Oxygen-Pressure-Limited Recovery of the Hematite {\alpha}-Fe$_2$O$_3$(0001) Surface from a Reduced Fe$_3$O$_4$(111)-Like Layer
Nishant Kumar, Matthias Blatnik, Jan \v{C}echal

TL;DR
This study investigates how oxygen pressure and temperature influence the oxidation and recovery of hematite surfaces, revealing oxygen supply as a key limiting factor in surface reconstruction processes.
Contribution
It provides real-time insights into the oxidation kinetics of hematite surfaces, highlighting the critical role of oxygen partial pressure and temperature in surface recovery.
Findings
Complete hematite surface recovery is linked to 2D honeycomb phase nucleation.
Higher temperatures accelerate nucleation but slow lateral growth at constant oxygen pressure.
Growth slows dramatically below an oxygen partial pressure threshold (~2×10^{-6} mbar).
Abstract
The oxidation kinetics of hematite {\alpha}-FeO(0001) surfaces are vital for its applications in catalysis, environmental remediation, and industrial processes. Despite prior studies, the roles of temperature, oxygen partial pressure, and oxygen chemical potential in controlling nucleation and growth kinetics are not fully understood. Using real-time Low Energy Electron Microscopy/Diffraction (LEEM/LEED), we systematically investigate the oxidation of a reduced FeO(111)-like surface layer to hematite under controlled conditions. We show that complete recovery of the hematite surface termination is closely linked to the nucleation and lateral growth of a two-dimensional honeycomb (H) phase. While higher temperatures accelerate nucleation, they slow lateral growth at constant oxygen pressure, indicating that oxygen supply limits the oxidation rate. Below an oxygen partial…
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