• 자원리싸이클링
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• 제21권4호
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• pp.35-43
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• 2012

본 연구는 날로 그 발생량이 증가하고 있는 산성광산배수의 처리과정에서 발생하는 슬러지를 재활용하기 위하여 수행되었으며, 슬러지의 주성분인 수산화철[$Fe(OH)_3$]이 중금속에 대한 흡착 능력이 우수한 점을 이용하여 슬러지를 광해방지용 중금속흡착제의 제조 원료로 활용하기 위한 연구를 수행하였다. 먼저 슬러지의 물성파악을 위하여 슬러지의 화학조성, 광물조성, 입도, 형상 등을 조사하였고 슬러지 첨가량, 시간, pH, 중금속 농도, 소결온도에 따른 중금속 종별 흡착능을 조사 검토하였다.

• 자원환경지질
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• 제33권2호
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• pp.147-163
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• 2000

The Buseok pluton in the Yeongju Batholith is a comagmatic plutonic rocks which haveconcentrically compositional zoning. The lithofacies of the Buseok pluton comprise hornblende biotite tonalite in the southern part of the pluton, porphyritic and equigranular biotite granodiorite in the northern part and biotite granite in the north-central part. The compositional variations change gradually with continuity both within and between the lithofacies. The concentrically zoned pattern is relatively mafic rocks composed of high-temperature mineral assemblages in margin of the southern part, passing inward and northward gradually to more felsic rock in core of the north-central part. Changes in the textures and microstructures, as well as in the mineral content, take place between rock types of the plutons. Darker colored, generally coarse-grained, well foliated tonalite pass inward to light colored, coarse-grained, poorly foliated granodiorite, and finally give way to lighter colored, medium-grained, nearly nonfoliated granite. The foliation are best developed in the marginal part of the tonalite. Here, the regional myolitic foliation in the tonalite is steep northward and parallels to its southeastern contact with the country rock, but the magmatic foliation from disc-shaped mafic microgranitoid enclaves is subvertical and parallels the contacts with the country rock. As the tonalite approaches biotite granite in composition, the foliation is indistinct. Modal and chemical data for the pluton show quantitative compositional variation from the margin of the southern part to the core of the north-central part. Quartz and K-feldspar increase toward the core of the pluton, whereas hornblende, biotite and color index decrease. /Abundances of $SiO_2$and $K_2O$$_2$O increase toward the core according to the variation in quartz and K-feldspar, whereas those of MnO, CaO, $TiO_2$, $Fe_2O_3$, MgO and $P_2O_5$ decrease corresponding to the variation in mafic and accessaries. The compositional zonation resulted from fractional crystallization involving downward settling of earlier crystals, accompanied by upward movement of melt and volatiles, and followed by accessary marginal accretion of crystalline material in the magma to the marginal part. Although a little crustal contamination by the wall rock is recognized from the isotope data, the contamination is not only dominated over but also appropriate for forming the compositional variation in the pluton.

• 자원환경지질
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• 제23권1호
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• pp.35-57
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• 1990

This study has been carried out on the Pegmatites, Naedeogri Granites, Nonggeori Granites and Metasedimentary rocks in the middle area of Taebaeksan region to investigate the geochemical properties and possibility of productivity. Pegmatites are characterized by metamorphosed anatectic pegmatite and differentiated magmatic pegmatite, and are mixed type of rare-element pegmatite and mica-bearing pegmatite by the classification of Ginsburg(1979). The petrological type of the igneous rocks is thought to be calcalkali, subalkaline and peralumious. According to chemical variations against D. I., differentiation trends from Naedeogri and Nonggeori Granites through non-mineralized pegmatites to mineralized pegmatites are supposed. From the relationship between oxided and $SiO_2$, pegmatites and Nonggeori Granite have shown similar tendencies and bulk composition of pegmatites and similar to metasedimentary rocks near the intrusives. By judging the correlations of trace elements, it is elucidated that pegmatites adjacent to Naedeogri and Nonggeori Granites have been originated in magma differentiation from these granites and the others have been differentiated by remelting or partial melting from metasedimentary rocks. $Sp_5$, $Sp_8$, and $Sp_9$ pegmatites are considered as productive rocks, and $Sp_4$, $Sp_6$, $Sp_7$, $Sp_{10}$, $Sp_{11}$, and $Sp_{12}$ pegmatites and granites are supposed to have a weak productivity, in terms of element ratios related with Sn mineralizations. Tourmalines in productive pegmatites are formed under the circumstance of Li-poor granitoids and associated with pegmatites, and the others are seemed to be originated in metapelites and metapsammites which are not coexisting with an Al-saturating phase. Three types of chemical zoning are noticed in tourmalines: (1) apparently homogeneous compositional patterns, (2) a continuous core-to-rim zoning and, (3) a discontinuous core-to-rim zoning. From results of EPMA of tourmalines, Al, Mg and Ca increase closer to rim, while Fe decreases.

• 한국세라믹학회지
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• 제52권1호
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• pp.33-40
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• 2015

Onggi, described as a 'breathing' type of pottery' has significantly influenced the traditional food culture of Korea. It is known that Onggi is an optimal type of storage for fermented foods such as soy sauce, salted seafood, and Kimchi, as air or liquid can penetrate through the body of this material. These foods gain flavor due to the breeding of aerobic bacteria at the beginning of the fermentation process. In this study, Onggi materials from five regions, Gangjin, Yeoju, Ulsan, Yesan, and Jeju, were collected and analyzed to determine their chemical and physical properties before and after sintering. The differences in the raw materials of other mining regions are examined in terms of their chemical and mineralogical compositions, specific surface area, particle size, and particle distribution. Among them, the Gangjin raw material has the greatest mean particle size of $92.29{\mu}m$, as well as the widest particle size distribution. Differences in the levels of $SiO_2$ and $Fe_2O_3$ are shown among Onggi raw materials. However, the crystalline phases formed after sintering are identical, except for the Jeju samples. At all sintering temperatures tested here, Gangjin Onggi showed the greatest porosity, leading to complete air permeation through the body within 90 minutes. These results taken together indicate that air permeation is strongly related to the pore structures in the Onggi body. This is assumed to affect the fermentation behavior.

• 자원환경지질
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• 제12권2호
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• pp.79-93
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• 1979

한반도 내에 부존되고 있는 중적광상들은 세 주요한 Metallousenetic Epoch (Pre-Cambrian E., Jurassic-early Cretaceous E., 및 late Cretaceous-early Tertiary E.)에 생성되었고 성인으로 열수작용과 접촉교대작용에 기인된다고 보고되었다. 이중 12개 광상(달성, 산내, 일광, 상동, 대화, 월악, 복수, 옥방, 쌍전, 홍성, 삼봉, 청양)을 본 연구의 대상으로 택하고 각 지역에서 채취한 표품중 모두 25개 시료에 대하여 지화학적 실험을 수행하였다. 즉 각 분쇄된 시료 (-80+120mesh)는 super panner, 중액, isodynamic separator, UV lamp를 이용한 물리적인 처리과정을 거쳐 최종으로 입체현미경 하에서 단체분리된 후 Jarrell-Ash 1.5m Grating Spectrometer를 이용하여 본 연구대상 시료로 개발한 Spectrochemical method (Carrier: NaCl, Internal standard: $La_2O_3$)로 정량 분석되었다. 본 연구에서 밝혀낸 국내 회중석 광내에 함유되는 희유 윈소의 종류는 모두 Al, Bi, Fe, Si, Mn, Pb, Mg, Sn, Mo, Cu, Sr, Cr, Y, Ag, Ti, Ni, As, Yb의 18개 원소이며, 이들은 각각의 절대적 및 상대적인 함량과 각 광화작용의 시기, 광상의 성인, 모암, 각 원소의 mobility 그리고 회중석광의 형광색 및 육안색과 비교 검토되었다. 본 연구의 결과로 회중석광이 정출되는 과정에서 유사한 지질환경의 물리화학적인 여건이 이루어지면 그 내에 함유되는 몇 성분원소들의 화학적인 특성은 매우 유사성을 보여주는 typochemical habit를 가짐을 알 수 있었다. 본 연구에서 밝혀진 한국산 회중석 광내의 희유성분(稀有成分)으로서 Y, Mn, Sr 원소들의 Geochemical mobility의 특성(特性)은 앞으로 회중석광의 심도탐광을 위하여 고려되어야하고, 더욱 연구개발되어야 할 것이다. 또한 상기 회중석 광내의 물리적 및 화학적으로 결합되어 있는 불순물의 희유성분들은 선광 제련 파정에서 금속성분의 추출농집공정(工程)에 유용한 자료가 될 것이다.

• Journal of Korean Society for Atmospheric Environment
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• 제18권E4호
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• pp.203-213
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• 2002

Receptor modeling is one of statistical methods to achieve reasonable air pollution strategies. In order to maintain and manage ambient air quality, it is necessary to identify sources and to apportion its sources for ambient particulate matters. The main purpose of the study was to survey seasonal trends of inorganic elements in the coarse and fine particles. Second, this study has attempted emission sources qualitatively by a receptor method, the PMF mo-del. After that. both PMF (positive matrix factorization) model and TTFA (target transformation factor analysis) model were applied to compare and to estimate mass contribution of coarse and fine particle sources at the receptor. A total of 138 sets of samples was collected from 1989 to 1996 by a low volume cascade impactor with 9 size fraction stages at Kyung Hee University in Korea. Sixteen chemical species (Si, Ca, Fe, K, Pb, Na, Zn, Mg, Ba, Ni, V, Mn, Cr, Br, Cu. Co) were characterized by XRF. The study result showed that the weighted arithmetic mean of coarse and fine particles were 51.3 and 54.4 $\mu\textrm{g}$/㎥, respectively. Contribution of both particle fractions were esti-mated using TTFA and PMF models. The number of estimated sources was seven according to TTFA model and 8 according to PMF model. Comparison of TTFA and PMF revealed that both methodologies exhibited similar trends in their contribution pattern. However, large differences between contributions were observed in some sour-ces. The results of this study may help to suggest control strategies in local countries where known source profiles do not exist.

• 한국진공학회:학술대회논문집
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• 한국진공학회 2011년도 제41회 하계 정기 학술대회 초록집
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• pp.260-260
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• 2011

투명 비정질 산화물반도체는 디스플레이의 구동소자인 박막 트랜지스터에 채널층으로 사용된다. 또한 투명하면서 유연성이 있는 소자를 저비용으로 제작할 수 있는 장점을 가진다. 투명 산화물반도체 재료 중 IGZO는 Si 또는 GaAs와 같은 공유결합성 반도체와는 다른 전자 배치로 전도대가 금속이온의 ns 궤도에서 형성되며, 가전도대가 산소 음이온의 2p 궤도에서 형성된다. 특히 큰 반경의 금속 양이온은 인접한 양이온과 궤도 겹침이 크게 발생하게 되며 캐리어의 효과적인 이동 경로를 제공해줌으로써 다른 비정질 반도체와는 다르게 높은 전하이동도(~10 $cm^2$/Vs)를 가진다. 따라서 저온공정에서 우수한 성능의 TFT소자를 제작할 수 있는 장점이 있다. 본 연구에서는 TFT 채널층으로 사용하기 위한 a-IGZO박막의 산소분압에 따른 특성변화를 분석 하였다. a-IGZO박막은 Pulsed Laser Deposition (PLD)를 이용하여 산소분압(20~200 mTorr) 변화에 따라 Glass기판에 증착하였다. 증착된 a-IGZO 박막의 구조적 특성으로는 X-ray diffraction (XRD), Field emission scanning electron microscopy (FE-SEM), 광학적 특성은 UV-vis spectroscopy 분석을 통해서 알아보았다. TFT 채널층의 조건으로는 낮은 off-current, 높은 on-off ratio를 위해 고저항 ($10^3\;{\Omega}cm$)의 진성반도체 성질과 source/drain금속과의 낮은 접촉저항(ohmic contact) 등의 전기적 성질이 필요하다. 따라서 이러한 전기적 특성확인을 위해 transmission line method (TLM)을 사용하여 접촉저항과 비저항을 측정하였고, 채널층으로 적합한 분압조건을 확인해볼 수 있었다.

• Transactions on Electrical and Electronic Materials
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• 제10권1호
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• pp.24-27
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• 2009

N-doped ZnO thin films were deposited on n-type Si(100) and homo-buffer layer, and undoped ZnO thin film was also deposited on homo-buffer layer by RF magnetron sputtering method. After deposition, all films were in-situ annealed at $800^{\circ}C$ for 5 minutes in ambient of $O_2$ with pressure of 10Torr. X -ray diffraction shows that the homo-buffer layer is beneficial to the crystalline of N-doped ZnO thin films and all films have preferable c-axis orientation. Atomic force microscopy shows that undoped ZnO thin film grown on homo-buffer layer has an evident improvement of smoothness compared with N-dope ZnO thin films. Hall-effect measurements show that all ZnO films annealed at $800^{\circ}C$ possess p-type conductivities. The undoped ZnO film has the highest carrier concentration of $1.145{\times}10^{17}cm{-3}$. The photoluminescence spectra show the emissions related to FE, DAP and many defects such as $V_{Zn}$, $Zn_O$, $O_i$ and $O_{Zn}$. The p-type defects ($O_i$, $V_{Zn}$, and $O_{Zn}$) are dominant. The undoped ZnO thin film has a better p-type conductivity compared with N-doped ZnO thin film.

• 한국신뢰성학회지:신뢰성응용연구
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• 제15권3호
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• pp.197-206
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• 2015

Failure analysis of pre-insulated pipe (SPPS 380, 400A) transporting high temperature water ($95{\sim}110^{\circ}C$) for a plant was carried out. The damaged area (${\Phi}5mm$) of pre-insulated pipe was found only on welds. The chemical composition of damaged pipe meets specification of carbon steel pipes for pressure service (KS D 3562). As results of microstructure analysis, crack propagated from outer to inside after pitting corrosion occurred on the outside surface. The non-metallic inclusion existed on the end of crack. And the non-metallic inclusion continuously and linearly formed along with the bond line of welds. Based on SEM-EDS analysis, the nonmetallic inclusions have higher Manganese (Mn) and Oxygen (O) content but sulfur (S) was not detected. As results of water quality analysis, hydrogen ion concentration and minerals like Fe, Mg, Si were in low level. But the content of dissolved oxygen (11.2 ppm) was slightly higher than that of standard. It seems that the cause of damaged pipe is grooving corrosion due to MnO inclusion formed on bond line and corrosion took place nearby welds.

• Corrosion Science and Technology
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• 제17권4호
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• pp.154-165
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• 2018

During the process of sulfur dioxide removal, flue gas desulfurization equipment provides a serious internal corrosion environment in creating sulfuric acid dew point corrosion. Therefore, the utilities must use the excellent corrosion resistance of steel desulfurization facilities in the atmosphere. Until now, the trend in developing anti-sulfuric acid steels was essentially the addition of Cu, in order to improve the corrosion resistance. The experimental alloy used in this study is Fe-0.03C-1.0Mn-0.3Si-0.15Ni-0.31Cu alloys to which Ru, Zn and Ta were added. In order to investigate the effect of $H_2SO_4$ concentration and the alloying elements, chemical and electrochemical corrosion tests were performed. In a low concentration of $H_2SO_4$ solution, the major factor affecting the corrosion rate of low alloy steels was the exchange current density for $H^+/H_2$ reaction, while in a high concentration of $H_2SO_4$ solution, the major factors were the thin and dense passive film and resulting passivation behavior. The alloying elements reducing the exchange current density in low concentration of $H_2SO_4$, and the alloying elements decreasing the passive current density in high concentration of $H_2SO_4$, together play an important role in determining the corrosion rate of Cu-bearing low alloy steels in a wide range of $H_2SO_4$ solution.