The Role of Atmosphere on Phase Transformations and Magnetic Properties of Ulvospinel

Catherine Groschner,S Lan,Andrew Wise,Alex Leary,M S Lucas,Changyong Park,David E Laughlin,Marina Diazmichelena,M E Mchenry

Magnetics, IEEE Transactions（2013）

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摘要

We have synthesized the antiferromagnetic mineral ulvospinel, Fe2TiO4, in Ar to assess the role of inert atmosphere on phase formation and magnetic properties. We report the role of atmosphere on a possible phase transition and the magnetic properties of this mineral. Atmosphere dependent transformations of ulvospinel are observed with increasing temperature. Oxidation of ulvospinel to form metastable titanomaghemite is shown to occur at 300° in atmospheric conditions. Only slight titanomaghematitzation was observed in samples transformed under pressure in in situ temperature dependent X-ray experiments. Formation of ilmenite and hematite from ulvospinel was observed under high temperature, high pressure, and low oxygen atmosphere conditions.

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关键词

neel temperature,x-ray diffraction,antiferromagnetic materials,high-pressure solid-state phase transformations,high-temperature effects,iron compounds,magnetisation,minerals,oxidation,fe2tio4,antiferromagnetic mineral ulvospinel,atmosphere dependent transformation,hematite formation,high-pressure effects,ilmenite formation,in situ temperature,low oxygen atmosphere condition,magnetic properties,magnetization,metastable titanomaghemite formation,phase transformations,temperature 300 degc,titanomaghematitzation,martian mineral,remnant magnetization,thermal magnetic property,titanomagnetite,magnetosphere,x ray diffraction,atmosphere,temperature

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