Partial dissociation of water on Fe3O4(001): adsorbate induced charge and orbital order.
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 (square root of 2 x square root of 2)R45 degrees 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).
Mulakaluri
Narasimham
N
Department of Earth and Environmental Sciences, University of Munich, Theresienstr. 41, 80333 Munich, Germany.
Pentcheva
Rossitza
R
Wieland
Maria
M
Moritz
Wolfgang
W
Scheffler
Matthias
M