Permeability of winter and spring first-year ice in the Antarctic marginal ice zone

This study was part of the 2019 Southern oCean seAsonal Experiment (SCALE) Winter and Spring Cruise of the South African icebreaker SA Agulhas II. First-year spring and winter sea ice were sampled from the Antarctic marginal ice zone. Consolidated pack ice was collected during both cruises, while pa...

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Bibliographic Details
Main Author: Lin, Xuefeng
Other Authors: Skatulla, Sebastian
Format: Master Thesis
Language:English
Published: Department of Civil Engineering 2022
Subjects:
Online Access:http://hdl.handle.net/11427/37472
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spelling ftunivcapetownir:oai:open.uct.ac.za:11427/37472 2023-12-03T10:13:56+01:00 Permeability of winter and spring first-year ice in the Antarctic marginal ice zone Lin, Xuefeng Skatulla, Sebastian 2022 application/pdf http://hdl.handle.net/11427/37472 eng eng Department of Civil Engineering Faculty of Engineering and the Built Environment http://hdl.handle.net/11427/37472 Engineering Master Thesis Masters MSc 2022 ftunivcapetownir 2023-11-03T00:17:01Z This study was part of the 2019 Southern oCean seAsonal Experiment (SCALE) Winter and Spring Cruise of the South African icebreaker SA Agulhas II. First-year spring and winter sea ice were sampled from the Antarctic marginal ice zone. Consolidated pack ice was collected during both cruises, while pancake ice floes and brash ice floes were collected during Winter and Spring Cruise, respectively. The ice cores analyses of temperature, salinity, and texture were subsequently performed during the Spring and Winter Cruise, and an additional falling head permeability test was conducted during the Spring Cruise. The brine volume is determined empirically from sea ice temperature and bulk salinity. The ice permeability is then calculated from the porosity-permeability relation. The mean permeability of spring pack ice is 2.6 × 10−11 ± 3.67 × 10−11 m2 , marginally higher than the winter pack ice with a mean permeability of 1.1×10−11±2.3×10−11 m2 . Comparing the permeability values of spring and winter consolidated pack ice shows a continuous increase in permeability with seasonal progressions and a rise in ice temperature. The falling head permeability test using kerosene has been made in-house by Hasham Taujoo to determine the in situ sea ice permeability during the Spring Cruise. The experimentally determined permeability values of spring consolidated pack ice were consistent with the above-stated permeability data. However, the permeability values of spring brash ice floes (1.4 × 10−11 ± 2.12 × 10−11 m2 ) determined from porositypermeability relation deviate from field observations due to the presence of large holes and cracks on the ice samples. Master Thesis Antarc* Antarctic Sea ice Southern Ocean University of Cape Town: OpenUCT Antarctic Southern Ocean The Antarctic Pancake ENVELOPE(-55.815,-55.815,52.600,52.600)
institution Open Polar
collection University of Cape Town: OpenUCT
op_collection_id ftunivcapetownir
language English
topic Engineering
spellingShingle Engineering
Lin, Xuefeng
Permeability of winter and spring first-year ice in the Antarctic marginal ice zone
topic_facet Engineering
description This study was part of the 2019 Southern oCean seAsonal Experiment (SCALE) Winter and Spring Cruise of the South African icebreaker SA Agulhas II. First-year spring and winter sea ice were sampled from the Antarctic marginal ice zone. Consolidated pack ice was collected during both cruises, while pancake ice floes and brash ice floes were collected during Winter and Spring Cruise, respectively. The ice cores analyses of temperature, salinity, and texture were subsequently performed during the Spring and Winter Cruise, and an additional falling head permeability test was conducted during the Spring Cruise. The brine volume is determined empirically from sea ice temperature and bulk salinity. The ice permeability is then calculated from the porosity-permeability relation. The mean permeability of spring pack ice is 2.6 × 10−11 ± 3.67 × 10−11 m2 , marginally higher than the winter pack ice with a mean permeability of 1.1×10−11±2.3×10−11 m2 . Comparing the permeability values of spring and winter consolidated pack ice shows a continuous increase in permeability with seasonal progressions and a rise in ice temperature. The falling head permeability test using kerosene has been made in-house by Hasham Taujoo to determine the in situ sea ice permeability during the Spring Cruise. The experimentally determined permeability values of spring consolidated pack ice were consistent with the above-stated permeability data. However, the permeability values of spring brash ice floes (1.4 × 10−11 ± 2.12 × 10−11 m2 ) determined from porositypermeability relation deviate from field observations due to the presence of large holes and cracks on the ice samples.
author2 Skatulla, Sebastian
format Master Thesis
author Lin, Xuefeng
author_facet Lin, Xuefeng
author_sort Lin, Xuefeng
title Permeability of winter and spring first-year ice in the Antarctic marginal ice zone
title_short Permeability of winter and spring first-year ice in the Antarctic marginal ice zone
title_full Permeability of winter and spring first-year ice in the Antarctic marginal ice zone
title_fullStr Permeability of winter and spring first-year ice in the Antarctic marginal ice zone
title_full_unstemmed Permeability of winter and spring first-year ice in the Antarctic marginal ice zone
title_sort permeability of winter and spring first-year ice in the antarctic marginal ice zone
publisher Department of Civil Engineering
publishDate 2022
url http://hdl.handle.net/11427/37472
long_lat ENVELOPE(-55.815,-55.815,52.600,52.600)
geographic Antarctic
Southern Ocean
The Antarctic
Pancake
geographic_facet Antarctic
Southern Ocean
The Antarctic
Pancake
genre Antarc*
Antarctic
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Sea ice
Southern Ocean
op_relation http://hdl.handle.net/11427/37472
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