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
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.