Abstract
ESR spectra of KBrO4 crystals irradiated with x rays at 10 or 26°K contain three ``families'' of intense signals. The signals observed at 10°K are assumed to derive from primary defects constituted by electrons and holes trapped on BrO4− ions. The families of signals are assigned to the species BrO4−, BrO4, and (BrO4)2−, each trapped in a number of distinct sites. Thermal processes starting at 20°K result in formation of the secondary defects O3− from BrO4−, and BrO2 from BrO4.

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