文摘
Differential electrochemical mass spectrometry (DEMS) analysis of the oxygen isotopologues produced by <sup>18sup>O-labeled Co-OEC in H<sub>2sub><sup>16sup>O reveals that water splitting catalysis proceeds by a mechanism that involves direct coupling between oxygens bound to dicobalt edge sites of Co-OEC. The edge site chemistry of Co-OEC has been probed by using a dinuclear cobalt complex. <sup>17sup>O NMR spectroscopy shows that ligand exchange of OH/OH<sub>2sub> at Co(III) edge sites is slow, which is also confirmed by DEMS experiments of Co-OEC. In borate (B<sub>isub>) and phosphate (P<sub>isub>) buffers, anions must be displaced to allow water to access the edge sites for an O–O bond coupling to occur. Anion exchange in P<sub>isub> is slow, taking days to equilibrate at room temperature. Conversely, anion exchange in B<sub>isub> is rapid (k<sub>assocsub> = 13.1 ± 0.4 M<sup>–1sup> s<sup>–1sup> at 25 °C), enabled by facile changes in boron coordination. These results are consistent with the OER activity of Co-OEC in B<sub>isub> and P<sub>isub>. The P<sub>isub> binding kinetics are too slow to establish a pre-equilibrium sufficiently fast to influence the oxygen evolution reaction (OER), consistent with the zero-order dependence of P<sub>isub> on the OER current density; in contrast, B<sub>isub> exchange is sufficiently facile such that B<sub>isub> has an inhibitory effect on OER. These complementary studies on Co-OEC and the dicobalt edge site mimic allow for a direct connection, at a molecular level, to be made between the mechanisms of heterogeneous and homogeneous OER.