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Luminescence as an indication of distortion in A3+2 B4+2 O7 type pyrochlores
Authors:RA McCauley  FA Hummel
Institution:Ceramic Science Section, Department of Material Sciences, The Pennsylvania State University, University Park, Penna 16802, U.S.A.
Abstract:The Eu3+ luminescent emission spectra of rare-earth titanate, titanate-stannate, stannate, hafnate and zirconate pyrochlores, A3+2B4+2O7, indicated that a linear relationship existed between the splitting of the 5D07F1 magnetic-dipole transition and the size of the cation present. Small A3+ cations and larger B4+ cations both produced a lattice with a lesser degree of deviation from Oh symmetry.
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