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The spatial distribution and particle size of some inorganic nitrogen, sulphur and chlorine species over the North Sea
The use of filter packs and a cascade impactor during a series of research cruises in the southern area of the North Sea has yielded detailed spatial distribution patterns of aerosol concentrations, Cl −, NO 3 −, SO 4 2−1 and NH 4 + and gaseous concentrations, HCl, HNO 3 and NH 3. The overall distri...
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Published in: | Atmospheric environment 1992, Vol.26 (9), p.1689-1699 |
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Main Authors: | , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | The use of filter packs and a cascade impactor during a series of research cruises in the southern area of the North Sea has yielded detailed spatial distribution patterns of aerosol concentrations, Cl
−, NO
3
−, SO
4
2−1 and NH
4
+ and gaseous concentrations, HCl, HNO
3 and NH
3. The overall distribution of the atmospheric concentrations closely parallels published modelled results for metallic species. The chemical transformations of these aerosols and gases are investigated together with their interactions with the seasalt aerosol. Aerosol chloride loss is greatest in the more polluted areas, whilst concentrations products of NH
3 with HNO
3 and HCl appear insufficient to sustain the existence of NH
4NO
3 and NH
4Cl. Nitrate is associated predominantly with larger particles and appears to be present substantially as a surface coating on marine aerosol. The total dry deposition input for nitrogen species is calculated for the southern sector with extrapolation to the whole of the North Sea, using particle size weighted deposition velocities of 0.63 and 0.21 cm s
−1 for NO
3
−1 and NH
4
+, respectively, and literature-derived values for the gaseous constituents. Finally the use of air-mass back trajectories illustrates the role of source regions in influencing the chemical composition of the North Sea atmosphere. |
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ISSN: | 0960-1686 0004-6981 |
DOI: | 10.1016/0960-1686(92)90067-U |