• 한국전기전자재료학회:학술대회논문집
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• 한국전기전자재료학회 2000년도 하계학술대회 논문집
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• pp.790-793
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• 2000

We have fabricated good quality superconducting YBa$_2$Cu$_3$$O_{7-x}$(YBCO) thin films on Hastelloy(Ni-Cr-Mo alloys) metallic substrates with CeO$_2$and BaTiO$_3$buffer layers in-situ by pulsed laser deposition in a multi-target processing chamber. YBCO film with CeO$_2$ single buffer layer shows T$_{c}$ of 71.64 K and the grain size less than 0.1 ${\mu}{\textrm}{m}$. When BaTiO$_3$is used as a single buffer layer, the grain size of YBCO is observed to be larger than that of YBCO/CeO$_2$by 200 times and the transition temperature of the film is enhanced to be about 84 K. CeO$_2$/BaTiO$_3$double buffer layer has been adopted to enhance the superconducting properties, which results in the enhancement of the critical temperature and the critical current density to be about 85 K and 8.4 $\times$ 10$^4$ A/cm$^2$ at 77 K, respectively mainly due to the enlargement of the grain size of YBCO film.ilm.

• 자원환경지질
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• 제11권4호
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• pp.169-182
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• 1978

The Weolagsan area consists of four units; (1) Low grade meta-sediments of the upper members of Ogcheon age unknown group such as Changri (mainly black slate and phyllitic rock), Majeonri (mainly alternation of slate, limestone and chert) and Hwanggangri Formation (pebble bearing phyllitic sediments); (2) Samtaesan Formation of Chosun System of Ordovician; (3) So called meta-volcanics and (4) Weolagsan Granite and its associations which intruded above mentioned meta-sediments and meta-volcanics. This study was focused to know the Woelagsan granite and its metasomatic effects to the country rocks petrographically and petrochemically. According to the field survey, microscopic work and some chemical analysis, the granite is a "normal granite" based on the Streckeisen's classification and belongs to a mass of the Central-zone younger group in Ogcheon geosynclinal belt. The granite metasomatized the country rocks along its northern contact zone. Zone of calcareous and cherty rocks (Majeonri formation) was silicified partly and skarned locally at the contact with the granite. The chemical analysis of the zone show no difinite variations in contents of $SiO_2$ and CaO with the distance from the granite. It seems to be indicated that the silicification of this part was not so metasomatized by the granite body, but thermally affected as much as to be partially remelted in the specific parts of the formations. Meta-volcanic rock zone was slightly chloritized near contact with the granite. Limestone of Samtaesan Formation was silicified and skarned along the contact zone by the granite body. The chemical analysis of the zone show some noticiable changes in compositions of $SiO_2$ and CaO with distance from the granite boundary. It can be imagined that the silicification of this zone was metasomatically originated by Woelagsan Granite. According to chemical analysis on several trace elements, the ratio of Zn/Cr and Ni/Cr are relatively higher than that of Cu/Cr in the above mentioned silicified zones. Generally the variation of these metal elements in the zones tend to be regular with distance from the granite body.

• 대한전기학회:학술대회논문집
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• 대한전기학회 1999년도 추계학술대회 논문집 학회본부 C
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• pp.873-875
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• 1999

We have fabricated good quality superconducting $YBa_{2}Cu_{3}O_{7-\delta}$ thin films on Hastelloy(Ni-Cr-Mo alloys) metallic substrate with $CeO_2$ and $BaTiO_3$ buffer layers in-situ by pulsed laser deposition in a multi-target processing chamber. We have chosen $CeO_2$ as a buffer layer which has cubic structure of $5.41{\AA}$ lattice parameter and only 0.2% of lattice mismatch with YBCO. $CeO_2$ layer may be helpful for power transmission due to its conducting property. In order to enhance the crystallization of YBCO films on metallic substrates. we deposited $CeO_2$ and $BaTiO_3$ buffer layers at various temperatures. The YBCO superconducting tape fabricated with $BaTiO_3$ and $CeO_2$ buffer layers shows 85K of transition temperature and about $8.4{\times}10^4A/cm^2$ of critical current density at 77K.

• 대한화학회지
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• 제13권2호
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• pp.137-140
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• 1969

This investigation was made to evaluate the corrosion inhibiting effects of urotropine for mild steel in HCl. 1) Formaldehyde produced by the decomposition of urotropine also showed positive inhibiting effects. 2) In the presence of the ions, such as $Cu^+$, $Cu^{++}$, $Fe^{+++}$, $SO_3^=$, $SO_4^=$, $NO_2^-$, $NO_3^-$, $Cr_2O_7^=$, the inhibiting capacity of the urotropine was decreased. Alkali and alkaline-earth metal ions had no effects but the halogen ions improved it. 3) From measurements of polarization curves, it was assumed that the anode reaction was more retarded by the urotropine and the halogen.

• 수산해양교육연구
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• 제19권1호
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• pp.1-7
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• 2007

The purpose of this study was to investigate geochemical characteristics of surface sediments in the Keum river estuary adjacent to coastal area. For this study we collected the 21 surface sediments samples. Mean size of surface samples was $3.24{\sim}6.65{\phi}$ on inner estuary and was $2.15{\sim}3.42{\phi}$ on outside estuary. Surface samples were composed of silt on inner estuary and were composed of sand which was more larger than $4{\phi}$ on outside estuary. Most major elements except CaO, $Na_2O$ showed good relationships between variation of contents and grain size. Contents of $Al_2O_3$, $Fe_2O_3$, MgO, $K_2O$, $TiO_2$, $P_2O_5$ and $M_nO$ were increased predominately owing to the variation of mean size of surface samples. Contents of Co, Cr, Cu, Li, Sr, Zn, La, Ce, Pb, Rb, Nd have a good relationships with grain size but Ba, Th, Sm have not. All of major and minor elements contents except $K_2O$ and Ba were less than world mean contents of shallow surface sediments but apprehend a high pollution possibility on silt sediments in the estuaries.

• 한국환경농학회지
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• 제19권1호
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• pp.51-57
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• 2000

단열이 되지 않은 소형 퇴비화용기를 이용하여 가정에서 발생되는 폐기물 중 종이류를 제외한 퇴비화 가능한 폐기물은 퇴비화하였다. 수분 조절제로서 가정에서 발생되는 폐 신문지를 사용하였다. 초기 퇴비화 혼합물질이 투입되기 시작하여 15주 후에 배출되었다. 실험 결과를 요약하면 다음과 같다 : 퇴비화용기가 단열재로 보온되지 않아 외부 온도의 영향을 크게 받았다. 따라서 퇴비화 후 건조물질 기준으로 분해 율은 $32.28{\sim}77.02%$로 외부 온도에 따라 차이가 현저하였다. 폐 신문지를 혼합하여 초기 수분을 $48.55{\sim}70.14%$로 조절하였음에도 배출된 퇴비의 수분 함량은 $62.38{\sim}87.03%$로 높았으며 pH는 $7.64{\sim}9.17$이었다. 배출된 퇴비 중 회분 및 총 질소 함량은 증가하였으나 $NO_3\;^--N$, $NO_2-N$, $NH_3-N$ 함량은 어떠한 경향을 보이지 않았다. 배출된 퇴비 중 중금속 및 비료성분의 함량은 초기 퇴비화 혼합물질보다 증가하였다. 수 분조절제로 폐 신문지를 1회 사용하였을 때 배출된 퇴비 중의 중금속 함량은 $Zn\;0.60{\sim}1.99mg/kg$, $Ph\;5.77{\sim}29.81mg/kg$, $Cd\;1.20{\sim}3.02mg/kg$, $Cr\;4.01{\sim}6.67mg/kg$, $Cu\;2.10{\sim}6.77mg/kg$, $As\;4.97{\sim}10.15mg/kg$, Hg ND이었으며 비료성분 함량은 $CaO\;0.08{\sim}1.91%$, $MgO\;0.46{\sim}2.80%$, $K_2O\;0.17{\sim}1.05%$, $P_2O_5\;0.96{\sim}3.33%$이었다. 그러나 배출된 건조 퇴비를 재사용하였을 때 배출된 퇴비 중의 중금속 함량은 $Zn\;5.04{\sim}5.77mg/kg$, $Pb\;64.42{\sim}68.62mg/kg$, $Cd\;6.07{\sim}6.29mg/kg$, $Cr\;14.40{\sim}17.08mg/kg$, $Cu\;6.77{\sim}15.44mg/kg$, $As\;10.43{\sim}17.50mg/kg$, Hg ND이었으며 비료성분 함량은 $CaO\;1.51{\sim}2.44%$, $MgO\;2.14{\sim}2.69%$, $K_2O\;2.15{\sim}2.71%$, $P_2O_5\;1.11{\sim}2.80%$이었다.

• 한국환경농학회지
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• 제15권3호
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• pp.282-288
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• 1996

가정에서 발생되는 음식쓰레기의 높은 수분함량 때문에 원활한 퇴비화가 어렵다. 따라서 본 논문은 가정 쓰레기 퇴비화 수분조절제로서 석탄회의 이용가능성을 알아보고자 하였다. 결과를 요약하면 아래와 같다. 1. 퇴비화기간동안 최고 상승온도는 봄철 $35^{\circ}C$, 여름철 $47^{\circ}C$ 그리고 겨울철 $43^{\circ}C$이었다. 2. 질량은 60일후 70.5% 감소되었으며, 부피는 평균 74.7% 감소되었다. 3. pH의 변화는 3계절 모두 비슷한 경향을 보였으며, 60일 후의 pH는 8.5 였다. 4. 수분함량은 퇴비화 초기에 감소 경향을 보인 후 점차 거의 일정하였다. 60일 후 퇴비의 수함량은 봄철 49.7%, 여름철 33.9%, 겨울철 56.5%였다. 회분함량은 퇴비기간동안은 큰 변화가 없었다. 5. 무기성분 함량은 $P_2O_5$ $0.06{\sim}4.03%$, CaO $0.01{\sim}2.87%$, MgO $0.18{\sim}1.43%$, $K_2O$ $0.39{\sim}2.03%$였다. 각종 중금속 함량은 Hg $ND{\sim}14.08{\mu}g/kg$, Cd $ND{\sim}0.80mg/kg$, Cu $4.99{\sim}28.95mg/kg$, Cr $ND{\sim}242.62mg/kg$, Pb $ND{\sim}20.24mg/kg$, Zn $ND{\sim}59.87mg/kg$이었다.

• 한국환경농학회지
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• 제15권2호
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• pp.179-187
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• 1996

실험실에서 주택용 소형 퇴비화용기로 사용 가능성이 확인된 이중 벽으로 만든 퇴비화용기를 단독주택의 가족이 4인인 한 가정에 설치하여 적용 가능성을 실험하였다. 그 결과를 요약하면 다음과 같다 : 1) 계절별 실험한 결과 퇴비 내에서 상승한 최고온도는 봄철 $31^{\circ}C$, 여름철 $36^{\circ}C$, 겨울철 $50^{\circ}C$였다. 2) 60일 후 생산된 퇴비의 pH는 겨울철 7.94, 봄철 8.21 그리고 여름철 8.29였다. 퇴비화기간의 경과에 따라 퇴비중 유기물함량은 감소 그리고 회분 함량은 증가하였음에도 불구하고 퇴비 중 각종 무기성분 및 중금속은 축적되지 않았다. 60일 후 회분함량은 겨울철 73.8%, 봄철 55.8% 그리고 여름철 57.0%였다. 질소함량은 0.2-5.8%의 범위였으며 겨울철에 가장 높았고 그리고 여름철에 가장 낮았다. 특히 높은 수분과 Cd의 함량은 퇴비화 가능한 가정쓰레기의 퇴비화에 문제점으로 지적되었다. 60일 후 계절 평균 약 58.5%의 무게가 감소하였다. 퇴비화과정 중 무기성분들의 함량범위는 3 계절 $P_2O_5\;1.50{\sim}4.41%$, $K_2O\;0.02{\sim}1.31%$, CaO $0.13{\sim}1.68%$, MgO $0.05{\sim}1.22%$였다. 또한 중금속성분들의 함량은 Zn $13{\sim}89mg/kg$, Cu $4{\sim}62mg/kg$, Cd $1{\sim}21mg/kg$, Pb $N.D.{\sim}97mg/kg$, Cr $N.D.{\sim}37mg/kg$, Hg $N.D.{\sim}1,38mg/kg$의 범위였다.

• 한국재료학회:학술대회논문집
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• 한국재료학회 2003년도 추계학술발표강연 및 논문개요집
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• pp.158-158
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• 2003

수평 전기로에서 CuGaTe2 다결정을 합성하여 HWE 방법으로 CuGaTe2 단결정 박막을 반절연성 GaAs(100) 위에 성장하였다. CuGaTe2 단결정 박막은 증발원과 기판의 온도를 각각 67$0^{\circ}C$, 41$0^{\circ}C$로 성장하였다. 이때 단결정 박막의 결정성이 10K에서 측정한 광발광 스펙트럼은 954.5nm (1.2989eV) 근처에서 exciton emission 스펙트럼이 가장 강하게 나타났으며, 또한 이중결정 X-선 요동곡선(DCRC)의 반폭치(FWHM)도 139arcsec로 가장 작게 측정되어 최적 성장 조건임을 알 수 있었다. Hall 효과는 van der Paw방법에 의해 측정되었으며, 온도에 의존하는 운반자 농도와 이동도는 293K에서 각각 8.72$\times$$10^{23}$개/㎥, 3.42$\times$$10^{-2}$$m^2$/V.s였다. 상온에서 CuGaTe2 단결정 박막의 광흡수 특성으로부터 에너지 띠간격이 1.22 eV였다 Band edge에 해당하는 광전도도peak의 온도 의존성은 Varshni 관계식으로 설명되었으며, Varshni 관계식의 상수값은 Eg(0) = 1.3982 eV, $\alpha$= 4.27$\times$$10^{-4}$ eV/K, $\beta$= 265.5 K로 주어졌다. CuGaTe2 단결정 박막의 광전류 단파장대 봉우리들로부터 10K에서 측정된 $\Delta$cr (crystal Field splitting)은 0.0791eV, $\Delta$s.o (spin orbit coupling)는 0.2463eV였다. 10K에서 광발광 봉우리의 919.8nm (1.3479eV)는 free exciton(Ex), 954.5nm (1.2989eV)는 donor-bound exciton 인 I2(DO,X)와 959.5nm (1.2921eV)는 acceptor-bound exciton 인 I1(AO,X) 이고, 964.6nm(1.2853eV)는 donor-acceptor pair(DAP) 발광, 1341.9nm (0.9239eV)는 self activated(SA)에 기인하는 광발광 봉우리로 고찰되었다.

• Journal of the korean society of oceanography
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• 제32권3호
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• pp.112-119
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• 1997

Coastal sediments collected near the Youngkwang Nuclear Power Plant were analysed for major(Al$_2$O$^_3$, Fe$^_2$O$^_3$, MgO, CaO, Na$^_2$O, K$^_2$O, TiO$^_2$, MnO), trace (Ba, Sr, V, Co, Cr, Cu, Ni, Zn, Pb) metal, and P$^_2$O$^_5$ contents. The composition of bulk metals from most stations fits within the range as those in the average crustal and sedimentary rocks, suggesting that the anthropogenic perturbation of these components is insignificant. The abundance and distribution of total contents for the majority of metals in the surface sediment could be explained by the grain size and were associated with mud (<63 ${\mu}$m) contents. However, distributions of Ca, K, Sr and Ba did not have any significant association with the sediment grain size. This may be due to the geochemical coherence among these metals in certain minerals abundant in coarse grained fractions. The distribution of Pb appears to be partly affected by the contribution from aerosol fallout. Using the R'-mode factor analysis, we show that the variance of the metal contents could be explained by four factors which account for 93.7% of the total variance. It appears that texturally controlled and/or sorting factors influenced by fine fraction are the most dominant factors which determine the relative abundance and distribution of metals in the study area.