Near
the interface of two contacting metallic bodies in relative
motion, the microstructure changes. This modified microstructure leads
to changes in material properties and thereby influences the tribological
behavior of the entire contact. Tribological properties such as the
friction coefficient and wear rate are controlled by the microstructure,
while the elementary mechanisms for microstructural changes are not
sufficiently understood. In this paper, the influence of the normal
load and the size of the counter body on the initiation of a tribologically
induced microstructure in copper after a single sliding pass is revealed.
A systematic variation in the normal load and sphere diameter resulted
in maximum Hertzian contact pressures between 530 MPa and 1953 MPa.
Scanning electron microscopy, focused ion beam, and transmission electron
microscopy were used to probe the subsurface deformation. Irrespective
of the normal load and the sphere diameter, a sharp line-like feature
consisting of dislocations, the so-called dislocation trace line,
was identified in the subsurface area at depths between 100 nm and
400 nm. For normal loads below 6.75 N, dislocation features are formed
below this line. For higher normal loads, the microstructure evolution
directly underneath the surface is mainly confined to the area between
the sample surface and the dislocation trace line, which itself is
located at increasing depth. Transmission Kikuchi diffraction and
transmission electron microscopy demonstrate that the misorientation
is predominantly concentrated at the dislocation trace line. The results
disclose a material rotation around axes roughly parallel to the transverse
direction. This study demonstrates the generality of the trace line
phenomena over a wide range of loads and contact pressures and the
complexity of subsurface processes under a sliding contact and provides
the basis for modeling the early stages in the microstructure evolution.