Abstract

A luminescence study of the Y 3Al 5O 12:Mn 4+ system is presented. Luminescence is due to 2E → 4A 2 transitions on Mn 4+ ions which substitute for Al 3+ ions in distorted octahedral sites. The technique of fluorescence line narrowing (FLN) is used to interrogate some of the details of this transition. The zero-phonon R lines are found to be a composite of transitions from Mn 4+ ions in different sites, the strongest line coming from Mn 4+ ions in regular Al 3+ sites. The ratio of R line to sideband in the emission from Mn 4+ ions in these regular sites is found to be unusually low, and this is taken as an indication of an ion-lattice coupling for the Mn 4+ ion which is significantly stronger than for the case of the Cr 3+ ion in Y 3Al 5O 12. Measurements of the luminescence decay rates as a function of temperature are given and we attempt to relate these data to models for nonradiative processes.

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