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Light changes the atmospheric reactivity of soot.


ABSTRACT: Soot particles produced by incomplete combustion processes are one of the major components of urban air pollution. Chemistry at their surfaces lead to the heterogeneous conversion of several key trace gases; for example NO(2) interacts with soot and is converted into HONO, which rapidly photodissociates to form OH in the troposphere. In the dark, soot surfaces are rapidly deactivated under atmospheric conditions, leading to the current understanding that soot chemistry affects tropospheric chemical composition only in a minor way. We demonstrate here that the conversion of NO(2) to HONO on soot particles is drastically enhanced in the presence of artificial solar radiation, and leads to persistent reactivity over long periods. Soot photochemistry may therefore be a key player in urban air pollution.

SUBMITTER: Monge ME 

PROVIDER: S-EPMC2872373 | biostudies-literature | 2010 Apr

REPOSITORIES: biostudies-literature

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Light changes the atmospheric reactivity of soot.

Monge Maria Eugenia ME   D'Anna Barbara B   Mazri Linda L   Giroir-Fendler Anne A   Ammann Markus M   Donaldson D J DJ   George Christian C  

Proceedings of the National Academy of Sciences of the United States of America 20100106 15


Soot particles produced by incomplete combustion processes are one of the major components of urban air pollution. Chemistry at their surfaces lead to the heterogeneous conversion of several key trace gases; for example NO(2) interacts with soot and is converted into HONO, which rapidly photodissociates to form OH in the troposphere. In the dark, soot surfaces are rapidly deactivated under atmospheric conditions, leading to the current understanding that soot chemistry affects tropospheric chemi  ...[more]

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