Chemical composition of precipitation near an industrial area at Izmir, Turkey
Wet and dry deposition samples were collected near an industrial area on the Aegean coast of Turkey. Concentrations of major ions (Cl −, SO 4 2−, NO 3, H +, Na +, K +, Cat 2+ Mg 2+ and NH 4 + were determined. The pH of the precipitation, calculated from the volume weighted H+ concentration, was foun...
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Published in: | Atmospheric environment (1994) Vol. 29; no. 10; pp. 1131 - 1143 |
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Main Authors: | , , , , , |
Format: | Journal Article |
Language: | English |
Published: |
Oxford
Elsevier Ltd
1995
Elsevier Science |
Subjects: | |
Online Access: | Get full text |
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Summary: | Wet and dry deposition samples were collected near an industrial area on the Aegean coast of Turkey. Concentrations of major ions (Cl
−, SO
4
2−, NO
3, H
+, Na
+, K
+, Cat
2+ Mg
2+ and NH
4
+ were determined. The pH of the precipitation, calculated from the volume weighted H+ concentration, was found to be 5.6, indicating extensive neutralization of the acidity in the rain. Neutralization was found to be a local process. The main base responsible for the neutralization of acidity was NH
3 from fertilizer used in the region. The CaCO
3 from resuspended soil accounts for 16% of the neutralized acidity. The annual wet deposition of ions was determined by two parameters, namely the precipitation amount and concentrations of ions in the precipitation. Precipitation amount accounted for approximately 70% of the annual wet deposition of ions in the Menemen region, whereas concentrations of ions in precipitation had only a minor influence. Although concentrations decrease with precipitation amount due to dilution in heavy rain, precipitation amount is not the only factor affecting concentrations of ions in precipitation. The main source of ions in wet deposition is the emissions from nearby industries. However, airborne NH
4NO
3 and (NH
4)
2SO
4 fertilizer particles may also contribute to observed concentrations of SO
2
2− and NO
3
− in rainwater. Dry deposition of most of the ions was higher than their annual wet deposition. |
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Bibliography: | ObjectType-Article-2 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 23 ObjectType-Article-1 ObjectType-Feature-2 |
ISSN: | 1352-2310 1873-2844 |
DOI: | 10.1016/1352-2310(95)00027-V |