Temperature-invariant crystal-glass heat conduction: From meteorites to refractories
成果类型:
Article
署名作者:
Simoncelli, Michele; Fournier, Daniele; Marangolo, Massimiliano; Balan, Etienne; Beneut, Keevin; Baptiste, Benoit; Doisneau, Beatrice; Marzari, Nicola; Mauri, Francesco
署名单位:
University of Cambridge; Columbia University; Centre National de la Recherche Scientifique (CNRS); Sorbonne Universite; Sorbonne Universite; Museum National d'Histoire Naturelle (MNHN); Centre National de la Recherche Scientifique (CNRS); Universite Paris Cite; Swiss Federal Institutes of Technology Domain; Ecole Polytechnique Federale de Lausanne; Swiss Federal Institutes of Technology Domain; Ecole Polytechnique Federale de Lausanne; Sapienza University Rome
刊物名称:
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
ISSN/ISSBN:
0027-8424; 1091-6490
DOI:
10.1073/pnas.2422763122
发表日期:
2025-07-15
页码:
e2422763122
关键词:
atomic disorder
thermal conductivity
meteorite
refractory materials
thermal-conductivity
tridymite
silica
cristobalite
diffusivity
DYNAMICS
rock
摘要:
The thermal conductivities of crystals and glasses vary strongly and with opposite trends upon heating, decreasing in crystals and increasing in glasses. Here, we show that the dominant conduction mechanisms of crystals (particle-like propagation) and glasses (wave-like tunneling) can compensate in materials with crystalline bond order and nearly glassy bond geometry, yielding a hybrid crystal-glass conductivity that is constant from the quantum to the classical regime (i.e., from below to above the Debye temperature). We showcase these arguments with a combined theoretical and experimental study on meteoritic silica (a tridymite carved from a sample found in Steinbach, Germany, in 1724) and on a geometrically amorphous tridymite phase found in refractory bricks used in furnaces for steel smelting. Our results prove that temperature-invariant conductivities are not limited to the classical regime, and pave the way to understand or control heat-transport phenomena in solids exposed to extreme temperature variations, ranging from planetary cooling to heating protocols to reduce the carbon footprint of industrial furnaces.
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