• Journal of Ceramic Processing Research
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• 제13권spc2호
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• pp.394-397
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• 2012

In this work, we studied the influence of the dopant elements concentration on the properties of SnO2 thin films deposited by pulsed laser deposition. X-ray diffraction (XRD), field emission scanning electron microscopy (FE-SEM), Hall effect measurement and UV-Vis studies were performed to characterize the deposited films. XRD results showed that the films had polycrystalline nature with tetragonal rutile structure. FE-SEM micrographs revealed that the as deposited films composed of dense microstructures with uniform grain size distribution. All the films show n-type conduction and the best transparent conductive oxide (TCO) performance was obtained on 6 wt% Sb2O5 doped SnO2 film prepared at pO2 of 60mtorr and Ts of 500 ℃. Its resitivity, optical transmittance, figure of merit are 7.8 × 10-4 Ω cm, 85% and 1.2 × 10-2 Ω-1, respectively.

• 자원환경지질
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• 제39권6호
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• pp.675-687
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• 2006

이 연구에서는 청풍지역 하상퇴적물에 대한 지구화학적 특성 규명을 통해, 주성분원소 및 미량원소에 대한 청풍지역의 자연배경치를 제시하고, 지구화학적 재해에 대해 예견하고자 한다. 이를 위해 물이 흐르고 있는 1차 수계를 대상으로 하상퇴적물시료를 채취하였고, 실험실에서 자연건조 시켰으며, 화학적 분석을 위해 알루미나 몰타르를 이용하여 200메쉬 이하로 분쇄하였다. 주성분원소 및 미량성분원소는 XRD, XRF, ICP-AES, NAA를 이용하여 분석하였다. 청풍지역 하상퇴적물의 기반암에 따른 지질집단별 지구화학적 특성 비교를 위해, 화강암질편마암지역, 메타텍틱편마암지역, 다도응회암지역, 유치역암 지역, 능주용암지역으로 분류하였다. 청풍지역 하상퇴적물 전체에 대한 주성분원소 함량은 $SiO_2\;47.31{\sim}72.81\;wt.%,\;Al_2O_3 \;11.26{\sim}21.88\;wt.%,\;Fe_2O_3\;2.83{\sim}8.39\;wt.%,\;CaO\;0.34{\sim}7.54\;wt.%,\;MgO\; 0.55{\sim}3.59\;wt.%,\;K_2O\;1.71{\sim}4.31\;wt.%,\;Na_2O\;0.56{\sim}2.28\;wt.%,\;TiO_2\;0.46{\sim}1.24\;wt.%,\;MnO\;0.04{\sim}0.27\;wt.%,\;P_2O_5\;0.02{\sim}0.45\;wt.%$이다. 청풍지역 하상퇴적물 전체에 대한 미량성분원소 및 희토류원소 함량은 $Ba\;700ppm{\sim}8990ppm,\;Be\;1.0{\sim}3.50ppm,\;Cu\;6.20{\sim}60ppm,\;Nb\;12{\sim}28ppm,\;Ni\;4.4{\sim}61ppm,\;Pb\;13{\sim}34ppm,\;Sr\;65{\sim}787ppm,\;V\;4{\sim}98ppm,\;Zr\;32{\sim}164ppm,\;Li\;21{\sim}827ppm,\;Co\;3.68{\sim}65ppm,\;Cr\;16.7{\sim}409ppm,\;Cs\;72{\sim}37.1ppm,\;Hf\;4.99{\sim}49.2ppm,\;Rb\;71.9{\sim}649ppm,\;Sb\;0.16{\sim}5.03ppm,\;Sc\;4.97{\sim}5ppm,\;Zn\;26.3{\sim}375ppm,\;Ce\;60.6{\sim}373ppm,\;Eu\;0.82{\sim}6ppm,\;Yb\;0.71{\sim}10ppm$의 범위를 보였다.

• 한국지구과학회지
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• 제27권1호
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• pp.49-60
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• 2006

본 연구는 나주지역 하상퇴적물에 대한 지구화학적 특성 연구이다. 이를 위해 1차 수계를 대상으로 139개의 하상퇴적물 시료를 채취하였다. 채취된 시료는 실험실에서 자연 건조시켰으며, XRF, ICP-AES, NAA를 이용하여 화학분석을 실시하였다. 기반암에 따른 지구화학적 특성을 알아보기 위하여, 화강암질편마암 지역, 편암류 지역, 화강암류 지역, 사질암 지역, 응회암 지역, 안산암 지역, 유문암 지역으로 분류하였다. 나주지역 하상퇴적물의 지질집단별 주성분원소 평균함량은 $SiO_2\;58.37{\sim}66.06wt.%,\;Al_2O_3\;13.98{\sim}18.41wt.%,\;Fe_2O_3\;4.09{\sim}6.10wt.%,\;CaO\;0.54{\sim}1.33wt.%,\;MgO\;0.86{\sim}1.34wt.%,\;K_2O\;2.38{\sim}4.01wt.%,\;Na_2O\;0.90{\sim}1.32wt.%,\;TiO_2\;0.82{\sim}1.03wt.%,\;MnO\;0.09{\sim}0.15wt.%,\;P_2O_5\;0.11{\sim}0.18wt.%$이다. 주성분원소의 평균함량 비교에서 $Al_2O_3$와 $K_2O$는 화강암질편마암 지역에서, $Fe_2O_3,\;CaO,\;P_2O_5$는 응회암 지역에서, MgO와 $TiO_2$는 안산암 지역에서, $Na_2O$는 유문암 지역에서 높고, $SiO_2$와 MnO 함량은 사질암 지역에서 약간 높다. 미량성분 및 희토류원소의 지질집단별 평균함량은 $Ba\;1278{\sim}1469ppm,\;Be\;1.1{\sim}1.5ppm,\;Cu\;18{\sim}25ppm,\;Nb\;25{\sim}37ppm,\;Ni\;16{\sim}25ppm,\;Pb\;21{\sim}28ppm,\;Sr\;83{\sim}155ppm,\;V\;64{\sim}98ppm,\;Zr\;83{\sim}146ppm,\;Li\;32{\sim}45ppm,\;Co\;7.2{\sim}12.7ppm,\;Cr\;37{\sim}76ppm,\;Cs\;4.8{\sim}9.1ppm,\;Hf\;7.5{\sim}25ppm,\;Rb\;88{\sim}178ppm,\;Sc\;7.7{\sim}12.6ppm,\;Zn\;83{\sim}143ppm,\;Pa\;11.3{\sim}37ppm,\;Ce\;69{\sim}206ppm,\;Eu\;1.1{\sim}1.5ppm,\;Yb\;1.8{\sim}4.4ppm$이다. Pb, Li, Cs, Hf, Rb, Sb, Pa, Ce, Eu, Yb 평균함량은 화강암질편마암 지역에서, Ba, Co, Cr 평균함량은 편암류 지역에서, Nb, Ni, Zr 평균함량은 사질암 지역에서, Sr 평균함량은 응회암 지역에서 높고, Be, Cu, V, Sc, Zn 평균함량은 안산암 지역에서 다른 지질집단에서 보다 높다.

• 자원환경지질
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• 제31권4호
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• pp.297-310
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• 1998

Geochemical characteristics of environmental toxic elements at the Narim mine area were investigated on the basis of major, minor, rare earth element geochemistry and mineralogy. Ratios of $Al_2O_3/Na_2O$ and $K_2O/Na_2O$ in soils and sediments range from 11.57 to 22.21 and from 1.86 to 3.93, and are partly negative and positive correlation against $SiO_2/Al_2O_3$ (3.41 to 4.78), respectively. These suggested that sediment source of host granitic gneiss could be due to rocks of high grade metamorphism originated by sedimentary rocks. Characteristics of some trace and rare earth elements of V/Ni (0.33 to 1.95), Ni/Co (2.00 to 6.50), Zr/Hf (11.27 to 53.10), La/Ce (0.44 to 0.55), Th/Yb (4.07 to 7.14), La/Th (2.35 to 3.93), $La_N/Yb_N$ (6.58 to 13.67), Co/Th (0.63 to 2.68), La/Sc (3.29 to 5.94) and Sc/Th (0.49 to 1.00) are revealed a narrow range and homogeneous compositions may be explained by simple source lithology. Major elements in all samples are enriched $Al_2O_3$, MgO, $TiO_2$ and LOI, especially $Fe_2O_3$ (mean=7.36 wt.%) in sediments than the composition of host granitic gneiss. The average enrichment indices of major and rare earth elements from the mining drainage are 2.05 and 2.91 of the sediments and are 2.02 and 2.60 of the soils, normalizing by composition of host granitic gneiss, respectively. Average composition (ppm) of minor and/or environmental toxic elements in sediments and soils are Ag=14 and 1, As=199 and 14, Cd=22 and 1, Cu=215 and 42, Pb=1770 and 65, Sb=18 and 3, Zn=3333 and 170, respectively, and extremely high concentrations are found in the subsurface sediments near the ore dump. Environmental toxic elements were strongly enriched in all samples, especially As, Cd, Cu, Pb, Sb and Zn. The level of enrichment was very severe in mining drainage sediments, while it was not so great in the soils. Based on the EPA value, enrichment index of toxic elements is 8.63 of mining drainage sediments and 0.54 of soils on the mining drainage. Mineral composition of soils and sediments near the mining area were partly variable being composed of quartz, mica, feldspar, amphibole, chlorite and clay minerals. From the gravity separated mineralogy, soils and sediments are composed of some pyrite, arsenopyrite, chalcopyrite, sphalerite, galena, goethite and various hydroxide minerals.

• 한국전기전자재료학회논문지
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• 제13권4호
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• pp.286-293
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• 2000

In this paper we investigated the structural dielectric and piezoelectric properties of 0.03Pb(Sb$\_$1/2//Nb$\_$1/2/)-0.97Pb(Zr$\_$0.495//Ti$\_$0.505/)O$_3$+0.5 wt% excess PbO + wt% MnO(X=0, 0.1, 0.3, 0.5, 0.7) ceramics to develop the high-power piezoelectric transformer. The piezoelectric transformers with dimension of 27.5$\times$27.5$\times$2.5［mm$^3$］were fabricated and their electrical properties were measured. Maxima of piezoelectric properties such as electro-mechanical coupling factor of 0.534 and mechanical quality factor of 1487 were obtained for the PSN-PZT with 0.3wt% MnO. voltage step-up ratios of piezoelectric transformers at 500［Ω］and no load were 0.78, 12.82, respectively. The maximum efficiency of piezoelectric transformer was 98.6% at 800［Ω］. While the 14W fluorescent lamp were driven by the piezoelectric transformer for more than 20［min］, increment of temperature in the piezoelectric transformer was 7［$\^{C}$］.

• 대한소아치과학회지
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• 제38권1호
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• pp.33-41
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• 2011

본 연구의 목적은 상업용으로 시판되고 있는 수종의 치과용 접착제를 세대별로 분류하여 서로 다른 광원에 노출 시켜 중합하고 접착면의 전단 강도 측정을 통해 결합강도를 비교함으로써 간접적으로 광원에 따른 접착제의 중합 양상을 알아보고 소아치과 영역에서 가장 권장할만한 치과용 접착제와 광원 종류의 조합을 알아보고자 함이다. 본 연구에서는 최근에 개발된 치과용접착제를 대상으로 다른 유형의 광원으로 중합하였을 때 영구치 상아질에 대한 결합력 비교 평가하여 임상에서 상아질결합제와 광중합 시스템의 적절한 조합을 선택하는데 도움을 주고자 시행하였으며, 실험재료로 Adper Scotchbond Multi-purpose Plus Adhesive (SM; 3M ESPE, USA), Adper Single bond 2 (SB; 3M ESPE, USA), Clearfil SE Bond (SE; Kuraray Medical Inc., Japan), Adper Prompt L-Pop (PL; 3M ESPE, USA), GBond (GB; GC Cooperation Toyko, Japan)을 이용하여 Elipar Free light 2(LED; 3M ESPE, USA), OptiLux 501 (Halogen, Kerr, USA), Flipo (PAC, LOKKI, FRA) 세 가지의 광원으로 중합하고 전단결합강도를 평가한 뒤 다음과 같은 결과를 얻었다. 1. Freelight 2로 중합하였을 때 전단결합강도는 SM이 가장 높았으며($28.22{\pm}5.56$), SB($21.68{\pm}7.44$), SE($20.13{\pm}9.88$), PL($14.18{\pm}5.88$), GB($14.30{\pm}6.81$) 순이었다. SM은 PL, GB와 유의한 차이가 있었으나 (p<0.05), SB, SE, PL, GB 간에는 차이가 없었다. 2. Optiux 501로 중합하였을 때 전단결합강도는 SM이 가장 높았으며 ($22.06{\pm}7.95$), PL($12.94{\pm}4.96$), SB($12.80{\pm}3.35$), SE($12.43{\pm}4.79$), GB($10.00{\pm}3.47$) 순이었고, SM만 유의한 차이가 있었으나 (p<0.05), 다른 군 간에는 차이가 없었다. 3. Flipo로 중합하였을 때 전단결합강도는 SM이 가장 높았으며 ($26.82{\pm}11.16$), PL($15.42{\pm}9.35$), SB($10.96{\pm}3.74$), SE($9.39{\pm}3.74$), GB($7.85{\pm}2.22$) 순이었다. SM은 SB, SE, GB 군과 유의한 차이가 있었으나 (p<0.05), 다른 군 간에는 차이가 없었다. 4. 광원에 따른 차이는 SB와 GB에서만 유의성이 있었고, 다른 결합제에서는 유의한 차이가 없었다. 광원에 따른 유의성을 나타낸 결합제 중 SB는 Freelight 2가 다른 광원에 비해 유의한 차이를 보였고 OptiLux 501과 Flipo간의 차이가 없었던 반면, GB는 Freelight 2와 Flipo 간에만 유의한 차이를 나타냈다.

• 자원환경지질
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• 제29권4호
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• pp.411-419
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• 1996

The Janggun magnetite deposits occur as the lens-shaped magnesian skarn, magnetite and base-metal sulfide orebodies developed in the Cambrian Janggun Limestone Formation. The K-Ar age of alteration sericite indicates that the mineralization took place during late Cretaceous age (107 to 70 Ma). The ore deposition is divided into two stages as a early skarn and late hydrothermal stage. Mineralogy of skara stage (107 Ma) consists of iron oxide, base-metal sulfides, Mg-Fe carbonates and some Mg- and Ca-skarn minerals, and those of the hydrothermal stage (70 Ma) is deposited base-metal sulfides, some Sb- and Sn-sulfosalts, and native bismuth. Based on mineral assemblages, chemical compositions and thermodynamic considerations, the formation temperature, $-logfs_2$, $-logfo_2$ and pH of ore fluids progressively decreased and/or increased with time from skarn stage (433 to $345^{\circ}C$, 8.8 to 9.9 atm, 29.4 to 31.6 atm, and 6.1 to 7.2) to hydrothermal stage (245 to $315^{\circ}C$, 11.2 to 12.3 atm, 33.6 to 35.4 atm, and 7.3 to 7.8). The ${\delta}^{34}S$ values of sulfides have a wide range between 3.2 to 11.6‰. The calculated ${\delta}^{34}S_{H_2S}$ values of ore fluids are relatively homo-geneous as 2.9 to 5.4‰ (skam stage) and 8.7 to 13.5‰ (hydrothermal stage), which are a deep-seated igneous source of sulfur indicates progressive increasing due to the mixing of oxidized sedimentary sulfur with increasing paragenetic time. The ${\delta}^{13}C$ values of carbonates in ores range from -4.6 to -2.5‰. Oxygen and hydrogen isotope data revealed that the ${\delta}^{38}O_{H_2O}$ and ${\delta}D$ values of ore fluids decreased gradually with time from 14.7 to 1.8‰ and -85 to -73‰ (skarn stage), and from 11.1 to -0.2‰ and -87 to -80‰ (hydrothermal stage), respectively. This indicates that magmatic water was dominant during the early skarn mineralization but was progressively replaced by meteoric water during the later hydrothermal replacement.