State estimation of the Stefan PDE: A tutorial on design and applications to polar ice and batteries

The Stefan PDE system is a representative model for thermal phase change phenomena, such as melting and solidification, arising in numerous science and engineering processes. The mathematical description is given by a Partial Differential Equation (PDE) of the temperature distribution defined on a spatial interval with a moving boundary, where the boundary represents the liquid–solid interface and its dynamics are governed by an Ordinary Differential Equation (ODE). The PDE–ODE coupling at the boundary is nonlinear and creates a significant challenge for state estimation with provable convergence and robustness.

This tutorial article presents a state estimation method based on PDE backstepping for the Stefan system, using measurements only at the moving boundary. PDE backstepping observer design generates an observer gain by employing a Volterra transformation of the observer error state into a desirable target system, solving a Goursat-form PDE for the transformation’s kernel, and performing a Lyapunov analysis of the target observer error system.

The observer is applied to models of problems motivated by climate change and the need for renewable energy storage: a model of polar ice dynamics and a model of charging and discharging in lithium-ion batteries. The numerical results for polar ice demonstrate a robust performance of the designed estimator with respect to the unmodeled salinity effect in sea ice. The results for an electrochemical PDE model of a lithium-ion battery with a phase transition material show the elimination of more than 15 % error in State-of-Charge estimate within 5 min even in the presence of sensor noise.