Preprints
https://doi.org/10.5194/egusphere-2026-4182
https://doi.org/10.5194/egusphere-2026-4182
30 Jul 2026
 | 30 Jul 2026
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

Brief communication: Ambient-pressure femtosecond laser ablation as a solid-phase sampling method for water ice

Robin Vinther Nielsen, Ioanna Bertsia-Kanatouri, Kerttu Maria Peensoo, Simon Alexander Munk Wael Fassel, Eirini Malegiannaki, and Vasileios Gkinis

Abstract. High-resolution ice-core analysis requires sampling methods that preserve millimeter to sub-millimeter spatial information. We evaluate ambient-pressure femtosecond laser ablation (fs-LA) as a solid-phase and geometry-tolerant sampling method for water ice under cold, dry laboratory conditions. At 35 µJ and 50 kHz, visible localized craters were produced at all tested exposure times, with mean inner diameters of approximately 87–165 µm. Crater formation was repeatable at a 0.5 mm pitch along 400-position scan paths. The 1 s exposure produced the smallest sampling footprint and largest fraction of craters without visible rims, supporting fs-LA as a platform for future cryospheric analyses.

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Robin Vinther Nielsen, Ioanna Bertsia-Kanatouri, Kerttu Maria Peensoo, Simon Alexander Munk Wael Fassel, Eirini Malegiannaki, and Vasileios Gkinis

Status: open (until 10 Sep 2026)

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Robin Vinther Nielsen, Ioanna Bertsia-Kanatouri, Kerttu Maria Peensoo, Simon Alexander Munk Wael Fassel, Eirini Malegiannaki, and Vasileios Gkinis

Data sets

Supporting data for: Ambient-pressure femtosecond laser ablation as a solid-phase sampling method for water ice Robin Vinther Nielsen et al. https://doi.org/10.5281/zenodo.21099024

Model code and software

LA Crater Analyzer Robin Vinther Nielsen https://github.com/MarsRob/LA_crater_analyzer

Robin Vinther Nielsen, Ioanna Bertsia-Kanatouri, Kerttu Maria Peensoo, Simon Alexander Munk Wael Fassel, Eirini Malegiannaki, and Vasileios Gkinis

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Short summary
Ice cores can preserve past climate information in layers, but melting or cutting samples for measurements can mix or blur that information. We tested femtosecond laser ablation, a method that removes material with ultrashort laser pulses, to sample ice directly in a cold laboratory. It made repeatable craters less than 0.2 millimeters wide, spaced 0.5 millimeters apart. This could support studies of very old ice cores, where layers are very thin, while leaving most of the sample intact.
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