Freezing point depression and freeze-thaw damage by nanofluidic salt trapping

A remarkable variety of organisms and wet materials are able to endure temperatures far below the freezing point of bulk water. Cryotolerance in biology is usually attributed to "antifreeze" proteins, and yet massive supercooling (<−40∘C) is also possible in porous media containing...

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Published in:Physical Review Fluids
Main Authors: Zhou, Tingtao, Mirzadeh, Mohammad, Pellenq, Roland J.-M., Bazant, Martin Z.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Physical Society 2020
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Online Access:https://doi.org/10.1103/physrevfluids.5.124201
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spelling ftcaltechauth:oai:authors.library.caltech.edu:9cr7s-nez04 2024-10-20T14:09:25+00:00 Freezing point depression and freeze-thaw damage by nanofluidic salt trapping Zhou, Tingtao Mirzadeh, Mohammad Pellenq, Roland J.-M. Bazant, Martin Z. 2020-12 https://doi.org/10.1103/physrevfluids.5.124201 unknown American Physical Society https://arxiv.org/abs/1905.07036 https://doi.org/10.1103/physrevfluids.5.124201 eprintid:107182 info:eu-repo/semantics/openAccess Other Physical Review Fluids, 5(12), Art. No. 124201, (2020-12) info:eu-repo/semantics/article 2020 ftcaltechauth https://doi.org/10.1103/physrevfluids.5.124201 2024-09-25T18:46:41Z A remarkable variety of organisms and wet materials are able to endure temperatures far below the freezing point of bulk water. Cryotolerance in biology is usually attributed to "antifreeze" proteins, and yet massive supercooling (<−40∘C) is also possible in porous media containing only simple aqueous electrolytes. For concrete pavements, the common wisdom is that freeze-thaw (FT) damage results from the expansion of water upon freezing, but this cannot explain the high pressures (>10 MPa) required to damage concrete, the observed correlation between pavement damage and deicing salts, or the FT damage of cement paste loaded with benzene (which contracts upon freezing). In this work, we propose a different mechanism—nanofluidic salt trapping—which can explain the observations, using simple mathematical models of dissolved ions confined between growing ice and charged pore surfaces. When the transport time scale for ions through charged pore space is prolonged, ice formation in confined pores causes enormous disjoining pressures via the ions rejected from the ice core, until their removal by precipitation or surface adsorption at lower temperatures releases the pressure and allows complete freezing. The theory is able to predict the nonmonotonic salt-concentration dependence of FT damage in concrete and provides some hint to better understand the origins of cryotolerance from a physical chemistry perspective. © 2020 American Physical Society. (Received 28 July 2020; accepted 9 November 2020; published 2 December 2020) The authors thank S. Yip, C. Qiao, J. Weiss, and M. Pinson for useful discussions. This work was carried out with the support of the Concrete Sustainability Hub at MIT. Published - PhysRevFluids.5.124201.pdf Submitted - 1905.07036.pdf Article in Journal/Newspaper ice core Caltech Authors (California Institute of Technology) Physical Review Fluids 5 12
institution Open Polar
collection Caltech Authors (California Institute of Technology)
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language unknown
description A remarkable variety of organisms and wet materials are able to endure temperatures far below the freezing point of bulk water. Cryotolerance in biology is usually attributed to "antifreeze" proteins, and yet massive supercooling (<−40∘C) is also possible in porous media containing only simple aqueous electrolytes. For concrete pavements, the common wisdom is that freeze-thaw (FT) damage results from the expansion of water upon freezing, but this cannot explain the high pressures (>10 MPa) required to damage concrete, the observed correlation between pavement damage and deicing salts, or the FT damage of cement paste loaded with benzene (which contracts upon freezing). In this work, we propose a different mechanism—nanofluidic salt trapping—which can explain the observations, using simple mathematical models of dissolved ions confined between growing ice and charged pore surfaces. When the transport time scale for ions through charged pore space is prolonged, ice formation in confined pores causes enormous disjoining pressures via the ions rejected from the ice core, until their removal by precipitation or surface adsorption at lower temperatures releases the pressure and allows complete freezing. The theory is able to predict the nonmonotonic salt-concentration dependence of FT damage in concrete and provides some hint to better understand the origins of cryotolerance from a physical chemistry perspective. © 2020 American Physical Society. (Received 28 July 2020; accepted 9 November 2020; published 2 December 2020) The authors thank S. Yip, C. Qiao, J. Weiss, and M. Pinson for useful discussions. This work was carried out with the support of the Concrete Sustainability Hub at MIT. Published - PhysRevFluids.5.124201.pdf Submitted - 1905.07036.pdf
format Article in Journal/Newspaper
author Zhou, Tingtao
Mirzadeh, Mohammad
Pellenq, Roland J.-M.
Bazant, Martin Z.
spellingShingle Zhou, Tingtao
Mirzadeh, Mohammad
Pellenq, Roland J.-M.
Bazant, Martin Z.
Freezing point depression and freeze-thaw damage by nanofluidic salt trapping
author_facet Zhou, Tingtao
Mirzadeh, Mohammad
Pellenq, Roland J.-M.
Bazant, Martin Z.
author_sort Zhou, Tingtao
title Freezing point depression and freeze-thaw damage by nanofluidic salt trapping
title_short Freezing point depression and freeze-thaw damage by nanofluidic salt trapping
title_full Freezing point depression and freeze-thaw damage by nanofluidic salt trapping
title_fullStr Freezing point depression and freeze-thaw damage by nanofluidic salt trapping
title_full_unstemmed Freezing point depression and freeze-thaw damage by nanofluidic salt trapping
title_sort freezing point depression and freeze-thaw damage by nanofluidic salt trapping
publisher American Physical Society
publishDate 2020
url https://doi.org/10.1103/physrevfluids.5.124201
genre ice core
genre_facet ice core
op_source Physical Review Fluids, 5(12), Art. No. 124201, (2020-12)
op_relation https://arxiv.org/abs/1905.07036
https://doi.org/10.1103/physrevfluids.5.124201
eprintid:107182
op_rights info:eu-repo/semantics/openAccess
Other
op_doi https://doi.org/10.1103/physrevfluids.5.124201
container_title Physical Review Fluids
container_volume 5
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