• 전기화학회지
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• 제16권3호
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• pp.184-189
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• 2013

졸-겔법 및 졸-겔법과 연소법을 함께 사용한 하이브리드법으로 각각 얻어진 건식 젤을 열처리하여 $Ba_2SiO_4:Eu^{2+}$ ($B_2S:Eu^{2+}$) 분말을 합성하였으며, 이들 공정에 따른 구조 및 발광 특성 변화를 조사 하였다. Si 공급원으로서는 tetraethyl orthosilicate (TEOS)를 사용하였다. 졸-겔법에 의한 건식 젤로 하소 과정 없이 합성한 경우 TEOS 양의 변화에 따라서 상전이가 관찰되었으며, 1.2M TEOS에서 $B_2S:Eu^{2+}$ 단일상을 얻었을 수 있었다. 반면에 하소 과정을 거친 1.2M TEOS로 합성된 분말에서는 졸-겔법과 하이브리드법 모두 $B_2S:Eu^{2+}$와 미량의 $BaSiO_3:Eu^{2+}$ ($BS:Eu^{2+}$) 상이 혼재하는 분말을 얻을 수 있었으나, 이들 분말은 하소 과정 없이 합성된 것보다 발광특성이 약 두배 정도 우수하였다. 하이브리드법에 의한 $B_2S:Eu^{2+}$는 졸-겔법에 의한 것에 비하여 발광강도가 약간 떨어지나 공정 시간을 획기적으로 단축 시킬 수 있는 장점을 보이고 있었다. 1.1M TEOS로 하소 과정을 거쳐 하이브리드법으로 얻어진 분말은 $B_2S:Eu^{2+}$ 단일상으로 구성되어 있었으며, $Eu^{2+}$이온의 $4f^65d^1{\rightarrow}4f^7$ 전이에 의한 가장 강한 강도를 갖는 녹색 발광 (505 nm) 스펙트럼을 보이고 있었다.

• 한국정보디스플레이학회:학술대회논문집
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• 한국정보디스플레이학회 2009년도 9th International Meeting on Information Display
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• pp.121-124
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• 2009

We developed a panel of innovative solution-based approaches for synthesis of multicomponent sulfide phosphor materials. The application of these synthesis strategies allowed for preparation of high-purity and high-brightness $BaAl_2S_4:Eu$ and $Ba_2SiS_4:Eu$ phosphors and led to the discovery of new phosphors suitable for application in the LED-based lighting including $Sr_2ZnS_3:Eu$, $CaBaSiS_4:Eu$ and $(Ba,Sr)_2ZnS_3:Eu$.

• 한국정보디스플레이학회:학술대회논문집
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• 한국정보디스플레이학회 2009년도 9th International Meeting on Information Display
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• pp.243-245
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• 2009

The single phase $Ba_2SiS_4$ doped with $Eu^{2+}$ was successfully synthesized by direct sulfurization of an oxide precursor prepared by a spray drying method using a novel water soluble silicon compound, which remains soluble in a given aqueous solution. The intensity of the emission peak of thus obtained $Ba_2SiS_4:Eu^{2+}$ was 1.75 times larger than that of a sample prepared by a solid state reaction method, and it approached 106% compared to one of the best commercially available YAG:$Ce^{3+}$ phosphor.

• 한국세라믹학회지
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• 제44권3호
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• pp.147-151
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• 2007

An improvement for the efficiency of the $Sr_{2}SiO_{4}:Eu$ yellow phosphor under the $450{\sim}470\;nm$ excitation range have been achieved by adding the co-doping element ($Mg^{2+}\;and\;Ba^{2+}$) in the host. White LEDs were fabricated through an integration of an blue (InGaN) chip (${\lambda}_{cm}=450\;nm$) and a blend of two phosphors ($Mg^{2+},\;Ba^{2+}\;co-doped\;Sr_{2}SiO_{4}:Eu$ yellow phosphor+CaS:Eu red phosphor) in a single package. The InGaN-based two phosphor blends ($Mg^{2+},\;Ba^{2+}\;co-doped\;Sr_{2}SiO_{4}:Eu$ yellow phosphor+CaS:Eu red phosphor) LEDs showed three bands at 450 nm, 550 nm and 640 nm, respectively. The 450 nm emission band was due to a radiative recombination from an InGaN active layer. This 450 nm emission was used as an optical transition of the $Mg^{2+},\;Ba^{2+}\;co-doped\;Sr_{2}SiO_{4}:Eu$ yellow phosphor+CaS:Eu red phosphor. As a consequence of a preparation of white LEDs using the $Mg^{2+},\;Ba^{2+}\;co-doped\;Sr_{2}SiO_{4}:Eu$ yellow phosphor+CaS:Eu red phosphor yellow phosphor and CaS:Eu red phosphor, the highest luminescence efficiency was obtained at the 0.03 mol $Ba^{2+}$ concentration. At this time, the white LEDs showed the CCT (5300 K), CRI (89.9) and luminous efficacy (17.34 lm/W).

• 한국정보디스플레이학회:학술대회논문집
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• 한국정보디스플레이학회 2009년도 9th International Meeting on Information Display
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• pp.1274-1275
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• 2009

We report on preparation of $CaBaSiS_4:Eu^{2+}$ material by an advanced chemical solution method and fluorescent properties of the new material. The emission spectrum of $CaBaSiS_4:Eu^{2+}$ has the main peak centered at 598 nm, with the corresponding excitation maximum at around 420 nm. The strongest emission intensity of this material approached 96% compared to one of the best commercially available YAG:$Ce^{3+}$ phosphor.

• 한국재료학회지
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• 제12권9호
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• pp.735-739
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• 2002

$(Y,Gd)BO_3$: Eu, $Zn_2$$SiO_4$ : Mn and $BaMgAl_{10}$ $O_{17}$ : Eu phosphors used in PDP were continuously irradiated by vacuum ultra violet generated from the penning gas (96%Ar+4%Xe) discharge and then the change of emitting intensity with time was investigated. The brightness of these phosphors decreased exponentially with VUV excitation time. The experimental data showed that the degradation rate increased in the order of $Zn_2$$SiO_4$ : Mn>(Y,Gd)$BO_3$: Eu>$BaMgAl_{10}$ $O_{17}$ : Eu phosphor. This different degradation property of phosphors was interpreted in terms of brightness saturation and stability against VUV irradiation. It was found that the degradation property of $(Y,Gd)BO_3$ : Eu red phosphor synthesized by ultrasonic thermal spray was superior to commercial phosphor.

• Transactions on Electrical and Electronic Materials
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• 제15권2호
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• pp.66-68
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• 2014

Most commercial white LED lamps use blue chip coated with yellow emitting phosphor. The use of blue excitable red and green phosphors is expected to improve the CRI. Several phosphors, such as $SrGa_2S_4:Eu^{2+}$ and $(Sr,Ba)SiO_4:Eu^{2+}$, have been suggested in the past as green components. However, there are issues of the sensitivity and stability of such phosphors. Here, we describe gallium substituted $YAG:Ce^{3+}$ phosphor, as a green emitter. YAG structures are already accepted by the industry, for their stability and efficiency. LEDs with improved CRI could be fabricated by choosing $Y_3Al_4GaO_{12}:Ce^{3+}$ (green and yellow), and $SrS:Eu^{2+}$ (red) phosphors, along with blue chip. Also, the effect of a slight change in chip wavelength is studied, for two phosphor-coated w-LEDs. The reduction in particle size of the coated phosphors also gives improved w-LED characteristics.

• 자원환경지질
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• 제23권2호
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• pp.245-259
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• 1990

Petrochemical analyses of granitic rocks including trace element, REE and oxygen isotope were carried out to understand petrogenesis of plutonic rocks from the Chungju, Wolaksan and Jecheon granite batholiths, which might be related with tungsten-base metal-fluorite mineralization in the Hwanggangri metallogenic province. Different geochemical characteristics such as major and trace elements were found between Jurassic Daebo granitic rocks (Chungju, Jecheon, Wonju, and Boeun granitic rocks) and Cretaceous Bulgugsa granitic rocks (Wolaksan, Muamsa and Sokrisan granitic rocks). Cretaceous granitoids are characterized by high $SiO_2$and $K_2O$ contents and low $TiO_2$, $Al_2O_3$, MgO and CaO contents. They also have relatively high contents of trace elements(Zn, V, Co, Cr, Sr, and Ba) in comparison with the Jurassic granitoids. (Eu)/($Eu^*$) and $(La/Lu)_{CN}$ ratios of Jurassic plutons vary from 0.78 to 1.13 and from 26.02 to 30.5, respectively, while the ratios of Cretaceous ones range from 0.22 to 0.28 and from 4.42 to 14.2, respectively. The REE patterns of the Cretaceous and Jurassic granitic rocks have quite different Eu anomalies: large negative Eu anomaly in the former, and mild or absent Eu anomaly in the latter. The large Eu negative of Cretaceous granitic rocks are interpreted as a differentiated product of fractional crystallization of granitic magma deduced by Rayleigh fractionation model(Tsusue et al., 1987). Oxygen isotopic compositions of quartz for Daebo and Bulgugsa granitic rocks range from 9.98 to 10.51‰ and from 8.26 to 9.56‰, respectively. The Daebo granitic rocks enriched in $^{18}0$ suggest that the magma be undergone different partial melting processes from the Bulgugsa ones. Of the Bulgugsa granitoids, Wolaksan and Sokrisan mass have different contents of trace elements and ${\delta}\;^{18}0$ values of the silicate minerals, which indicate that they are not from the identical source of magma. Many mineral deposits are distributed in and/or near the Wolaksan and Muamsa granitic rocks, but a few mineral deposits are found in and near the Chungju and Jecheon granite batholiths. It might be depend on geochemisty of the related igneous rocks which have low contents of Ba, Sr, Co, V, Cr, Ni, Zn and high contents of Nb and Y, and on lithology of country rocks such as cabonate and noncarbonate rocks.

• Geosciences Journal
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• 제23권1호
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• pp.1-20
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• 2019

We present data from the Mesozoic Keumkang, Palbong, and Baekhwa granites in Garorim Bay, in the southwestern part of the Gyeonggi massif, South Korea. Using major and trace element concentrations, Sr-Nd-Pb isotopic compositions, and sensitive high-resolution ion microprobe (SHRIMP) zircon U-Pb ages, we aim to constrain the petrogenesis of the granites and explain their origin within a broader regional geological context. SHRIMP U-Pb zircon ages of $232.8{\pm}3.2$, $175.9{\pm}1.2$, and $176.8{\pm}9.8$ Ma were obtained from the Keumkang, Palbong and Baekhwa granites, respectively. The Late Triassic Keumkang granites belong to the shoshonite series and show an overall enrichment in large ion lithophile elements (LILE), a depletion in high field strength elements (HFSE) relative to primitive mantle, compared with neighboring elements in the primitive mantle-normalized incompatible trace element diagram with notable high Ba and Sr contents, and negligible Eu anomalies. The Keumkang granites are typified by highly radiogenic Sr and unradiogenic Nd and Pb isotopic compositions: $(^{87}Sr/^{86}Sr)_i=0.70931-0.70959$, $(^{143}Nd/^{144}Nd)_i=0.511472-0.511484$ [$({\varepsilon}_{Nd})_i=-17.0$ to -16.7], and $(^{206}Pb/^{204}Pb)=17.26-17.27$. The Middle Jurassic Palbong and Baekhwa granites belong to the medium- to high-K calc-alkaline series, and show LILE enrichment and HFSE depletion similar to the Keumkang granites, but exhibit significant negative anomalies in Ba, Sr, and Eu. Furthermore, they have elevated Y and Yb contents at any given $SiO_2$ content compared with other Jurassic granitoids from the Gyeonggi massif. The Palbong and Baekhwa granites have slightly less radiogenic Sr and more radiogenic Nd and Pb isotopic compositions [$(^{87}Sr/^{86}Sr)_i=0.70396-0.70908$, $(^{143}Nd/^{144}Nd)_i=0.511622-0.511660$, $({\varepsilon}_{Nd})_i=-15.4$ to -14.7, $(^{206}Pb/^{204}Pb)=17.56-17.76$] relative to the Keumkang granites. The Keumkang granites are considered to have formed in a post-collisional environment following the Permo-Triassic Songrim orogeny that records continent-continent collision between the North and South China blocks, and may have formed by fractional crystallization of metasomatized lithospheric mantle-derived mafic melts. The Palbong and Baekhwa granites may have been produced from a gabbroic assemblage at pressures of less than ~15 kbar, associated with subduction of the paleo-Pacific (Izanagi) plate at the Eurasian continental margin. Elevated ${\varepsilon}_{Nd}(t)$ values in the granitoids from the southwestern part of the Gyeonggi massif relative to those of the central and northern parts, together with the comparatively shallow depth of origin, imply the presence of an exotic block in the Korean lithosphere.

• 자원환경지질
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• 제46권2호
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• pp.179-198
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• 2013

신장 위구르 자치구 바이청현 보즈구얼 지역의 A형 화강암체는 타림지대의 북쪽 끝과 동서쪽 방향의 알칼리 관입암대에 접하여 위치해 있다. 이 화강암체는 추휘석(aegrine)이나 아페소나이트(arfvedsonite)-석영-알칼리장석 섬장암, 또는 아페소나이트-알칼리장석 화강암, 흑운모-알칼리장석 섬장암으로 구성되며, 주요광물로는 알바이트(albite), K-장석, 석영, 아페소나이트(arfvedsonite), 추휘석, 시데로필라이트(siderophyllite) 등이 있으며 부성분 광물로는 지르콘(zircon), 파이로클로르(pyrochlore), 토라이트(thorite), 형석, 모나자이트(monazite), 바스네사이트(bastnaesite), 제노타임(xenotime), 아스트로필라이트(astrophyllite) 등이 있다. 이 알칼리 화강암체는 67.32%의 평균값을 갖는 $SiO_2$를 포함하고 평균 11.14%의 높은 $Na_2O+K_2O$(9.85~11.87%) 조성을 보이며 이 중 $K_2O$는 평균 4.73%의 조성을 보인다. $K_2O/Na_2O$의 비는 0.31~0.96 사이이며 $Al_2O_3$는12.58%부터 15.44%사이로 포함되고 총 $FeO^T$함량은 2.35~5.65%이내이다. CaO, MgO, MnO, $TiO_2$의 함량은 낮은 것으로 관찰된다. 희토류원소의 총량은 평균 $77{\times}10^{-6}$으로 비교적 높게 나타나고 경희토원소는 농축되어 있지만 중희토원소는 Eu원소의 부(-)의 이상과 함께 상대적으로 결핍되는 특징을 가진다. 또한 알칼리 화강암체의 chondrite-normalized 희토류원소의 패턴은 오른쪽으로 기울어진 갈매기형태를 보인다. Zr는 평균 $594{\times}10^{-6}$의 함량을 보이며 Zr+Nb+Ce+Y는 평균 $1362{\times}10^{-6}$의 함량을 나타낸다. 또한 이 알칼리 화강암체는 높은 HFSE(Ga, Nb, Ta, Zr, Hf)함량과 낮은 LILE(Ba, K, Sr)함량을 보인다. Nb/Ta의 비는 평균 16.5이며 Zr/Hf의 비는 평균 36.80이다. 지르콘은 경희토원소에서 결핍되고 중희토원소에서 농축되어있다. 지르콘의 chondrite-normalized 희토류원소는 Eu원소의 강한 부(-)의 이상과 함께 왼쪽으로 기울어진 갈매기형태를 보인다. 보즈구얼지역의 A타입 화강암체는 A1타입의 화강암과 유사한 특징을 나타낸다. 화강암질 마그마의 평균온도는 $832{\sim}839^{\circ}C$이며 보즈구얼 지역의 A타입 화강암체는 지각과 맨틀의 혼합양상을 보이며 고온, 무수, 낮은 산소의 퓨개시티(fugacity) 환경을 가진 판 내부의 비조산대에서 생성되었을 가능성이 있다.