• The Korean Journal of Ecology
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• 제15권2호
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• pp.173-180
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• 1992

Pb, Zn tolerance of phaseolus multiflorus was investigated, based on the elongation of root and stem, pollen Germination and progeny quality in various pb, zn concentrations. The result obtained by water culture showed that the growth of roots and steams of phaseolus multiflorus from pb-zn mine site is less inhivited than that of the control site. The flower of phaseolus multiflorus from which pollen was taken were grown without added pb, zn and percent germination of pollen observed in a range of pb, zn concentrations. The percent germination of pollen from pb-zn mine site was higher than the control site. phaseolus multiflorus collected at a pb-zn mine site and the control site was site were grown at different pb, zn concentrations, its progeny was retreated with same concentrations of pb-zn mine site was more vigorous than the control site. thus, pb-zn tolerance was able to expressed in both pollen and sporophytes.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2005년도 총회 및 춘계학술발표회
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• pp.20-23
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• 2005

The objective of this study is to examine a stabilized efficiency of heavy metals including Cd, Cu, Pb and Zn using slaked lime. Tailings from the Janggun Pb-Zn mine, the second Yeonhwa Pb-Zn mine, the Jisi Au-Ag mine and the Sangdong W mine were sampled and measured heavy metal concentrations contents using AAS as various extraction methods. During 156 hours, column test were undertaken to evaluate the possibility of stabilization by slaked lime. The result shows that $Ca(OH)_2$ has a good efficiency in heavy metal stabilization, especially at the Jisi mine with stabilized efficiencies of 97%(Cd), 99%(Cu), 86%(Pb) and 99%(Zn), respectively.

• 한국토양비료학회지
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• 제33권6호
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• pp.446-452
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• 2000

전라북도 김제시 금산면 소재 옥성 동-아연 주변 농경지 토양중에 존재하는 중금속의 식물흡수도와 이동도를 예측하기 위해 연속추출법을 이용한 화학적 형태조사 및 폐광산 유출수가 주변 농업용수에 끼치는 영향을 조사한 결과는 다음과 같다. 토양중 각 중금속의 화학적 형태별 함량 분포는 Cd의 경우 organically bound > exchangeable > carbonate > residual > sulfide form, Zn 의 경우 residual > sulfide > exchangeable > organically bound > carbonate > water soluble form, Cu와 Pb의 경우 carbonate > residual > organically form > sulfide > exchangeable form, Cr은 residual > organically bound > sulfide > carbonate > exchangeable form, 그리고 Ni는 residual > exchangeable > sulfide > carbonate > organically bound form의 순서로 나타났다. 중금속의 화학적 형태별 함량 분석 결과 치환태 중금속의 함량은 각각 Cd 30.2%, Zn 11.3%, Cu 2.0%, Pb 4.6%, Cr 0.6%, Ni 3.9%로 나타나, 중금속의 이동성과 식물체의 가급성은 Cr > Cu > Ni > Pb > Zn > Cd의 순서로 나타났다. 폐광 갱내수중 중금속의 평균 함량은 Cd 0.01, Zn 27.35, Cu 4.86, Pb 1.04, Cr 0.03, Ni $0.08mg\;L^{-1}$, 폐광 유출수의 경우 Zn 16.67, Cu 0.59, Pb 049, Cr 0.05, Ni $0.06mg\;L^{-1}$, 주변 농업용수의 경우 Zn 1.26, Cu 0.05, Pb 0.05, Ni $0.02mg\;L^{-1}$로 나타났으며, Cd, Cr은 검출되지 않았다.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2003년도 Proceedings of the international symposium on the fusion technology
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• pp.515-517
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• 2003

In order to assess the risk of adverse health effects on human exposure to arsenic and heavy metals influenced by past mining activities, environmental geochemical surveys were undertaken in the abandoned metal mine areas (Dongil Au-Ag-Cu-Zn, Okdong Cu-Pb-Zn, Songcheon Au-Ag, Dongjung Au-Ag-Pb-Zn, Dokok Au-Ag-Cu and Hwacheon Au-Ag-Pb-Zn mines). Arsenic and other heavy metals were highly elevated in the tailings from the Dongil, the Songcheon and the Dongjung mines. High concentrations of heavy metals except As were also found in tailings from the Okdong, the Dokok and the Hwacheon mines. These significant concentrations can impact on soils and waters around the tailing dumps. Risk compounds deriving from mine sites either constitute a toxic risk or a carcinogenic risk. The hazard index (H.I.) of As in the Dongil, the Okdong, the Songcheon and the Hwacheon mine areas was higher value more than 1.0. In the Okdong and the Songcheon mine areas, H.I. value of Cd exceeded 1.0. These values of As and Cd were the highest in the Songcheon mine area. Therefore, toxic risks for As and Cd exist via exposure (ingestion) of contaminated soil, groundwater and rice grain in these mine areas. The cancer risk for As in stream or ground water used for drinking water from the Songcheon, the Dongil, the Okdong, the Dongjung and the Hwacheon mine areas was 3E-3, 8E-4, 7E-4, 2E-4 and 1E-4, respectively.

• 한국환경농학회지
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• 제31권2호
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• pp.122-128
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• 2012

폐금속 광산에서 유출되는 광산배수로 인한 하류 수계의 환경오염 영향을 검토하기 위하여 삼보광산 하류 수계 내 하천수질, 퇴적토양 및 인근 논토양에 대한 중금속 오염도를 평가한 결과는 다음과 같다. 삼보광산 주변 광미댐 침출수의 Cd 평균 농도(0.018~0.035 mg/L)는 우리나라 농업용수 수질기준(0.01 mg/L)을 초과하였고, 미량성분 중 Zn, Fe 및 Mn 함량도 FAO의 관개용수 최대 권고치(Zn 2.0, Fe 5.0, Mn 0.2 mg/L)를 초과 하였다. 광산 하류 논토양의 Pb, Zn 평균함량은 우리나라 농경지의 토양오염 우려기준(Pb 200, Zn 300 mg/kg)을 초과 하였고, 중금속 오염지수 평균치는 상리가 1.2로 내리지역0.45보다 높게 나타났다. 광산 하류 수계 내 퇴적토의 Cd, Pb 및 Zn 함량은 우리나라 하천용지의 토양오염 우려기준(Cd 10, Pb 400, Zn 600 mg/kg)을 초과하였다. 또한 퇴적토의 중금속 오염지수(PI)는 상리지역 0.98~7.32, 내리지역 0.34~5.27로 지점별 편차가 컸으며, 하류 1km 지점 합류지점(SN-1, SN-2)까지 오염된 것으로 나타났다. 퇴적토의 부화계수(EFc) 평균치는 Cd>Pb>Zn>As>Cu>Cr>Ni 순으로 지점간의 편차가 큰 것으로 나타났다. 퇴적토의 중금속별 지화학적농축계수(Igeo)는 지점별로 약간의 차이는 있으나 Zn>Cd>Pb>Cu>As>Cr>Ni 순으로 높았으며, 특히 Zn의 경우 광산 침출수 영향을 받은 퇴적토에서 경보오염에서 위험오염(Igeo 3.1~6.2) 상태로 심하게 오염된 것으로 나타났다. 결과적으로 삼보광산 하류 하천수질 및 퇴적토의 오염도 평가를 종합해 볼 때 광산 침출수의 영향이 하류 수계 1 km 이상(SN-1, SN-2)까지 미치는 것을 확인할 수 있었다.

• 한국환경과학회지
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• 제16권12호
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• pp.1451-1462
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• 2007

Heavy metal concentrations in the soil were investigated for the abandoned Samkwang metal mine, Cheongyang-Gun, Chungnam Province, Korea. The concentrations of heavy metal(As, Cd, Cu, Ni, Pb, Zn) were determined in mine soils collected at the abandoned mine sites to obtain a general classification and specification of the pollution in this highly polluted region. The results estimated with the normal test and basis statistic on the central tendency and variation showed that the distribution of heavy metal concentration had significantly different at the range of all locations. The range of spatial distribution on the relationship of heavy metal concentration and pH was $4.8{\sim}8.8$ and heavy metal concentration on the type of land use was highest in forest land, and also Ni and Zn in farm and rice field showed the high concentration. The distribution of heavy metal concentration on the depth of a soil showed that the metal concentrations in subsoil were higher than of those in surface soil, while the concentration of Cu and Ni had no significant difference on the depth of soil. Results from the correlation analysis using the data except the extreme and unusual data revel that Zn-Cd(r=0.867), Zn-As(r=0.797), Zn-Pb(r=0.764), Cu-Cd(r=0.673), Cu-As(r=0.614) and Zn-Ni(r=0.605) were the most important parameters in assessing variations of heavy metal in soil. To discriminate pattern differences and similarities among samples, principal factor analysis(PFA) and cluster analysis(CF) were performed using a correlation matrix. This study suggests that PFA and CF techniques are useful tools for identification of important heavy metal and parameters. This study presents the necessity and usefulness of multivariate statistical assessment of complex databases in order to get better information about the quality of soil and gives the basis information to clean up the abandoned mine sites.

• 한국지하수토양환경학회지:지하수토양환경
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• 제18권1호
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• pp.85-93
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• 2013

This study is conducted to evaluate the leaching of contaminants from mine tailing by natural water and finally to estimate the leaching and transportation of heavy metal contaminants by rainfall. In order to identify contaminated heavy metal of soil, 17 soil, 2 tailing and 2 waste dump and 2 control samples were taken at mine area and analyzed total metal contents. The leaching experiments were conducted using distilled water. Cu, Pb, Zn was extracted from the reddish mine tailing in a short period time, especially the extraction rate of Cu (45.0%) was highest. The contaminants were leached from the yellowish mine tailing within an hour and the leaching rate of Cd (42.0%) and Zn (17.2%) were relatively high. The reddish soil from the waste dump showed leaching of Cu (5.1%), Pb (4.0%) and Zn (3.3%), however the leaching rate was low except Mi (14.2%). From the yellowish soil sampled from the dumping site, the leaching of Cu (8.2%) and Ni (9.7%) was high while the leaching of Zn (0.2%) were relatively low.

• 한국지하수토양환경학회지:지하수토양환경
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• 제16권4호
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• pp.38-52
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• 2011

Sorption and sequential desorption experiments were conducted for Zn using a natural soil (NS) in background status by aging (1, 30 and 100 days). The sorption isotherm showed that Zn had high sorption capacity but low sorption affinity in NS. Sequential desorption was biphasic with appreciable amount of sorbed Zn residing in the desorption-resistant fraction after several desorption steps. The biphasic desorption behavior of Zn was characterized by a biphasic desorption model that includes a linear term to represent labile or easily-desorbing fraction and a Langmuirian-type term to represent desorption-resistant fraction. The biphasic desorption model indicated that the size of the maximum capacity of desorption-resistant fraction ($q^{irr}_{max}$) increased with aging in NS. Desorption kinetics and desorption-resistance of Zn in the soils collected from mine tailings (MA, MB and MC collected from surface, subsurface soils and mine waste, respectively) were investigated and compared to the bioavailability to earthworm (Eisenia fetida). Desorption kinetic data of Zn were fitted to several desorption kinetic models. The ratio ($q_{e,d}/q_0$) of remaining Zn at desorption equilibrium ($q_{e,d}$) to initial sorbed concentration ($q_0$) was in the range of 0.53~0.90 in the mine tailings which was higher than that in NS, except MA. The sequential desorption from the mine tailings with 0.01M Na$NO_3$ and 0.01M $CaCl_2$ showed that appreciable amounts of Zn are resistant to desorption due to aging or sequestration. The SM&T (Standard Measurements and Testing Programme of European Union) analysis showed that the sum of oxidizable (Step III) and residual (Step IV) fractions of Zn was linearly related with its desorption-resistance ($q^{irr}_{max}$) determined by the sequential desorption with 0.01M Na$NO_3$ ($R^2$= 0.9998) and 0.01M $CaCl_2$ ($R^2$= 0.8580). The earthworm uptake of Zn and the desorbed amount of Zn ($q_{desorbed}$ = $q_0-q_{e,d}$) in MB soil were also linearly related ($R^2$ = 0.899). Our results implicate that the ecological risk assessment of heavy metals would be possible considering the relation between desorption behaviors and bioavailability to earthworm.

• 자원환경지질
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• 제43권1호
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• pp.21-31
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• 2010

산화제를 이용한 광산배수 정화에 관한 연구를 위하여 옥동광산으로부터 채수한 갱내수와 침출수를 산화제인 NaOCl와 $H_2O_2$를 이용하여 반응 실험을 실시하였다. 초기 갱내수의 pH와 EC는 각각 5.77, 831 uS/cm 이며, Mg(23.25 mg/l), Mn(14.90 mg/l), Zn(22.99 mg/l)이다. 광미적치장으로부터 유출되는 침출수의 pH와 EC는 6.38, 1920 uS/cm이며, Mg(98.75 mg/l), Mn(3.38 mg/l), Zn(6.16 mg/l)로 갱내수와 다른 양이온 농도 특성을 갖는다. 산화제의 종류와 양에 따라 양이온이 제거 되는 데 소요되는 시간적 차이가 있지만, 갱내수와 침출수에 포함된 Mg, Zn, Mn은 99%이상 제거되었다. Visual MINTEQ 계산결과 포화지수가 0보다 큰 값을 나타내는 화합물이 존재하지 않기때문에 초기 갱내수와 침출수로부터 침전 가능한 광물은 존재하지 않는다. 갱내수와 광미적치장 침출수를 NaOCl과 반응시킬 때 생성되는 침전물은 적갈색의 Mangano-calcite이며, 그 외 Calcite magnesian, Calcite 등의 광물을 포함하고 있다.

• 지질공학
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• 제20권1호
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• pp.79-87
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• 2010

본 연구지역에서 2009년 3월부터 9월 사이에 5개 지점(배경수(BW), 산성광산배수(AMD0, AMD1, AMD2, AMD3))에서 수온, pH, Eh, EC, DO 성분 등이 현장에서 6회 관측되었으며, 폐광산 갱내 출구부(AMD0) 지점에서는 유량이 측정되었다. 일광 폐광산에서 유출되는 산성광산배수는 pH 3 이하의 강산성수이며, Eh 성분은 400~600 mV의 범위이었다. 산성광산배수의 EC 값은 주변 배경수에 비해 10배 이상 높았으며, DO 성분은 유출지점 하류부로 갈수록 대기와의 접촉을 통해 그 값이 증가되었다. 산성광산배수 내 중금속 이온의 농도는 Fe > Cu > Zn > Mn > As > Cd 순이었으며, Fe 성분의 농도가 81.870~474.30 mg/L 로서 가장 높았다. 중금속 성분별 최대농도 관측시기는 5월(As, Cd), 6월(Fe), 7월(Cu, Zn, Mn) 이었으며, 최소농도는 4월(Cd, Mn)과 9월(Fe, Cu, Zn, As)에 관측되었다. 산성광산배수에 용존된 중금속의 유출질량은 Fe 성분 53.44 kg, Cu 성분 6.25 kg, Zn 성분 5.26 kg, Mn 성분 2.13 kg, As 성분 0.14 kg, Cd 성분 0.04 kg 정도이었다. 폐광산에서 갱내에서 1일 동안 유출되는 6개 중금속의 전체 질량은 67.26 kg 이었으며, Fe 성분이 전체 유출질량의 79% 정도를 차지하고 있었다.