D.D. Awschalom, J.M. Hong, et al.
Surface Science
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, J.M. Hong, et al.
Surface Science
G.N. Lewis, D.D. Awschalom, et al.
Physical Review B
J. Warnock, D.D. Awschalom, et al.
Physical Review Letters
M.B. Ketchen, D.D. Awschalom, et al.
IEEE Transactions on Magnetics