• Proceedings of the Korean Vacuum Society Conference
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• 2013.08a
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• pp.172-172
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• 2013

최근에 디스프로슘 이온이 도핑된 형광체의 백색 발광 현상 때문에 백색 발광 소재의 제조에 관한 연구가 상당한 관심을 끌고 있다. 본 연구에서는 $Eu^{3+}$와 $Dy^{3+}$ 이온의 몰 비를 변화시키면서 $BaNb_2O_6:RE^{3+}$ (RE=Eu, Dy) 형광체 분말을 합성한 결과를 보고한다. 특히 활성제 이온인 $Eu^{3+}$와 $Dy^{3+}$ 이온의 몰 비에 따른 $BaNb_2O_6$ 형광체 분말의 결정 구조, 입자의 모양과 크기, 흡광과 발광 스펙트럼의 변화를 관측하였고, 최적의 합성 조건을 제시하고자 한다. 파장 393 nm로 여기 시킨 $Dy^{3+}$ 이온의 몰 비에 따른 $BaNb_2O_6$ 형광체 분말의 발광 스펙트럼은 580 nm에 주 피크를 갖는 황색 스펙트럼이 관측되었다. 이 발광 신호는 $^4F_{9/2}-^6H_{13/2}$ 전이 신호이다. $Dy^{3+}$ 이온의 몰 비가 0 mol인 경우에는 발광 신호가 검출되지 않았다. $Dy^{3+}$ 이온의 몰 비가 0.10 mol일 때 발광 피크의 세기는 최대이었으며, $Dy^{3+}$ 이온의 몰 비가 더욱 증가함에 따라 발광 스펙트럼의 세기는 계속 증가하지 않고 갑자기 감소하기 시작하였다. 이것은 $Dy^{3+}$ 이온의 몰 비가 임계값을 초과하여 더욱 증가하면 모체 격자들 사이에 치환 고용되어 있는 $Dy^{3+}$ 이온들 사이의 거리가 더욱 가까워져서 $Dy^{3+}$ 이온들이 서로 용이하게 결합함으로써 내부 산란에 의하여 발광의 세기가 감소함을 의미한다. 흡광 스펙트럼의 경우에, $Dy^{3+}$ 이온의 몰 비가 0.01 mol일때 형광체 분말은 두 종류의 흡광 스펙트럼을 나타내었다. 첫째는 $Dy^{3+}$ 양이온과 $O^{2-}$ 음이온들 사이에 발생한 전하 전달 밴드에 의해 발생하는 310 nm를 정점으로 하여 280~340 nm 영역에 걸쳐서 광범위하게 분포하는 흡광 신호가 관측되었으며, 둘째는 $Dy^{3+}$ 이온의 $4f^9$ 전자 배열 내에서 발생하는 4f-4f 전이 신호로서, 이것은 350~500 nm 영역에 걸쳐서 비교적 밴드폭이 좁은 다수의 흡광 신호가 나타났다. 본 실험에서는 다섯 개의 피크를 갖는 흡광 신호가 검출되었는데, 이중에서 제일 강한 주 피크인 393 nm의 흡수 파장은 모체 격자 내에 있는 $Dy^{3+}$ 이온의 바닥 상태인 $^6H_{15/2}$ 준위에서 여기 상태인 $^4F_{7/2}$ 인 에너지 준위로 전이하면서 발생한 신호이며, 이에 비하여 상대적으로 흡광 세기가 약한 370, 432, 458, 370 nm의 흡수 파장이 관측되었다.

• The Journal of the Petrological Society of Korea
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• v.26 no.3
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• pp.271-280
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• 2017

The Dongcheondong granite is alkali feldspar granite in Dongcheondong, Gyeongju. The granite is coarse grained and consists of alkali feldspar, quartz, amphibole, and biotite. Alkali feldspar is perthitic orthoclase and quartz often shows undulatory extinction. Plagioclase often shows albite twins, and biotite and amphibole emplace as interstitial minerals. The Dongcheondong granite is plotted in A-type area having high ($Na_2O+K_2O)/Al_2O_3$ and low (MgO+CaO)/FeOT ratio. The Dongcheondong A-type granite has higher $SiO_2$, $Na_2O$, $K_2O$, Zr, Y, and REE contents (except for Eu) and lower $TiO_2$, $Al_2O_3$, CaO, MgO, Sr, Ba, and Eu contents than I-type granites in Gyeongsang Basin. These results show that the geochemical characteristics of the Dongcheondong A-type granite are distinguished from I-type granite in Gyeongsang Basin. A-type granite in the Dongcheondong is thought to has been generated by partial melting of I-type tonalite or granodiorite.

• Journal of the Mineralogical Society of Korea
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• v.19 no.2 s.48
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• pp.99-109
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• 2006

Igneous rocks occurring in the northwesern part of Keumsan area, Chungcheongnam-do were studied petrogeochemically. The geology of this area is composed mainly of the Precambrian biotite gneiss, age-unknown Ogchon supergroup, Jurassic biotite granite, and Cretaceous volcanic rocks, pink feldspar granite and quartz porphyry. The biotite granite is gradually changes to leucocratic nature by going from center to periphery of the rock mass. It shows variation, with distance from the center, in chemical components: $SiO_2,\;Na_2O\;and\;K_2O$ increase, whereas $Fe_2O_3,\;CaO,\;P_2O_5,\;MgO,\;and\;TiO_2$ decrease. Based on geochemical data, the biotite granite and quartz porphyry belong to subalkaline series and I-type. They show calc-alkaline differentiation trend. The biotite granite shows little negative Eu-anomaly pattern, whereas quartz porphyry show marked negative Eu-anomaly pattern, indicating that quartz porphyry was evolved further, when compared with biotite granite.

• Bulletin of the Korean Chemical Society
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• v.34 no.12
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• pp.3609-3614
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• 2013

Orthorhombic and hexagonal lanthanum(III) hydroxycarbonate ($LaCO_3OH$) and $Ln^{3+}$-doped $LaCO_3OH$ ($LaCO_3OH:Ln^{3+}$, where Ln = Ce, Eu, Tb, and Ho) powders were prepared by a hydrothermal reaction under ambient pressure and characterized by thermogravimetry, powder X-ray diffraction, infrared and luminescence spectroscopy, and field-emission scanning electron microscopy. The polymorph of $LaCO_3OH$ depended on the reaction temperature, inorganic salt additive, species of $Ln^{3+}$ dopant, and solvent. The calcination of orthorhombic $LaCO_3OH:Ln^{3+}$ (2 mol %) powers at $600^{\circ}C$ yielded a mixture of hexagonal and monoclinic $La_2O_2CO_3:Ln^{3+}$ powders. The relative quantity of the latter increased with decreasing ionic radius of the $Ln^{3+}$ dopant ion and increasing doping concentrations. On the other hand, the calcination of hexagonal $LaCO_3OH:Ln^{3+}$ (2 mol %) powders at $600^{\circ}C$ resulted in a pure hexagonal $La_2O_2CO_3:Ln^{3+}$ powder, regardless of the species of $Ln^{3+}$ ions (Ln = Ce, Eu, and Tb). The luminescence spectra of $LaCO_3OH:Ln^{3+}$ and $La_2O_2CO_3:Ln^{3+}$ were measured to examine the effect of their polymorph on the spectra.

• Proceedings of the Korean Institute of Electrical and Electronic Material Engineers Conference
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• 2009.11a
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• pp.173-173
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• 2009

높은 휘도를 갖는 $Eu^{2+}$가 도핑된 $Sr_3MgSi_2O_8$ 형광체는 고상반응법을 사용하여 합성하였다. 몰 비에 따른 조성을 정밀전자저울을 사용 무게를 칭량하여 에탄올을 용매로 하여 혼합, 건조 후 하소 온도는 $1000^{\circ}C$, 합성 온도는 $1200^{\circ}C$에서 $1400^{\circ}C$까지 $H_2$ 5% Ar 95% 환원분위기에서 소성 온도 별 결정상을 관찰하였고, 그 형태에 따라서는 Powder상태일 때와 Powder를 Press하여 bulk상태로써의 결정상의 변화를 연구하였다. 그 결과 분말상태와 성형을 가한 pellet의 두 가지 형태로 합성하여 비교한 결과 성형공정을 거친 시료의 경우가 분말 상태일 때 보다 좋지 못한 결정상이 관찰되었다. $Sr_3MgSi_2O_8$의 미세구조는 SEM으로 관찰하였다.

• Korean Journal of Materials Research
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• v.16 no.3
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• pp.145-150
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• 2006

Various colors of light emitting diodes(LED) and four-band white light sources are obtained using a violet LED and various phosphor films. $BaMg_2Al_{16}O_{27}:Eu\;(blue),\;SrGa_2S_4:Eu\;(green),\;and\;Eu(TTA)_3(PTA)$ (red) phosphors are dispersed in poly-vinyl-alcohol aqueous solutions, and phosphor films are prepared by coating the suspensions to PET film. The narrow band emission of $Eu(TTA)_3(PTA)$ phosphor has excellent red luminescent property for four-band white light excited by the violet LED.

• Economic and Environmental Geology
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• v.31 no.5
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• pp.399-413
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• 1998

Daegang granite is located around the Namwon-gun, Cheolabuk-do, and is an elongate stock $(80 km^{2})$ in the NNE-SSW direction. Daegang granite has the very same mineralogical and geochemical characteristics as those of the typical A-type granites; (1) it is a one feldspar hypersolvus granite, and is classified as an alkali feldspar granite in the lUGS scheme, (2) has small amounts of Fe-rich biotite (annite) and alkali amphibole (ribeckite) that are late in the crystallization sequence of the granitic magma, (3) always contains opaque oxides, fluorite and zircon, (4) shows high and quite homogeneous $SiO_2$, content (mostly 72~77 wt.%) and $(Na_{2}O+K_{2}O)/Al_{2}O_{3}$ ratio (0.90~0.98), (5) contains high Ga, lOOOO*Ga/Ai, $K_{2}O+Na_{2}O$, $(K_{2}O+Na_{2}O)/CaO$, $K_{2}O/MgO$, FeO/MgO, agpaitic index, Zr, Nb, Ce, Y, Zn value or ratio that resemble to those of the Australian A-type granites (Whalen et al., 1987), and (6) has enriched LREE and HREE that show flat variation pattern with slightly depleted in HREE and profound Eu anomalies (Eu/Eu*=0.04~0.l4). In the tectonic discrimination diagrams of Pearce et al. (1984) and Eby (1992), Daegang granite is classified as a within plate granite and $A_{2}-type$.

• Bulletin of the Korean Chemical Society
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• v.31 no.5
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• pp.1387-1388
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• 2010

• Journal of the Korean earth science society
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• v.27 no.1
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• pp.49-60
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• 2006

The purpose of this study is to investigate geochemical characteristics for stream sediments in the Naju area. We collected 139 stream sediments samples from primary channels. Samples were dried slowly in the laboratory and chemical analysis was carried out using XRF. ICP-AES and NAA. In order to investigate geochemical characteristics, the geological groups categorized into granitic gneiss area, schist area, granite area, arenaceous rock area, tuff area, andesite area, and rhyolite area. Average contents of major elements for geological groups are $SiO_2\;58.37{\sim}66.06wt.%,\;Al_2O_3\;13.98{\sim}18.41wt.%,\;Fe_2O_3\;4.09{\sim}6.10wt.%,\;CaO\;0.54{\sim}1.33wt.%,\;MgO\;0.86{\sim}1.34wt.%,\;K_2O\;2.38{\sim}4.01wt.%,\;Na_2O\;0.90{\sim}1.32wt.%,\;TiO_2\;0.82{\sim}1.03wt.%,\;MnO\;0.09{\sim}0.15wt.%,\;P_2O_5\;0.11{\sim}0.18wt.%$. According to the comparison of average contents of major elements, $Al_2O_3\;and\;K_2O$ are higher in granitic gneiss area, $Fe_2O_3,\;CaO,\;P_2O_5$ are higher in tuff area, MgO and $TiO_2$ are higher in andesite area, $Na_2O_$ is higher in rhyolite area, $SiO_2$, and MnO are higher in arenaceous rock area. Average contents of minor and rare earth elements for geological groups are $Ba\;1278{\sim}1469ppm,\;Be\;1.1{\sim}1.5ppm,\;Cu\;18{\sim}25ppm,\;Nb\;25{\sim}37ppm,\;Ni\;16{\sim}25ppm,\;Pb\;21{\sim}28ppm,\;Sr\;83{\sim}155ppm,\;V\;64{\sim}98ppm,\;Zr\;83{\sim}146ppm,\;Li\;32{\sim}45ppm,\;Co\;7.2{\sim}12.7ppm,\;Cr\;37{\sim}76ppm,\;Cs\;4.8{\sim}9.1ppm,\;Hf\;7.5{\sim}25ppm,\;Rb\;88{\sim}178ppm,\;Sc\;7.7{\sim}12.6ppm,\;Zn\;83{\sim}143ppm,\;Pa\;11.3{\sim}37ppm,\;Ce\;69{\sim}206ppm,\;Eu\;1.1{\sim}1.5ppm,\;Yb\;1.8{\sim}4.4ppm$. According to the comparison of average contents of minor and rare earth elements for geological groups, Pb, Li, Cs, Hf, Rb, Sb, Pa, Ce, Eu, and Yb are higher in granitic gneiss area; Ba, Co, and Cr in schist area; Nb, Ni, and Zr in arenaceous rock area; Sr in tuff area: and Be, Cu, V, Sc, and Zn are such in andesite area.

• Proceedings of the Korean Vacuum Society Conference
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• 2014.02a
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• pp.435-435
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• 2014

Eu(III)-doped Y2O3 nanorods were deposited onto a Si substrate using electrostatic spray system. The photoluminescence imaging profiles were compared between the electrospray film and powder form. Using electrostatic spraying technique is very advantageous to generate a uniform monolayer film without much clustering of nanorods. Strong emission peaks were observed between 580 and 730 nm in response to an indirect excitation transition. Our results indicate that the electrospray technique could be very useful for generating thin films for displays and sensors.