Fig. 2: Observation of the oxygen exchange between H218O and α-Fe216O3 by TPD and LEIS.
From: Rapid oxygen exchange between hematite and water vapor

a TPD spectrum (1 K/s) after a dose of ≈1.9 H218O/u.c. at 120 K. The β peak is observed mostly in the m/e = 20 signal, while the γ peak desorbs in two channels of similar intensity, indicating substantial oxygen exchange with the α-Fe216O3 substrate. b Oxygen exchange observed during 2.7 × 10−8 mbar H218O exposure at 350 K. Upon opening of the molecular beam shutter, roughly 1/3 of the signal is observed in the m/e = 18 channel. After ca. 360 s, almost all the signal is contained in the m/e = 20 channel due to the saturation of the surface with 18O. The overall water signal remains constant. c LEIS characterization (1 keV He+, scattering angle 90°) of the α-Fe216O3 as prepared (top), after the H218O exposure as shown in b (middle) and after a single H218O TPD experiment (bottom). The latter two spectra show substantial enrichment of the α-Fe216O3 surface with 18O. Source data are provided as a Source Data file.