• 대한안전경영과학회지
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• 제15권2호
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• pp.185-192
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• 2013

This research identified approachable management innovation technique from SCM point of view, and analyzed sales/logistics, integrated production planning, phenomenon of cooperation and suggested an innovation model over this for strengthening competitiveness of a case company. Process innovation model with an enterprise viewpoint is designed and suggested to solve the previous ares for improvement, and suggested various models of an ordering management model, available delivery management model, logistics operation model based on planning and S&OP model.

• 한국재료학회지
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• 제27권5호
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• pp.263-269
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• 2017

Fe-Si-Cr ferroalloy is predominantly produced by carbothermic reduction. In this study, silicothermic and carbothermic mixed reduction of chromite ore to produce Fe-Si-Cr alloy is suggested. As reductants, silicon and silicon carbide are evaluated by thermochemical calculations, which prove that silicon carbide can be applied as a raw material. Considering the critical temperature of the change from the carbide to the metallic form of chromium, thereduction experiments were carried out. In these high temperature reactions, silicon and silicon carbide act as effective reductants to produce Fe-Si-Cr ferroalloy. However, at temperatures lower than the critical temperature, silicon carbide shows a slow reaction rate for reducing chromite ore. For the proper implementation of a commercial process that uses silicon carbide reductants, the operation temperature should be kept above the critical temperature. Using equilibrium calculations for chromite ore reduction with silicon and silicon carbide, the compositions of reacted metal and slag were successfully predicted. Therefore, the mass balance of the silicothermic and carbothermic mixed reduction of chromite ore can be proposed based on the calculations and the experimental results.

• 자원리싸이클링
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• 제17권4호
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• pp.47-56
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• 2008

본 연구는 플라스틱과 무연탄을 혼합한 다음 소결하여 합금철용으로 사용 가능한 코크스를 얻기 위하여 수행 되었으며, 무연탄과 플라스틱의 연소 특성 및 물성을 조사하고, 선탄기초실험을 행하여 다음과 같은 결론을 얻었다. 1. 삼척지역의 3종 무연탄 시료에 대한 물성 측정 결과 각 무연탄 시료에는 $100{\mu}m$ 이상의 회분들이 $25{\sim}30%$ 정도 함유되어 있으며 발열량은 태안시료 5,205cal/g, 장성시료 4,893cal/g, 경동시료 4,873cal/g 이었다. 2. 선탄 기초 실험 결과 3종의 국산 무연탄을 중액선별로 선탄하는 경우에 중액의 비중이 2.4이고 석탄의 입도는 $35{\sim}140mesh$로 조절하는 것이 적당할 것으로 나타났다. 3. 플라스틱의 열분해 특성상 코크스용 점결제로 사용이 가능한 플라스틱은 분말 페놀수지, 액상 페놀수지, SAN, 멜라민수지 등 이며, 공정의 단순화를 위해서는 액상 페놀수지가 가장 적합한 것으로 판단되었다.

• 자원리싸이클링
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• 제17권6호
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• pp.57-61
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• 2008

본 연구는 페놀수지와 무연탄을 혼합한 다음 소결하여 합금철용으로 사용 가능한 코크스를 얻기 위하여 수행 되었으며 무연탄과 페놀수지를 혼합하여 성형코크스를 제조하는 경우에 있어서 코스의 강도에 미치는 여러 인자들의 영향을 검토하여 다음과 같은 결론을 얻었다. 합금철용 코크스 제조 공정은 $35{\sim}325$ mesh로 입도 조절된 저회분 함량의 무연탄에 액상 페놀수지를 6% 정도 첨가하여 혼합한 다음 $10{\sim}50\;kgf/cm^2$로 압착하여 펠릿을 제조하고, 이 펠릿을 $50^{\circ}C$에서 6시간 이상 탈수하고 $200^{\circ}C$에서 180분 동안 경화 시킨 다음 $1200^{\circ}C$에서 6시간 소결하면 $100{\sim}150\;kgf/cm^2$인 합금철용 코스가 얻어짐을 확인하였다.

• 한국분말야금학회:학술대회논문집
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• 한국분말야금학회 2006년도 Extended Abstracts of 2006 POWDER METALLURGY World Congress Part2
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• pp.824-825
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• 2006

Homogeneous microstructures of the PM compacts are difficult to attain when mixed elemental powders are used. This study examined the microstructures of pressed-and-sintered and MIM products that contain Ni and Mo.Ni-rich areas, which were lean in carbon and were soft and were found easily in regular specimens. Gaps or cracks near the Ni-rich or Mo-rich areas were also frequently observed. This problem worsened when Ni and Mo particles were large and were irregular in shape. By using ball milling treatment and ferroalloy powders, the microstructure homogeneity and mechanical properties were improved. The addition of 0.5wt%Cr further improved the distribution of Ni because Cr reduced the repulsion effect between nickel and carbon. With the elimination of Ni-rich areas, more bainites and martensites were formed and mechanical properties were significantly improved.

• Safety and Health at Work
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• 제4권3호
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• pp.123-135
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• 2013

Exposure to manganese (Mn) is associated with neurobehavioral effects. There is disagreement on whether commonly occurring exposures in welding, ferroalloy, and other industrial processes produce neurologically significant neurobehavioral changes representing parkinsonism. A reviewof methodological issues in the human epidemiological literature onMnidentified: (1) studies focused on idiopathic Parkinson disease without considering manganism, a parkinsonian syndrome; (2) studies with healthy worker effect bias; (3) studies with problematic statistical modeling; and (4) studies arising from case series derived from litigation. Investigations with adequate study design and exposure assessment revealed consistent neurobehavioral effects and attributable subclinical and clinical signs and symptoms of impairment. Twenty-eight studies show an exposure-response relationship between Mn and neurobehavioral effects, including 11 with continuous exposure metrics and six with three or four levels of contrasted exposure. The effects of sustained low-concentration exposures to Mn are consistent with the manifestations of early manganism, i.e., consistent with parkinsonism. This is compelling evidence thatMnis a neurotoxic chemical and there is good evidence that Mn exposures far below the current US standard of $5.0mg/m^3$ are causing impairment.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2009년도 특별 심포지엄
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• pp.57-65
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• 2009

Selection of good mineralized area is a combination of the integration of all the available geo-scientific (i.e., geological, geochemical, and geophysical) information, extrapolation of likely features from known mineralized terrenes and the ability to be predictive. The time-space relationships of the hydrothermal deposits in the East Asia are closely related to the changing plate motions. Also, two distinctive hydrothermal systems during Mesozoic occurred in Korea: the Jurassic/Early Cretaceous deep-level ones during the Daebo orogeny and the Late Cretaceous/Tertiary shallow geothermal ones during the Bulguksa event. Both the Mesozoic geothermal system and the mineralization document a close spatial and temporal relationship with syn- to post-tectonic magmatism. The Jurassic mineral deposits were formed at the relatively high temperature and deep-crustal level from the mineralizing fluids characterized by the relatively homogeneous and similar ranges of ${\delta}^{18}O$ values, suggesting that ore-forming fluids were principally derived from spatially associated Jurassic granitoid and related pegmatite. Most of the Jurassic auriferous deposits (ca. 165-145 Ma) show fluid characteristics typical of an orogenic-type gold deposits, and were probably generated in a compressional to transpressional regime caused by an orthogonal to oblique convergence of the Izanagi Plate into the East Asian continental margin. On the other hand, Late Cretaceous ferroalloy, base-metal and precious-metal deposits in the Taebaeksan, Okcheon and Gyeongsang basins occurred as vein, replacement, breccia-pipe, porphyry-style and skarn deposits. Diverse mineralization styles represent a spatial and temporal distinction between the proximal environment of sub-volcanic activity and the distal to transitional condition derived from volcanic environments. However, Cu (-Au) or Fe-Mo-W deposits are proximal to a magmatic source, whereas polymetallic or precious-metal deposits are more distal to transitional. Strike-slip faults and caldera-related fractures together with sub-volcanic activity are associated with major faults reactivated by a northward (oblique) to northwestward (orthogonal) convergence, and have played an important role in the formation of the Cretaceous Au-Ag lode deposits (ca. 110-45 Ma) under a continental arc setting. The temporal and spatial distinctions between the two typical Mesozoic deposit styles in Korea reflect a different thermal episodes (i.e., late orogenic and post-orogenic) and ore-forming fluids related to different depths of emplacement of magma (i.e., plutonic and sub-volcanic) due to regional changes in tectonic settings.

• 자원환경지질
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• 제40권5호
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• pp.517-535
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• 2007

중생대부터 한반도에서 나타나는 열수계는 쥐라기/전기 백악기 (약 $200{\sim}130$ Ma) 심부지질환경과 관련된 조산대형 열수계와 후기 백악기/제3기 (약 $110{\sim}45$ Ma) 천부지질환경의 후조산대형 열수계로 구분된다. 이러한 열수계에 수반된 금속광화작용은 시 공간적 관점에서 조산대형 및 후조산대형 화성활동의 특성을 반영하고 있다. 그리고 각 유형 광화유체의 ${\delta}^{18}O_{H2O}$는 쥐라기 조산대형 광상에 비하여 후기 백악기 후조산대형 광상에서 현저한 조성변화를 보이고 있다. 즉, 조산대형 광상은 경기 영남 육괴에 배태되며, 심부 지질조건에서 균질한 $^{18}O$-부화된 고온성 광화유체로부터 진화된 열수충진형 금광상과 희유금속 광상으로 인접한 대보화강암체 또는 분화된 페그마타이트로부터 유입된 마그마수 또는 일부 변성수로부터 유도되었다. 반면에 후기 백악기 광상은 태백산분지, 옥천 지향사대 및 경상분지의 전 지역에 걸쳐 광범위하게 산출되며, 철합금, 비철금속 및 귀금속 광상의 열수충진형, 열수교대형, 각력 파이프형, 반암형, 스카른형 광상과 같은 다양한 광상유형으로 배태되고 있다. 이러한 다양한 유형의 광화유체는 물-암석 반응에 따라 산소 동위원소비$({\delta}^{18}O)$가 폭 넓게 변화하는 산소 편이의 전형적인 특징을 보이는 반면 수소 동위원소비$({\delta}D_{H2O})$는 비교적 균질한 조성특징을 나타내고 있다. 또한 근지성 유형 광상의 산소 동위원소비는 부화된 경향을 보이지만, 점이성/원지성 유형 광상에서는 전반적으로 폭 넓게 변화하며 부분적으로 결핍된 특징을 보이고 있다. 즉 근지성 유형의 Cu(-Au)또는 Fe-Mo-W 광상에서는 탈가스화작용 이후에 나타나는 마그마수의 전형적인 특징을 보이는 반면, 다금속 광상과 귀금속 광상은 점이성 또는 원지성 유형으로 지표수(또는 순환수)의 혼입이 우세한 경향을 보인다.