Abstract
Indium-substituted polycrystalline nickel zinc ferrites of different compositions Ni0.65Zn0.35Fe2−x In x O4 (x = 0.00, 0.04, 0.08, 0.12, 0.16, 0.2) have been prepared by solid-state reaction route. Calcination and sintering of all samples were done in air atmosphere at 950 °C and 1250 °C, respectively, followed by natural cooling to room temperature. Characterization of the basic composition was done by X-ray diffractometry, saturation magnetization and Curie temperature. The effect of incorporation of larger indium ions in place of iron was studied with the help of saturation magnetization, Curie temperature, permeability, magnetic loss factor, DC electrical resistivity and dielectric properties. The highest magnetization and permeability values of the present system under study are 74.1 emu/g and 438 for the basic composition (concentration x = 0). The DC electrical resistivity was found to decrease up to x = 0.3 and increase thereafter. The variation in the electric and magnetic properties of this ferrite system is dominated by the decrease in iron concentration. Characteristic high dielectric constant values were recorded for these bulk ceramic materials.
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Introduction
Polycrystalline spinel ferrites are extensively investigated for their usefulness in modern technology. The tunable magnetic and electric properties of ferrites made them better candidates for electronic and electromagnetic applications, like transformer cores, inductors, electromagnetic suppressors (EMI), microwave absorbers, etc [1, 2]. Ferrite crystallizes into face centered cubic spinel, having general formula AB2O4, where A and B are divalent and trivalent metal cations. Ferrite structure comprises two types of sublattices, tetrahedral (A) site and octahedral sites (B). Cations are distributed between these two sublattices in two ways without changing the lattice symmetry. They are, normal (divalent ions occupy A site and trivalent ions occupy B site) and inverse spinel (divalent and trivalent ions distributed between both sites at random). The properties of ferrites strongly depend on not only the method of preparation, but also on the distribution of ions in the crystal lattice.
Several ferrite compositions were studied over the last few decades and some of them are found to be interesting in the application perspective. In the family of spinel ferrites, nickel–zinc mixed ferrites are commercially important magnetic materials because of their high saturation magnetization, high electrical resistivity and low losses. Owing to their moderate permeability values, this mixed ferrite system has some limitations in view point of applications. Thus far, various kinds of substitutions were done on these materials and the effects on their properties are thoroughly studied [3, 4]. Among all those substituted cations, incorporations of several diamagnetic (divalent and trivalent) ions in place of paramagnetic ions into ferrite systems were remarkably improved their magnetic and electric properties [5, 6]. Several researchers investigated trivalent diamagnetic ions such as Al3+ and In3+ ions, but mixed results were obtained, which depend on mode of preparation. Furthermore, In3+ ions are substituted at the expense of strong ferromagnetic iron ions which may change the interactions present within the system. Previous research study of indium-substituted nickel–zinc ferrite systems in bulk form showed some interesting variations in the electric and magnetic properties [7–10]. In those systems, reasonable amount of paramagnetic ions were maintained at the expense of strong ferromagnetic ions. The present research study is aimed at investigating the effect of substitution of In3+ ions in place of Fe3+ ions, on magnetic and electric properties. Since the substitution of indium in present system is in the place of strong ferromagnetic Fe3+ ions, which are very crucial in determining the magnetic as well as electric properties of ferrites, the ferrite system may undergo remarkable modifications in its behavior under the influence of electric and magnetic fields.
Because of the intrinsic complexity and less immediate applications, there is less information available on dielectric properties of Ni–Zn ferrites. When this ferrite system is incorporated with suitable substituent, it is possible to maintain moderate magnetic and dielectric characteristics simultaneously and these can be potential contenders for microwave absorbers and magneto-dielectric applications. Being diamagnetic, larger in size and variable site occupancy with concentration, prompted the present research study and the variations in the properties have been discussed in the limit of existing understanding.
Experimental details
Samples having the composition Ni0.65Zn0.35In x Fe2−x O4 with x values ranging from 0.00 to 0.20 in steps of 0.04 were prepared by solid-state reaction method. The starting materials of analytical reagent grade nickel oxide (99 %), zinc oxide (99 %), indium oxide (99.5 %) and iron oxide (99.5 %) in powder form. The solid-state reaction used for the preparation of the samples can be expressed as:
The initial ingredients were weighed in the required proportions using micro-analytical balance. The weighed materials were thoroughly mixed in an agate mortar–pestle for 3 h in dry medium and 3 h in acetone medium. This mixture was calcined at 950 °C for 4 h in air atmosphere. The pre-sintered powder was again crushed and ground thoroughly for 3 h in acetone to promote the homogeneity among the mixture. The resulting mixture was made into pellets and toroids under the pressure of 5 and 3 tons/in.2, respectively, using 15 % polyvinyl alcohol as binder. The dimensions of the pellets were of 4 mm thickness and 3 cm in diameter. The toroids were of 13 mm inner diameter and 18 mm outer diameter. Both the pellets and toroids were sintered at 1250 °C in air atmosphere for 2 h, followed by natural cooling to room temperature. The surfaces of all the samples were polished to remove any oxide layer formed during sintering.
The present series of samples were characterized by Philips X-ray diffractometer with Cu kα source (λ = 1.5418 Å). The interplanar spacing d hkl has been obtained from the intensity versus 2θ graph of X-ray diffraction pattern using Bragg’s law,
The plane indices (h k l) have been assigned to each peak using the X-ray data of the standard spinel structure. Lattice parameter ‘a’ has been calculated from each peak using equation, a = d \(\sqrt {(h^{ 2} + k^{ 2+ } l^{ 2} )}\) [11]. Nelson–Riley function for the high-intensity peaks calculated using the formula [12]:
Accurate determination of lattice parameter has been obtained from the extrapolation of lattice parameter ‘a’ versus F(θ).
Saturation magnetization was measured by Ponderometer (pendulum) method described by Rathenov and Sneok [13]. The ferrite samples used for measurements have the dimensions approximately 2 mm × 3 mm × 3 mm. Curie temperature was measured by the experimental setup described by Soohoo [14].
Inductance (L) measurements on the toroidal samples were carried out using LCR-Q-METER-SORTER at a small voltage of 10 mV. The average dimensions of the toroidal samples used in this study are as follows: outer diameter (OD) = 15 mm, inner diameter (ID) = 8 mm; thickness (h) = 4.5 mm. All toroidal samples were wound with 30 SWG enameled copper wire and 30 turns. Initial permeability at 1 kHz frequency and at room temperature was computed using, \(\mu_{i} = \frac{L}{{L_{0} }}\), where L is the inductance of toroidal sample, L 0 = 4.606 N 2 h log (OD/ID) 10−9 Henry is the air core inductance, and N is the number of turns.
The DC resistivity of the ferrite samples is measured with two-probe method. In this method, the sample is placed in between two spring-loaded copper electrodes connected to Digital Nano-ammeter model DNM-121. The freshly ground flat surfaces of the samples were coated with conducting (air-drying) silver paint and placed in an oven at 100 °C for 30 min to ensure good ohmic contacts. The electric current in the samples was measured with the help of digital nano-ammeter by applying a constant field of 1 V/cm between the parallel surfaces of the sample.
The present series of samples were investigated for dielectric properties by using LCR-Q-METER-SORTER (APLAB model 4912) at 1 kHz frequency and at room temperature. If C is the capacitance of the sample, d its thickness and A the surface area, then, dielectric constant ε′ = Cd/ε 0 A, where ε 0 is the dielectric constant of the air. The dielectric loss factor ε′′ has been calculated from the relation: ε′′ = ε′ tan δ, where tan δ is the loss tangent.
Results and discussion
Characterization
X-ray diffraction patterns of all the indium-substituted nickel–zinc ferrite samples have the standard planes (220), (311), (222), (400), (422), (511), (440) and (533), as well as no detectable additional peaks, which confirm the formation of single phase cubic spinel structure. X-ray diffraction pattern of the basic sample Ni0.65Zn0.35Fe2O4 is shown in Fig. 1a.
The characteristic d-spacings of the basic sample are in good agreement with values reported in standard JCPDS cards. The lattice constant for the basic sample was determined using Nelson–Riley extrapolation method. Nelson–Riley plot for the basic sample is shown in Fig. 1b.
The experimentally observed lattice constant (8.3738 Å) of the basic sample is in agreement with the reported value (8.382 Å) of the same composition [15].
Saturation magnetization
Magnetization of ferrites is strongly dependent on the exchange interactions between cations present at A and B sites. These exchange interactions are A–B, B–B and A–A interactions, either positive or negative. The parallel arrangement of cations is represented by positive and negative sign denotes anti-parallel arrangement of cations. These interactions depend on magnitude, sign, the extent and form of overlap of the 3d electron wave functions of the neighboring ions. The strength of the interaction is proportional to the distance between ions and the cations present in the ferrite system. Therefore, when the system is altered with larger/smaller cations it may influence the magnetization. Magnetization of ferrites also can be explained on Neel’s theory of ferrimagnetism (two sub lattice model) [16]. According to this model, the magnetization of ferrites depends on the magnetic moments of two sublattices [tetrahedral (A) and octahedral (B) sites]. From Neel’s two sublattice model, the expression for the total net magnetization of the ferrite structure M = |M B − M A|, where M B and M A are magnetizations of A and B sub lattices, respectively. The variation of saturation magnetization and Curie temperature with the increase of indium concentration is shown in Fig. 2.
Saturation magnetization of the present series of samples is observed to be decreased from x = 0 to 0.2 with increase in indium concentration, but the decrease is not perfectly linear. From the available literature [10], indium has variable site occupancy. For lower concentrations of indium, In3+ ions migrate to tetrahedral sites leading to the dilution of A-sublattice and decrease in the magnetic moment of the A-sublattice. This will result in the modifications of the exchange interactions. Moreover, the substitution of diamagnetic In3+ ions at the expense of ferromagnetic Fe3+ ions reduces number of magnetic ions to non-magnetic ions ratio at octahedral sites, results in the dilution in the net magnetic moment of the ferrite system as a whole, that is, there is a decrease of 0.04 × 5 = 0.2 Bohr magnetons per one formula unit. At higher concentrations of In3+ ions, because of the small octahedral preference of indium, these ions move to octahedral sites leading to the migration of Fe3+ ions from octahedral site to tetrahedral site, reducing octahedral magnetic moment (M B). Thus, the net magnetic moment of the system decreases. Furthermore, the incorporation of larger indium ions (0.62 and 0.8 Å in A and B sites) in place of iron ions (0.49 and 0.645 Å in A and B sites), makes the sublattices to stretch, resulted in the increase in distances between magnetic ions of A and B sites. As a result, the interaction between A and B site ions (A–B exchange interactions) weakens, which is evident by the fall of Curie temperature with increasing indium content. The saturation magnetization (74.1 emu/g) and Curie temperature (382 °C) of the basic sample are well in agreement with the reported values [17].
Permeability and magnetic loss
The variation of permeability and magnetic loss factor with composition at a standard frequency 1 kHz are shown in Fig. 3. The initial permeability slowly decreases from basic composition x = 0 to x = 0.04, after there is a sharp fall in the vicinity of x = 0.08, followed by a gradual decrease up to the last sample. The decrease in permeability can be explained as follows.
In general, Fe3+ ions occupy both tetrahedral and octahedral sites. From the available literature, it is known that the anisotropy contribution of the Fe3+ is positive for tetrahedral site and negative for octahedral site [18]. Since, the Fe3+ ions distributed over the two lattices, the net anisotropy is taken from the relative contribution of these ions towards anisotropy. For lower concentration of indium (x = 0.04), they prefer to occupy tetrahedral sites [19], thus, Fe3+ ions move to octahedral sites, consequently, decrease in the net anisotropy. Therefore, an increase in permeability is expected, but the decrease in magnetization (8.1 emu/g) dominates and resulted in the slight decrease of permeability (438–412.9). After x = 0.04, huge drop in permeability was observed and it is attributed to displacement of indium ions towards octahedral sites. With the increase in diamagnetic indium substitution, In3+ ions occupy octahedral sites, thus decrease in the concentration of Fe3+ ions at B site compared to A site. As a result, the net magnetic anisotropy contribution from iron ions distributed over two sites increases, so as the magnetic crystalline anisotropy constant K 1. According to the relation μ i α (\(M_{\text{s}}^{2}\) D m)/K 1 [6], permeability is inversely proportional to magneto crystalline anisotropy constant. So, the increase in anisotropy and decrease in magnetization M s is responsible for the decrease in permeability. In this present system, low concentration of Fe2+ ions are present, which are evident from the observed fall in resistivity values and the contribution of Fe2+ ions to the anisotropy is positive. But it is not taken into consideration, because the amount of Fe2+ ions present in B site is less than amount of Fe3+ ions moved to the tetrahedral site. The variation in magnetic loss factor is attributed to the formation of Fe2+ ions in octahedral sites, which are more at x = 0.04 and 0.08. This is supported by the decrease in resistivity.
DC electrical resistivity
The variation of dc electrical resistivity with composition is shown in Fig. 4.
The resistivity of the substituted indium (8.37 μΩ cm) is less than the replaced iron (9.61 μΩ cm) [20]; thus, a decrease in resistivity of the whole series is expected. But the resistivity is decreased initially up to x = 0.08 and then increased up to last composition. The variation in resistivity can be explained by the following manner. In general, the resistivity can be explained on the basis of electron hopping mechanism. The transfer of electron between same/different elements having different states is called hopping. It is assumed that Fe3+ can occupy both A and B sites, but it should be noted that Fe2+ ions at octahedral sites are responsible for electrical conduction [21].
At lower concentrations indium ions will occupy A site [10], thus there is a movement of Fe3+ ions from A to B site, thus increasing concentration of Fe3+ ions at B site. At high sintering temperatures, zinc volatilization occurs and they escape from the samples in the form of ZnO, thus, creating oxygen vacancies during the process [22]. In this situation, to maintain charge balance, formation of Fe2+ ions takes place, resulting in increasing the hopping possibility and this may be responsible for the decrease in resistivity up to x = 0.08. At higher concentrations most of the indium ions occupy B site leading to a less concentration of Fe3+ at B site, that is, less possibility of having Fe2+ ions. Thus, In3+ ions in the B site hinder the electron exchange between ions Fe2+ and Fe3+ located in equivalent crystallographic positions in the lattice and contribute to the increase in the resistivity. As a whole, the resistivity of the entire series of substituted samples was found less than the resistivity of basic composition 178.4 x 104 Ω cm. The resistivity values of the present series of samples are greater than two orders of the reported indium-substituted Ni–Zn ferrite with small concentration of titanium [10]. The increase in the resistivity of the present system may be due to the absence of titanium.
Dielectric properties
Ferrites, which are heterogeneous dielectric ceramic materials, mainly because of the formation of Fe2+ ions during sintering process, giving rise to dielectric polarization producing large dielectric constants. Especially in Ni–Zn mixed ferrite system, high dielectric constants are reported [23, 24], because of the formation of Fe2+ ions at the expense of zinc volatilization. Another cause is the presence of higher conductivity phases (grains) in the insulating matrix (grain boundaries) producing a local accumulation of charge under the influence of an applied electric field. The interface between the grains could be grain boundaries, intra-granular pores or voids which act as scattering centers for electrons. The dielectric behavior in ferrites could be explained on the basis hopping conduction mechanism which is similar to that of mechanism of dielectric polarization. Many researchers have established a strong correlation between conduction mechanism and dielectric constant of ferrites [25]. In these studies they have explained the dielectric behavior on the basis of number of available Fe2+ ions in the octahedral sites. The electron exchange Fe2+ ↔ Fe3+ results in a local displacement of electrons in the direction of applied electric field which determines the extent of polarization so as the dielectric constants of ferrites.
The variation of dielectric constant and loss factor at a frequency 1 kHz is shown in Fig. 5.
The observed variation in dielectric constant with indium concentration could be explained by local displacement of charge carriers in presence of applied electric field and variation of resistivity. At lower indium concentration, due to oxygen ion vacancies in the samples, there is an availability of additional electron and electron exchange between Fe2+ ↔ Fe3+. Thus, the excess charge carriers experience drift from the applied of field and leading to dielectric polarization. Which is clearly displayed in the dielectric constant values, especially in the vicinity of x = 0.08. At this concentration, lowest resistivity (highest conductivity) of the entire series was observed. At higher indium concentration, iron ions are less available for hopping, thus the electron is obstructed by larger indium ions in B site and the electrons/ions cannot follow the field resulting in a decrease of dielectric constant. This is well supported by the increase in resistivity. The high dielectric constant values are characteristic for bulk ferrites. These kinds of values were earlier reported by the author [23] for the same system with cadmium substitution and comparable results were also showed in similar system in bulk form [24]. Similar behavior is observed in dielectric loss factor also. Dielectric loss is attributed to several factors such as microstructure, defects, stoichiometry, Fe2+ concentration, etc. The variable Fe2+ concentration is responsible for dielectric loss in the present series of samples.
Conclusion
Indium-substituted Ni–Zn ferrite system was prepared by conventional double sintering solid-state reaction route. The basic composition was characterized with X-ray diffraction pattern and the observed characteristic peaks confirmed the method adopted for the process of ferrites was the correct one. The saturation magnetization and Curie temperature have been decreased with indium content. Firing the samples at elevated temperatures resulted in the formation of Fe2+ ions, affecting electrical properties. DC electrical resistivity was decreased initially and then increased up to the last composition. Dielectric constant and loss factor increased up to x = 0.08 then decreased afterwards. Highest dielectric constant is observed at x = 0.08 due to the presence of more Fe2+ ions. The dielectric constant and loss factor followed a trend opposite to the resistivity. The noticeable increase in permeability, dielectric constant and moderate resistivity of the samples x = 0.08 and 0.12 were observed and displayed the typical characteristics of magneto-dielectric and microwave-absorbing materials.
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Vara Prasad, B.B.V.S. Effect of indium substitution on the electrical and magnetic properties of Ni–Zn ferrite. J Theor Appl Phys 9, 267–272 (2015). https://doi.org/10.1007/s40094-015-0185-5
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DOI: https://doi.org/10.1007/s40094-015-0185-5