Surface chemical characterization and surface diffraction effects of real margarite (001): An angle-resolved XPS investigation

Citation
Gg. Biino et al., Surface chemical characterization and surface diffraction effects of real margarite (001): An angle-resolved XPS investigation, AM MINERAL, 84(4), 1999, pp. 629-638
Citations number
46
Categorie Soggetti
Earth Sciences
Journal title
AMERICAN MINERALOGIST
ISSN journal
0003004X → ACNP
Volume
84
Issue
4
Year of publication
1999
Pages
629 - 638
Database
ISI
SICI code
0003-004X(199904)84:4<629:SCCASD>2.0.ZU;2-5
Abstract
The (001) surface of natural pure margarite was chemically characterized by angle-resolved Xray photoelectron spectroscopy (ARXPS). The extreme surfac e sensitivity of ARXPS permits concluding that the chemical composition of the near-surface region differs from the bulk because of the strong anisotr opy of the margarite structure. Depth profiling was carried out by angle re solved spectroscopy that is a non destructive measuring technique. More gra zing polar angles sample increasingly superficial layers of the margarite. The topmost layers are made up of C, due to the mineral/atmosphere interact ion. At low grazing angles the concentration of Si increases, and both Al a nd Ca decreases; therefore we conclude that the tetrahedral sheet is the to pmost monolayer. Repulsion between the octahedral and tetrahedral sheets is probably responsible for the cleavage. Photoelectron diffraction effects a re also clearly evidenced by Si, Ca, and Al. Single-scattering cluster calc ulations were performed in simulating scanned angle core emission. The calc ulated patterns do not show a reasonable agreement with experimental data.