Abstract
ELECTRON spin resonance spectra obtained here for single crystals of ice, γ-irradiated and measured at 77° K, show structure not previously reported for the resonance near g = 2, which is generally assumed to be due to OH radicals. Earlier work by other authors has been directed mainly to the investigation of polycrystalline ice1, except for a report2 giving results on single crystals rather different from those reported here, and a recent communication3 published near the end of these preliminary experiments.
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References
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DIBDIN, G. New Structure in the Electron Spin Resonance Spectrum of γ-irradiated Single Crystals of Ice. Nature 209, 394–395 (1966). https://doi.org/10.1038/209394a0
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DOI: https://doi.org/10.1038/209394a0
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