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Methanesulphonic acid loss during ice-core storage: recommendations based on a new diffusion coefficient

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The loss of methanesulphonic acid (MSA) from stored ice cores can be significant over typical storage times, with diffusion to the ice-core surface controlling the loss. Methods for minimizing this loss are discussed and it is shown how measurements can be corrected by calculating the amount of MSA lost. A revised diffusion coefficient for MSA in solid ice, (4.1 × 10–13) ± (2.5 × 10–14) m2 s–1, is derived to improve such MSA loss corrections.

Document Type: Research Article


Publication date: December 1, 2009

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  • The Journal of Glaciology is published six times per year. It accepts submissions from any discipline related to the study of snow and ice. All articles are peer reviewed. The Journal is included in the ISI Science Citation Index.
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