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Quantification of ikaite in Antarctic sea ice

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Quantification of ikaite in Antarctic sea ice. / Fischer, Michael; Thomas, David N.; Krell, Andreas et al.
In: Antarctic Science, Vol. 25, No. 3, 06.2013, p. 421-432.

Research output: Contribution to journal › Article › peer-review

HarvardHarvard

Fischer, M, Thomas, DN, Krell, A, Nehrke, G, Göttlicher , J, Norman, L, Meiners, KM, Riaux-Gobin, C & Dieckmann, GS 2013, 'Quantification of ikaite in Antarctic sea ice', Antarctic Science, vol. 25, no. 3, pp. 421-432. https://doi.org/10.1017/S0954102012001150

APA

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

CBE

Fischer M, Thomas DN, Krell A, Nehrke G, Göttlicher J, Norman L, Meiners KM, Riaux-Gobin C, Dieckmann GS. 2013. Quantification of ikaite in Antarctic sea ice. Antarctic Science. 25(3):421-432. https://doi.org/10.1017/S0954102012001150

MLA

Fischer, Michael et al. "Quantification of ikaite in Antarctic sea ice". Antarctic Science. 2013, 25(3). 421-432. https://doi.org/10.1017/S0954102012001150

VancouverVancouver

Fischer M, Thomas DN, Krell A, Nehrke G, Göttlicher J, Norman L et al. Quantification of ikaite in Antarctic sea ice. Antarctic Science. 2013 Jun;25(3):421-432. doi: 10.1017/S0954102012001150

Author

Fischer, Michael ; Thomas, David N. ; Krell, Andreas et al. / Quantification of ikaite in Antarctic sea ice. In: Antarctic Science. 2013 ; Vol. 25, No. 3. pp. 421-432.

RIS

TY - JOUR

T1 - Quantification of ikaite in Antarctic sea ice

AU - Fischer, Michael

AU - Thomas, David N.

AU - Krell, Andreas

AU - Nehrke, Gernot

AU - Göttlicher , Jörg

AU - Norman, Louiza

AU - Meiners, Klaus M.

AU - Riaux-Gobin, Catherine

AU - Dieckmann, Gerhard S.

PY - 2013/6

Y1 - 2013/6

N2 - 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.

AB - 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.

U2 - 10.1017/S0954102012001150

DO - 10.1017/S0954102012001150

M3 - Article

VL - 25

SP - 421

EP - 432

JO - Antarctic Science

JF - Antarctic Science

SN - 0954-1020

IS - 3

ER -