Franceschi Giada, Brandstetter Sebastian, Balajka Jan, Sokolović Igor, Pavelec Jiří, Setvín Martin, Schmid Michael, Diebold Ulrike
Institute of Applied Physics, TU Wien, Wiedner Hauptstraße 8-10/E134, 1040 Wien, Austria.
Department of Surface and Plasma Science, Charles University in Prague, V Holesovickach 2, 180 00 Praha, Czech Republic.
Faraday Discuss. 2024 Feb 6;249(0):84-97. doi: 10.1039/d3fd00093a.
Natural minerals contain ions that become hydrated when they come into contact with water in vapor and liquid forms. Muscovite mica - a common phyllosilicate with perfect cleavage planes - is an ideal system to investigate the details of ion hydration. The cleaved mica surface is decorated by an array of K ions that can be easily exchanged with other ions or protons when immersed in an aqueous solution. Despite the vast interest in the atomic-scale hydration processes of these K ions, experimental data under controlled conditions have remained elusive. Here, atomically resolved non-contact atomic force microscopy (nc-AFM) is combined with X-ray photoelectron spectroscopy (XPS) to investigate the cation hydration upon dosing water vapor at 100 K in ultra-high vacuum (UHV). The cleaved surface is further exposed to ultra-clean liquid water at room temperature, which promotes ion mobility and partial ion-to-proton substitution. The results offer the first direct experimental views of the interaction of water with muscovite mica under UHV. The findings are in line with previous theoretical predictions.
天然矿物质含有离子,当它们与气态和液态水接触时会发生水合作用。白云母——一种具有完美解理面的常见层状硅酸盐——是研究离子水合作用细节的理想体系。劈开的云母表面排列着一系列钾离子,当浸入水溶液中时,这些钾离子很容易与其他离子或质子发生交换。尽管人们对这些钾离子的原子尺度水合过程有着浓厚的兴趣,但在可控条件下的实验数据仍然难以获得。在这里,原子分辨非接触原子力显微镜(nc-AFM)与X射线光电子能谱(XPS)相结合,以研究在超高真空(UHV)中于100 K下注入水蒸气时的阳离子水合作用。劈开的表面在室温下进一步暴露于超清洁液态水中,这促进了离子迁移和部分离子与质子的置换。这些结果提供了在超高真空下,水与白云母相互作用的首个直接实验观察结果。这些发现与先前的理论预测一致。