Utilizing the oxygen-atom trapping effect of Co 3 O 4 with oxygen vacancies to promote chlorite activation for water decontamination

Heterogeneous high-valent cobalt-oxo [≡Co(IV)=O] is a widely focused reactive species in oxidant activation; however, the relationship between the catalyst interfacial defects and ≡Co(IV)=O formation remains poorly understood. Herein, photoexcited oxygen vacancies (OVs) were introduced into Co 3 O 4 (OV-Co 3 O 4 ) by a UV-induced modification method to facilitate chlorite (ClO 2 – ) activation. Density functional theory calculations indicate that OVs result in low-coordinated Co atom, which can directionally anchor chlorite under the oxygen-atom trapping effect. Chlorite first undergoes homolytic O–Cl cleavage and transfers the dissociated O atom to the low-coordinated Co atom to form reactive ≡Co(IV)=O with a higher spin state. The reactive ≡Co(IV)=O rapidly extracts one electron from ClO 2 – to form chlorine dioxide (ClO 2 ), accompanied by the Co atom returning a lower spin state. As a result of the oxygen-atom trapping effect, the OV-Co 3 O 4 /chlorite system achieved a 3.5 times higher efficiency of sulfamethoxazole degradation (~0.1331 min −1 ) than the pristine Co 3 O 4 /chlorite system. Besides, the refiled OVs can be easily restored by re-exposure to UV light, indicating the sustainability of the oxygen atom trap. The OV-Co 3 O 4 was further fabricated on a polyacrylonitrile membrane for back-end water purification, achieving continuous flow degradation of pollutants with low cobalt leakage. This work presents an enhancement strategy for constructing OV as an oxygen-atom trapping site in heterogeneous advanced oxidation processes and provides insight into modulating the formation of ≡Co(IV)=O via defect engineering.