Abstract

Heat conduction in dielectric crystals originates from the propagation of atomic vibrations, whose microscopic dynamics is well described by the linearized phonon Boltzmann transport equation. Recently, it was shown that thermal conductivity can be resolved exactly and in a closed form as a sum over relaxons, $\mathit{i.e.}$ collective phonon excitations that are the eigenvectors of Boltzmann equation's scattering matrix [Cepellotti and Marzari, PRX $\mathbf{6}$ (2016)]. Relaxons have a well-defined parity, and only odd relaxons contribute to the thermal conductivity. Here, we show that the complementary set of even relaxons determines another quantity --- the thermal viscosity --- that enters into the description of heat transport, and is especially relevant in the hydrodynamic regime, where dissipation of crystal momentum by Umklapp scattering phases out. We also show how the thermal conductivity and viscosity parametrize two novel viscous heat equations --- two coupled equations for the temperature and drift-velocity fields --- which represent the thermal counterpart of the Navier-Stokes equations of hydrodynamics in the linear, laminar regime. These viscous heat equations are derived from a coarse-graining of the linearized Boltzmann transport equation for phonons, and encompass both limits of Fourier's law and of second sound, taking place, respectively, in the regimes of strong or weak momentum dissipation. Last, we introduce the Fourier deviation number as a descriptor that captures the deviations from Fourier's law due to hydrodynamic effects. We showcase these findings in a test case of a complex-shaped device made of graphite, obtaining a remarkable agreement with the very recent experimental demonstration of hydrodynamic transport in this material. The present findings also suggest that hydrodynamic behavior can appear at room temperature in micrometer-sized diamond crystals.

Highlights

  • Thermal transport in insulating crystals takes place through the evolution and dynamics of the vibrations of atoms around their equilibrium positions

  • Turning our attention to diamond, we first recall that it is characterized by a very large thermal conductivity, which originates from having large group velocities and weak umklapp scattering [80,81,82,83,84,85]; the latter condition being favorable to the emergence of hydrodynamic effects

  • These results suggest that a hydrodynamic window exists for diamond, and that hydrodynamic behavior might be measurable in this material at temperatures even larger than graphite

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Summary

INTRODUCTION

Thermal transport in insulating crystals takes place through the evolution and dynamics of the vibrations of atoms around their equilibrium positions. We provide a general and universal solution to the challenge of extending Fourier’s law all the way to the hydrodynamic regime, deriving from the LBTE two novel coupled mesoscopic heat transport equations that cover exactly and on equal footing Fourier diffusion, hydrodynamic propagation, and all regimes in between. To this aim, we first show that one can define the thermal viscosity of a crystal starting from an exact solution of the LBTE in terms of the eigenvectors of the scattering matrix We predict that hydrodynamic behavior can appear in diamond at room temperature for micrometersized crystals

THERMAL VISCOSITY
VISCOUS HEAT EQUATIONS
SECOND SOUND
CASE STUDY
FOURIER DEVIATION NUMBER
G Fourier
C W m δT gi ðwÞ pffiffiffiffiffiffiffiffiffiffiffiffi1
CONCLUSIONS
X α α0
Bose-Einstein eigenvector
Drift eigenvectors
Local equilibrium
X δE ñν Nν ðNν þ 1Þħqi vjν
Single-mode relaxation-time approximation
X 2 i j k l Nν ðNν þ 1Þ 1 ħ q vν q vν kB TðC4Þ
X i j δE
A C κDU κμk2 2

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