3. Flow kinematics
This section presents a detailed discussion of the different distortion measures that form the geometrical backbone of the CPFE framework. The review is given in terms of finite deformation measures as the small distortion case can always be derived from it. The kinematics of isothermal finite deformation describes the process where a body originally in a reference state (or “configuration”), B ⊂ R3, is deformed to the current state, S ⊂ R3, by a combination of externally applied forces and displacements over a period of time, Δt. In this treatment we choose the perfect single crystal as reference state. Other possible choices of a reference state would be the state just before deformation, or in an incremental formulation, the state at any time t. The latter has the disadvantage of a constantly changing reference state while the former might contain an undefined amount of crystal defects.
In crystal plasticity one has to distinguish three coordinate systems. The shape coordinate system is a curvilinear system, based on the physical shape of the body, which deforms congruently with the total changes in shape occurring during deformation. In contrast, the lattice coordinate system has coordinate axes fixed locally parallel to the crystallographic directions, i.e. the nodes of the coordinate network maintain a one-to-one correspondence with crystal lattice points during deformation except where singularities in the atomic array occur due to the defect cores. Therefore, the space defined by the deformed lattice coordinate system is connected to ordinary Euclidean space by functions that depend on the defect content and distribution [235]. The distinction between shape and lattice distortion is critical when internal stresses are to be calculated [236]. Since these stresses arise from internal reaction forces generated when atoms experience a relative displacement from their equilibrium positions, they can only be related to lattice deformations because shape deformations do not necessarily follow the deformation of the underlying crystal lattice. Deformations in the two types of coordinates are coincident only when no motion of crystal defects occurs, which is the usual assumption made for calculating elastic stresses from measurements of the small deformations of a coordinate system deposited on the surface or embedded within a body. Finally, it is often convenient to describe the deformations of the overall shape of a body and its associated lattice in terms of a third reference system, laboratory coordinates, that does not deform with the body. Computations of the deformation of both shape and lattice coordinate systems can be made in terms of their components in laboratory coordinates. This has the practical advantage of providing a reference system that is fixed throughout the deformation of the body.
To cast this in a formal way we represent the positions of neighboring material points relative to an arbitrary origin in the reference configuration by the vector dx. As a result of deformation, this vector is mapped into its image in the current configuration, dy =dx+du, where du is the differential total displacement vector. These vectors are related by the total, or shape, deformation gradient, F: