Akaganeite
Akaganeite, also written as the deprecated Akaganéite, is a chloride-containing iron oxide-hydroxide mineral, formed by the weathering of pyrrhotite, an iron-deficient sulfide.
Akaganeite is often described as the β phase of anhydrous ferric oxyhydroxide, but some chloride anions are commonly included in the structure, so a more accurate formula is. This formula derives from the more general expression, where x = 1/6 ≃ 0.167. As the anion is doubly negatively charged, to maintain the electroneutrality in the crystal lattice, the electrical charge deficit in must be compensated by two monovalent anions, one and one.
Nickel may substitute for iron, yielding the more general formula
Akaganeite has a metallic luster and a brownish yellow streak. Its crystal structure is monoclinic and similar to that of hollandite, characterised by the presence of tunnels parallel to the c-axis of the tetragonal lattice. These tunnels are partially occupied by chloride anions, which provide the crystal with its structural stability.
Occurrence
The mineral was discovered in the Akagane mine in Iwate, Japan, for which it is named. It was described by the Japanese mineralogist Matsuo Nambu in 1968, but named as early as 1961.Akaganeite has also been found in widely dispersed locations around the world and in rocks from the Moon that were brought back during the Apollo Project. The occurrences in meteorites and the lunar sample are thought to have been produced by interaction with Earth's atmosphere. It has been detected on Mars through orbital imaging spectroscopy.