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Dehydration of a crystal hydrate at subglacial temperatures

Water is one of the most important substances on our planet(1). It is ubiquitous in its solid, liquid and vaporous states and all known biological systems depend on its unique chemical and physical properties. Moreover, many materials exist as water adducts, chief among which are crystal hydrates (a...

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Autores principales: Eaby, Alan C., Myburgh, Dirkie C., Kosimov, Akmal, Kwit, Marcin, Esterhuysen, Catharine, Janiak, Agnieszka M., Barbour, Leonard J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10097597/
https://www.ncbi.nlm.nih.gov/pubmed/37045922
http://dx.doi.org/10.1038/s41586-023-05749-7
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author Eaby, Alan C.
Myburgh, Dirkie C.
Kosimov, Akmal
Kwit, Marcin
Esterhuysen, Catharine
Janiak, Agnieszka M.
Barbour, Leonard J.
author_facet Eaby, Alan C.
Myburgh, Dirkie C.
Kosimov, Akmal
Kwit, Marcin
Esterhuysen, Catharine
Janiak, Agnieszka M.
Barbour, Leonard J.
author_sort Eaby, Alan C.
collection PubMed
description Water is one of the most important substances on our planet(1). It is ubiquitous in its solid, liquid and vaporous states and all known biological systems depend on its unique chemical and physical properties. Moreover, many materials exist as water adducts, chief among which are crystal hydrates (a specific class of inclusion compound), which usually retain water indefinitely at subambient temperatures(2). We describe a porous organic crystal that readily and reversibly adsorbs water into 1-nm-wide channels at more than 55% relative humidity. The water uptake/release is chromogenic, thus providing a convenient visual indication of the hydration state of the crystal over a wide temperature range. The complementary techniques of X-ray diffraction, optical microscopy, differential scanning calorimetry and molecular simulations were used to establish that the nanoconfined water is in a state of flux above −70 °C, thus allowing low-temperature dehydration to occur. We were able to determine the kinetics of dehydration over a wide temperature range, including well below 0 °C which, owing to the presence of atmospheric moisture, is usually challenging to accomplish. This discovery unlocks opportunities for designing materials that capture/release water over a range of temperatures that extend well below the freezing point of bulk water.
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spelling pubmed-100975972023-04-14 Dehydration of a crystal hydrate at subglacial temperatures Eaby, Alan C. Myburgh, Dirkie C. Kosimov, Akmal Kwit, Marcin Esterhuysen, Catharine Janiak, Agnieszka M. Barbour, Leonard J. Nature Article Water is one of the most important substances on our planet(1). It is ubiquitous in its solid, liquid and vaporous states and all known biological systems depend on its unique chemical and physical properties. Moreover, many materials exist as water adducts, chief among which are crystal hydrates (a specific class of inclusion compound), which usually retain water indefinitely at subambient temperatures(2). We describe a porous organic crystal that readily and reversibly adsorbs water into 1-nm-wide channels at more than 55% relative humidity. The water uptake/release is chromogenic, thus providing a convenient visual indication of the hydration state of the crystal over a wide temperature range. The complementary techniques of X-ray diffraction, optical microscopy, differential scanning calorimetry and molecular simulations were used to establish that the nanoconfined water is in a state of flux above −70 °C, thus allowing low-temperature dehydration to occur. We were able to determine the kinetics of dehydration over a wide temperature range, including well below 0 °C which, owing to the presence of atmospheric moisture, is usually challenging to accomplish. This discovery unlocks opportunities for designing materials that capture/release water over a range of temperatures that extend well below the freezing point of bulk water. Nature Publishing Group UK 2023-04-12 2023 /pmc/articles/PMC10097597/ /pubmed/37045922 http://dx.doi.org/10.1038/s41586-023-05749-7 Text en © The Author(s), under exclusive licence to Springer Nature Limited 2023 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) .
spellingShingle Article
Eaby, Alan C.
Myburgh, Dirkie C.
Kosimov, Akmal
Kwit, Marcin
Esterhuysen, Catharine
Janiak, Agnieszka M.
Barbour, Leonard J.
Dehydration of a crystal hydrate at subglacial temperatures
title Dehydration of a crystal hydrate at subglacial temperatures
title_full Dehydration of a crystal hydrate at subglacial temperatures
title_fullStr Dehydration of a crystal hydrate at subglacial temperatures
title_full_unstemmed Dehydration of a crystal hydrate at subglacial temperatures
title_short Dehydration of a crystal hydrate at subglacial temperatures
title_sort dehydration of a crystal hydrate at subglacial temperatures
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10097597/
https://www.ncbi.nlm.nih.gov/pubmed/37045922
http://dx.doi.org/10.1038/s41586-023-05749-7
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