Open-access New synthesized bismuth-based pyrochlore compounds Bi1.5-xMxSb1.5-xM'xZnO7 (M= Fe; M'=Fe, Cr) (x=0.0; 0.10; 0.15): A structural study.

Abstract

New limited pyrochlore solid solutions of formula Bi1.5-xMxSb1.5-xM'xZnO7 (M= Fe; M'=Fe, Cr) (x=0; 0.10; 0.15) are prepared from simple oxides at 1080°C by using the ceramic method. All the crystal phases are indexed in the cubic system (space group; No.227). Rietveld refinement method of the Bi1.5Sb1.5ZnO7 (x=0) compounds using powder XRD analysis confirms an overall A2B2O7 cubic pyrochlore structure according to Bi1.53+Zn0.52+Sb1.55+Zn0.52+O7 formula with 10.44425(3) Å and Fd3¯m space group. The substitution of Bi(III) and Sb(V) by Fe(III) and Cr(III) in the Bi1.5Sb1.5ZnO7 phase shows the appearance of solid solutions limited to x=0.15. The variation of the cell’s parameter is recorded to the element’s ionic radii. The paramagnetic character is observed in all substituted compounds. The measurements of the electrical conductivity as a function of the temperature, make evidence of the semi-conductive property. Whilst, the magnetic susceptibility satisfies the modified Curie Weiss (CW) and shows the magnetic behavior due to the magnetic moments of the iron and chromium ions being involved in the synthesis of the compounds. Besides, the UV-Visible reflectance displays light absorption in the visible domain.

Keywords:
Pyrochlore; Oxides; Solid Solution; Magnetic susceptibility; Electric Conductivity

INTRODUCTION

Pyrochlore-type minerals are a family of compounds with a wide variety of chemical compositions of considerable interest, remarkable advantages, and variable physical properties. Their general formula is written in the form A2B2O6O’ or A2B2O6X (X being an anion), with “A” stands for relatively large mono-, bi- or trivalent cation such as Bi+3 (La, Ca, K, Ba, Y, Ce, Sr, …etc.), in coordination 8 and a radius often greater than 1Å, “B” for smaller cation such as Zn+2 (Sb, Nb, Ta, Ti, Sn, …etc.), in coordination 6. The position of the seventh anion (X) in the crystalline structure can be occupied by the anion O2-, OH-, or F- (1. They are face-centered cubic symmetry materials with 8 molecules per cell. The structure can be considered the nesting of the two relatively interdependent networks 2)-(4, where the oxygen atoms are in two different networks: A2O’ tetrahedral and B2O6 octahedral. There are two types of sublattices: A2O’ where the cation “A” is in coordination 8 (with 2 O’ atoms and 6 O atoms) inside a rhombohedron and B2O6 where the cation “B” is in octahedral coordination and shares vertices to form larger cavities 5. Previous studies have shown that the Bi1.5Sb1.5CuO7 compound has a pyrochlore-like structure where the copper is distributed between the sites A and B according to the formula (Bi1.5Cu0.5)(Sb1.5Cu0.5)O73. Whilst other compounds display similar organization typical of a pyrochlore with zinc i.e. (Bi1.5Zn0.5)(Sb1.5Zn0.5)O7 [6, 7] or (Bi1.5Zn0.5)(Nb1.5Zn0.5)O78), (9 or compounds with manganese Bi1.5Sb1.5−xNbxMnO710 and cobalt (Bi1.56Co0.44) (Sb1.48Co0.52)O711 or finally (Bi1.56Co0.44) (Sb1.48-xNbxCo0.52)O712.

The properties of these materials often change with temperature 1), (6), (14)-(16; they can be used therefore in different fields, such as ferroelectricity (as ionic conductors), or mixed conductors (ionic and electronic) in particular as metallic conductors, semi-conductors or even superconductors 17)-(21. They exhibit oxygen conductivity that allows them to be utilized in solid electrolyte fuel cells 22), (23. Besides, they have dielectric, piezoelectric, ferromagnetic, and anti-ferromagnetic properties 24)-(32. Their sensitive photocatalytic behavior towards visible light, 33), (34, high magnetoresistance 35), (36, and host matrix of nuclear waste 37), (38 have been proven. With such materials, it is possible to produce novel solid pyrochlore solutions by substituting cations at sites A and/or B under certain experimental operating conditions 6. Moreover, it may be noticed that non-oxidized pyrochlore structures based on chlorides and fluorides have been demonstrated 39), (40. Recently, a new solid solution of pyrochlore-type cobalt oxide was synthesized with the chemical formula Bi1.56-xCax Sb1.48Co0.96O7-δ and proved very interesting physical properties 41. Based on this study, a further investigation has been carried on by using the new synthetized bismuth-based pyrochlore compounds.

In the present study, the substitution of bismuth/ antimony by iron/chromium on the structural and magnetic/electrical properties in solid solutions that derive from the Bi1.5Sb1.5ZnO7 phase 7 was investigated. The phases studied were in the form Bi1.5-xMxSb1.5-xM'xZnO7 (M= Fe; M=Fe, Cr) (x=0.10; 0.15) and were synthesized using the ceramic method at high temperatures; x being the rate of substitution. All the compounds obtained were characterized by XRD, SEM, FTIR, and UV-Vis reflectance spectroscopy. In addition, the magnetic and electrical properties were also carried out to determine their physical properties.

EXPERIMENTAL

The materials were prepared by reaction in the solid state and subsequently limited solid solutions were obtained by taking the pyrochlore compound base of formula Bi1.5Sb1.5ZnO7 as recommended elsewhere 7. A series of microcrystalline samples of mass 2 g each were prepared, in solid and under air state conditions separately, from the stoichiometric mixtures of the precursor oxides Bi2O3 (99.9%), ZnO (99.9%), Sb2O3 (99.9%), F2O3 (99.9%), and Cr2O3 (99.9%) (Aldrich Chemical Company Ltd). Before heating, the mixtures were ground in an agate mortar, pestled for 1 hour, and then placed in sintered alumina crucibles. A first heating was carried out at 700°C for 24 hours (well below the melting point of Bi2O3, 825°C), followed by a second heating at 900°C for 72 hours. The third heating was carried out at 1000°C for 24 hours and finally, the samples were then made in a mortar in the form of pellets approximately 10 mm in diameter and 2 mm in thickness by applying a pressure of 400 kgf/cm2, to undergo a final sintering treatment at 1080°C for 48 hours. At the end, the samples were cooled to room temperature and taken out from the oven. Between two heat treatments, homogenization grinding was necessary and as a general rule, all these intermediate procedures of heating have been carried out to achieve the complete reaction between the starting oxides.

After having been synthesized and elaborated, the samples were then characterized by X-ray powder Diffraction (XRD) using a diffractometer (Siemens D5000) operating in Bragg- Brentano type focusing geometry (θ/2θ) with the wavelength Kα of copper (λ=1.542Å). All the data were collected in the domain 10°<2θ<80° with a step of 0.02°. The characterizations by infrared spectroscopy were carried out using the Perkin Elmer Spectrum type (Version 10.4.00). The same specimens, in the form of pellets, were examined under a scanning electron microscope SEM of type Hitachi S3400N then a UV- Vis - diffuse reflectance spectrometer of type JASCO apparatus. In addition, the measurements of the magnetic susceptibility of these samples were carried out by using the superconducting quantum interference magnetometer (SQUID). Finally, the electrical conductivity measurements were carried out using the classical two points method in the temperature range 425 - 800°C; The details of the electric conductivity measurements are described elsewhere. 41.

RESULTS AND DISCUSSION

Fig. 1 presents all the diffractograms of the system Bi1.5−xMxSb1.5−xMxZnO7 (M= Fe; M'=Fe, Cr) (x=0; 0.10; 0.15). Three limited solid solutions were obtained from formula Bi1.5-xFexSb1.5ZnO7 [BiFe], Bi1.5Sb1.5−xFexZnO7 [SbFe], and Bi1.5Sb1.5−xCrxZnO7 [SbCr]. All peaks are indexed in a face-centered cubic lattice (space group Fd3m), which are phases isotype to the basic compound Bi1.5Sb1.5ZnO77.

Figure 1:
XRD patterns for the limited solid solution in the pyrochlore system according to formula Bi1.5−xMxSb1.5−xM'xZnO7 (M= M'Fe [BiM]; =Fe, Cr [SbM') (x=0; 0.10; 0.15).

The refinement of the lattice parameters was carried out by the Rietveld method in the profile matching mode. Fig. 2 shows the evolution of the lattice parameter calculated for each system. The computed values of the lattice parameter, illustrate a regular decrease in the difference of the ionic radii of antimony (RVI=0.61Å), iron (RVI=0.55 Å), chromium (RVI=0.55 Å), bismuth (RVIII=1.17 Å) and iron (RVIII=0.92 Å) 42. On the other hand, Scherrer’s equation 43 was used to calculate the dimensions of the crystallites from the contribution of the size effect to the half-width of peaks. Indeed, the sizes in the interval range (37.2 - 55.8 nm), depend upon the synthesis method, the diffusion during the sintering, and the substitution rate (x). Table 1 summarizes the calculated dimensions as well as values of gap energy and magnetic susceptibility parameters which will discussed later on in the text. One can notice that the substitution in the “A” site keeps the same value; however, that in site “B” increases the average grain size with the same value for both iron and chromium.

Figure 2:
Variation of the lattice parameter of pyrochlore system Bi1.5−xMxSb1.5−xM'xZnO7 (M= Fe [BiM] M'=Fe, Cr [SbM') (x=0.10; 0.15).

Table 1
Crystallite dimensions, energy band gaps, effective magnetic moments, and colors for pyrochlore compounds.

The pyrochlore phase with the formula Bi1.5Sb1.5ZnO7 was further refined according to XRD data. The ideal pyrochlore structure (space group Fd-3m) was used as a starting model 11. The best agreement between experimental and calculated data was obtained for the disordered pyrochlore model. The results of the experimental composition refinement by this method are in satisfactory agreement with the assumed theoretical ones. The experimental, calculated, and difference diffractograms of (Bi1.5Zn0.5)(Sb1.5Zn0.5)O7 are shown in Fig. 3. A characteristic result of the structure refinement, is the displacement of bismuth atoms from the highly symmetric positions 16d down to the 96g ones and the disordering of the oxygen crystallographic position to the filled 48f and deficient 32e. The zinc metal cations (Zn2+) partially occupy the 96g and 16b positions with a percentage of 25% in each crystallographic site. This atomic distribution corresponds exactly to the calculated stoichiometric formula (Bi1.5Zn0.5)(Sb1.5Zn0.5)O7. Tables 2 & 3 present the results of refining the pyrochlore structure for the composition calculated by the Rietveld method in the space group Fd- 3m (N° 227). Fig. 4 gives the descriptions of the crystal structures by showing the location of the two sites “A” and “B” as well as the two types of oxygen. Table 4 yields some bond lengths in both sites. The refinement of the structure shows that the “B” site is formed by the two cations Sb5+ and Zn2+ forming a B-O6 octahedron with a bond length equal to 1.990(2) Å. Individual interatomic distances in the A-O8 polyhedron vary from 2.28 to 2.96 Å. The ion distribution model in the structure is similar to those described elsewhere for pyrochlores in Bi1.5Zn0.92Nb1.5O6.92 systems 8. The pyrochlore unit cell parameter is 10.44425(3) Å. This value is less than the one for Zn-containing pyrochlore i.e. 10.5616(1) Å based on bismuth niobate 8 and subsequently, the values determined for cobalt pyrochlores based on bismuth antimoniate i.e. 10.44896(2) Å 11. The lattice parameter is directly related to the value of the ionic radii of the cations constituting the crystalline structure.

Figure 3:
Theoretical, calculated, and difference XRD powder diffraction of Bi1.5Sb1.5ZnO7 pyrochlore structure.

Table 2
Rietveld refinement results.

Table 3
Atomic positions and site occupation.

Figure 4:
(Bi1.5Zn0.5)(Sb1.5Zn0.5)O7 cubic pyrochlore structure.

Table 4
Selected bond lengths (Å) and angles (°).

Fig. 5 presents the different surface morphologies of the phases from the photographs taken on the pellets. The micrographs of Bi1.5Sb1.5−xFexZnO7 and Bi1.5Sb1.5−xCrxZnO7 (x=0.1 and x=0.15) show relatively dense phases with a particle size that changes slightly depending on the substitution rate (x), the size of the ionic radii and probably the effect of the diffusion rate of the ionic species during the growth of the grains while sintering. In the case of Bi1.5-xFexSb1.5ZnO7 (x=0.10 and x=0.15), one can observe a more porous surface with an irregular lump-like morphology with a spherical shape of its grains despite the remarkable difference in the size of the ions [RBi(VIII)=1.17Å; RFe(VIII)=0.92Å]. The phases resulting from the substitution of Bi by Fe permit the formation of crystallites of smaller size leading to a morphology composed of them, which tends to settle along the same plane. Figure 6 displays the EDS analysis data of some synthesized samples. Indeed, all the metal cations Bi, Sb, Zn, Fe, and Cr are present. Table 5 summarizes the values expressed in mass percentage of all the cations forming the synthesized compounds.

Figure 5:
SEM phase micrographs: (A) Bi1.5Sb1.5−xFexZnO7; (B) Bi1.5Sb1.5−xCrxZnO7 and (C) Bi1.5-xFexSb1.5ZnO7 (x=0.10; x=0.15).

Figure 6:
EDS analysis data of some synthesized compounds.

Table 5
EDS analysis data.

The pyrochlore A2B2O7 phases have already been the subject of such analyses and the frequencies of the vibrations of the infrared lattice of certain compounds have been studied elsewhere 44), (45. Indeed, the interpretation of the FTIR spectra can provide further information on the nature of possible order defects in the pyrochlores 46. In our case, as shown in Fig. 7, the spectra display similarities where the absorption bands occurring in the range 400 - 2000 cm-1, correspond to the same vibrational frequencies that are generally attributed to vibrations of metal ions in the crystal lattice 47. The frequency of the strongest band is located at about 648 cm−1 and is attributed to the Zn-O stretching vibration in the ZnO6 octahedron. Another weak band located at about 480 cm−1 appears from the Bi-O or Sb-O stretching vibration 48. Moreover, two very weak vibration bands are observed in the 1000 and 1400 cm-1 domains and suggest that these modes are an indicator of the additional structural complexity of this network.

Figure 7:
FTIR spectra of the Bi1.5−xMxSb1.5−xZnO7 (M = Fe [BiM]; M' = Fe, Cr [SbM') compounds (x=0; 0.10; 0.15).

Fig. 8 exhibits the reflectance spectra of our synthesized samples. It is well shown that the basic compound Bi1.5Sb1.5ZnO7 absorbs radiation in the UV range. The absorbance increases drastically beyond 400 nm. The other compositions can shift the absorbance in the visible range between 500 and 400 nm for the two solid solutions (BiFe, SbFe, and SbCr). The UV-Vis spectrum can be used to calculate the band gaps of semiconductor material. The Kubelka-Munk (K-M) formalism is thus used to analyze the reflectance spectrum. The K-M Function F(R) is given by Eq.1 49), (50.

F R = 1 - R 2 2 R (A)

Figure 8:
UV-Vis-DRS reflection R(%) spectra of the compounds. (Inset: Plots of [F(R).hυ]2 vs. (hν)] for some different compounds.

Therefore, from Eq.A, the familiar K-M conversion follows straightforwardly. It is thus given by Eq. B

K S = F R = 1 - R 2 2 R (B)

where (R) is the absolute reflectance of the sample. In this formula, the molar coefficient “k” identifies (1-R)2, while the scattering factor “s” identifies 2R. The K-M transform of the measured spectroscopic observable is roughly proportional to the absorption coefficient and hence is approximately proportional to the concentration given by Eq. C. On the other hand, the optical band gap values are estimated from the Tauc relation. The Kubelka-Munk function F(R) is generally applied to convert the diffused reflectance (R) and consequently to calculate the optical reflectance data according to Eq.D.

α = F R = 1 - R 2 2 R (C)

where (α) is the absorption coefficient and F(R) is the Kubelka-Munk function. Thus, the Tauc relation can be written as,

F R · h ν = A h ν - E g n (D)

where n=2 and 1/2 represent the allowed indirect and direct transitions respectively. So, in this way, the indirect and direct band gaps can be assessed. The Tauc plot [F(R).hν]2 versus (hν) for a given compound, can be given. The plots of SbFe, SbCr, and BiFe compounds with different substitution rates are shown in Fig. 8. In consequence, the extrapolation of the linear regions in the plots i.e. F(R).hν)2 = 0, yields the direct energy band gaps. Their values for the different pyrochlore compositions are listed in Table 1.

It is clear from this table that the absorbance shifts towards the visible and contributes to the Energy Band Gap values of the synthesized samples.

Similarly, to the pyrochlore cobalt oxides 41, our newly synthesized bismuth-based pyrochlore compounds exhibit the best physical properties which are the magnetic susceptibility and the electric conductivity.

The magnetic data obtained for the compounds indicate that the magnetizatio n evolves according to the maximum magnetic field applied (i.e. 9.0 T) at absolute temperature 2.0 K. In such experimental conditions, the saturation cannot be reached. This behavior is similar for both pyrochlore compounds displayed in Fig.9. The field dependence of the magnetization confirms that the sample is overall naturally paramagnetic. The temperature dependence of the inverse magnetic susceptibility is shown in Fig. 10. Above 100K, the inverse magnetic susceptibility is linear and fits satisfactorily to the modified CW law. The observed effective magnetic moments ueff, calculated from the slopes of these linear fits, are listed in Table 1. The values found for our compounds are due to the contribution of the magnetic moments arising from the iron and chromium ions. These values are in concordance with those usually found in transition metal spin-free configurations 51. The four observed effective magnetic moments of iron ranging from 5.19 to 5.78 μB and those two observed of chromium (3.66; 3.98 μB) indicate that the spin-only values expected for Fe3+(3d5, high spin t2g3eg2) i.e. μobs = 5.6 - 6.1 μB52 and for Cr3+ (3d3, high spin t2g3) i.e. μobs = 3.7 - 3.9 μB52.

Figure 9:
Magnetization versus Applied magnetic field of Bi1.5−xMxSb1.5−xM'xZnO7-δ (M = Fe [BiM]; M'=Fe, Cr [SbM') with substitution rates 0.10 and 0.15 (unit KOe).

Figure 10:
Susceptibility versus temperature of Bi1.5−xMxSb1.5−xMxZnO7-δ (M= Fe [BiM]; M'=Fe, Cr [SbM') with substitution rates 0.10 and 0.15 (unit KOe).

It is well known that the electrical conductivity of any material describes its transport property ensured by its electronic/ionic species being involved. It increases naturally with the increase in concentration and is very sensitive to the variation of the temperature. The Arrehnius relation i.e. σ = σ0.exp[-Ea/(KBT)] is well known to describe the temperature dependence of physical parameters such as electric conductivity, dielectric relaxation, …etc. So by applying the decimal logarithm to electric conductivity versus the inverse temperature, one can find the values of the activation energy (Ea) and the reference conductivity (σ0). The electrical conductivity obeying the Arrhenius behavior may be described by Eq. E

log σ = log σ 0 - E a / K B T (E)

where σ0 represents a pre-exponential factor, Ea is the activation energy, KB Boltzmann constant, and T absolute temperature. Fig. 11 gives the temperature dependence of log (σ) for SbFe0.15 and SbCr with the same substitution rate of 0.15. The substitution of the antimony cation (Sb+5) by those of iron (Fe3+) and chromium (Cr3+), induces oxygen deficiency in the formulae of the limited solid solutions. These formulae can therefore be written simply as follows: Bi1.53+Sb1.355+Fe0.153+Zn2+O7-δ2- and Bi1.53+Sb1.355+Cr0.153+Zn2+O7-δ2-. The value of oxygen deficit is thus estimated in the formulae at δ = 0.15. The presence of oxygen deficiency in compounds makes it easier for both electronic and ionic conductivities. In the investigated temperature range of 425 - 800°C, the electronic conductivity data of SbCr0.15 lie above those of SbFe0.15. At higher temperatures, they exhibit almost the same values, while they become quite different from each other as the temperature decreases. Moreover, the function log(σ) vs. (1/T) yields a straight slope (Ea/KB) from which the value of Ea can be deduced graphically. Thus, the values of Ea are 1.35 eV and 0.97 eV for the SbFe0.15 and SbCr0.15 respectively. These interesting results reveal the semi-conducting behavior of these newly synthesized compounds. This electrical behavior is similar to the electrical conductivity of the solid solution of pyrochlore type with formula Bi1.56-xCaxSb1.48Co0.96O7 recently synthesized 41.

Figure 11:
Log (σ) vs. (1/T) of SbFe and SbCr at the same substitution rate of 0.15.

CONCLUSION

In the present investigation, we have explored the partial substitution of Bismuth by Iron and Antimony by Iron and Chromium in the pyrochlore material Bi1.5Sb1.5ZnO7. The substitution limit was found equal to x=0.15 for the three types of substitutions. XRD analysis revealed a pyrochlore structure for all the compositions. The lattice parameters evolve according to the ionic radii. The Scherrer equation showed grain size in the range of 37.2 - 55.8 nm. The micrographs of compounds show relatively dense phases with a particle size that changes slightly depending on the substitution rate (x). UV-Visible diffuse makes evidence of the absorbance shift towards the visible that contributes to the Energy Band Gap level. The lowest value is given by the compound Bi1.35Fe0.15Sb1.5ZnO7 (BiFe0.15). The values of the activation energy (Ea) are 1.35 eV and 0.97 eV for the SbFe0.15 and SbCr0.15 compounds respectively. These results reveal the semiconducting behavior of these pyrochlore materials. The magnetic measurements show the magnetic behavior of the samples. The calculated magnetic susceptibilities reveal values comprised between 3.66 and 5.78 μBohr in concordance with those usually found in transition metal spin-free configurations.

ACKNOWLEDGEMENTS

We would like to thank Dr Olivier Mentré, Research Director at CNRS, for his fruitful discussions and technical assistance in carrying out magnetism analyses and electrical measurements in his laboratory at the Lille National School of Chemistry (ENSCL-BP). 9010).

REFERENCES

Edited by

  • (AE: Fernando M. B. Marques)

Publication Dates

  • Publication in this collection
    29 Nov 2024
  • Date of issue
    2024

History

  • Received
    07 Jan 2024
  • Reviewed
    02 May 2024
  • Accepted
    06 July 2024
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