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Eu3+ probe ion for rare-earth dopant site structure in sol–gel derived LiYF4 oxyfluoride glass–ceramic
Affiliation:1. Department of Physics, University of the Free State, P.O. Box 339, Bloemfontein 9300, South Africa;2. Department of Applied Physics, Chandigarh University, Gharuan, Mohali, Punjab, 140413, India;1. Department of Energy Science, Sungkyunkwan University, Suwon 440-746, Republic of Korea;2. School of Chemical & Biological Engineering, Seoul National University, Seoul 151-744, Republic of Korea;3. Department of Materials Science and Engineering, Seoul National University, Seoul 151-742, Republic of Korea;4. Department of Materials Science and Engineering & Energy Systems Research, Ajou University, Suwon 443-749, Republic of Korea;5. Nano-Mechanical Systems Research Division, Korea Institute of Machinery and Materials (KIMM), Daejeon 305-343, Republic of Korea;6. School of Materials Science and Engineering, Kyungpook National University, Daegu 41566, Republic of Korea;7. School of Advanced Materials Science & Engineering, Sungkyunkwan University, Suwon 440-746, Republic of Korea
Abstract:Sol–gel route using metal alkoxides and trifluoroacetic acid as precursors has been used to prepare oxyfluoride glass–ceramic containing Eu3+-doped LiYF4 nanocrystals of about tens of nm size embedded in a silica matrix through controlled crystallization at higher temperatures of the xerogel. Photoluminescence spectra and decay curves recorded in the Eu3+-doped LiYF4 polycrystalline pellet and glass ceramic have been discussed using group-theoretical arguments. In the glass–ceramic Eu3+ ions are embedded dominantly inside the LiYF4 nanocrystals most probably as Eu–O center and/or dimer centers in low symmetry (C2v) sites; oxygen ions were incorporated in their neighborhood during the glass ceramization.
Keywords:Sol–gel  Glass ceramic  Nanocrystals  Photoluminescence
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