Research news on magnetite

Magnetite is an iron oxide mineral with the ideal chemical composition Fe₃O₄, structurally represented as Fe²⁺Fe³⁺₂O₄, and crystallizing in the inverse spinel structure. It exhibits mixed valence of iron and electron hopping between Fe²⁺ and Fe³⁺, imparting significant electronic conductivity. As a strongly ferrimagnetic material with high saturation magnetization and Curie temperature (~858 K), it is a key phase in rock magnetism, biomagnetism, and magnetic materials research. Magnetite participates in redox processes, can undergo the Verwey transition near 120 K associated with charge ordering, and serves as a reactive surface for adsorption and catalysis in geochemical and environmental systems.

Ancient atmospheric oxygen found in iron ore deposits

How do some of geology's most mysterious iron ore deposits form? This question has preoccupied the geosciences for more than a century. An international research team led by Dr. Stefan Peters from the Leibniz Institute for ...

Have we been wrong about why Mars is red?

Mars is easily identifiable in the night sky by its prominent red hue. Thanks to the fleet of spacecraft that have studied the planet over the last decades, we know that this red color is due to rusted iron minerals in the ...

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