The generalized Clapeyron equation and its application to confined ice growth

Abstract Most theoretical descriptions of stresses induced by freezing are rooted in the (generalized) Clapeyron equation, which predicts the pressure that a solid can exert as it cools below its melting temperature. This equation is central for topics ranging beyond glaciology to geomorphology, civ...

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Published in:Journal of Glaciology
Main Authors: Style, Robert W., Gerber, Dominic, Rempel, Alan W., Dufresne, Eric R.
Other Authors: University of Oregon, Eidgenössische Technische Hochschule Zürich, National Science Foundation, Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2023.28
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214302300028X
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spelling crcambridgeupr:10.1017/jog.2023.28 2024-06-23T07:54:15+00:00 The generalized Clapeyron equation and its application to confined ice growth Style, Robert W. Gerber, Dominic Rempel, Alan W. Dufresne, Eric R. University of Oregon Eidgenössische Technische Hochschule Zürich National Science Foundation Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung 2023 http://dx.doi.org/10.1017/jog.2023.28 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214302300028X en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 69, issue 276, page 1091-1096 ISSN 0022-1430 1727-5652 journal-article 2023 crcambridgeupr https://doi.org/10.1017/jog.2023.28 2024-06-05T04:04:31Z Abstract Most theoretical descriptions of stresses induced by freezing are rooted in the (generalized) Clapeyron equation, which predicts the pressure that a solid can exert as it cools below its melting temperature. This equation is central for topics ranging beyond glaciology to geomorphology, civil engineering, food storage and cryopreservation. However, it has inherent limitations, requiring isotropic solid stresses and conditions near bulk equilibrium. Here, we examine when the Clapeyron equation is applicable by providing a rigorous derivation that details all assumptions. We demonstrate the natural extension for anisotropic stress states, and we show how the temperature and pressure ranges for validity depend on well-defined material properties. Finally, we demonstrate how the range of applicability of the (linear) Clapeyron equation can be extended by adding higher-order terms, yielding results that are in good agreement with experimental data for the pressure melting of ice. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 69 276 1091 1096
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Most theoretical descriptions of stresses induced by freezing are rooted in the (generalized) Clapeyron equation, which predicts the pressure that a solid can exert as it cools below its melting temperature. This equation is central for topics ranging beyond glaciology to geomorphology, civil engineering, food storage and cryopreservation. However, it has inherent limitations, requiring isotropic solid stresses and conditions near bulk equilibrium. Here, we examine when the Clapeyron equation is applicable by providing a rigorous derivation that details all assumptions. We demonstrate the natural extension for anisotropic stress states, and we show how the temperature and pressure ranges for validity depend on well-defined material properties. Finally, we demonstrate how the range of applicability of the (linear) Clapeyron equation can be extended by adding higher-order terms, yielding results that are in good agreement with experimental data for the pressure melting of ice.
author2 University of Oregon
Eidgenössische Technische Hochschule Zürich
National Science Foundation
Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung
format Article in Journal/Newspaper
author Style, Robert W.
Gerber, Dominic
Rempel, Alan W.
Dufresne, Eric R.
spellingShingle Style, Robert W.
Gerber, Dominic
Rempel, Alan W.
Dufresne, Eric R.
The generalized Clapeyron equation and its application to confined ice growth
author_facet Style, Robert W.
Gerber, Dominic
Rempel, Alan W.
Dufresne, Eric R.
author_sort Style, Robert W.
title The generalized Clapeyron equation and its application to confined ice growth
title_short The generalized Clapeyron equation and its application to confined ice growth
title_full The generalized Clapeyron equation and its application to confined ice growth
title_fullStr The generalized Clapeyron equation and its application to confined ice growth
title_full_unstemmed The generalized Clapeyron equation and its application to confined ice growth
title_sort generalized clapeyron equation and its application to confined ice growth
publisher Cambridge University Press (CUP)
publishDate 2023
url http://dx.doi.org/10.1017/jog.2023.28
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214302300028X
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 69, issue 276, page 1091-1096
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2023.28
container_title Journal of Glaciology
container_volume 69
container_issue 276
container_start_page 1091
op_container_end_page 1096
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