Recovery of the hematite α-Fe₂O₃(0001) surface from a reduced Fe₃O₄(111)-like layer occurs via nucleation and lateral growth of a 2D honeycomb phase and is limited by oxygen partial pressure below ~2×10^{-6} mbar.
Defects and Cation Diffusi on in Magnetite (II)
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Oxygen-Pressure-Limited Recovery of the Hematite {\alpha}-Fe$_2$O$_3$(0001) Surface from a Reduced Fe$_3$O$_4$(111)-Like Layer
Recovery of the hematite α-Fe₂O₃(0001) surface from a reduced Fe₃O₄(111)-like layer occurs via nucleation and lateral growth of a 2D honeycomb phase and is limited by oxygen partial pressure below ~2×10^{-6} mbar.