• Ocean and Polar Research
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• 제42권2호
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• pp.97-113
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• 2020

In-situ observations were carried out in April 2015 to investigate the occurrence of water temperature inversion in a region west of Jeju Island. Analysis of in-situ in the western part of Jeju island showed that cold water moved to the southeast from the surface to the middle layer and warm water moved from the middle to the lower layer of the northwest direction. The water temperature inversion occurred at 84 stations (63.1%) out of 133 stations. At the boundary of the water temperature inversion layer, it was formed in the middle layer and disappeared. In the strongly appearing, it started from the middle layer to the lower layer. The shape of the water temperature inversion layer was different. As a result of horizontal water temperature slope analysis of the water temperature inversion zone, maximum 0.23℃/km was obtained and the mean was 0.06℃/km. The role of water temperature inversion as an indicator to determine the formation of water front. As a result of the water mass analysis, Jeju Warm Current Water and Tsushima Warm Current Water of high temperature and high salt intruded from the middle to the bottom. In the middle layer occurred as the Yellow Sea Cold Water of low water temperature and low salinity expanded.

• Ocean and Polar Research
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• 제44권3호
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• pp.191-207
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• 2022

Using the results of CTD casts made in Spring from 2017 to 2021, in this study we investigated the water mass distribution and occurrence of temperature inversion in the western seas of Jeju Island in spring. The distribution of water masses was characterized by cold and fresh water in the northwest and warm and saline water in the southeast, forming a strong thermohaline front running in the southwest-to-northeast direction. Strong temperature inversion mainly occurred in the frontal boundary when the cold water intrudes beneath the warm water at depths of 30-50 m. Analysis of the mixing ratio demonstrated that Jeju Warm Water is dominantly distributed in the western seas of Jeju Island, but its ratio can be modified depending on the southward extension of Yellow Sea Cold Water (YSCW). Results of in situ measurement showed that in 2020, the YSCW largely expanded to the western seas of Jeju Island, occupying approximately 40 % of the mixing ratio. Due to the expansion of YSCW, a strong thermohaline front was formed in the study area, thereby causing thick and strong temperature inversion. On the other hand, in 2018 the mixing ratio of YSCW was minimum (~18%) during the study period of 2017-2021, and thus a relatively weak frontal boundary was formed, without the occurrence of temperature inversion. The observational results also suggest that the interannual changes of water mass distribution and the associated temperature inversion in the western seas of Jeju Island are closely related with wind-driven Yellow Sea circulation in spring, which is the summer monsoon transition period.

• 해양환경안전학회지
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• 제15권3호
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• pp.165-171
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• 2009

1999년 10월, 12월의 국립수산과학원 정선관측 자료를 이용하여 수온역전 현상이 성층변동에 미치는 영향을 분석하였다. 10월, 12월 모두 수심 25-75m 사이에서 수온역전현상이 빈번하게 발생하며, 12월에는 표층 부근에도 수온역전현상이 나타났다. 고온, 고염분수인 쓰시마난류의 수평 이류가 10월, 12월에 나타나는 수온역전현상의 주원인으로 작용하며, 12월에는 연안역에서 외양역으로 수송되는 차가운 표층수의 영향이 함께 작용한다. 10월에는 북풍이 지속적으로 불지만 남해연안수가 외해역으로 확장하는 현상이 뚜렷하지 않는 반면, 북서풍계열의 풍속이 강해지고 쓰시마난류의 세력이 약해지는 12월에는 남해연안수가 상층부를 통해 외해역으로 확장하면서 수온역전현상을 나타나게 한다. 10월과 12월 모두 수온역전현상이 발생하는 해역을 따라 성층의 변동폭이 크게 나타난다.

• 한국해양학회지
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• 제27권4호
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• pp.259-267
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• 1992

황해동부에서 1991년 4월에 관측된 CTD자료를 분석한 결과, 해수의 직구조는 계절적 수온약층과 수온역전층에 의해 뚜렷이 구분되는 상부혼합층 및 중층저온수로 저층 고온수 삼층구조를 보여준다. 조사지역 남부에서 저층수는 중층수보다 수온이 $3^{\circ}C$ 높아 수온역전이 가장 뚜렷하다. 수온역전은 $100{\;}km{\;}{\times}{\;}100{\;}km$의 관측해역에 걸쳐 형성 되었고 약 1.5개월후에도 관측되었다. 이 저층수의 수온과 염분은 단면내 핵구조 및 남쪽에서 분쪽으로 향하는 설상분포를 보여, 조사해역 남쪽에 있는 봄철 해양전선의 해수가 북쪽으로 150 km 정도의 거리에 걸쳐 황해냉수 아래로 요입된 것을 제시한다.

• 해양환경안전학회지
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• 제10권1호
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• pp.55-59
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• 2004

1995년도 1996년 6월에 실시된 CREAMS 항해 관측 자료를 이용하여 Wasaka bay 연안역의 수온역전 현상을 조사하였다. 수온역전현상은 대부분 20m 이천의 상층부에 위치하였으며, 특히 쓰시마난류와 연안수와의 경계역 부분에 형성되었다. 쓰시마난류는 고온${\cdot}$고염분수의 특징을 가지며, 이러한 고수온은 경계역 부분에서 수온역전 현상을 초래하여 밀도 역전현상을 일으키는 작용을 하는 반면, 고염분은 밀도를 증가시켜 주는 작용을 하여 수온역전에 따른 밀도역전현상을 막아주는 역할을 한다.

• 한국응용과학기술학회지
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• 제21권4호
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• pp.267-273
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• 2004

에멀젼 구조가 변하는 에멀젼 변환은 이미 40년 전에 알려졌다. 에멀젼 변환에서는 O/W 에멀젼이 W/O 에멀젼으로, 또는 이와 반대로 구조가 변하므로 연석상과 분산상이 서로 바뀌게 된다. 그러나 3상 에멀젼에서는 이와 같은 에멀젼 변환뿐만 아니라 어떤 특정한 온도에서 연속상은 변하지 않고 분산상의 구조가 바뀌는 현상이 관찰되었다. 이 현상을 에멀젼이라고 불렀으며 에멀젼 전이가 일어나는 온도를 에멀젼 전이 온도라고 하였다. 에멀젼 전이는 이론적인 고찰의 결과이었으며 양친매성 분자/기름/물의 두 3성분계에 대해서 실험적으로 관찰하였다. 이는 이제까지 보고되지 않았던 새로운 현상이다. 본 논문에서는 에멀젼 전이와 에멀젼 전이를 비교 분석하였다.

• 공업화학
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• 제5권2호
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• pp.274-284
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• 1994

비이온성 계면활성제 $C_{12}E_5$, 비극성 오일 n-hexadecane, 물을 포함한 계에 oleyl alcohol 혹은 oleic acid 같은 극성 성분을 첨가했을 때의 Phase Inversion Temperature (PIT)를 측정한 결과, 첨가한 극성성분은 친유성 첨가제와 같이 PIT를 급격히 감소시킴을 알 수 있었다. PIT에서의 microemulsion phase의 surfactant film 조성 계산에 의하면 surfactant film에서의 극성 성분/계면활성제 비율이 증가할수록 PIT는 감소하였다. 또한 극성 성분의 첨가는 PIT에서의 microemulsion phase의 부피와 오일, 물의 solubilization parameter에도 큰 영향이 있었다. PIT의 감소에 따라, 예를 들면 극성 성분의 첨가량을 증가시킴에 따라, microemulsion phase의 부피는 급격히 증가하였으며 아울러 오일, 물 모두의 microemulsion phase에 대한 solubilization parameter가 급격히 증가하였다. 본 연구 결과를 비교할 수 있는 세척력 실험결과는 현재 없지만 PIT의 측정은 middle-phase microemulsion phase가 형성되는, 즉 많은 양의 오일을 제거할 수 있는 조건을 예측할 수 있는 유용한 방법임을 알 수 있었다.

• 설비공학논문집
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• 제3권5호
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• pp.386-394
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• 1991

Freezing of saturated porous media contained in a rectangular cavity has been studied experimentally. Water and different diameter glass beads consitituted the liquid and porous media. Solidification front shape, the effects of bead diameter and initial liquid temperature was investigated. When the hot wall temperature was below $4^{\circ}C$, the freezing rate was higher at the top than at the bottom due to the density inversion, but with increasing the hot wall temperature the freezing rate at the top was effected by the liquid temperature and was lower than at the bottom. With increasing the bead diameter, the difference of freezing rate between top and bottom was increased and depends on thermal conductivity. When the liquid temperature was low in the beginning, the freezing rate was high, but with increasing the time almost the same with those of high temperature liquid.

• 설비공학논문집
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• 제9권2호
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• pp.104-111
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• 1997

The freezing phenomenon of saturated water with the supercooled region in a horizontal circular cylinder has been studied experimentally by using the holographic real time interferometry technique. From the experiments, it was found that there were three types of freezing patterns. The first is the annular ice layer growing from the cylinder surface at a high cooling rate; the next is the asymmetric ice layer at a moderate cooling rate; and the last is the instantaneous ice layer growth over the full region at lower cooling rate. As the water was coolde from room temperature to the subfreezing point passing through the density inversion point, the freezing pattern was largely affected by the inversion phenomenon, which had much effected the free convection and was susceptible to influences from the cooling rate. When the cooling rate is high, supercooling energy is released before the water is sufficientry mixed by free convection. On the other hand, when the cooling rate is low, there is much time for the water to be mixed by free convection. This seems to be the reason why the different ice layer growths occur.

• 한국군사과학기술학회지
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• 제24권5호
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• pp.482-491
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• 2021

It is obvious that understanding the effects of shallow water environment of Korea is very important to guarantee the optimal performance of active sonar such as monostatic and bistatic sonar. For this reason, in this paper, we analyzed the detection performance characteristics for various depth deployments of sonar in summer, winter and water temperature inversion environments, which environments are frequently observed in shallow water of Korea such as the Yellow sea. To analyze only effects of water temperature structures on target detection performance, we applied range independent conditions for bottom, sea surface and water temperature characteristics. To understand the characteristics of detection performance, we conducted transmission loss and signal excess modeling. From the results, we were able to confirm the characteristics of detection performance of active sonar. In addition, we verified that operation depth of transmitter and receiver affects the detection performance. Especially in the water temperature inversion environment, it was confirmed that the shadow zone could be minimized and the detection range could be increased through bistatic operation.