This study presents a comprehensive magnetic and morpho-structural investigation of α-Fe2O3 nanostructures from two distinct origins: natural (geologically extracted) and synthesized (i.e., laboratory-synthesized by an auto-combustion sol–gel method and commercially purchased hematite). All samples underwent thermal treatments, designed to reproduce color changes typical of hematite pigments in archaeological contexts. Through a combination of DC magnetization measurements and Mössbauer spectroscopy, we demonstrated the possibility of differentiating the origin of hematite nanostructures based on their magnetic behavior. Interestingly, low-temperature NPD analysis revealed that the intensity of the magnetic peak (003) was partially suppressed but not completely extinguished as expected for a perfect antiferromagnetic alignment, which suggests a possible coexistence of weakly ferromagnetic and antiferromagnetic phases in distinct domains below the Morin transition.

Magnetism of nanostructured hematite: from cultural heritage to fundamental properties / Slimani, S.; Martinelli, A.; Omelyanchik, A.; Abdolrahimi, M.; Castagnotto, E.; Maltoni, P.; Laureti, S.; Barucca, G.; Yaacoub, N.; Locardi, F.; Ramzan, A.; Gaggero, L.; Ferretti, M.; Peddis, D.. - In: PHYSICAL CHEMISTRY CHEMICAL PHYSICS. - ISSN 1463-9076. - 28:6(2026), pp. 3963-3974. [10.1039/d5cp03945b]

Magnetism of nanostructured hematite: from cultural heritage to fundamental properties

Barucca G.;
2026-01-01

Abstract

This study presents a comprehensive magnetic and morpho-structural investigation of α-Fe2O3 nanostructures from two distinct origins: natural (geologically extracted) and synthesized (i.e., laboratory-synthesized by an auto-combustion sol–gel method and commercially purchased hematite). All samples underwent thermal treatments, designed to reproduce color changes typical of hematite pigments in archaeological contexts. Through a combination of DC magnetization measurements and Mössbauer spectroscopy, we demonstrated the possibility of differentiating the origin of hematite nanostructures based on their magnetic behavior. Interestingly, low-temperature NPD analysis revealed that the intensity of the magnetic peak (003) was partially suppressed but not completely extinguished as expected for a perfect antiferromagnetic alignment, which suggests a possible coexistence of weakly ferromagnetic and antiferromagnetic phases in distinct domains below the Morin transition.
2026
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11566/353157
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