• 한국수산과학회지
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• 제32권5호
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• pp.674-679
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• 1999

The effect of wind on the circulation in Kamak Bay in the southern sea of Korea was examined using a numerical shallow water model. The experiments were primarily focused on how the effect of wind influence the tidal residual current. According to wind directions, the residual currents were changed; the westerly wind created a strong anti-clockwise eddy in the northwestern area of the bay where the flow field is usually very weak; the easterly wind strengthened the flow field in the central area of the bay; the patterns of flow fields to the north and south winds were almost the same as one without the wind, although the flow field became slightly stronger, The model flirty reproduced features in the observed current field at Pyongsa.

• 한국기계가공학회지
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• 제21권6호
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• pp.15-21
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• 2022

This study considered the internal flow considering the internal shape of the CNG filling nozzle, which is widely distributed in Korea. The CNG filling nozzle is the last part to pass through in the CNG filling process and has a significant influence on the filling efficiency. The mechanism was identified by disassembling the CNG filling nozzle and performing a flow analysis according to the mechanism. Consequently, the energy loss owing to eddy currents in the flow was determined, and modeling was proposed to reduce the energy loss by simplifying the shape and parts.

• 한국수산과학회지
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• 제13권4호
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• pp.151-162
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• 1980

온산만내에서는 대조시 조류가 우세한 편이지만 (0.1 kt), 소조시의 표층류는 매우 불규칙하며(0.07 kt), 취송류와 지형성 소용돌이의 영향을 크게 받는다. 대조시 만북부에서는 썰물 때 동류하고 밀물 때 서류한다. 만남부에서는 밀물은 서북서류하고 철물은 동북동류이다. 만외에서는 조류가 우세하여 밀물 때 남-남남서류하고 썰물 때 북-북북동류한다. 최대유속은 $1\~1.1kt$로 관측되었다. 소조시의 항류는 북북동 14.3cm/sec였다. 우봉갑 남쪽 만입부에는 밀물갈때나 썰물갈 때 지름 약 1km미만의 시계방향 소용돌이가 존재하여 해수의 정체성이 비교적 강한편이다. 겨울의 취송류는 대체로 남류하며 최대유속은 약 0.1kt에 달한다. 온산만내에서 점원방출한 염료는 바람에 의해 변형되면서 주로 조류에 따라 만구쪽으로 이동, 분산하였고, 방출 3시간후의 평균확산계수는 $4.4\times10^4cm^2/sec$ 였다. 만외 만입부 시계방향의 환류내에서는 이보다 다소 낮은 값을 보였다.

• Ocean Systems Engineering
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• 제6권1호
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• pp.23-60
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• 2016

The major objective of this study was to develop further understanding of 3D nearshore hydrodynamics under a variety of wave and tidal forcing conditions. The main tool used was a comprehensive 3D numerical model - combining the flow module of Delft3D with the WAVE solver of XBeach - of nearshore hydro- and morphodynamics that can simulate flow, sediment transport, and morphological evolution. Surf-swash zone hydrodynamics were modeled using the 3D Navier-Stokes equations, combined with various turbulence models (${\kappa}-{\varepsilon}$, ${\kappa}-L$, ATM and H-LES). Sediment transport and resulting foreshore profile changes were approximated using different sediment transport relations that consider both bed- and suspended-load transport of non-cohesive sediments. The numerical set-up was tested against field data, with good agreement found. Different numerical experiments under a range of bed characteristics and incident wave and tidal conditions were run to test the model's capability to reproduce 3D flow, wave propagation, sediment transport and morphodynamics in the nearshore at the field scale. The results were interpreted according to existing understanding of surf and swash zone processes. Our numerical experiments confirm that the angle between the crest line of the approaching wave and the shoreline defines the direction and strength of the longshore current, while the longshore current velocity varies across the nearshore zone. The model simulates the undertow, hydraulic cell and rip-current patterns generated by radiation stresses and longshore variability in wave heights. Numerical results show that a non-uniform seabed is crucial for generation of rip currents in the nearshore (when bed slope is uniform, rips are not generated). Increasing the wave height increases the peaks of eddy viscosity and TKE (turbulent kinetic energy), while increasing the tidal amplitude reduces these peaks. Wave and tide interaction has most striking effects on the foreshore profile with the formation of the intertidal bar. High values of eddy viscosity, TKE and wave set-up are spread offshore for coarser grain sizes. Beach profile steepness modifies the nearshore circulation pattern, significantly enhancing the vertical component of the flow. The local recirculation within the longshore current in the inshore region causes a transient offshore shift and strengthening of the longshore current. Overall, the analysis shows that, with reasonable hypotheses, it is possible to simulate the nearshore hydrodynamics subjected to oceanic forcing, consistent with existing understanding of this area. Part II of this work presents 3D nearshore morphodynamics induced by the tides and waves.

• 한국해양학회지
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• 제29권2호
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• pp.152-163
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• 1994

1967년부터 1986년까지의 국립수산진흥원의 관측자료를 사용하여 동해 남서해역에 서 난수성 소용돌이 (고기압성 소용돌이)의 구조 및 공간분포의 특성과 변동에 대해 연구하였다. 난수성 소용돌이는 울릉도 남서쪽 부근에서 자주 관측되며, 타원형이 많 고, 평균크기는 약 130 km이다. 난수성 소용돌이의 월별분포에 의하면 8월에 관측되는 빈도가 가장 많고, 6월에 가장 적다. 이것은 난수성 소용돌이의 발생이 동한난류 세력 의 발달과 관계가 있음을 나타낸다. 난수성 소용돌이는 서쪽이나 북쪽 또는 남쪽으로 0.80∼2.50 cm/sec의 속도로 이동하거나 한 장소에서 수개월동안 정체한다. 이러한 움 직임은 주변의 해류와 로스비파 및 지형의 영양을 받는다. 난수성 소용돌이의 분포아 해저지형과의 관계는 소용돌이의 이동과 발달이 울릉분지에 의해 영향을 받고 있음을 시사한다. 난수성 소용돌이는 크게 2개의 군으로 나눌 수 있다. 하나는 경압성의 특성 이 강한 수심이 얕은 소용돌이 군이고, 다른 하나는 순압성의 특성이 강한 수심이 깊 은 소용돌이 군이다. 부산과 일본의 모니와의 해수면 차이로 대마난류의 수송량을 추 정할 수 있는데, 수심이 얕은 소용돌이의 분포가 여름철 수송량이 클 때와 일치하였 다. 반면에 수심이 깊은 소용돌이 군은 대마난류의 수송량과 아무런 관계도 보이지 않 았다.

• 한국철도학회논문집
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• 제17권5호
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• pp.328-335
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• 2014

도시철도 지하역사 냉방 기류 및 냉방 효율을 조사하기 위하여 수치해법을 이용하여 해석하고 현장 실험 결과와 비교하여 분석하였다. 해석 대상 역사로는 지하 8층의 깊이 43.6m인 서울 5호선 신금호 역사를 선정하였다. 전체 역사를 해석 영역으로 하였으며, 공조기 모드는 평상시 모드로 고정시켰다. 냉방 공조를 위하여 대합실 천정에 총 94개의 정사각형($0.6m{\times}0.6m$) 환기구를 모델하였으며, 승강장은 총 222개의 환기구가 승강장 천정에 모델되었다. 대합실에서 급기되는 공기는 $47,316m^3/h$, 배기되는 공기량은 $33,980m^3/h$이며, 승강장에서 급기되는 공기는 $33,968m^3/h$, 배기되는 공기량은 $76,190m^3/h$로 현장의 풍량을 반영하였다. 승강장에서 스크린도어(PSD)는 닫힌 경우와 열린 경우 각각을 조사하였다. 총 750만개의 격자가 사용되었으며, 전체 영역을 22개의 다중 블록으로 나누어서 계산하고, MPI를 이용하여 각각의 블록에서 계산된 결과를 교환하였다. LES 기법을 이용하여 운동량 방정식 및 에너지 방정식을 계산하였다.

• Journal of Chest Surgery
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• 제20권3호
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• pp.458-472
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• 1987

A heart supplies bloods of about 15, 000 liters to each human organ in a day. A normal function of heart valves is necessary to this act of heart. The disease of heart valve develops to a narrowness of a closure, resulting in an abnormal circulation of bloods. In an attempt to eliminate the affliction of heart valves, the operation method to repair with artificial heart valves has been developed and saved numerous patients over past 30 years. This replacement operation has been performed since early 1960`s in Korea, but all the artificial heart valves used are imported from abroad with very high costs until recent years. The artificial heart valve using pyrolytic carbon has been developed at KAIST, which was proved to be stable in the mechanical performance and durability. Therefore, the in viva performance of this valve was examined through animal tests. The artificial heart valves used in this study are tilting disc type valves, in which the disc were made of graphite coated with pyrolytic carbon and the cages were made of titanium. In viva testings of these valves were performed in 12 dogs, in which right ventriculo-pulmonary arterial [Croup I] or inter-aortic [Croup IV] valved conduit was implanted using polytetrafluoroethylene conduits containing KAIST valve and aortic valve [Group II] or pulmonary valve [Croup III] was replaced by a KAIST valve with a 21mm or 19mm tissue annulus diameter. In group I and II, pre-and post-operative transvalvular pressure gradient was measured and compared with other prosthetic valves. During post operative period laboratory examination was performed including hemoglobin, hematocrit, red cell count, white cell, lactic acid dehydrogenase and platelet. The eight surviving dogs were sacrificed and autopsy was performed at 2, 6, and 8 weeks. KAIST valve has low transvalvular gradient and relatively high orifice area. Average ventriculo-aortic peak systolic transvalvular gradient was 14 mmHg in 21 mm valve and 19 mmHg in 19 mm valve. The valve has slight intravascular hemolysis effect. Thrombogenic effect of low polishing quality and eddy currents around small orifice is high. The valve has vulnerability of disc movement. These animal tests suggest that the improvement of the heart valve design, surface polishing state and prescription methods.

• Ocean and Polar Research
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• 제28권4호
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• pp.395-405
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• 2006

We measured the fugacity of $CO_2$ $(fCO_2)$, temperature, salinity, nutrients and chlorophyll a in the surface water of the western North Pacific $(4^{\circ}30'{\sim}33^{\circ}10'N,\;144^{\circ}20'{\sim}127^{\circ}35'E)$ in September 2002. There were zonally several major currents which have characteristics of specific temperature and salinity (NECC, North Equatorial Counter Current; NEC, North Equatorial Current; Kuroshio etc.). Surface $fCO_2$ distribution was clearly distinguished into two groups, tropical and subtropical areas of which boundary was $20^{\circ}N$. In the tropical Int surface $fCO_2$ was mainly controlled by temperature, while in the subtropical area, surface $fCO_2$ was dependent on total inorganic carbon contents. Air-sea $CO_2$ flux showed a large spatial variation, with a range of $-0.69{\sim}0.79 mmole\;m^{-2}day^{-1}$. In the area of AE (Anticyclonic Eddy), SM(Southern Mixed region) and NM (Northern Mixed region), the ocean acted as a weak source of $CO_2$ $(0.6{\sim}0.79 mmole\; m^{-2}day^{-1})$. In NECC, NEC, Kuroshio and ECS (East China Sea), however, the fluxes were estimated to be $-0.3mmole\; m^{-2}day^{-1})$ for the first three regions and $-1.2mmole\; m^{-2}day^{-1})$ for ECS respectively, indicating that these areas acted as sinks of $CO_2$. The average air-sea flux in the entire study area was $0.15mmole\;m^{-2}day^{-1})$, implying that the western North Pacific was a weak source of $CO_2$ during the study period.

• Investigative Magnetic Resonance Imaging
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• 제10권2호
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• pp.70-80
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• 2006

목적: 본 연구의 목적은 스핀에코(spin-echo) 자기공명영상 시퀀스 (sequence)에서 혈류 (blood flow)의 영상 저하를 줄이기 위한 새로운 경사자장 널링 (Gradient moment nulling) 방법 연구에 있다. 대상 및 방법: 스핀에코 시퀀스에서 사용하는 180도 펄스 주위에 혈류 보상과 동시에 180도 펄스의 불완전에서 생기게 되는 영상 저하를 줄일 수 있는 역할을 하는 경사자장을 이용한다. 이 경사자장은 혈류의 1차 (linear flow), 2차 (acceleration flow) 및 3차 (jurk flow) 운동에 대해 항상 같은 형태를 같기 때문에 통일된 경사자장의 형태를 갖는다. 이 기술을 이용하여 1차, 2차 및 3차 혈류 움직임에 의한 보상을 할 수 있는 스핀에코 시퀀스를 만들고 그 것을 펜텀과 사람의 뇌 영상에 사용하였다. 결과: 시뮬레이션을 이용한 혈류의 움직임에 대한 보상을 확인하였고 본 연구에서 제시된 새로운 기술이 기존에 제시된 기술에 비하여 향상된 결과를 펜텀 실험과 사람의 뇌 영상에서 보여 주었다. 결론: 본 연구에서 제시된 방법을 임상에 이용하면 혈류의 움직임에 대한 보상을 최적화 할 수 있으리라고 본다.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume I
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• pp.21-24
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• 2006

Processes controlling the interannual variation of mixed layer temperature (MLT) averaged over the NINO3 domain ($150-90^{\circ}W$, $5^{\circ}N-5^{\circ}S$) are studied using an ocean data assimilation product that covers the period of 1993 to 2003. Advective tendencies are estimated here as the temperature fluxes through the domain's boundaries, with the boundary temperature referenced to the domain-averaged temperature to remove the dependence on temperature scale. The overall balance is such that surface heat flux opposes the MLT change but horizontal advection and subsurface processes assist the change. The zonal advective tendency is caused primarily by large-scale advection of warm-pool water through the western boundary of the domain. The meridional advective tendency is contributed mostly by Ekman current advecting large-scale temperature anomalies though the southern boundary of the domain. Unlike many previous studies, we explicitly evaluate the subsurface processes that consist of vertical mixing and entrainment. In particular, a rigorous method to estimate entrainment allows an exact budget closure. The vertical mixing across the mixed layer (ML) base has a contribution in phase with the MLT change. The entrainment tendency due to temporal change in ML depth is negligible comparing to other subsurface processes. The entrainment tendency by vertical advection across the ML base is dominated by large-scale changes in wind-driven upwelling and temperature of upwelling water. Tropical instability waves (TIWs) result in smaller-scale vertical advection that warms the domain during La Ni? cooling events. When the advective tendencies are evaluated by spatially averaging the conventional local advective tendencies of temperature, the apparent effects of currents with spatial scales smaller than the domain (such as TIWs) become very important as they redistribute heat within the NINO3 domain. However, such internal redistribution of heat does not represent external processes that control the domain-averaged MLT.