The generalized Clapeyron equation and its application to confined ice growth

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 engine...

Full description

Bibliographic Details
Main Authors: Robert W. Style, Dominic Gerber, Alan W. Rempel, Eric R. Dufresne
Format: Article
Language:English
Published: Cambridge University Press 2023-08-01
Series:Journal of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S002214302300028X/type/journal_article
_version_ 1797770517330001920
author Robert W. Style
Dominic Gerber
Alan W. Rempel
Eric R. Dufresne
author_facet Robert W. Style
Dominic Gerber
Alan W. Rempel
Eric R. Dufresne
author_sort Robert W. Style
collection DOAJ
description 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.
first_indexed 2024-03-12T21:23:26Z
format Article
id doaj.art-2cee0ce36935480086e199cceee69073
institution Directory Open Access Journal
issn 0022-1430
1727-5652
language English
last_indexed 2024-03-12T21:23:26Z
publishDate 2023-08-01
publisher Cambridge University Press
record_format Article
series Journal of Glaciology
spelling doaj.art-2cee0ce36935480086e199cceee690732023-07-28T10:47:45ZengCambridge University PressJournal of Glaciology0022-14301727-56522023-08-01691091109610.1017/jog.2023.28The generalized Clapeyron equation and its application to confined ice growthRobert W. Style0https://orcid.org/0000-0001-5305-7658Dominic Gerber1https://orcid.org/0000-0002-4231-0694Alan W. Rempel2Eric R. Dufresne3Department of Materials, ETH Zürich, 8093 Zürich, SwitzerlandDepartment of Materials, ETH Zürich, 8093 Zürich, SwitzerlandDepartment of Earth Sciences, University of Oregon, Eugene, Oregon, USADepartment of Materials, ETH Zürich, 8093 Zürich, SwitzerlandMost 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.https://www.cambridge.org/core/product/identifier/S002214302300028X/type/journal_articleAnisotropic icecrystal growthfrozen groundrecrystallizationice physics
spellingShingle Robert W. Style
Dominic Gerber
Alan W. Rempel
Eric R. Dufresne
The generalized Clapeyron equation and its application to confined ice growth
Journal of Glaciology
Anisotropic ice
crystal growth
frozen ground
recrystallization
ice physics
title 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_short The generalized Clapeyron equation and its application to confined ice growth
title_sort generalized clapeyron equation and its application to confined ice growth
topic Anisotropic ice
crystal growth
frozen ground
recrystallization
ice physics
url https://www.cambridge.org/core/product/identifier/S002214302300028X/type/journal_article
work_keys_str_mv AT robertwstyle thegeneralizedclapeyronequationanditsapplicationtoconfinedicegrowth
AT dominicgerber thegeneralizedclapeyronequationanditsapplicationtoconfinedicegrowth
AT alanwrempel thegeneralizedclapeyronequationanditsapplicationtoconfinedicegrowth
AT ericrdufresne thegeneralizedclapeyronequationanditsapplicationtoconfinedicegrowth
AT robertwstyle generalizedclapeyronequationanditsapplicationtoconfinedicegrowth
AT dominicgerber generalizedclapeyronequationanditsapplicationtoconfinedicegrowth
AT alanwrempel generalizedclapeyronequationanditsapplicationtoconfinedicegrowth
AT ericrdufresne generalizedclapeyronequationanditsapplicationtoconfinedicegrowth