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Auteurs principaux: Foini, Laura, Kurchan, Jorge, Pappalardi, Silvia
Format: Preprint
Publié: 2026
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Accès en ligne:https://arxiv.org/abs/2605.19450
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author Foini, Laura
Kurchan, Jorge
Pappalardi, Silvia
author_facet Foini, Laura
Kurchan, Jorge
Pappalardi, Silvia
contents In this work we ask what the self-consistency of a classical hydrodynamic description imposes on a quantum system. The quantum fluctuation-dissipation theorem, when read in the time domain, acts as a blurring of the fine details of the correlation functions on a Plankian time-scale. We track this blurring along rays inside the light cone for three phenomenological hydrodynamic equations -- diffusion, telegraph and diffusive-telegraph -- and find that the interior of the cone splits into a classical region, where correlation and response satisfy the classical fluctuation-dissipation relation, and a quantum region, where they deviate sharply from it. Preserving a finite classical region as the temperature is lowered forces the effective relaxation rate to be at least Planckian, recovering bounds on diffusivity, equilibration time and shear viscosity. In this way, Planckian scaling of the diffusion constant emerges not as a quantum constraint on microscopic dynamics, but as the price a system pays to remain describable by classical hydrodynamics down to low temperatures.
format Preprint
id arxiv_https___arxiv_org_abs_2605_19450
institution arXiv
publishDate 2026
record_format arxiv
spellingShingle Planckian dissipation from classical hydrodynamics
Foini, Laura
Kurchan, Jorge
Pappalardi, Silvia
Statistical Mechanics
Quantum Gases
Strongly Correlated Electrons
High Energy Physics - Theory
In this work we ask what the self-consistency of a classical hydrodynamic description imposes on a quantum system. The quantum fluctuation-dissipation theorem, when read in the time domain, acts as a blurring of the fine details of the correlation functions on a Plankian time-scale. We track this blurring along rays inside the light cone for three phenomenological hydrodynamic equations -- diffusion, telegraph and diffusive-telegraph -- and find that the interior of the cone splits into a classical region, where correlation and response satisfy the classical fluctuation-dissipation relation, and a quantum region, where they deviate sharply from it. Preserving a finite classical region as the temperature is lowered forces the effective relaxation rate to be at least Planckian, recovering bounds on diffusivity, equilibration time and shear viscosity. In this way, Planckian scaling of the diffusion constant emerges not as a quantum constraint on microscopic dynamics, but as the price a system pays to remain describable by classical hydrodynamics down to low temperatures.
title Planckian dissipation from classical hydrodynamics
topic Statistical Mechanics
Quantum Gases
Strongly Correlated Electrons
High Energy Physics - Theory
url https://arxiv.org/abs/2605.19450