The interpretation of cryogenic temperature friction is enhanced by th
e concurrent evaluation of the low-temperature mechanical properties o
f sliding materials. Absolute sliding stability is greatly desired but
difficult to attain in cryogenic systems. Experiments performed to in
vestigate the material factors necessary for smooth motion indicate th
at interfacial shear creep plays a key role in sliding stabilization.
Because viscous creep is typically not observed at cryogenic temperatu
res, we conclude that it is not possible to guarantee sliding stabilit
y based solely on material selection criteria.