The
oxygen evolution reaction (OER) from water requires the formation
of metastable, reactive oxygen intermediates to enable oxygen–oxygen
bond formation. Conversely, such reactive intermediates could also
structurally modify the catalyst. A descriptor for the overall catalytic
activity, the first electron and proton transfer OER intermediate
from water, (M–OH*), has been associated with significant distortions
of the metal–oxygen bonds upon charge-trapping. Time-resolved
spectroscopy of in situ, photodriven OER on transition metal oxide
surfaces has characterized M–OH* for the charge trapping and
the symmetry of the lattice distortions by optical and vibrational
transitions, respectively, but had yet to detect an interfacial strain
field arising from a surface coverage M–OH*. Here, we utilize
picosecond, coherent acoustic interferometry to detect the uniaxial
strain normal to the SrTiO3/aqueous interface directly
caused by Ti–OH*. The spectral analysis applies a fairly general
methodology for detecting a combination of the spatial extent, magnitude,
and generation time of the interfacial strain through the coherent
oscillations’ phase. For lightly n-doped SrTiO3,
we identify the strain generation time (1.31 ps), which occurs simultaneously
with Ti–OH* formation, and a tensile strain of 0.06% (upper
limit 0.6%). In addition to fully characterizing this intermediate
across visible, mid-infrared, and now GHz-THz probes on SrTiO3, we show that strain fields occur with the creation of some
M–OH*, which modifies design strategies for tuning catalytic
activity and provides insight into photo-induced degradation so prevalent
for OER. To that end, the work put forth here provides a unique methodology
to characterize intermediate-induced interfacial strain across OER
catalysts.