• The Korean Journal of Ecology
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• 제28권3호
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• pp.169-180
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• 2005

이 종설은 산성강하물의 원인물질을 개관하고 한국, 아시아 및 세계의 산성 강하물량을 추산하며 산성비 실태를 밝히는 데 목적이 있다. 서울의 이산화황$(SO_2)$ 농도는 $1996\sim2003$년 사이에 연평균 10%씩 감소하였고 이산화질소$(NO_2)$ 농도는 8%씩 증가하였다. 서울의 빗물은 $1980\sim1991$년 사이에 연평균 pH $4.19\sim4.68$의 심한 산성비가 내렸다. 빗물의 산성도를 총 음이온 농도로 평가한 결과 한국 평균(101.3 ${\mu}equiv{\cdot}L^{-1}$), 광릉(199.2 ${\mu}equiv{\cdot}L^{-1}$) 및 관악산(341.5 ${\mu}equiv{\cdot}L^{-1}$)의 순으로 높았다. 세계 16개 국 38장소의 빗물의 총 음이온 농도를 기준으로 빗물의 산성도를 5등급으로 구분한 결과 말레이시아의 Tana Rata(16.2 ${\mu}equiv{\cdot}L^{-1}$)가 가장 청정한 비가, 중국의 중경(541.1 ${\mu}equiv{\cdot}L^{-1}$)이 가장 오염된 비가 내리고 있음이 비교되었다. 앞으로 산성 강하물은 구미에서 감소되지만 아시아 중남미 아프리카에서 증가될 전망이다.

• The Korean Journal of Ecology
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• 제16권1호
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• pp.17-26
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• 1993

We investigated the ph change of water caused by several fuel gases regarded as the main cause of the air pollution, To find out the main cause of increase of the acidity of the rain. We measured it while injrcting each fuel gas directiy to the distilled water. It was observed that bunker-c oil gas and anthracite coal gas were the main cause to make the ph of the solution lowest. We examined the effects of simulated acidic water solutions on several plant species. Simulated acidic rain made by bunker-c oil gas has significant symptom on the saxifraga stolonifera and commelina communis, while no injury was observed on plants exposed to simulated rainfall made by anthracite coal gas.

• 한국환경과학회지
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• 제7권2호
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• pp.123-132
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• 1998

The experiment was performed to elucidate the effect of simulated acrid rain on growth of the seven crops(caucus carota vu sativa DC. , Fagopyrum esculenkm Moench, Brassica cmpespis subsp. napus var. pekinensis Makino , Raphuus satlws vu. hortensis for. acnMormis Makino, Brassica dbogjabra Bailey, Caphslcum mum L., and Perilla frutescens Britton). The pH levels of simulated acid rain ranged pH 3.1, 3.6, 4.1, 4.6, 5.1 and 5.6. The germination 10 each crop was influenced from stimulated acrid rain except buckwheat and kale. A general decrease of growth in crops was observed with Increasing pH concentrations. The pattern of soluble protein was observed a tendency to decrease from acidic pH eradlents. According to acidity, total DNA contents of each crop was showed a definite reduction. In conclusion, plant growth was stimulated decreasln and the chanties of total Protein Patterns and BNA contents extracted from leaves trended with stimulated acrid rain was showed seriously.

• 한국대기환경학회지
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• 제13권4호
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• pp.249-256
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• 1997

To identify the long-term influence of acid rain treatment on tree growth, acid rain of various composition (pH 2.0, pH 4.0 and pH 5.6 as control) was applied to several landscape trees for five months (April through August, 1991). Tree height, pH values and $Al^{3+}$ concentration in soil were investigated. Acid rain treatments seemed to promote height growth in the first year (1991), but have become an inhibiting factor over five years. All of coniferous species and most broad-leaved species, except Acer ginnala, showed opposite trends in height responses to acid rain treatments between the first (1991) and last (1996) year. In contrast, Acer ginnala showed similar trends to acid rain treatments in the height growth between 1991 and 1996. This result suggested that Acer ginnala has a characteristic adapability to acid rain stress. pH values of surface soil were lower than those of 30 cm soil depth. This fact suggested that acid rain treatments made surface soil acidic condition. In addition, physiological characteristics (photosynthesis, stomatal condition and biomass) have to be investigated to identify the relationship between long-term effects of $AL^{3+}$ concentration and growth.

• 한국산림과학회지
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• 제84권1호
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• pp.103-113
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• 1995

산림생태계(山林生態系)의 산성우(酸性雨)에 대한 완충능(緩衝能)과 민감성(敏感性)을 분석하기 위해서 리기다소나무림(林) 굴참나무림(林)의 수관통과수(樹冠通過水), 수간류(樹幹流) 및 토양층 용탈용액(溶脫溶液)의 성분을 각각 분석하였고, GIS의 IDRISI system을 이용하여 토양도(土壤圖)와 식생도(植生圖)를 영상(映像) 변환(變換)시킨 후 중첩시켜 토양(土壤) 모암(母岩)에 따른 임상(林相)의 분포를 분석하였다. 모암(母岩) 및 토양(土壤)은 산성암(酸性岩), 퇴적암(堆積巖)으로 구분하고 산성(酸性), 중성(中性), 염기성(鹽基性), 변성잔적토(變成殘積土)로 세분하였다. 식생층(植生層)을 통과한 강우의 평균 pH는 굴참나무림(林)보다 리기다소나무림(林)에서 낮았으며, 두 수종 모두 임외강우(林外降雨)보다 수관통과수(樹冠通過水)에서는 높은 반면에 수간류(樹幹流)에서 낮았다. 식생층(植生層)을 통과한 강우(降雨)내 $SO{_4}^{2-}$, $NO_3{^-}$ 및 $Cl^-$의 양은 수관통과수(樹冠通過水)보다 수간류(樹幹流)에서 높았고, 토양으로 투입되는 $SO{_4}^{2-}$, $NO_3{^-}$ 및 $Cl^-$ 양은 임외(林外)보다 리기다소나무림(林)에서 각각 7.2, 4.3 및 2.5배, 굴참나무림(林)에서 각각 4.4, 2 및 2.5배 많았으며 굴참나무림(林)보다 리기다소나무림(林)에서 많았으나, 치환성(置換性) 양이온의 농도는 리기다소나무림(林)에서 4.1배, 굴참나무림(林)에서 4.6배로 굴참나무림(林)에서 높았다. 토양층(土壤層) 용탈용액(溶脫溶液)의 평균 pH는 수관통과수(樹冠通過水) pH보다는 낮은 반면에, 수간류(樹幹流)보다 높은 경향을 보였으며, 수종별(樹種別)로는 리기다소나무림(林) 지역에서 낮았다. 산성물질(酸性物質)에 의해서 토양층(土壤層)으로부터 용탈되는 양료(養料)와 $Al^{3+}$ 양(量)은 관엽수림(關葉樹林)보다 침엽수림(針葉樹林)이 많았고, 이들 양은 토양(土壤) 용탈용액(溶脫溶液)내 산성물질(酸性物質) 증가함에 따라 유의적으로 증가하였다. 산림생태계중(山林生態系中) 리기다소나무림(林)은 식생층 용탈용액에 $SO{_4}^{2-}$, $NO_3{^-}$ 및 $Cl^-$ 양이 많은 것으로 보아 산성물질(酸性物質)의 침적량(沈積量)과 차단량(遮斷量)이 많은 것으로 인정되는 동시에 토양으로부터 양료손실이 많았고 반면 굴참나무림(林)은 수관층(樹冠層)에서 양(陽)이온치환(置換)과 $H^+$ 소비가 많았고, 토양에서 양료손실(養料損失)이 적어 식생과 토양층의 완층력(緩衝力)이 우수했다. 대전지역의 산림토양은 산성암잔적토가 69%, 퇴적 및 변성암잔적토가 25%, 중성 및 염기성암잔적토는 6%를 차지하고 있는데, 양이온 치환용량(置換容量)이 부족한 산성암(酸性岩)에서 풍화된 토양(土壤)이 가장 많은 면적을 차지하고 있었고, 산성우(酸性雨) 대해서 가장 민감성(敏感性)을 나타내는 산성암이면서 동시에 침엽수림(針葉樹林)으로 구성된 임지는 소나무림(林)과 리기다소나무림(林)林으로 전체 면적중 50%를 차지하고 있었다.

• Journal of Plant Biology
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• 제37권3호
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• pp.301-308
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• 1994

The individual and combined effects of acidic rain, Mg deficiency (-Mg) and Al surplus (＋Al) on the growth of shoots and roots of pitch pine seedlings and the effect of humic substances (Lit) on Al toxicity were investigated. The growth of height and dry matter were not significantly less for pitch pine seedlings sprayed with simulated acid rain (SAR) of pH 3.5 than for those sprayed with SAR of pH 5.6. But treatments of Al and ＋Al-Mg in soil solution reduced the growth of seedlings in terms of height of shoots, and dry matter of shoots or roots. Effect of Mg deficiency on the growth of seedlings was apparent only when Al was treated simutaneously. The growth of seedlings, regardless of rain pH, decreased in the following order: control=-Mg>Lit＋Al>＋Al>＋Al-Mg. Treatments of Al and ＋Al-Mg in soil solution reduced the total length of secondary and teritary roots of seedlings regardless of rain pH, and decreased in the following order: the primary root

• 한국대기환경학회지
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• 제8권1호
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• pp.45-51
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• 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.

• 한국토양환경학회지
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• 제3권2호
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• pp.31-39
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• 1998

오염지역과 비오염지역으로부터 채집한 토양에서 토양의 습도, 유기물의 함량, 토양산도 등 물리적인 특징과 토양미생물의 분포와 같은 생물학적인 특징이 조사되었다. 지역에 따른 유기물의 함량과 토양산도는 큰 차이를 나타내었으나, 식물군락에 의한 토양수분과 유기물 함량의 차이점은 발견할 수 없었다. 토양의 산도는 미생물의 분포수와 상관관계를 나타내었다. 이러한 것은 식물이 자라는 토양에 변이를 주는 것으로 산성비와 관련이 있는 것으로 추정된다.

• 한국환경과학회지
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• 제8권3호
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• pp.271-280
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• 1999

This study was carried out to investigate the characteristics of acidity in the precipitation and weather patterns that were influenced it at Kimhae area from March, 1992 to June, 1994. The range of pH value in the precipitation at Kimhae is 3.45 to 6.80 and the average is pH 4.62, and the major anion components associated with acidity in the precipitation are $Cl^-, SO_4^{-2}, NO_3^-$. These distributions are to be expected the influence of industrialization such as, urbanization and construction of industrial complex at Kimhae area and the long range trasporting of air pollutants from China. The weather patterns governing the acid rain at Kimhae were classified broadly into four types(Cyclone(type I-a, type I-b), Migratory Anticyclone(type II), Tropical Cyclone(type III), Siberia High(type IV) and weather pattern which had the most occurrence frequency of acid rain was type I-a and the average pH value of precipitation in this pattern was 4.45, and we are found that the source area of air mass which was accompanied with high acidic precipitation in Kimhae was the central China include with Peking through the analysis of surface weather maps, 850 hPa wind fields, and the streamline analyses.

• 자원환경지질
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• 제28권3호
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• pp.243-249
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• 1995

In order to investigate the origin of sulfate in rain waters and to evaluate the feasibility of using sulfur isotope method as a tracer of atmospheric pollutants, the sulfur isotopic ratio of sulfate in rain waters collected in Chonju city from October 1994 to March 1995 was monitored and was compared with those of possible sources proposed by previous works. The pH of rain waters shows an intermediate acidic range from 4.45 to 6.88 and their daily variation appears to be well correlated with to the amount of precipitation. The sulfur isotopic ratios of sulfate in rain waters show a highly restricted range from 0.0 to + 1.8‰. The ${\delta}^{34}S$ values are similar to those of soil and pine tree surrounding Chonju city, but largely deviate from those of China. D-parameter($d={\delta}D-8{\delta}^{18}O$) of rain waters varies from 9.4 to 28.8. The values indicate that the rain waters in Chonju city are originated from the rainy front of China continent. All data obtained from this study suggested that sulfate in the rain waters collected in Chonju city was mainly derived from the sulfur dioxide gas emitted by the petroleum combustion. Therefore, sulfur isotopic study for the precipitation provided an excellent tool for environmental assessment in this region and for tracing the source of atmospheric pollutants.