• 한국대기환경학회지
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• 제2권2호
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• pp.9-18
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• 1986

For identification and apportionment of sources emitting particulate matters in environment, the multi-elemental characterization of size-density fractionated particulate matters was carried out. Eight types of samples were tested; soil, flyash released from burning of bunker-Coil, diesel oil, coal, and soft coal, urban road-way dust, urban dust fall, and airborne particulate matter. The fractions of particulate matters obtained by heavy liquid separation methos with a series of dichloromethane-bromoform were then analyzed using atomic absorption spectrophotometry for Ni, Cr, Cu, An, Fe, Al, and Mg. Each sample showed a different concentration profile as a function of density, and a number of useful conclusions concerning characterization of elemental distribution were obtained. From the density distributions of elements in soil, the maximum value was found for all elements in the density range of 2.2 $\sim 2.9g.cm^{-3}$, including the density of $SiO_2$. However, the distribution of metallic compounds with the density lower than $2.2g.cm^{-3}$ was prevalent in urban roadway dust, urban dust fall, and airborne particulate matter. And the density distribution curves of these urban dusts also have the higher distribution at the density of 2.2 - 2.9g.cm^{-3}$, including the density of wind-blown silica. This tendency generally was prevalent in the natural source elements, such as Al, Fe, Mn, and Mg. The maximum values were found in the density ranges of 1.3 $\sim 2.2g.cm^{-3}$ from the density distribution of elements in oil fired flyash. These distributions of anthropogenic source elements, such as Zn, Ni, Cu, and Cr were higher predominately than those of natural source elements. And the higher distribution was found in the density range of $2.2 \sim 2.9g.cm^{-3}$ from the density distribution of elements in coal and soft-coal fired flyash. These distributions showed similar patterns to soil. But anthropogenic source elements somewhat predominated at the density ranges of $1.3 \sim 2.2g.cm{-3} and 2.9g.cm^{-3}$ to soil. Therefore the higher distribution of anthropogenic source elements in the density ranges of $1.3 \sim 2.2g.cm^{-3} and 2.9g.cm^{-3}$ was considered as anthropogenic origin.

• 한국식품조리과학회지
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• 제4권1호
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• pp.53-57
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• 1988

국산차 기술개발을 위한 기초 자료를 얻고자 국내산 및 스리랑카제품의 특성에 대하여 분석한 결과는 다음과 같다. 1. 국산 홍차는 스리랑카 홍차에 비하여 섬유함량이 50% 높은 반면 탄닌 및 카페인함량은 크게 낮았다. 탄닌의 경우 3.5배, 카페인함량은 50%의 차이를 나타내었다. 또한 회분, 조지방, 조단백질의 함량은 두 제품간에는 큰 차이가 없었다. 2. 스리랑카 홍차에서는 P 3,000ppm, K 15,000ppm, Mg 1,400ppm, Ca 4,000ppm, Cu 22ppm, Cr 21ppm 및 Zn 45ppm으로 국산 홍차보다 높은 함량이었으며, 국산홍차에서는 F 225ppm, Mn 1,950ppm, Fe 265ppm, Sr 6ppm 및 Al 4,100ppm으로 스리랑카 홍차보다 높은 함량이었다. Pb와 Cd는 양 제품에서 검출되지 않았다. 3. 국산 홍차에서는 6종류의 유기산이 분리·동정되었는데 quinic acid와 gallic acid의 함량이 높았다. 스리랑카 홍차에서는 8종류의 유기산이 동정되었으며 shikimic acid, citric acid 및 quinic acid가 주요 유기산이었다. 4. Sucrose의 함량은 스리랑카 홍차보다 국산 홍차가 2.5배 높았다. 5. 홍차의 특수성분인 theaflavin, thearubigin, theobromine의 함량은 스리랑카 홍차에서 높은 경향을 나타내었다.

• 분석과학
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• 제16권3호
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• pp.226-231
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• 2003

국내와 국외에서 생산된 두 가지 종류의 AAS 기기를 이용하여 대기분진 시료를 분석하였다. 국내에서 생산된 제품의 경우, 단색화 장치의 성능면에서 선택된 파장들에 대한 광량의 세기가 우수하게 관찰되었다. 그리고 원자화장치의 경우, 재현성을 높이기 위하여 미세방울을 제외한 모든 큰 방울을 폐기 잔유물이 남지 않도록 하였다. 기기의 검출부에서는 저역 통과 filter를 사용하여, 데이터의 노이즈를 줄였다. Au 표준 용액을 이용한 검출한계 실험 분석치는 약 $0.015{\mu}g/L$ 수준의 높은 감도로서 외국사의 성능과 뚜렷한 큰 차이를 구분하기는 어려웠다. 본 연구진은 이러한 분석기법을 활용하여 서울시내 7개 지역 주요 관측점을 중심으로 2001년부터 2002년 봄까지 일년 동안 대기보전시료를 채취하였다. 이들 시료를 이용하여 분진 중에 결합된 중금속성분의 (Pb, Cu, Mn, Cd, Ni, Fe, Cr, Co, Mg, Al) 농도를 분석하였다.

• Journal of Radiation Protection and Research
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• 제43권4호
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• pp.160-169
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• 2018

Background: This study aims to develop an integrated optical system that can simultaneously or selectively measure the signals obtained from radioluminescence (RL), thermoluminescence (TL), and optically stimulated luminescence (OSL), which are luminescence phenomena of materials stimulated by radioactivity, heat, and light, respectively. The luminescence mechanism of various materials could be investigated using the glow curves of the luminescence materials. Materials and Methods: RL/TL/OSL integrated measuring system was equipped with a X-ray tube (50 kV, $200{\mu}A$) as an ionizing radiation source to irradiate the sample. The sample substrate was used as a heating source and was also designed to optically stimulate the sample material using various light sources, such as high luminous blue light emitting diode (LED) or laser. The system measured the luminescence intensity versus the amount of irradiation/stimulation on the sample for the purpose of measuring RL, TL and OSL sequentially or by selectively combining them. Optical filters were combined to minimize the interference of the stimulation light in the OSL signal. A long-pass filter (420 nm) was used for 470 nm LED, an ultraviolet-pass filter (260-390 nm) was used for detecting the luminescence of the sample by PM tube. Results and Discussion: The reliability of the system was evaluated using the RL/OSL characteristics of $Al_2O_3:C$ and the RL/TL characteristics of LiF:Mg,Cu,Si, which were used as dosimetry materials. The RL/OSL characteristics of $Al_2O_3:C$ showed relatively linear dose-response characteristics. The glow curve of LiF:Mg,Cu,Si also showed typical RL/OSL characteristics. Conclusion: The reliability of the proposed system was verified by sequentially measuring the RL characteristics of radiation as well as the TL and OSL characteristics by concurrent thermal and optical stimulations. In this study, we developed an integrated measurement system that measures the glow curves of RL/TL/OSL using universal USB-DAQs and the control program.

• 한국대기환경학회지
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• 제4권2호
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• pp.57-66
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• 1988

Sandy dust phenomena was observed from April 19 to 23, 1988 in Seoul and suspended particulate was collected by Andersen air sampler during this period. The samples were analyzed for 16 components $(SO_n^{2-}, NO_3^-, Cl^-, PO_4^{3-}, NH_4^+, F^-, Al, Fe, K, Cu, Mn, Na, Pb, Mg, Ca, Cd)$. The conclusions are as follwes: 1. Total suspended particulate concentation during the period of sandy dust phenomena was 489 $\mug/m^3$ (ordinary times: 140-125 $mug/m^3$) 2. The water - soluble ion component concentration of suspended particulate during the period of sandy dust phenomena was few and the metal concentration of that was more than that of ordinary times. 3. The cumulative frequency distribution of suspended particulates in logarithmic diagram did not show similar to normal log distribution during the period of sandy dust phenomena. 4. $SO_4^{2-}, NO_3^-, Cl^-, and PO_4^{3-}$ was onsided to coarse particle, and $NH_4^+$ and F to fine particle in the size distribution of water - soluble ion components during the period of sandy dust phenomena. 5. Metal concentration was high and Al, Fe, Cu, Mn, Na, Mg, and Ca was onsided to coarse particle, and K, Pb, and Cd to fine particle in the size distribution of metal components. 6. During the period of sandy dust phenomena the quantity of respirable particle (< 1 $\mum$) was about 3 times and that of metal components were about 2 - 11 times than that of ordinary times. 7. The concentrations of $NO_3^-, Cl^-, NH_4^+$ at ordinary times were 1.1 - 4 time than that of the period of sandy dust phenomena.

• 소성∙가공
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• 제27권6호
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• pp.339-346
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• 2018

This study investigated the microstructure and wear properties of extruded hyper-eutectic Al-Si (15wt.%) alloy in an engine oil environment. The wear mechanism of the material was also analyzed and compared to conventional gray cast iron. In microstructural observation results of Al-15wt.%Si alloy, primary Si phase ($45.3{\mu}m$) and eutectic Si phase ($3.1{\mu}m$) were found in the matrix, and the precipitations of $Mg_2Si({\beta}^{\prime})$, $Al_2Cu({\theta}^{\prime})$ and $Al_6(Mn,Fe)$ were also detected. In the case of gray cast iron, ferrite and pearlite were observed. It was also observed that flake graphite ($20-130{\mu}m$) were randomly distributed. Wear rates were lower in the Al-Si alloy as compared to those of gray cast iron in all load conditions, confirming the outstanding wear resistance of Al-15wt.%Si alloy in engine oil environment. In the $4kg_f$ condition, the wear rate of gray cast iron was $6.0{\times}10^{-5}$ and that of Al-Si measured $0.8{\times}10^{-5}$. The microstructures after wear of the two materials were analyzed using scanning electron microscope (SEM) and electron backscatter diffraction (EBSD). The primary Si and eutectic Si of Al-Si alloy effectively mitigated the abrasive wear, and the Al matrix effectively endured to accept a significant amount of plastic deformation caused by wear.

• 자원환경지질
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• 제46권2호
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• pp.199-206
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• 2013

대현 금-은광상은 Cambro-Ordovician 석회암질 대리암내에 발달된 NE 방향성의 단열대를 따라 형성된 2개의 열수성 석영맥으로 구성된다. 모암변질시 원소 분산과 이득/손실을 알아보기 위해 모암, 열수변질대 및 금-은 광맥에서 시료를 채취하였다. 모암변질시 뚜렷한 변질대가 관찰되지 않으며 구성광물은 주로 방해석, 돌로마이트, 석영과 소량 녹염석 등이다. 이 광상의 광석광물은 유비철석, 자류철석, 황철석, 섬아연석, 황석석, 황동석, 방연석, 에렉트럼, 자연 창연 및 은 광물 등이 산출된다. 분석된 자료를 기초로, 모암은 주로 $SiO_2$, CaO 및 $CO_2$로 구성되며 소량 $Al_2O_3$, $Fe_2O_3(T)$ 및 MgO 등이 함유되어 있다. 광체로부터 모암으로 감에 따라 $SiO_2$, $Fe_2O_3(T)$, MgO, CaO 및 $CO_2$ 함량은 변화 폭이 크게 관찰된다. 모암변질시 모암의 물리-화학적 물성 때문에 원소 분산은 현저히 관찰되지 않으며 단지 광체 주변부에서만 관찰된다. 모암변질시 이득원소들은 $Fe_2O_3(T)$, 총 S, Ag, As, Bi, Cd, Cu, Ni, Pb, Sb, Sn, W 및 Zn이고 손실원소들은 $SiO_2$, MnO, MgO, CaO. $CO_2$ 및 Sr 이다. 따라서 우리의 결과물은 황강리 광화대내 석회암질 대리암을 모암으로 갖는 광상들의 지화학탐사시 활용될 수 있을 것이다.

• 한국지구과학회지
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• 제27권1호
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• pp.49-60
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• 2006

본 연구는 나주지역 하상퇴적물에 대한 지구화학적 특성 연구이다. 이를 위해 1차 수계를 대상으로 139개의 하상퇴적물 시료를 채취하였다. 채취된 시료는 실험실에서 자연 건조시켰으며, XRF, ICP-AES, NAA를 이용하여 화학분석을 실시하였다. 기반암에 따른 지구화학적 특성을 알아보기 위하여, 화강암질편마암 지역, 편암류 지역, 화강암류 지역, 사질암 지역, 응회암 지역, 안산암 지역, 유문암 지역으로 분류하였다. 나주지역 하상퇴적물의 지질집단별 주성분원소 평균함량은 $SiO_2\;58.37{\sim}66.06wt.%,\;Al_2O_3\;13.98{\sim}18.41wt.%,\;Fe_2O_3\;4.09{\sim}6.10wt.%,\;CaO\;0.54{\sim}1.33wt.%,\;MgO\;0.86{\sim}1.34wt.%,\;K_2O\;2.38{\sim}4.01wt.%,\;Na_2O\;0.90{\sim}1.32wt.%,\;TiO_2\;0.82{\sim}1.03wt.%,\;MnO\;0.09{\sim}0.15wt.%,\;P_2O_5\;0.11{\sim}0.18wt.%$이다. 주성분원소의 평균함량 비교에서 $Al_2O_3$와 $K_2O$는 화강암질편마암 지역에서, $Fe_2O_3,\;CaO,\;P_2O_5$는 응회암 지역에서, MgO와 $TiO_2$는 안산암 지역에서, $Na_2O$는 유문암 지역에서 높고, $SiO_2$와 MnO 함량은 사질암 지역에서 약간 높다. 미량성분 및 희토류원소의 지질집단별 평균함량은 $Ba\;1278{\sim}1469ppm,\;Be\;1.1{\sim}1.5ppm,\;Cu\;18{\sim}25ppm,\;Nb\;25{\sim}37ppm,\;Ni\;16{\sim}25ppm,\;Pb\;21{\sim}28ppm,\;Sr\;83{\sim}155ppm,\;V\;64{\sim}98ppm,\;Zr\;83{\sim}146ppm,\;Li\;32{\sim}45ppm,\;Co\;7.2{\sim}12.7ppm,\;Cr\;37{\sim}76ppm,\;Cs\;4.8{\sim}9.1ppm,\;Hf\;7.5{\sim}25ppm,\;Rb\;88{\sim}178ppm,\;Sc\;7.7{\sim}12.6ppm,\;Zn\;83{\sim}143ppm,\;Pa\;11.3{\sim}37ppm,\;Ce\;69{\sim}206ppm,\;Eu\;1.1{\sim}1.5ppm,\;Yb\;1.8{\sim}4.4ppm$이다. Pb, Li, Cs, Hf, Rb, Sb, Pa, Ce, Eu, Yb 평균함량은 화강암질편마암 지역에서, Ba, Co, Cr 평균함량은 편암류 지역에서, Nb, Ni, Zr 평균함량은 사질암 지역에서, Sr 평균함량은 응회암 지역에서 높고, Be, Cu, V, Sc, Zn 평균함량은 안산암 지역에서 다른 지질집단에서 보다 높다.

• 한국재료학회지
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• 제28권9호
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• pp.534-538
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• 2018

The annealing characteristics of a cold rolled Al-6.5Mg-1.5Zn alloy newly designed as an automobile material is investigated in detail. The aluminum alloy in the ingot state is cut to a thickness of 4 mm, a total width of 30 mm and a length of 100 mm and then reduced to a thickness of 1 mm (reduction of 75 %) by multi-pass rolling at room temperature. Annealing after rolling is performed at temperatures ranging from 200 to $400^{\circ}C$ for 1 hour. The tensile strength of the annealed material tends to decrease with the annealing temperature and shows a maximum tensile strength of 482MPa in the material annealed at $200^{\circ}C$. The tensile elongation of the annealed material increases with the annealing temperature, while the tensile strength does not, and reaches a maximum value of 26 % at the $350^{\circ}C$ annealed material. For the microstructure, recovery and recrystallization actively occur as the annealing temperature increases. The recrystallization begins to occur at $300^{\circ}C$ and is completed at $350^{\circ}C$, which results in the formation of a fine grained structure. After the rolling, the rolling texture of {112}<111>(Cu-Orientation) develops, but after the annealing a specific texture does not develop.

• 한국지구과학회지
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• 제26권8호
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• pp.800-808
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• 2005

광주광역시 향등지역에서 화강암의 풍화에 따른 토양단면의 지화학적 특성을 파악하기 위하여 11개의 시료를 화학분석 하였다. 모암에서부터 풍화암까지 주성분원소 중 Si, Ca, Na, Mg, P, Mn은 감소하고 Ti, Fe, K는 증가하는 경향을 보인다. 미량성분원소의 경우 Rb, Sr, Pb, Ba은 증가하는 경향을 보이며, As, Co늘 감소하는 경향을 보인다. 또한 Zn, Cr, Ni등은 부분적으로 집적된 경향을 보이나 전체적으로는 모암과 풍화토에서 거의 비슷한 함량을 갖는다. 희토류원소는 전체적으로 상부로 갈수록 증가하는데 경희토류원소(LREE)는 풍화초기에 기반암에서 용탈되어 풍화암(saprock)에서 집적되지만, 중희토류원소(HREE)의 경우는 상대적으로 집적되지 못하여 풍화초기에 약간 감소하는 경향을 나타낸다.