• 한국표면공학회지
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• 제46권6호
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• pp.258-263
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• 2013

4 mol% Yttria-stabilized zirconia (4YSZ) coatings are fabricated by Air Plasma Spray (APS) and Electron Beam Physical Vapor Deposition (EB-PVD) with top coating of thermal barrier coating (TBC). NiCrAlY based bond coat is prepared as 150 ${\mu}m$ thickness by conventional APS (Air Plasma Spray) method on the NiCrCoAl alloy substrate before deposition of top coating. Each 4YSZ top coating shows different tribological behaviors based on the inherent layer structures. 4YSZ by APS which has splat-stacked structure shows lower friction coefficient but higher wear rate than 4YSZ by EB-PVD which has columnar structure. For 4YSZ by APS, such results are expected due to the sliding wear accompanied with local delamination of splats.

• 한국분말재료학회지
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• 제20권6호
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• pp.460-466
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• 2013

4 mol% Yttria-stabilized zirconia (4YSZ) coatings with $200{\mu}m$ thick are fabricated by Electron Beam Physical Vapor Deposition (EB-PVD) for thermal barrier coating (TBC). $150{\mu}m$ of NiCrAlY based bond coat is prepared by conventional APS (Air Plasma Spray) method on the NiCrCoAl alloy substrate before deposition of top coating. 4 mol% YSZ top coating shows typical tetragonal phase and columnar structure due to vapor phase deposition process. The adhesion strength of coating is measured about 40 MPa. There is no delamination or cracking of coatings after thermal cyclic fatigue and shock test at $850^{\circ}C$.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2003년도 추계학술발표회
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• pp.409-412
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• 2003

Total extraction of stream sediments in the Kwangyang mine area shows their significant pollution with most trace metals such as Cr, Co, Fe, Pb, Cu, Ni, Zn and Cd, due to sulfide oxidation in waste dumps. Calculations of enrichment factor shows that Chonam-ri creek sediments are more severely contaminated than Sagok-ri sediments. Using the weak acid (0.1N HCl) extraction and sequential extraction techniques, the transport and sediment-water partitioning of heavy metals in mine drainage were examined for contaminated sediments in the Chonam-ri and Sagok-ri creeks of the Kwangyang Au-Ag mine area. Calculated distribution coefficient (Kd) generally decreases in the order of Pb $\geq$Al > Cu > Mn > Zn > Co > Ni $\geq$ Cd. Sequential extraction of Chonam-ri creek sediments shows that among non-residual fractions the Fe-Mn oxide fraction is most abundant for most of the metals. This indicates that precipitation of Fe hydroxides plays an important role in regulating heavy metal concentrations in water, as shown by field observations.

• 전기화학회지
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• 제8권4호
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• pp.172-176
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• 2005

차세대 5V급 양극활물질로 각광받고 있는 $LiNi_{0.5}Mn_{1.5}O_4$는 기존의 $LiMn_2O_4$ spinel 물질의 $Mn^{3+}$을 $Ni^{2+}$으로 치환하여 5V 영역에서 $Ni^{2+}/Ni^{4+}$ 산화/환원 반응이 가능하게 한 물질이다. 기존의 $LiMn_2O_4$는 낮은 초기 용량과 충 방전에 따른 빠른 용량감소를 보이는 단점을 가지고 있어 이 문제를 극복하기 위해 Mn의 일부를 다른 금속으로 치환하여 $LiM_yMn_{2-y}O_4$ (M=Cr, Al, Ni, Fe, Co, Cu, Ca)을 만드는 방법이 활발히 연구되고 있다. 본 연구에서는 기계 화학적 합성법을 이용하여 합성한 $LiNi_{0.5}Mn_{1.5}O_4$의 전기화학적 특성에 대해 연구하였다. 이 물질은 기존의 $LiMn_2O_4$보다 에너지 밀도가 높으며 저가 및 친환경성 등으로 앞으로 HEV 등에서 그 활용성이 크게 기대된다. 볼밀을 이용하여 여러가지 조건(출발물질 조건, 볼밀조건, 열처리조건 등)에서 $LiNi_{0.5}Mn_{1.5}O_4$을 합성한 결과 기계화학적 방법으로는 $Ni^{2+}$가 $Mn^{3+}$를 완전히 치환하지 못하여 $4.0{\sim}4.1V$의 전압에서 $Mn^{3+}/Mn^{4+}$의 산화/환원과 관련된 peak가 발생하였다. Ni 원료 물질로써 수산화 물질을 사용하고 열처리 온도를 $800^{\circ}C$로 하였을 때 최상의 성능을 나타내었다.

• 자원환경지질
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• 제30권5호
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• pp.417-431
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• 1997

Characteristics of sedimentary rocks and enrichment of toxic elements in shale and coal from the Chungnam coal field were investigated based upon geochemistry of major, trace and rare earth elements. Shale and coal of the area are interbedded along the Traissic to the Jurassic Daedong Supergroup, which can be subdivided into grey shale, black shale and coal. The coal had been mined, however all the mines are abandonded due to the economic problems. The shale and coal are characterized by relatively low contents of $SiO_2$, and $Al_2O_3$ and high levels of loss-on-ignition (LOI), CaO and $Na_2O$ in comparison with the North American Shale Composite (NASC). Light rare earth elements (La, Ce, Yb and Lu) are highly enriched with the coal. Ratios of $Al_2O_3/Na_2O$ and $K_2O/Na_2O$ in shale and coal range from 30.0 to 351.8 and from 4.2 to 106.8, which have partly negative correlations against $SiO_2/Al_2O_3$ (1.24 to 6.06), respectively. Those are suggested that controls of mineral compositions in shale and coal can be due to substitution and migration of those elements by diagenesis and metamorphism. Shale and coal of the area may be deposited in terrestrial basin deduced from high C/S (39 to 895) and variable composition of organic carbon (0.39 to 18.40 wt.%) and low contents of reduced sulfur (0.01 to 0.05 wt.%). These shale and coal were originated from the high grade metamorphic and/or igneous rocks, and the rare earth elements of those rocks are slightly influenced with diagenesis and metamorphism on the basis of $Al_2O_3$ versus La, La against Ce, Zr versus Yb, the ratios of La/Ce (0.38 to 0.85) and Th/U (3.6 to 14.6). Characteristics of trace and rare earth elements as Co/Th (0.07 to 0.86), La/Sc (0.31 to 11.05), Se/Th (0.28 to 1.06), V/Ni (1.14 to 3.97), Cr/V (1.4 to 28.3), Ni/Co (2.12 to 8.00) and Zr/Hf (22.6~45.1) in the shale and coal argue for inefficient mixing of the simple source lithologies during sedimentation. These rocks also show much variation in $La_N/Yb_N$ (1.36 to 21.68), Th/Yb (3.5 to 20.0) and La/Th (0.31 to 7.89), and their origin is explained by derivation from a mixture of mainly acidic igneous and metamorphic rocks. Average concentrations in the shale and coal are As=7.2 and 7.5, Ba=913 and 974, Cr=500 and 145, Cu=20 and 26, Ni=38 and 35, Pb=30 and 36, and Zn=77 and 92 ppm, respectively, which are similar to those in the NASC. Average enrichment indices for major elements in the shale (0.79) and coal (0.77) are lower than those in the NASC. In addition, average enrichment index for rare earth elements in coal (2.39) is enriched rather than the shale (1.55). On the basis of the NASC, concentrations of minor and/or environmental toxic elements in the shale and coal were depleted of all the elements examined, excepting Cr, Pb, Rb and Th. Average enrichment indices of trace and/or potentially toxic elements (As, Cr, Cu, Ni, Pb, U and Zn) are 1.23 to 1.24 for shale and 1.06 to 1.22 for coal, respectively.

• 환경위생공학
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• 제24권1호
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• pp.33-39
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• 2009

In order to investigate effect of metal ion and antioxidant on rancidity of crude rapeseed oil (CRO), $Fe^{2+}$, $Cu^{2+}$, $Co^{2+}$, $Ni^{2+}$, $Cr^{2+}$, $Sn^{2+}$, $Mn^{2+}$, $Zn^{2+}$, and antioxidants including BHA, Vitamin C, and Tocopherol were used. The specific gravity and refractive index of CRO were $0.92g/cm^3$ and 1.45, respectively. The chromaticities of light, red, and yellow in CRO were 88.6 and 98.7, respectively. Among various fatty acids, Oleic acid (C18:1) concentration was highest, 62.3% and Linoleic acid (C18:2) concentration was 19.16%. In the case of Linolenic acid (C18:3) and Palmitic acid (C16:0), they were 9.88 and 5.2%, respectively. The concentrations of unsaturated fatty acids and saturated fatty acid were 92.2 and 7.8%, respectively. The degree of expediting rancidity of CRO was an order of $Fe^{2+}$> $Cu^{2+}$> $Cr^{2+}$> $Zn^{2+}$> $Ni^{2+}$> $Al^{2+}$> $Mn^{2+}$> $Mn^{2+}$> $Sn^{2+}$> $Co^{2+}$> $Li^{2+}$. Especially, when $Cu^{2+}$ and $Fe^{2+}$ was used, the peroxide value concentration was about 4.0 fold higher than non addition of them. The inhibition effect of rancidity of CRO using antioxidant with $Cu^{2+}$ and $Fe^{2+}$ was an order of BHA> Vitamin C> Tocopherol.

• Ocean and Polar Research
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• 제25권4호
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• pp.447-457
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• 2003

In order to understand the distribution of changes of geochemical characteristics in surface sediments according to various environmental changes around the artificial Lake Shihwa, surface sediments were sampled at $13{\sim}15$ sites form 1997 to 1999 and analyzed by C/S analyzer, ICP/MS and AAS. The average $S/C_{org}$ ratio was 0.35 in the surface sediments, which is similar to 0.36, the characteristic ratio of marine sediments. Heavy metal contents and enrichment factors in the surface sediments tended to be decreasing from the head to the mouth of the Lake Shihwa. With the deposition of fine-grained sediments in the central part of lake, anoxic water column induced the sulfides compounds with Cu, Cd and Zn. Metals such as Al, Fe, Cr, Co, Ni, Cu, Zn and Cd except for Mn and Pb showed relatively high correlation coefficients among them. The contents of Cr, Co, Ni, Cu, Zn and Cd in the surface sediments of the lake were two to five times higher than those in the lake before dike construction and also in outer part of the dike. These are mainly due to the Input of untreated industrial and municipal waste-waters into the lake, and the accumulation of heavy metals by limitation of physical mixing. Although metal contents of the surface sediments at the sites near the water-gate due to outer seawater inflow tended to be lower than those during the desalination, heavy metals were deposited in areas around the new industrial complex in the evidence of spatial distribution of heavy metals in the sediments. This is mainly due to the input of untreated waste-waters from tributaries.

• 한국표면공학회지
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• 제40권4호
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• pp.175-179
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• 2007

An Fe-Ni-Co based superalloy Incoloy 909 (Incoloy 909) has been used for gas turbine engine component material. This alloy is susceptible to high temperature oxidation and corrosion because of the absence of corrosion resistant Cr. For the improvement of durability of the component of Incoloy 909 aluminizing-chromate coating by pack cementation process has been investigated at relatively low temperature of about $550^{\circ}C$ to protect the surface microstructure and properties of Incoloy 909 substrate. As a previous study to aluminizing-chromate coating by pack cementation of Incoloy 909, the optimal aluminizing process has been investigated. The size effects of source Al powder and inert filler $Al_O_3$ powder and activator selection have been studied. And the dependence of coating growth rate on aluminizing temperature and time has also been studied. The optimal aluminizing process for the coating growth rate is that the mixing ratio of source Al powder, activator $NH_4Cl$ and filler $Al_O_3$ are 80%, 1% and 19% respectively at aluminizing temperature $552^{\circ}C$ and time 20 hours.

• 한국환경농학회지
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• 제20권1호
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• pp.20-27
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• 2001

보은광산지역 하천수의 pH는 $6.8{\sim}8.2$로 약산성에서 약 알카리성에 걸친 수질변화를 보여주며, 건기보다는 우기의 하천수가 산성우의 영향으로 인해 다소 pH가 낮게 나타났다. 방치된 폐석 등의 영향으로 Mg, Ca, $HCO_3$, $SO_4$, Al, Fe, Zn, Ni, Co, Cr, Cd, Sr, U 이 하천수내에 부화되어 나타나며, Na, K, As, Cu, $NO_3$, Cl 등은 낮은 농도함량을 보여 이들 원소에 대해 폐광석으로부터의 영향이 거의 없는 것으로 보인다. 주요 양이온 농도는 Mg>Ca>Na>K의 순서로 함량변화를 보이며, 음이온의 함량변화는 $SO_4>HCO_3>Cl>NO_3$의 순서로 나타나 본 하천수는 $Mg-SO_4$ 타입을 보인다. 하천수의 우기와 건기의 이온의 농도변화는 ${\pm}30$ % 이내에서 나타나며, Na, K, $HCO_3$, U, Sr, Cr은 우기 중에 낮은 농도를 보여 우수에 의해 희석되어졌을 가능성이 크다. 우기중에 높은 농도를 보이는 Ca, Mg, $NO_3$, Cd, Co는 약산성의 우수에 의해 기반암이나 폐석으로부터 쉽게 용출되는 원소들이라 판단되었다. TDS, EC 및 Ca, Na, Mg, $HCO_3$, $SO_4$, Fe, Ni, Sr, U등의 원소는 광산으로부터 멀어질수록 하류를 향해 농도가 감소하는 경향을 보여, 이들 원소에 대해서 광폐석이 특히 주요한 오염원으로 작용하고 있으며, 이들 원소의 농도를 컨트롤하는 인자는 희석작용이나 흡착작용 등이 복합적으로 관여하고 있을 것으로 생각된다. 본 광산지역의 하천수내에 일어나는 화학적 현상은 크게 두 가지로 얘기할 수 있다. 철을 함유한 황화광물(황철석 등)의 산화로 인한 Fe과 $SO_4$의 하천수내에 부화현상과 풍화된 기반암에서 탄산의 용출이나 이온교환작용에 의한 중화작용으로 하천은 산성을 띠기보다 오히려 약 알카리성을 띠는 특징을 보인다. 기반암의 영향으로 하천의 지나친 산성화는 일어나지 않을 것으로 보이나 하천내의 이온함량은 비오염수에 비해 극히 높은 값을 보여 방치된 폐석이 잠재적인 위험성을 내포하고 있음을 시사한다. 또한 알카리상태에서 부화된 철은 철수산화물의 형태로 침전되어 하천의 적화현상을 일으키는 주원인 물질로 작용한다. 이들 철산화물은 침전되면서 동시에 하천내의 용존 중금속을 흡착이나 공침에 의해 동시에 침전시키는 역할을 하는 것으로 방치될 경우 2차적 오염원으로 작용할 우려가 있어, 이들 철산화물에 대한 보다 상세한 연구가 필요하다고 사려된다.

• 비파괴검사학회지
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• 제29권5호
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• pp.450-457
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• 2009

열차폐 코팅 시편에 대하여 열충격을 주기적으로 가한 후 발생하는 결함을 관찰하였다. 실험에 사용 된 열차폐 코팅 시편은 인코넬-738로 제작된 모재 위에 CoNiCrAlY 본드 코팅층과 $ZrO_2-8wt%Y_2O_3$ 세라믹탑 코팅층이 플라즈마 용사 방법으로 올려진 형태로 되어있다. 열충격 시험은 $1000^{\circ}C$의 고온으로 가열했다가 상온으로 급격하게 냉각시키는 가혹한 조건으로 실행되었고, 사이클 수가 증가함에 따라 열충격의 피로도 또한 증가하였다. 시험후 시편 내부의 미세 조직 변화와 결함을 전자현미경으로 관찰하고, 시편의 기계적인 특성을 측정하여 그 변화 양상을 살펴보았다. 열충격 주기실험후 본드 코팅층과 세라믹 탑 코팅층 사이에 발생하는 TGO 산화물층에 대한 변화 양상과 이에 대한 와전류 신호를 측정하여 TGO층 성장 거동의 비파괴적인 평가를 위한 실험을 진행하였다. 본 연구를 통하여 마이크로 단위의 TGO층에 대한 와전류검사의 적용 가능성을 확인하고 열차폐 코팅의 수명을 예측할 수 있는 가능성을 제시하였다.