• 한국해양환경ㆍ에너지학회지
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• 제5권4호
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• pp.27-40
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• 2002

한국 남해연안에서의 해수순환을 알아보기 위하여 수치모델을 이용하여 개방경계에서 조석강제력에 의한 조류와 해수수송량을 이용한 해류를 재현하였다 주요 4대 분조에 의한 조류모델의 결과, 제주해협에서 최강 동향류 세기가 최강 서향류 세기보다 약 2배정도 더 크게 나타났다. 수치실험에 의해서 계산된 해류분포에서 거제도 남측에 나타나는 반원형의 해류분포가 나타났는데, 그 분포가 해저지형의 변화에 의해서 발생되는 것으로 수치실험을 통하여 밝혀졌다. 조류와 해류를 통시에 고려한 해수순환모델 결과, 제주해협에서는 남해로 유입되는 동향류가 우세한 반면에 남해에서 서해쪽으로 유출되는 서향류의 세기는 미약한 것으로 조사되었다. 이러한 견과는 장기적인 관점에서의 물질교환을 고려할 때, 고흥연안의 해상 부유물질이 제주해협을 통하여 서해쪽으로 이동하기 어렵게 만드는 원인중의 하나라고 판단된다.

• Computers and Concrete
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• 제26권5호
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• pp.377-384
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• 2020

A two-dimensional particle flow cod (PFC) is used to study the effect of missile impact on the concrete target. For this purpose firstly calibration of numerical model was performed so that tensile strength of numerical models and experimental sample were the same. Secondly, a concrete model was built. The number of concrete layers and the angle of concrete layers related to horizontal axis were changed. Their numbers were 1, 2, 3 and 4. The angles were 0°, 15°, 30°, 45°, 60°, 75° and 90°. A semi-circle missile was simulated at top of the concrete layers. Its velocity in opposite side of Y direction was 100 m/s. three measuring circles were situated at the below the missile in the model to receive the applied force. The load in the missile and measuring circles together with failure pattern were registered at the beginning of the impaction. The results show that concrete layers number and concrete layers angle have important effect on the failure load while the failure pattern was nearly constant in all of the models.

• 패션비즈니스
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• 제10권5호
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• pp.159-179
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• 2006

This research checked about the necessity for the development of men's dress forms in the first investigation for the educational circle and the men's wear industry. Somatotype characteristics were analyzed in the second investigation of body measurement with the subjects of 200 male adults in their twenties residing in Busan. The following are the results of the present research to develop male dress forms for patternmaking: 1. In the group analysis for the characterization of front body types, three somatotypes were found and named H, Semi X, and Y. In the cluster analysis of side body types, four types were identified: D, I, d, and q. In the combination of front and lateral body types, four kinds were chosen: semi X-I, semi X-q, semi Y-I, and Y-q. 2. Through the comparison of plane figures by the plaster method as well as horizontal and vertical cross sections by the sliding gauge method, semi X-I was finally chosen as the standard somatotype for male dress form development. 3. Compared with the sliding gauge method of the present dress forms, the research dress form reflected better the shapes of the parts of the back and hips and the position of the waist, especially for males in their 20's. In addition, the dress form in the current research had superior points in all the items of clothing evaluation. Based on the above results, the sizes and models of the men's dress forms for patternmaking were developed.

• 한국농촌건축학회논문집
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• 제14권4호
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• pp.11-18
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• 2012

This study is to establish the dwelling principle and architectural characteristics of Powhatan Indian Community in Eastern part of North America. To find a pattern and dwelling principle of town building and housing, I have researched both site survey of Powhatan at Jamestown Settlement in Virginia and a related references of North America Indian. In addition of study, I have tried to understand their life style in 17C, a spatial characteristics of space composition, and a using materials of Yehakin which means Powhatan's house in the exhibition hall of Jamestown Settlement. The results of this paper are as follows: First, the form of Powhatan house is like a longhouse which has two types that are oblong and rectangular house. Usually they had lived in the style of oblong house. Second, there are three patterns to set up the semi-permanent settlement of Powhatan, which are circle-type, street-type, and free-type of village. Third, the fire place of interior space that is most importance element to heat and cook is put it into the center of room, and the other beds and shelves are arranged by the side of wall which is covered of rush matt.

• 대한기계학회:학술대회논문집
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• 대한기계학회 2001년도 춘계학술대회논문집E
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• pp.772-776
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• 2001

The flow structures of turbulent shear layer behind oil fences with different tip configurations were investigated experimentally using flow visualization and PIV velocity field measurement. An oil fence was installed in a circulating water channel and the flow structure around the fence tip was mainly analyzed in this experiment. The four tip configurations tested in this experiment are knife edge; semi-circle edge, circular edge and rectangular edge. The 300 instantaneous velocity fields were measured using the single-frame PIV system and they were ensemble averaged to give the mean velocity field and spatial distribution of turbulent statistics. Free stream velocity was fixed at 10ms/sec and the corresponding Reynolds number based on the fence height was Re=4000. As a result, for the oil fence with rectangular edge, the streamwise velocity component was decreased. On the other hand it was increased for the oil fence with circular edge. For all four fences tested in this study, general flow pattern of the lower shear layer is analogous but the upper layer shows difference depending on the tip configurations. The oil fence with circular edge has more diffusive upper shear layer than that of the others. The shear layer of the oil fence with rectangular edge has relatively thin thickness. The oil fence with circular edge was found to be proper shape for tandem fence.

• 자원환경지질
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• 제38권6호
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• pp.633-642
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• 2005

동중국해 북부 대륙붕에 발달한 후기 홀로세 니질 퇴적체의 분포양상과 층서의 발달 특성을 밝히기 위해 고해상도 Chirp 탄성파 단면 자료를 이용하여 분석하였다. 고해상 탄성파 단면도상에서 음향기반암(기저 경계면 B)위에 2개의 퇴적층서(Unit 1과 2)가 나타나며 이들은 침식 경계면(중간 반사면 M)으로 경계된다. 하위 퇴적층서 Unit 1은 음향학적으로 평행 또는 준평행 반사층리와 수로 충진 퇴적상이 나타난다. 상위 퇴적층서 Unit 2는 반투명 내부 퇴적상과 7m 이하 퇴적두께의 렌즈형태로 발달해 있다. 시퀀스 층서분석으로부터 이들 퇴적층서는 마지막 저해수준 이후 형성되었다. 해침 퇴적체(Unit 1)는 최후 빙기동안 형성된 층서 경계면위에 바로 분포한다. 해침 퇴적체는 침식곡의 염하구 환경하에서 하천, 델타, 그리고 조간대 환경의 복합 퇴적물로 구성된다. 해침 퇴적체 바로 위는 침식 저지형의 최대 범람면이 나타난다. 최대 범람면위에 발달한 고해수준 퇴적체(Unit 2)은 저지대를 충진하는 니질 퇴적체로 구성된다. 니질 퇴적체는 제주도 남쪽 약 140km 떨어진 곳에 마치 태풍 같은 모양의 원형 형태로 수심 약 60-90m 사이에 집중적으로 발달해 있다. 이 퇴적체의 분포 면적과 부피는 각각 약 $3,200km^2$와 약 $10.7\times1109m^3$이다. 니질 퇴적체의 기원은 고황하와 양자강에서 배출된 부유퇴적물의 혼합기원으로 해석된다. 원형의 분포형태는 북부 동중국해에 발달한 반시계 방향의 와류 순환계로 인해 형성된 것으로 판단된다.