Ionic Adsorption Clay

Ionic Clay+ 4 related classifications

Ionic adsorption clays are formed by the weathering of rare-earth-rich granite rocks in subtropical climates. The rare earth elements are adsorbed onto the surface of clay minerals. They are the world's primary source of Heavy Rare Earths (HREEs) and are mined extensively in Southern China and developing in Brazil.

Processing

DifficultyLow

Processing & Metallurgy

Simplest processing: In-situ or heap leaching with an electrolyte solution (like ammonium sulfate) desorbs the rare earths without needing to dissolve the rock. However, environmental management of the leachate is critical.

Related Projects

5 Found

Processing Facilities

3 Found

Facilities receiving feedstock from Ionic Adsorption Clay mining projects.

Typical Composition

The set of elements typically dominant in Ionic Adsorption Clay deposits.