• Proceedings of the Korean Society of Dyers and Finishers Conference
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• 2012.03a
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• pp.58-58
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• 2012

산소와 아연의 화합물인 산화아연은 UVA, UVB 산란효과가 있는 논케미컬 자외선 차단 성분으로 물, 알코올에는 녹지 않지만 산, 알칼리, 암모니아수 등에는 녹는다. 자외선을 방지하며 입자경은 500nm전후이다. 굴절률은1.9~2.0으로 내광성, 내건성, 내열성이 커서 햇빛이나 다른 자극으로 보호막을 형성하며 수렴, 방부, 항균작용을 한다. 이러한 특징을 띄는 금속산화물 산화아연을 내광성이 약한 p-aramid섬유에 코팅해 내광성 증진을 나타내려한다. 이에 따라 본 실험에서는 암모니아수와 Zinc acetate로부터 sol-gel 합성법에 따른 ZnO 합성 실험을 수행하였다. 반응물 농도에 따른 ZnO 입자의 형상과 입자 분포를 통해 결정크기를 알아보았다. 결과 분석을 위하여 X-ray 회절분석(XRD)를 이용해 ZnO입자의 결정성을 분석하였고, 패턴의 형상과 결정크기를 전계방출형 투과전자현미경(FE-TEM)을 통해 관찰하였다.

• Transactions of the Korean hydrogen and new energy society
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• v.5 no.1
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• pp.19-24
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• 1994

표면상태가 $LaNi_{4.7}Al_{0.3}$의 활성화에 미치는 영향을 조사하기 위해서 여러가지 산화 상태에서의 incubation time을 관찰하였다. Incubation time은 입자의 크기, 파쇄후 경과시간, 합금방법에 따라 다르게 나타났다. 재료를 파쇄한후 실험한 날짜에 따라 incubation time은 초기에는 증가하다가 최대점을 지난후 감소하고 다시 최소점을 보인후 증가하는 현상을 보였다. 이것은 Ni cluster와 산화층의 복합적인 작용인 것으로 생각된다. Ni cluster의 양과 산화층의 두께는 공기에 노출되는 시간이 증가함에 따라 증가하였다.

• Journal of the Korean Institute of Telematics and Electronics
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• v.18 no.1
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• pp.7-19
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• 1981

Anodization method is utilized in order to measure diffusion profiles of boron and arsenic in silicon. The solution used for silicon anodization is Ethylene glycol +KNO3(0.04N), The thickness of silicon which is consumed by a single 200V anodization is 460$\pm$40A regardless of wafer type. The profiles of boron and arsenic in silicon after predeposition process are investigated. The diffusion coefficients of both dopants depending on impurity concentration are extrated from these profiles. The base pull-in effect has been observed in prototype npn transistors with arsenic doped emitter.

• Journal of the Korean Chemical Society
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• v.52 no.1
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• pp.23-29
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• 2008

Simple Keggin type tungsten and molybdenum heteropoly acids, H3PW12O40 and H3PMo12O40, were usedas water-tolerant catalysts for the oxidation of alcohols with 34% hydrogen peroxide in normal drinking water. Accordingto our findings, H3PW12O40 may be used as a simple, effective, and cheap catalyst for this type of transformation in nor-mal drinking water with excelent yields. Efects of diferent solvents at 25-80oC and changing concentration of catalystand substrate on the reaction progress were also studied.

• Proceedings of the Korean Vacuum Society Conference
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• 2011.08a
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• pp.382-382
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• 2011

이차원 결정인 그래핀(graphene)은 전하도핑(charge doping)과 기계적 변형에 민감하기 때문에 기판의 물리 및 화학적 구조 및 특성에 따라 그래핀의 물성이 크게 영향을 받는다고 알려져 있다. 특히 널리 사용되고 있는 산화실리콘($SiO_2$/Si) 기판에 존재하는 나노미터 크기의 굴곡과 전하 트랩(charge trap)은 전하 이동도 및 화학적 안정성 등의 면에서 그래핀 고유의 뛰어난 물성을 제한하는 것으로 알려져 있다. 본 연구에서는 비정질 산화실리콘 기판을 대조군으로 삼아 편평도가 높은 결정성 h-BN (hexagonal boron nitride) 기판이 그래핀에 미치는 영향을 관찰하였다. 화학기상증착법(chemical vapor deposition 또는 CVD)으로 성장시킨 그래핀을 각 기판에 전사시킨 후 라만 분광법을 통해 전하 도핑 및 기계적 변형 정도를 측정하였다. h-BN 위에서는 외부 환경에서 기인하는 전하 도핑 정도가 산화실리콘 기판보다 적게 관찰되었다. 또한 h-BN 위에 고착된 그래핀 시료에서는 기판-그래핀 상호작용에서 기인하는 것으로 보이는 새로운 라만 분광 특성이 관찰되었다.

• Economic and Environmental Geology
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• v.39 no.6 s.181
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• pp.653-662
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• 2006

Quartz veins from the Jukwangri area of Hwawon-myeon are epithermal quartz veins that are filling the NW or NE-trending faults within Precambrian metasedimentary rocks. Based on their prolongation and ore grades, No. 1 quartz vein can be traced for about 200 m and varies 0.1 to 3 m in thickness. Mineralization of No. 1 quartz vein can be divided into hypogene and supergene stages. Hypogene stage is associated with hydrothermal alteration minerals(phyllic and argillic zones) such as illite, sericite and sulfides such as pyrite, arsenopyrite, sphalerite. chalcopyrite, galena, argentian tetrahedrite. Supergene stage is composed of Fe-Mn oxide, Zn-Fe oxide and Pb oxide. Fluid inclusion data indicate that homogenization temperature and salinity of hypogene stage range from 187 to $306^{\circ}C$ and ken 0.0 to 6.2 wt.% eq. NaCl, respectively. They suggest that ore forming fluids were progressively cooled and diluted from mixing with meteoric water. Oxygen($-4.1{\sim}4.1%o$) and hydrogen($-107{\sim}-88%o$) isotope com-positions indicated that hydrothermal fluids were derived from meteoric and evolved by progressive mixing with meteoric water during mineralization.

• Journal of the Korean earth science society
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• v.27 no.5
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• pp.548-556
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• 2006

The purpose of this study is to clarify the relict landform development of fluvial terrace and the soil characteristics occurring on the fluvial deposits. The physico-chemical properties of soil that are developed on terrace deposits and X-ray diffraction analysis of clay were investigated specifically. The horizon of $A_1$ consists of silt loam with reddish-brown color (5YR4/3). Its soil structures is a weak, fine, subangular, and blocky, breaking to granular. The horizon of $B_{1t}\;and\;B_{2t}$ are silt clay with either a yellowish red (5YR5/6), bright red (2.5YR4/6) color. This soil structure is weak, subangular, and blocky, with thin discontinuous bright red (2.5YR4/6) clay cutans and soft manganese concretions. This red soil structure is made on heavy-textures. It is packed compactly with parent materials of high fluvial surface sediments, and usually has a $A_1-B_{1t}-B_{2t}-C$ profile, from top to bottom. In most cases, clay accumulation in the B-horizon and clay cutans on ped surfaces are observed, which means the argillic horizon has formed. The soils derived from fluvial surface deposits are associated with soils. The soils on the high fluvial surface are considered to be a kind of paleo-red soil which were developed by strong desilicification and rubefaction, and strong leaching of bases under warmer bio-climatic condition during the old Pleistocene period. According to these morphological and anlaytical characteristics,geomorphological features and bio-climatic conditions under which the soil have developed on the high terrace sediment indicate that the soil should be classified as paleo-red soils.

• Economic and Environmental Geology
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• v.39 no.5 s.180
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• pp.583-595
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• 2006

Quartz veins from the Hwawon area are an epithermal quartz vein that is filling the fault zone within Precambrian metasedimentary rocks and Jurassic granite. Mineralization can be divided into hypogene and supergene stages. Hypogene stage is associated with hydrothermal alteration minerals(propylitic and argillic zones) such as epidote, chlorite, illite, sericite and sulfides such as pyrite, sphalerite, chalcopyrite, galena, bornite, cubanite, argentian tetrahedrite, Pb-Ag-S system and Pb-Te-S system. Supergene stage is composed of Fe-Mn oxide, Zn-Fe oxide and Pb oxide. Fluid inclusion data indicate that homogenization temperatures and salinity of hypogene stage range from $291.2^{\circ}C$ to $397.3^{\circ}C$ and from 0.0 to 9.3 wt.% eq. NaCl, respectively. It suggests that ore forming fluids were cooled and diluted with the mixing of meteoric water. Oxygen($-0.7{\sim}3.5%_{\circ}$(white quartz: $-0.7{\sim}3.5%_{\circ}$, transparent quartz: $2.4%_{\circ}$)) and hydrogen($-70{\sim}55%_{\circ}$(white quartz: $-70{\sim}55%_{\circ}$, transparent quartz: $-62%_{\circ}$)) isotopic composition indicates that hydrothermal fluids were derived from magmatic and evolved by mixing with meteoric water during mineralization.

• Journal of the Korean Magnetics Society
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• v.7 no.1
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• pp.55-67
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• 1997

Double exchange interaction leads to the ferromagnetism by the direct coupling between conduction electrons and magnetic ions. The most intriguing feature of double exchange is the explicit connection of the conductivity with the magnetism, which has drawn much interest in relation to the colossal magnetoresistance (CMR) recently observed in manganese oxide compounds. In this review, we explain the basic physics of double exchange and examine the classical discussions.

• Tunnel and Underground Space
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• v.22 no.5
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• pp.321-329
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• 2012

Laboratory tests for measuring absorption, porosity, P-wave velocity and uniaxial compressive strength (UCS) were performed to examine weathering characteristics of ilmenite by microorganism. Physical property changes were quantitatively estimated with comparing culture period on the condition of abiotic oxidation without microorganism and biooxidation with microorganism. As a result, the measured pH during 45 days was distributed in the range from 3.82 to 4.26, on the other hand, biooxidation showed the range from 2.20 to 2.57. The measured absorption according to microorganism and culture period represented 0.052% at final stage in the case of abiotic oxidation and 0.073% in the case of biooxidation. Porosity showed 0.206% at final stage in the case of abiotic oxidation and 0.281% in the case of biooxidation. In general, the values by biooxidation showed higher than that by abiotic oxidation. Change range of P-wave velocity with culture period showed that the measured value as 1410 m/s at final stage in the case of biooxidation was lower than 1886 m/s of that in the case of abiotic oxidation. The UCS was decreased with increasing culture period in all specimens and represented 241.1 MPa at final stage in the case of abiotic oxidation and 140.0 MPa in the case of bioxidation. In conclusion, it implies that influence of physical property on ilmenite by biooxidation related with microorganism was larger than that by abiotic oxidation.