Weekly rain samples were collected in coastal areas of the Shihwa Basin (Korea) from June 2000 to November 2007. The study region includes industrial, rural, and agricultural areas. Wet precipitation was analyzed for conductivity, pH, Cl
−, NO
3−, SO
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Weekly rain samples were collected in coastal areas of the Shihwa Basin (Korea) from June 2000 to November 2007. The study region includes industrial, rural, and agricultural areas. Wet precipitation was analyzed for conductivity, pH, Cl
−, NO
3−, SO
42−, Na
+, K
+, Mg
2+, NH
4+, and Ca
2+. The major components of precipitation in the Shihwa Basin were NH
4+, volume-weighted mean (VWM) of 44.6 µeq∙L
−1, representing 43% of all cations, and SO
42−, with the highest concentration among the anions (55%) at all stations. The pH ranged from 3.4 to 7.7 with a VMM of 4.84. H
+ was weakly but positively correlated with SO
42− (
r = 0.39,
p < 0.001) and NO
3− (
r = 0.38,
p < 0.001). About 66% of the acidity was neutralized by NH
4+ and Ca
2+. The Cl
−/Na
+ ratio of the precipitation was 37% higher than seawater Cl
−/Na
+. The high SO
42−/NO
3− ratio of 2.3 is attributed to the influence of the surrounding industrial sources. Results from positive matrix factorization showed that the precipitation chemistry in Shihwa Basin was influenced by secondary nitrate and sulfate (41% ± 1.1%), followed by sea salt and Asian dust, contributing 23% ± 3.9% and 17% ± 0.2%, respectively. In this study, the annual trends of SO
42− and NO
3− (
p < 0.05) increased, different from the trends in some locations, due to the influence of the expanding power generating facilities located in the upwind area. The increasing trends of SO
42− and NO
3− in the study region have important implications for reducing air pollution in accordance with national energy policy.
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