Physico-chemical characteristics and ikaite content of brine and ice samples taken during SIPEX and DDU campaigns in East Antarctica, 2007

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Auteurs principaux: Fischer, Michael, Thomas, David Neville, Krell, Andreas, Nehrke, Gernot, Göttlicher, Jörg, Norman, Marc D, Meiners, Klaus M, Riaux-Gobin, C, Dieckmann, Gerhard S
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Langue:en
Publié: PANGAEA 2013
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author Fischer, Michael
Thomas, David Neville
Krell, Andreas
Nehrke, Gernot
Göttlicher, Jörg
Norman, Marc D
Meiners, Klaus M
Riaux-Gobin, C
Dieckmann, Gerhard S
author_facet Fischer, Michael
Thomas, David Neville
Krell, Andreas
Nehrke, Gernot
Göttlicher, Jörg
Norman, Marc D
Meiners, Klaus M
Riaux-Gobin, C
Dieckmann, Gerhard S
collection Datos científicos de ciencias marinas y ambientales
contents Calcium carbonate precipitation in sea ice is thought to potentially drive significant CO2 uptake by the ocean. However, little is known about the quantitative spatial and temporal distribution of CaCO3 within sea ice, although it is hypothesized that high quantities of dissolved organic matter and/or phosphate (common in sea ice) may inhibit its formation. In this quantitative study of hydrous calcium carbonate as ikaite, sea ice cores and brine samples were collected from pack and land fast sea ice between September and December 2007 during two expeditions, one in the East Antarctic sector and the other off Terre Adélie. Samples were analysed for CaCO3, salinity, dissolved organic carbon/nitrogen, inorganic phosphate, and total alkalinity. No relationship between these parameters and CaCO3 precipitation was evident. Ikaite was found mostly in the uppermost layers of sea ice with maximum concentrations of up to 126 mg ikaite per litre melted sea ice being measured, although both the temporal and horizontal spatial distributions of ikaite were highly heterogeneous. The precipitate was also found in the snow on top of the sea ice at some of the sampling locations.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_847684
institution PANGAEA
language en
publishDate 2013
publisher PANGAEA
record_format pangaea
spellingShingle Physico-chemical characteristics and ikaite content of brine and ice samples taken during SIPEX and DDU campaigns in East Antarctica, 2007
Fischer, Michael
Thomas, David Neville
Krell, Andreas
Nehrke, Gernot
Göttlicher, Jörg
Norman, Marc D
Meiners, Klaus M
Riaux-Gobin, C
Dieckmann, Gerhard S
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; SPP1158
Calcium carbonate precipitation in sea ice is thought to potentially drive significant CO2 uptake by the ocean. However, little is known about the quantitative spatial and temporal distribution of CaCO3 within sea ice, although it is hypothesized that high quantities of dissolved organic matter and/or phosphate (common in sea ice) may inhibit its formation. In this quantitative study of hydrous calcium carbonate as ikaite, sea ice cores and brine samples were collected from pack and land fast sea ice between September and December 2007 during two expeditions, one in the East Antarctic sector and the other off Terre Adélie. Samples were analysed for CaCO3, salinity, dissolved organic carbon/nitrogen, inorganic phosphate, and total alkalinity. No relationship between these parameters and CaCO3 precipitation was evident. Ikaite was found mostly in the uppermost layers of sea ice with maximum concentrations of up to 126 mg ikaite per litre melted sea ice being measured, although both the temporal and horizontal spatial distributions of ikaite were highly heterogeneous. The precipitate was also found in the snow on top of the sea ice at some of the sampling locations.
title Physico-chemical characteristics and ikaite content of brine and ice samples taken during SIPEX and DDU campaigns in East Antarctica, 2007
topic Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; SPP1158
url https://doi.org/10.1594/PANGAEA.847684