Natural The mineral
millerite is also a nickel sulfide with the molecular formula NiS, although its structure differs from synthetic stoichiometric NiS due to the conditions under which it forms. It occurs naturally in low temperature hydrothermal systems, in cavities of carbonate rocks, and as a byproduct of other nickel minerals. crystals In nature, nickel sulfides commonly occur as solid solutions with iron sulfides in minerals such as
pentlandite and
pyrrhotite. These minerals have the formula Fe9−xNixS8 and Fe7−xNixS6, respectively. In some cases they are high in nickel (larger values of x).
In glass manufacturing Float glass contains a small amount of nickel sulfide, formed from the sulfur in the fining agent and the nickel contained in metallic alloy contaminants. Nickel sulfide inclusions are a problem for
tempered glass applications. After the tempering process, nickel sulfide inclusions are in the metastable alpha phase. The inclusions eventually convert to the beta phase (stable at low temperature), increasing in volume and causing cracks in the glass. In the middle of tempered glass, the material is under
tension, which causes the cracks to propagate and leads to spontaneous glass fracture. That spontaneous fracture occurs years or decades after glass manufacturing. ==References==