Abstract

The possibility to finely control nanostructured cubic ferrites (M(II)Fe2O4) paves the way to design materials with the desired magnetic properties for specific applications. However, the strict and complex interrelation among the chemical composition, size, polydispersity, shape and surface coating renders their correlation with the magnetic properties not trivial to predict. In this context, this work aims to discuss the magnetic properties and the heating abilities of Zn-substituted cobalt ferrite nanoparticles with different zinc contents (ZnxCo1-xFe2O4 with 0 < x < 0.6), specifically prepared with similar particle sizes (∼7 nm) and size distributions having the crystallite size (∼6 nm) and capping agent amount of 15%. All samples have high saturation magnetisation (Ms) values at 5 K (>100 emu g(-1)). The increase in the zinc content up to x = 0.46 in the structure has resulted in an increase of the saturation magnetisation (Ms) at 5 K. High Ms values have also been revealed at room temperature (∼90 emu g(-1)) for both CoFe2O4 and Zn0.30Co0.70Fe2O4 samples and their heating ability has been tested. Despite a similar saturation magnetisation, the specific absorption rate value for the cobalt ferrite is three times higher than the Zn-substituted one. DC magnetometry results were not sufficient to justify these data, the experimental conditions of SAR and static measurements being quite different. The synergic combination of DC with AC magnetometry and (57)Fe Mössbauer spectroscopy represents a powerful tool to get new insights into the design of suitable heat mediators for magnetic fluid hyperthermia.

Highlights

  • Nanostructured metal oxides of the formula MIIFe2O4 (MII = Fe2+, Co2+, Mn2+, Ni2+, etc.), commonly referred to as cubic ferrites, are one of the most important materials for their ferrimagnetic properties closely related to their spinel structure

  • Tetrahedral sites are filled by divalent cations in a direct or normal spinel (MII)[MIII]2O4, whereas trivalent cations replaced them in an inverse spinel (MIII)[MII;MIII]2O4.1

  • CoFe2O4 shows a predominantly inverse structure with Co2+ ions mainly on octahedral sites and Fe3+ ions almost located between octahedral and tetrahedral sites but the observed inversion degree is often lower than 1.4 ZnFe2O4 is assumed to be a normal spinel with all Fe3+ ions on octahedral sites and all Zn2+ on tetrahedral sites

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Summary

Introduction

Nanostructured metal oxides of the formula MIIFe2O4 (MII = Fe2+, Co2+, Mn2+, Ni2+, etc.), commonly referred to as cubic ferrites, are one of the most important materials for their ferrimagnetic properties closely related to their spinel structure. Ð1Þ where δ is a parameter related to the inversion degree (i = 1−δ) and it is equal to 1 for a normal spinel and 0 for an inverse one.[2] The nature of MII strongly affects the magnetic properties of the material, such as magnetisation or anisotropy.[3] CoFe2O4 shows a predominantly inverse structure with Co2+ ions mainly on octahedral sites (square bracket) and Fe3+ ions almost located between octahedral and tetrahedral sites (round bracket) but the observed inversion degree is often lower than 1.4 ZnFe2O4 is assumed to be a normal spinel with all Fe3+ ions on octahedral sites and all Zn2+ on tetrahedral sites. As a consequence of their structure, CoFe2O4 is 10124 | Nanoscale, 2016, 8, 10124–10137

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