Skutterudite is the name of a CoAs3-based mineral that was first extensively mined as a source of cobalt and nickel in the region of Skutterud, Norway.
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Skutterudite is a cobalt arsenide mineral containing variable amounts of nickel and iron substituting for cobalt with the ideal formula CoAs3.
Named in 1845 by Wilhelm Karl von Haidinger after its discovery locality, Skutterud, Modum, Norway. The earliest name that possibly refers to any ...
Skutterudite
Skutterudite is a cobalt arsenide mineral containing variable amounts of nickel and iron substituting for cobalt with the ideal formula CoAs₃. Some references give the arsenic a variable formula subscript of 2–3. High nickel varieties are referred... Wikipedia
Cleavage: Distinct on, and; in traces on
Color: Tin-white to silver-gray, tarnishes gray or iridescent; in polished section, gray, creamy or golden white
Crystal class: Diploidal (m3); H-M symbol: (2/m 3)
Crystal system: Cubic
Formula (repeating unit): CoAs3
Fracture: Conchoidal to uneven
Luster: Metallic
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Skutterudite in particular has the potential for excellent electrical properties. Skutterudite is a material consisting of cobalt and arsenic, often ...
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Skutterudite is an ore of Cobalt and Nickle. As a healing stone Skutterudite is powerfully stabilizing while also expanding one's consciousness. A stone of the ...
The current review summarizes and discusses the latest research activities (after 2014) on p- and n-type skutterudite thermoelectrics.
Bright, untarnished, metallic crystals of skutterudite up to 1 cm. Location: Bou Azzer, Morocco. Scale: Picture size 3 cm.
Skutterudite, one of a series of cobalt and nickel arsenide minerals that occur with other cobalt and nickel minerals in moderate-temperature veins.
Mined in 2003 in Jiangxi, China, this stibnite is one of the largest surviving specimens from what has become one of the world's most ...
Skutterudite materials are widely considered for thermoelectric waste heat recovery. While the skutterudite structure effectively scatters the high frequency ...
