• 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.

• 한국광물학회지
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• 제27권4호
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• pp.207-222
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• 2014

폐-광석으로부터 금속구리분말을 회수하기 위하여 더미 미생물용출, Fe 제거와 전기분해실험을 수행하였다. Cu가 0.034% 함유된 폐-광석시료에 대하여 더미 용출실험을 수행한 결과, Cu 용출률은 박테리아 용출-용액에서 61%, 황산 용출-용액에서 62%로 나타났다. Fe를 효과적으로 제거하기 위하여 더미 용출-용액에 NaOH, $H_2O_2$ 및 $Ca(OH)_2$를 각각 적용한 결과 $H_2O_2$가 가장 효과적인 Fe 제거제로 선정되었다. 전해질 용액을 준비하기 위하여 $H_2O_2$를 더미 용출-용액에 처리한 결과 박테리아 용출-용액에서 Fe가 99%, 황산 용출-용액에서 60%로 제거된 반면에 Cu 제거율은 각각 5%와 7%로 나타났다. 이 용액에 대하여 전기분해 실험을 수행한 결과 Cu 회수율이 박테리아 용출-용액에서 98%, 황산 용출-용액에서 76%로 나타났다. 모수석 형태의 금속구리분말이 양쪽 용출-용액에서 회수되었다.

• 자원환경지질
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• 제5권4호
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• pp.211-217
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• 1972

The Second Yeon Hwa Mine which belongs to a so called Lead-Zines Belt Area in the central east Korea is located at about 10 km northeast of the Seogpo railway station on Yeongdong Line. The exploitation of the mine started in June, 1969 and furnished the machinary ore dressing plant in November, 1971. The current monthly production of rude ore is 15,000 meteric tons. The results of the study on the lead-zinc-copper deposits of the Second Yeonhwa mine are summerized as follows: (1) main ore deposits of the mine are localized in the Pungchon Limestion formation of Cambrian age, (2) related ingneous rock with ore deposits is granite porphyry, which distributed in NS and $N50^{\circ}W$ trend, (3) ore solution ascended along the $N50^{\circ}W$ trend which represents folding axis and fault plane and mineralized selectively in the limestone formation. (4) high grade ore deposits are localized in concave and convex boundaries of granite porphyry, and hanging walls of shale bed ($P_2S$ shale bed) in Pungchon Limestone formation and (5) skarn minerals are consisted of garnet, hedenbergite, diopside, and sulfide minerals are composed of zincblenede, galena, phyrhotite, pyrite and some amount of chalcopyrite and arsenopyrite.

• 자원환경지질
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• 제17권4호
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• pp.245-258
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• 1984

Geoje copper ore deposits are fissure filled copper veins which developed in late Cretaceous pyroclastics, andesite and shale. Mineral paragenesis reveals a division of the hydrothermal mineralization into three stages: Stage I, deposition of pyrite, magnetite, specularite, quartz and chlorite; Stage II, deposition of chalcopyrite, sphalerite, galena, tetrahedrite, aikinite, cosalite, electrum, quartz and chlorite; Stage III, deposition of barren calcite. Filling temperatures of fluid inclusions in quartz of stage I range from 171 to $282^{\circ}C$ whereas fluid inclusions in quartz and sphalerite of stage II range from 213 to $262^{\circ}C$ and from 186 to $301^{\circ}C$ respectively. Salinities of fluid inclusions in quartz of stage I range from 5.2 to 11.2 weight percent equivalent to NaCl. Salinities of fluid inclusions in quartz and sphalerite of stage II range from 6.6 to 10.9 and from 7.1 to 14.4 weight percent equivalent NaCl. Salinities of ore fluid during major mineralization stage in this deposits reveal nearly the same ranges as those of many copper deposits in Koseong copper mining district which located about 30km apart from Geoje mine. But filling temperatures of fluid inclusions formed during major copper mineralization stage in this deposits show slightly lower than those of copper deposits in Koseong copper mining district.

• 한국지하수토양환경학회지:지하수토양환경
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• 제14권1호
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• pp.29-35
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• 2009

본 연구에서는 석탄광산 배수(CMD)를 전기정화법으로 처리 시 발생되는 슬러지를 흡착제로 금속광산 산성배수(AMD)중 중금속 처리 시 pH와 온도변화에 따른 중금속 흡착 거동을 연구하고자 하였다. 실험결과 CMDS의 pH$_{zero\;point\; charge}$:(pH$_{zpc}$)는 5로 나타났다. pH영향의 경우 구리, 아연, 카드뮴, 철은 pH 증가에 따라 제거율은 증가하였고, 구리의 경우 흡착량은 pH와 상관없이 0.64 mg g$^{-1}$ sludge로 나타났다. pH 5 이상일 때 기타 중금속 흡착량은 pH3일 때의 1.1 배로 나타났고 크롬의 경우 pH 7 이상에서 다소 증가하였는데 이는 크롬이 $Cr(OH)_{6}^{3-}$형태로 미량 용출되었기 때문이다. 온도의 영향에서 pH3일때 온도증가에 따라 중금속 흡착량은 증가하였고, 선택도Cd>Fe>Zn>Cu순으로 나타났다. pH 5이상에서 최대 흡착량(q$_{max}$)은 Cu와 Zn의 경우 각각 2.747mg g$^{-1}$와 2.525mg g$^{-1}$로 더 이상의 흡착이 일어나지 않아 온도의 영향을 받지 않은 것으로 판단된다.

• Geomechanics and Engineering
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• 제9권2호
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• pp.195-205
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• 2015

Barricade failures generally occur at the early times of paste backfill when it is fresh in the stopes. The backfill strength increases and need for barricading pressure decreases as a result of the hydration reactions. In this study, paste backfill barricades of Cayeli copper mine were investigated to design cemented mineral processing plant tailings as barricade body concrete. Paste backfill in sub-level caving stopes of the mine needs to be barricaded for only four or five days. Therefore, short term strength and workability tests were applied on several cemented tailings material designs. Barricade failure mechanisms, important points of barricade designing and details of the new concrete material are explained in this work. According to the results obtained with this experimental study, the tailings were assessed to be used in concrete applied as temporary supports such as cemented paste backfill barricades.

• 대한지하수환경학회지
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• 제6권3호
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• pp.120-125
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• 1999

충북 단양에 위치한 조일 광산에서 채취한 구리와 아연으로 오염된 광미(광산 폐기물로서 금속 추출 후 남은 찌꺼기) 처리방안으로서 생물학적 용출기법(bioleaching)의 효율 증진에 관한 연구를 수행하였다. 기본 배지 조성(9 K medium) 중 미생물의 성장 및 증식에 영향을 미치는 에너지원, 인, 질소원의 농도를 변화시켜가며 배지 조성에 따른 중금속의 생물학적 용출 특성을 관찰하였다. 먼지, 배지조성 중 인의 농도를 0 mM. 3.0 mM, 6.0 mM 각각 조절하여 중금속의 용출효율을 관찰한 결과. 인을 첨가하지 않았을 때 아연. 구리 각각 98.8%와 47.5%의 용출효율을 보인 반면 인의 농도가 6.0mM 로증가 시켰을 경우. 오히려 중금속의 용출효율이 감소하였다. 배지내 질소원의 농도를 0 mM. 45 mM, 90 mM로 조절하여 중금속의 용출정도를 알아본 결과. 45 mM 농도로 주입하였을 때 아연. 구리 각각 85%,와46.4%로 90 mM 농도에보다 더 높은 용출효율 나타내었다. 에너지원 변화에서는 아연의 경우 에너지원을 첨가하지 않았을 때 93%의 용출효율을 보였고. 구리의 경우는 160 mM 첨가했을 때 46.4%로 가장 높은 중금속 용출효율을 보였다.

• 한국지하수토양환경학회지:지하수토양환경
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• 제20권4호
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• pp.83-89
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• 2015

Soil samples collected in an area of Gahak Mine were investigated for the characterization of mineralogical and physicochemical properties of contaminants in soils. It is found that soils in the study area are contaminated by lead (Pb), copper (Cu), zinc (Zn), cadmium (Cd), in which their concentrations are 595.3 mg/kg, 184.9 mg/kg, 712.8 mg/kg, and 10.64 mg/kg, respectively. All the concentrations exceed the concern criteria of Korean standard. Upon distribution patterns of metals identified by the sequential extraction procedure, our results show that more than 50% of metals are found as a residual type, and 30% are accounted for the association of Fe/Mn oxides. Interestingly, XRD results show that minium (Pb₃O₄) and cuprite (Cu₂O) are identified in the soil samples, suggesting that the sources of the contaminants for Pb and Cu are these minerals. In SEM images, tens of µm of Pb oxides and Pb silicate-minerals are observed. We, therefore, note that the contamination of metals in the study area results from the direct influx and disturbance of tailings. Our findings indicate that the characterization of physicochemical and mineralogical properties of contaminated soils is a critical factor and plays an important role in optimizing recovery treatments of soils contaminated in mine development areas.

• 자원환경지질
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• 제53권3호
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• pp.235-244
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• 2020

폐광산 지역에서 발생하는 광산배수의 오염원소중 하나인 구리(Cu)는 낮은 농도에서도 독성을 지니고 있어 수계환경에 노출되기 전에 처리되어야 한다. 본 연구에서는 경남 고성군 S광산의 갱내수 정화시설의 Cu 제거효율을 개선하기 위해 석회석과 폐상퇴비를 혼합한 자연정화 기반의 반응조를 이용하여 약 9개월 동안 현장 파일럿실험을 수행하였다. 반응조별 유입수 대비 pH 증가량과 Cu 제거효율은 Successive Alkalinity Producing System (SAPS) > Reducing and Alkalinity Producing System (RAPS) > 석회석반응조 순으로 나타났다. SAPS조와 RAPS조에서는 석회석의 영향과 동시에 유기물의 분해로 인한 알칼리도의 부과로 석회석반응조보다 높은 pH 환경을 조성하였다. pH가 증가할수록 Cu 제거효율이 높아지는 결과를 통해 pH 상승이 Cu를 처리하는 주된 기작임을 확인할 수 있었다. 또한 황산염환원박테리아(Sulfate Reduction Bacteria, SRB)가 SAPS조에서 가장 많이 활성화 된 것을 확인 할 수 있어, 황산염환원반응도 Cu를 제거시키는 기작에 관여함을 판단할 수 있었다. 본 연구는 S광산에서 발생하는 광산배수의 특성에 알맞은 맞춤형 정화공정을 도출하기 위해 현장 그대로의 조건에서 실험을 수행한 것에 의의가 있으며, 향후 정화시설의 개선에 있어 공법 선정에 도움을 줄 수 있을 것이다.

• Journal of Microbiology and Biotechnology
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• 제26권11호
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• pp.1983-1992
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• 2016

Pseudomonas strains isolated from the heavily contaminated Lubin copper mine and Zelazny Most post-flotation waste reservoir in Poland were screened for the presence of integrons. This analysis revealed that two strains carried homologous DNA regions composed of a gene encoding a DNA_BRE_C domain-containing tyrosine recombinase (with no significant sequence similarity to other integrases of integrons) plus a three-component array of putative integron gene cassettes. The predicted gene cassettes encode three putative polypeptides with homology to (i) transmembrane proteins, (ii) GCN5 family acetyltransferases, and (iii) hypothetical proteins of unknown function (homologous proteins are encoded by the gene cassettes of several class 1 integrons). Comparative sequence analyses identified three structural variants of these novel integron-like elements within the sequenced bacterial genomes. Analysis of their distribution revealed that they are found exclusively in strains of the genus Pseudomonas.