Investigating PAH relative reactivity using congener profiles, quinone measurements and back trajectories

M. S. Alam, Juana Maria Delgado Saborit, C. Stark, Roy Harrison

Research output: Contribution to journalArticlepeer-review

174 Downloads (Pure)


Abstract. Vapour and particle-associated concentrations of 15 polycyclic aromatic hydrocarbons (PAH) and 11 PAH quinones have been measured in winter and summer campaigns at the rural site, Weybourne in eastern England. Concentrations of individual PAH are 20–140 times smaller than average concentrations at an English urban site. The concentrations of PAH are greatest in air masses originating from southern England relative to those from Scandinavia and the North Atlantic, while quinone to parent PAH ratios show an inverse behaviour, being highest in the more aged North Atlantic polar air masses. While concentration of 1,2-naphthoquinone decline from summer to winter, those of 1,4-naphthoquinone and anthraquinone increase suggesting a photochemical formation pathway. A comparison of congener concentration profiles measured at Weybourne with those from an urban source area (Birmingham) reveals differential losses at the rural site, especially evident in fluoranthene: pyrene ratios and consistent with the known rates of vapour phase reactions of 3 and 4 ring compounds with hydroxyl radical. The ratios of quinones to their parent PAH at Weybourne are greater than those in the urban source area indicating either more rapid loss processes for PAH, or formation of quinones during advection of the air mass, or probably both.
Original languageEnglish
Pages (from-to)25741-25768
JournalAtmospheric Chemistry and Physics Discussions
Issue number10
Publication statusPublished - 2013

Bibliographical note

This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.


Dive into the research topics of 'Investigating PAH relative reactivity using congener profiles, quinone measurements and back trajectories'. Together they form a unique fingerprint.

Cite this