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Using the pulse radiolysis method, the effects of repeated pulses on the slowly-decaying components of et− in an ice crystal after a pulse, have been studied around 100°K and the effect of warming the sample after an intense irradiation. The trap of the stabilized electron is produced by the electron irradiation. The radiation-produced traps disappear on warming to 150°K. An ESR signal of et− in irradiated-crystalline ice is detected. Possible kinds of the trap are discussed. The experimental results are explained by assuming the trap is a radiation-produced vacancy of a water molecule at the lattice.
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Keisuke Kawabata (1976) studied this question.
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