• 제목/요약/키워드: metallic deposit

검색결과 49건 처리시간 0.03초

아연도금층의 조직, 외관, 및 경도에 미치는 미량 금속첨가의 영향 (The Effect of Trace Metallic Additives on Microstructure, Surface Appearance and Hardness of Zn Electrodeposits)

  • 예길촌;김대영;안덕수
    • 한국표면공학회지
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    • 제37권1호
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    • pp.28-39
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    • 2004
  • The effect of trace metallic additives on microstructure, surface appearance and hardness of zinc electrodeposits was investigated by using sulfate bath and flow cell system. The preferred orientation of Zn deposit with Fe additive was (103)(104)+(002) mixed texture and that of Zn deposits with both Fe-Ni and Fe-Co additives was (10 1), while Zn deposits with Fe-Cr additives had (002) preferred orientation. The surface morphology of the zinc deposits was closely related to the preferred orientation of the deposits. The glossiness of Zn deposit with Fe-Ni additives was higher than that of pure Zn deposit, while the glossiness of Zn deposits with both Fe-Co and Fe-Cr additives was lower than that of pure Zn deposit. The hardness of Zn deposits with both Fe-Ni and Fe-Co additives was noticeably higher than that of Zn-Fe deposit, while that of Zn deposit with Fe-Cr additives was similar to that of Zn-Fe deposit.

MINERALOGICAL, FLUID INCLUSION AND ISOTOPE STUDIES AT THE CINEAM EPITHERMAL GOLD DEPOSIT WEST- JAVA(Review on epithermal gold deposit in Java)

  • Widi, Bambang-Nugroho;Sunuhadi, Dwi-Nugroho;Bambang-Setiawan
    • 대한자원환경지질학회:학술대회논문집
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    • 대한자원환경지질학회 2003년도 춘계 학술발표회 논문집
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    • pp.19-19
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    • 2003
  • Cineam gold deposit is one of an epithermal gold deposit of Low Sulfidation type, which is located in the Sunda-Banda magmatic Arc Zone. Its existence in this region has led to a new concept or few point on the Sunda - Banda Magmatic Arc. Even the deposit is classified as a small scale in mine, however, mineralogically, fluid inclusion and isotopes studies are very interesting to be studied. (omitted)

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BIW 전착도장에서의 컴퓨터 시뮬레이션 적용사례 (Introduction of Computer Simulation for BIW Electrocoating Process)

  • 손대홍;정희진;안승호;김병수;김정연;최병삼
    • Corrosion Science and Technology
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    • 제15권2호
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    • pp.78-83
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    • 2016
  • The e-coating to inhibit induced corrosion can deposit a coating not only on the exterior surface but also on the inside of whole metallic components of body-in-white (BIW). But it is difficult to deposit paint films on the inside area because metallic components are multi layered. It may cause shortness of e-coating thickness. The only way to properly verify e-coating thickness is by performing the use of tear-down prototypes. When paint films' thickness is inadequate, a structural modification on each metallic component is needed. Verification of the thickness improvement for a structural modification requires much manual effort and leads to increasing development time. Recently, the simulation technology has been developed to predict the e-coating thickness in e-coating field. By applying the simulation to BIW, improvement in paint thickness quality and shortening of development period are expected. The paper explains a validated solution that allows simulating the effect of design changes to the e-coating thickness and current density, thereby delivering results within a time frame of a few days.

레이저 증착법을 이용한 금속기판상 고온초전도 박막증착 및 특성분석 (Fabrication and Characterization of High Temperature Superconducting Thin Film on Metallic Substrate Using Laser Ablation)

  • 이상렬
    • 대한전기학회:학술대회논문집
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    • 대한전기학회 1995년도 추계학술대회 논문집 학회본부
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    • pp.329-331
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    • 1995
  • Laser ablation was used to fabricate superconducting $YBa_2Cu_3O_{7-x}$ (YBCO) thin films on metallic substrates with an YSZ buffer layer. An ArF excimer laser with an wavelength of 193 nm was used to deposit both YSZ buffer layer and superconducting thin film. The characterizations of thin films were performed and compared. With a 200 nm YSZ buffer layer, c-axis orientation and $T_c$=85 K were obtained for a 200 nm-thick YBCO film.

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전남(全南) 옥매산광상(玉埋山鑛床)의 열수변질작용(熱水變質作用) 및 광석광물(鑛石鑛物)에 대한 광물학적(鑛物學的) 연구 (Hydrothermal Alteration and Mineralogy of Alunite and Kaolinite in the Ogmae Deposit, Southwest Jeonnam)

  • 김영희;문희수;김종환;유장한;김인준
    • 자원환경지질
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    • 제23권3호
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    • pp.287-308
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    • 1990
  • The Ogmae alunite-kaolinite deposit occurs in acidic tuff, the Hwangsan Tuff, of upper Crataceous age in the Haenam volcanic field, SW Jeonnam. This deposit characterized by advanced argillic alteration formed $71.8{\pm}2.8{\sim}73.9{\pm}2.8$ Ma ago in very shallow depth environment with acid-sulfate solution. Wallrock alteration can be classified into four zones from the center to the margin of the deposit: alunite, kaolinite, illite, and silicified zone. The mineral assemblage in the alunite zone, ore zone, is alunite-quartz-pyritekaolinite. Consideration of stability relation of these minerals suggests that the maximum alteration temperature is estimated at about $250^{\circ}C$ with solution pH of 3 or below assuming that pressure does not exceed 0.3 Kb. Alunite occurs as two different types; replacement and vein-type deposit. The former one consists of fine grained alunite and the later one coarse grained and relatively pure alunite that formed by open space filling. Isomorphous substitution of Na for K in these two types of alunites range 0 to 40 %, indicating that Na/K ratio in the solution is spontaneously changed during the alteration process. Alunite which has higher Na substitution probably formed in an earlier stage while the solution sustain high Na/K ratio. K-Ar age of alunites indicate that the replacement alunite formed earlier($73.9{\pm}2.8Ma$) than the vein-type alunite($71.8{\pm}2.8Ma$). The ${\delta}^{34}S$ value of pyrite and alunite indicate that those minerals formed at isotopically nonequillibrium state. The ${\delta}^{16}O$ and ${\delta}D$ values, of kaolintics 5.0 to 9.0‰ and -54 to -99‰, respectively, indicate that those are formed by hydrothermal solution having magmatic origin which have been diluted by low ${\delta}D$ meteoric water.

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가곡 스카른광상 암석의 물리적 특성 (Physical Properties of Rocks at the Gagok Skarn Deposit)

  • 신승욱;박삼규;김형래
    • 지구물리와물리탐사
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    • 제16권3호
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    • pp.180-189
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    • 2013
  • 물리탐사는 금속광상에서 광화대를 탐사하는데 효율적인 방법으로 국내 외에서 전략광물자원을 개발하기 위하여 널리 이용되고 있다. 물리탐사 결과로부터 광화대를 정확하게 해석하기 위하여 암석의 물리적 특성을 이해하는 것이 매우 중요하다. 따라서 이 연구는 국내 대표적 스카른 광상인 가곡광산의 광석 및 모암을 대상으로 실내에서 다양한 물성을 측정하였으며, 그 결과로부터 가곡 스카른 광상을 구성하는 지층의 물리적 특성을 파악하고자 하였다. 암석시료는 시추코어 및 노두에서 채취하였으며, 시료의 물성은 실내 암석물성 측정시스템을 이용하여 밀도, 대자율, 전기비저항, 광대역 유도분극을 측정하였다. 그 결과 광석은 모암에 비하여 낮은 전기비저항과 높은 대자율 및 밀도를 보였으며, 광대역 유도분극에서 큰 위상과 특정한 임계주파수가 나타났다. 광석의 광대역 유도분극 측정 자료를 Cole-Cole 역산을 통하여 얻은 충전성과 시간상수로부터 황화광물의 함량과 입자의 크기를 추정할 수 있어 스카른 광상 탐사에서 유용할 것으로 기대된다.

국내 맥상광체조사를 위한 3차원 쌍극자-쌍극자 전기비저항 탐사의 적용성 분석 (Feasibility of 3D Dipole-Dipole Electrical Resistivity Method to a Vein-Type Ore Deposit)

  • 민동주;정현기;이효선;박삼규;이호용
    • 지구물리와물리탐사
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    • 제12권3호
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    • pp.268-277
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    • 2009
  • 최근들어 국내 광산탐사가 다시 활성화되면서 물리탐사를 이용한 광산탐사 연구가 늘고 있으며, 물리탐사는 금속광상 뿐만 아니라 비금속광상 탐사에도 활용되어 왔다. 금속광상탐사의 경우 주변에 비해 전기전도도가 높다는 특성에 기초하여 전기비저항 탐사가 많이 이용되며, 대부분 2차원 탐사가 수행된다. 그러나 실제 광맥구조는 주향 방향으로 물성차가 없는 2차원 구조가 아니라 광맥의 폭이 변하거나 광맥의 폭이 좁아지다가 사라지는 3차원 구조이다. 이 연구에서는 이러한 3차원 구조의 효과가 2차원 탐사자료에서 어떻게 나타나는지 조사하였다. 또한 측선이 주향에 수직하지 않은 경우 측선의 방향이 자료해석에 미치는 영향도 함께 살펴보았다. 광맥의 폭이 변하는 모형에 적용해 본 결과 실제 광체가 지표 가까이에 존재하지만 보다 큰 규모의 저비저항대가 심부에 나타났으며, 광체가 존재하다가 사라지는 경우 측선이 광체로부터 떨어져 있음에도 불구하고 마치 직하부에 저비저항대가 존재하는 것처럼 영상화되었다. 이는 모두 3차원 효과에 의한 현상으로 광체가 전혀 존재하지 않는 곳을 시추부지로 선정하도록 유도할 수 있다. 측선이 주향방향과 수직하지 않고 일정한 각을 이루는 경우 측선이 주향에 수직한 경우에 비해서 이상대가 약간 더 넓고 얕게 나타남을 알 수 있었으며, 측선이 주향과 이루는 각이 $45^{\circ}$ 보다 작을 경우 하부 구조가 매우 왜곡되어 나타남을 알 수 있다. 이러한 결과들을 종합해 볼 때, 실제 광상탐사에 전기비저항 탐사를 수행할 경우 2차원 탐사보다는 3차원 탐사를 수행하는 것이 바람직할 것으로 판단된다.

GIS를 이용한 강하분진 중 금속원소의 공간분포분석 (Spatial Distribution Analysis of Metallic Elements in Dustfall using GIS)

  • 윤훈주;김동술
    • 한국대기환경학회지
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    • 제13권6호
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    • pp.463-474
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    • 1997
  • Metallic elements in dustfall have been known as notable air pollutants directly or indirectly influencing human health and wealth. The first aim of this study was to obtain precise spatial distribution patterns of 5 elements (Pb, Zn, K, Cr, and Al) in dustfall around Suwon area. To predict isometric lines of metal fluxes deposited on unsupervised random sites, the study has applied both spatial statistics as a receptor model and a GIS (geographic information system). Total of 31 sampling sites were selected in the study area (roughly 3 by 3 km grid basis) and dustfall samples were then collected monthly basis by the British deposit gauges from Dec., 1995 to Nov., 1996. The metallic elements in the dustfall were then analyzed by an atomic absorption spectrometer (AAS). On the other hand, a base map overlapped by 7 layers was constructed by using the AutoCAD R13 and ARC/INFO 3.4D. Four different spatial interpolation and expolation techniques such as IDW (inverse distance weighted averaging), TIN (triangulated irregular network), polynomial regression, and kriging technique were examined to compare spatial distribution patterns. Each pattern obtained by each technique was substantally different as varing pollutant types, land of use types, and topological conditions, etc. Thus, our study focused intensively on uncertainty analysis based on a concept of the jackknife and the sum of error distance. It was found that a kriging technique was the best applicalbe in this study area.

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아연도금층의 조직 및 물성에 미치는 미량금속원소(Mg-Fe-X)의 복합첨가의 영향(II) (Effect of Trace Metallic Additives of Mg-Fe-X on Microstructure and Properties of Zn Electrodeposits)

  • 예길촌;김대영;안덕수
    • 한국표면공학회지
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    • 제37권2호
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    • pp.99-109
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    • 2004
  • The effect of trace metallic additives on microstructure, glossiness and hardness of Zinc electrodeposits was investigated by using sulfate bath and flow cell system. The preferred orientation of Zn deposits with Mg-Fe additives was (10$\ell$)+(002) mixed texture, while that of Zn deposits with Mg-Fe-Cr additives was ( $10\ell$). The preferred orientation of Zn deposits with Mg-Fe-X(X:Ni,Co) additives changed from ($10\ell$)+(002) to ($10\ell$) with increasing Mg additive from 5 to 10 g/$\ell$. The surface morphology of the Zinc deposits was closely related to the preferred orientation of the deposits. The glossiness of Zn deposits with Mg-Fe additives was similar to that of pure Zn deposit. The glossiness of Zn deposits with Mg-Fe-X(X:Ni,Cr) additives was lower than that of Zn deposits with Mg-Fe additives, while that of Zn deposits with Mg-Fe-Co additives was higher than that of Zn-Mg-Fe deposits. The hardness of Zn deposits with Mg-Fe-X(Ni,Co,Cr) increased with current density and amount of Mg additive. Hardness of Zn deposits was decreased and increased in comparison with Zn-Mg-Fe deposits for Mg-Fe-Co and Mg-Fe-Cr additives, respectively.

아연도금층의 조직 및 물성에 미치는 미량금속원소(Al-Fe-X)의 복합첨가의 영향(I) (Effect of Trace Metallic Additives of Al-Fe-X on Microstructure and Properties of Zn Electrodeposits)

  • 예길촌;김대영;서경훈;안덕수
    • 한국표면공학회지
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    • 제36권6호
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    • pp.444-454
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    • 2003
  • The effect of trace metallic additives of Al-Fe-X on microstructure, glossiness and hardness of Zn electrodeposits was investigated by using sulfate bath. The preferred orientation of Zn deposits with Al-Fe additives was (10 l)(l:3,4,2), while that of Zn deposits with Al-Fe-X(Ni,Co) additives was either (002) or (002)+(103)ㆍ(104) mixed orientation. The preferred orientation of Zn deposits with Al-Fe-Cr additives changed from (002)+(10 l) to (10 l) orientation with increasing amount of Al additive. The surface morphology of the Zn deposits was closely related to the preferred orientation of the deposits. The glossiness of Zn deposits with Al-Fe additives increased in comparison with that of pure Zn deposit. That of the Zn deposits with Al-Fe-X additives was related to the morphology of the deposits and changed according to type of additives. The hardness of Zn deposits with Al-Fe-X(Ni,Co,Cr) additives was noticeably higher than that of Zn deposits with Al-Fe additives.