2022
DOI: 10.1021/acs.jpca.2c00291
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Catalytic Coupling of Free Radical Oxidation and Electrophilic Chlorine Addition by Phase-Transfer Intermediates in Liquid Aerosols

Abstract: While examining the heterogeneous reaction of chlorine atoms with alkenes, in the presence of Cl2, we have observed an unexpectedly large enhancement of reactivity and the predominance of chlorinated reaction products even under high O2 conditions, where Cl atom recycling is expected to be minimal. These observations cannot be explained by known free radical oxidation or cycling mechanisms, but rather we find evidence for the multiphase catalytic coupling of free radical oxidation with electrophilic Cl2 additi… Show more

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Cited by 2 publications
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“…Aqueous aerosols are known to control cloud nucleation and to affect the climate, air quality, and human health. A complete understanding of their role in atmospheric phenomena remains challenging as the properties of nanometric aqueous particles differ greatly from those of a bulk solution. The chemical evolution of atmospheric aerosols as well as their ability to initiate cloud formation is mostly controlled by the properties of the gas–water interface. , Phenomena such as microconfinement, high surface electric field, preferred molecular orientation, ,,, and lower water densities at the interface , affect reaction rates , and photochemical processes, thus enhancing certain reaction channels while suppressing others. Because atmospheric aerosols contain a wide range of solutes, it has become important to improve our understanding of how chemical composition changes surface reactivity …”
Section: Introductionmentioning
confidence: 99%
“…Aqueous aerosols are known to control cloud nucleation and to affect the climate, air quality, and human health. A complete understanding of their role in atmospheric phenomena remains challenging as the properties of nanometric aqueous particles differ greatly from those of a bulk solution. The chemical evolution of atmospheric aerosols as well as their ability to initiate cloud formation is mostly controlled by the properties of the gas–water interface. , Phenomena such as microconfinement, high surface electric field, preferred molecular orientation, ,,, and lower water densities at the interface , affect reaction rates , and photochemical processes, thus enhancing certain reaction channels while suppressing others. Because atmospheric aerosols contain a wide range of solutes, it has become important to improve our understanding of how chemical composition changes surface reactivity …”
Section: Introductionmentioning
confidence: 99%