EGU24-12902, updated on 25 Oct 2024
https://doi.org/10.5194/egusphere-egu24-12902
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Advancing towards high-quality water isotope measurements in ice cores: a micro-destructive approach using Laser Ablation coupled with Cavity Ring Down Spectroscopy

Eirini Malegiannaki1,2, Daniele Zannoni2, Pascal Bohleber2,4, Ciprian Stremtan6, Agnese Petteni2, Barbara Stenni2, Carlo Barbante2,3, Dorthe Dahl-Jensen1,5, and Vasileios Gkinis1
Eirini Malegiannaki et al.
  • 1Niels Bohr Institute, Physics of Ice, Climate and Earth, Copenhagen, Denmark (irenemalegiannaki@gmail.com)
  • 2Ca' Foscari University of Venice, Department of Environmental Sciences, Informatics and Statistics, Venice, Italy
  • 3Institute of Polar Sciences, National Research Council (CNR-ISP), Venice, Italy
  • 4Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
  • 5Centre for Earth Observation Science, University of Manitoba, Winnipeg, Canada
  • 6Teledyne Photon Machines, Bozeman, MT USA

Addressing the intricate challenges of water isotope analysis in polar ice cores, especially in extracting detailed climate records from older and thinner ice layers, the innovative integration of Laser Ablation (LA) with Cavity Ring Down Spectroscopy (CRDS) is introduced. The micro-destructive LA technique, which employs a nanosecond excimer pulsed laser operating at 193 nm for ice surface irradiation, demonstrates potential in achieving continuous, high-resolution sampling and gas phase sample generation, complementing the CRDS analyzer's precision in measuring water isotopes in gaseous state. Recent advancements include the successful adaptation of an existing LA system, previously coupled with an Inductively Coupled Plasma - Mass Spectrometer (ICP-MS) for ice core impurity analysis, to establish a connection with the CRDS analyzer. This was accomplished by making adjustments to the coupling procedure and laser parameters, to ensure efficient gas sample generation and robust delivery for water isotope analysis. A method for creating ice standard samples by transforming liquid water standards into ice yielded ice isotope standards, crucial for setting up initial measurement protocols. Their implementation on both standard ice samples and sections of ice cores revealed valuable insights into areas for improvement. This represents a significant step towards establishing a reliable method for high-quality water isotope analysis in ice cores, aiming to significantly enrich our understanding of long-term climate trends.

How to cite: Malegiannaki, E., Zannoni, D., Bohleber, P., Stremtan, C., Petteni, A., Stenni, B., Barbante, C., Dahl-Jensen, D., and Gkinis, V.: Advancing towards high-quality water isotope measurements in ice cores: a micro-destructive approach using Laser Ablation coupled with Cavity Ring Down Spectroscopy, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-12902, https://doi.org/10.5194/egusphere-egu24-12902, 2024.