3.1 Structural and magnetic properties
X-ray diffraction (XRD) patterns of CoFe2–xErxO4 nanoparticles (x = 0.0, 0.01, 0.03, 0.05) heat treated at 600oC for 3h are shown in Fig. 1. The prominent diffraction peaks corresponding to the miller indices (220), (311), (222), (400), (422), (511) and (440) observed in the spectra for all the samples are identical to cubic spinel phase (JCPDS card No 20-1086) with space group Fd3̅m. A clear investigation of XRD spectra ruled out the formation of secondary phase, whereas several other researchers reported an insignificant amount of secondary phase in rare earth doped ferrites due to higher mol percentage of dopant concentration [25–27]. Therefore, the adopted method of preparation in the present work promisingly produced Er3+ doped Cobalt spinel ferrite and the lower heating temperature 600oC is also sufficient to obtain pure single-phase ferrite. The lattice parameter of the samples was determined using the following relation.
aexp = dhkl\(\sqrt{{h}^{2}+{k}^{2}+{l}^{2}}\) (1)
where dhkl is the interplanar spacing of the crystal system. The lattice constant is found to 7increase from 8.3547 to 8.3723 Å with increasing Er3+ content shown in Table 1. This variation in lattice constant is a direct consequence of the difference in the ionic radii of Er3+ and Fe3+ ions 0.89Å and 0.645Å, respectively. In general, most of the rare-earth elements couldn’t enter in to the host lattice due to (i) their larger size (ii) preferential occupancy of sublattice and (iii) exceed solubility limit in the host lattice. In the present work, reasonable ionic radii, linear increase in lattice constant with no secondary phase formation confirms that Er3+ ions occupy the host lattice. It was an expected result, where octahedral and tetrahedral sublattice expands in such a way that they do not disturb the final structure of the spinel unit cell. This kind of variation or modification in the unit cell increases the distance between cations, bond lengths and bond angles, where they can significantly impact magnetic and electrical properties. Williamson-Hall method was used to estimate the average crystallite of Er doped Cobalt ferrite nanoparticles by considering FWHM of all the prominent peaks to separate the size and strain broadenings influence on crystallite size and listed in Table 1. It is clear that, average crystallite size increases with increasing Er3+ doping similar to other reports [28]. Figure 3 shows TEM image of pure and doped cobalt ferrite revels that particles distributed homogenously. The particle was estimated using Image J software and listed in Table 1, which are in good agreement with XRD results. Further, structural parameters like X-ray Density (ρx), Lattice Strain (ε) of the samples were calculated and listed in Table 1 using standard equations to understand the influence of Er3+ ions. In order to justify the magnetic properties and solubility of Er3+ ions in to the host lattice Theoretical cation distribution and lattice parameter were calculated using the following relation and listed Table 1.
Table 1
Composition (x), Experimental (a) and theoretical lattice parameters (ath), Crystallite size (DW−H), Density (ρ) and Strain (ε) of Er doped Cobalt ferrite nanoparticles heat treated at 650oC for 3h.
Composition
|
Lattice Constant
|
Crystallite size
|
Density
|
Strain
|
(x)
|
a (Å)
|
ath (Å)
|
DW−H (nm)
|
X-ray
|
(ε) x10− 3
|
0.00
|
8.3547
|
8.4089
|
28
|
5.24
|
1.276
|
0.01
|
8.3612
|
8.4124
|
34
|
5.26
|
0.865
|
0.03
|
8.3692
|
8.4189
|
32
|
5.3
|
0.977
|
0.05
|
8.3723
|
8.4255
|
35
|
5.33
|
0.816
|
$${a}_{th} = \frac{8}{3\sqrt{3}}\left[\left({r}_{A}+{R}_{0}\right)+\sqrt{3}\left({r}_{B}+{R}_{0}\right)\right]$$
2
Where \({R}_{0}\)is the radius of oxygen ion (1.38Ao),\({r}_{A}\) and\({ r}_{B}\) are the ionic radii to tetrahedral (A-Site) and octahedral (B-Site) respectively. In general, Co2+ and partial Fe3+ions prefer to occupy B site and remaining Fe3+ occupy A site. However, due to substitution of different radii ions a marginal shift or migration occurs among A and B sites. In order to estimate the cation distribution experimental magnetic moments are also considered and the following distribution proposed and listed in Table 2. It is clear that a fraction Co2+ ions migrated from B site to A site, to accommodate Er3+ ions at B site. The good agreement between theoretical and experimental lattice constant suggests that Er3+ ions prefer to occupy octahedral (B) site.
Table 2
Estimated cation distribution of Er doped Cobalt ferrite nanoparticles heat treated at 650oC for 3h.
Composition
|
Cation Distribution
|
x
|
A site
|
B Site
|
0.00
|
Fe1
|
Co1Fe1O4
|
0.01
|
Co0.05Fe0.95
|
Co0.95Er0.01Fe1.04O4
|
0.03
|
Co0.05Fe0.95
|
Co0.95Er0.03Fe1.02O4
|
0.05
|
Co0.05Fe0.95
|
Co0.95Er0.05Fe1O4
|
Raman spectra of the pure and doped cobalt ferrite in the spectral range 200-800cm-1 region are depicted in Fig. 3. Raman spectra is merely useful to understand the modifications/adjustments that occur in the lattice due to the incorporation of foreign ions by studying vibrational and rotational band spectrum of corresponding materials. According to group theory the following phonon modes the following set of phonon modes in the normal spinel structure at ambient temperature [29]
Γ = A1g(R) + Eg(R) + T1g + 3T2g(R) + 2A2u + 2Eu + 5T1u(IR) + 2T2u (3)
where R and IR are Raman and Infrared activity modes and g and u are representing symmetry and asymmetric modes, respectively. In the above Eq. (2), 5T1u modes are infrared active, A1g + Eg+T1g+2T2g are Raman active modes which are generally observed at in the range 150–750 cm-1. For an instance, A1g and Eg are associated with symmetric stretching and bending of anion and T2g is due to asymmetric stretching of anion at A and B sites. Each mode is a result of changes in the motion/position of ‘O’ ions and both A and B sites [30,31]. In particular, vibrational mode above 600cm-1 is a direct consequence of ‘O’ and tetrahedral (A-site) cations and below are in response to ‘O’ and octahedral (B-site) cations [32]. Therefore, any change in the position of ions would affect the shape and position of Raman bands. There are four major bands observed in Fig. 2 at ~ 323,~ 475, ~ 637 and ~ 692 cm-1 respectively. These bands are assigned to five Raman active modes of vibrations Eg, T2g, A1g(2) amd A1g(1), respectively which reconfirms the formation of spinel phase. The significant variation in the position and shape suggests the incorporation of Er3+ ions in to the host lattice.
In order to evaluate the influence of Er3+ on magnetic properties low temperature magnetic measurements were carried out on powder samples. Figure 3 shows FC-ZFC curves at 500Oe for Er doped Cobalt ferrite for the composition x = 0.00 and 0.02. It is clear that the both ZFC and FC curves distinctly separated and they will not meet at 300K. This suggest that blocking temperature is higher than the room temperature and the separation between FC-ZFC suggest the presence of large anisotropy at lower temperature region. Similar behavior in magnetization at lower temperature was reported in the literature [8,33]. Further, Fig. 3c shows room temperature hysteresis loops of Er doped Cobalt ferrite. The saturation magnetization slightly increases with increasing Er3+ concentration. As mentioned earlier in theoretical cation distribution, a fraction of Co2+ and Fe3+ are migrated between A and B sites, which further result in the observed increase in net magnetization as a function of Er doping concentration.
3.2 Humidity response
Metal oxide-based materials are widely explored for humidity sensor applications due to their high mechanical and chemical stability coupled with high sensitivity low cost, and operable at different ambient conditions. Preliminary analysis of Room temperature resistance at different relative humidity ranges 0–100% were measured for Er3+ doped Cobalt ferrite disc shaped pellets (thickness 3mm and diameter 10mm) and shown in Fig. 4. These disc shaped pellets were coated with air dried silver paste on both sides for electroding and annealed at 250oC for 5 min to achieve good ohmic contacts. Finally, these pellets were placed between electrodes and enclosed in a box and measured the resistance at room temperature for different relative humidities. It was observed that Resistance decreases for all the samples in similar way with increasing relative humidity. It is well established fact that method of processing and conditions, heat treatment, density, porosity, crystallite size, grain size, stoichiometry, valence state of the constituent ions present A and B sites are the influential parameters in determining sensing capabilities of the material. In general, hopping of charge carriers between ferrous and ferric ions is the fundamental conduction mechanism in spinel ferrites. A close investigation of Fig. 4 infers that, resistance decreases with increasing humidity concentration in a non-linear trend. Further, Er3+ doped samples show higher resistance than the pristine cobalt (x = 0.00), which was due to decreasing the concentration of Fe3+ ions at octahedral B site [19]. In the present work all the Er3+ doped Cobalt ferrite samples show a good response in resistivity with increasing humidity. Further, Resistance increases with increasing Er concentration and decreases with Relative Humidity. This is due to the increase of conductivity for higher humidity concentration. The sensing response, time as a function of frequency and temperature are in progress and will be reported shortly. Considering their low cost, magnetic response and environmental stability, these materials are potentially suitable for sensor industry.