EGU21-15629
https://doi.org/10.5194/egusphere-egu21-15629
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

The Quasi-Liquid Layer on ice observed with NEXAFS

Jérôme Gabathuler1, Yanisha Manoharan1, Huanyu Yang1, Anthony Boucly2, Luca Artiglia2, Markus Ammann1, and Thorsten Bartels-Rausch1
Jérôme Gabathuler et al.
  • 1Surface chemistry, PSI, villigen, Switzerland
  • 2LSK, PSI, villigen, Switzerland

The Quasi-Liquid Layer on ice observed with NEXAFS

Gabathuler, Y. Manoharan, H. Yang, A. Boucly, A. Luca, M. Ammann, T. Bartels-Rausch

Paul Scherrer Institute, Villigen, Switzerland

 

 

As temperature approaches the melting point of ice from below, the hydrogen-bonding network at the air – ice interface evolves from a well-defined hexagonal structure towards more randomly spatialized interactions. The general agreement is that a Quasi-Liquid-Layer (QLL) exists at the surface of the ice, and reports on the thickness of this disordered interfacial layer range from 2 nm to 25 nm at 271 K, depending on the probing technique (atomic force microscopy (AFM), ellipsometry, optical reflectivity, sum-frequency generation (SFG)) [1]. These large differences partly arise from the fact that the different techniques are probing different properties of the interface, and the delicate calibration into the thickness of the QLL contributes greatly to the uncertainty.

 

We investigate the QLL using Near Edge X-ray Absorption Fine Structure (NEXAFS) spectroscopy, as Bluhm and his group did in 2002 [2]. The technique probes Auger electrons emitted upon X-ray absorption, thus, NEXAFS becomes inherently sensitive to the upper few nm of the air-ice interfacial region. This work focuses on the probing depth associated with this method and proposes a comprehensive treatment of the data, to help resolve the discrepancy of current thickness data. The importance of the QLL’s thickness comes from its contribution to environmental science as a reservoir for chemical impurities and as a host of chemical reactions with an impact on atmospheric and cryospheric composition.

 

We will present a first data set of NEXAFS from neat ice between – 40 °C and 0°C acquired at the ISS endstation at the Swiss Light Source of the Paul Scherrer Institute. Results including error bars will be compared to earlier studies. The preliminary analysis suggests that the interfacial disorder seems to be less pronounced than reported in many earlier studies, very much in agreement with recent SFG [3] and AFM data [4].

 

 

 

Literature References:

 

 

Acknowledgment:

We thank A. Laso for technical help, SNF for funding (grant 178962)

 

How to cite: Gabathuler, J., Manoharan, Y., Yang, H., Boucly, A., Artiglia, L., Ammann, M., and Bartels-Rausch, T.: The Quasi-Liquid Layer on ice observed with NEXAFS, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-15629, https://doi.org/10.5194/egusphere-egu21-15629, 2021.

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