• 한국세라믹학회지
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• 제52권5호
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• pp.350-355
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• 2015

To develop ceramic composite anodes of solid oxide fuel cells without metal catalysts, a small amount of barium carbonate was added to an $(La_{0.8}Sr_{0.2})(Cr_{0.5}Mn_{0.5})O_3(LSCM)$ - YSZ ceramic composite anode and its catalytic effects on the electrode performance were investigated. A barium precursor solution with citric acid was used to synthesize the barium carbonate during ignition, while a barium precursor solution without citric acid was used to create hydrated barium hydroxide. The addition of barium carbonate to the ceramic composite anode caused stable fuel cell performance at 1073 K; this performance was higher than that of a fuel cell with $CeO_2$ catalyst; however, the addition of hydrated barium hydroxide to the ceramic composite anode caused poor stability of the fuel cell performance.

• 한국결정성장학회:학술대회논문집
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• 한국결정성장학회 1996년도 The 9th KACG Technical Annual Meeting and the 3rd Korea-Japan EMGS (Electronic Materials Growth Symposium)
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• pp.258-292
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• 1996

In the last year great interest appears to YBCO thin films preparation on different substrate materials. Preparation of epitaxial film is a very difficult problem. There are many requirements to substrate materials that must be fullfilled. Main problems are lattice mismatch (misfit) and similarity of structure. From paper [1] or follows that difference in interatomic distances and angles of substrate and film is mire important problem than similarity of structure. In this work we present interatomic distances and angle relations between substrate materials belonging to ABCO4 group (where A-Sr or Ca, B-rare earth element, C-Al or Ga) of different orientations and YBCO thin films. There are many materials used as substrates for HTsC thin films. ABCO4 group of compounds is characterized by small dielectric constants (it is necessary for microwave applications of HTsC films), absence of twins and small misfit [2]. There most interesting compounds CaNdAlO4, SrLaAlO4 and SrLaGaO4 were investigated. All these compounds are of pseudo-perovskite structure with space group 14/mmm. This structure is very similar to structure of YBCO. SLG substrate has the lowest misfit (0.3%) and dielectric constant. For preparation of then films of substrates of this group of compound plane of <100> orientation are mainly used. Good quality films of <001> orientations are obtained [3]. In this case not only a-a misfit play role, but c-3b misfit is very important too. Sometimes, for preparation of thin films substrates of <001> and <110> orientations were manufactured [3]. Different misfits for different YBCO faces have been analyzed. It has been found that the mismatching factor for (100) face is very similar to that for (001) face so there is possibility of preparation of thin films on both orientations. SrLaAlO4(SLA) and SrLaGaO4(SLG) crystals of general formula ABCO4 have been grown by the Czochralski method. The quality of SLA and SLG crystals strongly depends on axial gradient of temperature and growth and rotation rates. High quality crystals were obtained at axial gradient of temperature near crystal-melt interface lower than 50℃/cm, growth rate 1-3 mm/h and the rotation rate changing from 10-20pm[4]. Strong anisotropy in morphology of SLA and SLG single crystals grown by the Czochralski method is clearly visible. On the basics of our considerations for ABCO4 type of the tetragonal crystals there can appear {001}, {101}, and {110} faces for ionic type model [5]. Morphology of these crystals depend on ionic-covalent character of bonding and crystal growth parameters. Point defects are observed in crystals and they are reflected in color changes (colorless, yellow, green). Point defects are detected in directions perpendicular to oxide planes and are connected with instability of oxygen position in lattice. To investigate facets formations crystals were doped with Cr3+, Er3+, Pr3+, Ba2+. Chromium greater size ion which is substituted for Al3+ clearly induces faceting. There appear easy {110} faces and SLA crystals crack even then the amount of Cr is below 0.3at.% SLG single crystals are not so sensitive to the content of chromium ions. It was also found that if {110} face appears at the beginning of growth process the crystal changes its color on the plane {110} but it happens only on the shoulder part. The projection of {110} face has a great amount of oxygen positions which can be easy defected. Pure and doped SLA and SLG crystals measured by EPR in the<110> direction show more intensive lines than in other directions which allows to suggest that the amount of oxygen defects on the {110} plane is higher. In order to find the origin of colors and their relation with the crystal stability, a set of SLA and SLG crystals were investigated using optical spectroscopy. The colored samples exhibit an absorption band stretching from the UV absorption edge of the crystal, from about 240 nm to about 550 m. In the case of colorless sample, the absorption spectrum consists of a relatively weak band in the UV region. The spectral position and intensities of absorption bands of SLA are typical for imperfection similar to color centers which may be created in most of oxide crystals by UV and X-radiation. It is pointed out that crystal growth process of polycomponent oxide crystals by Czochralski method depends on the preparation of melt and its stoichiometry, orientation of seed, gradient of temperature at crystal-melt interface, parameters of growth (rotation and pulling rate) and control of red-ox atmosphere during seeding and growth (rotation and pulling rate) and control of red-ox atmosphere during seeding and growth. Growth parameters have an influence on the morphology of crystal-melt interface, type and concentration of defects.

• 환경위생공학
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• 제5권1호
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• pp.7-13
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• 1990

대구지방의 중요 하천인 낙동강, 금호강 및 신천을 대상으로 이들간의 수질차이와 홍수 전(8월24일)과 후(9월8일)의 수질차이를 비교하는 한편, 각 하천수가 Spirodela polyhiza Shleiden의 생육에 미치는 영향을 조사하였다. 홍수 전의 화학 성분 농도는 대부분 금호강과 신천이 서로 유사하며(COD, 19.6~21.4; alkalinity, 177~183; ${NH_4}^{+},\; 20.7~24.4;\;{NO_3}^{-}\;39~4.3;\;{PO_4}^{3-},\;3.4~3.7;Ca^{2+},\;68.5~69.7;\;Mg^{2+},\;42;\;Cl^{-},\;90~92;SiO_2, \;10.4~11.2;\;{SO_4}^{2-},\;11~32;\;LAS,\;3.0~3.8;\;Cr^{3+,6+}$, 0.007~0.010ppm), 낙동강에 비해 훨씬 높았다.(${NH_4}^{+},\;{SO_4}^{2-},\;{PO_4}^{3-}$ 및 LAS는 30~40배 : COD, alkalinity,${NO_3}^{+},\;Mg^{2+},\;Cl^{-}$ 및 $Cr^{3+,6+}$은 2~5배). 특히 금호강은 다른 하천과는 달리 Secchi disk transparency가 극히 낮고(17cm), DO가 검출되지 않았다. Phytoplankton 군집의 general diversity index($\bar{H}$)는 낙동강, 금호강 및 신천이 각각 3.1, 2.7 및 1.6으로 신천의 오염도가 가장 높았다. 홍수기 후에는 특히 다음과 같은 성분이 증가하였다.(낙동강-${NH_4}^{+},1.0;\;{NO_3}^{-},9.6;\;SiO_2,\;12.8;\;{SO_4}^{2-}\;5.4ppm$; 금호강 DO, 1.0;${NO_2}^{-},\;0.92;\;{NO_3}^{-},\;22.2;{SiO_2},\;17.6ppm$; 신천-DO, 3.0;${NO_2}^{-},\;1.4;\;{NO_3}^{-},\;22.2;{SiO_2},\;19.2;{SO_4}^{2-}\;25ppm$). S.polyrhiza의 생육은 금호강수에서 가장 왕성한 반면(최대 RGR, 26%/day), 금호강수에서는 배양 7일째 생장이 중지되었고, 배양 11일째의 total chlorophy 일 함량은 낙동, 금호 및 신천수에서 각각 1.04, 1.88 및 1.25mg/g frond였다. 이들 하천수에 함유된 LAS(0.1~3.8ppm), $Cd^{2+}$(0~0.02ppm) 및 $Cr^{6+}$(0.004~0.010ppm)은 이 식물의 생육을 크게 저해하지 않았다.

• 한국수소및신에너지학회논문집
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• 제34권6호
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• pp.587-593
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• 2023

This research project focused on the production of hydrogen through ammonia decomposition reactions while investigating how the reactivity of this process varies when employing different catalysts. Several metal oxide supports (Al₂O₃, La₂O₃, CeO₂) were utilized as catalysts, with active metals from both the transition metal group (Co, Ni, Fe, Cr, Cu) and the noble metal group (Ru, Rh, Pd, Pt) impregnated onto these supports. Furthermore, the study examined how the reactivity evolves with changes in reaction temperature when employing the prepared catalysts. Additionally, the research delved into the distinctive activation energies associated with each of the catalysts. In this research, In the noble metal catalyst system, the order of high activity for ammonia decomposition reaction to produce hydrogen is Ru > Rh > Pt ≈ Pd. In the transition metal catalyst system, the order of high activity is Co > Ni > Fe > Cr > Cu.

• 자원환경지질
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• 제32권6호
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• pp.611-631
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• 1999

Enviromental geochemisty and heary metal contamination at the Kongjueil mine creek were underaken on the basis of physicohemical properties and mineralogy for various kinds of water (surface, mine and ground water),soil, precipitate and sediment collected of April and December in 1998. Hydrgeochemical composition of the water samples are characterized by relatively significant enricant of Ca+Na, alkiali ions $NO_3$ and Cl inground and surfore water, wheras the mine waters are relatively eneripheral water of the mining creek have the characteristics of the (Ca+Mg)-$(HCO_3+SO_4)$type. The pH of the mine water is high acidity (3.24)and high EC (613$\mu$S/cm)compared with those of surface and ground water. The range of $\delta$D and $\delta^{18}O$ values (relative to SMOW) in the waters are shpwn in -50.2 to -61.6% and -7.0 to -8.6$\textperthousand$(d value=5.8 to 8.7). Using computer program, saturation index of albite, calcite, dolomite in mine water are nearly saturated. The gibbiste, kaolinite and smectite are superaturated in the surface and ground water, respectively. Calculated water-mineral reaction and stabilities suggest that weathing of silicate minerals may be stable kaolinite owing to the continuous water-rock reaction. Geochemical modeling showed that mostly toxic heavy metals may exist larfely in the from of metal-sulfate $(MSO_4\;^2)$and free metal $(M^{2+})$ in nmine water. These metals in the ground and surface water could be formed of $CO_3$ and OH complex ions. The average enrichment indices of water samples are 2.72 of the groundwater, 2.26 of the surface water and 14.15 of the acid mine water, normalizing by surface water composition at the non-mining creek, repectively. Characteristics of some major, minor and rate earth elements (Al/Na, K/Na, V/Ni, Cr/V, Ni/Co, La/Ce, Th/Yb, $La_N/Yb_N$, Co/Th, La/Sc and Sc/Th) in soil and sediment are revealed a narrow range and homogeneous compositions may be explained by acidic to intermediate igneous rocks. And these suggested that sediment source of host granitic gneiss colud be due to rocks of high grade metamorphism originated by sedimentary rocks. Maximum concentrations of environmentally toxic elements in sediment and soil are Fe=53.80 wt.% As=660, Cd=4, Cr=175, Cu=158, Mn=1010, Pb=2933, Sb=4 and Zn=3740 ppm, and extremely high concentrations are found are found in the subsurface soil near the ore dump and precipitates. Normalizing by composition of host granitic gneiss, the average enerichment indices are 3.72 of the sediments, 3.48 of the soils, 10.40 of the precipitates of acid mine drainage and 6.25 of the soils near the main adit. The level of enerichment was very severe in mining drainage sediments, while it was not so great in the soils. mineral composition of soil and sediment near the mining area were partly variable being composed of quartz, mica, feldspar, chlorite, vermiculite, bethierin and clay minerals. reddish variable being composed of quartz, mica, feldspar, chlorite, vermiculite, bethierin and clay minerals. Reddish brown precipitation mineral in the acid mine drainage identifies by schwertmanite. From the separated mineralgy, soil and sediment are composed of some pyrite, arsenopyite, chalcopyrite, sphalerite, galena, malachite, goethite and various kinds of hydroxied minerals.

• 한국전기화학회:학술대회논문집
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• 한국전기화학회 2004년도 수소연료전지공동심포지움 2004논문집
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• pp.297-302
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• 2004

• 전기화학회지
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• 제13권4호
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• pp.256-263
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• 2010

본 연구에서는 고체산화물 연료전지의 공기극 집전체로 사용되고 있는 고가의 Ag 소재를 대체하고자 전도성 세라믹이 코팅된 mesh 형태의 Crofer 22 APU 집전체를 개발하였다. 고전자전도성의 $(La_{0.80}Sr_{0.20})_{0.98}MnO_3$ (LSM)을 습식 스프레이법으로 코팅하여 고온 산화 및 전기적 특성의 열화를 억제하고자 하였다. $800^{\circ}C$의 산화 실험 결과에 의하면 LSM이 코팅된 Crofer mesh의 면저항(area-specific resistance)은 mesh의 제작에 사용된 와이어 지름과 접촉 부위의 형상등 실제 접촉점의 수 및 면적을 좌우하는 mesh의 특성에 의해 좌우되었다. 또한 LSM 코팅 후 $H_2/N_2$ 분위기에서의 열처리를 통해 Crofer mesh와 LSM 코팅층 계면에서의 Cr 함유 산화물의 형성을 효과적으로 억제하여 전기적 특성의 열화를 억제할 수 있다.

• 암석학회지
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• 제6권1호
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• pp.1-18
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• 1997

이 연구에서는 한반도 남해안 도서지역중 거제도 일대의 화산암류를 대상으로 암석 기재, 암석화학적 특성을 알아보고, 화산암류의 조구적 위치 및 성인에 대하여 고찰하고자 한다. 본 역의 화산암류는 백악기의 퇴적암층을 기반으로 피복하여 주로 안산암질 화성쇄설암과 용암류가 교호로 누적된 산상 즉, 최하부는 두터운 화산각력암, 응회각력암 및 라필리응회암 누층으로 구성되고, 상부로 감에 따라 상대적으로 안산암 용암류가 라필리응회암과 응회암을 협재하며 빈번하게 노출되고 최상부에는 데사이트-유문암질 용결회류응회암류가 분포한다. 본 역의 화산암류는 주성분 화학조성으로 볼 때, 현무암에서 현무암질안산암, 안산암, 데사이트 그리고 유문암에 이르는 넓은 성분 조성을 하며 전형적인 BAR조합을 나타낸다. 본 역의 화산암류는 칼크-알칼리암계열에 속하며, SiO2에 대한 K2O 성분에서 medium-K의 조성을 나타내고, La, Th 및 Nb 상관도에서 조산대안산암(orogenic andesite)의 영역에 도시된다. 미량원소 함량을 MORB값으로 표준화한 spider diagram에서 Sr, K, Rb, Ba, Th 등이 다른 원소에 비하여 상대적으로 높은 값을 가지는 반면, Nb, P, Ti, Cr의 함량이 낮은, 지판의 침강 섭입에 관련된 대륙연번부/도호의 조구적환경에 관련된 암석들에 나타나는 특징을 잘 나타낸다. 희토류원소를 chondrite로 표준화한 그림에서는 전체적으로 LREEs가 HREEs에 비하여 부화되어 있으며, 현무암에서 현무암질안산암, 안산암, 데사이트 및 유문암으로 감에따라 Eu의 '-'이상이 점진적으로 커지며, 변화패튼이 대체로 평행한 배영을 보여주므로 본 역의 암석들은 동원마그마에서 유래하였음을 알 수 있다. 지구조위치 판별도에서 본 역의 화산암류는 지판이 침강 섭입하는 지판경계부에서 생성된 마그마로부터 유래한 화산암의 조구적 위치 즉 정상적인 대륙연변호(normal continental margin arc)의 영역에 해당한다. 거제도지역의 화산암류는 약 10% 정도의 맨틀물질의 부분용융으로 형성된 현무암질 시원마그마가 생성되어 지각으로 상승하는 과정에서 분별되어 칼크-알칼리 안산암질 마그마가 형성되었으며, 이 마그마로부터 계속 분별결정작용, 동화작용 및 마그마 혼합 등의 과정을 거치면서 다양한 화산암류를 형성한 것으로 해석된다.

• 한국광물학회지
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• 제13권3호
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• pp.147-163
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• 2000

The mineralogy and chemical composition of reddish to brownish yellow residual soils, so called "Hwangto" have been examined according to representative host rocks. The result of the study indicates that Hwangto consists of 40-80% clay minerals and various minerals such as quartz, feldspar, hornblende, goethite, and gibbsite. Clay minerals include kaolinite, halloysite, illite, hydroxy interlayered vermiculite (HIV), mica/vermiculite interstratifield mineral and chlorite. The mineralogical constituents and contents of Hwangto were different depending on the types of host rocks. Moreover, the Jurassic granitic rocks contain relatively more kaolin minerals, whereas the Cretaceous granitic rocks contain more HIV and illite. In addition, reddish Hwangto contains relatively more kaolinite and HIV, and yellowish Hwangto contains more illite and halloysite. It is suggested that feldspars and micas of host rocks were chemically weathered into illite, halloysite, illite/vermiculite interstratified minerals, and HIV, and finally into kaolinite. Compared with their host rocks, the major chemical compositions of Hwangto tend to contain more $Al_2O_3,\;Fe_2O_3,\;H_2O$ in amount and less Ca, Mg, and Na. Hwangto contains relatively high amount of trace elements, P, S, Zr, Sr, Ba, Rb, and Ce including considerable amount of Li, V, Cr, Zn, Co, Ni, Cu, Y, Nb, La, Nd, Pb, Th in excess of 10 ppm. Relatively high amount of most trace elements were detected in the Hwangto. The major and minor chemical compositions of the Hwangto were different depending on the types of host rocks. However, their difference was in the similar range compared with the compositions of host rocks.

• 대한기계학회논문집B
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• 제31권12호
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• pp.1033-1041
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• 2007

This paper studied the characteristics of performance and temperature in a unit cell of a planar type SOFC under various conditions by employing computational fluid dynamics (CFD). In order to derive thermal stress distribution and performance characteristics, the 3-D model simulation for a single channel was performed in various conditions which include interconnect materials $(LaCrO_3/AISI430)$, gas flow direction (co-flow/counter-flow) and inlet temperature (923 K/1173 K). From these results of a single channel, the most effective conditions were applied to the unit stack with multi-channel and the temperature distribution is displayed. Considering both thermal stress and performance, the best combination is 923 K inlet temperature, counter-flow and interconnector of stainless steel. As the end results, flow, thermal and current density distributions were found in the model with multi-channel applied to the best combination and were concentrated in the middle of channels than in the edge.