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Facile Preparation of Ultrafine Aluminum Hydroxide Particles with or without Mesoporous MCM-41 in Ambient Environments
Published on: May 11, 2017
NH3 adsorption and competition with H2O on a hydroxylated aluminosilicate surface
Giada Franceschi1, Andrea Conti1, Luca Lezuo1
1Institute of Applied Physics, TU Wien, 1040 Vienna, Austria.
Ammonia (NH3) and water (H2O) adsorb similarly on microcline feldspar, but water displaces ammonia. This challenges theories on ammonia's role in ice nucleation on silicate dust.
Area of Science:
- Geochemistry
- Surface Science
- Atmospheric Chemistry
Background:
- The interaction of ammonia (NH3) with aluminosilicates is crucial but poorly understood due to experimental challenges with insulating materials.
- A knowledge gap exists regarding NH3's role in ice nucleation on silicate dust, with its precise function remaining debated.
Purpose of the Study:
- To investigate the fundamental interactions between NH3 and microcline feldspar (KAlSi3O8), a key ice-nucleating mineral.
- To elucidate the adsorption behavior of NH3 on the microcline (001) surface and its interplay with surface hydroxyls and water.
Main Methods:
- Atomically resolved non-contact atomic force microscopy (nc-AFM)
- X-ray photoelectron spectroscopy (XPS)
- Density functional theory (DFT)-based calculations
Main Results:
- NH3 and H2O adsorb molecularly at identical sites on the microcline (001) surface, forming hydrogen bonds with surface silanol (Si-OH) and aluminol (Al-OH) groups.
- Adsorption energies for NH3 and H2O are closely matched.
- NH3 is readily replaced by H2O on the surface.
Conclusions:
- NH3 and H2O compete for the same adsorption sites on microcline feldspar.
- The findings challenge the hypothesis that ice nucleation on microcline involves an ordered H2O layer forming on pre-adsorbed NH3 molecules.
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