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Surface-atmosphere exchange of inorganic water-soluble gases and associated ions in bulk aerosol above agricultural grassland pre- and postfertilisation

TitleSurface-atmosphere exchange of inorganic water-soluble gases and associated ions in bulk aerosol above agricultural grassland pre- and postfertilisation
Publication TypeJournal Article
Year of Publication2018
AuthorsRamsay R., Di Marco C.F, Heal M.R, Twigg M.M, Cowan N., Jones M.R, Leeson S.R, Bloss W.J, Kramer L.J, Crilley L., Sorgel M., Andreae M., Nemitz E.
JournalAtmospheric Chemistry and Physics
Date Published2018/11
Type of ArticleArticle
ISBN Number1680-7316
Accession NumberWOS:000451729400002
Keywordsambient air; ammonia exchange; annular; denuder; dry deposition; flux measurements; Meteorology & Atmospheric Sciences; particle deposition; reactive nitrogen-compounds; sulfur-dioxide; surface/atmosphere exchange; technical note

The increasing use of intensive agricultural practices can lead to damaging consequences for the atmosphere through enhanced emissions of air pollutants. However, there are few direct measurements of the surface-atmosphere exchange of trace gases and water-soluble aerosols over agricultural grassland, particularly of reactive nitrogen compounds. In this study, we present measurements of the concentrations, fluxes and deposition velocities of the trace gases HCl, HONO, HNO3, S-2 and NH3 as well as their associated water-soluble aerosol counterparts Cl-, NO2-, NO3-, SO42- and NH(4)(+ )as determined hourly for 1 month in May-June 2016 over agricultural grassland near Edinburgh, UK, pre- and postfertilisation. Measurements were made using the Gradient of Aerosols and Gases Online Registrator (GRAEGOR) wet-chemistry two-point gradient instrument. Emissions of NH3 peaked at 1460 ng m(-2) s(-1) 3h after fertilisation, with an emission of HONO peaking at 4.92 ng m(-2) s(-1) occurring 5h after fertilisation. Apparent emissions of NO3- aerosol were observed after fertilisation which, coupled with a divergence of HNO3 deposition velocity (V-d) from its theoretical maximum value, suggested the reaction of emitted NH3 with atmospheric HNO3 to form ammonium nitrate aerosol. The use of the conservative exchange fluxes of tot-NH4+ and tot-NO3- indicated net emission of tot-NO3-, implying a ground source of HNO(3 )after fertilisation. Daytime concentrations of HONO remained above the detection limit (30 ng m(-3)) throughout the campaign, suggesting a daytime source for HONO at the site. Whilst the mean V-d of NH4+ was 0.93 mm s(-1) in the range expected for the accumulation mode, the larger average V-d for Cl- (3.65 mm s(-1)), NO3- (1.97 mm s(-1)) and SO42- (1.89 mm s(-1)) reflected the contribution of a super-micron fraction and decreased with increasing PM2.5/PM10 ratio (a proxy measurement for aerosol size), providing evidence - although limited by the use of a proxy for aerosol size - of a size dependence of aerosol deposition velocity for aerosol chemical compounds, which has been suggested from process-orientated models of aerosol deposition.

Short TitleAtmos. Chem. Phys.
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