• Title/Summary/Keyword: 인의 연속추출법

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용출액의 pH 변화가 토양내 중금속 용출에 미치는 영향과 그에 따른 국내 토양오염 공정시험방법의 문제점

  • 오창환;유연희;이평구;이영엽
    • Proceedings of the KSEEG Conference
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    • 2003.04a
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    • pp.76-79
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    • 2003
  • 국내의 토양오염 공정시험방법에서는 Zn, Ni 추출시 산분해법에 가까운 방법을 사용하는 반면, Cd, Cu, Pb, $Cr^{6+}$ 추출시 0.1N HCl용액으로 산처리하여 1시간을 진탕한 후 이를 필터로 여과하여 분석용액을 추출하는 용출법을 사용하고 있다(환경부, 2001). 시료내에는 완충 물질이 존재하기 때문에 용출법 사용시 초기 pH 인 1(0.1N HCl)이 유지되지 않아 완충능력이 높은 토양의 경우 현재 국내 공정법상의 용출법이 중금속 오염정도를 추정하는데 적절치 않을 수 있다. (중략)

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Effect of Temperature on the Adsorption of Pb(II), Cu(II), Zn(II), and Cd(II) onto Natural Clays Using Combined Adsorption-Sequential Extraction Analysis (혼합 흡착-연속추출법을 이용한 자연 점토의 납(Pb), 구리(Cu), 아연(Zn), 카드뮴(Cd) 흡착 시 온도 영향)

  • Dho, Nam Young;Lee, Seung Rae
    • Journal of the Korean GEO-environmental Society
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    • v.2 no.3
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    • pp.17-35
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    • 2001
  • In this study, we conducted a combined adsorption-sequential extraction analysis(CASA) to investigate temperature effects of single adsorption of lead, copper, zinc and cadmium on natural clays. As a result, it was found that in a single adsorption of lead and copper, about 50% of adsorption was occluded in carbonate phase, and in case of cadmium, about 80% of adsorption was occluded in exchangeable phase. At temperature below $25^{\circ}C$ about 60% of zinc was occluded in exchangeable phase but above $40^{\circ}C$ about 50% of zinc was occluded in carbonate phase. The effect of temperature on each occluded phase was largely observed in Fe-oxide, Mn-oxide and organic occluded phases. Besides, the adsorption of metals on natural clays was an endothermic reaction with the exception of exchangeable phase adsorption.

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Effect of Temperature on Adsorption of Zinc(II) onto Natural Clay by Combined Adsorption-sequential Extraction Analysis (혼합 흡착-연속추출법을 이용한 점토 차수재의 아연(Zn)흡착 시 온도 영향에 관한 연구(I))

  • 도남영;이승래
    • Journal of the Korean Geotechnical Society
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    • v.16 no.2
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    • pp.91-102
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    • 2000
  • 자연점토지반에서의 중금속 흡착시 온도변화에 따른 영향은 지금까지 2차적인 것으로 간주되었다. 그러나 최근 몇몇 연구자들에 의하면 온도변화가 중금속 흡착 거동에 큰 영향을 미친다고 보고하였다. 따라서 본 연구에서는 자연점토 지반에 대한 중금속 아연(Zn) 흡착시 온도변화에 따른 흙의 각 구성성분별 흡착거동을 살펴보기 위해 혼합 흡착-연속추출법(combined absorption-sequential extraction analysis, CASA)을 사용하였다. 실험결과 중금속 아연의 농도가 저농도(50mg/L 미만)일 경우 자연지반에서의 분배양상은 주로 탄산염 형태로 존재하고, 또한 온도의 증가에 따라 탄산염 형태의 흡착량이 증가하는 것을 알 수 있다. 하지만 고농도(50mg/L 이상)의 경우 분배양상은 주로 이온교환형태로 존재한다는 것을 알 수 있다. 그러나 고농도에서의 이러한 분배형태는 온도의 증가에 따라 탄산염형태의 흡착량이 약 20%정도 증가하는 결과를 얻었다. 결론적으로 중금속 아연의 자연점토지반의 각 구성성분 별 흡착거동은 이온교환 형태를 제외하고 온도증가에 따라 증가하는 흡열반응(ΔH0>0)인 것으로 나타났고, 또한 고농도에서의 분배형태는 이온교환 형태에서 탄산염 형태로 변화되는 것을 알 수 있다. 그리고 이온교환 형태의 경우 온도변화에 따라 독립적인 거동을 보였다.

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Phosphate Desorption of Kaolinite KGa-1b (Source Clay) (카올리나이트 KGa-1b (표준 점토)의 인산염 탈착 특성)

  • Cho, Hyen-Goo;Kim, Soo-Oh;Choo, Chang-Oh;Do, Jin-Young
    • Journal of the Mineralogical Society of Korea
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    • v.22 no.4
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    • pp.289-295
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    • 2009
  • The characteristics of phosphate desorption on kaolinite was studied by batch adsorptiondesorption experiments. Desorption procedure was carried out through sequential extraction method at pH 4. The phosphorous contents were measured using UV-VIS-IR spectrophotometer with 820 nm wavelength. The adsorption-desorption reaction of P on kaolinite was irreversible, and most of adsorbed P on kaolinite were not easily dissolved to aqueous solution, but may might be fixed on kaolinite surface. The desorption isotherms were well fitted with the Freundlich and Temkin equations in the case of short reaction and long reaction time, respectively. The desorption reaction was divided into the early fast reaction and the later slow reaction. The percentage of desorption generally decreased with increasing adsorbed P concentration and increasing desorption reaction time.

Solidification/Stabilization of Heavy Metals in Sewage Sludge Prior to Use as a Landfill Cover Material (매립지 복토재로의 활용을 위한 하수슬러지 내 중금속의 고형화/안정화)

  • Park, Youn-Jin;Shin, Won-Sik;Choi, Sang-June;Lee, Hoon-Ha
    • Journal of Korean Society of Environmental Engineers
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    • v.32 no.7
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    • pp.665-675
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    • 2010
  • The effects of chemical binders (ladle slag, ordinary portland cement (OPC), hydroxyapatite and calcium hydroxide) on the solidification/stabilization of heavy metals (Cd, Cu, Ni, Pb, Zn) in sewage sludge were evaluated by chemical leaching tests such as EDTA extraction, TCLP and sequential extraction. The results of EDTA extraction showed that heavy metal concentrations in sewage sludge were highly reduced after solidification/stabilization with slag, cement or calcium hydroxide. However, EDTA interrupted solidification/stabilization of heavy metals by hydroxyapatite. The TCLP-extracted heavy metal concentrations in sewage sludge after solidification/stabilization with chemical amendments were highly reduced. However, Cu concentration in the sewage sludge solidified/stabilized with slag, cement or calcium hydroxide increased because the pH of TCLP solution was higher than 7. Mixtures of sludge 1 : slag 0.2 : calcium hydroxide 0.1 (wt ratio) showed the least leachability in batch TCLP and EDTA extraction. The results of sequential extraction (SM&T, formaly BCR) indicated that the distribution of heavy metals changed from exchangable and carbonate fractions to strongly bound organic fraction. It was found that maximum leachate concentrations of Ba, Cd, Cr and Pb from sewage sludge amended with slag and calcium hydroxide were far below US EPA TCLP regulations.

Effect of Temperature on Cu Adsorption and Competitive Adsorption of Zn and Cu onto Natural Clays using Combined Adsorption-sequential Extraction Analysis(II) (혼합 흡착-연속추출법을 이용한 점토 차수재의 구리(Cu) 흡착 및 아연과 구리 경쟁 흡착 시 온도 영향에 관한 연구(II))

  • 도남영;이승래
    • Journal of the Korean Geotechnical Society
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    • v.16 no.4
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    • pp.157-170
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    • 2000
  • In this study, we conducted a combined adsorption-sequential extraction analysis(CASA) to investigate temperature effects of single and competitive adsorption of zinc and copper on natural clays. As a result, it was found out that in a single adsorption of zinc, the adsorption was mostly in the exchangeable phase, with increase n temperature. In a competitive adsorption of zinc, this trend was so strong that the exchangeable phase adsorption increase up to 80~90%. On the other hand, about 50% of copper was adsorbed in the carbonate occluded phase in single and competitive adsorptions. In the single adsorption the adsorption of carbonate occluded phase increased by 5% with the temperature increase and in the competitive adsorption the increase rate is about twice. The adsorption of zinc and copper on natural clays is an endothermic reaction with the exception of exchangeable phase adsorption.

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Geochemical Properties of Sedimentary Phosphorus of Daechung Lake in Autumn, Korea (추계 대청호 퇴적물 내 인의 지화학적 특성)

  • Shim, Moo Joon;Yang, Yun Mo;Oh, Da Yeon;Hwang, Yun Ho;Lee, Soo Hyung
    • Korean Journal of Ecology and Environment
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    • v.48 no.3
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    • pp.168-175
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    • 2015
  • This study was conducted in autumn to determine phosphorus (P) fraction in sediments of Daechung Lake, to elucidate controlling factors for sedimentary P, and to compare with the other areas. For this study, sediment samples were collected at 6 sites only once on November 2014 using ponar grab and analyzed for solid-phase P (Loosely adsorbed, Fe-bound, Al-bound, detrital apatite, and refractory organic P) by sequential extraction. Total phosphorus (TP) was relatively high in front of Daechung Dam and Hoinam where fish farm was run until 1997. The dominant sedimentary P form was Al-bound P, followed by Fe-bound P, which could be released from sediment to water column during suboxic state. Based on principal component analysis, Al-bound P, Fe-bound, and TP were controlled by grain size of sediments. Loosely adsorbed, detrital apatite, and refractory organic P were relatively highly accumulated at the mouth of major tributaries where suspended sediments were delivered. Sedimentary P concentrations in Daechung Lake sediments were not higher than in other lake sediments. Therefore, based on these results, major controlling factors were grain size and input of suspended sediments from tributaries.

Mineralogical Characteristics of Marine Sediments Cores from Uleung Basin and Hupo Basin, East Sea (동해 울릉분지와 후포분지 해양 퇴적물 코어의 광물학적 특성)

  • Lee, Su-Ji;Kim, Chang-Hwan;Jun, Chang-Pyo;Lee, Seong-Joo;Kim, Yeongkyoo
    • Journal of the Mineralogical Society of Korea
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    • v.28 no.1
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    • pp.71-81
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    • 2015
  • This study was carried out in order to investigate the mineralogical characteristics of the core sediments (03GHP-02 and HB13-2), obtained from the Ulleung Basin and Hupo Basin, Korea. The results on mineral compositions, clay mineral compositions, and the total contents and sequential extraction of different fractions of the phosphorus in core samples showed that those values are different in two cores and also at different depths. In both samples, mineral compositions were the same, composed mainly of quartz, microcline, albite, calcite, opal A, pyrite, and clay minerals (illite, chlorite, kaolinite, and smectite). However, the sample from Hupo Basin contains more opal A. Both samples, especially the ones from Hupo Basin contains more smectite than those reported from East Sea, indicating the influence of paleo-Hwangwei River and the Tertiary Formation of Korea Peninsula. For the samples from Uleung Basin, at 0.7-3.5 m range in depth, the low content of opal A and the low illite crystallinity index can be inferred to indicate the relatively cool climate, corresponding to the ice age. Also, the content of total phosphorus was low in those samples. It was reported that East Sea at that time was isolated from the neighboring seas due to the decrease of the sea level, and as a result, the influx of sediments was supposed to be little through the strait and rivers. For the samples from Hupo Basin, there is no significant changes in clay mineral composition and the distribution of phosphorus with increasing depth. This little change can be interpreted to indicate that the sediments comprising the core might be deposited in a relatively short period of time or deposited in sedimentary environment in which there's no significant changes in sediment supplies. The values of crystallinity index of clay minerals are high in those samples, indicating that it was relatively warm during that time. Although the increase of fluctuation pattern can be observed, showing that the climate of this period often changed, it is supposed that it was generally warm.

Recovery of Copper from Spent Copper Solution of Printed Circuit Board Process by Solvent Extraction Method (인쇄회로기판 제조과정에서 발생되는 동폐액의 용매추출에 의한 재활용)

  • Moon, Young-Hwan
    • Clean Technology
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    • v.2 no.1
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    • pp.47-52
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    • 1996
  • The solvent extraction method was applied on a spent solution containing copper, which was produced in a printed circuit board process, to recover copper and to reuse the etching solution. Lix 64 N ($\alpha$-Hydroxyoxime + $\beta$-Hydroxybenzophenone Oxime) was used as a solvent. The acidic spent copper solution was mixed with and alkaline copper solution to pH=2. The solvent including 30 volume% of Lix 64 N extracted 17.1gr/l of copper from the mixed spent copper solution. In the continuous bench scale experiment, 4 stages for extraction, 2 stages for stripping and 4 stages for washing were used. Recovered copper was recycled as copper sulfate and the raffinate was reused as copper etchant. The percentage of copper recovery and the purity of copper sulfate were higher than 99.9%, respectively.

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The Distribution Characteristics and Contamination of Heavy Metals in Soil from Dalcheon Mine (달천광산 토양 내 중금속의 존재형태 및 오염도)

  • Suh, Ji-Won;Yoon, Hye-On;Jeong, Chan-Ho
    • Journal of the Mineralogical Society of Korea
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    • v.21 no.1
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    • pp.57-65
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    • 2008
  • The geochemical partitioning of arsenic in contaminated soils from a of wet land and tailing of the abandoned mine is examined. Chemical analysis and sequential extraction method by ultrasound-sonication extraction are applied to investigate the mobility and chemical existence conditions of arsenic as well as heavy metals. The results of this study showed that heavy metals concentration of tailings showed as a following order: Fe > As > Cu > Pb > Cr. The highest metal concentration was recognized in samples less than $63\;{\mu}m$ fraction in their particle sizes. Exchangeable and carbonate fractions in soil samples showed following Cu > As > Pb > Fe > Cr for tailings, and Fe > Pb > Cu > As > Cr for reservoir soils, respectively. Arsenic was bound as exchangeable fraction in tailings and its concentration appeared higher than those of the other metals. Thus, As can be easily dispersed into soil and water environments. The obtained results can be used to design soil remediation plan in the study area and require further detailed study to investigate severe environmental pollution of surface water as well as rivers with respect to heavy metals in terms of speciation analysis of toxic elements such as As and Cr.