• Proceedings of the Korea Air Pollution Research Association Conference
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• 2001.11a
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• pp.43-44
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• 2001

산업의 발달과 함께 화석연료의 소비가 증가하면서 산성강하물(Acid precipitation)에 대한 관심이 증가하여 왔다. 산성강하물은 주로 화석연료의 연소를 통해 대기로 배출된 질소와 황 산화물들로, 산화ㆍ환원, 산ㆍ염기 중화반응 등 다양한 변환과정을 거쳐 비나 눈과 같은 습성과정이나 가스나 입자상 물질과 같은 건성과정을 통해 다시 토양과 호수 등에 침적되어 이들을 산성화시키는 원인이 된다. 따라서 산성강하물에 대한 이해를 위해서는 강수의 화학조성과 아울러 가스와 입자상으로 존재하는 질소와 황화합물에 대한 관측이 필수적이다. (중략)

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2000.04a
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• pp.297-298
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• 2000

1960년대 후반 이후 대기오염 및 산성비 등 산성강하물에 의한 산림생태계의 쇠퇴 및 피해가 유럽과 북미에서 보고되고 있으며, 최근 중국, 일본 등 동아시아 각국의 급속한 경제발전으로 인하여 산성비의 원인물질인 황산산화물과 질소산화물 배출량의 급속한 증가는 산림생태계의 피해를 가속화 할 것으로 예측되고 있다. 우리 나라의 경우 산성강하물에 의한 대규모의 산림피해는 아직까지 보고되고 있지 않으나, 산성비에 포함된 산성강하물의 토양내로의 부하의 증가는 토양을 산성화시켜 수목의 생육에 악영향을 미칠 가능성이 있다. (중략)

• Journal of Conservation Science
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• v.26 no.4
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• pp.437-443
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• 2010

The influence of noxious corrosive gas, which is the product of fossil fuel, and the acidic descent material, which becomes the reason for such reaction, on wax which protects the cultural assets, and the habitat factor were researched. It could be viewed that corrosion occurred rapidly due to the acidic descent material, which have the long staying on the material, rather than harmful corrosive gas. Also, it could be figured out that such corrosion began from whitening phenomenon of coated wax. As the acidity increased, more whitening phenomenon occurred, and eventually, it could be found out that whitening effect began due to the acidic descent material, corrosive gas and various 0.1 M acid solution, which lead to the exposure of internal metal, and corrosion occurred. The wax with the greatest resistance to the acidity due to its least changing aspect seemed to be Renaissance wax, except sulfuric acid.

• The Korean Journal of Ecology
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• v.28 no.6
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• pp.417-431
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• 2005

Soils of Korea experienced with long-term acidic deposition have been exhaustively leached exchangeable base cation (BC) for plant nutrient comparable with soils of forest decline areas in Europe and N. America. Ratios of $BC/Al^{3+}$ of most soils are below than 1, which value is critical load for plant growth. Acid soil applied with dolomitic liming is increased as much as 20% and 244% in concentrations of $Ca^{2+}$ and $Mg^{2+}$, respectively, as well as shrub leaves increase much cation uptake by 1 year later. Ions of $NO_3^-$ and $NH_4^+$ in acid rain are absorbed by the canopy acted as the sink but f is leached out from the canopy to throughfall as the source at Gwangneung forest with a little of acidic deposition, however, such sink and source functions are not found at Kwanaksan forest because of so much deposition. In coniferous and deciduous forested watershed ecosystems ions of $K^+$, $Cl^-$, $NO_3^-$ and $SO_4^{2-}$ from throughfall are retained in forest floor but ions of $Na^+, $Mg^{2+}$ and $Ca^{2+}$ are leached from the floor to streamwater.

• The Korean Journal of Ecology
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• v.17 no.1
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• pp.69-78
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• 1994

The acidic deposition (wet) was collected at three different locations; representative industrial (Kun-Jang industrial areas), semiindustrial (Kunsan City) and nonindustrial (Daeya areas) region between March, 1991 and June, 1993. Samples were analyzed for major chemical components along with pH. Also the responses of Hypnum filunzaeforme to the acidic deposition adjusted to pH 4.6, 3.6 and 2.6 with 1:4 molar ratio of nitric to sulfuric acid were investigated. Seasonal variation of pH showed the lowest in early spring and the highest in summer. The annual mean concentrations of $S0_4^{2-},\;NO_3^{-}\;and\;NH_4^{+}$ were 2.94 (81.0%), 0.48 (13.2%) and 0.21 (5.78%) mg/l in industrial region and 0.61 (64.21%), 0.25 (26.3%) and 0.9 (9.5%) mg /I in nonindustrial region, respectively. $S0_4^{2-}$ contents of industrial region was 4 times higher than those of nonindustrial region. The ratio of $S0_4^{2-}\;to\;NO_3^{-}$ was 4.75~7.35 in industrial region and 0.69-6.36 in nonindustrial region. The acidic deposition near industrial region was associated with excess ions, expecially $S0_4^{2-}$. Nitrate reductase activity(NRA) of mosses was inhibited by acidic deposition in both regions. The time required for the maximum NRA induction by 2mM $KNO_3$ was shortened in mosses collected from industrial region. Photosynthesis of H. plumaejorme began to decrease with acidic deposition by pH below 4.6, and was completely inhibited at pH 2.6 in both regions. Water potential of mosses treated with acidic deposition was almost constant during 18 days, however after withholding the supply of acidic deposition, it was rapidly decreased.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 1992.10a
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• pp.80-84
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• 1992

• Proceedings of the Zoological Society Korea Conference
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• 1995.10b
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• pp.186.2-186
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• 1995

• Journal of Korea Soil Environment Society
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• v.1 no.2
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• pp.15-21
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• 1996

Effects of acid deposition on the acidification of surface water over a short term period were studied during June~October, 1995. A reservoir located in Chunchon, Kangwondo was selected for this study because this reservoir had received little man-made pollutants. Geological survey within the study area was carried out and the pH of a small and shallow stream flowing from the mountain valley down to the reservoir was monitored. Rainfall was measured by using a rain gauge and the precipitation was collected by automatic precipitation sampler. During the study period, rain pH was in the range of 3.81~5.77 with an average of 4.8. The EC was in the range of 5~189$\mu$S/cm with an average of 10.6$\mu$S/cm. ionic composition of the rainfall showed that of the anions, deposition of ${SO_4}^{2-}$, was highest with 3,119.7 kg/$\textrm{km}^2$, and it was $NH^{4+}$ with 1,053.2kg/$\textrm{km}^2$ for cations. The surface water pHs were maintained neutral or weak basic representing little evidence of acidification regardless of the acidic rainfall pH. Every time of sampling, however, the pHs exhibited increasing tendency as elevation of measuring site of the stream became lowered, which indicated the impacts of acid-base reactions by acidic or basic substances during travel of water downstream. This result suggested the necessity of further research to determine the respective buffering capacity of soil and underlying rocks.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2001.11a
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• pp.115-115
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• 2001

강수중에 존재하는 이온성분은 강수의 화학적 조성을 변화시키는 주요 요인이 되는 물질로서 자연적 또는 인위적으로 배출된 대기오염물질을 비롯하여 토양입자를 구성하고 여러가지 성분들이 수용액 중에 용해되어 존재하게 된다. 강수의 pH는 이와 같은 용해성분들의 화학적 구성상태에 따라서 결정되게 된다. 따라서 강수의 pH별 이온성분들의 분포특성을 파악하는 것은 산성강하물의 산도증가에 직접적인 원인이 되는 산도유발물질의 종류나 산성강하물의 생성과정의 추정에 있어서 매우 중요한 역할을 하게 된다. (중략)

• The Korean Journal of Ecology
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• v.28 no.3
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• pp.169-180
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• 2005

Nitrogen dioxide concentration was being grown ca. 8% per year although sulphur dioxide concentration was being reduced ca. 10% per year in Seoul from 1996 to 2003. The rainwater was heavily acidic with pH 4.19 to 4.68 in Seoul during 1980 to 1991. Acidity score on the basis of the total anion concentration of rainwater follows the higher in sequence with Seoul(Kwanaksan)(341.5 ${\mu}equiv{\cdot}L^{-1}$), Gwangneung(199.2 ${\mu}equiv{\cdot}L^{-1}$) and whole Korea mean(10.3 ${\mu}equiv{\cdot}L^{-1}$). Rainwaters from 38 sampling sites of 16 countries in the world, on the basis of the acidity score, are classified and designated as five acid rain grades(ARG): the least score is founded in Tana Rata(16.2 ${\mu}equiv{\cdot}L^{-1}$), Malaysia where has the best rain but the greatest founded in Chongquing(541.1 ${\mu}equiv{\cdot}L^{-1}$), China where has the worst rain in the world. Even though acidic deposition decrease with time in the world generally, it is expected to increase in Asia, Africa and Mid-South America.