Crossref journal-article
International Glaciological Society
Annals of Glaciology (1782)
Abstract

Analysis of an ice sample with an estimated age of 125 years, from the Antarctic Peninsula, using a scanning electron microscope with a cold stage and an X-ray micro-analysis facility, shows that H2SO4 occurs mainly at triple junctions. Sea salts show no such localization. The different behaviour may be due to the freezing-point behaviour of each chemical substance, and to the effect this has both in the atmosphere and during recrystallization in the ice sheet. If this finding applies generally to other parts of the Antarctic ice sheet, it has major implications for many of the physical properties of Antarctic ice. In particular, it leads to a better understanding of the d.c. electrical conductivity of such ice.

Bibliography

Wolff, E. W., Mulvaney, R., & Oates, K. (1988). The Location of Impurities in Antarctic Ice. Annals of Glaciology, 11, 194–197.

Authors 3
  1. E.W. Wolff (first)
  2. R. Mulvaney (additional)
  3. K. Oates (additional)
References 23 Referenced 22
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Dates
Type When
Created 7 years, 11 months ago (Sept. 21, 2017, 6:22 a.m.)
Deposited 2 years, 4 months ago (April 3, 2023, 5:35 a.m.)
Indexed 2 months ago (July 2, 2025, 3:30 p.m.)
Issued 37 years, 8 months ago (Jan. 1, 1988)
Published 37 years, 8 months ago (Jan. 1, 1988)
Published Online 8 years, 4 months ago (May 3, 2017)
Published Print 37 years, 8 months ago (Jan. 1, 1988)
Funders 0

None

@article{Wolff_1988, title={The Location of Impurities in Antarctic Ice}, volume={11}, ISSN={1727-5644}, url={http://dx.doi.org/10.3189/s026030550003528x}, DOI={10.3189/s026030550003528x}, journal={Annals of Glaciology}, publisher={International Glaciological Society}, author={Wolff, E.W. and Mulvaney, R. and Oates, K.}, year={1988}, pages={194–197} }