The structure and the magnetic properties of a series of Fe2O3-SiO2 nanocomposites (9-33 wt % Fe2O3), prepared by a sol-gel method and submitted to thermal treatments in the temperature range 300-900 degrees C, were investigated through XRD, TEM, EPR, and magnetic susceptibility measurements. Superparamagnetic iron(III) oxide nanoparticles with a narrow size distribution, dispersed over the amorphous silica matrix, are present in all the samples. They are mostly amorphous, antiferromagnetic in the samples treated at low temperatures. At T > 700 degrees C, a lot of gamma-Fe2O3 crystalline ferrimagnetic nanoparticles (4-6 nm) are formed, while a further increase of the temperature results in the gamma- to alpha-Fe2O3 transformation. The variation of iron oxide content affects the abundance of gamma-Fe2O3 formation, which reaches the maximum percent values in the more dilute samples. In the more concentrated samples, while the amount of maghemite is still growing, antiferromagnetic alpha-Fe2O3 begins to form. As a consequence, the saturation magnetization lowers in the samples with higher Fe2O3 content. Also, interparticle interactions, evidenced by fitting susceptibility values versus temperature and by EPR observations, contribute to such a decrease.

Structural and magnetic properties of Fe2O3 nanoparticles dispersed over a silica matrix

Sangregorio C
1998

Abstract

The structure and the magnetic properties of a series of Fe2O3-SiO2 nanocomposites (9-33 wt % Fe2O3), prepared by a sol-gel method and submitted to thermal treatments in the temperature range 300-900 degrees C, were investigated through XRD, TEM, EPR, and magnetic susceptibility measurements. Superparamagnetic iron(III) oxide nanoparticles with a narrow size distribution, dispersed over the amorphous silica matrix, are present in all the samples. They are mostly amorphous, antiferromagnetic in the samples treated at low temperatures. At T > 700 degrees C, a lot of gamma-Fe2O3 crystalline ferrimagnetic nanoparticles (4-6 nm) are formed, while a further increase of the temperature results in the gamma- to alpha-Fe2O3 transformation. The variation of iron oxide content affects the abundance of gamma-Fe2O3 formation, which reaches the maximum percent values in the more dilute samples. In the more concentrated samples, while the amount of maghemite is still growing, antiferromagnetic alpha-Fe2O3 begins to form. As a consequence, the saturation magnetization lowers in the samples with higher Fe2O3 content. Also, interparticle interactions, evidenced by fitting susceptibility values versus temperature and by EPR observations, contribute to such a decrease.
1998
Inglese
102
40
7721
7726
5
Sì, ma tipo non specificato
MEDIATED SYNTHESIS; NANOCRYSTALLINE GAMMA-FE2O3; MOSSBAUER-SPECTROSCOPY; IRON-OXIDE; PARTICLES; NANOCOMPOSITES; BEHAVIOR; FORM
5
info:eu-repo/semantics/article
262
Cannas, C; Gatteschi, D; Musinu, A; Piccaluga, G; Sangregorio, C
01 Contributo su Rivista::01.01 Articolo in rivista
none
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/177209
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