Argon versus helium as carrier gas for LA-ICP-MS impurity mapping on ice cores

• It is possible to achieve mapping with LA-ICP-MS at up to 500 Hz with Ar as carrier gas in a system that is originally designed for He. • Maps obtained on ice core samples show higher intensities in Ar than in He, indicating a potential sensitivity boost for the analysis of ultra-clean Antarctic ice. • Artifact-free maps were obtained on Murrina glass using Ar as a carrier gas and a tube cell for aerosol collection. Impurity records in polar ice cores have provided invaluable insights into atmospheric aerosol concentrations of the past environment. The investigation of the oldest, deepest and highly thinned ice core layers is one of the most pressing tasks in today’s state-of-the-art ice core research. This calls for impurity analysis at high spatial resolution, which has to take into account post-depositional processes through the interaction of impurities with the ice matrix. To this end, mapping the impurity distribution in ice with laser ablation inductively-coupled plasma mass spectrometry (LA-ICP-MS) has great potential. Here we explore to what extent the use of Ar as a carrier gas has merits in ice core impurity mapping with LA-ICP-MS. This is motivated by the fact that a) the use of Ar is more economical over He, especially when used in conjunction with large volume sample cells, and b) an increase in sensitivity has previously been reported when adding ”wet” Ar to He as a carrier gas. We show that, albeit not fully matching the single-pulse-performance of He, it is possible to achieve mapping at up to 500 Hz with Ar in a system that is originally designed for He. In contrast to what we find on NIST glass standards and a sample of decorative murrina glass, maps obtained on ice core samples show higher intensities in Ar than in He. In an extreme case example, we show how Ar may permit to obtain signals in a deep interglacial ice sample from Antarctica with very low impurity concentrations, which was not possible when using He with the same LA-ICP-MS system.

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Publication Details

Journal
Talanta Open
Published
2025-03-22
DOI
https://doi.org/10.1016/j.talo.2025.100437
Citations
2
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
2.60

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article

Argon versus helium as carrier gas for LA-ICP-MS impurity mapping on ice cores

Ciprian Stremtan, Rémi Dallmayr, Kristina Mervič, Martin Šala et al.
2 citations
Talanta Open
Geology and Paleoclimatology Research
2.60
article

Argon versus helium as carrier gas for LA-ICP-MS impurity mapping on ice cores

Ciprian Stremtan, Rémi Dallmayr, Kristina Mervič, Martin Šala, Pascal Bohleber
article en
2 citations

Abstract

• It is possible to achieve mapping with LA-ICP-MS at up to 500 Hz with Ar as carrier gas in a system that is originally designed for He. • Maps obtained on ice core samples show higher intensities in Ar than in He, indicating a potential sensitivity boost for the analysis of ultra-clean Antarctic ice. • Artifact-free maps were obtained on Murrina glass using Ar as a carrier gas and a tube cell for aerosol collection. Impurity records in polar ice cores have provided invaluable insights into atmospheric aerosol concentrations of the past environment. The investigation of the oldest, deepest and highly thinned ice core layers is one of the most pressing tasks in today’s state-of-the-art ice core research. This calls for impurity analysis at high spatial resolution, which has to take into account post-depositional processes through the interaction of impurities with the ice matrix. To this end, mapping the impurity distribution in ice with laser ablation inductively-coupled plasma mass spectrometry (LA-ICP-MS) has great potential. Here we explore to what extent the use of Ar as a carrier gas has merits in ice core impurity mapping with LA-ICP-MS. This is motivated by the fact that a) the use of Ar is more economical over He, especially when used in conjunction with large volume sample cells, and b) an increase in sensitivity has previously been reported when adding ”wet” Ar to He as a carrier gas. We show that, albeit not fully matching the single-pulse-performance of He, it is possible to achieve mapping at up to 500 Hz with Ar in a system that is originally designed for He. In contrast to what we find on NIST glass standards and a sample of decorative murrina glass, maps obtained on ice core samples show higher intensities in Ar than in He. In an extreme case example, we show how Ar may permit to obtain signals in a deep interglacial ice sample from Antarctica with very low impurity concentrations, which was not possible when using He with the same LA-ICP-MS system.

Talanta OpenVol. 11
Goethe University Frankfurt (DE), Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), National Institute of Chemistry (SI)
Javna Agencija za Raziskovalno Dejavnost RS, European Research Council
Openalex Percentile: Top 13%
Geology and Paleoclimatology Research
2.60
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