Thermoluminescence of forsterite and fused quartz as a candidate for the extended red emission
Citation
Koike, C., Chihara, H., Koike, K., Nakagawa, M., Okada, M., Tsuchiyama, A., ... & Atobe, K. (2002). Thermoluminescence of forsterite and fused quartz as a candidate for the extended red emission. Meteoritics & Planetary Science, 37(11), 1591-1598.Publisher
The Meteoritical SocietyJournal
Meteoritics & Planetary ScienceAdditional Links
https://meteoritical.org/Abstract
Thermoluminescence of silicates interesting in interstellar and circumstellar medium after irradiation of gamma-rays and fast neutron is investigated in detail. The silicates are forsterite, orthoenstatite, olivine, quartz, and crystalline silicon. The irradiated enstatite shows weak and broad peaks at 545 and 760 nm. On the contrary, irradiated bulk and powder samples of forsterite show strong and broad peak at 640-660 nm. Although thermoluminescence of bulk-forsterite is very similar to ERE of Red Rectangle, iradiated powdered-forsterite did not reveal any sharp emission features over broad band. Further, possibility of thermoluminescence of crystalline silicon is investigated, which luminescence scarcely appears. It is emphasized that the prominent carrier of ERE is forsterite and fused quartz.Type
Articletext
Language
enISSN
1945-5100ae974a485f413a2113503eed53cd6c53
10.1111/j.1945-5100.2002.tb00813.x