• 암석학회지
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• 제16권4호
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• pp.217-232
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• 2007

푸우오오 용암분출은 1983년에 분출이 시작된 이래 현재까지 활동하고 있으며, 다양한 성분 변화와 ($5.6{\sim}10.1wt.%$ MgO), 지표분출 면적을 가지는(${\sim}2km^3$) 하와이의 역사적인 분출 중에 하나이다(Garcia et al., 1999). 다년간에 걸쳐 하와이 분출에 대한 연구가 수행되어 왔으나, 최근 수년 이내에 분출된 푸우오오 용암의 지질학적인 특성에 대한 연구 결과의 부재와 푸우오오 분출 역사를 통한 하와이 마그마 분출과정의 특성을 파악하고자 시공간적으로 채취한 시료를 바탕으로 광물과 암석의 조직과 화학조성연구를 수행하였다. 박편 상에서 단사휘석이나 사장석 반정은 드물고 감람석이 대부분의 반정을 차지한다. 이것은 푸우오오 지역이 마그마 분화 초기단계에 머물러 있다는 것을 지시한다. MgO를 상대로 주원소에 대해 도시해 본 결과 MgO가 증가함에 따라 $TiO_2,\;Al_2O_3,\;Na_2O,\;SiO_2$는 감소하는 경향을 보인다. 미량원소의 경우 $K_2O$값에 대한 Zr, Y, Sr 그리고 V 도표에서 P18과 P19시료가 타 용암에 비해 진화가 더 진행된 영역에 도시되고 있다. 2003 년에서 2006년 분출년도 간에 높은 Ni 함량이 나타나는데, 이것은 동일 기원마그마의 유입에 의한 결과이다.

• 한국지구과학회지
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• 제28권3호
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• pp.324-342
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• 2007

제주도 동부 성산 일출봉 일대 현무암류에 대한 암석기재, 암석화학적 특징 및 마그마 성인에 대하여 연구하였다. 본 지역의 지질은 층서적으로 최하부에 표선리현무암이 놓이며, 그 위에 성산리현무암이 분포하는데, 이는 라필리스톤층 및 고토양층에 의해 하부용암류와 상부용암류로 구분된다. 본 지역에서 산출되는 용암류는 반정 광물의 종류 및 조직에 따라 크게 침상장석 감람석 현무암과 비현정질 현무암으로 구분할 수 있다. 본 지역의 화산암류는 TAS분류도에서 알칼리계열 현무암과 비알칼리계열 현무암으로 분류되며, 비알칼리 계열 현무암은 쏠리아이트암으로 분류된다. 쏠리아이트 현무암은 알칼리현무암에 비하여 $SiO_2,\;FeO^T$, CaO 함량이 높고, $TiO_2,\;K_2O,\;P_2O_5$ 함량과 다른 불호정성원소 함량의 낮은 값을 가지는 특징을 보인다. MgO 함량 변화에 따른 미량 원소 변화에서 호정성 미량 원소의 변화 경향은 대체로 정(+)의 상관 관계를 나타내고, Th을 마그마 분화 척도로 사용한 불호정성 미량 원소의 변화 경향도 정(+)의 상관 관계를 나타낸다. 암석화학적 고찰 결과는 본 지역의 암석이 동질기원 마그마 물질의 부분용융의 차이에 의해 생성되었음을 지시한다.

• Korean Chemical Engineering Research
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• 제46권1호
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• pp.131-136
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• 2008

용매 N-methyl-2-pyrrolidone(NMP)과 dimethyl acetamide(DMAc)를 각각 사용하고 물을 비용매로 사용하는 상반전 기법에 의해, 실리카($SiO_2$)와 티타니아($TiO_2$) 나노입자가 각각 충진된 poly(vinylidene fluoride-co-hexafluoropropylene) (PVdF-HFP) 고분자 전해질을 제조하고, 이를 고용량 양극재료인 $Li[Ni_{0.15}Co_{0.10}Li_{0.20}Mn_{0.55}]O_2$를 주성분으로 하는 양전극과 리튬금속 음전극 사이에 채용하는 리튬금속 고분자 2차전지를 제작하여 그 충방전 특성을 조사하였다. 고분자 전해질 제조에 사용한 용매에 상관없이 실리카 충진재의 함량이 40~50 wt%인 상반전막을 고분자 전해질로 적용하였을 때 가장 높은 방전용량(180 mAh/g)을 나타내었으며, 이 경우 대개 80 사이클까지 초기용량의 99% 정도의 지속성을 보이다가 그 이후 급격한 용량 감소를 보였다. 이 용량 감소는 상반전막이 보장하는 용량 유지능력이 더이상 발휘될 수 없는 상태로 고분자 전해질에 리튬 dendrite가 침적되었기 때문이라 생각된다.

• 자원환경지질
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• 제56권6호
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• pp.745-764
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• 2023

In the Republic of Congo, Banded iron formations (BIFs) occur in two areas: the Chaillu Massif and the Ivindo Basement Complex, which are segments of the Archean Congo craton outcropping in the northwestern and southwestern parts of the country. They show interesting potential with significant mineral resources reaching 2 Bt and grades up to 60% Fe. BIFs consist mostly of oxide-rich facies (hematite/magnetite), but carbonate-rich facies are also highlighted. They are found across the country within the similar geological sequences composed of amphibolites, gneisses and greenschists. The Post-Archean Australian Shale (PAAS)-normalized patterns of BIFs show enrichment in elements such as SiO₂, Fe₂O₃, CaO, P₂O₅, Cr, Cu, Zn, Nb, Hf, U and depletion in TiO₂, Al₂O₃, MgO, Na₂O, K₂O, Sc, Th, Ba, Zr, Rb, Ni, V. REE diagrams show slight light REEs (rare earth elements; LREEs) compared to heavy REEs (HREEs), and positive La and Eu anomalies. The lithological associations, as well as the very high (Eu/Eu^*)_SN ratios> 1.8 shown by the BIFs, suggest that they are related to Algoma-type BIFs. The positive correlations between Zr and TiO₂, Al₂O₃, Hf suggest that the contamination comes mainly from felsic rocks, while the absence of correlations between MgO and Cr, Ni argues for negligeable contributions from mafic sources. Pr/Pr^* vs. Ce/Ce^* diagram indicates that the Congolese BIFs were formed in basins with redox heterogeneity, which varies from suboxic to anoxic and from oxic to anoxic conditions. They were formed through hydrothermal vents in the seawater, with relatively low proportions of detrital inputs derived from igneous sources through continental weathering. Some Congolese BIFs show high contents in Cr, Ni and Cu, which suggest that iron (Fe) and silicon (Si) have been leached through hydrothermal processes associated with submarine volcanism. We discussed their tectonic setting and depositional environment and proposed that they were deposited in extensional back-arc basins, which also recorded hydrothermal vent fluids.

• 한국표면공학회지
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• 제49권6호
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• pp.530-538
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• 2016

There is a close relationship between the performance and the heat generation of the electronic device. Heat generation causes a significant degradation of the durability and/or efficiency of the device. It is necessary to have an effective method to release the generated heat. Based on demands of the printed circuit board (PCB) manufacturing, it is necessary to develop a robust and reliable plating technique for substrates with high thermal conductivity, such as alumina ($Al_2O_3$), aluminium nitride (AlN), and silicon nitride ($Si_3N_4$). In this study, the plating of metal layers on an insulating silicon nitride ($Si_3N_4$) ceramic substrate was developed. We formed a Pd-$TiO_2$ adhesion layer and used APTES(3-Aminopropyltriethoxysilane) to form OH groups on the surface and adhere the metal layer on the insulating $Si_3N_4$ substrate. We used an electroless Ni plating without sensitization/activation process, as Pd particles were nucleated on the $TiO_2$ layer. The electrical resistivity of Ni and Cu layers is $7.27{\times}10^{-5}$ and $1.32{\times}10^{-6}ohm-cm$ by 4 point prober, respectively. The adhesion strength is 2.506 N by scratch test.

• 한국분말야금학회:학술대회논문집
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• 한국분말야금학회 2002년도 추계학술강연 및 발표대회
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• pp.8-8
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• 2002

TiC core/(Ti,Mo)C rim structure in TiC-$Mo_2C$-Ni base cermet which is generally prepared by sintering below 145$0^{\circ}C$ had been believed to be generated by the solid diffusion of Mo atoms 1 into TiC grains (D. Moskowitz and M.Humenik, 1r.:1966). Afterward, it was clarified that the c core/rim structure is generated by solution/re-precipitation mechanism : (1) $Mo_2C$ grains and s small TiC grains dissolve into the Ni liquid, (2) the dissolved Mo, Ti and C atoms migrate to the s surface of TiC coarse grains, (3) the Mo, Ti and C precipitate on the surface of TiC coarse g grains and form (Ti,Mo)C solid solution rim, and (4) the Ostwald ripening (grain growth by s solution/re-precipitation mechanism) of TiC-core/(Ti,Mo)-rim grains continues, and thus the w width of (Ti,Mo)C rim (at the same time, the grain size) increases with sintering time, etc. ( (H.Suzuki, K.Hayashi and O.Terada: 1973). The TiC-core was found not to disappear even by s sintering at 190$0^{\circ}C$ (ibid.: 1974) Recently, FeSi core/$Fe_2Si_5$-rim structure in Fe-66.7at%Si thermoelectric aIloy was found to also h hardly shrink and disappear by long heating at an appropriate temperature (1999: M.Tajima and K K.hayashD. Then, the authors considered its cause, and clarified experimentaIly that the disappearance of FeSi-core/$Fe_2Ski_5$-rim structure could be attributed to the exhaustion of diffusion-contributable vacancies in core/rim structure (N.Taniguchi and K.Hayashi:2001). At p present, the authors and my coworker are investigating whether the non-disappearance of TiC c core can be explained also from the new hypothesis "Exhaustion of diffusion-contributable v vacancies in corelrim structure".ure".uot;.

• Journal of Magnetics
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• 제17권2호
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• pp.78-82
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• 2012

CoNiFe(CNF)/$BaTiO_3(BTO)$/CoNiFe(CNF) multilayered thin films were deposited on Pt/Ti/$SiO_2$/Si substrates by using pulsed laser deposition (PLD) system. We fabricated three different thin films of BTO, BTO/CNF and CNF/BTO/CNF for magneto-capacitor and studied their crystalline structure, surface and interface morphology, and magnetic and electrical properties. When three different structures of multilayered thin film were compared, magnetization of CNF/BTO/CNF thin films was decreased by magnetic and dielectric interaction. Also we confirmed that capacitance of CNF/BTO/CNF multilayered thin film was enhanced as being near tetragonal structure with increasing of c/a ratio because of atomic bonding at interface between BTO dielectric and CNF magnetic materials. Finally, we studied the change of the capacitance of CNF/BTO/CNF multilayered thin film with magnetic field for emergence of magnetocapacitance and suggested a possibility of enhanced capacitance.

• 한국진공학회:학술대회논문집
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• 한국진공학회 2013년도 제44회 동계 정기학술대회 초록집
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• pp.618-618
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• 2013

Graphene is only one atom thick planar sheet of sp2-bonded carbon atoms arranged in a honeycomb crystal lattice, which has flexible and transparent characteristics with extremely high mobility. These noteworthy properties of graphene have given various applicable opportunities as electrode and/or channel for various flexible devices via suitable physical and chemical modifications. In this work, for the development of all-graphene devices, we performed to synthesize alternately patterned structure of mono- and multi-layer graphene by using the patterned Ni film on Cu foil, having much different carbon solid solubilities. Depending on the process temperature, Ni film thickness, introducing occasion of methane and gas ratio of CH4/H2, the thickness and width of the multi-layer graphene were considerably changed, while the formation of monolayer graphene on just Cu foil was not seriously influenced. Based on the alternately patterned structure of mono- and multi-layer graphene as a channel and electrode, respectively, the flexible TFT (thin film transistor) on SiO2/Si substrate was fabricated by simple transfer and O2 plasma etching process, and the I-V characteristics were measured. As comparing the change of resistance for bending radius and the stability for a various number of repeated bending, we could confirm that multi-layer graphene electrode is better than Au/Ti electrode for flexible applications.

• 한국광물학회지
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• 제10권1호
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• pp.60-73
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• 1997

The talc of the Daeheung, Pyeongan, and Cheongdang (Shinyang) talc deposits in the Yesan-Gongju-Cheongyang area is a hydrothermal alteration product of serpentinite originated from ultramafic rocks. The mineral assemblages in alteration zones are: serpentine, serpentine-talc, talc, talc-chlorite, talc-phlogopite-chlorite, and talc-tremolite-chlorite. Chemical distributions in both the Al2O3-FeO-MgO system and the immobile elements suggest that the serpentine-talc and talc rocks are the reaction product of ultramafic rocks and silicic hydrothermal solution without addition of other granitic components, whereas chlorite-, phlogopite-, and tremolite-bearing rocks are the metasomatic alteration product of serpentinite by hydrothermal solution affected by granitic gneiss. Discontinuities in the immobile element ratios of mineral assemblages are due to changes in their mineralogy. The relative contents of Al2O3, TiO2, Zr in the talc-phlogopite-chlorite and talc-tremolite-chlorite rocks increase irregularly with increasing phlogopite, tremolite, and/or chlorite contents in contrast to other ore types. But the relative contents of Cr, Ni, and Co are uniform in all the mineral assemblages. Chemistry of each mineral assemblage formed by steatitization of serpentinite suggests that Cr, Co, Ni, MgO, and Fe2O3 are relatively immobile during the alteration, whereas SiO2, Al2O3, CaO, and K2O are highly increased. The contents of chlorite, phlogopite, and tremolite in each mineral assemblage might be controlled by addition of Al2O3, K2O, and CaO, respectively. The high contents of other elements than immobile elements in the altered rocks as compared with unaltered rocks indicate that a large amount of elements were introduced from hydrothermal solution up to about 8∼41% in total mass showing maximum value in the talc-phlogopite-chlorite rock.

• 자원환경지질
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• 제56권6호
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• pp.799-816
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• 2023

Mineralogical and geochemical studies of shales within the Lower Anambra Basin was conducted to unravel the depositional environment, provenance, maturity, paleo-weathering conditions, and tectonic settings. Mineralogical studies conducted using X-ray diffraction analysis revealed that the samples were composed of kaolinite, montmorillonite, chlorite, and illite. KaolinIite is the dominant mineral, constituting approximately 41.5% of the bulk composition, whereas the non-clay minerals are quartz, ilmenite, and sillimanite. Geochemical analysis showed a predominance of SiO₂, Al₂O₃, and Fe₂O₃ contents of the shale samples with mean values of 52.29%, 14.09%, and 6.15% for Imo Shale (IS); 52.31%, 16.70%, and 7.39% for Mamu Shale (MS); 43.21%, 21.33%, and 10.36% for Enugu Shale (ES); 53.35%, 15.64%, and 7.17% for Nkporo Shale (NS); and 51.24%, 17.25%, and 7.78% for Agwu Shale (AS). However, the shales were depleted in Na₂O, MgO, K₂O, MnO, TiO₂, CaO, and P₂O₅. The trace element ratios of Ni/Co and Cu/Zn of the shale suggest an oxic depositional environment. The average SiO₂ vs. Al₂O₃ ratio of the shales indicated textural maturity. Compared to the PAAS standard, the shales plot below the PAAS value of 0.85, suggesting a high degree of maturity and intensive chemical weathering, further confirmed on a CIA vs. PIA plot. On log (K₂O/Na₂O) against SiO₂ and tectonic setting discriminant function diagrams, the shales plot mostly in the field of passive continental margin tectonic setting. The discriminant function diagrams as well as Al₂O₃/TiO₂ ratio of the shales showed that they were derived from a mixed source (mafic and intermediate igneous rocks).