D.D. Awschalom, M.R. Freeman
Journal of Luminescence
At high coverages and low temperatures oxygen on exfoliated graphite takes the form of a bilayer film plus bulk solid clusters. A transition at 47 K is interpreted as prewetting in which a thick film is formed. Evidence for this transition is seen in heat-capacity and magnetic-susceptibility measurements. © 1983 The American Physical Society.
D.D. Awschalom, M.R. Freeman
Journal of Luminescence
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Physical Review B
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Physical Review Letters
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