The interest in blue iron minerals as pigments for painting was greatly enlarged in the early tenth century A.D. with the use of vivianite, which in
medieval Europe became a suitable alternative to the very expensive commodity imported from Afghanistan—lapis lazuli or lazurite, with general
formula (Na, Ca)4(AlSiO4)3(SO4, Cl, S). This mineral is a member of the ultramarines, a family of closely
related pigments based on the framework structure of sodalite [1] and whose blue color is due to the presence of sulfur polyanions
(S3−) partially replacing sulfate or chloride anions in cages within the tetrahedral aluminous-silicate framework. Conversely,
vivianite—a mineral with ideal formula Fe3(PO4)2·8H2O — owes its diagnostic indigo-blue color
to intervalence charge transfer (IVCT) between iron ions filling dimers of edge-sharing octahedra in the crystal structure.
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