• 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.

• 자원환경지질
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• 제9권1호
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• pp.13-26
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• 1976

The basic rocks distributed in the Okchon paleogeosynclinal zone have been previously considered as intrusive in majority, but as sedimentary parensis in few variety. The present study is to find out some clues to conclude otherwise, if any, by clarifying 1) the nature and characteristics of the rocks, 2) type of the associated sedimentary rocks if any, and 3) their occurrence in related to regional geologic structure. The finding are as follows: 1) The basic rocks are identified and classified to hornblende gabbro, amphibolite, basalt and andesite (in part metamorphosed to meta-volcanics), green schist and peridotite(which appears in separate locality from the others). 2) Associated sedimentary rocks which appear to overlie the basic rocks are known as Kunjasan and Baekwhasan formations. The two formations are probably same, but been used differently by different authers at different localities. The rocks is exclusively consisted of cherty looking siliceous quartzite and some localitis it shows very calcarious nature. The formation seems to indicate a sort of pelagic siliceous sediments although it contain some pebbles. 3) The basic rock suites are always underlain by the same continuous, great thrust, which separates the Okchon paleogeosyncline zone from the neogeosynclinal zone in the area studied. The comparison of Okchon basic rocks suite to the ophiolite suites in other parts of the world indicates some similarity with which the writers suggested the probalility of Okchon basic rocks being ophiolites that occur along ancient geosuture line now represented by the great thrust.

• 한국정보통신학회논문지
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• 제3권3호
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• pp.639-650
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• 1999

본 논문에서는 정현파형 브러시리스 직류 전동기의 속도제어를 위해 두 개의 스위칭 라인에 의해 구성된 채터링 둔감영역을 갖는 가변구조 속도제어기를 설계한다. 슬라이딩 모드 과정 중 과도상태에서 발생하는 고주파 채터링을 저주파로 한정시키기 위해 데드 존(Dead Zone) 함수의 도입을 제안하고, 정상상태에서의 채터링 및 정상상태 오차를 제거하기 위해서는 제어입력에 시변이득을 적용한다. 제안된 데드 존 함수는 두개의 스위칭 함수로 구성된 슬라이딩 영역을 표시하며 이 영역에 시스템의 상태가 존재 시제어 구조를 PI제어기로 변경하여 채터링이 발생하지 않으며 이 영역의 이탈 시만 가변구조제어를 적용하므로 채터링이 발생하게 되어 과도상태의 고주파 채터링을 저주파로 감소시킬 수 있다. 설계된 속도 제어기에 대해 컴퓨터 시뮬레이션과 실험을 통하여 그 성능을 보인다.

• 한국분말재료학회지
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• 제29권1호
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• pp.8-13
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• 2022

In this study, we have prepared a Ti-6Al-4V/V/17-4 PH composite structure via a direct energy deposition process, and analyzed the interfaces using scanning electron microscopy (SEM) and transmission electron microscopy (TEM). The joint interfaces comprise two zones, one being a mixed zone in which V and 17-4PH are partially mixed and another being a fusion zone in the 17-4PH region which consists of Fe+FeV. It is observed that the power of the laser used in the deposition process affects the thickness of the mixed zone. When a 210 W laser is used, the thickness of the mixed zone is wider than that obtained using a 150 W laser, and the interface resembles a serrated shape. Moreover, irrespective of the laser power used, the expected σ phase is found to be absent in the V/17-4 PH stainless steel joint; however, many VN precipitates are observed.

• 생태와환경
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• 제46권3호
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• pp.332-342
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• 2013

주변 토지 이용이 다른 소부당과 명동저수지의 수변부와 개방수역간에 동물플랑크톤 군집 분포와 먹이망을 파악하기 위해 2011년 5월부터 10월까지 조사를 수행하였다. 소부당과 명동저수지의 동물플랑크톤은 각각 51종, 65종이 출현하였으며, 수변부와 개방수역간에 뚜렷한 밀도 차이를 보였다(t-test, P<0.05). 지각류와 요각류는 수변부에서 높은 밀도를 보인 반면, 윤충류는 개방수역에서 더 높은 밀도를 나타냈다(t-test, P<0.05). 수변부에서 출현한 동물플랑크톤 종은 주로 부착성 성향을 가진 종이었다(Lecane, Monostyla, Alona 그리고 Chydorus). Chl.a의 농도가 높은 명동저수지에서는 부유성 윤충류(Brachionus, Keratella 그리고 Polyarthra)의 높은 밀도가 관찰 되었다. Two-way ANOVA 결과, 윤충류는 서식처의 특성과 토지 이용이 다른 두 저수지간에 뚜렷한 차이를 보인 반면, 지각류와 요각류는 서식처의 특성에만 의존하는 것으로 나타났다. 저수의 영양상태가 주변 토지 이용과 밀접하게 연관되는 점을 감안하면, 윤충류는 서식처의 특성 뿐만 아니라 저수지의 영양상태에 따른 먹이자원에도 밀접하게 연관되는 것으로 보인다. 그러나 지각류와 요각류는 먹이자원보다 서식처의 특성에 주로 영향받는다. 안정동위원소 분석 결과, 부유성 Chl.a의 높은 값에도 불구하고 동물플랑크톤은 주로 부착입자 유기물에 대해 의존하였다. 이것은 실잠자리 유충, 검정물방개 그리고 새뱅이 같은 무척추동물과의 먹이 경쟁을 피하기 위한 것으로 사료된다. 결과적으로 동물플랑크톤 군집 분포는 습지의 공간적 특성 및 먹이자원에 의해 결정되는 것으로 보인다. 흥미로운 점은 동물플랑크톤 군집 밀도를 결정하는 수생식물이나 식물플랑크톤 등은 수체 내의 영양염류의 농도에 영향받으며, 이는 습지 주변 토지 피복이 매우 중요하게 고려된다는 것이다.

• 자원환경지질
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• 제2권4호
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• pp.73-90
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• 1969

The area studied is a southwestern part of Okcheon geosynclinal zone which streches diagonally across the Korean peninsula in the mid-central parts of South Korea, and is bounded by Charyeong mountain chains in the north and by Sobaek mountain chains in the south. The general trend of the zone is of NE-SW direction known as Sinian direction. Okcheon system of pre-Cambrian age occupies southwestern portion of Okcheon geosynclinal zone, and Choseon and Pyeongan systems of Cambrian to Triassic age in northeastern portion of the zone. It was defined by the writer that the former was called "Okcheon Paleogeosynclinal zone" and the latter "Okcheon Neogeosynclinal zone," although T. Kobayashi named them "Metamorphosed Okcheon zone" and "Non-metamorphosed Okcheon zone" respectively and thought that sedimentary formations in both zones were same in origin and of Paleozonic age, and C.M. Son also described that Okchon system was of post-Choseon (Ordovician) and pre-Kyeongsang (Cretaceous) in age. According to the present study two zones are separated by great fault so that the geology in both zones is not only entirely different in origin and age, but also their geolosical structures are discontinuous. Stratigraphy and structure of Okcheon system are clearly established and defined by the writer and its age is definitely pre-Cambrian. It is clarified by present study that the meta-sediments in and at vicinity of Charyeong mountain chains are correlated to Weonnam series of pre-Cambrian age which occupies and continues from northeast to southwest in and at south of Sobaek mountain chains, and both metasediments constitute basement of Okcheon system. Pyeongan, Daedong and Kyeongsang systems were deposited in few narrow intermontain basins in Okcheon paleogeosynclinal zone after it was emerged at the end of Carboniferous period. Granites of Jurassic and Cretaceous ages and volcanics of Cretaceous age are cropped out in the zone. Jurassic granite is aligned generally with the trend of Okcheon geosynclinal zone, whereas Cretaceous granite lacks of trend in distribution. Many isoclinal folds and thrust faults caused by Taebo orogeny at the end of Jurassic period are also parallel with Sinian directieon and dip steeply to northwest. Charyeong, Noryeong, Sobaek, and Deogyu mountain chains are located in areas of anticlinorium, and Kyongsang system in narrow synclinal zones. Folds in Okcheon neogeosynclinal zone are generally of N 70-80W direction but deviate to Sinian direction at the western parts of the zone. This phenomena is interpreted by the fact that the folds were originated by Songrim disturbance at the end of Triassic period and later partly modified by Taebo orogeny. Thrust faults of Taebo orogeny coentinue from Okcheon paleogeosynclinal zone into neogeosynclinal zone, forming imbricated structure as previously described. Strike-slip faults perpendicular to Sinian direction and shear faults diagonally across it by 55 degrees also prevail in neogeosynclinal zone. It is concluded from viewpoints on geology and geological structure that l)Okchon geosyncline had changed its location and affected by numerous disturbances through geologic time, and 2)mountain chains in the area such as Charyeong, Noryeong, Sobaek, and Deogyu were originated as folded mountains. Differing from others, however, Sobaek range was probably formed at the time of Songrim disturbance and modified later by Taebo orogeny. It is cut by Danyang-Jeomchon fault at the vicinity of Joryeong near Munkyeong village and does not continue to southwest beyond the fault, whereas southwestern portion of erstwhile Sobaek range continues to Taebaek rangd northeastward from Deogyusan passing through Sangju, Yecheon, and Andong. From these evidences, the writer has newly defined the erstwhile Sobaek range in such a way that Sobaek range is restricted only to northeastern portion and Deogyu range is named for the southwestern portion of previous Bobaek range.

• 한국해양공학회지
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• 제9권2호
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• pp.156-166
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• 1995

Regrading the development of offshore natural gas field near Sakhalin Island which is an ice-infested area, this study aims to estimate the dynamic ice load for construction of offshore structures operating in this region. In this paper the design ice load and dynamic responses of a slender Arctic structure upon continuous ice movement are sutdied. Crushing agter a certain elastic deformation is assumed as a primary failure mechanism at the contact zone between semi-infinite level ice edge and the face of structure. Dynamic interaction forces are calculated using a modified Korzhavin's equation and a two-dimensional ice-structure interaction model is adopted. To verify the numerical model, dynamic analysis is performed for on of the Baltic Sea channel markers whose response patterns were presiously observed.

• 한국분말재료학회지
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• 제10권1호
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• pp.26-33
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• 2003

Al-l4wt.%Ni-l4wt.% Mm(Mm=misch metal) alloy powders rapidly solidified by the gas atomization method were subjected to mechanical milling(MM). The morphology, microstructure and hardness of the powders were investigated as a function of milling time using scanning electron microscopy(SEM), transmission electron microscopy(TEM) and Vickers microhardness tester. Microstructural evolution in gas-atomized Al-l4wt.%Ni-l4wt.% Mm(Mm=misch metal) alloy powders was studied during mechanical milling. It was noted that the as-solidified particle size of $200\mutextrm{m}$ decreases during the first 48 hours and then increases up to 72 hours of milling due to cold bonding and subsequently there was continuous refinement to $20\mutextrm{m}$ on milling to 200 hours. Two microstructurally different zones, Zone A, which is fine microstructure area and Zone B, which has the structure of the as-solidified powder, were observed. The average thickness of the Zone A layer increased from about 10 to $15\mutextrm{m}$ in the powder milled for 24 hours. Increasing the milling time to 72 hours resulted in the formation of a thicker and more uniform Zone A layer, whose thickness increased to about $30~50\mutextrm{m}$. The TEM micrograph of ball milled powder for 200 hours shows formation of nano-particles, less than 20 nm in size, embedded in an Al matrix.

• 한국강구조학회 논문집
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• 제19권1호
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• pp.117-127
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• 2007

이 연구에서는 기둥에 축방향 하중을 받고 있는 강재 상자단면 접합부의 강도를 이론적 해석적 검토를 통하여 평가하였다. 2층 교각구조에서는 기둥에 작용하고 있는 축방향 하중의 영향으로 T형 접합부 강도가 저하되게 된다. 이러한 현상을 검토하기 위해 비선형 유한요소해석을 수행하였고, 실험결과와의 비교를 통하여 유한요소 해석프로그램 및 해석방법의 타당성을 검증하였다. 강재라멘교각 접합부의 설계변수 중 패널존의 폭-두께비 파라메타와 플랜지와 복부판의 단면적비 및 기둥에 작용하는 축방향 하중의 영향을 비선형 유한요소해석을 통하여 검토하였다. 또한 이 연구에서는 축방향 하중의 증가에 따른 T형 상자단면 접합부의 응력분포를 이용하여 이론적인 강도평가식을 유도하였다. 또한 1층 교각 구조의 상자단면 접합부 강도특성과 비교하였다. 결국, 패널존의 폭-두께비 파라메타와 단면적비의 영향을 고려하여 T형 접합부의 강도평가식을 제안하였다.

• ALGAE
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• 제23권4호
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• pp.317-326
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• 2008

Marine algal flora and community structure were investigated seasonally at three sites in Ilkwang Bay on the southern east coast of Korea from May 2007 to February 2008. Total 103 species including 10 of green algae, 17 of brown algae, 76 of red algae were collected and identified. Among these species, 21 species were found throughout the year. Ulva pertusa, Enteromorpha linza, Grateloupia lanceolata, Chondracanthus intermedia and Caulacanthus ustulatus were distributed dominantly in upper intertidal zone. By contrast, crustose coralline algae, Grateloupia spp., Chondracanthus tenellus, Prionitis cornea and Sargassum spp. occurred predominantly in middle intertidal zone. Grateloupia spp., Sargassum spp., Ecklonia cava and Ulva pertusa were dominant in lower intertidal zone. Annual mean biomass in wet weight was 478.3 g m$^{-2}$. Maximum biomass was recorded in site 1 (731.8 g m$^{-2}$), and minimum was recorded in site 3 (78.5 g m$^{-2}$). The R/P, C/P and (R + C)/P value reflecting flora characteristics were 4.47, 0.59 and 5.06, respectively. Two groups produced by cluster analysis, one including sites 1, 2 and the other including site 3, showed meaningful difference in similarity, each other. Site 3 showed the limited species composition due to inflow of fresh water and absence of solid substratum. However, there was no significant difference between site 1 and site 2. In conclusion, the number of marine algae species and biomass in Ilkwang Bay were markedly reduced comparing with the previous studies. These suggest that a solution for reconstruction of the poor marine algal vegetation is considerably demanded.