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Updated: Sep 3, 2026

Developing Photosensitizer-Cobaloxime Hybrids for Solar-Driven H2 Production in Aqueous Aerobic Conditions
Published on: October 5, 2019
Investigating the photosensitized chemistry of proxies for tropospheric brown carbon
Jiejing Kong1, Mingzhu He2, Jintao Liu2
1Guangdong Key Laboratory of Environmental Catalysis and Health Risk Control, School of Environmental Science and Engineering, Institute of Environmental Health and Pollution Control, Guangdong University of Technology, Guangzhou 510006, China; Universite Claude Bernard Lyon 1, CNRS, IRCELYON, UMR 5256, Villeurbanne, F-69100, France.
Abstract:
Brown carbon (BrC) profoundly influences secondary organic aerosol (SOA) formation via photosensitized reactions in atmospheric condensed phases, yet the intrinsic oxidative power of its excited triplet state remains mechanistically unresolved. We reveal that the BrC proxy 1,4-naphthoquinone (NQ) undergoes dual photochemical pathways in deoxygenated aqueous systems, simultaneous self-photoconversion and substrate oxidation, enabled by two distinct, long-lived triplet states (3NQ* and 3OH-NQ*) with 3(n, π*) configurations generated under 355 nm irradiation. Crucially, 3NQ* acts as an endogenous oxidant, driving efficient hydrogen abstraction from key organic classes without requiring external oxidants. Oxidation kinetics exhibit a striking hierarchy governed by bond dissociation energies and one-electron oxidation potentials: alkanes (104 M-1s-1) < oxygenated alkanes (105 M-1s-1) < phenols (106 M-1s-1). Radical intermediates (alkyl, alkoxyl, phenoxy) dehydrogenate into stable products (e.g., benzoquinone from phenol), while the self-photoconversion product OH-NQ regenerates a secondary triplet (3OH-NQ*), amplifying oxidative cascades. This establishes 3BrC* as the dominant sink for phenols in BrC-rich haze, particularly under acidic, O2-limited conditions. Our findings provide kinetic and mechanistic benchmarks for integrating triplet-state chemistry into atmospheric models, advancing predictions of SOA formation in regions plagued by severe particulate pollution.
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