The polar decomposition in continuum mechanics and material isotropy remove the reference rotation from an elastic Cauchy stress tensor. Half-turns around principal stretch axes leave the diagonal left stretch tensor fixed, so material frame indifference forces the stress's off-diagonal entries to vanish in those axes. Rotations within repeated-stretch eigenspaces also force isotropic stress there. Consequently stress and the left Cauchy-Green deformation tensor are coaxial symmetric tensors.
Let , and . Differentiating the deformation gives
For the neo-Hookean solid, . The constrained nominal stress tensor is therefore . The multiplier cannot be set arbitrarily to a constant; equilibrium and the traction-free curved surface determine it.
Push the nominal stress to the Cauchy stress tensor: since , . In the current cylindrical orthonormal basis, the left Cauchy-Green deformation tensor has entries
Thus , , and . Static radial equilibrium without body force gives
The current outer radius is . Setting integrates the reaction field:
The other curved-surface traction components vanish because .
On the reference end , the outward reference normal is , and the nominal traction has components . The third row of is . Hence the nominal end traction of a twisted neo-Hookean cylinder is
The current here are evaluated at . These components are per unit reference area, not per unit current area.
For the moment, use current lever arms and reference-area traction. Its axial component is
The axial traction gives no axial moment. This torque also agrees with the reference-energy derivative at fixed axial stretch: the twist-dependent energy per reference length is . It is important that is twist per reference length, not twist per current length.
Use both material isotropy and material frame indifference. The polar decomposition in continuum mechanics writes , where is the left stretch tensor. Isotropy removes the reference rotation: . Choose an orthonormal eigenbasis of . A half-turn about any principal axis leaves fixed but reverses appropriate off-diagonal entries of . Frame indifference therefore makes those entries zero. If a principal stretch is repeated, rotations in its eigenspace additionally force the stress to be isotropic there. Thus the principal stresses share the stretch axes: this proves coaxiality of isotropic elastic stress with and with .
For simple shear, the left Cauchy-Green deformation tensor is
Its principal axes make an angle with the coordinate axes satisfying when . If the two principal stresses are , rotating their diagonal matrix back gives
Consequently the universal simple-shear normal-stress identity is
Equivalently, it follows immediately from the off-diagonal entry of . At , the undeformed material has isotropic stress, so the identity holds there too. No particular elastic constitutive equation has been used.
Figure 1.
Principal stress and stretch axes of an isotropic elastic material under simple shear
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