• 한국광물학회지
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• 제31권1호
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• pp.23-32
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• 2018

뇌록은 조선시대 건축물의 바탕칠(가칠)에 사용된 녹색 안료이며, 불국사 대웅전 등 주요 건축물의 단청에 사용되었다. 본 연구에서는 한국 전통 안료 원료인 뇌록을 이용하여 소성온도에 따른 광물학적 특성 변화를 살펴보았다. 포항 뇌성산 일대에 국부적으로 산출하고 있는 뇌록은 주구성 광물이 셀라도나이트(celadonite)이며, 주요 구성 원소는 Fe, Si, K, Mg 등으로 주로 Fe가 풍부한 운모류임을 알 수 있다. $105^{\circ}C{\sim}1000^{\circ}C$까지 단계적 소성실험 결과, 색상이 녹색 ${\rightarrow}$ 담녹색 ${\rightarrow}$ 갈색 ${\rightarrow}$ 적색으로 변하였으며, 열분석에서는 $616^{\circ}C$ 부근에서 결정수의 탈수작용에 의한 흡열반응이 확인되었다. 광물의 변화는 $600^{\circ}C$ 이상에서 결정면[($11{\bar{1}}$), ($02{\bar{1}}$)]이 붕괴되고, $1000^{\circ}C$ 이상에서 철산화물이 형성되었다. 따라서 뇌록의 정출 온도가 $600^{\circ}C$ 이하인 것으로 추정되며, 셀라도나이트만이 확인되는 것으로 보아 Stage I 단계만의 변질을 겪은 것으로 판단된다.

• 한국산학기술학회논문지
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• 제9권2호
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• pp.500-507
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• 2008

파우더류 화장품의 제조 시 사용되어지는 분쇄기 중 스크린밀, 핀밀, 제트밀을 이용하여, 대표적인 화장품용 안료(탈크, 마이카, 나이론파우더, 실리카, 이산화티탄)를 분쇄하여 각 안료들의 분쇄 특징과 분쇄기의 특성에 대한 연구를 수행하였다. 또한 분쇄평가를 위해 산화철을 흔적물질로써 사용하여 실험하여 CIE LAB의 변화로써 평가하였다. 스크린밀과 핀밀의 분쇄는 박편상 분체에서는 종횡단면의 분쇄 중 종단분쇄가 더 많이 발생하고 제트밀에서는 종횡 단면의 분쇄가 모두 발생하는 것으로 사료되고 구상파우더인 나이론파우더와 실리카의 경우, 1차 입자화 혹은, 역으로 정전기적 인력에 의한 약한 응집이 나타나지만, 제트밀에서는 분쇄압력 2bar의 조건 이상에서는 나이론파우더의 합일 혹은 변형이 발생하고, 실리카는 심한 파쇄가 발생하였고, 이산화티탄은 모든 분쇄기에서 1차입자화가 되었다. 분쇄에 따른 산화철의 색상변화는 핀밀이 가장 우수한 결과를 보였다. 이들 결과로부터 실질적인 제품 제조 공정에서는 박편상 및 침상 원료의 사전처리 이용에는 제트밀을 이용하고, 색상 발현을 위한 분쇄, 즉 조색은 스크린밀과 핀밀을 이용하는 것이 좋을 것으로 판단된다. 또한 산업적인 공정조건을 고려하면, 스크린밀은 4회 분쇄 시, 핀밀은 2회 분쇄 시, 제트밀은 1bar의 분쇄압력 조건 하에서 전반적인 분쇄효율이 우수한 것으로 사료된다.

• 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.

• 대한미생물학회지
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• 제11권1호
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• pp.69-78
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• 1976

There have been increasing reports of mycobacterioses in man and animals caused by "atypical" or "opportunist" mycobacteria. At the presnt, "opportunist mycobacterioses" are not generally responsive to antituberculosis drugs, and therefore, create considerable problems with regard to chemotherapy and control measures. In recent years studies have been made to isolate opportunist mycobacteria from soil, house-dusts and tap-water. It seemed quite interesting to define the extent of circumstantial presence of "opportunist" mycobacteria and nocardia in the soils of school-ground of primary schools and middle-high schools. This communication is the results of pilot study to isolate and identify "opportunist" mycobacteria and nocardia from 504 soil specimens of 72 schools in Seoul City. 1. Of a total of 59 isolates from 504 soil specimens tested, 32 strains were identified as opportunist mycobacteria and 27 strains as nocardia. 2. Isolation rates of opportunist mycobacteria by the areas(of specimen collection) were as follows: 36.4% in the southern area of Han-River, 33.3% in the central area, 22.7% in the outskirt area and 16.6% in the intermediate area. There observed no apparent difference in the isolation rates both-between the areas and between primary schools and middle-high schools. However, a significant difference was noted in the isolation rates between the places of soil sampling in a given school(P<0.05), i.e., the highest was the soil of refuge heaps(15.2%), and tap-water pole area(11.1%), the school-lavatory entrance(9.7%), the school gate entrance(5.5%), and iron-bar play ground(2.7%). The soil specimens from the center of school ground and from school building entrance yielded none of mycobacterial isolates. 3. Isolation rates of nocardia by the areas were as follows: 33.3% in the central area, 31.8% in the outskirt area, 27.3% in the southern ares of Han-River and 11.1% in the intermediate area. As in the case of mycobacteral isolates, there observed no apparent differences in the isolation rates both between the areas and between primary schools and middle-high schools, but a significant difference was noted between the places of soil sampling(P<0.05), i.e., the highest was the soil of school building entrance(15.2%), and of school gate entrance(6.9%), refuge heaps(5.5,%), iron-bar play ground(4.1%), the school-lavatory entrance(2.7%) and tap-water pole area(2.7%), respectively. The soil specimens from the center of, school ground yielded none of nocardia isolates. 4. Of the 32 strains of isolated mycobacteria. 15 strains were slow-growing mycobacteria and the remaining 17 strains belonged to the rapid growers. Of the 15 slow-growers. 4 strains were M. scrofulaceum-szulgai complex, 3 M. gordonae, 4 M. terrae-triviale complex, 2 M. avium-intracellulare-xenopi complex, and 2 unclassified schotochromogens. Of the 17 strains of rapid growers, 12 were M. diernhoferi, 2 M. fortuitum-peregrinum complex, 2 M. vaccae and one M. flavescens. 5. Of the 27 strains of nocardia isolated, 11 strains were N. transvalensis, 5 N. convoluta, 5 N. erythropolis, one N. vaccinii, one N. polychromogens-paraffinae complex and 4 untypable strains of orange-pigmented nocardia spp.

• Geomechanics and Engineering
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• 제36권1호
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• pp.51-69
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• 2024

Currently, composite lining mountain tunnels in China are generally classified based on the [BQ] method for the surrounding rock grade. Increasingly, tunnel field construction is replicated indoors for scale down model tests. However, the development of analogous materials for model tests of composite lining tunnels with different surrounding rock grades is still unclear. In this study, typical Class III and V surrounding rock analogous materials and corresponding composite lining support materials were developed. The whole processes of excavation-support dynamics of the mountain tunnels were simulated. Data on the variation of deformations, contact pressures and strains on the surrounding rock were obtained. Finally, a comparative analysis between model tests and numerical simulations was performed to verify the rationality of analogous material development. The following useful conclusions were obtained by analyzing the data from the tests. The main analogous materials of Class III surrounding rock are barite powder, high-strength gypsum and quartz sand with fly ash, quartz sand, anhydrous ethanol and rosin for Class V surrounding rock. Analogous materials for rockbolts, steel arches are replaced by aluminum bar and iron bar respectively with both shotcrete and secondary lining corresponding to gypsum and water. In addition, load release rate of Class V surrounding rock should be less than Class III surrounding rock. The fenestration level had large influence on the load sharing ratio of the secondary lining, with a difference of more than 30%, while the influence of the support time was smaller. The Sharing ratios of secondary lining in Class III surrounding rock do not exceed 12%, while those of Class V surrounding rock exceed 40%. The overall difference between the results of model tests and numerical simulations is small, which verifies the feasibility of similar material development in this study.

• 한국주조공학회지
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• 제36권6호
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• pp.202-207
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• 2016

The effects of Fe and Si additions on the microstructures and mechanical properties of aluminum bronze have been investigated. In a bar-type specimen cast in a die mold, the addition of Fe promoted the dendritic solidification of the ${\alpha}$ phase. The hardness values increased slightly in the Fe-added specimen with heat treatment, while these values was increased significantly in the specimens with Si or with combined additions of Fe and Si. When a centrifugal casting bush with combined addition of Fe and Si was heat treated, the FeSi compound within the matrix was finely dispersed, and was observed to be the origin of cup-cone type conical dimple failure in the tensile fracture surface. The mechanical properties of the heat treated centrifugal casting bushes, whose nominal alloy compositions were (Cu-7.0Al-0.8Fe-3.0Si)wt%, exhibited tensile strength of $703-781N/mm^2$, elongation of 6.6-11.7% and hardness of Hv 222.6-249.2. These high values of strength and elongation were attributed to the strengthening of the matrix due to the combined addition of Fe and Si, and to precipitation of fine the FeSi compound.

• 자원환경지질
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• 제28권2호
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• pp.109-121
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• 1995

인도네시아 빠찌딴 광화대 동-아연 광상은 금 또는 연 광화작용을 수반하여 동부자바 Southern Mountain zone내 제3기 퇴적암류와 화산암류의 열극을 충진한 열수 석영 백상광체로 까시한(Kasihan), 점퐁(Jompong), 금뽈(Gempol) 지역에 밀집 분포한다. 주 광화시기의 광석광물로는 황철석, 황동석, 섬아연석, 방연석 등이 각 지역별로 특징적인 광석광물들과 공생관계로 보이며 산출한다. 즉 까시한 지역의 경우 초기 공생광물군으로써 황철석 자류철석 철함유량이 높은(약 20 mole % FeS) 섬아연석과 Au 함량이 매우높은 (91.4 to 94.0 atomic % Au) 에렉트럼 및 (Cu-)Pb-Bi계 유염광물 등이 산출하며, 점퐁지역은 황철석, 유비철석(29.5~30.3 atomic % As), 섬아연석 등이 공생관계를 보여주며 산출된다. 반면, 금뽈지역의 경우 황철석, 자철석, 적철석 등의 초기 산출이 특징적이다. 광석광물의 침전은 0.8~10.1 wt. % NaCl 상당염농도를 갖는 광화유체로부터 약 $350^{\circ}C$에서 약 $200^{\circ}C$에 걸쳐 진행되었으며, 까시한 및 점퐁지역의 경우 초기 광화유체의 비등현상과 이에 수반된 냉각 회석 작용에 기인한 광액 진화에 의하여, 금뽈지역의 경우 천수의 유입에 의한 냉각 희석작용이 우세하게 진행된 광액 진화에 기인하여 야기되었다. 광화유체의 비등현상 및 유체포유물 연구결과에 근거한 빠찌딴 광화대 주 광화시기의 압력조건은 약 (${\geq}95{\sim}255$ bars로, 까시한($\approx$ 140~255 bar) $\rightarrow$ 점퐁 ($\approx$ 120~170 bar) $\approx$ 금뽈 (${\geq}95$ bar)의 순으로 광화대내 지역별 상대적인 광화심도 차이가 확인된다. 광물공생관계를 이용한 열역학적 연구결과, 온도감소에 따른 유황분압의 변화와 산소분압 조건이 각 지역별로 상이함은 광화대내 각 지역별 열수계에서 상기 광화심도에 관련한 천수의 역할(water/rock 비등)차이에 기인된 결과로 해석된다. 유체내 산소 및 수소안정동위원소 연구결과, 이들 동위원소 값이 광화작용의 진행과 함께 점차 감소함은 상대적으로 낮은 water/rock 비 값은 갖는 환경하에서 동위원소 교환반응을 이뤄 평형상태에 이른 광화초기 열수계내에 광화작용의 진행과 함께 산화상태의 차갑고 동위원소적 교환반응이 적게 이뤄진 천수의 혼입이 점증하였음을 지시하며, 각 지역별 동위원소비 값의 차이는 광화심도에 관련된 water/rock비 및 동위원소 교환반응차 등에 의한 결과로 사료된다.

• Smart Structures and Systems
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• 제12권1호
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• pp.1-22
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• 2013

Magnetic nanoparticle based bioseparation in microfluidics is a multiphysics phenomenon that involves interplay of various parameters. The ability to understand the dynamics of these parameters is a prerequisite for designing and developing more efficient magnetic cell/bio-particle separation systems. Therefore, in this work proof-of-concept experiments are combined with advanced numerical simulation to design and optimize the capturing process of magnetic nanoparticles responsible for efficient microfluidic bioseparation. A low cost generic microfluidic platform was developed using a novel micromolding method that can be done without a clean room techniques and at much lower cost and time. Parametric analysis using both experiments and theoretical predictions were performed. It was found that flow rate and magnetic field strength greatly influence the transport of magnetic nanoparticles in the microchannel and control the capturing efficiency. The results from mathematical model agree very well with experiments. The model further demonstrated that a 12% increase in capturing efficiency can be achieved by introducing of iron-grooved bar in the microfluidic setup that resulted in increase in magnetic field gradient. The numerical simulations were helpful in testing and optimizing key design parameters. Overall, this work demonstrated that a simple low cost experimental proof-of-concept setup can be synchronized with advanced numerical simulation not only to enhance the functional performance of magneto-fluidic capturing systems but also to efficiently design and develop microfluidic bioseparation systems for biomedical applications.

• 한국정밀공학회지
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• 제13권1호
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• pp.53-61
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• 1996

A clear understanding of the surface formation mechanism due to cutting is very important to help produce a good quality surface. Much of the roughness along the length of a bar being cut in a lathe can be explained in terms of macroscopic tool shape and feed rate. However, the roughness along the direction of cutting requires a different explanation. The formation of surface roughness is a problem in flow and fracture of materials in the vicinity of the tool edge. On a microscopic scale the cutting edge is rounded because it is impossible to grind a perfectly sharp cutting edge. Even if a perfectly sharp cutting edge were obtained it would soon become dull as a result of rapid breakdown and wear of the cutting edge. A research project is proposed in which in the main object is to model the surface formation mechanism due to cutting. The tool was assumed to be dull, that is, its edge has a finite radius. In order to study the effect of the radius of cutting edge on the surface formation, tools having different cutting edges were used. For orthogonal cutting experiment, cast iron and glass were chosen as brittle materials. Plowing forces acting in the cutting edge were estimated and its effect on the surface roughness was studied by observing the machined surface using optical microscope.

• Macromolecular Research
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• 제13권6호
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• pp.521-528
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• 2005

Electrospun polyacrylonitrile (PAN) nanofibers were carbonized with or without iron (III) acetylacetonate to induce catalytic graphitization within the range of 900-1,500$^{circ}C$, resulting in ultrafine carbon fibers with a diameter of about 90-300 nm. Their structural properties and morphologies were investigated. The carbon nanofibers (CNF) prepared without a catalyst showed amorphous structures and very low surface areas of 22-31 $m^{2}$/g. The carbonization in the presence of the catalyst produced graphite nanofibers (GNF). The hydrogen storage capacities of these CNF and GNF materials were evaluated through the gravimetric method using magnetic suspension balance (MSB) at room temperature and 100 bar. The CNFs showed hydrogen storage capacities which increased in the range of 0.16-0.50 wt$\%$ with increasing carbonization temperature. The hydrogen storage capacities of the GNFs with low surface areas of 60-253 $m^{2}$/g were 0.14-1.01 wt$\%$. Micropore and mesopore, as calculated using the nitrogen gas adsorption-desorption isotherms, were not the effective pore for hydrogen storage.