• Open Access

“Cooling by Heating”—Demonstrating the Significance of the Longitudinal Specific Heat

Jon J. Papini, Jeppe C. Dyre, and Tage Christensen
Phys. Rev. X 2, 041015 – Published 29 November 2012

Abstract

Heating a solid sphere at its surface induces mechanical stresses inside the sphere. If a finite amount of heat is supplied, the stresses gradually disappear as temperature becomes homogeneous throughout the sphere. We show that before this happens, there is a temporary lowering of pressure and density in the interior of the sphere, inducing a transient lowering of the temperature here. For ordinary solids this effect is small because cpcV. For fluent liquids the effect is negligible because their dynamic shear modulus vanishes. For a liquid at its glass transition, however, the effect is generally considerably larger than in solids. This paper presents analytical solutions of the relevant coupled thermoviscoelastic equations. In general, there is a difference between the isobaric specific heat cp measured at constant isotropic pressure and the longitudinal specific heat cl pertaining to mechanical boundary conditions that confine the associated expansion to be longitudinal. In the exact treatment of heat propagation, the heat-diffusion constant contains cl rather than cp. We show that the key parameter controlling the magnitude of the “cooling-by-heating“ effect is the relative difference between these two specific heats. For a typical glass-forming liquid, when the temperature at the surface is increased by 1 K, a lowering of the temperature at the sphere center of the order of 5 mK is expected if the experiment is performed at the glass transition. The cooling-by-heating effect is confirmed by measurements on a glucose sphere at the glass transition.

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  • Received 27 June 2012

DOI:https://doi.org/10.1103/PhysRevX.2.041015

This article is available under the terms of the Creative Commons Attribution 3.0 License. Further distribution of this work must maintain attribution to the author(s) and the published article’s title, journal citation, and DOI.

Published by the American Physical Society

Authors & Affiliations

Jon J. Papini, Jeppe C. Dyre, and Tage Christensen*

  • DNRF Centre “Glass and Time,” IMFUFA, Department of Sciences, Roskilde University, Postbox 260, DK-4000 Roskilde, Denmark

  • *tec@ruc.dk

Popular Summary

When a bulk piece of material is heated at its surface, does its center become hotter or cooler? It turns out that the answer to this seemingly banal question is not obvious at all at a fundamental level. In this paper, we report, first through a theoretical analysis and prediction and then with experimental confirmation, an extraordinary phenomenon of cooling at the center of a supercooled liquid drop heated at its free surface.

Most liquids, when supercooled, eventually end up in the glassy state. Just before the glassy state sets in, such a liquid shows remarkable features. It becomes viscoelastic, or either solid- or liquidlike, depending on whether the time scale of your observation is below or above a threshold time. And, the threshold time increases rather dramatically as the temperature of the liquid is lowered. What is the implication of these properties for the heat-transport process in the supercooled liquid? The ordinary heat-diffusion theory, which treats the heat transport and the mechanical deformation (including expansion and shear deformation) as independent processes, is fundamentally inadequate for describing surface-heating-induced physical processes in the liquid. Based on a theory that couples heat transport to mechanical deformation governed by viscoelasticity, however, we have predicted a measurable, transient center-cooling effect induced by surface heating for a supercooled glucose ball. With a highly sensitive experimental apparatus, we have measured a temperature drop of 7 mK at the center of a glucose ball of 19 mm in diameter in response to a temperature elevation of 5 K at the free surface, confirming both qualitatively and quantitatively the theoretical prediction.

The physics underlying this intriguing phenomenon is not obvious. Heating a piece of material at its surface leads to heat-induced expansion in the material. But, whether that expansion proceeds outward or inward depends on the material’s mechanical properties and how the surface is mechanically constrained. If the expansion proceeds outward, as in the case of the glucose ball in our experiment, a negative pressure change results from that outward expansion and propagates to the interior of the material, causing the temperature there to go down. But, if the material is an ordinary liquid, the pressure change is so short lived that this center-cooling effect is nonexistent for all practical purposes. In a stark contrast, in the case of a supercooled viscoelastic glucose ball, two of its properties combine to make the pressure change measurable: its solidlike characteristic on short, but experimentally accessible time scales, and even more important, a large difference in how the liquid absorbs heat under the condition of either constant pressure or constant volume.

Our work adds a new fascinating page to the fundamental physics of classical materials.

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Vol. 2, Iss. 4 — October - December 2012

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