D.D. Awschalom, K.W. Schwarz
Physical Review Letters
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, K.W. Schwarz
Physical Review Letters
D.D. Awschalom, J. warnock
IEEE Transactions on Magnetics
M. Kohl, D.D. Awschalom
Journal of Applied Physics
Alex Harwit, M.B. Ritter, et al.
Applied Physics Letters