Abstract
The interaction of water with Fe3O4(001) is studied by density functional theory calculations including an on-site Coulomb term. For isolated molecules, dissociative adsorption is strongly promoted at surface defect sites, while at higher coverages a hydrogen-bonded network forms with alternating molecular and dissociated species. This mixed adsorption mode and a suppression of the (2×2)R45°reconstruction are confirmed by a quantitative low energy electron diffraction analysis. Adsorbate induced electron transfer processes add a new dimension towards understanding the catalytic activity of magnetite(001).
| Item Type: | Journal article |
|---|---|
| Faculties: | Geosciences > Department of Earth and Environmental Sciences > Crystallography and Materials Science |
| Subjects: | 500 Science > 530 Physics 500 Science > 540 Chemistry 500 Science > 550 Earth sciences and geology |
| URN: | urn:nbn:de:bvb:19-epub-18949-5 |
| Language: | English |
| Item ID: | 18949 |
| Date Deposited: | 10. Mar 2014 14:17 |
| Last Modified: | 04. Nov 2020 13:00 |

