한국환경농학회지 (Korean Journal of Environmental Agriculture)

  • 제25권1호
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  • Pages.1-6
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  • 2006
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  • 1225-3537(pISSN)
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  • 2233-4173(eISSN)
한국환경농학회 (The Korean Society of Environmental Agriculture)
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익산지역 강수성분의 연차적 변이

Yearly Changes of Precipitation Component in the Iksan Area

  • 발행 : 2006.03.31
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초록

본 연구는 산성비의 대한 장기적이고 종합적인 대책방안을 마련하기 위한 기초 자료를 제공코자 1997년부터 2003년까지 7년 동안 산성강우 현상을 중심으로 조사하였다. 강수의 연차적 산성비 강하비율은 1997년 70.0%, 1998년 56.3%, 2003년 36.4%를 나타냈으나, 강우량이 적은 1999년부터 2002년의 산성비 강하비율은 $6.9{\sim}19.2%$를 보였다. 산성우에 대한 영향 평가시 단기간에 의한 것보다 장기적인 영향으로 발생하기 때문에 산성강하물의 농도뿐만 아니라 침착량의 해석이 필요하다. 강수중 주요 이온성분의 연평균 습성침착량은 각 이온성분의 당량농도에 강수량을 곱하여 산출하였다. 각 이온 성분의 침착량을 살펴보면 음이온은 ${SO_4}^{2-}>Cl^->{NO_3}^-$순이었으며, 양이온의 경우는 ${NH_4}^+>Ca^{2+}>Na^+>Mg^{2+}>K^+$순으로 많았다. 강수 중 주요성분에 대한 상관분석 결과 pH와 강수 이온 성분중 $Ca^{2+}$와 $Na^+$성분을 제외한 모든 성분에서 부의 상관을 나타냈으며 그 외 각 성분간의 상관은 정의 상관을 나타냈다. pH와 ${SO_4}^{2-}$간의 상관계수는 -0.508로 고도의 유의성을 나타냈는데 이는 ${SO_4}^{2-}$성분이 강수중 산성도를 증가시키는 주요원인 물질중 가장 큰 역할을 하고 있음을 추정할 수 있었다. 또한 ${SO_4}^{2-}$와 ${NO_3}^-$ 이온은 $Ca^{2+},\;Mg^{2+},\;K^+,\;{NH_4}^+\;and\;Na^+$ 등 양이온과 고도의 유의성을 보였다.

This study was carried out to investigate yearly change in the precipitation component and the source strength to acid precipitation at Iksan area from 1997 to 2003. The average ratio of acid precipitation was 70.0% in 1997, 56.3% in 1998 and 36.4% in 2003. On the other hand, it ranged from 6.9 to 19.2% when precipitation was less from 1999 to 2002. The average annual wet depositions of major ionic component in precipitation were calculated by multiplying equivalent concentration by precipitation. The order of major anion component in precipitation was ${SO_4}^{2-}>Cl^->{NO_3}^-$. On the other hand, the concentration of cation component were ${Ca_2}^+>Na^+>{NH_4}^+>{Mg_2}^+>K^+$ in order. The negative correlation was shown between pH and ionic component in precipitation except for ${Ca_2}^+\;and\;Na^+$. The correlation coefficient between pH and ${SO_4}^{2-}$ was highly significant as -0.508, which suggests that ${SO_4}^{2-}$ played important role in increasing the acidity of precipitation. Also the anions such as ${SO_4}^{2-}\;and\;{NO_3}^-$ were highly significant with cations such as ${Ca_2}^+,\;{Mg_2}^+,\;K^+,\;{NH_4}^+\;and\;Na^+$. As a result though pH was enable to use the acidity index of precipitation in somewhere, evaluating only pH in precipitation was insufficient as the index to establish corresponding strategy for acid rain.

키워드

참고문헌

  1. Intergovernmental Panel on Oimate Change (IPCC), (1995) Draft Summary for Policymakers of The Contribution of Working Group I to The IPCC Second Assessment Report
  2. Lidens, G.E., Wright, R. E., Galloway, J.N. and Butler, T.J. (1979) Acid rain, Scientific American 241(4), 39-47
  3. Hatakeyama, S. (1993) Effects of stratospheric ozone depletion and/ or global warming on acid rain, countermeasure of environment resource, Atmos. Environ. 29(3) 827
  4. Seinfeld J.H. (1986) Atmospheric chemistry and physics of air pollution, John Wiley and Sons, 699
  5. Sequeira R.A. (1982) Acid rain: An assessment based on acid-base considerations, JAPCA 32, 241-245
  6. American Chemical Society, (1982) Acid deposition: Many new findings on this field were reported at the recent meeting of the American Chemical Society, Environ. Sci. Technol. 323A-327 A
  7. Guidobaldi, F.G. and Mecchi, A.M. (1993) Corrosion of ancient marble monuments by rain: Evalution of pre-industrial recession rates by laboratory simulations, Atmos. Environ. 27B(3), 339-351
  8. Westenbarger, D.A. and Frisvold, G.B. (1994) Agricultural exposure to ozone and acid precipitation, Atmos. Environ. 27(10), 2231-2239
  9. Fujita,S., Ichikawa, Y., Kawaratani, R.K., and Tonooka, Y. (1991) Atmosphere Environment 25, 1409-1411 https://doi.org/10.1016/0960-1686(91)90250-B
  10. Lee K.B., Kang J.G., Kim J.G., Rhee G.S., and So J.D. (1996) Yearly changes in the precipitation component and investigation on the source strength to acid rain in the Iksan area. J. Korean Environ. Agri. 15(2), 188-197
  11. Lee J.S. and Kim B.Y. (1994) Effect of acid rain on vegetation. J. Korean Environ. Agri. 13(3), 346-35
  12. Lee J.S., Jung Y.K., and Lee K.S. (1999) Chemical Composition of rainwater in Taean area. J. Korean Environ. Agri. 18(3), 204-208
  13. Ministry of Environ. (2000) The standard method of water analysis
  14. William Horwitz. (1980) Methods of analysis of the association of official analytical chemists. A.O.A.C, p.550-552
  15. Smith, R.M., Twiss, P.C., Krauss, P.K., and Brown, M.J. (1970) Effect of dry deposition in rain water. Proc. Soil Sci. Soc. Amer. 34, 112
  16. Allan R.J. and Jonasson I.R. (1978) Alkaline snowfaiis in Ottawa and Winnipeg Canada, Atmos. Environ. 12, 1169-1173 https://doi.org/10.1016/0004-6981(78)90364-5
  17. Grant, L. (1972). On the relation between pH and the chemical coposition in atmospheric precipitation, Tellus, 24, 550-560 https://doi.org/10.1111/j.2153-3490.1972.tb01581.x
  18. CRIEPI (1992) Acidic deposition in Japan, CRIEPI report, 5-36

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  2. Chemical weathering and associated CO2 consumption in six major river basins, South Korea vol.129, pp.3-4, 2011, https://doi.org/10.1016/j.geomorph.2011.02.028