Abstract
The energy transfer between Yb 3+ and Ho 3+ ions and the energy migration on Yb 3+ ions as a function of temperature were studied in gadolinium gallium garnet crystals doped with Yb 3+ (5%) and Ho 3+ (3%). It was found that the commonly accepted energy transfer theories do not provide a good description of the system studied. The application of several theories gives contradictory results.
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