• 한국정보디스플레이학회:학술대회논문집
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• 한국정보디스플레이학회 2002년도 International Meeting on Information Display
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• pp.807-810
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• 2002

$GdPO_4$:Tb phosphor particles with spherical shape and high photoluminescence were prepared by spray pyrolysis. The brightness of prepared $GdPO_4$:Tb under the vacuum ultraviolet(VUV) illumination was comparable with that of the commercial $Zn_2SiO_4$:Mn phosphor particles. The photoluminescence spectra of $GdPO_4$:Tb phosphor particles had maximum peak at 547 nm, and the sharp peaks at 480 nm, 580 nm, and 620 nm. The spherical morphology of prepared $GdPO_4$:Tb particles was completely maintained even after the posttreatment up to 1100 $^{\circ}C$. When the posttreatment temperature was over 1100 $^{\circ}C$, the particles did not have the spherical shape anymore. The average particle size of $GdPO_4$:Tb phosphor particles prepared by using $(NH_4)_2HPO_4$ was changed from 0.5 to 1.9 ${\mu}m$ and its effect on the PL intensity was investigated. It was found that the optimized $GdPO_4$:Tb particles have a good excitation spectrum comparable to that of the commercial $Zn_2SiO_4$:Mn phosphor particles under the VUV illumination from 140 to 220 nm. We concluded that the $GdPO_4$:Tb phosphor particles with spherical shape prepared by spray pyrolysis is a promising candidate for a green-emitting PDP phosphor.

• 한국재료학회지
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• 제31권12호
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• pp.677-681
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• 2021

The Mn-Zn ferrite powders were prepared by high energy ball milling, then compacted and sintered at various temperatures to assess their sintering behavior and magnetic properties. The initial ferrite powders were spherical in shape with the size of approximately 70 ㎛. After 3 h of ball milling at 300 rpm, aggregated powders ~230 nm in size and composed of ~15 nm nanoparticles were formed. The milled powders had a density of ~70 % when compacted at 490 MPa for 3 min. In the samples subsequently sintered at 1,273 K ~ 1,673 K for 3 h, the MnZnFe₂O₄ phase was detected. The density of the sintered samples had a tendency to increase with increasing sintering temperature up to 1,473 K, which produced the highest density of 98 %. On the other hand, the sample sintered at 1,373 K had the highest micro-hardness of approximately 610 Hv, which is due to much finer grains.

• 대한화학회지
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• 제31권6호
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• pp.503-508
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• 1987

3,4 : 9,10-dibenzo-1,12-diaza-5,8-dioxacyclotetradecane $(NenOenH_4)$과 전이금속이온$(Cu^{2+},\;Ni^{2+},\;Co^{2+},\;Zn^{2+},\;Mn^{2+})$과의 착물의 안정도상수를 50%다이옥산-수용액에서 이온강도를 0.1로 하고, 전위차법적정으로 측정한 결과, 전이금속이온과 리간드가 만드는 착물의 안정도상수의 순서는 Williams-Irving서열과 일치한다.

• 환경위생공학
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• 제9권2호
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• pp.8-23
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• 1994

During the period from Mar., 1991 to Feb., 1992 66 tSP samples were collected by Hi volume air sampler at 1 sampling site in Seoul and the amount of concentration of 21 components(SO$_{4}$$^{2-}$, NO$_{3}$$^{-}$, NH$_{4}$$^{+}$, Cl$^{-}$, Al, Ba, Ca, Cd, Cr, Cu, Fe, It Mg, Mn, Na, Ni, Pt Si, Ti, Zn, Zr ) were measured. And monthly and seasonal variation were surveyed and the principal component analysis( PCA ) were carried out with respect to these amount of pollutants, minimum of visibility and radiation on a horizontal surface. The total amount of soluble ion in water was high in order o(SO$_{4}$$^{2-}$> NO$_{3}$$^{-}$> N%'>Cl$^{-}$ and metal ion was high in order of Na> Ca>Si> Fe> Al> K> Mg> Zn> Pb> Cu>Ti> Mn > Ba> Cr> Zr> Ni> Cd. There was Seasonal variation in concentration for SO$_{4}$$^{2-}$, NH$_{4}$$^{+}$, Cl$^{-}$, Na, Al, Ca, Bt Mg, Fe and Si. It was assumed that the components of the highest concentration on April were depend on yellow sand and the frequency of wind velocity and direction. As the results of PCA, the amount of pollution components was able to characterized with two principal components(Z$_{1}$, Z$_{2}$ ). The first principal components Z$_{1}$ was considered to be a factor indicating the pollutants originated from natural generation and The second principal components Z$_{2}$ was considered to be a factor indicating the pollutants originated from human work. The monthly concentration of pollutants in ISP, minimum of visibility and radiation on a horizontal surface was possible to evaluate by the use of these two principal components Z$_{1}$ and Z$_{2}$ .

• Restorative Dentistry and Endodontics
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• 제33권4호
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• pp.369-376
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• 2008

이 연구의 목적은 3 종의 포틀랜드 시멘트 (포틀랜드 시멘트, 백색 포틀랜드 시멘트, 초속경 시멘트)와 white MTA의 성분 및 세포독성을 비교하는 것이다. 성분비교를 위해서 X선 회절기 (XRD), X선 형광분석기 (XRF), 유도결합플라즈마 원자방출분광 분석기 (ICP-AES)를 사용하였으며, 세포독성비교를 위해서는 우무확산법 (agar diffusion test)을 사용하였다. 분석 결과, white MTA와 백색 포틀랜드 시멘트는 포틀랜드 시멘트나 초속경 시멘트에 비해 적은 양의 마그네슘 (mg), 철 (Fe), 아연 (Zn), 그리고 망간 (Mn)을 함유하고 있었다. 또한 초속경 시멘트는 다른 시멘트 및 white MTA에 비해 많은 산화 알루미늄 ($Al_2O_3$)을 함유하고 있었다. MTA와 포틀랜드 시멘트의 주된 성분은 tricalcicium silicate ($3CaO{\cdot}SiO_2$), dicalcium Silicate ($2CaO{\cdot}SiO_2$), tricalcium aluminate ($3CaO{\cdot}Al_2O_3$), 그리고 tetracalcium aluminoferrite (4CaO{\cdot}Al_2O_3{\cdot}Fe_2O_3)등이었다 세포독성 실험결과를 Kruskal-Wallis Exact test와 Bonferroni 사후 검정법을 사용하여 분석 한 결과 white MTA와 3 종의 포틀랜드 시멘트 군 사이에서 통계적으로 유의성 있는 차이를 보이지 않았다 (p > 0.05). White MTA와 3종의 포틀랜드 시멘트의 주성분은 유사하였으나 알루미늄 (Al), 마그네슘 (mg), 철 (Fe), 아연 (Zn), 그리고 망간 (Mn) 등의 함량에서는 차이를 보였으며 이러한 차이들은 물리적 성질에 영향을 미칠 것으로 보인다.

• 자원환경지질
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• 제25권1호
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• pp.27-39
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• 1992

Several pyrophyllite deposits occur around the Milyang area where Cretaceous andesitic rocks and spatially related granitic rocks are widely distributed. Pyrophyllite ores consist mainly of pyrophyllite, and quartz with small amount of sericite, pyrite, dumortierite, and diaspore. The andesitic rocks and spatially related granitic rocks in this area suggest that they could be formed from the same series of a calc-alkaline magma series. The contents of $SiO_2$, $Al_2O_3$, LOI(loss on ignition) are enriched, and $K_2O$, $Na_2O$, CaO, MgO, $Fe_2O_3$ are depleted in altered andesitic rocks and ores. Enrichment of As, Cr, Sr, V, Sb and depletion of Ba, Cs, Ni, Rb, U, Y, Co, Sc, Zn are characteristic during mineralization. The pyrophyllite ores can be discriminated from the altered-and unaltered wall-rocks by an increasing of $(La/Lu)_{cn}$ from 4.18~22.13 to 8.98~55.05. In R-mode cluster analysis, Yb-Lu-Y, La-Ce-Hf-Th-U-Zr, $TiO_2-V-Al_2O_3$, Sm-Eu, $CaO-Na_2O-MnO$, Cu-Zn-Ag, $K_2O-Rb$ are closely correlated. In the discriminant analysis of multi-element data, $P_2O_5$, As, Cr and $Fe_2O_3$, Sr are helpful to identify the ores from the unaltered-and altered wall-rocks. In the factor analysis, the factors of alteration of andesitic rocks and ore mineralization were extracted. In the change of ions per unit volume, $SiO_2$, $Al^{3+}$ and LOI are enriched and $Na^+$, $K^+$, $Ca^{2+}$, $Mg^{2+}$, $Mn^{2+}$ and $Fe^{3+}$ are depleted during the alteration processes. The Milyang and the Sungjin pyrophyllite deposits could be mineralized by hydrothermal alteration in a geochemical condition of low activity ratio of alkaline ions to hydrogen ion with reference to spatially related granitic rocks.

• 대한화학회지
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• 제44권3호
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• pp.220-228
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• 2000

청송 달기약수(상탕,중탕,하탕)의 수질특성을 파악하기 위해 1999년 5월부터 2000년 2월까지 약 1년 동안 계절별로 총 28개 항목의 함유성분을 분석하여 다음과 같은 결론을 얻었다. 각 탕별 약수의 수질에 큰 차이가 있었다. 하탕약수는 Mg과 Na이 상대적으로 높았?만? 중탕약수는 Ca, K, Si, Fe, Mn, 전기전도도, 총염기도, DO, $Cl^-$, $SO_4^{2-}$등에서 상대적으로 높은 값을 보였다. 건강상 유해성분인 As, Cd, $Cr^{6+}$, Hg는 검출되지 않았으며, Pb는 기준이하로 나타났다. 먹는물 수질기준을 초과한 항목으로는 경도, Fe와 Mn이었다. 그러나 샘물의 경우에는 이 기준을 적용하지 아니한다고 규정하였다. 약수의 계절별 특징으로는 온도를 제외한 기타 항목에서는 뚜렷한 차이가 없었다. 음용수에서 섭취할 수 있는 미네랄 양을 알아보고자 미국 국립과학아카데미의 하루 요구허용량과 섭취 음용수의 양을 1.O L로 하고 購종善嗤?기준으로 계산한 결과, Ca 35.05%, Mg 36.43%, Na 5.88∼10.63%, K 0.19∼0.57%, Mn 21.86∼43.72%, Zn 0.65%, Cr,Cu, P 등은 0.01% 이하이고, Fe는 95.1%이었다. 따라서 달기약수는 철분이 풍부한 약수임을 알 수 있었다.달기약수는 K index가 111.7∼254.6,O index가 2.3∼4.5로서 Hashimoto가 주장한 K index 5.2,O index 2.O을 상회하므로 건강에 좋고 맛있는 물의 조건을 만족하고 있다.

• 자원환경지질
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• 제38권4호
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• pp.481-492
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• 2005

이 연구에서는 광주지역 하상퇴적물에 대한 지질집단별 지구화학적 특성에 대해 규명 하고자 한다. 이를 위해 물이 흐르고 있는 1차 수계를 대상으로 하상퇴적물시료 104개를 채취하였고, 실험실에서 자연건조 시켰다. 화학분석을 위한 시료는 알루미나 몰타르를 이용하여 200메쉬 이하로 분쇄하였고, XRF ICP-AES, NAA분석을 실시하였다. 연구지역 하상퇴적물에 대해, 지질집단별 지구화학적 특성 비교와 기존 암석에 대한 연구에서 얻어진 암석화학적인 특성과의 비교를 위해, 선캠브리아기 화강편마암 지역, 쥬라기 화강암 지역, 백악기 화순안산암 지역으로 분리하였다 광주지역 하상퇴적물의 주성분원소 함량은 $SiO_2\;51.89\~70.63\;wt.\%,\;Al_2O-3\;12.91\~21.95\;wt.\%,\;Fe_2O_3\;3.22\~9.89\;wt.\%,\;K_2O\;1.85\~4.49\;wt.\%,\;MgO\;0.68\~2.90\;wt.\%,\;Na_2O\;0.48\~2.34\;wt.\%,\;CaO\;0.42\~6.72\;wt.\%,\;TiO_2\;0.53\~l.32\;wt.\%,\;P_2O_5\;0.06~0.51\;wt.\%\;and\;MnO\;0.05\~0.69\;wt.\%.$이다. 하상퇴적물과 암석에 대한 AMF 삼각도에서, 암석은 칼크-알칼리계열에 도시되는데 비하여, 하상퇴적물은 솔레아이트 계열과 칼크-알칼리계열의 경계부위에 도시된다. 이는 $Fe_2O_3$ 함량이 암석에서보다 하상퇴적물에 더 많이 함유되어 있는 것과 관련이 있는 것으로 보인다. $SiO_2$에 대한 $K_2O+Na_2O$의 비교그림에서, 하상퇴적물은 암석에서와 같이 subalkaline 계열에 점시된다. 하상퇴적물의 미량성분원소 및 희토류 원소 함량은 $Ba 590\~2170ppm$, Be$1\~2.4$ppm, Cu $13\~179ppm$, Nb $20\~34ppm$, Ni$10\~50ppm$, Pb $17\~30$ppm, Sr $70\~1025$ ppm, V$42\~135$ ppm, Zr$45\~171$ ppm, Li$19\~77$ppm, Co$4.3\~19.3$ppm, Cr$28\~131$ppm, Cs$3.1\~17.6$ ppm, Hf $5\~27.6$ ppm, Rb $388\~202$ ppm, Sb$0.2\~l.2$ ppm, Sc$6.4\~17$ ppm, Zn $47\~389$ ppm, Pa $8.8\~68.8$ ppm, Ce$62\~272$ppm, Eu$1\~2.7$ppm and Yb$0.9\~6$ppm의 범위를 보인다.

• 한국재료학회지
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• 제19권10호
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• pp.533-537
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• 2009

This paper presents a new method for the improvement of color temperature without the change of the driving scheme using transparent dielectric layers with various metal oxides (CeO$_2$, Co$_3$O$_4$, CuO, Fe$_2$O$_3$, MnO$_2$, NiO) in plasma display panels (PDP). In this study, we fabricated ZnO-B$_2$O$_3$-SiO$_2$-Al$_2$O$_3$ glasse with various metal oxides and examined the optical properties of these glasses. As the metal oxides were added to the glasses, the visible transmittances of the dielectric layers decreased and the transmittances in special wavelength regions were reduced at different rates. The change of the transmittance in each wavelength range induced the variation of the visible emission spectra and the change of the color temperature in the PDP. The addition of Co$_3$O$_4$ and CuO slightly decreased the intensity of the blue light, but the intensities of the green and the red light were significantly decreased. Therefore, the color temperature can be improved from 6087K to 7378K and 7057K, respectively.

• 자원환경지질
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• 제30권5호
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• pp.443-450
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• 1997

The main purpose of this study is to investigate mineralogical and chemical changes during natural weathering, and assess the mobility of major and trace elements. Yongwol power plant utilize anthracite coal which is mainly composed of illite, kaolinite, pyrophyllite and quartz in mineralogy. Coal and coal-derived fly ash samples were sampled by the electrostatic precipitator in Yongwol coal-fired power plant in Korea. Short term weathered fly ash were also collected in ash disposal mound, and two profile soil samples were taken from an ash near the power plant. Amorphous materials are the main component of the fly ash, and mullite, quartz, magnetite and heamatite are present in all coal-derived fly ash. In chemistry, Si and Al are the most abundant elements of the total content. The ash samples were fractionated into upper $90{\mu}m$ and under $45{\mu}m$ size. Finer particles show higher concentrations in metal contents including Co, Cr, Cu, Ni, V, Zn and Pb. Concentration of Zn and Pb are nearly 4 times higher concentration in the finer particles. For the profile samples, the concentrations of $SiO_2$, $Na_2O$, MgO and $K_2O$ generally show increasing trends with depth, whereas those of $Fe_2O_3$ and $TiO_2$ appear to decrease with depth. Content of MnO does not show any specific depth trend. For the trace elements, Co, Cu, Ni and V show increasing concentrations with depth.