CO
2
electroreduction
(CO
2
RR) is a sustainable
alternative for producing fuels and chemicals. Metal cations in the
electrolyte have a strong impact on the reaction, but mainly alkali
species have been studied in detail. In this work, we elucidate how
multivalent cations (Li
+
, Cs
+
, Be
2+
, Mg
2+
, Ca
2+
, Ba
2+
, Al
3+
, Nd
3+
, and Ce
3+
) affect CO
2
RR and
the competing hydrogen evolution by studying these reactions on polycrystalline
gold at pH = 3. We observe that cations have no effect on proton reduction
at low overpotentials, but at alkaline surface pH acidic cations undergo
hydrolysis, generating a second proton reduction regime. The activity
and onset for the water reduction reaction correlate with cation acidity,
with weakly hydrated trivalent species leading to the highest activity.
Acidic cations only favor CO
2
RR at low overpotentials and
in acidic media. At high overpotentials, the activity for CO increases
in the order Ca
2+
< Li
+
< Ba
2+
< Cs
+
. To favor this reaction there must be an interplay
between cation stabilization of the *CO
2
–
intermediate, cation accumulation at the outer Helmholtz plane (OHP),
and activity for water reduction.
Ab initio
molecular
dynamics simulations with explicit electric field show that nonacidic
cations show lower repulsion at the interface, accumulating more at
the OHP, thus triggering local promoting effects. Water dissociation
kinetics is increasingly promoted by strongly acidic cations (Nd
3+
, Al
3+
), in agreement with experimental evidence.
Cs
+
, Ba
2+
, and Nd
3+
coordinate to
adsorbed CO
2
steadily; thus they enable *CO
2
–
stabilization and barrierless protonation to
COOH and further reduction products.