A mesocosm study of physical-biological interactions in artificial sea ice: Effects of brine channel surface evolution and brine movement on algal biomass

The impact of changing physico-chemical boundary conditions in sea ice on biological processes was investigated during a 20-day-long simulated freeze-melt cycle in an 180-m3 mesocosm filled with artificial seawater and addition of a mixed Arctic sea-ice community. Ice formation started at Tair of -1...

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Published in:Polar Biology
Main Authors: Krembs, C, Mock, T, Gradinger, R
Format: Article in Journal/Newspaper
Language:unknown
Published: 2001
Subjects:
Online Access:https://ueaeprints.uea.ac.uk/id/eprint/33145/
https://doi.org/10.1007/s003000000219
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spelling ftuniveastangl:oai:ueaeprints.uea.ac.uk:33145 2023-05-15T15:13:01+02:00 A mesocosm study of physical-biological interactions in artificial sea ice: Effects of brine channel surface evolution and brine movement on algal biomass Krembs, C Mock, T Gradinger, R 2001 https://ueaeprints.uea.ac.uk/id/eprint/33145/ https://doi.org/10.1007/s003000000219 unknown Krembs, C, Mock, T and Gradinger, R (2001) A mesocosm study of physical-biological interactions in artificial sea ice: Effects of brine channel surface evolution and brine movement on algal biomass. Polar Biology, 24 (5). pp. 356-364. ISSN 0722-4060 doi:10.1007/s003000000219 Article PeerReviewed 2001 ftuniveastangl https://doi.org/10.1007/s003000000219 2023-01-30T21:30:41Z The impact of changing physico-chemical boundary conditions in sea ice on biological processes was investigated during a 20-day-long simulated freeze-melt cycle in an 180-m3 mesocosm filled with artificial seawater and addition of a mixed Arctic sea-ice community. Ice formation started at Tair of -15°C with a growth rate of 0.7-1.2 mm h-1 for 10 days. The last 10 days (Tair of = -5°C), ice thickness remained around 20 cm. Ice temperature gradients inside the ice were linear and determined brine salinities. Brine was collected by means of centrifugation and its volume ranged from 5 to 30% of total ice volume. Surface areas of interconnected brine channels were determined with two similar techniques and maximum values ranged between 1.5 and 4.8 m2 kg-1 ice. Measurements determined with a modified method varied considerably and differed by a maximal factor of 2.0-6.5. Brine channel surfaces increased during the experiment as a result of the warming of the ice. The inoculated algal community was dominated by flagellates < 10 µm. The low diatom biomass increased in the ice after the air temperature rise with rates comparable to field data (µ=0.2-0.3 day-1). Comparison with brine salinities points towards the hypothesis of vertical brine stability being a controlling factor for ice algal growth. We infer from brine channel surface measurements that persistence of brine channel surfaces during spring might be an important prerequisite for the commencement of net diatom biomass accumulation. Advantages and limitations of mesoscale mesocosms as alternatives in ice biological work are discussed. Article in Journal/Newspaper Arctic Polar Biology Sea ice University of East Anglia: UEA Digital Repository Arctic Polar Biology 24 5 356 364
institution Open Polar
collection University of East Anglia: UEA Digital Repository
op_collection_id ftuniveastangl
language unknown
description The impact of changing physico-chemical boundary conditions in sea ice on biological processes was investigated during a 20-day-long simulated freeze-melt cycle in an 180-m3 mesocosm filled with artificial seawater and addition of a mixed Arctic sea-ice community. Ice formation started at Tair of -15°C with a growth rate of 0.7-1.2 mm h-1 for 10 days. The last 10 days (Tair of = -5°C), ice thickness remained around 20 cm. Ice temperature gradients inside the ice were linear and determined brine salinities. Brine was collected by means of centrifugation and its volume ranged from 5 to 30% of total ice volume. Surface areas of interconnected brine channels were determined with two similar techniques and maximum values ranged between 1.5 and 4.8 m2 kg-1 ice. Measurements determined with a modified method varied considerably and differed by a maximal factor of 2.0-6.5. Brine channel surfaces increased during the experiment as a result of the warming of the ice. The inoculated algal community was dominated by flagellates < 10 µm. The low diatom biomass increased in the ice after the air temperature rise with rates comparable to field data (µ=0.2-0.3 day-1). Comparison with brine salinities points towards the hypothesis of vertical brine stability being a controlling factor for ice algal growth. We infer from brine channel surface measurements that persistence of brine channel surfaces during spring might be an important prerequisite for the commencement of net diatom biomass accumulation. Advantages and limitations of mesoscale mesocosms as alternatives in ice biological work are discussed.
format Article in Journal/Newspaper
author Krembs, C
Mock, T
Gradinger, R
spellingShingle Krembs, C
Mock, T
Gradinger, R
A mesocosm study of physical-biological interactions in artificial sea ice: Effects of brine channel surface evolution and brine movement on algal biomass
author_facet Krembs, C
Mock, T
Gradinger, R
author_sort Krembs, C
title A mesocosm study of physical-biological interactions in artificial sea ice: Effects of brine channel surface evolution and brine movement on algal biomass
title_short A mesocosm study of physical-biological interactions in artificial sea ice: Effects of brine channel surface evolution and brine movement on algal biomass
title_full A mesocosm study of physical-biological interactions in artificial sea ice: Effects of brine channel surface evolution and brine movement on algal biomass
title_fullStr A mesocosm study of physical-biological interactions in artificial sea ice: Effects of brine channel surface evolution and brine movement on algal biomass
title_full_unstemmed A mesocosm study of physical-biological interactions in artificial sea ice: Effects of brine channel surface evolution and brine movement on algal biomass
title_sort mesocosm study of physical-biological interactions in artificial sea ice: effects of brine channel surface evolution and brine movement on algal biomass
publishDate 2001
url https://ueaeprints.uea.ac.uk/id/eprint/33145/
https://doi.org/10.1007/s003000000219
geographic Arctic
geographic_facet Arctic
genre Arctic
Polar Biology
Sea ice
genre_facet Arctic
Polar Biology
Sea ice
op_relation Krembs, C, Mock, T and Gradinger, R (2001) A mesocosm study of physical-biological interactions in artificial sea ice: Effects of brine channel surface evolution and brine movement on algal biomass. Polar Biology, 24 (5). pp. 356-364. ISSN 0722-4060
doi:10.1007/s003000000219
op_doi https://doi.org/10.1007/s003000000219
container_title Polar Biology
container_volume 24
container_issue 5
container_start_page 356
op_container_end_page 364
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