Quantification of ikaite in Antarctic sea ice


Contact
Michael.Fischer [ at ] awi.de

Abstract

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 Ade´lie. 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.



Item Type
Article
Authors
Divisions
Primary Division
Programs
Primary Topic
Peer revision
ISI/Scopus peer-reviewed
Publication Status
Published
Eprint ID
32838
DOI 10.1017/S0954102012001150

Cite as
Fischer, M. , Thomas, D. N. , Krell, A. , Nehrke, G. , Göttlicher, J. , Norman, L. , Meiners, K. M. , Riaux-Gobin, C. and Dieckmann, G. S. (2013): Quantification of ikaite in Antarctic sea ice , Antarctic Science, 25 (3), pp. 421-432 . doi: 10.1017/S0954102012001150


Download
[img]
Preview
PDF
S0954102012001150a.pdf

Download (539kB) | Preview
Cite this document as:

Share


Citation

Research Platforms
N/A

Campaigns


Actions
Edit Item Edit Item