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Publication

The Metallofullerene Field-Induced Single-Ion Magnet HoSc2N@C-80

Jan Gui-Hyon Dreiser
2014
Journal Articles

Résumé

The low-temperature magnetic properties of the endohedral metallofullerene HoSc2N@C-80 have been studied by superconducting quantum interference device (SQUID) magnetometry. Alternating current (ac) susceptibility measurements reveal that this molecule exhibits slow relaxation of magnetization in a small applied field with timescales in the order of milliseconds. The equilibrium magnetic properties of HoSc2N@C-80 indicate strong magnetic anisotropy. The large differences in magnetization relaxation times between the present compound and the previously investigated DySc2N@C-80 are discussed.

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https://infoscience.epfl.ch/entities/publication/178bd4a9-9b70-44e6-b2d3-5b6db0ca615f

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Jan Gui-Hyon Dreiser
2014
Journal Articles

Résumé

Source officielle

https://infoscience.epfl.ch/entities/publication/178bd4a9-9b70-44e6-b2d3-5b6db0ca615f

À propos de ce résultat

Concepts associés (20)

Résonance magnétique nucléaire

vignette|175px|Spectromètre de résonance magnétique nucléaire. L'aimant de 21,2 T permet à l'hydrogène (H) de résonner à . La résonance magnétique nucléaire (RMN) est une propriété de certains noyaux atomiques possédant un spin nucléaire (par exemple H, C, O, F, P, Xe...), placés dans un champ magnétique. Lorsqu'ils sont soumis à un rayonnement électromagnétique (radiofréquence), le plus souvent appliqué sous forme d'impulsions, les noyaux atomiques peuvent absorber l'énergie du rayonnement puis la relâcher lors de la relaxation.

Magnetocrystalline anisotropy

In physics, a ferromagnetic material is said to have magnetocrystalline anisotropy if it takes more energy to magnetize it in certain directions than in others. These directions are usually related to the principal axes of its crystal lattice. It is a special case of magnetic anisotropy. In other words, the excess energy required to magnetize a specimen in a particular direction over that required to magnetize it along the easy direction is called crystalline anisotropy energy.

Magnetic domain

A magnetic domain is a region within a magnetic material in which the magnetization is in a uniform direction. This means that the individual magnetic moments of the atoms are aligned with one another and they point in the same direction. When cooled below a temperature called the Curie temperature, the magnetization of a piece of ferromagnetic material spontaneously divides into many small regions called magnetic domains. The magnetization within each domain points in a uniform direction, but the magnetization of different domains may point in different directions.

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