The characteristics of the deformation bands (DBs), formed in cyclically de
formed copper single crystals with various orientations, were summarized sy
stematically. The Formation mechanism of DBs was also explored. It was show
n that the apperance of DBs seems to be a general phenomenon in cyclically
deformed copper single crystals with various slip orientations, especially
with double- or multiple-slip orientations, for which the critical plastic
strain amplitude needed for the formation of DBs is rather low (about 10(-3
)). The DB denoted by DBI develops roughly along the primary slip plane {11
1}, and the habit piano of DBII is close to the conventional kink plane {10
1}. The habit planes of DBI and DBII are strictly perpendicular to each oth
er. An analysis based on the crystallographic deformation geometry showed t
hat the local irreversible rotation of crystal which exists during symmetri
cal push-pull loading may be responsible for the Formation of DBI and DBII.
When a certain crystallographic geometrical condition is satisfied, DBI an
d DBII are very hard to form coincidentally. In addition, a favourable macr
oscopic state of stress might also be responsible for the occurrence of oth
er types of DB, such as (001) DB in the [011] crystal. Finally, the disloca
tion structure relevant to DBs was observed tentatively by electron channel
ling contrast in scanning electron microscopy. It was revealed that the DBs
formed in copper single crystals during cyclic straining may exhibit quite
different microstructures, depending upon the crystallographic orientation
.