State Estimation of the Stefan PDE: A Tutorial on Design and Applications to Polar Ice and Batteries
Shumon Koga, Miroslav Krstic

TL;DR
This paper introduces a PDE backstepping observer for the Stefan PDE system, enabling accurate state estimation of phase change phenomena like ice melting and battery charge levels using boundary measurements.
Contribution
It develops a novel PDE backstepping observer design for nonlinear PDE-ODE coupled systems with moving boundaries, demonstrated on climate and battery models.
Findings
Robust state estimation for polar ice models despite salinity effects.
Over 15% reduction in State-of-Charge error within 5 minutes in battery models.
Effective boundary measurement-based estimation for phase change systems.
Abstract
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…
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Taxonomy
TopicsFreezing and Crystallization Processes
