• 한국전기전자재료학회:학술대회논문집
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• 한국전기전자재료학회 2009년도 하계학술대회 논문집
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• pp.363-364
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• 2009

본 연구는 IEC/TC 90 규격을 참조하여 Cu stabilizer/Ag/$LaMnO_3$/IBAD-MgO/$Y_2O_3$/$Al_2O_3$/Hastelloy C276/Cu stabilizer의 구조를 가지는 coated conductor의 DC 임계 전류의 결정에 대한 사전 연구를 위해 (1) 시편의 냉각시간, (2) 전류 선의 용량을 변화하여 임계 전류의 변화를 관찰하여 다음과 같은 결과를 얻었다. (1) 5분 이상의 시편 냉각시간은 COV가 약 0.4% 정도로 거의 임계 전류 결정에 영향을 주지 않았으며, 냉각 시간이 길면 길수록 임께 전류 이하에서 전압의 기저면이 낮아지는 경향을 보였다. (2) 전류 선의 용량이 클수록 임계 전류 이하에 전압의 기저면이 낮아지는 경향을 보였다.

• 광물과 암석
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• 제35권2호
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• pp.153-168
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• 2022

치악산 편마암복합체에서 방사성원소를 포함하고 있는 광물을 파악하고, 주변 지하수에 포함되어 있는 방사선원소(우라늄)와의 연관성을 확인하고자 암석학적 및 광물 화학 분석을 수행하였다. 현미경 및 전자현미경 분석 결과, 주 구성광물은 사장석, 흑운모, 석영, 알칼리장석, 녹니석 그리고 방해석이며, 부수광물은 스펜, 갈렴석, 인회석, 저어콘, 토라이트, 티탄철석, 황철석 그리고 방연석 등 총 14종을 확인하였다. 토라이트의 경우 거정의 갈렴석 내 ~1 mm의 크기로 소량 관찰된다. 희토류 원소를 많이 포함하고 있는 갈렴석은 각기 다른 3 가지 산출양상을 보인다. EPMA 분석 결과, 거정의 갈렴석에서는 TiO₂~1.70 wt.%, Ce₂O₃~11.86 wt.%, FeO~13.31 wt.%, MgO~0.90 wt.% 그리고 ThO₂~1.06 wt.% 원소들의 함량이 높게 나타나며, Al₂O₃ 17.35 ± 2.15 wt.% (n = 7), CaO 12.13 ± 1.81 wt.% (n = 7) 평균 함량이 가장 낮은 값을 보인다. 티탄철석을 둘러싸고 있는 스펜 집합체의 가장자리에 존재하는 갈렴석은 Al₂O₃~24.00 wt.%, Nd₂O₃~5.10 wt.%, Sm₂O₃~0.66 wt.%, Dy₂O₃~0.86 wt.% 그리고 Y₂O₃~1.38 wt.% 원소들의 함량이 높게 나타나며, TiO₂ 0.35 ± 0.21 wt.% (n = 11), Ce₂O₃ 5.25 ± 1.03 wt.% (n = 11), FeO 9.84 ± 0.26 wt.% (n = 11), MgO 0.12 ± 0.05 wt.% (n = 11) 그리고 La₂O₃ 1.49 ± 0.29 wt.% (n = 11) 등과 같이 평균 함량이 가장 낮은 값을 보인다. 모암의 기질부에서 관찰되는 갈렴석의 화학성분은 앞서 설명한 갈렴석의 중간 정도의 값을 가진다. 연구대상인 치악산 편마암복합체 내 미그마타이트질 편마암에는 주목할 만큼의 우라늄 함량을 가지는 광물이 발견되지는 않았다. 따라서 지하수에서 나타나는 우라늄의 기원과 주변 지질과의 연관성을 명확하게 밝혀내지는 못했다. 하지만 방사성 원소인 토륨 원소 및 희토류 원소를 다량 포함하는 갈렴석이 풍부하게 존재하는 것이 이번 연구결과로 확인되었다.

• 한국전기전자재료학회:학술대회논문집
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• 한국전기전자재료학회 2009년도 춘계학술대회 논문집
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• pp.9-9
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• 2009

Coated conductor is required to have good critical current property for high efficiency of electric power applications. Until now, long coated conductor does not show high Jc over 3 MA/$cm^2$ in thick superconducting layer because of texture degradation by thick superconducting layer. In this study, in order to overcome this issue, thicker superconducting layer was deposited with optimized conditions to reduce the degradation of critical current density. SmBCO superconducting coated conductor was deposited with 1~3 um of thickness at $750\sim850^{\circ}C$ under 15~20 mTorr of oxygen partial pressure using batch type EDDC( evaporation using drum in dual chamber). The buffered substrate for superconducting layer deposition was used IBAD-MgO template with the architecture of $LaMnO_3/MgO/Y_2O_3/Al_2O_3$/Hastelloy. After fabrication of coated conductor, critical current was measured by 4-prove method under self-magnetic field and 77K. In addition, surface morphology and texture were analyzed by SEM and XRD, respectively. 3 um thick SmBCO coated conductor shows highest $I_C$ values of 638A/cm-w in 1 m long in the world.

• 한국전기전자재료학회:학술대회논문집
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• 한국전기전자재료학회 2009년도 춘계학술대회 논문집
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• pp.1-2
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• 2009

The high critical current ($I_c$, A) of SmBCO coated conductor in a magnetic field, the high production rate and the high material yield are promising for applications. The inhomogeneity of Ie at the long length coated conduct is very important problem for electric application. So we researched the reason of inhomogeneity of $I_c$ at long length tape prepared by batch type co-evaporation system called by EDDC. The long length SmBCO coated conductors were developed on $LaMnO_3/IBAD-MgO/Y_2O_3/Al_2O_3$/Hastelloy C276 template. The distribution of $I_c$ are from 0 to 397 A/cm at 77 K and self field. We have studied the microstructures of these films by using SEM, EDS and X-ray diffraction. The XRD and composition by EDS results of SmBCO film reveals subtle difference. But, the microscopic observation by SEM show the microcrack at the sample with low $I_c$.

• 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.