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NH3 adsorption and competition with H2O on a hydroxylated aluminosilicate surface

  • Giada Franceschi
  • , Andrea Conti
  • , Luca Lezuo
  • , Rainer Abart
  • , Florian Mittendorfer
  • , Michael Schmid
  • , Ulrike Diebold

Veröffentlichungen: Beitrag in FachzeitschriftArtikelPeer Reviewed

Abstract

The interaction between ammonia (NH3) and (alumino)silicates is of fundamental and applied importance, yet the specifics of NH3 adsorption on silicate surfaces remain largely unexplored, mainly because of experimental challenges related to their electrically insulating nature. An example of this knowledge gap is evident in the context of ice nucleation on silicate dust, wherein the role of NH3 for ice nucleation remains debated. This study explores the fundamentals of the interaction between NH3 and microcline feldspar (KAlSi3O8), a common aluminosilicate with outstanding ice nucleation abilities. Atomically resolved non-contact atomic force microscopy, x-ray photoelectron spectroscopy, and density functional theory-based calculations elucidate the adsorption geometry of NH3 on the lowest-energy surface of microcline, the (001) facet, and its interplay with surface hydroxyls and molecular water. NH3 and H2O are found to adsorb molecularly in the same adsorption sites, creating H-bonds with the proximate surface silanol (Si-OH) and aluminol (Al-OH) groups. Despite the closely matched adsorption energies of the two molecules, NH3 readily yields to replacement by H2O, challenging the notion that ice nucleation on microcline proceeds via the creation of an ordered H2O layer atop pre-adsorbed NH3 molecules.

OriginalspracheEnglisch
Aufsatznummer164312
FachzeitschriftJournal of Chemical Physics
Jahrgang160
Ausgabenummer16
DOIs
PublikationsstatusVeröffentlicht - 28 Apr. 2024

Fördermittel

This work was supported by the European Research Council (ERC) under the European Union\u2019s Horizon 2020 research and innovation program (Grant Agreement No. 883395, Advanced Research Grant \u201CWatFun\u201D). The computational results presented have been achieved using the Vienna Scientific Cluster (VSC). Priv-Doz. Uwe Kolitsch from the Natural History Museum in Vienna is acknowledged for providing the samples used for this work. The authors acknowledge TU Wien Bibliothek for financial support through its Open Access Funding Programme.

ÖFOS 2012

  • 105120 Petrologie

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