Trends in the HER are studied on selected metals (M= Cu, Ag, Au, Pt, Ru, Ir,
Ti) in acid and alkaline environments. We found that with the exception of
Pt, Ir and Au, due to high coverage by spectator species on non-noble metal
catalysts, experimentally established positions of Cu , Ag, Ru and Ti in the
observed volcano relations are still uncertain. We also found that while in
acidic solutions the M-Hupd binding energy most likely is controlling the
activity trends, the trends in activity in alkaline solutions are controlled
by a delicate balance between two descriptors: the M-Had interaction as well
as the energetics required to dissociate water molecules. The importance of
the second descriptor is confirmed by introducing bifunctional catalysts
such as M modified by Ni(OH); e.g. while the latter serves to enhance
catalytic decomposition of water, the metal sites are required for
collecting and recombining the produced hydrogen intermediates.