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. 2018 Nov 20;9:4896. doi: 10.1038/s41467-018-07281-z

Table 1.

Visible-light driven water oxidation by 1a

Entry Oxidantb Catalyst Lightc Solvent O2 (μmol g−1)d
1 S2O82– 1 Visible H2O 1025
2 IO4 1 Visible H2O 6300
3 None 1 Visible H2O 0
4 IO4 None Visible H2O 0
5 IO4 1 Dark H2O 0
6 IO4 {[α-PW11O39Fe]2O}10– (2)e Dark H2O 60 ± 20
7 IO4 {[α-PW11O39Fe]2O}10– (2)e Visible H2O 60 ± 20
8 IO4 Fe3+ f Visible H2O 0
9 IO4 1g Visible Dry MeCN 0
10 IO4 1g Visible 1:1 H2O:MeCN 1640

aAll reactions were carried out at pH 8 for 8 h (40 ± 1 °C)

bOxidant concentrations were 20 mM

cLight source was a 150 W Xe lamp with a λ ≥ 420-nm cutoff filter

dValues reported are per gram of the α-Fe2O3 cores, or of the catalysts listed in column three

eThese two control experiments (entries 6 and 7) rule out oxygen evolution by reaction of periodate with the Fe(III) atoms complexed within the hematite-bound POM ligands. They were carried out at pH 5 to ensure integrity of the molecular dimer, 2. In 8 h at pH 5, 1 gave 3200 μmol O2 g−1

fAfter air oxidation of FeSO4 at pH 5 and 8

gCarried out using an organic-solvent soluble form of 1, and R4N+IO4 (R = n-butyl)