• 한국IT서비스학회지
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• 제12권4호
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• pp.255-265
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• 2013

This paper proposes a DEA-AR model for the efficiency evaluation of the iron ore brands in an integrated steel mill. The input factor is defined as unit cost of each brand based on CIF and two output factors are chosen as Fe and Al which are the important ingredients of iron ore. The relative importance between two output factors is determined by several experts using AHP model. The efficiency of each brand is determined using DEA and DEA-AR models. The negative correlation between the DEA-AR efficiency and the unit cost (CIF) is shown as significant whereas no significant correlation exist between the efficiency and the output factors. Also, the Kruskal Wallis rank sum test shows that there exist efficiency differences among the iron ore types whereas no difference is shown among the countries. The result could be utilized in selecting good brands of iron ores based on the DEA-AR efficiency in an integrated steel mill.

• 한국연소학회:학술대회논문집
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• 한국연소학회 2004년도 제28회 KOSCO SYMPOSIUM 논문집
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• pp.141-148
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• 2004

Coal combustion in an iron ore sintering bed is a key parameter that determines quality of the sintered ores and productivity of the process. In this study, effects of the different types of coal coke and anthracite - on the combustion in the iron ore sintering bed are investigated by modeling and experiment. Fuel characteristics of coke and anthracite are observed through a few basic analysis and thermo-gravimetric analysis. It was found that coke has a higher reactivity than anthracite due to the difference of surface area and density. Those characteristics are reflected to the 1-D unsteady simulation of the iron ore sintering bed. Calculation results show that different reactivity of the fuel can affect the bed combustion, which implies the further investigation should be performed for obtaining optimal combustion conditions in the sintering bed.

• 한국연소학회지
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• 제9권2호
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• pp.30-37
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• 2004

Coal combustion in an iron ore sintering bed is a key parameter that determines quality of the sintered ores and productivity of the process. In this study, effects of the different types of coal - coke and anthracite - on the combustion in the iron ore sintering bed are investigated by modeling and experiment. Fuel characteristics of coke and anthracite are observed through a set of basic analysis and thermo-gravimetric analysis. Coke has a higher reactivity than anthracite due to the difference of surface area and density, and these characteristics are reflected in the 1-D unsteady simulation of the iron ore sintering bed. Calculation results show that different reactivity of the fuel can affect the bed combustion.

• 한국지구과학회지
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• 제23권1호
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• pp.97-104
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• 2002

Mulgeum, Yangseong, Maeri and Kimhae iron ore deposits in Gyeongnam Province are hydrothermal skarn type magnetite ore deposits in propylitized andesitic rock near the contact with Cretaceous Masanite. Symmetrical zoned skarns are commonly developed around the magnetite veins. The skarn zones away from the vein are quartz-garnet skarn, epidote skarn and epidote-orthoclase skarn. Oxygen isotope analyses of coexisting minerals from andesitic rock, Masanite and major skarn zones, and of magnetite, hematite and quartz were conducted to provide the information on the formation temperature, the origin and the evolution of the hydrothermal solution forming the iron ore deposits. Becoming more distant from the ore vein, temperatures of skarn zones represent the decreasing tendency, but most ${\delta}^{18}O$ and ${\delta}^{18}O_{H2O}$ values of skarn minerals represent no variation trend, and also the values are relatively low. Judging from all the isotopic data from the ore deposits, the major source of hydrothermal solution altering the skarn zones and precipitating the ore bodies was magmatic water derived from the deep seated Masanite. This high temperature hydrothermal solution rising through the fissures of propylitized andesitic rock was mixed with some meteoric water, and occurred the extensive isotopic exchange with the propylitized andesitic rock, and formed the skarns. During these processes, the temperature and ${\delta}^{18}O_{H2O}$ value of hydrothermal solution were lowered gradually. At the main stage of iron ore precipitation, because all the alteration was already finished, the new rising hydrothermal solution formed only the magnetite ore without oxygen isotopic exchange with the wall rock.

• 한국연소학회:학술대회논문집
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• 한국연소학회 2006년도 제32회 KOSCO SYMPOSIUM 논문집
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• pp.181-188
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• 2006

Operation parameters for large scale industrial facility such as iron making plant are carefully selected through elaborate tests and monitoring rather than through a mathematical modeling. One of the recent progresses for better energy utilization in iron ore sintering process is the distribution pattern of fuel inside a macro particle which is formed with fines of iron ore, coke and limestone. Results of model tests which have been used as a basis for the improved operation in the field are introduced and a theoretical modeling study is presented to supplement the experiment-based approach with fundamental arguments of physical modeling, which enables predictive computation beyond the limited region of tests and adjustment. A single fuel particle model along with one-dimensional bed combustion model of solid particles are utilized, and thermal processes of combustion and heat transfer are found to be dominant consideration in the discussions of productivity and energy utilization in the sintering process.

• 한국연소학회:학술대회논문집
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• 한국연소학회 2012년도 제44회 KOSCO SYMPOSIUM 초록집
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• pp.21-24
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• 2012

In the iron ore sinter process, temperature distribution pattern in sintering bed is related with productivity and quality of sintered ore. Evenly heat distribution make the uniform quality of sintered ore but in normal operating condition, upper part of bed has lack of heat and scarce quality of sintered ore, thus yeild rate is decreased and productivity is diminished. Therefore, using the additional fuel in the upper part of bed is considered and effect of fuel is discussed. (max. 80 words).

• 자원리싸이클링
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• 제23권4호
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• pp.12-20
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• 2014

본 연구에서는 자원고갈에 따른 철광석의 자원화 가능성에 대한 연구를 수행하였다. 이를 위하여 Fe함량이 각각 64%(A광석)와 57%(B광석)인 Fe품위를 갖는 2종의 철광석 시료를 대상으로, 광석의 파쇄거동 특성 및 조직학적 측면에서 비교분석을 통하여 광종별 품위향상 가능성을 알아보고자 하였다. SEM 분석결과, 철광석 A의 경우 철산화물과 맥석이 분리된 형태로 분포되어 있으며, B광석의 경우는 철산화물과 맥석이 혼재되어 분포되어 있었다. 이는 B광석에 비해 A광석이 분쇄에 의한 단체분리가 보다 용이함을 의미한다. 따라서 A광석은 적절한 입도로 분쇄 후 자력선별 등에 의한 품위 향상이 가능할 것으로 판단된다. 반면 B광석은 단체분리를 위하여 A광석보다 미립으로 분쇄하여야 할 것으로 판단되나, 열처리 전 62 ~ 68% Fe조성이 열처리 후 약 81%로 증가하는 경향을 보여, 열처리를 적용한 품위 향상이 가능할 것으로 사료된다.

• 자원환경지질
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• 제27권6호
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• pp.523-535
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• 1994

충주 광산은 한반도의 대표적인 층상 규제형 (strata-bound type) 철광상의 하나이다. 광산 부근의 지질은 규암 및 편암류로 구성되는 변성 퇴적암 (계명산층)과 후기의 관입 화성암으로 이루어져 있다. 철광층은 주로 변성암의 편리와 조화적 관계를 가지며 층상 또는 렌즈상으로 산출되고 부분적으로 불규칙한 괴상으로 발달되기도 한다. 광상은 산출상태, 구조 및 조직, 구성 광물의 공생특성 등에 의해 호상광석과 괴상광석으로 구분된다. 호상광석 (banded ore)은 적철석, 적철석+자철석, 자철석 및 석영이 우세한 분대 (meso- bands)의 반복에 의한 대상구조가 특정적이다. 괴상광석 (massive ore)은 화강암질 암석의 접촉부를 따라 불규칙한 형태로 산출되며, 대부분이 자철석으로 구성된다. 철산화광물 및 규산염 광물의 입자 크기는 호상광석에서 보다 괴상광석에서 더 조립질을 나타낸다. 호상 및 괴상광석을 구성하는 자철석의 조성은 거의 순수한 $Fe_3O_4$로 구성되지만, Mn의 함량에서 차이가 있음을 알 수 있다 (호상광석; 0.14~0.27 MnO wt.%, 괴상광석; 0.10~0.15 MnO wt.%). 적철석은 Ti 성분이 호상 (0.87~1.27 $TiO_2$ wt.%) 및 괴상 (3.51~6.96 $TiO_2$ wt.%) 광석에서 뚜렷한 차이를 보인다. 광석에 수반되는 흑운모의 화학조성은 호상광석이 괴상광석에서보다 FeO, $TiO_2$ 및 $Al_2O_3$ 값은 낮고, MgO와 $SiO_2$는 높다. 충주 철광상은 퇴적작용 내지 변성작용의 특성을 나타내는 대상 (층상)구조와 괴상조직 및 교대조직등의 다양한 변화과정을 반영하고 있으며, 산출상태, 광석광물의 조성 및 조직적 특성은 괴상광석 형성이 호상 광석보다 더 환원적인 환경 또는 고온의 온도 조건에서 야기되었음을 지시한다. 철광상은 초기 철의 퇴적(공급)작용과 후기의 변성작용에 의해 2차 부화작용에 의해 복합적으로 형성된 것으로 추정된다. 호상광석은 광역변성작용에 의해, 괴상광석은 화강암 관업에 의한 영향으로 사료된다.

• 산업기술연구
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• 제27권A호
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• pp.31-38
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• 2007

Recently produced concrete has a tendency to overcome environmental defects. Porous and planting Eco-concrete requires the neutralization process and enough void in concrete to contain water, to pass air freely, and provides necessary nutrients to vegetation roots. The biological environment in concrete is not suitable for planting because the concrete possesses strong alkali constituent of pH 11-13. This study evaluated the strength and serviceability of concrete as well as the chemical characteristics of concrete mixed by low-grade iron ore left in the abandoned mine and treated by Ammonium monohydrogen phosphate, $(NH_4)_2HPO_4$. Test variables include two kinds of coarse aggregates such as crushed stones and low-grade iron ore, the duration time and the period for neutralization treatment by Ammonium monohydrogen phosphate, $(NH_4)_2HPO_4$, and the proportion ratio of cement, blast furnace slag and silica fume.

• 자원환경지질
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• 제33권1호
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• pp.1-18
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• 2000

Lens shaped and stratiform titanomagnetite orebodies in the Boreumdo iron mine are closely associated with amphibolite which intruded into Precambrian metasediments. Mineralogical and petrochemical analyses of amphilbolite and titanomagnetite ores were carried out in order to interpret the origin of amphilbolite and the genesis of titanomagnetite ore deposits. Amphibolites belong to orthoamphilbolite interms of Niggli value and mineralogy, and are characterized by the occurrence of relict olivine. The amphilbolites responsible for titanomagnetite mineralization have extremely high content of $TiO_2$, ranging from 2.12 to 4.59 wt.% with the average value of 3.43 wt.%. Amphibole minerals in amphibolites are consist mainly of calcic amphiboles such as hornblende, ferroan pargasitic hornblende and tremolite. Most plagioclases belong to andesine ($An_{30-50}$\ulcorner). The metamorphic temperature and geobarometric pressure which are calculated by the calcic amphibole-plagioclase geothermometer and calcic amphilbole geobarometer are estimated to be 537$^{\circ}C$~579$^{\circ}C$(avg. 555$^{\circ}C$) and 2.9~6.6 kbar (avg. 4.5 kbars), respectively. It shows a typical amphibolite facies. Based on the mineral chemistry and petrochemisty of amphibolites and iron ores which are composed mainly of titanomagnetite and ilmenite in the Boreumdo iron mine, the titaniferous oxide melts could be immiscibly separatd from the titaniferous ultrabasic magma. The genesis of the Boreumdo titanomagnetite ore deposits are analogous to the Soyeonpyeongdo and Yonchon iron ore deposits in terms of their mineralogy, mineral chemistry and geologic setting.