Microstructure evolution of young sea ice from a Svalbard fjord using micro-CT analysis

Abstract We analysed the three-dimensional microstructure of sea ice by means of X-ray-micro computed tomography. Microscopic (brine- and air- pore sizes, numbers and connectivity) and macroscopic (salinity, density, porosity) properties of young Arctic sea ice were analysed. The analysis is based o...

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Published in:Journal of Glaciology
Main Authors: Salomon, Martina Lan, Maus, Sönke, Petrich, Chris
Other Authors: Norges Forskningsråd
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2021
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2021.119
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143021001192
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spelling crcambridgeupr:10.1017/jog.2021.119 2024-03-03T08:42:06+00:00 Microstructure evolution of young sea ice from a Svalbard fjord using micro-CT analysis Salomon, Martina Lan Maus, Sönke Petrich, Chris Norges Forskningsråd 2021 http://dx.doi.org/10.1017/jog.2021.119 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143021001192 en eng Cambridge University Press (CUP) https://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 68, issue 269, page 571-590 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 2021 crcambridgeupr https://doi.org/10.1017/jog.2021.119 2024-02-08T08:43:08Z Abstract We analysed the three-dimensional microstructure of sea ice by means of X-ray-micro computed tomography. Microscopic (brine- and air- pore sizes, numbers and connectivity) and macroscopic (salinity, density, porosity) properties of young Arctic sea ice were analysed. The analysis is based on ice cores obtained during spring 2016. Centrifuging of brine prior to CT imaging has allowed us to derive confident relationships between the open, vertically connected and total porosity of young sea ice at relatively high temperatures. We analysed the dependence of the microscopic properties on vertical position and total brine porosity. Most bulk properties (salinity, density) and pore space properties (pore sizes and their distribution) show a strong dependence on total brine porosity, but did not change significantly over the course of the field work. However, significant changes were observed for pore numbers (decreasing over time) and pore connectivity (increasing over time). CT-based salinity determinations are subject to larger than standard uncertainties (from conductivity), while the CT method yields important information about the salinity contributions from closed and open pores. We also performed a comparison of CT-based air porosity with calculations based on density from hydrostatic weighing. The consistency is encouraging and gives confidence to our CT-based results. Article in Journal/Newspaper Arctic Journal of Glaciology Sea ice Svalbard Cambridge University Press Arctic Svalbard Journal of Glaciology 1 20
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Salomon, Martina Lan
Maus, Sönke
Petrich, Chris
Microstructure evolution of young sea ice from a Svalbard fjord using micro-CT analysis
topic_facet Earth-Surface Processes
description Abstract We analysed the three-dimensional microstructure of sea ice by means of X-ray-micro computed tomography. Microscopic (brine- and air- pore sizes, numbers and connectivity) and macroscopic (salinity, density, porosity) properties of young Arctic sea ice were analysed. The analysis is based on ice cores obtained during spring 2016. Centrifuging of brine prior to CT imaging has allowed us to derive confident relationships between the open, vertically connected and total porosity of young sea ice at relatively high temperatures. We analysed the dependence of the microscopic properties on vertical position and total brine porosity. Most bulk properties (salinity, density) and pore space properties (pore sizes and their distribution) show a strong dependence on total brine porosity, but did not change significantly over the course of the field work. However, significant changes were observed for pore numbers (decreasing over time) and pore connectivity (increasing over time). CT-based salinity determinations are subject to larger than standard uncertainties (from conductivity), while the CT method yields important information about the salinity contributions from closed and open pores. We also performed a comparison of CT-based air porosity with calculations based on density from hydrostatic weighing. The consistency is encouraging and gives confidence to our CT-based results.
author2 Norges Forskningsråd
format Article in Journal/Newspaper
author Salomon, Martina Lan
Maus, Sönke
Petrich, Chris
author_facet Salomon, Martina Lan
Maus, Sönke
Petrich, Chris
author_sort Salomon, Martina Lan
title Microstructure evolution of young sea ice from a Svalbard fjord using micro-CT analysis
title_short Microstructure evolution of young sea ice from a Svalbard fjord using micro-CT analysis
title_full Microstructure evolution of young sea ice from a Svalbard fjord using micro-CT analysis
title_fullStr Microstructure evolution of young sea ice from a Svalbard fjord using micro-CT analysis
title_full_unstemmed Microstructure evolution of young sea ice from a Svalbard fjord using micro-CT analysis
title_sort microstructure evolution of young sea ice from a svalbard fjord using micro-ct analysis
publisher Cambridge University Press (CUP)
publishDate 2021
url http://dx.doi.org/10.1017/jog.2021.119
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143021001192
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
genre Arctic
Journal of Glaciology
Sea ice
Svalbard
genre_facet Arctic
Journal of Glaciology
Sea ice
Svalbard
op_source Journal of Glaciology
volume 68, issue 269, page 571-590
ISSN 0022-1430 1727-5652
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2021.119
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 20
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