• 암석학회지
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• 제4권2호
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• pp.144-152
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• 1995

단양에서 동남동으로 약 6km 떨어진 천동리 지역에는 조선누층군의 최하부층인 장신규암과 영남육괴의 선캠브리아기로 추측되어온 엽리상 화강암(소위 화강암질 편마암)이 직접 접하고 있다. 이들의 관계는 전통적으로 장산규암이 엽리상 화강암을부정합으로 피복한 것으로 생각되었다. 그러나, 장판 규암의 하부에 관찰되는 소위 기저역암은 주로 규암으로 엽리상 화강암의 역을 전혀 가지고 있지 않아 두 암석 단위의 경계를 부정합으로 보기는 힘들다. 반면, 이지연의 최근 구조지질학적 연구는 이 경계가 여성전단운동에 의한 단층접촉임을 보이고 있다. 그러나, 이 전단대의 전단감각과 운동시기에 대해서는 아직 분명하지 않다. 우리는 옥동 단층의 일부인 천동리 지역 반취성전단대(semi-brittle shear zone)에서 나타나는 엽리상 패쇄암(foliated cataclasite)과 천매압쇄암(phyllonite)의 중구조 및 미구조 관찰하였는데, 이들은 북서측의 장산규암층이 남동측의 엽리상 화강암에 대해서 북동측으로 이동한 전단감각(top-to-the-northeast shearing)을 나타낸다(즉, 우수 주향이동), 전단운동의 시기를 제한하는 한 방법으로, 전통적으로 선캠브리아기루 추정되나 그 관입시기가 확인되지 않는 엽리상 화강암에 대하여 Pb-Pb 연대측정을 시도하였다. 즉, 구조운동을 받은 화강암체의 관입시기는 구조운동 시기으 l상한을 지시할 수 있기 때문이다. 엽리상 화강암의 전암 및 장석과 포획암의 전암에 대한 Pb 동위원소 자료는 $^{207}Pb/^{204}Pb-^{206}Pb/^{204}Pb$ 그림에서 $2.16{\pm}0.15$ Ga ($2{\sigma}$;MSWD=4.4)의 연대를 정의한다. 이 연대는 엽리상 화강암의 관입시기로 해석되는데, 보고된 영남육괴의 화성활동 시기와 잘 일치한다. 이 원생대 초기의 관입시기는 전통적인 생각기 옭음을 확인해 주며 전단운동의 시기를 알기위해서는다른 방법이 시도되어야 함을 지시한다.

• 자원환경지질
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• 제13권3호
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• pp.167-184
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• 1980

The granitic plutons associated with Ogcheon geosynclinal zone can be grouped into three different subzones; SE-Subzone for the migmatitic and schistose granites of the southeast margin, 101-181m.y. old; NW-Subzone for those of the northwest margin, 112-163m. y. old; and C-Subzone for those of central part of the zone, 63-183m.y. old. The intrusives in C-Subzone are further subdivided into the older, adamellite to granodiorite (148-183m.y. old) and the younger, perthitic granites (63-106m,y. old). The metallogenic distribution of South Korea suggests that, in the Ogcheon Zone, it is possible to delineate an elongated polymetallogenic province in the general orientation of the zone intimately related with the migmatite and plutonic zones mentioned. Moreover, the mineralization in the province was basically controlled by the patterns of local geology involving country rocks and related igneous bodies, that permit subdivision of the province into the following three parts: Northeast (NE) Province consists dominantly of thick Paleozoic calcareous sediments; Middle (M) Province is characterized by predominant argillaceous and partly calcareous sediments of Precambrian to Late Paleozoic age; and Southwest (SW) Province consisting mainly of volcanic and arenaceous sediments of Mesozoic age. The three different plutonic zones with three different country rock provinces above mentioned make a combination which consists of nine classes. Each class can be assumed to be characterized by specific mineralization type. In order to classify the mineralization types, the present study sampled twenty six ore deposits and mineralized areas in Ogcheon zone as shown figure 2; eight ore deposits from plutonic SE-Subzone, ten from the plutonic NE-Subzone and eight from the plutonic C-Subzone. The characteristics of the classes are as follows: NE-SE is predominant in Au-Ag vein and Sn-migmatite of katazonal occurrence; NE-C is most productive in Pb-Zn and remarkable in Fe contact deposit in mesozone and partly Pb-Zn-Cu skarn in limestone and subordinate in mesozone and partly Pb-Zn pipes; M-SE is considerable in Au-Ag vein and rare elements (Nb, Ta, etc.) of pegmatite; M-C is predominant in F-veins in epizone and Mo-W, Fe, Cu veins occur in replacement type; M-NW is productive in Fe metamorphic and skarn types, partly remarkable in Cu, Pb-Zn contact; SW-SE is barren in mineralization related to Jurassic igneous rocks; SW-C is predominant in alunite and pyrophyllite in tuffs; and SW-NW is scarece in Pb-Zn, Cu, As and Au-Ag veins.

• Design & Manufacturing
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• 제6권1호
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• pp.73-78
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• 2012

The aim of this dissertation is inferring factors controlling the complex strain behavior of the material and the characteristics of the Fine-Blanking in the most narrow area at the shear zone where we are performing the Fine-Blanking. And also this is for inspecting and presenting their uses and the possibilities to make the results data based in order to utilize easily. Therefore, to analyze of shere zone's strain behaviour, the Fine-Blanking process need to be modelled defining the quadratic-nodded and axi-symmetrical elements as the problems of large deformation axi-symmetry and the non-linear contact. For the method of inputting strain-stress values of the material, the piece-wise linear technics were used, the Implicit-Finite Element method also used making balance of forces on each step by the long intervals, calculates and converges many times was done. The materials used for the analysis was the Steel SNCM220 5.5mm respectively. As the result of FEM analysis, we know that shear stress value in the beginning of punch penetration is distributed widely and done high both in the center of the late-thickness and on the both sides centering around shear strain zone as the punch penetration is increasing. Also.

• 한국광학회지
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• 제19권2호
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• pp.116-121
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• 2008

본 연구는 2차원 PLS(Point Light Source) 배열과 디스플레이 장치의 조합을 통하여 시역형성용 광학판이 없는 3차원 영상을 재생하는 방법에 관한 것이다. PLS를 사용하여 3차원 영상을 디스플레이 하는 경우 기존의 시차장벽(parallax barrier), 렌티큘러(lenticular), 마이크로 렌즈(microlens lens) 등의 광학판을 사용할 때 발생하는 여러 가지 광학적 문제점 등을 해소할 수 있다. PLS로 사용된 LED 광원이 가져야 할 특성을 조사하였으며 PLS 배열을 통한 입체영상 디스플레이의 시역에 대해 실험을 통하여 입증 하였다.

• 한국윤활학회:학술대회논문집
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• 한국윤활학회 1998년도 제28회 추계학술대회
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• pp.106-114
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• 1998

Tribological investigation of ultra thin film magnetic storage disks which have two different kinds of start/stop zone of laser textured bump disk and mechanically textured disk for before CSS test and after CSS test. To measure surface roughness, height reduction before/after CSS test and obtain accurate topographies, AFM(Atomic Force Microscope) which is most powerful recently has been used. The result of statistical analysis showed that both laser textured bump height and mechanically textured zone height have been reduced about 4~7nm after 15000 cycle CSS test. Using commercial Nano-Indenter, ramping load scratch test has been performed to investigate friction characteristic for laser textured zone and mechanically textured zone before/after CSS test.

• 대한기계학회논문집
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• 제10권1호
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• pp.34-42
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• 1986

본 논문에서는 균열면이 원호(circular arc)를 이루고, Comninou 모델과 같이 균열면의 일부가 접촉되어 있는 경우 L적분이 적분경로에 무관함을 증명하고 이를 이용하여 재료가 서로 다른 원형 개재물과 기재와의 경계면에 존재하는 계면 균열에서의 응력확대계수를 구하는 방법에 대해 살펴보았다. 기지가 무한 고체이고 접촉역이 작아 접촉역의 존재가 균열선단에서 멀리 떨어진 곳에서의 응력장에 거의 영향을 끼치지 아`는 경우에는 접촉역을 가정하지 않은 문제에 대한 해, 즉 진동특성을 나타내는 해로 부터, L적분의 성질을 이용하여, 접촉역을 가정하였을 때의 응력확대 계수를 간단한 꼴로 표시할 수 있었고, 유한의 기지에 원형 개재물이 존재하는 문제에 대해서는 F.E.M을 사용하여 L적분을 계산함으로써 응력확대계수를 구할 수 있었다.

• 지질공학
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• 제20권1호
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• pp.71-78
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• 2010

강원도 삼척시 가곡면과 태백시 철암동에 위치한 가곡광산은 묘봉층 및 풍촌층내의 석회암과 화강반암의 접촉부에 배태된 접촉교대광산이다. 본 광산에서 지구물리탐사는 갱내 및 광산 주변부에 광화대의 부존 여부와 그 연장선을 파악하기 위하여 갱구 부근에서 자력탐사, 갱내에서 전기비저항 탐사 및 갱도-갱도 전기비저항 토모그래피탐사를 실시하였다. 자력탐사는 광화대의 영향으로 인한 이상대가 확연히 나타나지 않았지만, 전기비저항 탐사 및 토모그래피 탐사는 광화대에 대한 영상이 성공적으로 반영되었는데, 이는 본 연구지역에 존재하는 $N50^{\circ}W$계의 단층 연장선과 관련된 것으로 해석되어진다.

• 상하수도학회지
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• 제27권2호
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• pp.261-272
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• 2013

Algae boom (Red tide) in south coastal area of Korea has been appeared several times during a decade. If algae boom appears in the desalination plant, media filter and UF filter are clogged quickly, and the plant should be shutdown. In general, Algae can be removed from water by flotation better than by sedimentation, because of the low density of algal cell. The purpose of this study conducts the CFD simulation of DAF flotation basin to apply the design of the dissolved air flotation with ball filter in the Test Bed for SWRO desalination plant. In this study, Eulerian-Eulerian multiphase model was applied to simulate the behavior of air bubbles and seawater. Density difference model and gravity were used. But de-sludge process and mass transfer between air bubbles and seawater were ignored. Main parameter is hydraulic loading rate which is varied from 20 m/hr to 27.5 m/hr. Geometry of flotation basin were changed to improve the DAF performance. According to the result of this study, the increase of hydraulic loading rate causes that the flow in the separation basin is widely affected and the concentration of air is increased. The flow pattern in the contact zone of flotation basin is greatly affected by the location of nozzle header. When the nozzle header was installed not the bottom of the contact zone but the above, the opportunity of contact between influent and recycle flow was increased.

• 자원환경지질
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• 제7권3호
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• pp.101-122
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• 1974

The study area is located in between Susanri and Hwanggangri where the formations of Okcheon group and Chosun group supposedly come in contact so that the area is structurally very import. Present study reveals that the meta-volcanic rocks distribute from south to north along contact zone of Okcheon and Chosun groups in the center of the area. Meta-volcanic rocks seem to be originated from the andesite or andesitic basalt rocks which was known to be Surchangri formation consist of phyllite and black slate by previous workers. The meta-volcanic rocks intruded along the fault zone one existed between Okcheon and Chosun groups but obliterated at present by the intrusion of volcanic rocks. The fault seems to be overthrust, and one of the positive evidences of thrust fault is the Yamisan nappe structure in Yamisan near Susanri. This interpretation coincides with O.J. Kim's work which states that the Precambrian Okcheon group is largely overturned and thrusted over the Chosun group. The relation between the Surchangri and the Majeonri formation marks facies change. This fact together with northpluging anticlinal structure made it possible that both formation came into contact along direction without fault. Yongam formation is not overlain unconformably used to be believed by previous workers, but interbed in the Great Limestone series of Chosun goup. It is also clarified that the rock formerly designated as limesilicate rock was meta-liparite. The origin of amphibole pebbles in the Kunjasan formation is of primary and secondary ones; the secondary pebbles were formed by metamorphism of the fragments of limestone or dolomite.

• 로봇학회논문지
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• 제8권3호
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• pp.186-196
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• 2013

Since its introduction (e.g., [4, 6]), virtual coupling technique has been de facto way to connect a haptic device with a virtual proxy for haptic rendering and control. However, because of the single dependence on spring-damper feedback action, this virtual coupling suffers from the degraded transparency particularly during contact tasks when large device/proxy-forces are involved. In this paper, we propose a novel virtual coupling technique, which, by utilizing passive decomposition, reduces device-proxy position deviation even during the contact tasks while also scaling down (or up) the apparent inertia of the coordinated device-proxy. By doing so, we can significantly improve transparency between multiple degree of freedom (possibly nonlinear) haptic device and virtual proxy. In other to use passive decomposition, disturbance observer of [3] is adopted to estimate human force with some dead-zone modification to avoid "winding-up" force estimation in the presence of device torque saturation. Some preliminary experimental results are also given to illustrate efficacy of the proposed technique.