Abstract
Pale green and purple jadeites have been studied by a microscope spectrophotometric method. Absorption and photoluminescence spectra of these jadeites revealed that the green and purple colors were attributed to the existence of Fe3+ and Ti3+ ions in the octahedral site, respectively. The crystal-field parameters of these ions were successfully obtained. Fe3+ parameters derived from five absorption bands were: Dq=1290cm−1, B=566cm−1, C=3470cm−1. Ti3+ had a broad absorption band of 70nm, full width at half maximum (fwh) with a peak at 545nm and a crystal-field splitting of Dq=1840cm−1. Fe3+ gave rise to a broad emission band (81 nm fwh) with a peak at 796nm, while Ti3+ did not give luminescent centers in the infrared region. These facts support that both ions occupy the octahedral site.