Abstract
Seasonal variations in the chemical characteristics of wet and bulk deposition samples collected in Erzurum were investigated for the period March 2002–January 2003. Major cations (Ca 2+, K +, Mg 2+) and major anions ( SO 4 2 - , NO 3 - ) were determined in bulk and wet deposition samples; pH was also measured in wet deposition. The average pH of the wet deposition at Erzurum was 6.6 due to extensive neutralization of the acidity. A strong relationship between pH and SO 4 2 - concentrations was observed in all seasons; however, only a weak relationship was found between pH and NO 3 - . On a seasonal basis, the correlation between Ca 2+ and SO 4 2 - concentrations was stronger in winter than in summer. Seasonal variations of ions were examined in both wet and bulk deposition samples. Although maximum concentrations of anions generally occurred during winter and spring, cation concentrations peaked in summer for both wet and bulk deposition. Results indicated that Ca 2+ was the dominant cation and SO 4 2 - the dominant anion in all deposition samples at Erzurum. Even though correlations among the crustal ions (calcium, magnesium and potassium) were high, the relationship between anthropogenic ions (sulfate and nitrate) was less clear in bulk deposition.
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