• Journal of Ecology and Environment
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• 제34권3호
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• pp.315-322
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• 2011

We investigated the effect of Pb uptake by Pinus densiflora and the Pb fraction in forest soil. We also investigated the change in soil physicochemical characteristics, microbial activity, and root exudates of Pinus densiflora in Pb-contaminated soils. Three-year-old pine seedlings were exposed to 500 mg/kg Pb for 12 months. The metal fractions were measured using sequential extraction procedures. Additionally, factors that affect solubility (three soil enzyme activities and amino acids of root exudate compounds) were also determined. The results showed that Pb contamination significantly decreased enzyme activities due to soil characteristics. In addition, organic matter, nitrate content, and Pb concentration were time dependent. The results indicate that changes in the Pb fraction affected Pb uptake by pine trees due to an increase in the exchangeable Pb fraction. The concentrations of organic acids were higher in Pb-spiked soil than those in control soil. Higher rhizosphere concentrations of oxalic acid resulted in increased Pb uptake from the soil. These results suggest that pine trees can change soil properties using root exudates due to differences in the metal fraction.

• 한국세라믹학회지
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• 제25권5호
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• pp.523-531
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• 1988

The dielectric and piezoelectric properties with compositions in Pb(Ni1/3Nb2/3)O3-PbTiO3-PbZrO3-(PNN-PT-PZ)solid solution ceramics were investigated. In this study, the compsition ranges were 30 PNN 45mole%, 20 PT 50mole% and 50 PZ5mole%. As PT fraction were increased the grain size was increased and the fired density was decreased, but the changes of PNN fraction had no effect on the grain size. The Curie temperature was increased when PT and PNN fraction were increased. The displacement was increased but had a great hysteresis loss when PT fraction was increased. In morphotropic phase boundary, the maximum piezoelectric and electromechanical coupling factor were indicated. Morphotropic phase boundary(MPB) was 34 PT 36mole% in chang of compositions.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2003년도 추계학술발표회
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• pp.56-63
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• 2003

Fractional composition and mobility of sediments some heavy metals in Okdong stream are investigated. The fractional scheme for sediment heavy metal was made for five chemically defined heavy metal forms as adsorbed fraction, carbonate fraction, reducible fraction, organic fraction, and residual fraction (Tessier et at., 1979). The most abundant fraction of the sediment heavy metal is reducible and secondly abundant organic fraction. Adsorbed fraction is minor part of the total heavy metals. Mobilization of sediment heavy metals in stream Okdong is occur 19.8∼56.7% of total cadmium concentrate. The most abundant fraction of the sediment metal is organic fraction in Cu, Pb metals investigated. Labile fraction of sediment metals are 0.5%∼48.5% of total Zn, 2.6%∼48.1% of total Pb, 0.2∼36.9% of total Cu respectively, Most of labile fraction consists of reducible fraction for Cd, Zn, adsorbed fraction for Pb, reducible fraction for Cu, adsorbed fraction for Ni. The Mobilization of Zn and Cu is most likely to occur when oxygen depletes and that of Pb and Ni occurs when physical impact, oxygen depletion and pH reduction.

• 한국환경보건학회지
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• 제22권2호
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• pp.25-31
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• 1996

The species of four heavy metals (Cr, Cu, Ni and Pb) associated with sediments (viz exchangeable, carbonates, reducible, organic and residual fractions) were determined with respect to the particle sizes and depths at four locations of the lower Kumho river. In the exchangeable fraction, 3.7~19.52% of Ni and 2.8~14.81% of Pb were found, and in the carbonates fraction 2.12~19.43% of Ni and 1.39~15.42% of Pb were found. The reducible fraction retained about 8.66~44.93% of Cr, 0.41~9.79% of Cu, 17.38~35.74% of Ni and 9.5~44.89% of Pb. In the organic fraction about 0~21.06% of Cr, 2.95~35.74% of Cu, 0~14.66% of Ni and 0~10.65% of Pb were found. The residual fraction retained about 52.6~83.53% of Cr, 63.86~86.39% of Cu, 39.66~66.16% of Ni and 39.97~71.75% of Pb. The order of release or mobility of heavy metals was Ni > Pb > Cr > Cu. Mobile fraction of heavy metals by particle sizes (1.0~0.5 mm and 0.5~0.25 mm) was found to be higher in particle sizes 1.0~0.5 mm than that of 0.5~0.25 mm. The release or mobility of heavy metals by depths (0~5 cm, 5~10 cm and 10~15 cm) was found to be higher in the upper sediments than in the lower sediments, except Cu.

• 생태와환경
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• 제38권3호통권113호
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• pp.334-340
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• 2005

The chemical forms of Cd, Cu, Pb, and Zn were analysed by sequential extraction technique to evaluate the effects of drying and heating of dredged sediments from Lake Chungcho. The most abundant fraction of Cd, Cu, and Zn in the wet and untreated sediment was organic/sulfidic fraction that is state in reducing environment such as the bottom condition of Lake Chungcho, while Pb dominated in residual fraction. This means that the source of Cd, Cu, and Zn in the Chungcho lake sediment is related to the organic degradation and Pb to the erosion from surrounding rocks. With drying and oxidation by dredging, heating treatment, and disposal of the lake sediment, the chemical forms of studied metals changed greatly from organic/sulfidic fraction to adsorbed and reducible fractions which are more labile in oxygenated environment. Organic/sulfidic fraction of Cd, Cu and Pb in the wet sediment was transformed with drying and heating treatments to the labile ones like adsorbed and reducible fraction, but Zn to carbonate and reducible fraction. Heating of the sediment at $320^{\circ}C$ greatly increased the labile fraction of Cd and Cu, while that at $105^{\circ}C$ for Pb and Zn. It is believed that the increase in labile forms of heavy metals in the sediments by drying and heating is caused by the contact with oxygen during drying and heating and by the increase of pH of the pore water at the expense of organic/sulfidic fraction. It is concluded that the drying and oxidation currently used in the treatment of dredged sediment can increase labile forms of heavy metals in the sediment, and the potential of the metal availability from the sediment.

• 한국대기환경학회지
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• 제12권5호
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• pp.523-528
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• 1996

Aerosol Particles were collected in a heaby traffic region in pusan. Samples were collected in two size fractions with a two-stage sampler during the day and the night. Elemental concentrations of these aerosol particles were determined by a PIXE(Proton Induced X-ray Emission) analysis method. The results suggest that the elements originating mainly from natural sources such as Si, Ca, Fe, Cl, and K are dominent in the coarse fraction, but the elements such as S, Pb, Br, and Zn are dominent in the fine fraction. Br/Pb ratio are evaluated in both coarse and fine size fraction, and which are mainly emitted automobile sources. The study further also discussed other Br/Pb ratio related works described elsewhere. Sulfur in the fine fraction was continuously increased during the sampling period without time variation.

• 한국토양비료학회지
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• 제32권4호
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• pp.375-382
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• 1999

본 연구는 폐 금속광산으로부터 발생한 중금속이 주변 환경으로 오염 확산되는 특성과 이를 중금속으로 오염된 토양의 효과적인 복원 방안을 모색하기 위하여 토양내 중금속의 거동 특성을 바탕으로 한 반응 특성을 조사하였다. 토양내 중금속의 이동성과 생물에 의한 흡수에 영향을 미치는 화학적 존재 형태를 중금속이 다량 함유되어 있는 충남 청양의 구봉 폐 금광의 광미와 인위적으로 중금속을 오염시킨 농경지 토양에서 중금속의 토양과의 화학적 결합 형태를 연속 축출법에 의해 분리하였으며, 그 순서에 따라 토양 내에서 다음과 같이 용해도와 이동성이 감소한다: Soluble fraction> exchangeable>carbonate>Fe-Mn oxide>organic>residual fraction. 광미중에 결합 부위에 가장 높은 친화력을 보인 Pb는 대부분 Fe-Mn Oxide와 Carbonate fraction에 존재하였고 이 두 Fraction에 각각 48.3%와 26.8% 나타났다. Cu와 Cd는 각각 organic과 carbonate fraction이 71.8% 42.9%로 가장 높게 나타났다. 이들 fraction은 비교적 이동성이 강한 fraction으로 중금 속의 오염 조사시 반드시 평가되어야 하며, 복원방안 결정시 반드시 고려되어야 할 것이다. 중금속을 인위적으로 흡착시킨 토양에 있어서 중금속은 대부분 Exchangeable, carbonate 그리고 Fe-Mn oxide fraction 흡착되어 있는 것으로 나타났다. 예산통에 있어서 흡착된 Pb는 이들 fraction에 91%가 존재하였고, Cu는 Fe-Mn Fraction에 30.4% 그리고 Cd는 exchangeable fraction에 67.9% 가 존재하였다. 월곡통에 있어서는 흡착된 Cd는 Exchangeable fraction에 93.2%가 존재하였고, Pb와 Cu는 대부분 exchangeable, carbonate와 Fe-Mn Oxide에 흡착되어 있었다. 따라서 토양내 이들 중금속이 가해질 경우 대부분 독성이 강한 오염원으로서 잠재적인 이동성과 생물학적 흡수가능성을 갖는 것으로 나타났다.

• 한국지하수토양환경학회지:지하수토양환경
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• 제10권2호
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• pp.44-51
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• 2005

옥동천 퇴적물을 대상으로 중금속의 존재형태 및 이동성에 관하여 조사하였다. 퇴적물내의 중금속의 존재형태는 adsorbed fraction, carbonate fraction, reducible fraction, organic fraction, and residual fraction 다섯 가지 형태로 분류하였으며, 존재형태 중 제일 많은 부분을 차지하는 부분은 reducible fraction이며 다음으로 organic fraction라 residual fraction으로 나타났다. Adsorbed fraction은 중금속의 존재형태 미미한 부분으로 나타났다. 옥동천 퇴적물내 의 총 카드뮴 중 수체로 이동 가능한 부분은 $19.8{\sim}56.7%$이며, 구리, 납의 경우 대부분이 organic fraction으로 나타났다. 구리와 납의 경우 이동 가능한 형태는 납의 경우 총 납의 농도 중 $2.6{\sim}48.1%$, 구리는 $0.2{\sim}36.9%$로 나타났으며, 아연은 $0.5{\sim}48.5%$로 나타났다. 카드뮴, 아연, 구리의 경우 이동 가능한 부분 중 대부분이 reducible fraction이며, 납과 니켈의 경우 adsorbed fraction으로 나타났다. 구리와 아연의 이동이 기능한 경우는 수중의 산소의 유무에 의해 결정되며, 납이나 니켈의 경우 수중에서의 물리적 영향, 수소이온의 농도가 증가, 산소의 고갈 등에 의해 수층으로 이동할 가능성이 높다.

• 한국환경과학회지
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• 제26권7호
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• pp.847-858
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• 2017

For 26 soil series distributed more than 1% among 63 soil series in Jeju Island, natural uncultivated soil samples were collected. For these soils, the chemical speciation of eight heavy metals (Cd, Cr, Cu, Mn, Ni, Pb, V, and Zn) was examined. Further, the Plant Bioavailability (PB) and Mobility Factor (MF) of these heavy metals were evaluated using Tessier's 5-step sequential extraction method (exchangeable, carbonate, reducible (bound to Fe/Mn oxides), oxidizable (bound to organic matter), and residual fraction). The main form present was residual fraction for Cd and Zn; residual and oxidizable fractions for Cr, Cu, Ni, and Pb; reducible fraction for Mn; and carbonate fraction for V. The average plant availability and average mobility factor were found to be V (57.37%) > Zn (12.49%) > Cd (11.76%) > Cu (11.19%) > Pb (9.37%) > Cr (9.09%) > Mn (3.13%) > Ni (2.63%), and Mn (61.04%) > V (59.94%) > Zn (31.54%) > Cd (17.65%) > Cr (15.66%) > Ni (13.89%) > Pb (13.80%) > Cu (13.53%), respectively.

• 한국지하수토양환경학회지:지하수토양환경
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• 제16권1호
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• pp.42-50
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• 2011

Potential risk of heavy metals to various receptors including humans depends on the bioavailability of the heavy metals in soil. In this study, the heavy metal extraction methods using 0.1N HCl and aqua regia were compared with the Tessier's sequential extraction method to assess whether these two methods can be used to determine the plant-available heavy metal concentrations. The contamination characteristics of copper (Cu), cadmium (Cd), lead (Pb), and arsenic (As) found in soils collected from 75 sites around the closed Janghang smelter were analyzed by extracting heavy metals using 0.1 N HCl, aqua regia, and the Tessier's sequential extraction method. The portion of metals bioavailable to plants is considered as the sum of the fraction 1 (exchangeable) and the fraction 2 (carbonates binding) of the Tessier's 5-step sequential extraction method, which were determined to be 3.1 ${\pm}$ 3.82, 0.6 ${\pm}$ 0.15, 20.6 ${\pm}$ 18.78, and 7.0 ${\pm}$ 6.48 mg/kg for Cu, Cd, Pb, and As, respectively, in this study. When the extraction using aqua regia and the Tessier's extraction method were compared, the extracted Cu and Pb concentrations did not show significant differences, whereas the extracted Cd and As concentrations showed significant differences. These results indicate that the portion of Cd and As in the fraction 5 of the Tessier's sequential extraction can not be extracted using aqua regia. Using aqua regia, which is the official test method, higher concentrations of Cu, Cd, Pb and As were extracted than the sum of the fraction 1 and 2. The results show that only 9, 40, 39 and 10% of Cu, Cd, Pb and As using aqua regia can be uptaken by plants (i.e., plant-available). Using 0.1N HCl, the portion of Cd equivalent to about 66% the fraction 1 could be extracted, while, with Pb, the portion of the fraction 1 and about 90% of the fraction 2 could be extracted. With As, the portion equivalent to the fraction 1, 2 and 79% of the fraction 3 was extracted, while with Cu, the portion equivalent to the fraction 1, 2, 3 and 20% of the fraction 4 was extracted using 0.1N HCl.