Tank study of physico-chemical controls on gas content and composition during growth of young sea ice

During an ice tank experiment, samples were taken to study the processes of acquisition and alteration of the gas properties in young first-year sea ice during a complete growth-warming-cooling cycle. The goal was to obtain reference levels for total gas content and concentrations of atmospheric gas...

Full description

Bibliographic Details
Main Authors: Tison, J. L., Haas, Christian, Gowing, M. M., Sleewaegen, S., Bernard, A.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2002
Subjects:
Online Access:https://epic.awi.de/id/eprint/4437/
https://hdl.handle.net/10013/epic.15012
id ftawi:oai:epic.awi.de:4437
record_format openpolar
spelling ftawi:oai:epic.awi.de:4437 2024-09-15T18:15:42+00:00 Tank study of physico-chemical controls on gas content and composition during growth of young sea ice Tison, J. L. Haas, Christian Gowing, M. M. Sleewaegen, S. Bernard, A. 2002 https://epic.awi.de/id/eprint/4437/ https://hdl.handle.net/10013/epic.15012 unknown Tison, J. L. , Haas, C. orcid:0000-0002-7674-3500 , Gowing, M. M. , Sleewaegen, S. and Bernard, A. (2002) Tank study of physico-chemical controls on gas content and composition during growth of young sea ice , Journal of Glaciology . hdl:10013/epic.15012 EPIC3Journal of Glaciology Article isiRev 2002 ftawi 2024-06-24T03:54:51Z During an ice tank experiment, samples were taken to study the processes of acquisition and alteration of the gas properties in young first-year sea ice during a complete growth-warming-cooling cycle. The goal was to obtain reference levels for total gas content and concentrations of atmospheric gases (O2, N2, CO2) in the absence of significant biological activity.The range of total gas content values obtained (3.5 to 18 ml of gas per kilo of ice) was similar to previous measurements or estimates. However, major differences occurred between the current and quiet basins, showing the role of water dynamics at the ice-water interface in controlling bubble nucleation processes.Extremely high CO2 concentrations were observed in all the experiments (up to 57% in volume parts). It is argued that these could have resulted from two unexpected biases in the experimental settings.Concentrations of bubbles nucleated at the interface are controlled by diffusion both from the ice-water interface towards the well-mixed reservoir, and between the interface water and the bubble itself. This double kinetic effect results in a transition of the gas composition in the bubbles from values close to solubility in sea water towards values close to atmospheric, as the ice cover builds up. Article in Journal/Newspaper Journal of Glaciology Sea ice Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description During an ice tank experiment, samples were taken to study the processes of acquisition and alteration of the gas properties in young first-year sea ice during a complete growth-warming-cooling cycle. The goal was to obtain reference levels for total gas content and concentrations of atmospheric gases (O2, N2, CO2) in the absence of significant biological activity.The range of total gas content values obtained (3.5 to 18 ml of gas per kilo of ice) was similar to previous measurements or estimates. However, major differences occurred between the current and quiet basins, showing the role of water dynamics at the ice-water interface in controlling bubble nucleation processes.Extremely high CO2 concentrations were observed in all the experiments (up to 57% in volume parts). It is argued that these could have resulted from two unexpected biases in the experimental settings.Concentrations of bubbles nucleated at the interface are controlled by diffusion both from the ice-water interface towards the well-mixed reservoir, and between the interface water and the bubble itself. This double kinetic effect results in a transition of the gas composition in the bubbles from values close to solubility in sea water towards values close to atmospheric, as the ice cover builds up.
format Article in Journal/Newspaper
author Tison, J. L.
Haas, Christian
Gowing, M. M.
Sleewaegen, S.
Bernard, A.
spellingShingle Tison, J. L.
Haas, Christian
Gowing, M. M.
Sleewaegen, S.
Bernard, A.
Tank study of physico-chemical controls on gas content and composition during growth of young sea ice
author_facet Tison, J. L.
Haas, Christian
Gowing, M. M.
Sleewaegen, S.
Bernard, A.
author_sort Tison, J. L.
title Tank study of physico-chemical controls on gas content and composition during growth of young sea ice
title_short Tank study of physico-chemical controls on gas content and composition during growth of young sea ice
title_full Tank study of physico-chemical controls on gas content and composition during growth of young sea ice
title_fullStr Tank study of physico-chemical controls on gas content and composition during growth of young sea ice
title_full_unstemmed Tank study of physico-chemical controls on gas content and composition during growth of young sea ice
title_sort tank study of physico-chemical controls on gas content and composition during growth of young sea ice
publishDate 2002
url https://epic.awi.de/id/eprint/4437/
https://hdl.handle.net/10013/epic.15012
genre Journal of Glaciology
Sea ice
genre_facet Journal of Glaciology
Sea ice
op_source EPIC3Journal of Glaciology
op_relation Tison, J. L. , Haas, C. orcid:0000-0002-7674-3500 , Gowing, M. M. , Sleewaegen, S. and Bernard, A. (2002) Tank study of physico-chemical controls on gas content and composition during growth of young sea ice , Journal of Glaciology . hdl:10013/epic.15012
_version_ 1810453627479785472