Na₂SO₄ and MgSO₄ salts during the Holocene period derived by high-resolution depth analysis of a Dome Fuji ice core

Authors: Iizuka, Yoshinori; Hondoh, Takeo; Fujii, Yoshiyuki

Source: Journal of Glaciology, Volume 52, Number 176, January 2006 , pp. 58-64(7)

Publisher: International Glaciological Society

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Abstract:

We analyzed the profiles of ionic chemical species in three 500 mm sections of an ice core from Dome Fuji, Antarctica, dated 3.0, 8.9 and 13.3 kyr BP (before present), and compared the profiles to those in the surface snow. The 3.0 and 8.9 kyr sections are from the Holocene and the 13.3 kyr section slightly predates the Holocene. The analyses were done on 2 mm thick slices within each section. At each depth, the primary ionic species were Na⁺, H⁺, Cl⁻ and SO₄²⁻. The SO₄²⁻, Na⁺ and Mg²⁺ levels varied with depth in each section over distances ranging from several millimeters to several centimeters. Also, the correlation coefficients between Na⁺ and SO₄²⁻ and between Mg²⁺ and SO₄²⁻ for each depth were 0.90 or greater, in contrast to the value of 0.59 or less in the surface snow (defined here as 0-3.4 m from the surface). These results suggest that almost all Na⁺ and Mg²⁺ in the Holocene ice exists as Na₂SO₄ and MgSO₄ salts, and the formation of these salts occurs not only in the atmosphere during transport, but also in the firn layer.

Document Type: Research article

DOI: http://dx.doi.org/10.3189/172756506781828926

Publication date: 2006-01-01

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