arXiv · 2609.06026
A globally defined polyconvex isotropic energy satisfying the true-stress-true-strain monotonicity condition (TSTS-M++)
Abstract
Polyconvexity is a standard ingredient in the variational existence theory of finite elasticity, whereas true-stress-true-strain monotonicity (TSTS-M++) requires a positive incremental Cauchy-stress response. These two constitutive restrictions are independent, and Wollner, Holzapfel and Neff left open whether a compressible isotropic energy defined on the whole of $\mathrm{GL}^{+}(3)$ can satisfy both. We give an explicit affirmative answer. For every $\mu>0$ and $k>0$, the stored-energy function $W_k(F)=\frac{\mu}{2k}\bigl[\exp\bigl(k(\lVert F\rVert^2+3J^{-1}+J-7)\bigr)-1\bigr]$, $J=\det F$, is polyconvex and strictly rank-one convex. Its Cauchy-stress response satisfies TSTS-M++ globally if and only if $k\ge 1/(8\sqrt{3})$. In this regime every symmetric Cauchy stress corresponds to a unique positive-definite stretch, while the reference stretch is stress free with positive infinitesimal shear and bulk moduli. Stress bijectivity has the strictly smaller sharp threshold $k_{\mathrm{B}}\approx 0.00827233304$: at equality the stress map is a global homeomorphism with a nondifferentiable inverse, and above it the map is a global $C^{\infty}$ diffeomorphism. Thus, for $k_{\mathrm{B}}\le k<1/(8\sqrt{3})$, the map $V\mapsto\sigma(V)$ remains globally bijective while TSTS-M++ fails at finite strain. In the TSTS-M++ regime, every prescribed inner radius of a finite plane-strain annulus with a traction-free outer wall has a unique radial equilibrium, and its inner pressure increases smoothly and strictly from zero to infinity.
Explore related subjects
Keep this discovery
Dongxin Bai, Yunhao Wu, Yong Li, Kai Zhang, Patrizio Neff. 2026-09-05. A globally defined polyconvex isotropic energy satisfying the true-stress-true-strain monotonicity condition (TSTS-M++). https://arxiv.org/abs/2609.06026
Cite the original work for its findings. Save a collection to share your selection of sources.