On the detection of surface spin freezing in iron oxide nanoparticles and its long-term evolution under ambient oxidation

TL;DR

This study investigates surface spin freezing in iron oxide nanoparticles, examining how long-term ambient oxidation affects magnetic properties, especially exchange bias effects, in magnetite and maghemite samples over four years.

Contribution

It provides new insights into the long-term evolution of surface spin freezing and exchange bias effects in iron oxide nanoparticles under ambient conditions.

Findings

Surface spin freezing effects are strongest in magnetite-like nanoparticles.

Aging reduces SSF effects but they remain more prominent in magnetite than maghemite.

Ambient oxidation causes a transition from magnetite to maghemite, softening spin-disordered shells.

Abstract

Exchange bias effects linked to surface spin freezing (SSF) are commonly found in iron oxide nanoparticles, while signatures of SSF in low-field temperature-dependent magnetization curves have been much less frequently reported. Here, we present magnetic properties of dense assemblies of similar-sized (~ 8 nm diameter) particles synthesized by a magnetite (sample S1) and a maghemite (sample S2) method, and the influence of long-term (4-year) sample aging under ambient conditions on these properties. The size of the exchange bias field of the different sample (fresh or aged) states is found to correlate with (a) whether a low-temperature hump feature signaling the SSF transition is detected in out-of-phase ac susceptibility or zero-field-cooled (ZFC) dc magnetization recorded at low field and with (b) the prominence of irreversibility between FC and ZFC curves recorded at high field. Sample S1 displays a lower magnetization than S2, and it is in S1 where the largest SSF effects are found. These effects are significantly weakened by aging but remain larger than the SSF effects in S2, where the influence of aging is considerably smaller. A non-saturating component due to spin disorder in S1 also weakens with aging, accompanied by, we infer, an increase in the superspin and the radius of the ordered nanoparticle cores. X-ray diffraction and M\"ossbauer spectroscopy provide indication of maghemite-like stoichiometry in both aged samples as well as thicker disordered particle shells in aged-S1 relative to aged-S2 (crystallographically-disordered and spin-disordered according to diffraction and M\"ossbauer, respectively). The pronounced diminution in SSF effects with aging in S1 is attributed to a (long-term) transition, caused by ambient oxidation, from magnetite-like to maghemite-like stoichiometry, and a concomitant softening of the spin-disordered shell anisotropy...