1 Introduction

In recent years, among the family of spinel ferrites, cobalt ferrite has been rigorously investigated due to its tremendous applications in high-density magnetic recording media, microwave devices, high-sensitivity sensor and biomedical industries [1,2,3,4]. Apart from the promising electronic applications, they are also suitable and widely used in environmental remediation applications due to their excellent physical and chemical properties like high saturation magnetization, low cost, size- and shape-dependent and catalytic properties [5, 6].

The structural, electrical, magnetic and dielectric properties of cobalt ferrite are governed by the factors like method of preparation, sintering time and temperature, chemical composition, type and concentration of dopant. The spinel unit cell consists of cubic closed-pack arrangement of oxygen ions with 64 tetrahedral (A) and 32 octahedral interstitial sites (B). Out of these 96 interstitial sites, only 8 and 16 cations are occupied in A and B sites, respectively, which are aligned in a mutually opposite direction. Thus, there is a great probability to tune the properties of the cobalt ferrite by rearranging the cations present in A and B sites. This is because magnetic and electrical properties are predominantly depending on cationic and charge distribution. Introducing a fraction of magnetic or non-magnetic ions with different valency states in the spinel ferrite affects significantly its structure, which further plays a crucial role in tuning its physical properties for various industrial applications. The rare-earth ions have unpaired 4f electrons, and they have a strong spin–orbit coupling. The substitution of rare-earth ions with Fe3+ site will cause 4f–3d coupling which is helpful to determine magneto-crystalline anisotropy of the material; therefore, it is possible to develop a magnetic core useful for low- and high-frequency applications. Several authors reported that substitution of rare-earth ions enhances the electromagnetic characteristics of the cobalt ferrite. Nikumbh et al. [7] reported decrease in magnetic parameters due to the substitution of Nd3+, Sm3+ and Gd3+ in cobalt ferrite. On the other hand, Tahmineh et al. [8] and Dascalu et al. [9] observed that Tb3+ could enhance the saturation magnetization of cobalt ferrite and make it a suitable candidate for recording head applications. Thus, the objective of the present study is to investigate the influence of Nd3+ doping on structural, electrical and magnetic properties of cobalt ferrite system. Moreover, due to the larger ionic radii of Nd3+, it requires higher energy to enter into the spinel lattice. Therefore, standard ceramic route has been chosen in the present work and it is expected that they must occupy the larger B sites, which produce an unusual magnetic behavior upon Nd3+ substitution.

2 Experimental

Neodymium (Nd3+)-substituted cobalt ferrite with chemical composition CoNdxFe2−xO4 (x = 0, 0.010, 0.015, 0.020, 0.025, 0.030) was synthesized by standard ceramic method. High-purity analytical-grade (analytical reagent (AR)) precursors of CoO (99.9%), Fe2O3 (99.9%) and NdO(99.9%) were used as starting materials in desired stoichiometric proportions. The starting precursors were weighed and mixed thoroughly in agate motor and calcined at 1173 K for 4 h. These powders were compacted in the form of pellets by adding 5% polyvinyl alcohol (PVA) as a binder. Finally, the powder materials and pellets were sintered again at 1473 K for 4 h followed by natural cooling to room temperature. The sintered samples are subjected to various characterization techniques to understand the modifications in structural, electrical and magnetic properties as a function of Nd3+ concentration.

Cobalt ferrite powders were analyzed to identify the phase formation by using Panalytical X’Pert Pro MPD X-ray diffractometer (XRD) with Cu Kα radiation (λ = 0.154056 nm) in the range of 10°–80°. The infrared spectra were recorded in the range of 4000–400 cm−1 with Shimadzu Fourier transform infrared spectroscopy (FTIR) Prestige-21. Microstructural changes were studied using LEO 435 VP scanning electron microscope (SEM). Prior to scanning, surfaces of the pellets were coated with a thin layer of platinum. The magnetization measurement was carried out by LAKESHORE VSM-7410 vibrating sample magnetometer (VSM) with maximum applied field of 2 T at room temperature. The room-temperature direct-current (DC) electrical resistivity measurements were done on the disk-shaped pellets using standard two-probe method at a small electric field of 1 V·cm−1 for all samples.

3 Results and discussion

3.1 XRD results

XRD patterns of CoNdxFe2−xO4 (x = 0, 0.010, 0.015, 0.020, 0.025, 0.030) samples are shown in Fig. 1. It is clear from that all the samples exhibit cubic spinel phase, and prominent peaks corresponding to (220), (311), (222), (400), (422), (511) and (440) planes are in accordance with standard JCPDS card No. 22-1086. The lattice constant a was calculated according to the following equation:

$$a_{\exp } = d\sqrt {h^{2} + k^{2} + l^{2} }$$
(1)

where d is the inter-planar distance of each plane and (hkl) are Miller indices. Nelson–Riley extrapolation method was used to find the accurate lattice constant, as listed in Table 1 [10]. It is clear from Table 1 that lattice constant increases linearly with Nd3+ and then decreases when x > 0.02. The observed increase is due to the replacement of Fe3+ (0.065 nm) at B site by larger ionic radii Nd3+ (0.0995 nm). Similar variation in lattice constant with Nd3+ substitution in different ferrite systems has been reported in studies [11, 12]. However, the decrease in lattice constant for the composition x ≥ 0.020 is ascribed to the possible diffusion of Nd3+ to the grain boundaries instead of entering into the lattice site. Therefore, the percolation limit of Nd3+ concentration to accommodate into the octahedral spinel lattice is 0.02 mol %. Hameda et al. [13] and Farid et al. [14] observed similar variation in lattice constant in their investigation with Nd3+ substitution. The average crystallite size for all the samples was calculated using the following Debye–Scherer’s equation, as listed in Table 1:

$$D_{311} = \frac{0.9\lambda }{\beta \cos \theta }$$
(2)

where D311, λ, β and θ are volume-averaged crystallite size, wavelength of X-ray (0.15406 nm), full width at half maximum of (311) peak and diffraction angle, respectively. The average crystallite size varies randomly with Nd3+ content increasing between 46 and 49 nm. The calculated X-ray density (dx) of all the samples was calculated by the following formula:

$$d_{x} = \frac{{ZM_{\text w} }}{{N_{\text A} V_{\text C} }}$$
(3)

where Z is the number of formula units in a unit cell, Mw is the molecular weight of the sample, NA is the Avogadro’s number and VC is volume of the cell. From Table 1, a linear dependence of X-ray density on Nd3+ concentration is observed. This variation in density is a direct consequence of higher molecular weight of Nd3+ than Fe3+ concentration. It is worthwhile to mention the influence of large ionic radii on hoping lengths of spinel lattice. The following equations were used to calculate the tetrahedral hopping length (LA) and octahedral hopping length (LB):

$$L_{\text{A}} = \frac{1}{4}a\sqrt 3 \;{\text{and}}\;L_{\text{B}} = \frac{1}{4}a\sqrt 2$$
(4)

Figure 2 shows the composition dependence of hoping lengths at A and B sites. It can be observed that hopping lengths follow the similar trend with that of lattice constant, suggesting the increase in the distance between the ions in the respective sublattice. The separation between the ions due to the substitution of larger Nd3+ modifies the magnetic and electrical properties.

Fig. 1
figure 1

XRD patterns of CoNdxFe2−xO4 (x = 0, 0.010, 0.015, 0.020, 0.025, 0.030) samples

Table 1 Average crystallite size, X-ray density, FTIR frequency band positions (ν1 and ν2) and grain size of CoNdxFe2−xO4 (x = 0, 0.010, 0.015, 0.020, 0.025, 0.030) samples
Fig. 2
figure 2

Hopping lengths (L) of CoNdxFe2−xO4 (x = 0, 0.010, 0.015, 0.020, 0.025, 0.030) samples

3.2 FTIR and microstructure study

Infrared spectra of Nd3+-substituted cobalt ferrite are shown in Fig. 3. Two prominent absorption bands in the range of 350–400 and 550–600 cm−1 are noticed. The high-frequency absorption band ν1 corresponds to the stretching vibration of the octahedral metal oxygen bond, and low-frequency band ν2 is due to the metal oxygen vibrations at tetrahedral sites. The positions of the bands are listed in Table 1. Both tetrahedral and octahedral band positions are shifted to higher frequency side. The shift in band positions is due to the variation in Fe3+ ↔ O2− bond length and cation redistribution. In the present work, occupation of Nd3+ in octahedral B site with larger ionic radii is responsible for the observed shift in absorption bands. It is also observed from Fig. 3 that broadening of ν2 band increases with Nd3+ concentration increasing, which suggests the occupancy of Nd3+ on octahedral B sites [15].

Fig. 3
figure 3

FTIR spectra of CoNdxFe2−xO4 (x = 0, 0.010, 0.015, 0.020, 0.025, 0.030) samples

The typical SEM images of CoNdxFe2−xO4 (x = 0, 0.010, 0.015, 0.020, 0.025, 0.030) are presented in Fig. 4. It is well known that grain size and structure influence the physical properties of ferrites. Grain growth is closely related to the grain boundary mobility, because there is a competition between the driving force for grain boundary movement and the retarding force exerted by the pores during the grain growth [16]. The grain size is calculated using linear intercept method and presented in Table 1. It is to be noted that the addition of Nd3+ significantly impedes the grain growth. The observed variations in grain size and formation of secondary phase are consistent with reported results in the literature by various authors, but in different ferrite systems [17, 18].

Fig. 4
figure 4

SEM images of CoNdxFe2−xO4: a x = 0, b x = 0.010, c x = 0.015, d x = 0.020, e x = 0.025 and f x = 0.030

3.3 Electrical resistivity

The electrical properties of spinel ferrite are strongly influenced by the microstructure, availability of cations (Fe3+ and Fe2+) and their distribution among A and B sites, which in turn depend on the synthesis processes and conditions. It can be seen from Fig. 5 that room-temperature (303 K) DC electrical resistivity increases with Nd3+ content increasing. It is known that conduction in spinals is due to the charge transfer of electrons between cations on B sites of different valences, because A–A hopping does not exist as there are only Fe3+ on this sublattice and any Fe2+ formed during processing preferentially occupy the B sites, and B–B hopping is more dominant than A–B hopping [19]. In the present work, substitution of Nd3+ at the expense of Fe3+ reduces the availability of ferric ions at B site. This in turn enhances the resistivity of the ferrite. However, hopping takes place among Fe2+ and Fe3+ due to the presence of secondary phase at grain boundaries. This may be responsible for the slight increment in the resistivity.

Fig. 5
figure 5

Room-temperature DC electrical resistivity of CoNdxFe2−xO4 (x = 0, 0.010, 0.015, 0.020, 0.025, 0.030) samples

3.4 Magnetic properties

The magnetism of the spinel ferrite is due to the super-exchange coupling of uncompensated electron spins of the individual magnetic ions through oxygen ions. Owing to this super-exchange interaction, the spins are aligned antiparallel in the two (A and B) sublattices of spinel structure [20]. Therefore, the net magnetic moment is the difference between individual magnetic moments of A and B sublattice, i.e., M = |MB − MA|, where MA and MB are magnetic moment of ions residing at A and B sites, respectively. Figure 6 represents the hysteresis loops of Nd3+-substituted cobalt ferrite, which clearly shows the ferromagnetic behavior. From these plots (Fig. 6), the saturation magnetization (Ms), coercivity (Hc) and ratio of remanence to saturation magnetization (Mr/Ms) were calculated, as listed in Table 2. It is well known that the 4f electrons are responsible for the magnetic moment of rare-earth ions and their magnetic ordering temperature is effective at 40 K [21]. Therefore, the effect of Nd3+ on net magnetic moment of spinel is almost negligible. However, due to their presence at octahedral (B) site, some of Fe3+ may shift to tetrahedral (A) site, which in turn alters the magnetic properties.

Fig. 6
figure 6

Magnetic hysteresis loops for CoNdxFe2−xO4 (x = 0, 0.010, 0.015, 0.020, 0.025, 0.030) samples and inset being variation of magnetization with Nd concentration

Table 2 Saturation magnetization (Ms), coercivity (Hc), remanence magnetization (Mr) and magnetic moment (nB) of CoNdxFe2−xO4 (x = 0, 0.010, 0.015, 0.020, 0.025, 0.030) samples

It is observed that as the concentration of Nd3+ increases, saturation magnetization (Ms) decreases. The value of Ms is seen to decrease from 60 mA·m2·g−1 for undoped cobalt ferrite to 35 mA·m2·g−1 for CoNd0.03Fe1.97O4. The effective magnetic moment of Nd3+ is 3.2 µB, which is smaller than that of Fe3+ (5.0 µB). Therefore, substitution of Fe3+ by Nd3+ at B site causes Ms to decrease. In the present investigation, saturation magnetization values are higher than the reported values [22,23,24]. The coercivity decreases from 19.9 mT (x = 0) to 17.4 mT (x = 0.030) with Nd3+ content. This is due to the decrease in magnetic anisotropy of the system. The behavior of coercivity can be understood from Brown’s relation given by:

$$H_{\text{c}} = \frac{{2K_{1} }}{{\mu_{0} M_{\text{s}} }}$$
(5)

where K1 is the magnetic anisotropy, \(\mu_{\text{o}}\) is the permeability of free space and Ms is the saturation magnetization. According to the above relation, Hc is inversely proportional to Ms and directly related to K1. It is reported that substitution of Nd3+ reduces the anisotropy constant [5, 18, 25]. The coercivity of the pure cobalt ferrite predominantly originated from the single-ion anisotropy of the octahedral Co2+. Similar to Co2+, Nd3+ also shows a strong spin–orbit coupling and contributes to the anisotropy, when they are located in the B sites of spinel ferrites. However, remarkable decrease in coercivity may be ascribed to the larger lattice distortion and smaller reduction in crystalline size. Therefore, for all samples, contribution of the anisotropy leads to the decrease in coercivity.

4 Conclusion

Nd3+-substituted cobalt ferrite was synthesized using standard ceramic method, and its effects on structural, electrical and magnetic properties were studied. XRD study shows the formation of single phase with cubic spinel structure. Crystallite size and grain size are affected by the substitution of Nd3+, suggesting that growth of crystallite size is obstructed by the substitution of Nd3+. The room-temperature DC electrical resistivity increases and saturation magnetization decreases with Nd3+ substitution increasing. Finally, it is concluded that the properties of cobalt ferrite get affected by changing parameters such as amount of substitution, method of processing, sintering temperature as well as cationic distribution and play a major role.