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Jae-Young Yu,박영윤,Randall E. Mielke,Max L. Coleman 한국지질과학협의회 2007 Geosciences Journal Vol.11 No.4
: The meteoric water deposited in the Chuncheon area was collected from July 2002 to May 2004 and its chemical and isotopic compositions were analyzed to examine if the isotopic data can help trace the sources of the sulfur pollutant and understand the details of acid formation processes in the air. The chemical compositions of the meteoric water indicate that the sulfate mostly comes from anthropogenic sources. The sulfur isotopic compositions of the dissolved sulfate in the meteoric water (34SSO4) vary from 2.6 to 7.5 with little seasonal differences, which are significantly different from those of the sulfur in the coal being locally consumed (4.5 to 0.7). This difference indicates that the local coal consumption gives insignificant contribution to the pollutant sulfur in the acid deposition of the area. The relationship between 34SSO4 and the concentration of sulfate suggests that the sources of pollutant sulfur are variable and inhomogeneous.The oxygen isotopic compositions of the dissolved sulfate in the meteoric water (18OSO4) range from 9.0 to 17.2, which are generally lower in winter than in spring. Comparison between the measured and calculated values of 18OSO4 suggests that the oxygen isotopic exchange between sulfite and water occurs before its oxidation to sulfate. The extent of isotopic exchange seems to be not controlled by equilibrium but by kinetic fractionation. The poor correlation between 18OSO4 and the oxygen isotopic composition of the meteoric water confirms the disequilibrium nature of the isotopic exchange.