Hydrogen
production by electrochemical water splitting is limited
by the sluggish oxygen evolution reaction (OER). In order to improve
our understanding of the underlying mechanisms, information about
the atomic surface structure of the active state of the electrode
is required. Here, we present environmental transmission electron
microscopy studies of Ca-birnessite (K0.20Ca0.21MnO2.21·1.4H2O) electrodes under conditions
close to those of the OER. Remarkably, in H2O vapor, a
highly dynamic state of the surface and subsurface develops with a
thickness of the formed dynamic layer of up to 0.6 nm, which is absent
in O2 and inert gases. Electron beam-induced effects are
carefully studied, showing high stability of the material against
radiation damage in high vacuum until a dose rate of 42,000 e–/(Å2 s). In contrast, in H2O, the dynamic surface layer develops and forms a stationary state
even at low dose rates, down to 5000 e–/(Å2 s). Electron energy-loss spectroscopy reveals an increase
in the Mn oxidation state in H2O and in O2 ambient.
Our results are interpreted as the formation of a few-angstrom-thick,
dynamic, and hydrated surface layer of birnessite in H2O, with an increased Mn valence state. Such a dynamic surface layer
with a flexible Mn coordination and valence state might be optimal
for oxygen evolution due to the higher effective interaction volume
beyond the surface area and a flexible bond coordination of partially
hydrated Mn species.