The second important mechanism of plastic deformation is
twinning.
It results when a portion of crystal takes up an
orientation that is related to the orientation of the rest of the untwined
lattice in a definite, symmetrical way.
The twinned portion of the crystal is a mirror image of
the parent crystal. The plane of symmetry is called twinning plane.
Each atom in the twinned region moves by a homogeneous
shear a distance proportional to its distance from the twin plane.
The
lattice strains involved in twinning are small, usually in order of fraction of
inter-atomic distance, thus resulting in very small gross plastic deformation.
The important role of twinning in plastic deformation is
that it causes changes in plane orientation so that further slip can occur.
Twinning generally occurs when slip is restricted,
because the stress necessary for twinning is usually higher than that for slip.
Thus, some HCP metals with limited number of slip
systems may preferably twin.
Also, BCC metals twin at low temperatures because slip
is difficult.
Of course, twinning and slip may occur sequentially or
even concurrently in some cases.
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