The dynamics of water
at mineral surfaces has attracted much attention
due to the marked differences, compared to the bulk, in the ability
of interfacial water populations to redistribute vibrational energy,
largely due to perturbations in the local hydrogen-bonding environments
at interfaces. However, many unanswered questions persist regarding
these geochemically and technologically relevant systems. The evolution
of our understanding and current state-of-the-art interpretation are
reviewed for three important mineral/aqueous interfaces (Al2O3, SiO2, and CaF2). While we focus
on time-resolved vibrational Sum Frequency Generation (vSFG), as it
is inherently surface specific, we include complementary time-resolved
techniques such as IR and THz spectroscopies, which combined can provide
a broader picture of interfacial dynamics at mineral surfaces. We
show that vibrational dynamics are uniquely positioned to inform on
structure at interfaces, which could be missed using conventional
static vibrational spectra. Insights presented here shine light on
previous successes and suggest future avenues for transient vibrational
spectroscopy at mineral/aqueous interfaces.