Size (Å)	Density (g/cm3)
0	8.38615	520	5.2847
0.1	8.37572	688	5.2392
0.2	8.35311	504	5.2161
0.3	8.36258	642	5.1328
0.4	8.33272	582	5.1216
0.5	8.33749	537	5.0470
0.6	8.33045	420	4.9959
0.7	8.32861	410	4.9583
0.8	8.32516	365	4.8666
0.9	8.27064	280	4.8992
1.0	8.25813	266	4.8534
1.5	8.16640	241	4.6668

Figure 2

The change in the lattice parameter and X-ray densities of CoAlFe2−O4.

As shown in Figure 3, X-ray patterns (XRD) of CoAl0.1Fe1.9O4 were sintered at different temperatures. An average CoAl0.1Fe1.9O4 crystallite size increase by increasing the calcining temperature is observed in Table 2. All the samples were single-phase structures of spinel ferrite, which indicates the absence of an additional phase. No significant changes were observed in the lattice parameter of all samples. The average crystallite size of CoAl0.1Fe1.9O4 increased with an increase in calcination temperature [5].

Figure 3

XRD patterns of ferrite CoAl0.1Fe1.9O4 calcined at different temperatures.

Table 2

XRD data of ferrite CoAl0.1Fe1.9O4 calcined at different temperatures.

Temperature (℃)	Lattice Parameter (Å)	Average Crystallite Size (Å)	Density (g/cm3)
unsintered	8.37425	337	5.2378
600	8.36801	346	5.2537
1000	8.37572	688	5.2392

3.2. Scanning Electron Microscopy (SEM)

Figure 4 shows SEM micrographs of CoAlFe2−O4 (x = 0, 0.1) samples, which were annealed at 1000 °C for 3 h. Uniformly-sized, well-crystallized grains of CoAlFe2−O4 were obtained. Figure 5 illustrates the grain-size distribution of CoAlFe2−O4 (x = 0, 0.1) ferrites. The average grain size of CoFe2O4 and CoAl0.1Fe1.9O4 was about 137.5 nm and 130.5 nm, respectively. The average grain size decreased when aluminum substituents were increased. The XRD pattern confirms that the average crystallite size tends to decrease with increasing Al content. The average grain size was greater than a nanoparticle (100 nm), and the sintering temperature of the sample was very high because grain size increased with increasing annealing temperature [9].

Figure 4

Scanning electron microscopy (SEM) micrographs of CoFe2O4 (x = 0) and CoAl0.1Fe1.9O4 (x = 0.1) calcined at 1000 °C.

Figure 5

Histogram of grain-size distribution for CoFe2O4 (x = 0) and CoAl0.1Fe1.9O4 (x = 0.1), which were calcined at 1000 °C.

3.3. Mössbauer Spectroscopy

Figure 6 shows the Mösbauer spectra of CoAlFe2−O4 acquired at room temperature. The hyperfine parameters, isomer shift (I.S.), magnetic hyperfine field (Hhf), quadrupole shift (Q.S.), relative area (A0), and line width (Г), were obtained by fitted spectra using Mösswinn 3.0 software (FAST Corporation, Oberhaching, Germany), and calibration was relative to a 25 μm thick sample of high-purity alpha iron. The characteristic features of the spectra were as follows: there were two Zeeman-splitting sextets; one sextet was assigned to Fe3+ ion at the tetrahedral site, while the other sextet was attributed to Fe3+ ions at the octahedral site. This proved the ferromagnetism of the samples. The first sextet had a larger value of isomer shift, and it was assigned to octahedral B site. The second sextet had a smaller value of isomer shift, and was assigned to tetrahedral A site. Compared to the tetrahedral A-site ions, the bond separation of Fe3+ ions was greater in the octahedral B site of the Fe3+-O2− complex (Table 3). This minimized the overlapping of orbits of Fe3+ ions at the octahedral B-site; the larger isomeric shift was attributed to smaller covalency at octahedral B site [6].

Figure 6

Mössbauer spectra of CoAlFe2−O4 samples calcined at 1000 °C.

Table 3

Mössbauer parameters of CoAlFe2−O4 samples, which were calcined at 1000 °C.

Content (x)	Component	Isomer Shift (I.S.) (mm/s)	Quadrupole Shift (Q.S.) (mm/s)	H(T)	Line Width (Γ) (mm/s)	Relative Area (A0) (%)
0	Sextet (A)	0.238	−0.011	48.852	0.366	28.4
	Sextet (B)	0.355	0.0004	45.889	0.338	71.6
0.1	Sextet (A)	0.245	−0.002	48.387	0.376	29.88
	Sextet (B)	0.332	−0.017	45.563	0.348	70.2
0.2	Sextet (A)	0.236	0.019	47.733	0.417	22.9
	Sextet (B)	0.334	0.001	45.360	0.348	77.1
0.3	Sextet (A)	0.236	−0.030	47.293	0.381	15.8
	Sextet (B)	0.311	−0.002	44.824	0.348	84.2
0.4	Sextet (A)	0.236	0.015	46.594	0.526	22.5
	Sextet (B)	0.307	−0.006	43.361	0.358	77.5
0.5	Sextet (A)	0.224	0.102	45.589	0.329	7.5
	Sextet (B)	0.305	−0.003	42.156	0.374	92.5
0.6	Sextet (B)	0.273	−0.048	40.664	0.424	100
0.7	Sextet (B)	0.297	−0.003	34.682	0.402	100
0.8	Sextet (B)	0.301	0.008	37.958	0.394	100
0.9	Sextet (B)	0.320	−0.003	35.164	0.341	87.6
	Double	0.302	0.670	-	0.466	12.4
1.0	Sextet (B)	0.306	−0.045	31.352	0.283	82.6
	Double	0.321	0.726	-	0.406	17.4
1.5	Double	0.318	0.752	-	0.389	100

It is well known that the values of isomeric shift are in the range of 0.6–1.7 mm/s for Fe2+(S = 2) ions; the values of isomeric shift are in the range of 0.1–0.5 mm/s for Fe3+(S = 1/2, 3/2, 5/2) ions [10]. As shown in Table 3, the values of I.S. indicate that iron is in Fe3+ state. By increasing the aluminum content, the values of the magnetic hyperfine field decreased at tetrahedral A and octahedral B sites. This is because magnetic ions (Fe3+ ions) are substituted by nonmagnetic ions (Al3+ ions), affecting the supertransferred hyperfine fields [5]. For all samples, the quadrupole shift value was very small for the magnetic sextet at the A and B site. This indicates that spinel ferrites have local cubic symmetry. The spectra of CoAlFe2−O4 (0.6 ≤ x ≤ 0.8) included the magnetic sextet of B site; the magnetic sextet of A site vanished. This indicates that Fe3+ ions existed only in the octahedral B site. When the spectrum of CoAlFe2−O4 (composition with x = 0.9 and 1.0) was analyzed, a single sextet and a central paramagnetic doublet were observed; this indicates relaxation effects. When the nonmagnetic Al content was increased in CoAlFe2−O4, the samples changed into a superparamagnetic character. The behavior of the sample went from a completely magnetic state to a mixed state of magnetic and superparamagnetic order [11,12]. For samples with x = 1.5, Mössbauer spectra consisted only of a central doublet; this exhibits a superparamagnetic character. The central doublet was attributed to the nearest nonmagnetic neighbors of magnetically isolated Fe3+ ions. This leads to the deficiency of long-range magnetic ordering [13,14].

The cation distribution of CoAlFe2−O4 ferrite can be written as follows:(Co

Based on the above cation distribution, the absorption-area ratio of A sites to B sites can be written as follows [12]: where f and f are the recoil-free fractions of Fe3+ ions in tetrahedral A sites and octahedral B sites, respectively. The Mössbauer absorption area is proportional to the distribution of iron ions of A sites and B sites. In the current study, we assumed that f and f are equal [12]. Table 4 shows the cation distribution of all samples, and it was calculated using Equation (3).

Table 4

The cationic distribution of all samples, which were calcined at 1000 °C.

Sample	Cation Distribution
CoFe2O4	(Co0.43Fe0.57)A[Co0.57Fe1.43]BO4
CoAl0.1Fe1.9O4	(Co0.43Fe0.57)A[Co0.57Fe1.33Al0.1]BO4
CoAl0.2Fe1.8O4	(Co0.43Fe0.41Al0.16)A[Co0.57Fe1.39Al0.04]BO4
CoAl0.3Fe1.7O4	(Co0.43Fe0.27Al0.3)A[Co0.57Fe1.43]BO4
CoAl0.4Fe1.6O4	(Co0.43Fe0.36Al0.21)A[Co0.57Fe1.27Al0.19]BO4
CoAl0.5Fe1.5O4	(Co0.43Fe0.11Al0.46)A[Co0.57Fe1.39Al0.04]BO4
CoAl0.6Fe1.4O4	(Co0.43Al0.57)A[Co0.57Fe1.40Al0.03]BO4
CoAl0.7Fe1.3O4	(Co0.43Al0.57)A[Co0.57Fe1.30Al0.13]BO4
CoAl0.8Fe1.2O4	(Co0.43Al0.57)A[Co0.57Fe1.20Al0.23]BO4
CoAl0.9Fe1.1O4	(Co0.43Al0.57)A[Co0.57Fe1.10Al0.33]BO4
CoAl1.0Fe1.0O4	(Co0.43Al0.57)A[Co0.57Fe1.00Al0.43]BO4
CoAl1.5Fe0.5O4	(Co0.43Al0.57)A[Co0.57Fe0.50Al0.93]BO4

3.4. Magnetic Analysis

Figure 7 illustrates the hysteresis loops of CoAlFe2−O4 samples at room temperature. For all the samples, magnetization reached saturation when the strength of the magnetic field was 10,000 Oe. Table 5 shows that saturation magnetization decreased with an increase in Al3+ ion content. The saturation magnetization can be expressed with the following equation [12]: where n is the magnetic moment and M is the relative molecular mass. The relative molecular mass of CoAlFe2−O4 decreased with an increase in Al content. The change in magnetic moment n was determined by Néel’s theory of magnetism. The magnetic moment of Al3+, Co2+, and Fe3+ ions was 0 μB, 3 μB, and 5 μB [15,16,17], respectively. Néel’s theory of magnetism was used to develop two sublattice models, which were then used to explain cation distribution in the Mössbauer spectra (Table 4). Magnetic moment n is expressed by Equation (5) [15,16]: where M and M are magnetic moments of the B and A sublattices, respectively. Figure 8 illustrates the changes in experimental and calculated magnetic moments, with changes in Al3+ ion content.

Figure 7

The hysteresis loops of CoAlFe2−O4 samples calcined at 1000 °C.

Table 5

Magnetic parameters of CoAlFe2−O4 calcinated at 1000 °C obtained from hysteresis measurements.

Content (x)	Ms (emu/g)	Hc (Oe)	Mr (emu/g)	nB
0	80.89	802.77	37.15	3.40
0.1	75.66	802.76	37.75	3.14
0.5	47.43	301.11	22.54	1.87
1.0	16.13	150.56	5.45	0.59
1.5	1.06	150.38	0.10	0.04

Figure 8

Variation in the experimental magnetic moment and calculated magnetic moment with changes in aluminum concentration.

Figure 8 illustrates that the experimental and calculated magnetic moment decreases with an increase in Al content (x ≤ 0.1). According to Equation (4), calculated saturation magnetization decreased with an increase in Al3+ ion substitution. The change trend of experimental and calculated saturation magnetization was similar for x ≤ 0.1, and there was deviation between experimental and calculated saturation magnetization, which can be attributed to the actual situation of ion distribution being more complicated than that obtained from the Mössbauer spectra. For the substituents (x ≥ 0.5), there was a big difference between calculated saturation magnetization and experimental saturation magnetization, and the experimental value was smaller than the calculated value for saturation magnetization [18,19,20]. This can be explained by the three-sublattice model of Yafet-Kittel (YK) [16]. It is reasonable that the spin-canting arrangement of the magnetic moment appeared on B sites of the sample when the content of nonmagnetic Al3+ ion substituents was too high in cobalt ferrite samples. This led to a decrease in A–B interaction and an increase in B–B interaction, which subsequently decreased magnetization.

Table 5 shows that the coercivity of CoAlFe2−O4 decreased with an increase in Al3+ ion content (x). Based on the results of the Mössbauer spectroscopy, we inferred that Co2+ ions of CoFe2O4 samples were located at the tetrahedral A sites and octahedral B sites. The magnetocrystalline anisotropy is primarily attributed to Co2+ ions of octahedral sites, which are present in pure cobalt ferrite CoFe2O4 [7]. The electron configuration of Co2+ ions is 3d7 [21]. The anisotropy is attributed to Co2+ ions in the octahedral site, causing frozen orbital angular momentum and spin coupling [22]. The Al3+ ions elicit zero angular momentum (l = 0), which does not affect magnetic anisotropy [23,24,25]. When Al3+ ions were replaced with Fe3+ ions, the spin-orbit coupling weakened and magnetocrystalline anisotropy decreased.

Equation (6) describes the relationship between the following parameters: coercivity H, magnetic anisotropy K1, and saturation magnetization M [7]:

When magnetic anisotropy decreased with an increase in Al3+ ions, it led to a decrease in coercivity.

Figure 9 shows the magnetic hysteresis curves of an unsintered CoAl0.1Fe1.9O4 sample at room temperature; magnetic hysteresis curves of CoAl0.1Fe1.9O4 sample were also obtained after sintering them at 600 °C and 1000 °C, respectively. Table 6 shows that the saturation magnetization of CoAl0.1Fe1.9O4 sample increased with an increase in sintering temperature; these changes were attributed to an increase in particle size [5]. There is no significant change in the saturation magnetization of the unsintered CoAl0.1Fe1.9O4 sample; moreover, the CoAl0.1Fe1.9O4 sample did not show any significant change even after being annealed at 600 °C. This confirms that the uncalcined sample has good crystallinity, which was further established by XRD.

Figure 9

Room-temperature hysteresis curves of CoAl0.1Fe1.9O4 samples calcined at different temperatures.

Table 6

Magnetic data for CoAl0.1Fe1.9O4 sample calcined at different temperatures.

Temperature (°C)	Ms (emu/g)	Hc (Oe)	Mr (emu/g)	nB
unsintered	65.52	902.92	32.77	2.72
600	63.78	1605.13	33.53	2.65
1000	75.66	802.76	37.75	3.14

With a steadily increasing sintering temperature, the coercivity of CoAl0.1Fe1.9O4 sample initially increased and then steadily decreased. This may be attributed to variation in grain size. The coercivity of the single-domain region is given by the following equation: HC = g–h/D2. In the multidomain region, the relationship between coercivity and grain size is established by the following equation: HC = (a + b)/(D). Here, ‘D’ is the diameter and ‘g, h, a, and b’ are constants of the particle [5,26]. Hence, coercivity increased with increasing grain size in the single-domain region. In the multidomain region, coercivity decreased with an increase in particle diameter [27,28]. In our study, we determined the grain size of CoAl0.1Fe1.9O4 samples that were calcined at different temperatures; the grain size of CoAl0.1Fe1.9O4 samples varied from the single-domain region to the multidomain region. With an increasing annealing temperature, the coercivity of CoAl0.1Fe1.9O4 sample increased initially and then decreased.

4. Conclusions

XRD analysis reveals the single-phase structure of CoAlFe2−O4 samples that were calcined at 1000 °C. The lattice constant decreased when smaller Al3+ ions were replaced with larger Fe3+ ions. The XRD spectra of CoAl0.1Fe1.9O4 samples were obtained after sintering them at different temperatures; these samples were prepared with a sol-gel autocombustion method, so they had good crystallinity. SEM results indicate that well-crystallized particles of uniform size were present in the sample. We obtained the Mössbauer spectra of CoAlFe2−O4 samples, which were calcined at 1000 °C. The Mössbauer spectra reveal that with an increase in aluminum concentration, CoAlFe2−O4 samples undergo a transition from ferrimagnetic behavior to superparamagnetic behavior. Cation distribution was estimated from the Mössbauer data. The coercivity and saturation magnetization of CoAlFe2−O4 samples decreased with an increase in Al content (x). The changes in saturation magnetization can be attributed to Néel’s theory and the Yafet-Kittel model. Coercivity decreased with an increase in aluminum content, which is attributed to the weakening of magnetocrystalline anisotropy. The coercivity and saturation magnetization of CoAl0.1Fe1.9O4 sample initially increased and then steadily decreased. Particle size increased with an increase in annealed temperature.