EGU25-3750, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-3750
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Friday, 02 May, 09:25–09:35 (CEST)
 
Room 0.11/12
Surface topography and ice nucleation activity of alkali feldspar
David Andreas Heuser1, Michael Hagn1, Johanna Seidel2, Elena Petrishcheva1, Rainer Abart1, and Alexei Kiselev2
David Andreas Heuser et al.
  • 1University of Vienna, Department of Lithospheric Research, Vienna, Austria
  • 22Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany

Alkali feldspar undergoes a variety of phase transformations during cooling from magmatic crystallization leading to increasing ordering of Al and Si on the tetrahedrally coordinated lattice sites and to grain-internal microstructures such as twins and exsolution lamellae and associated surface topography. Both, Al-Si ordering as well as the specific surface topography may contribute to the extraordinary ice nucleation activity of alkali feldspar. We studied seven natural alkali feldspars ranging from homogeneous and featureless gem-quality sanidine with disordered Al-Si to hydrothermally altered microcline with ordered Al-Si, several generations of exsolution lamellae and micropore-rich regions associated with domains of hydrothermal albitization. (010) and (001) cleavage plates were produced from each feldspar sample and mounted in a cooling stage. Then an array of 7nl droplets of ultra-pure water was applied and cooled at 2 K/min. Droplet freezing events were recorded with an infrared camera.

The highest freezing temperatures are observed on (010) cleavage plates of K-rich (XK=0.94) microcline that exhibits 1-8 µm wide albite exsolution lamellae and 20-100 µm wide microporous regions along cracks related to hydrothermal albitization. In contrast, featureless (001) plates of gem-quality sanidines show freezing at over 10 K lower temperatures. The enhanced ice nucleation activity is tentatively ascribed to Si-Al ordering [1] and to heterogeneous ice nucleation on the surface features related to the grain-internal microstructures [2]. Which one of the two factors is more important is still unresolved.

 

[1] Franceschi G., Conti A., Lezuo L., Abart R.,  Mittendorfer F., Schmid M., Diebold U. (2023) How Water Binds to Microcline Feldspar (001), J. Phys. Chem. Lett., Vol. 15, 1, 15–22, https://doi.org/10.1021/acs.jpclett.3c03235

[2] Kiselev, A., Keinert, A., Gaedeke, T., Leisner, T., Sutter, C., Petrishcheva, E., Abart, R. (2021) Effect of chemically induced fracturing on the ice nucleation activity of alkali feldspar. Atmospheric Chemistry and Physics, 21 (15): 11801-11814, DOI 10.5194/acp-21-11801-2021

How to cite: Heuser, D. A., Hagn, M., Seidel, J., Petrishcheva, E., Abart, R., and Kiselev, A.: Surface topography and ice nucleation activity of alkali feldspar, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-3750, https://doi.org/10.5194/egusphere-egu25-3750, 2025.