• 한국연소학회:학술대회논문집
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• 한국연소학회 2001년도 제23회 KOSCO SYMPOSIUM 논문집
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• pp.161-168
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• 2001

Sintering bed of iron ore in the steel making process is one of typical applications of solid fuel bed, which has relatively uniform progress of fuel and simple processes of combustion. The sintering bed was modelled as an unsteady one-dimensional progress of fuel layer containing the two phases of solid and gas. Cokes added to the raw mix of which the amount is about 3.5% of the total weight was assumed to form a single particle with other components. In the early predition results presented in this paper, the flame propagation within the bed was not sustained after the top surface of the bed was ignited with hot gas. It suggests that the model should be extended to consider the multiple solid phase, which can treat the ore particles and the coke particles separately.

• Conservation and Restoration of Cultural Heritage
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• 제1권1호
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• pp.9-22
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• 2012

The most widely excavated iron artifacts used as weapons or farm tools from central southern regions of Korea were subjects of non-metallic inclusion analysis through metallographic examination, microhardness measurement, and scanning electron microscopy with energy dispersive X-ray spectroscopy. Through metallographic interpretation and study of the analyzed results, the steel manufacturing and iron smelting using heat processing in the iron artifacts excavated from the central southern region of the ancient Korean peninsula was studied, and the analysis of the non-metallic inclusions mixed within the metallic structures was interpreted as the ternary phase diagram of the oxide to infer the type of iron ores for the iron products and the temperature of the furnace used to smelt them. Most of the ancient forged iron artifacts showed $Al_2O_3/SiO_2$ with high $SiO_2$ contents and relatively low $Al_2O_3$ contents for iron ore, indicating t hat for $Al_2O_3$ below 5%, it is presumed that magnetic iron ores were reduced to bloom iron (sponge iron) with direct-reduction process for production. The temperature for extraction of wustite for $Al_2O_3$ below 1% was found to be $1,020{\sim}1,050^{\circ}C$. Considering the oxide ternary constitutional diagram of glassy inclusions, the steel-manufacturing temperature was presumed to have been near $1,150{\sim}1,280^{\circ}C$ in most cases, and minimum melting temperature of casting iron part excavated in Daeseong-ri. Gyeonggi was near $1,400^{\circ}C$, and it is thought that hypoeutectic cast iron of about 2.3% carbon was casted and fragility of cast iron was improved by decarburizing in solid state.

• 대한기계학회논문집B
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• 제28권7호
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• pp.747-754
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• 2004

Thermo-fluid characteristics in coke oven, sintering machine and blast furnace in iron-making facility are key processes related to the quality and productivity of the pig iron. Solid material in the processes usually forms a bed in a gas flow. For simulation of the processes by mathematical model, the solid beds are idealized to be a continuum and a reacting solid flow in the gas flow. Governing equations in the form of partial differential equations for the solid material can be constructed based on this assumption. Iron ore sintering bed is simulated and limited amount of parametric study have been performed. The results have a good agreement with the experimental results or physical phenomena, which shows the validity and applicability of the model.

• 한국입자에어로졸학회지
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• 제9권4호
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• pp.221-230
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• 2013

We demonstrated the efficacy of magnetic nanoparticles (MNPs) produced from a low grade iron ore as an adsorbent for the removal of Cr(VI), a toxic heavy metal anion present in wastewater. The adsorption of Cr(VI) by these MNPs strongly depended on the dosage of MNPs, the initial concentration of the Cr(VI) solutions, and pH. The highest Cr(VI) adsorption efficiency of 22.0 mg/g was observed at pH 2.5. The adsorption data were best fit with the Langmuir isotherm and corresponded to a pseudo-second-order kinetic model. The used adsorbent was regenerated by eluting in highly alkaline solutions. Sodium bicarbonate showed the highest desorption efficiency of 83.1% among various eluents including NaOH, $Na_2HPO_4$, and $Na_2CO_3$. Due to the high adsorption capacity, the simple magnetic separation, and the high desorption efficiency, this nano-adsorbent produced from inexpensive and abundant resources may attract the attention of the industries to apply for removing various metal anionic contaminants from wastewater.

• 지구물리와물리탐사
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• 제15권4호
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• pp.177-189
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• 2012

복합 물리탐사(전기비저항, MT)와 지질(시추 자료 및 코어 물성)정보에 대해 지구통계학적 복합해석 기법을 적용하여 3차원 광체 모델링 평가를 수행하였다. 우선, 복합 물리탐사를 통해 시추공 및 그 외의 전체적인 지역에 대한 비저항대 분포를 파악할 수 있었으며, 코어 물성 시험을 통해 연구지역의 자철석(광체)이 코어 내부의 밀도가 높은 전도성 성분(Fe)에 의해 밀도의 증가에 따라 비저항이 감소하는 상관관계를 나타냄을 파악하였다. 3차원 광체 모델링을 수행하기 위해 사용된 자료는 전기비저항 탐사, MT 탐사, 물성 자료와 시추 자료 등이며, 전체 획득 자료 및 시추 자료에서 추출한 광체의 품위 자료를 이용하였다. 본 연구에서는 자료의 복합 해석을 위해 지구통계학적 기법 중에서, 부족한 실제 측정 자료의 평균 및 분산을 잘 재생시키는 실현 값을 통해 지역적으로 변화하는 불균질성을 잘 묘사하는 순차 가우시안 시뮬레이션(sequential Gaussian simulation)을 사용하였다. 획득된 전체 자료와 품위 자료만을 이용하여 도출한 시뮬레이션 결과, 광체가 기존에 연구되어 존재하는 잔광체의 일정 부분에서 유사한 분포를 나타냈으며, 추가적으로 하부 깊은 심도에 대해 광체의 분포 양상을 추정할 수 있었다.

• 자원환경지질
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• 제27권2호
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• pp.117-130
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• 1994

Titanomagnetite ore bodies in the Yonchon iron mine are closely associated with alkali gabbroic rocks of middle Proterozoic age which intruded Precambrian metasedimentary rocks. The orebodies can be divided into massive ores in gabbroic rock, skarn ores in calcareous xenoliths and banded ores in gneissic gabbro. Gabbroic rocks from the Yonchon iron mine have unusually high content of $TiO_2$ with an average values of 3.46 wt%. Iron ores are ilmenite (42.25~51.56 wt% in $TiO_2$) and titanomagnetite (1.29~6.57 wt% in $TiO_2$) and the former is dominant Small amount of magnetite, hematite, sphene and sulfide minerals are included in the ores. Grandite garnet, titanoaugite and tschermakite are in iron skarn ores. Hornblendes from ores and gabbroic rocks have a relatively homogeneous isotopic composition with ${\delta}D$ between -110.0 and -133.9‰, and ${\delta}^{18}O$ of +4.5 to +6.5‰, and calculated to have formed in fluids with ${\delta}O_{H_2O}$ of + 6.7 to +8.7‰. and ${\delta}_{H_2O}$ of -87.9 to -111.8‰, which has a similar isotopic value of primary magmatic water. Based on intrusive age, occurrence, mineral chemistry and isotopic compositions of magnetite ores and gabroic rocks, it will be concluded that the gabbroic rocks are responsible for the titanomagnetite mineralization. The titaniferous magnetite melt was immiscibly separated from the high titaniferous gabbroic melts of Proterozoic age.

• 자원환경지질
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• 제27권4호
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• pp.345-361
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• 1994

Lens shaped titanomagnetite ore bodies in the Soyeonpyeong iron mine are embedded in amphibolites, which were intruded into Precambrian metasediments such as garnet-mica schist, marble, mica schist, and quartz schist. Mineral chemistry, K-Ar dating and hydrogen and oxygen stable isotopic analysis for the amphibolites and titanomagnetite ores were conducted to interpret petrogenesis of amphibolite and ore genesis of titanomagnetite iron ore deposits. Amphibolites of igneous origin have unusually high content of $TiO_2$, ranging from 0.94 to 6.39 wt.% with an average value of 4.05 wt.%. REE patterns of the different lithology of the amphibolite show the similar trend with an enrichment of LREE. Amphiboles of amphibolites are consist mainly of calcic amphiboles such as ferro-hornblende, tschermakite, ferroan pargasite, and ferroan pargasitic hornblende. K-Ar ages of hornblende from amphibolite and gneissic amphibolite were determined as $440.04{\pm}6.39Ma$ and $351.03{\pm}5.21Ma$, respectively. This indicates two metamorphic events of Paleozoic age in the Korean peninsula which are correlated with Altin orogeny in China. The titanomagnetite mineralization seems to have occurred before Cambrian age based on occurrence of orebodies and ages of host amphibolites. The Soyeonpyeong iron ores are composed mainly of titanomagnetite, ilmenite, and secondary minerals such as ilmenite and hercynite exsolved in titanomagnetite. The temperature and the oxygen fugacity estimated by the titanomagnetite-ilmenite geothermometer are $500{\sim}600^{\circ}C$ (ave. $550^{\circ}C$) and about $2{\pm}10^{-23}bar$, respectively. Hornblendes from ores and amphibolites which responsible for magnetite ore mineralization, have a relatively homogeneous isotopic composition ranging from +0.8 to +3.9 ‰ in ${\delta}^{18}O$ and from -87.8 to -113.3 ‰ in ${\delta}D$. The calculated oxygen and hydrogen isotopic compositions of the fluids which were in equilibrium with hornblende at $550^{\circ}C$, range from 2.8 to 5.9‰ in ${\delta}^{18}O_{H2O}$ and from -60.41 to -81.31 ‰ in ${\delta}D_{H2O}$. The ${\delta}^{18}O_{H2O}$ value of magnetite ore fluids are in between +6.4 to + 7.9 ‰. All of these values fall in the range of primary magmatic water. A slight oxygen shift means that $^{18}O$-depleted meteoric water be acted with basic fluids during immiscible processes between silicate and titaniferous oxide melt. Mineral chemistry, isotopic compositions, and occurences of amphibolites and orebodies, suggest that the titanomagnetite melt be separated immisciblely from the titaniferous basic magma.

• 무역학회지
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• 제43권3호
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• pp.125-145
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• 2018

발틱해운거래소는 건화물 해상무역 지수인 BDI(Baltic Dry Index) 지수를 발표하고 있는데, BDI 지수는 철광석, 석탄, 곡물 등 주요 건화물을 운송하는 벌크선박의 평균 용선료를 의미한다. 현재 BDI 산출의 기초가 되는 용선료 데이터는 케이프사이즈 40%, 파나막스 30%, 스프라막스 30%의 비중으로 반영되고 있다. 이처럼 케이프사이즈는 건화물 시장을 구성하는 다양한 사이즈의 선박 중에서도 대장 역할을 담당하고 있다. 본 연구는 벡터오차수정모형(Vector Error Correction Model; VECM)을 활용하여 변수 간의 인과관계를 검증하였으며, 이를 통해 케이프사이즈 용선료에 영향을 미치는 변수 간의 장기균형모델을 도출하고자 하였다. 분석결과, 케이프사이즈 선복량 1% 증가시 용선료 0.08% 감소, 엔달러 환율 1% 증가시 0.01% 감소, 세계 GDP 1% 증가시 0.02% 증가, 철광석과 석탄 물동량 1% 증가시 각각 0.11%, 0.09% 증가, 벙커유 가격 1% 증가시 0.04% 증가하는 실증분석 결과를 계측하였다. 벌크선 중 핸디막스, 파나막스급 활용도가 낮아지고 상대적으로 케이프사이즈의 활용도가 높아지고 있는데 본 연구는 케이프사이즈를 대상으로 하여 분석을 수행하였다는 점에서 의의가 있다.

• 보존과학회지
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• 제29권2호
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• pp.139-147
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• 2013

충주 수룡이 원모롱이 야철지에서 수습한 슬래그와 노벽을 분석하여 제철관련 정보를 알아보고자 하였다. 슬래그의 전철량은 36.98~44.47wt%이며 이는 고대 제철조업에서 나타나는 일반적인 철 회수율이다. 슬래그에 포함된 CaO는 노벽에 포함된 0.36wt%보다 많으므로 조재제로서 제련 시 의도적으로 첨가한 것으로 추정된다. 노벽의 경우 $Al_2O_3$의 함량이 낮아 고알루미나질의 내화점토를 사용하지 않은 것으로 획인되었다. 슬래그의 미세조직과 주성분 분석을 통해 Fayalite와 Wustite가 나타난 No.1~3 슬래그는 철광석으로 제련한 것으로 보인다. 그러나 No. 4 슬래그의 경우 $TiO_2$을 함유한 Ulvospinel이 나타나 사철을 이용하여 제련했을 가능성이 높다. 그러므로 이 지역에서는 제철 원료로서 철광석과 함께 사철도 이용하였을 가능성이 있으며 노벽은 $Al_2O_3$의 함량이 낮은 일반점토를 사용하여 제작한 것으로 보인다.

• 자원환경지질
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• 제2권1호
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• pp.13-33
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• 1969

The Mulkum mine, located in Mulkum-myon, Yangsan-Kun, Kyeongsang Province, is one of the biggest iron mine in Korea. The geology of this mine and its vicinity consists of Chusan andesitic rocks and Datae-dong andesite porphyry of the Kyeongsang System which were intruded by biotite granite widely distributed near the vicinity of Mulkum-ni. The ore deposits, embedded in Dotae-dong andesite porphyry, are fissure-filling vein type in origin. Up to present ore bodies of Main vein, No. 2 vein, Eastern No. 1, 2 vein and Western No. 1 vein are exploited. Generally the veins strike N 10-25 E and dip to 60-90 SE. The proved length of vein is more than 500 meters and its depth 150 meters in Main vein with 3-4 meters of thickness in average. Ore minerals are mainly magnetite and locally associated with small amounts of hematite, sphecularite and chalcopyrite. Gangue minerals are quartz, epidote, chlorite, pyroxene, and garnet, etc. The modes of occurrence of vein are as follow; 1. Branching and parallel vein patterns are observed around main shaft in -1 level. 2. Multiple cymoid loops and subrectangular vein patterns are observed around main shaft in -2 level. 2. Single vein patterns are observed in -3 and -5 level. The ore-shoots plunge northeasterly about 20-30 degrees. In conclusion, the tectonically fractured zone belongs to the poorly mineralized zone and shoots are formed as single vein type. The general trends of one-shoots must be applied the prospecting of the deep-seated ore body in the deposits.