Ch. 7 - Dislocations and Strengthening Mechanisms Flashcards
Edge dislocation
Localized lattice distortion exists among the end of an extra half-plane of atoms, which also defines the dislocation line.
Screw dislocation
Results from a shear distortion; its dislocation line passes through the center of a spiral, atomic plane ramp.
Slip
Process by which plastic deformation is produced by dislocation motion. Permanent plastic deformation results from the movement of dislocations in response to an applied shear stress.
Slip plane
Crystallographic plane alone which the dislocation line traverses.
Dislocation density
The total dislocation length per unit volume, of the number of dislocations that intersect a unit area of a random section.
10e3 for carefully molded crystals. 10e9 for heavily deformed metals. 10e5 for heat treated metals. 10e2 for ceramic materials. 0.1 for single silicon crystals used in integrated circuits.
Lattice strain
Atomic lattice distortion exists around the dislocation line because of the extra half-plane of atoms. As a consequence, there are regions in which compressive, tensile, and shear lattice strains are imposed on the neighboring atoms.
Compressive strain above extra half-plane.
Tensile strain below extra half-plane.
Slip plane
The preferred plane alone which slip occurs. This is the plane with the densest atomic packing.
Slip direction
The direction of skip movement. This direction corresponds to the direction that is most closely packed with atoms in the most densely packed plane (ie: this direction has the highest linear density).
Slip system
The combination of the slip plane and slip direction.
Burger’s vector
This vector’s direction corresponds to a dislocation’s slip direction and its magnitude depends on the crystal structure.
Resolved shear stresses
Edge, screw, and mixed dislocations move in response to shear stresses applied along the slip plane in the slip direction. Shear components exist at all alignments to the stress direction except parallel and perpendicular. These shear components are known as resolved shear stresses. Their magnitude depends on the applied stress and the orientation of both the slip plane and slip direction within the plane.
TR = (stress)cos(phi)cos(lambda)
Phi: angle between the normal vector of the slip plane and the direction of the force.
Lambda: angle between the slip and stress directions.
Critical resolved shear stress
In response to some tensile or compressive stress, slip in a single crystal commenced on the most favorably oriented slip system when the resolved shear stress reaches some critical value. This value is the minimum shear stress required to initiate slip, and is a property of the material that determines when yielding occurs.
Yield stress = Critical resolved shear stress / (cos(phi)*cos(lambda))max
Slip lines
For a single crystal in tension, slip will occur along a number of equivalent and most favorably oriented planes and directions at various positions along the specimen length. Forms small steps on the surface of the single crystal that re parallel to one another and loop around the circumference of the specimen. Each step results from the movement of a large number of dislocations along the same slip plane.
HCP, BCC, and FCC slip systems
HCP have few slip systems. This is why HCP metals are more brittle. No more than 6 slip systems.
FCC and BCC have a lot of slip systems. This is why FCC and BCC metals are so ductile. At least 12 slip systems.
Plastic deformation of polycrystalline materials
Random crystallographic orientations of grains means that slip varies from one grain to the next. Dislocation motion occurs along slip system that has most favorable orientation.
During dislocation, grain boundaries do not usually come apart. Therefore, each individual grain is constrained in its distortion by neighboring grains. Grains usually go from equiaxial to stretched out.
Polycrystalline materials are stronger than single-crystal equivalents, so it takes more stress to initiate slip. Even though a single grain may be orientated favorably for slip, adjacent grains may not be.