This article provides an overview on the inorganic chemistry of cadmium. Cadmium is a bluish-white metal, the 67th most abundant element in the Earth's crust, and found in some minerals. The structure of the stable form at room temperature ( form) is hexagonal. Occurrence, production, and applications have been surveyed. CdII forms relatively few minerals: the most important are two sulfides, greenockite, and hawleyite. CdII, however, gives isomorphous replacement in several Zn minerals. For this reason, sphalerite (ZnS) is the main industrial source of cadmium. The metal is mainly obtained as a by-product of the metallurgy of Zn. Cadmium and its compounds find applications in several industrial materials: electrode materials in Ni–Cd batte...