• 자원환경지질
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• 제30권1호
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• pp.35-49
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• 1997

The coal formation of the Deokpyeong area are interbedded along metapelites of the Ogcheon Supergroup, which are composed mainly of graphite, quartz, muscovite and associated with small amounts of biotite, chlorite, pyrite and barite. The ratios of $SiO_2/Al_2O_3$, $Al_2O_3/Na_2O$ and $K_2O/Na_2O$ of the coaly metapelite are variable and wide range from 1.80 to 10.21, from 27.8 to 388.8 and from 7.6 to 61.8, respectively. These coal formation were deposited in basin of marine environments, and the REE of these rocks are not influenced with metamorphism and hydrothermal alterations on the basis of $Al_2O_3$ versus La, La against Ce, the ratios of La/Ce (0.19 to 0.99) and Th/U (0.02 to 4.75). These rocks also show much variation in $La_N/Yb_N$ (1.19 to 22.89), Th/Yb (0.14 to 21.43) and La/Th (0.44 to 13.67), and their origin is explained by derivation from a mixture of sedimentary and igneous rocks. The wide range in trace and REE element characteristics as Co/Th (0.12 to 2.78), La/Sc (0.33 to 10.18), Sc/Th (0.57 to 5.73), V/Ni (8 to 2347), Cr/V (0.02 to 0.67) and Ni/Co (1.56 to 32.95) of these coaly metapelites argues for inefficient mixing of the various source lithologies during sedimentation. Deep to pale green barium-vanadium muscovites (vanadium-oellacherite) have been found in this coal formations. Modes of occurrence and grain size of muscovite are heterogeneous, but most of the barium and vanadium-bearing muscovites occur along the boundaries between graphite and quartz grains, ranging from 200 to $350{\mu}m$ in length and from 40 to $60{\mu}m$ in width. Results of X-ray diffraction data of the minerals characterized to be monoclinic system with $a=5.249{\AA}$, $b=8.939{\AA}$, $c=20.924{\AA}$ and ${\beta}=95.894^{\circ}$. Representative chemical formula of the muscovite was $(Na_{0.09}K_{1.44}Ba_{0.46})(Al_{2.75}Ti_{0.07}V_{0.56}Fe_{0.08}Mg_{0.50})(Si_{6.12}Al_{1.88})O_{22}$. The V possibly substitute octahedral Al, and the Ba is coupled substitution of $K^+Si^{4+}=Ba^{2+}Na^+Ca^{2+}$, which compositional ranges of V and Ba are from 0.42 to 0.69 and from 0.34 to 0.56 based on $O_{22}$, respectively. Formation mechanism of the barium-vanadium muscovites in the coaly metapelite is shown that the formed by high pressure and temperature from regional metamorphism origanated during diagenesis at the interface between a basinal brine and organic matter.

• 폴리머
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• 제32권3호
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• pp.263-269
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• 2008

키토산에 기초한 소수성 항암제의 전달체를 개발하기 위하여, 젖산염 키토산을 소수성기로써 담즙산 중의 하나인 리소콜릭산(lithocholic acid, LA)을 이용하여 화학적으로 개질하였다. LA가 결합된 키토산 나노입자(COS-LA)의 물리화학적 특성을 $^1H$-NMR, dynamic light scattering(DLS) 그리고 spectrofluorophotometer를 이용하여 조사하였다. 항암제로써 파클리탁셀(paclitaxel)이 봉입된 CLs-Tx(COS-LA-paclitaxel) 나노입자는 투석 방법을 이용하여 제조되었고 HPLC를 통하여 약물의 봉입량을 측정하였다. DLS를 이용하여 측정한 파클리탁셀이 봉입된 나노입자의 크기는 약 300 nm를 나타내었다. 또한 임계미셀형성(CMC) 농도는 LA의 치환도에 의존한다는 것을 확인하였다. 이상의 결과로부터 본 연구에서 제조한 LA가 결합된 젖산염 키토산이 파클리탁셀 전달체로서 매우 높은 응용 가능성을 나타내고 있음을 확인하였다.

• International Journal of Internet, Broadcasting and Communication
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• 제7권1호
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• pp.75-92
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• 2015

This paper presents the application of the bond valence method to estimate the valence charge distribution in several perovskite systems: $La_{{\tilde{1}}x}Pb_xMnO_3$ (x=0.1-0.5), $La_{0.6}Sr_{0.{\tilde{4}}x}Ti_xMnO_3$ (x=0.0-0.25) and $La_{{\tilde{1}}x}Sr_xCoO_3$ (x=0.1-0.5); the reviewing of their crystal structures is also incorporated. The results showed the failure of the elastic bonding mechanism in all studied systems and revealed the general deficit of the valence charge in their unit cells. This valence deficit was not associated with the structural defects and was not equally localized in all coordination spheres. As the content of substitution increased, the charge deficit declined systematically from balanced level, signifying the transfer of valence charge from the ${\tilde{B}}O_6$ to ${\tilde{A}}O_{12}$ spheres. This transfer depended on the valence deviation of spheres and the average reached near 2 electron per unit cell. The possible impact of the limitted accuracy of the available structural data on the bond valence results has also been considered.

• 한국세라믹학회지
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• 제52권5호
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• pp.344-349
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• 2015

An interconnect is the key component of solid oxide fuel cells that electrically connects unit cells and separates fuel from oxidant in the adjoining cells. To improve their surface stability in high-temperature oxidizing environments, metallic interconnects are usually coated with conductive oxides. In this study, lanthanum nickelates ($LaNiO_3$) with a perovskite structure are synthesized and applied as protective coatings on a metallic interconnect (Crofer 22 APU). The partial substitution of Co, Cu, and Fe for Ni improves electrical conductivity as well as thermal expansion match with the Crofer interconnect. The protective perovskite layers are fabricated on the interconnects by a slurry coating process combined with optimized heat-treatment. The perovskite-coated interconnects show area-specific resistances as low as $16.5-37.5m{\Omega}{\cdot}cm^2$ at $800^{\circ}C$.

• 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.

• 대한화학회지
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• 제24권1호
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• pp.1-7
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• 1980

메탄올, 에탄올 및 에탄올-물 혼합용매중에서 메틸클로로휘메이트, 메틸티올클로로휘메이트, 메틸티오노클로로휘메이트 및 메틸디티오클로로휘메이트의 가용매분해반응에 대한 속도상수를 전기전도도법으로 구하고 활성화 파라미터를 계산하였다. 결과로 메틸클로로휘메이트는 항상 $S_N2$ 메카니즘으로 반응하며, 가수분해 순위는 $CH_3S(CS)Cl>CH_3S(CO)Cl>CH_3O(CS)Cl>CH_3O(CO)Cl$ 로 $S_N1$ 반응성이 감소하고, 메탄올에서는 $CH_3S(CS)Cl$은 $S_N1$으로, 기타는 $S_N2$로 반응하고, 에탄올에서는 모두 $S_N2$로 반응하나 아직도 메틸클로로디티오휘메이트는 $S_N1$ 반응성이 어느정도 작용함을 알았다. 또한 에탄올-물 혼합용매에서 물함량이 큰 부분에서는 티오치환체의 $S_N1$ 반응성이 증가하며 메틸클로로디티오휘메이트는 $S_N1$으로 반응함을 알았다. 에탄올-물 혼합용매중에서 $S_N1$ 반응성의 순위는 가수분해속도의 순위와 같았다.

• 한국광물학회지
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• 제5권2호
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• pp.109-121
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• 1992

본 연구는 토파즈의 인공착색 처리 방법을 설정하기 위하여 브라질, 중국, 인도, 나이지리아, 스리랑카 등 5개국에서 산출된 토파즈를 대상으로, 전자현미분석(EPMA), 중성자활성분석(NAA), X선 회절분석, 라만 분광분석, 주사현미경(SEM), 부식시험, 굴절률측정, 비중측정, 유체 포유물 관찰 등의 실험을 실시하여 광물학적, 화학적 특성에 관한 연구를 수행하였다. 연구 결과 토파즈는 산지에 따라 화학적, 구조적 및 물리적 특성의 차이를 나타내었으며 특히, F와 OH 고용체 함량의 차이는 물리적, 구조적 특성과 밀접한 관련성이 있음이 확인되었다. F에 대한 OH로 치환정도가 가장 높은 인도산 토파즈는 굴절률, 단위포상수 b, 단위포 체적 및 ${\Delta}021$값이 가장 크고, 비중값은 가장 작으며 스리랑카산, 중국산, 브라질산, 나이지리아산순으로 F에 대한 OH로 치환 정도가 낮다. F에 대한 OH로 치환정도가 가장 낮은 나이지리아산 토파즈는 굴절률, 단위포상수 b, 단위포 체적 및 ${\Delta}021$값이 가장 작고, 비중값은 가장 크다. 토파즈내에 함유되는 미량원소종은 Na, Fe, Br, Co, Ce, La, Sm, Th, Au, Sc, Cr 등이며 이러한 미량원소의 정성정량적 특성은 물리적 특성에는 거의 영향을 미치지 않았다. 라만 분광분석 결과 토파즈의 피크는 산지에 따라 강도의 차이를 나타내었으며 브라질산과 인도산은 455∼458($cm^{-1}$)근처의 피크, 중국산은 282∼284($cm^{-1}$) 근처의 피크가 나타나지 않았다. 산지에 따른 결정구조결함 특성은 주로 point-bottom pit의 negative crystal defect(인도산, 나이지리아산)와 curl-bottom pit의 net work defect(브라질산, 중국산)로 구분되며, 결정내에 발달하는 미세한 균열을 따라 형성된 선결함 양상(linear defect)을 보여준다. 유체 포유물의 특징은 브라질산이 액상 $CO_2$를 가지는 III형이고, 중국산에는 유체 포유물이 거의 관찰되지 않으며 단지 $10{\mu}m$이하의 매우 작은 크기인 초생포유물의 극소량 존재한다. 인도산은 기체가 풍부한 II형이고, 나이지리아산은 암염, 실바이트 등의 고체 포유물을 함유하는 IV형이며 스리랑카산은 거의 대부분의 유체 포유물이 2차 생성의 I형이 주로 형성되어 있다. 본 연구의 결과는 광물학적 특성의 차이를 갖는 산지별 토파즈의 인공착색을 위한 처리 방법을 설정하는 유용한 기초 자료로 이용될 수 있을 것이다.