[Zurück]

F. Mirabella, J. Balajka, J. Pavelec, M. Göbel, F. Kraushofer, M. Schmid, G. Parkinson, U. Diebold:
"Atomic-scale studies of Fe₃O₄(001) and TiO₂(110) surfaces following immersion in CO₂ acidified water";
ChemPhysChem, 21 (2020), S. 1788 - 1796.

Difficulties associated with the integration of liquids into a UHV environment make surface‐science style studies of mineral dissolution particularly challenging. Recently, we developed a novel experimental setup for the UHV‐compatible dosing of ultrapure liquid water and studied its interaction with TiO2 and Fe3O4 surfaces. Herein, we describe a simple approach to vary the pH through the partial pressure of CO2 (urn:x-wiley:14394235:media:cphc202000471:cphc202000471-math-0001 ) in the surrounding vacuum chamber and use this to study how these surfaces react to an acidic solution. The TiO2(110) surface is unaffected by the acidic solution, except for a small amount of carbonaceous contamination. The Fe3O4(001)‐(urn:x-wiley:14394235:media:cphc202000471:cphc202000471-math-0002 ×urn:x-wiley:14394235:media:cphc202000471:cphc202000471-math-0003 )R45° surface begins to dissolve at a pH 4.0-3.9 (urn:x-wiley:14394235:media:cphc202000471:cphc202000471-math-0004 =0.8-1 bar) and, although it is significantly roughened, the atomic‐scale structure of the Fe3O4(001) surface layer remains visible in scanning tunneling microscopy (STM) images. X‐ray photoelectron spectroscopy (XPS) reveals that the surface is chemically reduced and contains a significant accumulation of bicarbonate (HCO3−) species. These observations are consistent with Fe(II) being extracted by bicarbonate ions, leading to dissolved iron bicarbonate complexes (Fe(HCO3)2), which precipitate onto the surface when the water evaporates.

CO2 dissolution magnetite TiO2 water drop

http://dx.doi.org/10.1002/cphc.202000471

http://dx.doi.org/10.1002/cphc.202000471