Complex stress potential for antiplane shear 2026-10-14
A harmonic conjugate satisfying and makes a holomorphic function. Its derivative packages the two antiplane shear stresses into the displayed complex field. On multiply connected domains a global potential additionally requires the appropriate periods to vanish; prescribed displacement jumps can instead be represented by branches of the potential.
Past exam of the mathematics course of the University of Cambridge 2003 iii Paper 70 4 a Solution Created 2026-10-03 Updated 2026-10-14
For antiplane shear, the only nonzero infinitesimal strains are and . Their trace is zero. The isotropic constitutive law consequently giveswith every other component zero. The first two equations of motion vanish because the fields are independent of . The third is , henceThe PDF omits the final equals-zero; this is the equation supplied by momentum balance.
For a steadily moving field put and . In the subsonic case , the equation becomes . With it reduces to . Thus is a harmonic function and, on a simply connected region, has a harmonic conjugate; there is a holomorphic function such thatThis is steadily moving antiplane shear. The representation is local on more general domains unless the conjugate's periods vanish. The subsonic condition is essential: at or above the shear-wave speed the coordinate rescaling is degenerate or the equation is hyperbolic rather than this elliptic harmonic problem.
Past exam of the mathematics course of the University of Cambridge 2004 iii Paper 72 4 Solution 2026-10-14
For antiplane shear, the infinitesimal displacement is . The isotropic linear elasticity constitutive law gives and , together with the symmetric entries . All other stress tensor components vanish. Static force balance without body force becomes , so satisfies the Laplace equation.
Locally choose a harmonic conjugate by and . Compatibility follows from the Laplace equation. These are the Cauchy-Riemann equations for , and henceThus the complex stress potential for antiplane shear supplies both stresses and, by integration, the displacement. A global potential must have the displacement periods appropriate to the cracked body; these periods also help fix homogeneous solutions.
For the additional crack-induced field, set and . Only loads the prospective faces, since is tangential to their normal. Denote upper and lower boundary values by . The imposed cancellation of face tractions is . The traction data and geometry are invariant under the displacement reflection . For the induced correction with no independently added loading, uniqueness up to a rigid translation allows the odd displacement choice. Then is even, is odd, and on the real axis. Therefore the Hilbert problem for an antiplane crack isThe second condition expresses continuation through uncracked material. There is real and the additional vanishes. This scalar Riemann-Hilbert problem is supplemented by at most inverse-square-root stress singularities at the crack tips and the usual correction with no additional remote resultant or imposed dislocation. Without a far-field or period normalization, the face conditions alone permit homogeneous terms. The formulas below select this normalized induced field and explicitly identify the excluded terms.
Steadily moving antiplane shear 2026-10-14
For subsonic motion , an antiplane shear displacement satisfies . The displayed rescaling makes it a harmonic function of , so locally for a holomorphic function . Set . The Cauchy-Riemann equations then give . Keeping this potential normalization explicit avoids losing a factor of in the dynamic stress field. At sonic or supersonic speeds the elliptic harmonic reduction does not apply.