Uniqueness of solutions in high-energy x-ray based `eigenstrain tomography' and other inverse eigenstrain problems: Counter examples and necessary conditions for well-posedness
Christopher Wensrich, Sean Holman, William Lionheart, Matias Courdurier, Roxanne Jackson
TL;DR
The paper analyzes the uniqueness of eigenstrain tomography for reconstructing 3D residual stress from diffraction data in isotropic solids. It shows that using a single measured component yields non-unique solutions, but that three independent components (diagonal or shear) can enforce a unique full elastic strain/stress field under equilibrium and zero-traction conditions. It proves that any residual stress field can be represented by a diagonal eigenstrain and that some fields cannot be generated by isotropic eigenstrains, implying that restricting to hydrostatic eigenstrains is not robust. Together, these results define rigorous minimal experimental and computational requirements for well-posed inverse eigenstrain problems and inform practical strategies for eigenstrain tomography.
Abstract
Eigenstrain tomography combines diffraction-based strain measurement with elasticity theory to reconstruct full three-dimensional residual stress fields within solids. Notwithstanding a number of recent examples, the uniqueness of such reconstructions has not yet been clearly established. In this paper, we examine the underlying inverse problem in detail and construct explicit counterexamples demonstrating non-uniqueness for a recent implementation of x-ray eigenstrain tomography involving reconstruction from a single measured component of strain. We follow on to explore minimum conditions for well-posedness and conclude that the full elastic strain tensor within an isotropic sample can be uniquely reconstructed from three measured components; specifically the three shear components, or the three diagonal components. We further prove two key results related to eigenstrain reconstruction in a general sense; 1. That any possible residual stress field can be generated by a diagonal eigenstrain and 2. That residual stress fields exist that cannot be generated by isotropic eigenstrains. Together, these findings establish rigorous minimum experimental and computational requirements for well-posed eigenstrain tomography techniques and inverse eigenstrain problems in general.
