抄録
Barium magnesium silicate, BaMgSiO4, sintered together with H3BO3 in a reducing atmosphere is known to show photochromism, with the generation of a pink color following UV irradiation. It is thought that this photochromism originates from oxygen vacancies in the silicate. In this work, we investigated the nominal Ba-deficient composition Ba1-xMgSiO4-x (0 ≤ x ≤ 0.05) in an attempt to effectively generate oxygen vacancies in the silicate. BaMgSiO4 phases were obtained from a combination of BaCO3, MgO and SiO2, without the addition of H3BO3, by sintering in a reducing atmosphere. All samples were pink-colored after UV irradiation and this photochromism was confirmed to be an intrinsic property of BaMgSiO4. The color densities of our samples were inferior to that of a previously reported sample sintered with the addition of H3BO3, and the addition of H3BO3 is believed to improve the photochromism color density. A tendency for the color density to decrease with increasing Ba-deficiency was found among our samples. The observed degradation of the photochromism is discussed based on nonstoichiometry in the BaMgSiO4 phase.