Q. Jiang et Mf. Beatty, On compressible materials capable of sustaining axisymmetric shear deformations. Part 4: Helical shear of anisotropic hyperelastic materials, J ELAST, 62(1), 2001, pp. 47-83
Conditions on the form of the strain energy function in order that homogene
ous, compressible and isotropic hyperelastic materials may sustain controll
able static, axisymmetric anti-plane shear, azimuthal shear, and helical sh
ear deformations of a hollow, circular cylinder have been explored in sever
al recent papers. Here we study conditions on the strain energy function fo
r homogeneous and compressible, anisotropic hyperelastic materials necessar
y and sufficient to sustain controllable, axisymmetric helical shear deform
ations of the tube. Similar results for separate axisymmetric anti-plane sh
ear deformations and rotational shear deformations are then obtained from t
he principal theorem for helical shear deformations. The three theorems are
illustrated for general compressible transversely isotropic materials for
which the isotropy axis coincides with the cylinder axis. Previously known
necessary and sufficient conditions on the strain energy for compressible a
nd isotropic hyperelastic materials in order that the three classes of axis
ymmetric shear deformations may be possible follow by specialization of the
anisotropic case. It is shown that the required monotonicity condition for
the isotropic case is much simpler and less restrictive. Restrictions nece
ssary and sufficient for anti-plane and rotational shear deformations to be
possible in compressible hyperelastic materials having a helical axis of t
ransverse isotropy that winds at a constant angle around the tube axis are
derived. Results for the previous case and for a circular axis of transvers
e isotropy are included as degenerate helices. All of the conditions derive
d here have essentially algebraic structure and are easy to apply. The gene
ral rules are applied in several examples for specific strain energy functi
ons of compressible and homogeneous transversely isotropic materials having
straight, circular, and helical axes of material symmetry.