• Economic and Environmental Geology
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• v.43 no.5
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• pp.477-490
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• 2010

The Gagok stratabound skarn deposit is the result of the intrusion of the Cretaceous granitic pluton into the Paleozoic calcareous rocks. The subvolcanic intrusion ranges in composition from quartz monzonite to granite porphyry with I-type, calc-alkaline and weakly peraluminous characteristics. Both endoskarn and exoskarn are developed at the Gagok Zn-(Pb) deposit, with more exoskarn than endoskarn. Geochemical and mineralogical characteristics in the Seongok and Wolgok orebodies can be treated in terms of self-organization. Sphalerites in the Gagok ore can also incorporate minor amounts of Mn, Cd, Cu and In. Trace element concentrations in different orebodies vary because fractionation of a given element into sphalerite is influenced by formation temperature and the amount of sphalerite in the ore. A group of high In/Zn and Cd/Zn ratios in ores, and low Mn/Fe ratios in sphalerites are correlated with proximal processes of a magmatic source. The pattern of minor/trace element variations in ores and sphalcrites can be used for petrogenetic interprctation, e.g., orebody zonation related to crystallization temperature and fluid d sources.

• Resources Recycling
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• v.23 no.6
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• pp.12-21
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• 2014

Nickel oxide ores are composed of two kinds of minerals; one is saprolite that is processed by smelting to obtain nickel products, and the other is limonite that is used in hydrometallugical processes. It is not efficient economically to process the mixture of limonite and saprolite, so the processes to saparate the ore mixture should be developed. In the present study, the mixture was separated by dry-classification after liberationg using grindability difference between limonite and saprolite. Consequently, it is possible to obtain the limonite with less than 10% of Mg+Si contents, which could be treated by hydrometallurgical processes, when the limonite contain less than 30% of saprolite.

• Geophysics and Geophysical Exploration
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• v.24 no.4
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• pp.180-193
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• 2021

The complex resistivity method is an exploration technique that can obtain various characteristic information of underground media by measuring resistivity and phase in the frequency domain, and its utilization has recently increased. In this paper, a three-dimensional inversion algorithm for the CR data was developed to increase the utilization of this method. The Poisson equation, which can be applied when the electromagnetic coupling effect is ignored, was applied to the modeling, and the inversion algorithm was developed by modifying the existing algorithm by adopting comlex variables. In order to increase the stability of the inversion, a technique was introduced to automatically adjust the Lagrangian multiplier according to the ratio of the error vector and the model update vector. Furthermore, to compensate for the loss of data due to noisy phase data, a two-step inversion method that conducts inversion iterations using only resistivity data in the beginning and both of resistivity and phase data in the second half was developed. As a result of the experiment for the synthetic data, stable inversion results were obtained, and the validity to real data was also confirmed by applying the developed 3D inversion algorithm to the analysis of field data acquired near a hydrothermal mine.

• Geophysics and Geophysical Exploration
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• v.7 no.4
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• pp.217-224
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• 2004

Self-potential and electrical resistivity methods were conducted for locating the auriferous mineralized zone, called Jija Vein, of Sambo mine, Limsu-ri, Haeje-myeon, Muahn-gun, Jeollanam-do. The host rocks of the mineralization include gneiss, rhyolite and felsic dyke. Ore vein is mainly fissured-filling type and sulfide minerals, such as pyrite, are disseminated in country rock. By the electrical responses from SP and surface resistivity methods., the mineralized zone is supposed to extend about 360 m directed N5W with the width of 20 m to 30 m. From resistivity tomograms using inclined borehole to surface, the ore body shape is interpreted as the width of 20 m in depth 40 m to 50 m.

• 한국신재생에너지학회:학술대회논문집
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• 2010.06a
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• pp.116.1-116.1
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• 2010

저급 연료원인 오일샌드는 아스팔트와 같은 중질유를 10% 이상 함유한 모래 또는 사암으로서, 겉으로는 시커먼 흙이나 모래처럼 보이나 내부에는 bitumen, 모래(점토) 및 물 등이 광물질 70~80%, bitumen 10~18%, 물 3~5% 정도의 비율로 혼합되어 있는데, 가열 또는 용매 추출 방식으로 오일샌드에 포함되어 있는 bitumen을 분리하여 정제하면 원유를 생산할 수 있으므로 고유가 시대의 대체에너지원으로 세계적인 석유회사들이 개발을 진행하고 있다. 따라서, 본 연구에서는 이러한 저급 연료원인 오일샌드 bitumen의 활용기술 개발을 위하여 기초특성 분석 결과 bitumen과 가장 유사한 특성을 가지는 것으로 파악된 중질잔사유를 대상으로 가스화를 통한 액체연료 전환을 위해 고점도 시료공급장치, 가스화기, 집진장치, 탈황장치, 수성가스 전환장치, 합성가스 압축장치, DME 전환장치 등으로 구성되는 시스템을 구축한 후 시험을 진행하였다.

• Proceedings of the Plant Resources Society of Korea Conference
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• 2012.05a
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• pp.6-6
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• 2012

천연물의약품은 식물, 동물, 미생물 및 이의 세포내용물과 광물 등 자연계에 존재하는 물질을 의약품으로 사용한 것으로 말하며, 이들 중 대부분은 식물 유래이다. 식물추출물은 다양한 성분들이 서로 상호작용하면서 혼합되어 있는 형태로 다양한 질환에 대한 조합치료 (combination therapy)에 이용될 수 있어, 생체내에서 다중 타겟에 영향을 미치므로 천연물의 조추출물 (crude extract) 또는 다양한 성분이 함유되어 있는 용매분획물의 형태를 의약품으로 개발하거나, 이로부터 분리된 단일 성분 화합물 및 이의 합성유도체에 대하여 새로운 의약품, 즉 신약을 개발하고자 하는 노력이 시도되고 있다. 2011년 현재 전체의약품 시장에서 천연물의약품 및 천연물유래 의약품이 약 60%이상을 차지하고 있다. 그러나, 국내 천연물의약품 즉, 천연물신약의 개발은 2010년 기준으로 식약청 임상허가 신청현황에서 70%가 관절염과 관련된 의약품일 정도로 고령화에 따른 건강기능식품의 개발방향과 일치되고 있는 경향을 나타내고 있어 다양한 질환을 타겟으로 한 의약품의 개발이 미흡것으로 나타나고 있다. 이러한 경향은 천연물신약개발에 대한 프로세스에 대한 이해의 부족으로 새로운 시도가 이루어지지 않고 있음을 시사하며, 따라서 천연물신약허가에 필요한 제출자료 및 각 자료생산을 위한 방법 등 천연물신약 개발 및 허가를 위한 프로세스에 대하여 설명하였다.

• Proceedings of the Korean Institute of Electrical and Electronic Material Engineers Conference
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• 2003.07a
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• pp.237-242
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• 2003

투어멀린(Tourmaline)은 비대칭 쌍극자를 가진 유극성 결정체로 광물 중에서 영구적으로 전기분극 특성을 띄고 있는 유일한 물질로써, 일명 "전기석"이라고 알려져 있다. 자체의 미약 전류(약 0,06mA)와 함께 음이온 및 원적외선의 발생으로 최근 우리 주변에서 건강과 환경정화를 위한 관심 대상의 투어멀린은 육방정계의 압전성 및 초전성을 띄는 붕규산염으로, 물분자를 만나면 수소($H^+$)와 수산기($OH^-$)로 분해하여 친수기와 소수기를 구분하여 발생하며, $H^+$와 $OH^-$는 각각 $H_2O$와 결합하여 활성이 강한 hydronium ion($H_3O^+$)과 계면활성 작용이 있는 hydroxyl ion($H_3O_2^-$)을 생성한다. 물속에서 불안정한 상태로 존재하는 수산기는 hydroxyl (-)ion을 형성하여 약 알카리성($pH{\sim}7.4$)을 띄고, 물의 클러스터(cluster)를 세분화하는 수질개선 기능과 함께 살균, 항균 및 세균번식억제 효과를 갖는 것으로 확인되었다. 따라서 투어멀린 소결체를 활용하여 그 처리수의 특성조사 및 기능개발과 함께 대장균의 번식억제 작용 및 살균작용과 수질개선 기능 등 유용한 결과의 분석으로부터 다양한 응용성을 확보하였다.

• Journal of Periodontal and Implant Science
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• v.32 no.4
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• pp.801-809
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• 2002

The ultimate goal of periodontal therapy is to promote the regeneration of lost periodontal tissue, there have been many attempts to develop a method to achieve this goal, hut none of them was completely successful. The purpose of this study is to evaluate the effects of Bio-Oss(R) on alkaline Phosphatase (ALP) activity in human fetal osteoblasts (hFOB1). The results of this study were as follows, in ALP Activity, 100 ${\mu}g/ml$ Bio-Oss(R) treated group showed significantly increased value than negative control group, but positive group($10^{-7}$ M dexamethasone treated group) showed the highest ALP activity at 3 day. In mineralization assay, numerous mineralized nodules were identified as darkly stained spots in 100${\mu}g/ml$ Bio-Oss(R) treated group than two control groups, whereas a small number of mineralized nodules were showed in the positive control. ALP may relate to the initial phase of bone nodule formation. On the basis of these results, this study showed Bio-Oss(R) is capable of accelerating new bone formation through hFOBl differentiation in vitro.

• Mineral and Industry
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• v.26
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• pp.1-12
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• 2013

In this study, an accelerated carbonation process was applied to stabilize hazardous heavy metals of industrial solid waste incineration (ISWI) bottom ash and fly ash, and to reduce $CO_2$ emissions. The most commonly used method to stabilize heavy metals is accelerated carbonation using a high water-to-solid ratio including oxidation and carbonation reactions as well as neutralization of the pH, dissolution, and precipitation and sorption. This process has been recognized as having a significant effect on the leaching of heavy metals in alkaline materials such as ISWI ash. The accelerated carbonation process with $CO_2$ absorption was investigated to confirm the leaching behavior of heavy metals contained in ISWI ash including fly and bottom ash. Only the temperature of the chamber at atmospheric pressure was varied and the $CO_2$ concentration was kept constant at 99% while the water-to-solid ratio (L/S) was set at 0.3 and $3.0dm^3/kg$. In the result, the concentration of leached heavy metals and pH value decreased with increasing carbonation reaction time whereas the bottom ash showed no effect. The mechanism of heavy metal-stabilization is supported by two findings during the carbonation reaction. First, the carbonation reaction is sufficient to decrease the pH and to form an insoluble heavy metal-material that contributes to a reduction of the leaching. Second, the adsorbent compound in the bottom ash controls the leaching of heavy metals; the calcite formed by the carbonation reaction has high affinity of heavy metals. In addition, approximately 5 kg/ton and 27 kg/ton $CO_2$ were sequestrated in ISWI bottom ash and fly ash after the carbonation reaction, respectively.

• Economic and Environmental Geology
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• v.21 no.2
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• pp.149-164
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• 1988

Electrum-sulfide mineralization of the Samgwang and Sobo mines of the Cheongyang Au-Ag area was deposited in two stages of quartz and calcite veins that fill fault zones in granite gneiss. Radiometric dating indicates that mineralization is Early Cretaceous age (127 Ma). Fluid inclusion and sulfur isotope data show that ore mineralization was deposited at temperatures between $340^{\circ}$ and $180^{\circ}C$ from fluids with salinities of 1 to 8 wt. % equiv. NaCl and a ${\delta}^{34}S_{{\sum}S}$ value of 2 to 5 per mil. Evidence of fluid boiling (and $CO_2$ effervescence) indicates a range of pressures from < 200 to $\approx$ 700 bars, corresponding to depths of ${\approx}1.5{\pm}0.3\;km$ in a hydrothermal system which alternated from lithostatic toward hydrostatic conditions. Au-Ag deposition was likely a result of boiling coupled with cooling. Meaured and calculated hydrogen and oxygen isotope values of ore-forming fluids indicate a significant meteoric water component, approaching unexchanged paleometeoric water values. Comparison of these values with those of other Korean Au-Ag deposits reveals a relationship among depth, Au/Ag ratio and degree of water-rock interaction. All investigated Korean Jurassic and Cretaceous gold-silver-bearing deposits have fluids which are dominantly evolved meteoric waters, but only deeper systems (${\geq}1.5\;km$) are exclusively gold-rich.