Lably
Skip to content

Cuprospinel

Copper iron mixed oxide mineral

  • 6 min read
  • 3 chapters

Related on Lably

Through Mineral, Copper and Iron

The type locality of cuprospinel is Baie Verte, Newfoundland, Canada, where the mineral was found in an exposed ore dump. The mineral was first characterized by Ernest Henry Nickel, a mineralogist with the Department of Energy, Mines and Resources in Australia, in 1973. Cuprospinel is also found in other places, for example, in Hubei province, China and at Tolbachik volcano in Kamchatka, Russia.

Properties

Structural

Cuprospinel, like many other spinels has the general formula AB2O4. Yet, cuprospinel is an inverse spinel in that its A element, in this case copper (Cu2+), only occupies octahedral sites in the structure and the B element, iron (Fe2+ and Fe3+), is split between the octahedral and tetrahedral sites in the structure. The Fe2+ species will occupy some of the octahedral sites and there will only be Fe3+ at the tetrahedral sites. Cuprospinel adopts both cubic and tetragonal phases at room temperature, yet as temperature is elevated the cubic form is most stable.

Magnetic

CuFe2O4 nanoparticles have been characterized as a superparamagnetic material with saturated magnetization of Ms = 49 emu g−1, remanent magnetization (Mr = 11.66 emu g−1) and coercivity (Hc = 63.1 mT). The magnetic properties of CuFe2O4 are correlated with the size of particles. Particularly, the decreasing in saturated magnetization and remanence correspond to the decreasing in the size of CuFe2O4 particles, whereas the coercivity increases.

Sign in to keep reading

2 more chapters are free with a Lably account.

More in Energy