Marine short-lived halogenated compounds, emitted from algae, phytoplankton, and other marine biota, significantly affect both the troposphere and the stratosphere. Here, we show that such compounds might also be photochemically produced through photosensitized reactions in surface water. Gas-phase products were detected and identified by high-resolution mass spectrometry, more particularly by means of an atmospheric pressure chemical ionization source coupled to an Orbitrap mass spectrometer. Under simulated solar irradiation, halogenated organic compounds were produced and detected in the gas phase when a proxy of dissolved organic matter, i.e., 4-benzoylbenzoic acid, was excited into its triplet state. We present a mechanism explaining t...
Benzene, toluene, ethylbenzene and xylenes can contribute to hydroxyl reactivity and secondary aeros...
Trace gases comprise less than 1% of the Earth's atmosphere, but are responsible for numerous proces...
This document is the Accepted Manuscript version of a Published Work that appeared in final form in ...
SSCI-VIDE+CARE+MRT:CEM:SPR:CGOInternational audienceMarine short-lived halogenated compounds, emitte...
SSCI-VIDE+CARE+MRT:CGONational audienceAir/water interfaces are omnipresent in the environment, and ...
Diatomic halogen molecules diffusing into the marine atmosphere are photodissociated to atoms in day...
Photochemical halogenation of dissolved organic matter (DOM) may represent an important abiotic proc...
Reactions of dissolved organic matter (DOM) with photochemically generated reactive halogen species ...
Sea-spay aerosols (SSA) released from the marine boundary layer (MBL) through wave breaking and bubb...
International audiencePolycyclic aromatic hydrocarbons and dimethyl sulfoxide (DMSO) are ubiquitous ...
Photochemical halogenation of dissolved organic matter (DOM) may represent an important abiotic proc...
ABSTRACT: We report on experiments that probe photosensitized chemistry at the air/water interface, ...
Halogens play key roles in the chemical composition of marine boundary layers, the free troposphere ...
Ultrahigh resolution mass spectrometry of marine dissolved organic matter (DOM) has suggested the pr...
The ocean plays a significant role in the trace gas composition of the atmosphere, via sea-to-air em...
Benzene, toluene, ethylbenzene and xylenes can contribute to hydroxyl reactivity and secondary aeros...
Trace gases comprise less than 1% of the Earth's atmosphere, but are responsible for numerous proces...
This document is the Accepted Manuscript version of a Published Work that appeared in final form in ...
SSCI-VIDE+CARE+MRT:CEM:SPR:CGOInternational audienceMarine short-lived halogenated compounds, emitte...
SSCI-VIDE+CARE+MRT:CGONational audienceAir/water interfaces are omnipresent in the environment, and ...
Diatomic halogen molecules diffusing into the marine atmosphere are photodissociated to atoms in day...
Photochemical halogenation of dissolved organic matter (DOM) may represent an important abiotic proc...
Reactions of dissolved organic matter (DOM) with photochemically generated reactive halogen species ...
Sea-spay aerosols (SSA) released from the marine boundary layer (MBL) through wave breaking and bubb...
International audiencePolycyclic aromatic hydrocarbons and dimethyl sulfoxide (DMSO) are ubiquitous ...
Photochemical halogenation of dissolved organic matter (DOM) may represent an important abiotic proc...
ABSTRACT: We report on experiments that probe photosensitized chemistry at the air/water interface, ...
Halogens play key roles in the chemical composition of marine boundary layers, the free troposphere ...
Ultrahigh resolution mass spectrometry of marine dissolved organic matter (DOM) has suggested the pr...
The ocean plays a significant role in the trace gas composition of the atmosphere, via sea-to-air em...
Benzene, toluene, ethylbenzene and xylenes can contribute to hydroxyl reactivity and secondary aeros...
Trace gases comprise less than 1% of the Earth's atmosphere, but are responsible for numerous proces...
This document is the Accepted Manuscript version of a Published Work that appeared in final form in ...