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Research Article | Open Access

Stability and decay analysis of stress-diffusive viscoelastic rate fluids

Xi Wang1Xueli Ke2( )
School of Mathematics, Northwest University, Xi'an 710127, China
School of Mathematics and Information Science, Henan Polytechnic University, Jiaozuo 454000, China
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Abstract

This paper focused on a class of three-dimensional incompressible viscoelastic rate-type fluids with stress diffusion. To simplify the analysis, we considered a model where the elastic stress was spherical. It is worth noting that while the existence of solutions for such fluids has been studied, their stability properties remain largely unexplored. So inspired by [1], this paper employed the bootstrap argument, the Schonbek's method, and repeated use of Besov space properties to prove, for the first time, stability of the solution under some additional conditions on the initial data — but without further smallness restrictions. Our results showed that the velocity decays faster than the typical algebraic rate, while the spherical component of the elastic strain tensor exhibited global exponential decay. Finally, using the decay rates, we derived the stability result for any given globally smooth solution—namely, that a sufficiently small perturbation yielded a unique globally smooth solution which stayed close to the original reference solution. We thereby extended the analysis of [1] on inhomogeneous Navier-Stokes equations to a viscoelastic fluid with stress diffusion.

CLC number: 76A15, 35Q35, 35D30

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AIMS Mathematics
Pages 26187-26236

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Cite this article:
Wang X, Ke X. Stability and decay analysis of stress-diffusive viscoelastic rate fluids. AIMS Mathematics, 2025, 10(11): 26187-26236. https://doi.org/10.3934/math.20251153

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Received: 18 September 2025
Revised: 30 October 2025
Accepted: 06 November 2025
Published: 13 November 2025
©2025 the Author(s), licensee AIMS Press.

This is an open access article distributed under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0)