• Proceedings of the IEEK Conference
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• 1998.10a
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• pp.649-652
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• 1998

본 논문에서는 MICROTEC〔3,4〕시뮬레이터를 이용하여 소트키 다이오드를 형성하고 금속-반도체 쇼트키 접촉에서 턴 온 전압과 항복 전압을 관찰하였다. 또한 여러 가지 쇼트키 장벽 높이를 가지는 금속을 사용하여 동일한 디바이스에서 이들 금속-반도체 접촉에 전압을 인가했을 때, 순 방향에서 턴 온 특성을 관찰하여 턴 온 전압과 역 방향에서의 항복 현상을 관찰하여 항복 전압을 확인하였다. 사용된 금속은 Au(0.8V), Mo(0.68V), Pt(0.9V), Ti(0.5V) 이며 반도체는 실리콘 n/n 구조가 형성되었다. 쇼트키 다이오드는 대 전력용 보다는 높은 속도의 스위칭 디바이스에 주로 응용되고 있으며 장벽의 높이가 높을수록 뚜렷한 정류 특성을 나타내어 순 방향 바이어스에서 빠른 턴 온 특성이 예상되는데 시뮬레이션 결과 또한 잘 일치하였다. 그리고 다이오드의 I-V 특성을 관찰하기 위해 역 방향 바이어스에서의 항복 전압을 관찰하였는데 쇼트키 장벽이 높을수록 낮은 항복 전압이 나타났다. 또한 디바이스 공정에서 epitaxial과 열처리 공정 후의 2차원적인 농도 분포를 나타내었다.

• Textile Coloration and Finishing
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• v.6 no.4
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• pp.92-99
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• 1994

혈액이 이물질과 접촉하면 응고하는 성질은 생명유지를 위해서는 단단히 중요한 일이나, 인공재료를 이용하여 질병을 치료하고자 할 때는 이러한 혈전형성은 장애요인으로 작용한다. 1960년대부터 최근까지 항혈전성을 가진 재료에 대한 연구가 활발히 전개되고 있는데 그 동향도 조금씩 변모하여가고 있고, 접근해가는 방식이 여러가지로 세분화되고 있다. 여러 논문과 총설, 혹은 서적을 참고로 하면 재료의 분류를 항혈전을 일으키는 메카니즘을 몇가지로 나누고 여기에 포함되는 것들을 열거하는 방식을 채택하고 있다. 한편, 의료에 직접적으로 관여하는 재료는 대부분이 섬유고분자재료가 차지하고 있으며 이분야의 관계자들의 의료에의 공헌도는 아주 높으며 의료 관계자로부터의 기대 또한 크다. 특히 혈액과 접촉하여 혈책적합성을 나타내는 재료또한 대부분이 섬유고분자재료가 차지하고 있기 때문에 섬유고분자재료의 입장에서 이들을 분류하고 각각의 항혈전성 메카니즘과 응용방식의 이해가 우선되어야 할 것이며, 이를 바탕으로 해야 좀더 진보된 형태의 항혈전성 섬유고분자재료의 발달이 가능하리라 본다. 따라서, 이 논문에서는 항혈전성을 나타내는 각각의 섬유고분자들을 그 중심으로 하여 항혈전성 재료를 소개하고자 한다.

• Proceedings of the KSME Conference
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• 2003.04a
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• pp.1021-1024
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• 2003

In this work, we fabricated various 2D metallic and polymeric nanopatterns with the feature resolution of sub-micrometer scale by using the method of microcontact printing ($\mu$ P) based on soft lithography. Silicon masters for the micromolding were made by e-beam lithography. Composite poly(dimethylsiloxane) (PDMS) molds were composed of a thin, hard layer supported by soft PDMS layer. Finally, monodisperse metal or polymer particles could be obtained in the prepared pattern for the application of electronic devices.

• Proceedings of the Korean Society of Precision Engineering Conference
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• 2003.06a
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• pp.1224-1226
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• 2003

In this work, we developed a high resolution printing technique based on transferring a pattern from a PDMS stamp to a Pd and Au substrate by microcontact printing Also, we fabricated various 2D metallic and polymeric nano patterns with the feature resolution of sub-micrometer scale by using the method of microcontact printing (${\mu}$CP) based on soft lithography. Silicon masters for the micro molding were made by e-beam lithography. Composite poly(dimethylsiloxane) (PDMS) molds were composed of a thin, hard layer supported by soft PDMS layer. From this work, it is certificated that composite PDMS mold and undercutting technique play an important role in the generation of a clear SAM nanopattern on Pd and Au substrate.

• Proceedings of the Optical Society of Korea Conference
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• 2000.02a
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• pp.230-231
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• 2000

최근 자동차, 항공기 등 연소과정을 수반하는 산업이 발전함에 따라 연소환경에 대한 관심이 높아지고 있다. 그런데 연소환경을 접촉식 방법으로 측정하게 되면, 측정기기가 연소환경에 영향을 주기 때문에 정확한 측정을 하기는 어렵다. 그래서 레이저를 이용한 비접촉식방법이 활용되고 있으며,$^{(1)}$ 그 중에서 LIGS(laser induced grating spectrosopy)나 DFWM(degenerate four wave mixing)$^{(1)}$ 은 신호대 잡음비가 높기 때문에 미세량으로 존재하는 분자를 검출하는데 유용할 뿐만 아니라 2차원 영상수집도 가능하다. 또한 LIGS의 시분해 신호를 분석하면 연소장내의 온도와 입자의 밀도 등을 산출할 수 있다. 본 실험에서는 대기압에서 불완전 연소장의 soot에 대한 신호를 수집, 분석하여 화염 위치에 따른 온도 변화와 soot의 농도 등을 정량적으로 조사했다.$^{(2)}$ (중략)

• Proceedings of the KSME Conference
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• 2003.11a
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• pp.1168-1173
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• 2003

When the tube contacted to support and antivibration bar of the steam generator in unclear power plant, the contact area is worn out by their relative displacement. In the study, wear depths of the tube inclined to tube support and antivibration bar are approximately predicted by a method using the contact load and relative displacement. In the case of the inclined contact, the results show wear depths of the steam generator tube predicted by the impact model are larger than those by the sliding model.

• The monthly packaging world
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• s.282
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• pp.93-101
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• 2016

딸기 포장재용으로 새로이 개발된 공중부양형 구조의 용기를 가지고 딸기가 유통 중 발생할 수 있는 짓물림 방지효과가 있는지를 분석하기 위해 일본 후쿠오카 현 쯔꾸시 시에서 도쿄까지 트럭과 항공기에 의한 수송시험을 했다. 일반적으로 사용되는 EPS용기는 수송 중 딸기 간 포장면적이 많아 흠집 발생면적이 컸으며, PET 트레이 위에 딸기를 배열시키는 '보통들이형 용기'는 과일끼리의 접촉부분에서 짓물림 현상이 많이 발생했다. 개발된 '공중부양형 용기'는 과일끼리의 접촉 없이, 유연한 PE필름으로 포장돼 수송 중 발생하는 딸기의 흠집 발생이 가장 적었다. 또한 'EPS 용기' 및 'PET용기'에 25Hz의 정상 진동을 가한 결과, 용기 내부에 발생하는 진동의 주파수 종류에 차이가 있음을 확인할 수 있었다. 'EPS용기'에서는 가진동의 25Hz보다도 큰 주파수의 진동을 많이 확인할 수 있었다

• The Journal of the Petrological Society of Korea
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• v.10 no.2
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• pp.57-81
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• 2001

In the amphibolites of the Hwanggangri area, three metamorphic zones are established like hornblende-actinolite zone (H-AZ), hornblende zone (HZ) and diopside zone (DZ) by the main mineral assemblages. Hornblende zone and hornblende-actinolite zone develope away from the diopside zone that experienced the highest thermal effect. Thus, this pattern identifies the decreasing metamorphic grade of the contact metamorphism with increasing distance from the granitic pluton. The mineral assemblages of this rock are classified into six representative groups such as $\circled1$ actinolite+plagioclase+chlorite, $\circled2$ actinolite+hornblende+plagioclase+chlorite$\pm$epidote$\pm$biotite, $\circled3$ actinolite+hornblende+plagioclass$\pm$biotite$\pm$epidote, $\circled4$ hornblende+plagioclase$\pm$biotite$\pm$chlorite, $\circled5$ hornblende+plagioclase+diopside+actinolite$\pm$epidote$\pm$chlorite, $\circled6$hornblende+plagioclase+diopside$\pm$biotite$\pm$epidote. Two metamorphic events m recognized in the amphibolites of the study area that the first metamorphism is the regional metamorphism dominantly occurred in the whole Ogcheon metamorphic belt and it gave rise to the growth of actinolite at the core or center of the amphibole grains of coarse and medium size. Its metamorphic grade ranges from the greenschist facies to epidote-amphibolite facies. The second metamorphism overlapped is the contact metamorphism caused by the adjacent granitic pluton, and its metamorphic grade is thought to reach to the low pressure part of upper amphibolite facies. According to the calculation by TWEEQU thermobarometry and amphibole-plagioclase thermometry, the metamorphic temperature of initial regional metamorphism is $439-537^{\circ}C$ under pressure of 4.6-7.3 kb and its peak temperature and pressure are considered to reach to the range of 492-537 and 5.2-7.3 kb. And the temperature range of contact metamorphism occurred by intrusion of cretaceous granitic body, is $588-739^{\circ}C$ under pressure of 2.6-5.2 kb and its peak temperature and pressure are estimated as having the range of $697-739^{\circ}C$ and 3.8-5.2 kb that this amphibolites are estimated to pass through the metamorphic evolution of both the rise of temperature and the drop of pressure.

• Economic and Environmental Geology
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• v.12 no.3
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• pp.147-176
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• 1979

The Yeonhwa II zinc-lead mine is characterized by a dozen of moderately dipping tabular orebodies of skarn and zinc-lead sulfides, developed in accordance with the ENE-trending bedding thrusts and bedding planes of the Pungchon Limestone and underlying Myobong Formation, mostly along the contacts of a ENE-trending sill and a NW-trending dike of quartz mononite porphyry. The orebodies occur in three groups: (1) the footwall Wolgok orebodies with respect to the sill, (2) the hangingwall Wolgok orebodies, and (3) the Seongok orebodies extended from dike contacts into carbonate beds. Mineral compositions of these orebodies are dominated by calc-silicates (skarn) associated with ore minerals of sphalerite, galena, and chalcopyrite, as well as sulfide gangue of pyrrhotite. A pair of exo- and endo-skerns in the Wolgok footwall contact aureole between the Pungchon Limestone and quartz monzonite porphyry on the -120 level represents a well-developed symmetrical pattern of mineral zoning: a garnet/quartz zone in the center of exoskarn, two zones of pyroxene with ore minerals on both sides of the garnet/quartz zone, further outwards-an epidote/chlorite-bearing hornfelsic zone in the Myobong slate beyond a zone of unaffected limestone, and an epidote-dominated zone of endo skarn on the opposite side toward fresh quartz monzonite porphyry. These features indicate a combination of two effects on the skarn formation: (1) differences in composition of the host rocks(sedimentary and ignous), and (2) progressive outward migration of inner zones on outer zones on the course of metasomatic replacement of the pre-existing minerals. Microprobe analyses of garnet, pyroxene, pyroxenoids, epidote, and chlorite for nine major elements on a total of 23 mineral grains revealed that: the pyroxenes are hedenbergitic, in most zones, with a gradual decrease of Fe- and Mn-contents toward the central zone, whereas the garnets are andraditic in outer zones, but are grossularitic in the central zone. This indicates a reverse relationship of Fe-contents between pyroxene and garnet across the exoskarn zones. Pyroxenoids are lacking in wollastonite but are dominated by pyroxmangite, rhodonite and bustamite, indicating a Mn-rich nature in bulk chemistry. Pseudomorphic fluorite after garnet occurs abundantly reflecting a fluorine-enhanced evidence of the skarn-forming fluids. Epidote contains 0.19-0.25mole fraction of pistacite, and chlorite is Mn-rich but is Mg-poor. Sulfide mineralization took place with the most Fe-rich pyroxene rather than with garnet as indicated by the fact that the highest value of hedenbergite mole fraction occurs in the ore-bearing pyroxene zone. The Yeonhwa II ores are characterized by high zinc and low lead in metal grade, with minor quantity of copper content in almost constant grade. The hangingwall Wolgok and Seongok orebodies, that formed in a more open environment with respect to their local configurations of geologic setting, are more variable in metal grades and ratios, than are the footwall Wolgok orebodies formed in a more closed condition in a narrow interval of sedimentary beds.

• The Journal of the Petrological Society of Korea
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• v.7 no.3
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• pp.190-206
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• 1998

The microstructures and time-relationship between deformation and growth of metamorphic minerals(metamorphism) of the Paleozoic metasedimentary rocks(Joseon Supergroup and Pyeongan Group) in the Janggunbong area at the central-south part in the North Sobaegsan Massif, Korea, have been analyzed in this paper. The first phase metamorphism (low-pressure type metamorphism), recognized as the crystallization of stack-type chloritoid and biotite and augen-type old andalusite, occurred under non-deformational condition before D1 deformation related to the formation of an E-W trending isocline-synclinal fold(Janggunbong fold) and associated its axial plane S1 foliation, and produced regional mineralogical zoning of E-W trend in the Paleozoic rocks. The second phase metamorphism(medium-pressure type metamorphism), related to the growth of staurolite and garnet porphyroblasts with straight or curved internal foliations(Si), occurred under non-deformational condition after D1 deformation related to the formation of E-W trending thrusts modifying the Janggunbong fold and during D2 deformation related to the formation of E-W trending Yecheon shear zone. This metamorphism also produced regional mineralogical zoning of E-W trend. After D2 deformation occurred the intrusion of Jurassic Chunyang granite and associated its contact metamorphism which crystallized patchy-type young andalusite and prismatic- or fibrous-type sillimanite and coarse-grained garnet. This metamorphism occurred under non-deformational condition before D3 deformation related to the formation of S3 crenulation cleavage and during early phase of D3 deformation, and formed narrow mineralogical zoning of N-S trend near Chunyang granite.