• Tribology and Lubricants
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• 제13권2호
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• pp.82-88
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• 1997

This paper describes an empirical equation which can be used to predict the engine condition of supersonic aircraft. The equation, which is derived from the trend analysis of JOAP data, represents the concentration of Fe particles in the engine oil. The result of the trend analysis shows that the concentration of Fe particles is a function of running time of engine oil. Meanwhile the slope of Fe concentration is a function of running time of engine. Threfore, the empirical equation was derived as $w=a(t_e).t_o+b$. However, the equation could not enough to diagnose the damaged part of engine quantitatively. To make up for the weak points of the equation, qualitative analysis was carried out. For that purpose wear debris were collected from the abnormal engine and analyzed by EDS to detect the damaged parts of engine.

• 한국광물학회지
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• 제27권4호
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• pp.311-320
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• 2014

슬래그를 매립한 토양을 대상으로 자기분리연구를 수행하였다. 토양세척을 거친 토양과 토양세척 전 토양을 대상으로 습식자기분리와 건식자기분리를 수행하여 분리된 부분과 분리되지 않은 부분의 중금속 농도를 측정하여 중금속의 농축효과를 측정하였다. 습식자기분리의 경우 토양세척 전 시료의 자력분리율이 상대적으로 높으며 토양세척 후 시료의 경우 약 40% 정도가 자기분리 되었다. 토양 : 물의 비가 농축효과에는 큰 영향을 미치지 못하며, Fe, Pb, Cu, Zn, Cd의 세척 전 토양과 세척 후 토양의 자기분리에 의한 평균 농축비는 3.2, 2.1, 12.1, 2.5, 1.5와 17.4, 7.0, 15.7, 9.6, 7.0으로 토양 세척을 거친 경우 자기분리에 의해 토양 세척 전 토양에 비해 더 큰 토양 부피 감량효과를 기대할 수 있다. 건식자기분리의 경우에도 자기분리에 의해 중금속의 농축효과를 얻을 수 있으나 자기분리에 의한 회수율이 너무 높은 경우 오염토 저감을 기대하기 어렵다. 철과 같은 강자성체를 포함하는 토양의 경우 자기분리에 의해 토양세척의 효과와 유사하게 오염토양의 양을 줄일 수 있고, 오염이 한쪽에 농축되는 결과를 얻을 수 있다.

• 환경위생공학
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• 제19권4호
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• pp.9-18
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• 2004

In this study, the observation data for the yellow sandy dust phenomena from the year 1999 to 2003 at background sites in Korea were collected at Global Atmospheric Observatory at An-Myeon island and its temporal variation were analyzed. The chemical characteristics of the fine particles were also analyzed in order to evaluate sources of the yellow sandy dust particles. The results showed that the monthly average mass concentration of the fine particles was the highest in springtime and the lowest in summertime in general. The magnitude of its variation was also the highest in March in which the occurrence of yellow sandy dust was the most frequent and thus the number of samples was the largest, while the lowest in June through September. The yearly variation of ion components contributions to the total mass concentration of the fine particles was slowly decreasing, showing that $63\%$ in 1999, $59\%$ in 2000 and $56\%$ in 2003. The most prevalent ion components in the fine particles were found to be $NO_3$ and $SO_4^{2-}$, which are known to be source materials of acidic precipitation, and $NH_4^+$, a neutralizing material of the acid precipitation. Relative proportion of metal components in the fine particles was calculated as $14\%$ in average, and their concentrations are in an order of Fe > Al > Na > Ca > Zn > Pb > Cu > Mn > Ni > Cd > Cr > Co > U. The results indicated that main sources of the metals was soil-originated Fe, Al, Ca, and Mg, and the contribution of anthropogenic air Pollution-originated Zn, Pb, Cu, Mn were also high and keep slightly increasing. Statistical analysis showed that the chemical components could be divided into soil-originated group of Mg, Al, Ca, Fe, and Mn and air pollution-originated group of $NO_3$, Zn, Pb, and they are occupying more than $60\%$of all the components in the dusty sand. The results explain that An-Myeon island is more influenced by soil-originated source than ocean-originated one and also the influencing strength of anthropogenic poilution-originated source is less than $50\%$ of that of soil-originated sources. Compared to non-yellow sandy period, the yellow sandy dust period showed that the amounts of soil-originated $Mg^{2+}$ and $Ca^{2+}$ and ocean-originated $Na^+$ and $Cl^-$ were increased to more than double and the metals of Mg, Al, Ca, Fe were also highly increased, while micro metal components such as Pb, Cd, Zn, which have a tendency of concentrating in air, were either decreased or maintained at nearly constant level. In the period of yellow sandy dust, a strong positive correlation was observed between water soluble ions and between metals in terms of its concentration, respectively. Factor analysis showed that the first group being comprised of about $43\%$ of the total inorganic components was affected by soil and they are ions of $Na^+,\;Mg^{2+}\;and\;Ca^{2+}$ and metals of Na, Fe, Mn and Ni. The result also showed that the metals of Mg and Cr were classified as second group and they were also highly affected by soil sources.

• Mass Spectrometry Letters
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• 제2권2호
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• pp.53-56
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• 2011

[ $C_8$ ]functionalized magnetic nanoparticles were synthesized by coating magnetic $Fe_3O_4$ nanoparticles with silicaamine groups using 3-aminopropyltriethoxysilane and by subsequently modifying the amine groups with chloro(dimethyl)octylsilane to produce octyl groups on the surface of the MNPs. The $C_8$-functionalized MNPs were used to enrich peptides from tryptic protein digests of myoglobin and ${\alpha}$-casein. The enriched peptides were analyzed by matrix-assisted laser desorption/ionization time-of-flight mass spectrometry (MALDI-TOF-MS). MALDI-MS was also used to investigate desalting of the $C_8$-functionalized MNPs. Sample solutions were prepared in 1.0 M NaCl, and the successful removal of salt was observed. Enrichment with $C_8$-functionalized MNPs was very effective for separating and concentrating tryptic peptides.

• Journal of Electrical Engineering and Technology
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• 제7권2호
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• pp.184-192
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• 2012

The torque and unbalanced magnetic forces in permanent magnet machines are resultants of the tangential, axial and normal magnetic forces, respectively. Those are in general influenced by pole-teeth-winding configuration. A study of the torque and unbalanced magnetic forces of a small flux concentrating permanent magnet transverse flux machine (FCPM-TFM) in segmented compact structure is presented in this paper. By using FLUX3D software from Cedrat, Maxwell stress tensor has been solved. Finite element (FE-) magneto static study followed by transient analysis has been conducted to investigate the influence of unsymmetrical winding pattern, in respect to the rotor, on the performance of the FCPM-TFM. Calculating the magnetic field components in the air gap has required an introduction of a 2D grid in the middle of the air gap, whereby good estimations of the forces are obtained. In this machine, the axial magnetic forces reveal relatively higher amplitudes compared to the normal forces. Practical results of a prototype motor are demonstrated through the analysis.

• 한국전자통신학회논문지
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• 제17권4호
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• pp.607-616
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• 2022

본 논문에서는 전기 자동차 응용을 위해 연자성 분말 코어가 있는 새로운 축방향 자속 영구자석 모터를 제안한다. 권선 및 연자성 분말 코어는 매우 조밀한 구조를 형성하도록 설계할 수 있으므로 토크 밀도를 크게 향상시킨다. 우수한 자속 집중 능력을 얻기 위해 두 대의 토로이드형 내부 고정자형 모터가 설계 및 분석되었으며, 설계된 모터에는 고성능 전기자동차 애플리케이션 적용을 위해 네오디움 자석이 사용되었다. 3차원 유한 요소 방법은 전자기 매개변수 및 성능을 분석하는 데 사용되었으며, 성능 비교를 위해 상용 축방향 자속 영구자석 모터가 사용되었다. 제안된 모터는 기존 구동모터에 비해 약 5.8% 무게가 가벼워지고 약 8Nm 정도 높은 토크를 생성하였다.

• 자원리싸이클링
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• 제28권3호
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• pp.53-58
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• 2019

폐납축적지 재활용 공정에서 발생한 납드로스는 비소 등의 유해물질을 함유하고 있어 적절한 처분이 요구되고 있다. 본 연구에서는 볼밀과 믹서밀로 분쇄한 납드로스를 대상으로 자력선별을 실시하여 비소 성분을 농축하고자 하였다. 볼밀에 의해 $150{\mu}m$ 이하로 분쇄된 시료를 대상으로 10000 G와 2000 G의 자석봉으로 순차적 자력선별을 실시한 결과, 10000 G의 비자착물에서는 비소성분이 검출되지 않아 유해물질이 제거된 산물을 확보가능하였다. 추가적인 2000 G 자력선별의 자착물에는 비소가 18.87 %까지 농축되는 것을 확인하였다. 또한 볼밀 분쇄시 $300{\mu}m$ 이상인 분쇄산물을 대상으로 믹서밀로 $150{\mu}m$ 이하로 분쇄하고 4000 G와 2000 G의 자석봉으로 순차적인 자력선별을 실시한 결과 2000 G의 자착물에 비소가 21.021 %로 농축된 것이 확인되었다. 비소는 XRD 결과에서 $Fe_2As$로 존재하는 것을 확인하였으며, 분쇄와 자력선별에 의해 비소 성분이 원시료의 0.6 %에서 21.021 %까지 농축되는 것을 확인하였다.

• 한국광물학회:학술대회논문집
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• 한국광물학회.대한자원환경지질학회.대한광업진흥공사 2002년도 추계 공동 심포지엄 논문집: 국내 자원의 현황과 전망
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• pp.119-136
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• 2002

Contrasts in the style of the gold-silver mineralization in geologic and tectonic settings in Korea, together with radiometric age data, reflect the genetically different nature of hydrothermal activities, coinciding with the emplacement age and depth of Mesozoic magmatic activities. It represents a clear distinction between the plutonic settings of the Jurassic Daebo orogeny and the subvolcanic environments of the Cretaceous Bulgugsa igneous activities. During the Daebo igneous activities (c.a. 200-150 (?) Ma) coincident with orogenic time, gold mineralization took place between c.a. 195 and 135 (127 ?) Ma. The Jurassic Au deposits commonly show several characteristics; prominent association with pegmatites, low Ag/hu ratios in the ore-concentrating parts, massive vein morphology and a distinctively simple mineralogy including Fe-rich sphalerite, galena, chalcopyrite, arsenopyrite, Au-rich electrum, pyrrhotite and/or pyrite. During the Bulgugsa igneous activities $(110\~50Ma)$, the precious-metal deposits are generally characterized by such features as complex vein morphology, medium to high AE/AU ratios in the ore concentrates, and diversity of ore minerals including base-metal sulfides, pyrite, arsenopyrite, Ag-rich electrum and native silver nth Ag sulfides, Ag-Sb-As sulfosalts and Ag tellurides. Vein morphology, mineralogical, fluid inclusion and stable isotope results indicate the diverse genetic natures of hydrothermal systems in Korea. The Jurassic Au-dominant deposits (orogenic type) were formed at the relatively high temperature $(about\;300^{\circ}\;to\;450^{\circ}C)$ and deep-crustal level $(4.0{\pm}1.5\;kb)$ from the hydrothermal fluids containing more amounts of magmatic waters $(\delta\;^{18}O_{H2O}\;5\~10\%_{\circ})$. It can. It can be explained by the dominant ore-depositing mechanisms as $CO_2$ boiling and sulfidation, suggestive of hypo- to mesothermal environments. In contrast, the Cretaceous Au-dominant $(l13\~68\;Ma),\;Au-Ag \;(108\~47\;Ma)$ and Ag-dominant $(103\~45\;Ma)$ deposits, which correspond to volcanic-plutonic-related type, occurred at relatively low temperature $(about\;200^{\circ}\;to\;350^{\circ}C)$ and shallow-crustal level $(1.0\{pm}0.5\;kb)$ from the ore-forming fluids containing more amounts of less-evolved meteoric waters$(\delta\;^{18}O_{H2O}\;-10\~5\%_{\circ})$. These characteristics of the Cretaceous precious-metal deposits can be attributed to the complexities in the ore-precipitating mechanisms (mixing, boiling, cooling), suggestive of epi- to mesothermal environments. Therefore, the differences of the emplacement depth between the Daebo and the Bulgugsa igneous activities directly influence the unique temporal and spatial association of the deposit styles.

• 대한자원환경지질학회:학술대회논문집
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• 대한자원환경지질학회 2002년도 추계 공동 심포지엄 논문집
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• pp.119-136
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• 2002

Contrasts in the style of the gold-silver mineralization in geologic and tectonic settings in Korea, together with radiometric age data, reflect the genetically different nature of hydrothermal activities, coinciding with the emplacement age and depth of Mesozoic magmatic activities. It represents a clear distinction between the plutonic settings of the Jurassic Daebo orogeny and the subvolcanic environments of the Cretaceous Bulgugsa igneous activities. Dunng the Daebo igneous activities (c.a. 200～150 (\ulcorner) Ma) coincident with orogenic time, gold mineralization took place between c.a. 195 and 135 (127 \ulcorner) Ma. The Jurassic Au deposits commonly show several characteristics; prominent association with pegmatites, low Ag/Au ratios In the ore-concentrating parts, massive vein morphology and a distinctively simple mineralogy including Fe-rich sphalerite, galena, chalcopyrite, arsenopyrite, Au-rich electrum, pyrrhotite and/or pyrite. During the Bulgugsa igneous activities (110～50 Ma), the precious-metal deposits are generally characterized by such features as complex vein morphology, medium to high Ag/Au ratios in the ore concentrates, and diversity of ore minerals including base-metal sulfides, pyrite, arsenopyrite, Ag-rich eletrum and native silver with Ag sulfides, Ag-Sb-As sulfosalts and he tellurides. Vein morphology, mineralogical, fluid inclusion and stable isotope results indicate the diverse genetic natures of hydrothermal systems in Korea. The Jurassic Au-dominant deposits (orogenic type) were formed at the relatively high temperature (about 300$^{\circ}$ to 45$0^{\circ}C$) and deep-crustal level (4.0$\pm$1.5 kb) from the hydrothermal fluids containing more amounts of magmatic waters ($\delta$$^{18}$ $O_{H2O}$; 5～10$\textperthousand$). It can be explained by the dominant ore-depositing mechanisms as $CO_2$ boiling and sulfidation, suggestive of hypo- to mesothermal environments. In contrast, the Cretaceous Au-dominant (l13～68 Ma), Au-Ag (108～47 Ma) and AE-dominant (103～45 Ma) deposits, which correspond to volcanic-plutonic-related type, occurred at relatively low temperature (about 200$^{\circ}$ to 35$0^{\circ}C$) and shallow-crustal level (1.0$\pm$0.5 kb) from the ore-forming fluids containing more amounts of less-evolved meteonc waters ($\delta$$^{18}$ $O_{H2O}$;-10～5$\textperthousand$). These characteristics of the Cretaceous precious-metal deposits can be attributed to the complekities in the ore-precipitating mechanisms (mixing, boiling, cooling), suggestive of epi- to mesothermal environments. Therefore, the differences of the emplacement depth between the Daebo and the Bulgugsa igneous activities directly influence the unique temporal and spatial association of the deposit styles.les.

• 자원환경지질
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• 제28권6호
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• pp.587-597
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• 1995

한반도 중부지역과 동남부지역에 분포하는 금-은 광상들의 광화작용은 쥐라기 중기로부터 백악기 말기에 걸쳐서 진행되었으며, 이들 광상은 유행별로 산출지역 및 산출시기에 연관된 지질학적 지화학적 생성환경의 차이를 나타내고 있다. 중부지역 금-은 광상은 북동-남서의 방향성을 갖고 산출분포하는 중생대 화강암류 및 주변 선캠브리아기 변성암류내에 분포하지만, 동남부지역 금-은 광상은 백악기 퇴적암 및 화산암류내에 주로 배태되고 있다. 이는 한반도 대표적인 화성활동인 쥐라지 대보화성활동 및 백악기 불국사 화성활동과 각각 밀접한 성인적 연관성을 시사하고 있다. 이러한 각 광상들의 광화작용 특성(광물공생관계, 조직, 구조 등)과 연대측정결과 및 지질학적 분포특성은 쥐라가 중기로부터 백악기 말기에 이르기까지 광상형성과 연관된 열수유체의 성인적 차이를 의미하고 있다. 즉, 쥐라기로부터 초기 백악기에는 금광단일형 광상의 광화작용이 우세하게 진행되었으나, 후기 백악기에 이르면서 금-은혼합형광상 및 은광단일형 광상의 광화작용이 우세하게 야기되었음을 알 수 있다. 쥐라기 금광단일형 광상들은 괴상의 맥상 산출특성 및 단순한 광석 광불 공생관계를 보여주는 단성광맥으로 높은 fineness 값을 나타내지만, 백악기 금-은혼합형 광상과 은광단일형 광상은 다양하고 복잡한 구조 및 조치특성 갖는 복성 광맥내에 함은황인 및 황화광물과 함은tellurides 및 자연은 등을 포함하는 등 상대적으로 복잡한 광석광물 공생과계를 보여준다. 한편 황화광물의 지질온도계와 유체포유물 연구의 결과등에 의하면 백악기 금-은혼합형 광상과 은광단일형 광상은 천부(<0.5 kb)에서 천수가 우세한 광화유체로부터 $200^{\circ}{\sim}350^{\circ}C$ 온도조건하에서 주된 광화작용이 진행되었지만, 쥐라기 금광단일형 광상은 마그마기원의 열수용액으로부터 고온$(300^{\circ}{\sim}500^{\circ}C)$ 및 고압$({\approx}4-5kb)$의 생성환경하에서 광화작용이 진행되었음을 시사한다.