Fig 10b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice
A model of the thermo-elastic behaviour of saline ice is formulated, and model solutions describing thermo-elastic waves (TEW) propagating into a half-space of the ice are investigated. The model is based on a proposal that saline ice is a matrix, which encompasses both closed brine pockets and perm...
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The Royal Society
2016
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ftdatacite:10.6084/m9.figshare.4246640.v1 2023-05-15T18:29:47+02:00 Fig 10b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice Marchenko, Aleksey Lishman, Ben 2016 https://dx.doi.org/10.6084/m9.figshare.4246640.v1 https://rs.figshare.com/articles/dataset/Fig_10b_from_The_influence_of_closed_brine_pockets_and_permeable_brine_channels_on_the_thermo-elastic_properties_of_saline_ice/4246640/1 unknown The Royal Society https://dx.doi.org/10.1098/rsta.2015.0351 https://dx.doi.org/10.6084/m9.figshare.4246640 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Mechanics Thermodynamics 40602 Glaciology FOS Earth and related environmental sciences 91306 Microelectromechanical Systems MEMS FOS Mechanical engineering 20301 Acoustics and Acoustical Devices; Waves FOS Physical sciences dataset Dataset 2016 ftdatacite https://doi.org/10.6084/m9.figshare.4246640.v1 https://doi.org/10.1098/rsta.2015.0351 https://doi.org/10.6084/m9.figshare.4246640 2021-11-05T12:55:41Z A model of the thermo-elastic behaviour of saline ice is formulated, and model solutions describing thermo-elastic waves (TEW) propagating into a half-space of the ice are investigated. The model is based on a proposal that saline ice is a matrix, which encompasses both closed brine pockets and permeable channels filled with brine. Experiments on the thermal expansion of saline ice samples, and on TEW in saline ice, have been performed in the cold laboratories of the University Centre in Svalbard and in University College London. The experimental data are compared with theoretical conclusions. The experimental data support our hypothesis that the brine in saline ice is divided between closed pockets and open, permeable channels. Dataset Svalbard University Centre in Svalbard DataCite Metadata Store (German National Library of Science and Technology) Svalbard |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Mechanics Thermodynamics 40602 Glaciology FOS Earth and related environmental sciences 91306 Microelectromechanical Systems MEMS FOS Mechanical engineering 20301 Acoustics and Acoustical Devices; Waves FOS Physical sciences |
spellingShingle |
Mechanics Thermodynamics 40602 Glaciology FOS Earth and related environmental sciences 91306 Microelectromechanical Systems MEMS FOS Mechanical engineering 20301 Acoustics and Acoustical Devices; Waves FOS Physical sciences Marchenko, Aleksey Lishman, Ben Fig 10b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice |
topic_facet |
Mechanics Thermodynamics 40602 Glaciology FOS Earth and related environmental sciences 91306 Microelectromechanical Systems MEMS FOS Mechanical engineering 20301 Acoustics and Acoustical Devices; Waves FOS Physical sciences |
description |
A model of the thermo-elastic behaviour of saline ice is formulated, and model solutions describing thermo-elastic waves (TEW) propagating into a half-space of the ice are investigated. The model is based on a proposal that saline ice is a matrix, which encompasses both closed brine pockets and permeable channels filled with brine. Experiments on the thermal expansion of saline ice samples, and on TEW in saline ice, have been performed in the cold laboratories of the University Centre in Svalbard and in University College London. The experimental data are compared with theoretical conclusions. The experimental data support our hypothesis that the brine in saline ice is divided between closed pockets and open, permeable channels. |
format |
Dataset |
author |
Marchenko, Aleksey Lishman, Ben |
author_facet |
Marchenko, Aleksey Lishman, Ben |
author_sort |
Marchenko, Aleksey |
title |
Fig 10b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice |
title_short |
Fig 10b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice |
title_full |
Fig 10b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice |
title_fullStr |
Fig 10b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice |
title_full_unstemmed |
Fig 10b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice |
title_sort |
fig 10b from the influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice |
publisher |
The Royal Society |
publishDate |
2016 |
url |
https://dx.doi.org/10.6084/m9.figshare.4246640.v1 https://rs.figshare.com/articles/dataset/Fig_10b_from_The_influence_of_closed_brine_pockets_and_permeable_brine_channels_on_the_thermo-elastic_properties_of_saline_ice/4246640/1 |
geographic |
Svalbard |
geographic_facet |
Svalbard |
genre |
Svalbard University Centre in Svalbard |
genre_facet |
Svalbard University Centre in Svalbard |
op_relation |
https://dx.doi.org/10.1098/rsta.2015.0351 https://dx.doi.org/10.6084/m9.figshare.4246640 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.4246640.v1 https://doi.org/10.1098/rsta.2015.0351 https://doi.org/10.6084/m9.figshare.4246640 |
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1766213152552255488 |