(Table 1) Micro-inclusion counts and ion concentrations in the five GRIP ice-core sections

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Hauptverfasser: Sakurai, Toshimitsu, Iizuka, Yoshinori, Horikawa, Shinichiro, Johnsen, Sigfús Jóhann, Dahl-Jensen, Dorthe, Steffensen, Jørgen Peder, Hondoh, Takeo
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Sprache:en
Veröffentlicht: PANGAEA 2009
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author Sakurai, Toshimitsu
Iizuka, Yoshinori
Horikawa, Shinichiro
Johnsen, Sigfús Jóhann
Dahl-Jensen, Dorthe
Steffensen, Jørgen Peder
Hondoh, Takeo
author_facet Sakurai, Toshimitsu
Iizuka, Yoshinori
Horikawa, Shinichiro
Johnsen, Sigfús Jóhann
Dahl-Jensen, Dorthe
Steffensen, Jørgen Peder
Hondoh, Takeo
collection Datos científicos de ciencias marinas y ambientales
contents We provide the first direct evidence that a number of water-soluble compounds, in particular calcium sulfate (CaSO4 2H2O) and calcium carbonate (CaCO3), are present as solid, micron-sized inclusions within the Greenland GRIP ice core. The compounds are detected by two independent methods: micro-Raman spectroscopy of a solid ice sample, and energy-dispersive X-ray spectroscopy of individual inclusions remaining after sublimation. CaSO4 2H2O is found in abundance throughout the Holocene and the last glacial period, while CaCO3 exists mainly in the glacial period ice. We also present size and spatial distributions of the micro-inclusions. These results suggest that water-soluble aerosols in the GRIP ice core are dependable proxies for past atmospheric conditions.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_833919
institution PANGAEA
language en
publishDate 2009
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Micro-inclusion counts and ion concentrations in the five GRIP ice-core sections
Sakurai, Toshimitsu
Iizuka, Yoshinori
Horikawa, Shinichiro
Johnsen, Sigfús Jóhann
Dahl-Jensen, Dorthe
Steffensen, Jørgen Peder
Hondoh, Takeo
AGE; Calcium cation; Chloride anion; Depth, bottom/max; DEPTH, ice/snow; Depth, top/min; Diameter; Epoch; Greenland; Greenland Ice Core Projects; GRIP; GRIP__Campaign; GRIP/GISP/NGRIP; International Polar Year (2007-2008); IPY; ISTUK; ISTUK electromechanical drill; Magnesium cation; Nitrate ion; Number; Particle concentration; Sampling/drilling ice; Sodium cation; Standard deviation; Sulfate anion; Thickness
We provide the first direct evidence that a number of water-soluble compounds, in particular calcium sulfate (CaSO4 2H2O) and calcium carbonate (CaCO3), are present as solid, micron-sized inclusions within the Greenland GRIP ice core. The compounds are detected by two independent methods: micro-Raman spectroscopy of a solid ice sample, and energy-dispersive X-ray spectroscopy of individual inclusions remaining after sublimation. CaSO4 2H2O is found in abundance throughout the Holocene and the last glacial period, while CaCO3 exists mainly in the glacial period ice. We also present size and spatial distributions of the micro-inclusions. These results suggest that water-soluble aerosols in the GRIP ice core are dependable proxies for past atmospheric conditions.
title (Table 1) Micro-inclusion counts and ion concentrations in the five GRIP ice-core sections
topic AGE; Calcium cation; Chloride anion; Depth, bottom/max; DEPTH, ice/snow; Depth, top/min; Diameter; Epoch; Greenland; Greenland Ice Core Projects; GRIP; GRIP__Campaign; GRIP/GISP/NGRIP; International Polar Year (2007-2008); IPY; ISTUK; ISTUK electromechanical drill; Magnesium cation; Nitrate ion; Number; Particle concentration; Sampling/drilling ice; Sodium cation; Standard deviation; Sulfate anion; Thickness
url https://doi.org/10.1594/PANGAEA.833919