• Journal of Korean Society for Atmospheric Environment
• /
• v.8 no.1
• /
• pp.45-51
• /
• 1992

A study on acidity in fog, dew and frost was carried out. Samples were taken during May 1990-February 1991 at two sites in Chongwon, Choongbook. The acidity of dew and of fog collected from grass at site A was 4.89 and 5.46, respectively. Dew in summer showed very strong acidity. The volume of dew deposited on grass was much less than the volume of rain, but dew is effective to diffuse acid predursors and acid materials. Dew and fog can remove more effectively atmospheric acid materiasl deoposited on grass by diurnal turbulent motion rather than direct absorption of acid predursors and materials in the atmosphere. In a polluted area, acidic dew and fog can be occurred by the direct absorption and oxidation of acidic predursors in the atmosphere as well as the role of wet removal on grass surface. Acidity of frost collected on teflon surface showed little difference to acidity of dew and fog on teflon surface. This suggests a similar absorption mechanism of atmospheric precursors and materials into dew and frost in the atmosphere. Strong acidity in dew, fog and frost appeared to occur from local pollution sources of several ten kilometres. In particular, strong acidity in dew, fog, and frost together with acid rain can accelerate a damage in ecosystems. Discussion is made on scientific analyses and seasonal variations of acidity of fog, dew and frost. A mechanism on acidification of fog, dew and frost is also discussed.

• Korean Journal of Agricultural and Forest Meteorology
• /
• v.2 no.2
• /
• pp.31-40
• /
• 2000

This study was carried out to compare pH and chemical properties of dew in three forest stands(Mt. Nam-Seoul, Shingal-Yongin, Hangdong-Pyungchang)from May, 1998 to September, 1999. The results of this study were as follows; The acidity of dew in Seoul, which has a metropolitan environment, measured pH5.57 $\pm$ 0.41. The highest acidity was measured in Yongin(pH5.50 $\pm$ 0.96), while pH in Pyungchang was 6.36 $\pm$ 0.57. Ion concentration in Pyungchang was lower than in other two regions, with a similar tendency of seasonal cation changes to those in Seoul and Yongin. Anion changes in Pyungchang, however, was inconsistent with those in other two regions. Although analyses of correlation coefficients showed that there was no significant correlation between overall ion concentrations and pH of dew, there was highly significant correlations between some cations and anions in Seoul and Yon gin, leading a suggestion that those ions were coupled from one source.