The thermal transformations in phosphorites during flash calcination w
ere investigated by FT-IR spectroscopy, X-ray diffraction and chemical
analyses. During flash calcination changes occur, both in the composi
tion of the phosphorite and in the crystallochemistry of the fluor-car
bonate-apatite (francolite). The former changes include: decomposition
of a great part of the calcite in the rock and oxidation of organic m
atter. The latter changes include: partial removal of the structural c
arbonate; partial relocation of the remaining carbonate ions in the ap
atite structure; a new arrangement of hydroxyl groups and fluorine on
the hexagonal axis; partial condensation of the orthophosphate groups
and increase of crystallite sizes. Isomorphous substitution of PO4-3 i
n apatite by SO4-2 and SiO4-4 may take place.