Implicit-explicit time integration method for fractional advection-reaction-diffusion equations

TL;DR

This paper introduces a new implicit-explicit adaptive time integration method for fractional advection-reaction-diffusion equations, improving stability and efficiency for complex subdiffusive flow simulations.

Contribution

The paper develops a novel $ heta$-method that generalizes existing explicit and implicit schemes, with spectral analysis and efficient solvers tailored for fractional PDEs.

Findings

Method accurately simulates 2D fractional diffusion.

Effectively captures viscoelastic flow macrostructures.

Shows stability and efficiency in subdiffusive flow modeling.

Abstract

We propose a novel family of asymptotically stable, implicit-explicit, adaptive, time integration method (denoted with the $\theta$-method) for the solution of the fractional advection-diffusion-reaction (FADR) equations. This family of time integration method generalized the computationally explicit $L_1$-method adopted by Brunner (J. Comput. Phys. {\bf 229} 6613-6622 (2010)) as well as the fully implicit method proposed by Jannelli (Comm. Nonlin. Sci. Num. Sim., {\bf 105}, 106073 (2022)). The spectral analysis of the method (involving the group velocity and the phase speed) indicates a region of favorable dispersion for a limited range of Peclet number. The numerical inversion of the coefficient matrix is avoided by exploiting the sparse structure of the matrix in the iterative solver for the Poisson equation. The accuracy and the efficacy of the method is benchmarked using (a) the two-dimensional (2D) fractional diffusion equation, originally proposed by Brunner, and (b) the incompressible, subdiffusive dynamics of a planar viscoelastic channel flow of the Rouse chain melts (FADR equation with fractional time-derivative of order $\alpha=\nicefrac{1}{2}$) and the Zimm chain solution ($\alpha=\nicefrac{2}{3}$). Numerical simulations of the viscoelastic channel flow effectively capture the non-homogeneous regions of high viscosity at low fluid inertia (or the so-called `spatiotemporal macrostructures'), experimentally observed in the flow-instability transition of subdiffusive flows.