Precipitation chemistry in Japan was discussed on the basis of nation-wide monitoring results of Acid Deposition Survey of Japan Environment Agency in terms of ionic composition, concentrations and deposition of major ions. The volume-weighted mean ionic-composition of p recipitation collected fr om April 1989 to March 1993 was interpreted from the viewpoints of atmospheric chemistry to be composed of three contributions: 1) sea-salt derived ions including sodium, chloride, and magnesium ions, 2) sulfuric and nitric acids originated from man-made air p ollutants, sulfur dioxide and nitrogen ox ides, and 3) basic species such as ammonia and calcium c ompounds. Approximately 70% of t he origin al sulfuric and nitric acids were explained to have been neutralized to yield resultant pH of 4.76. pH at each site ranging from pH 4.5 to pH 5.8. A nnual mean concentrations and deposition of n on-seasalt sulf ate, nitrate, and ammonium were obtained, respectively, with their ranges in parentheses as follow s: 19.3(2.6-29.5), 14.1 (1.8-25.0), 18.3 (0.6-29.8) μmol L
-1, 26.1 (4.7-49.8), 19.4 (3.1-40.8), 2 5.9(1.1-55.4) mmol m
-2y
-1. Spatial distribution of annual mean concentration and deposition of th ese three ions w ere suggested highly u niform over the country from the ratios of the standard deviatio ns to the means. Seasonal variation of concentration and deposition of selected major ions o n Japan Sea were clarified, and discussed in terms of longrange transport from the Asian continent. Wintertime nonseasalt sulfate ion was shown to be remarkably increased in the concentration and deposition on Japan Sea side, and similar variations were observed for nitrate, ammonium, non-seasalt calcium i ons. O n the Pacific Ocean side, however, no distinct seasonal variations were found for these ions. Precipitation chemistry in Japan was compared with those in Europe, North America in terms of pH and pAi. The latter index was defined as the negative logarithm of the sum of non-seasalt sulfate and nitrate ion concentrations, which physically means the hypothetical pH under the assumption that no sulfuric and nitric acids in precipitation had been neutralized with atmospheric bases. In Europe, pAi was considerably low and the degree of neutralization was very small to offer lowest pH among the three regions of interest. In North America, pAi was likely to be lower than those in Europe, but the degree of neutralization wa s also high so a s to lower the pH. Both pH and pAi of t he precipitation in J apan were between those in t he two regions. Concentrations and deposition of non-seasalt sulfate and nitrate ions w ere discussed o n a global scale.
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