Meaning
Plastic deformation occurs when crystal layers slide over one another along the primary horizontal plane. The occurrence of basal slip is the dominant mechanism for permanent shape change in hexagonal close packed structures. It represents the easiest path for atoms to move under shear stress.
Shear Threshold
Movement begins only when the resolved shear stress reaches a specific magnitude known as the critical value. In materials where basal slip is the primary mode of movement, the energy required to initiate deformation is lower than in other systems. This threshold determines the maximum load a component can handle before its geometry is permanently altered.
Atomic Displacement
Layers of atoms shift across the base plane of the unit cell without breaking the overall continuity of the lattice. When basal slip happens, the crystal effectively lengthens or flattens depending on the direction of the applied force. The lack of alternative slip systems in certain minerals makes this process highly directional.
Mechanical Hardening
Resistance to further deformation increases as dislocations accumulate along the sliding planes. While basal slip allows for initial ductility, it eventually leads to work hardening as the moving parts of the lattice encounter grain boundaries. Engineers measure this demonstrated rate to ensure that the material capability meets the requirements of the final application.