Field‐assisted ion exchange of protons in type III silica for Cs or Nu ions from a molten salt was investigated. Although electrolysis occurred, infrared measurements showed no change in hydroxyl content after ion exchange for extended periods. Scanning electron microprobe studies of cesium‐exchanged specimens revealed a high‐cesium‐content layer =2,μm thick; this layer is believed to result from surface reaction with the molten salt.
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Leil et al. (1984) studied this question.
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