Abstract

The structural and magnetic properties of Fe monolayers and bilayers on the W(001) substrate and the effects of oxygen adsorption were determined using the all-electron total-energy local-density full-potential linearized augmented plane-wave method. The strong ferromagnetism of the free Fe monolayer is completely destroyed by the Fe-W interaction for monolayer Fe/W(001); instead, a c(2\ifmmode\times\else\texttimes\fi{}2) antiferromagnetic configuration becomes the ground state. For bilayer Fe/W(001), a tetragonal rather than bcc structure is formed. The ferromagnetism of the previous ``dead'' Fe layer is restored by the additional adsorbed Fe layer; the magnetic moment in the interface and surface Fe layers increase to 1.68${\mathrm{\ensuremath{\mu}}}_{\mathit{B}}$ and 2.43${\mathrm{\ensuremath{\mu}}}_{\mathit{B}}$, respectively. These ferromagnetic Fe layers induce a sizable magnetic moment (0.22${\mathrm{\ensuremath{\mu}}}_{\mathit{B}}$) in the interfacial W layer. Finally, oxygen adsorption on bilayer Fe/W(001) is found to decrease greatly the magnetism of the interfacial Fe layer---to only 0.7${\mathrm{\ensuremath{\mu}}}_{\mathit{B}}$---but not to affect the top Fe layer.

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