• 대한화학회지
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• 제33권5호
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• pp.510-515
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• 1989

테트라에틸렌펜타아민과 포름알데히드의 주형축합반응으로부터 새로운 펜타아자 거대두고리 리간드인 1,3,6,9,12-펜타아자비시클로[10,2,1]펜타데칸(D)의 니켈(II) 및 구리(II) 착화합물 $[Ni(D)]^{2+},\;[Cu(d)]6{2+}\;그리고\;[Cu(D)Cl]^+$를 합성하였다. 거대두고리 리간드인 D에는 한 개의 이미다졸리딘 고리가 있다. $[Ni(D)]^{2+}와 [Cu(D)]^{2+}$는 5-5-5-6 킬레이트고리 배열로 된 평면사각형 구조를 이루며, 5-배위 착이온인 $[Cu(D)Cl]^+$의 구조는 그의 전자스펙트럼으로 볼 때 사각피라미드일 것으로 보인다. 이들 니켈(II) 및 구리(II) 착화합물의 합성과 확인 그리고 분광학적인 특성과 화학적인 특성이 논의된다.

• Bulletin of the Korean Chemical Society
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• 제34권12호
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• pp.3743-3748
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• 2013

A tetradentate ligand of 2-phenyl-4,6-di(pyridin-2-yl)pyrimidine (L) has been synthesized and its complexes with $ZnI_2$ and CuI have been obtained by hydrothermal method. single crystal X-ray diffraction analysis indicates that ligand L coordinates with Zn(II) ions to form a simple four-coordinate di-nuclear complex, while the complexation of L with Cu(I) constructs a one-dimensional chain polymer. The existence of $I^-$ ion hampers the L to assemble grid-type complexes with Zn(II) and Cu(I). Fluorescence spectra show that the L emits blue fluorescence while its Cu(I) polymer decrease the fluorescence intensity and Zn(II) complex quenches the fluorescence.

• Journal of Microbiology and Biotechnology
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• 제11권6호
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• pp.964-972
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• 2001

The kinetics of copper ion biosorption by Pseudomonas stutzeri cells immobilized in alginate was investigated. During the first few minutes of the metal uptake, the copper biosorption was rapid and then became progressively slower until an equilibium was rapid, and then became progressively slower until an equilibrium was reached. At a biomass concentration of 100g/l, the copper biosorption reaction reached approximately 90% of the equilibrium position within 30 min. A Freundich-type adsorption isotherm model was constructed based on kinetics with different amounts of biomass. When using this model, the experimental values only agreed well with the predicted values in a solution containing less than 200 mg/l Cu(II). Desorption of the bound copper ions was achieved using electrolytic solutions of HCl, $H_2SO_4$, EDTA, and NTA (0.1 or 0.5 M). Metal desorption with 0.1 M NTA allowed the reuse of the biosorbent for at least ten consecutive biosorption/desorption cycles, without an apparent decrease in its metal biosorption capability. A packed-bed column reactor of the immobilized biomass removed approximately 95% of the metal in the first 30 liter of wastewater [containing 100 mg/l Cu(II)] delivered at a rate of 20 L/day, and, thereafter, the rate gradually decreased.

• 한국수산과학회지
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• 제12권2호
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• pp.113-117
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• 1979

백합에 대한 수은, 구리 및 카드뮴의 독성정도를 구명하기 위하여 $1978.6.28\~7.15$간 정수식으로 실험을 실시하였다. 실험결과 수은 및 구리 용액에는 농도가 커질수록 점액을 분비하는 개체가 많아졌으나 카드뮴용액과 정상해수에 투입한 백합은 점액을 방출하지 않았다. 1mg/l 농도의 수조에서 15시간후에 분비한 점액은 수은에서는 $42.9\%$, 구리에서는 $14.3\%$ 나타냄으로서 수은이 구리보다 혐기도가 더 컸다. 농도와 사망률과의 관계에서 96시간후에 반치사농도(96hr-LC50)는 수은 0.67mg/l, 구리 7.04mg/l, 카드뮴 7.10mg/l, 로서 독성의 순위는 수은-구리-카드뮴이었다. 또한 각수조에서 $50\%$의 폐사를 일으키는데 소요한 시간(Lethal Tim 50)은 일반적으로 농도가 클수록 L. T.50값이 작아짐으로서 일정 농도에서는 노출시간이 반응을 유발시키는 자극이 되고 있으며 실제 중금속의 40mg/l에서 L.T.50값은 수은 55.8시간, 구리 104.8시간, 카드뮴 111.9시간으로서 동일농도에서는 수은-구리-카드뮴순으로 사망이 일어 났음을 밝혔다.

• 공업화학
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• 제7권6호
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• pp.1053-1060
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• 1996

Sodium amide에 의한 methyl propyl ketone과 ethyl formate의 반응으로 킬레이트 추출제의 하나인 $\beta$-ketohexanal(이하 KHA)를 합성하고, KHA-클로로포름에 의한 구리의 추출평형 실험을 통하여 추출특성을 고찰하였다. 흡광도를 측정하여 추출제 KHA의 상간 분배계수와 해리상수, KHA와 구리간 킬레이트의 안정도 상수와 분배계수 및 총괄 추출 평형상수등을 구하고, 추출기구를 구명하였다 합성한 추출제에 의한 구리의 추출율은 pH 5 이상에서 거의 100%이었고, Cu-Zn-Cd 혼합 금속으로부터 구리의 선택적 추출이 가능하였다. KHA-클로로포름에 의한 구리의 추출 화학종은 $CuR_2$였으며 추출 평형 식은 $Cu^{2+}+2{\overline{HR}}{\rightarrow}{\overline{CuR{_2}}}+2H^+$로 표시되었다.

• 공업화학
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• 제8권4호
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• pp.645-652
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• 1997

백금 회전전극을 이용하여 확산지배영역에서의 구리 착화합물의 환원에 대한 전기화학적 특성조사 및 이에 대한 속도인자들을 구하였다. 황산염 용액내에서 Cu(II)의 환원은 2전자, 1단계 반응이며, 염화물 용액내에서의 Cu(II)는 1전자, 2단계 반응으로 환원된다. 환원반응에서의 전달계수는 황산염 용액내에서 Cu(II)가 가장 작으며, 할로겐염 중에서 Cu(I)의 전달계수는 1에 가까운 값을 나타내었다. 염화물 용액안에서 구리이온의 환원에 대한 표준속도상수는 Cu(II)의 환원이 Cu(I)을 출발물질로 할 경우보다 100배 정도 빠른 값을 나타내었다. 그리고 확산계수는 $Cl^-$존재시의 Cu(II), $I^-$, $Br^-$, $Cl^-$존재시의 Cu(I) 및 $SO_4^{-2}$존재시의 Cu(II)의 순으로 증가하였으며, 각 용액 내에서의 구리이온의 반지름 및 확산에 대한 활성화 에너지도 위의 순서와 동일하게 감소하였다. 회전전극상의 구리전착의 경우 전착전위 및 농도에 따라 불균일한 전착표면을 형성하였으며, 이러한 전착표면의 불균일성은 UV/VIS로 분석이 가능하였다.

• BMB Reports
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• 제32권4호
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• pp.370-378
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• 1999

The effects of carnosine and related compounds (CRC) including anserine, homocarnosine, histidine, and ${\beta}$-alanine, found in most mammalian tissues, were investigated on in vitro glucose oxidation and glycation of human serum albumin (HSA). Carnosin and anserine were more reactive with D-glucose than with L-lysine. In the presence of $10\;{\mu}M$ Cu (II), although carnosine and anserine at low concentrations effectively inhibited formation of ${\alpha}$-ketoaldehyde from D-glucose, they increased generation of $H_2O_2$ in a dose-dependent manner. Carnosine, homocarnosine, anserine, and histidine effectively inhibited hydroxylation of salicylate and deoxyribose degradation in the presence of glucose and $10\;{\mu}M$ Cu (II). In the presence of 25 mM D-glucose, copper and ascorbic acid stimulated carbonyl formation from HSA. Except for ${\beta}$-alanine, CRC effectively inhibited the copper-catalyzed carbonyl formation from HSA. The addition of 25 mM D-glucose and/or $10\;{\mu}M$ Cu (II) to low density lipoprotein (LDL) increased formation of conjugated dienes. CRC effectively inhibited the glucose and/or copper-catalyzed LDL oxidation. CRC also inhibited glycation of HSA as determined by hydroxymethyl furfural and lysine with free ${\varepsilon}$-amino group. These results suggest that CRC may play an important role in protecting against diabetic complications by reacting with sugars, chelating copper, and scavenging free radicals.

• 대한화학회지
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• 제35권4호
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• pp.429-431
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• 1991

• Bulletin of the Korean Chemical Society
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• 제25권6호
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• pp.809-812
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• 2004

Complexation reactions of nitrilotriacetate (NTA) and penicillamine with $Cu^{2+}$ and $Co^{2+}$ have been studied in solution phase using paper electrophoresis technique. The stability constants of the complexes Cu(II)-nitrilotriacetate-penicillamine and Co(II)-nitrilotriacetate-penicillamine have been found to be $6.64{\pm}0.03\;and\;5.86{\pm}0.05$ (logarithm stability constant values), respectively at 35$^{\circ}C$ and ionic strength 0.1 M.

• 자원환경지질
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• 제26권3호
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• pp.311-325
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• 1993

The Ohto and Tohyun copper mine which are located 4 km southeast of Euiseong, Gyeongsangbukdo, Republic of Korea show various common geologic and mineralogic features. Both copper deposits are of hydrothermal-vein types, and associated with fracture system developed during formation of the Geumseong-san caldera in late Cretaceous age. According to structures and mineral assemblages, the mineralization processes have progressed in four stages: three hypogene mineralization stages and one supergene stage. Three hypogene stages are 1) stage I forming $N5{\sim}20^{\circ}E$ veins in the Ohto mine, 2) stage II building $N5^{\circ}W{\sim}N5^{\circ}E$ veins in the Tohyun mine, and 3) stage ill bringing $N80^{\circ}E$ veins which crosscut veins of the stage II. The vein ores consist mainly of pyrite, arsenopyrite, galena and chalcopyrite, minor or trace amounts of magnetite, hematite, pyrrhotite, stannite, bournonite, boulangerite, stibnite, galenobismutite, native bismuth, marcasite, geothite and malachite. The main gangue minerals are quartz and calcite. Wallrock is altered by sericitization, chloritization, pyritization, carbonitization and argillization. Arsenic and copper contents in arsenopyrite increase from stage I to stage III (from 31.28 to 33043 atom.% As) and (from 0.04 to 0040 atom.% Co). Going from stage I to stage III Fe and Mn contents in sphalerite decreases from 12.56 to 0.44 wt.% and from 0.24 to 0.01 wt.%, respectively. The compositional data of arsenopyrite in the early stage I indicate a temperature of $420{\sim}365^{\circ}C$ and sulfur fugacity of $10^{-6.5}{\sim}10^{-8.3}$ atm. Chalcopyrite and pyrrhotite assemblage suggest that Middle stage I was deposited at below $334^{\circ}C$. The compositional data of arsenopyrite in early stage II suggest a temperature range of $425{\sim}390^{\circ}C$ and sulfur fugacity codition of $10^{-6.4}{\sim}10^{-7.3}$ atm. Based on fluid inclusion the Middle stage II was regarded as to be deposited at $420{\sim}337^{\circ}C$ (Chi et al., 1989). Referring composition of sphalerite and stannite middle-late stage II seem to be deposited around $246^{\circ}C$ and $10^{-16.5}$ atm. sulfur fugacity. The ${\delta}^{34}S$ values of sulfide minerals in the Stage I, II, III range from 4.9 to 7.6%0 and indicate igneous ore fluid origin. Based on differences in mineral assemblages, chemical composition and chemical environments of Ohto and Tohyun mine its mineralization are considered to be formed at diffent mineralization ages and by different ore fluids.