Microstructure evolution of young sea ice from a Svalbard fjord using micro-CT analysis
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 cor...
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Cambridge University Press
2022
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Online Access: | https://doi.org/10.1017/jog.2021.119 https://doaj.org/article/0fffd56758e64eb69b9754ca16ee0288 |
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ftdoajarticles:oai:doaj.org/article:0fffd56758e64eb69b9754ca16ee0288 2023-05-15T15:08:38+02:00 Microstructure evolution of young sea ice from a Svalbard fjord using micro-CT analysis Martina Lan Salomon Sönke Maus Chris Petrich 2022-06-01T00:00:00Z https://doi.org/10.1017/jog.2021.119 https://doaj.org/article/0fffd56758e64eb69b9754ca16ee0288 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143021001192/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2021.119 0022-1430 1727-5652 https://doaj.org/article/0fffd56758e64eb69b9754ca16ee0288 Journal of Glaciology, Vol 68, Pp 571-590 (2022) Sea ice sea-ice geophysics sea-ice growth and decay ice coring ice physics Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2022 ftdoajarticles https://doi.org/10.1017/jog.2021.119 2023-03-12T01:30:54Z 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 Directory of Open Access Journals: DOAJ Articles Arctic Svalbard Journal of Glaciology 68 269 571 590 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Sea ice sea-ice geophysics sea-ice growth and decay ice coring ice physics Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
Sea ice sea-ice geophysics sea-ice growth and decay ice coring ice physics Environmental sciences GE1-350 Meteorology. Climatology QC851-999 Martina Lan Salomon Sönke Maus Chris Petrich Microstructure evolution of young sea ice from a Svalbard fjord using micro-CT analysis |
topic_facet |
Sea ice sea-ice geophysics sea-ice growth and decay ice coring ice physics Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
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. |
format |
Article in Journal/Newspaper |
author |
Martina Lan Salomon Sönke Maus Chris Petrich |
author_facet |
Martina Lan Salomon Sönke Maus Chris Petrich |
author_sort |
Martina Lan Salomon |
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 |
publishDate |
2022 |
url |
https://doi.org/10.1017/jog.2021.119 https://doaj.org/article/0fffd56758e64eb69b9754ca16ee0288 |
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, Vol 68, Pp 571-590 (2022) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143021001192/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2021.119 0022-1430 1727-5652 https://doaj.org/article/0fffd56758e64eb69b9754ca16ee0288 |
op_doi |
https://doi.org/10.1017/jog.2021.119 |
container_title |
Journal of Glaciology |
container_volume |
68 |
container_issue |
269 |
container_start_page |
571 |
op_container_end_page |
590 |
_version_ |
1766339956778729472 |