To that end, we have performed DFT-based theoretical studies of the ORR on metals. Previously we have shown that the intrinsic activity of oxygen reduction by Li forms a volcano-like trend with respect to the adsorption energy of oxygen on different metals.5 Similar to the hydrogen version of the ORR, Pt and Pd are likewise found to be the most active metals and are located at the top of the volcano. The aprotic nature of non-aqueous Li-O2 cells, however, makes the one-electron reduction of O2 to the superoxide anion (O2-) possible besides concerted Li+/e- transfer, and indeed often at higher potential than molecular LiO2.5 Our calculations, in conjunction with spectro-electrochemical studies, now identify O2- as a common intermediate in dimethyl sulfoxide (DMSO) electrolytes containing proton or lithium.6 When the DMSO contains a poor proton source, O2- appears as the first stable intermediate during the ORR, with H2O2 appearing at higher overpotentials. When DMSO contains a Li+ source instead, O2- is again the first reaction intermediate, whereas surface LiO2 does not appear until the potential is much more negative of bulk Li2O2 formation potential. Therefore, the superoxide anion plays a key role in the ORR under a diverse range of electrode conditions, and needs to be taken into consideration when predicting the activity of ORR in non-aqueous Li-O2 cells.
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