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A novel probe to sample dissolved and particulate matter in sea ice at high vertical resolution

Bibliographic Data

ID19569093
AuthorsMatthew Corkill (0000-0002-5847-3738, University of Tasmania), Takenobu Toyota (Hokkaido University of Science), Daiki Nomura (0000-0003-3047-4023, Hokkaido University), Klaus M Meiners (0000-0001-7118-9136, University of Tasmania), Pat Wongpan (0000-0002-7113-8221, University of Tasmania), Ryota Akino (Hokkaido University), Nana Samori (0009-0009-8660-1571, Hokkaido University), Masaki Yoshimura (0009-0008-7830-3446, Hokkaido University), Ashley T Townsend (0000-0002-2972-2678, University of Tasmania), Trevor Corkill (10Antec Proprietary Limited, Midvale, Western Australia, Australia), Delphine Lannuzel (0000-0001-6154-1837, University of Tasmania)
Year2025
Volume13
Issue1
Publication date2025-04-08
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueElementa Science of the Anthropocene (JOURNAL)
Journal identifiersISSN: 2325-1026 • E-ISSN: 2325-1026
PublisherUniversity of California Press (PUBLISHER • US)
DOI10.1525/elementa.2024.00053
OpenAlexW4409233575
LanguageEN
References cited47

Sea ice can be interspersed vertically with both permeable and impermeable layers. These features can be smaller than a few centimetres but are important for understanding biogeochemical cycles in sea ice. Traditionally, sea-ice samples are collected by drilling into the ice with a rotating core barrel with a cutting head. Ice cores are extracted and then cut into sections that are melted to collect the variable of interest. Drawbacks to this method include difficulty cutting sections smaller than a few centimetres thick and contamination of samples. Brines may also drain from their in-situ locations and be lost, meaning that important micro-environments in sea ice may be overlooked or misrepresented. To address these drawbacks, we developed a sea-ice melt probe that bores into sea ice and collects high-resolution samples. The capability of the melt probe to delineate a layer of dye in artificial sea ice was tested during cold laboratory-based experiments. Complementary field experiments were carried out in first-year landfast sea ice during February–March 2023 at Saroma-ko Lagoon, Japan. Experiments consisted of testing the high-vertical-resolution capability of the melt probe as well as its ability to be deployed on snow-covered sea ice. The melt probe was able to delineate a layer of dye at a finer resolution (20 mm) than traditional ice coring (approximately 50–100 mm) and could sample sea-ice brine in the field at a high vertical resolution. Melt-probe samples were also used to measure iron in sea ice without contamination. This proof-of-concept study provides an alternative method of sampling sea ice with the ability to support new research on fine-scale structures, with applications for sampling dissolved and particulate sea-ice constituents including trace metals, macro-nutrients, microplastics and gases

Chromatography · Particulates · Sea ice · Arctic and Antarctic ice dynamics · Chemistry · Computer Science · Cryospheric studies and observations · Environmental Science · Methane Hydrates and Related Phenomena · Geology · Oceanography

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    Open Access•K Hans Wedepohl•Geochimica et Cosmochimica Acta•1995

  • Methods for biogeochemical studies of sea ice

    Open Access•Lisa A Miller, Francois Fripiat et al.•Elementa Science of the…•2015

  • The biogeochemical role of a microbial biofilm in sea ice

    Open Access•Arnout Roukaerts, Florian Deman et al.•Elementa Science of the…•2021

  • Iron in sea ice

    Open Access•Delphine Lannuzel, Martin Vancoppenolle et al.•Elementa Science of the…•2016

Citation velocityhistorical
Highly citedNo

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