Inferring intermediate states by leveraging the many-body Arrhenius law
Vishwajeet Kumar, Arnab Pal, Ohad Shpielberg
TL;DR
The paper addresses inferring metastable states in escape dynamics of interacting diffusive particles within deep traps by generalizing the Arrhenius law to a many-body regime, yielding $\Phi_{\mathrm{MP}} \asymp \exp[- \beta \Delta U\, g(\bar{\rho})]$ with $g(\bar{\rho})=1-U_{\rm top}(\bar{\rho})/\Delta U$. It shows that non-monotonic traps generate kinks in $g(\bar{\rho})$ that count and locate metastabilities via the MEC, and introduces a thermodynamic-like formalism with a free-energy $\mathcal{F}=-\frac{1}{\beta \Delta U}\log \Phi_{\mathrm{MP}}$ and response functions $\mathcal{R}_n$ to characterize these transitions. Finite-$\beta \Delta U$ scaling is developed using macroscopic fluctuation theory applied to the SEP, establishing observable precursors to the kinks through $\mathcal{R}_2$ and $\mathcal{R}_3$, and providing analytic and numerical support for both monotone and non-monotone traps. The approach offers a practical route to quantify underlying energy landscapes from escape statistics, with potential experimental validation in colloidal transport and biological pore translocation, and sets the stage for extensions to higher dimensions and more complex interactions.
Abstract
Metastable states appear as long-lived intermediate states in various natural transport phenomena which are governed by energy landscapes. As such, these intermediate metastable states dominate the system's dynamics at coarse grained times. Moreover, they can strongly influence the overall pathways through which the energy landscape is explored. Thus, quantifying these metastabilities is crucial for uncovering the key details of the underlying landscape. Here, we introduce a robust method based on a generalized many-body Arrhenius law to identify metastable states in escape problems involving interacting particles with excluded volume. Experimental platforms such as colloidal transport or macromolecular translocation through biological pores can offer promising settings to validate our predictions.
