Fig 4b 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...
Main Authors: | , |
---|---|
Format: | Dataset |
Language: | unknown |
Published: |
2016
|
Subjects: | |
Online Access: | https://doi.org/10.6084/m9.figshare.4246664.v1 https://figshare.com/articles/dataset/Fig_4b_from_The_influence_of_closed_brine_pockets_and_permeable_brine_channels_on_the_thermo-elastic_properties_of_saline_ice/4246664 |
id |
ftroysocietyfig:oai:figshare.com:article/4246664 |
---|---|
record_format |
openpolar |
spelling |
ftroysocietyfig:oai:figshare.com:article/4246664 2023-05-15T18:29:47+02:00 Fig 4b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice Aleksey Marchenko Ben Lishman 2016-11-22T16:19:27Z https://doi.org/10.6084/m9.figshare.4246664.v1 https://figshare.com/articles/dataset/Fig_4b_from_The_influence_of_closed_brine_pockets_and_permeable_brine_channels_on_the_thermo-elastic_properties_of_saline_ice/4246664 unknown doi:10.6084/m9.figshare.4246664.v1 https://figshare.com/articles/dataset/Fig_4b_from_The_influence_of_closed_brine_pockets_and_permeable_brine_channels_on_the_thermo-elastic_properties_of_saline_ice/4246664 CC BY 4.0 CC-BY Mechanics Thermodynamics Glaciology Microelectromechanical Systems (MEMS) Acoustics and Acoustical Devices Waves saline ice thermal expansion thermo-elastic waves permeability Dataset 2016 ftroysocietyfig https://doi.org/10.6084/m9.figshare.4246664.v1 2022-01-01T19:58:52Z 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 The Royal Society: Figshare Svalbard |
institution |
Open Polar |
collection |
The Royal Society: Figshare |
op_collection_id |
ftroysocietyfig |
language |
unknown |
topic |
Mechanics Thermodynamics Glaciology Microelectromechanical Systems (MEMS) Acoustics and Acoustical Devices Waves saline ice thermal expansion thermo-elastic waves permeability |
spellingShingle |
Mechanics Thermodynamics Glaciology Microelectromechanical Systems (MEMS) Acoustics and Acoustical Devices Waves saline ice thermal expansion thermo-elastic waves permeability Aleksey Marchenko Ben Lishman Fig 4b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice |
topic_facet |
Mechanics Thermodynamics Glaciology Microelectromechanical Systems (MEMS) Acoustics and Acoustical Devices Waves saline ice thermal expansion thermo-elastic waves permeability |
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 |
Aleksey Marchenko Ben Lishman |
author_facet |
Aleksey Marchenko Ben Lishman |
author_sort |
Aleksey Marchenko |
title |
Fig 4b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice |
title_short |
Fig 4b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice |
title_full |
Fig 4b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice |
title_fullStr |
Fig 4b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice |
title_full_unstemmed |
Fig 4b from The influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice |
title_sort |
fig 4b from the influence of closed brine pockets and permeable brine channels on the thermo-elastic properties of saline ice |
publishDate |
2016 |
url |
https://doi.org/10.6084/m9.figshare.4246664.v1 https://figshare.com/articles/dataset/Fig_4b_from_The_influence_of_closed_brine_pockets_and_permeable_brine_channels_on_the_thermo-elastic_properties_of_saline_ice/4246664 |
geographic |
Svalbard |
geographic_facet |
Svalbard |
genre |
Svalbard University Centre in Svalbard |
genre_facet |
Svalbard University Centre in Svalbard |
op_relation |
doi:10.6084/m9.figshare.4246664.v1 https://figshare.com/articles/dataset/Fig_4b_from_The_influence_of_closed_brine_pockets_and_permeable_brine_channels_on_the_thermo-elastic_properties_of_saline_ice/4246664 |
op_rights |
CC BY 4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.4246664.v1 |
_version_ |
1766213159900676096 |