Abstract
We analyzed the (0001) surface structures of hematite and chromia bulk single crystals by low energy electron diffraction (LEED). The hematite crystal was annealed in an O2 atmosphere, pO2≈3 × 10 -8mbar, for several hours. The chromia crystal was sputtered with Ar+ ions, E = 1keV, and afterward heated up to 900°C for 5min under ultra-high-vacuum (UHV) conditions. I(V)-curve data sets of 12 symmetrically independent diffraction spots were measured at room temperature in the energy range E = 150-500eV. Charging effects hindered measurements at lower energies. Our analysis of the hematite single crystal surface indicates that it is terminated by a single iron layer which is occupied at ≈50\%. Relaxation effects along the c-axis are quite large and involve several iron double layers. For the chromia surface the results indicate that termination with a single Cr seems not to hold. Most probably the surface is terminated by two partially occupied Cr sites or chromyl groups. Relaxations in deeper layers are small in contrast to α-Fe2O3(0001).
Item Type: | Journal article |
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Faculties: | Geosciences > Department of Earth and Environmental Sciences > Crystallography and Materials Science |
Subjects: | 500 Science > 550 Earth sciences and geology |
Language: | English |
Item ID: | 18919 |
Date Deposited: | 10. Mar 2014, 14:17 |
Last Modified: | 04. Nov 2020, 13:00 |