X-ray diffraction refinement of the crystal structure of eosphorite ha
s been carried out with reference to the orthorhombic space group Cmca
. The structure is similar to that previously described by Hanson (196
0), but the standard deviations are improved. Optical absorption and p
hotoluminescence have also been studied for this mineral. Two sharp em
ission lines, denoted as R1 and R2, superimposed to a broad band (630-
750 nm) have been related to the presence of Cr3+ ions. The excitation
spectrum of these emissions confirms that the absorption (excitation)
bands centred at 431 nm and 585 are related to with 4A2 --> 4T1 and 4
A2 --> 4T2 spin allowed transitions of this ion.