• 한국지구과학회지
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• 제23권3호
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• pp.259-269
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• 2002

북서태평양과 동해에서 채취된 4개의 코어는 퇴적구조, 생물교란정도와 내부침식면을 기준으로 과거 1만년 부근에서 상부와 하부로 구분된다. 특히, 시코쿠분지의 코어 KT94-10 상부퇴적물은 낮은 퇴적율, 높은 생물교란작용, 내부침식면, 사엽층리 등으로 특징지워지는데, 이러한 퇴적특징의 조합은 저탁류퇴적층이나 반원양성 퇴적물과는 다른 저층류퇴적물로 해석된다. 그러나 하부는 저층류의 영향을 받은 퇴적층이 관찰되지 않고, 생흔화석만 관찰되는 무구조 니질층의 특징을 보인다. 한편 동해 코어(95PC3)에서는 어떠한 저층류 관련 퇴적물도 관찰되지 않는다. 상부는 생물교란 니질층으로, 하부는 엽층리 니질층으로 구성되어 있으며 환원적 환경을 표시하는 황철석을 포함하고 있다. 결과적으로 북서태평양과 동해 코어의 퇴적특징은 심층류순환이 10,000년 전부터 빨라졌음을 표시하고 있다. 또 같은 시기일지라도, 심층수순환은 동해보다 북서태평양이 더 활발함을 보여주고 있다.

• Structural Engineering and Mechanics
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• 제64권2호
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• pp.233-241
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• 2017

Earlier numerous studies have been done on implementation of Tuned Liquid Damper (TLD) for structural vibration control by many researchers. As per current review there is no significant study on a sloped bottom TLD. TLD's are passive devices. A TLD is a tank rigidly attached to the structure and filled partially by liquid. When fundamental linear sloshing frequency is tuned to structure's natural frequency large sloshing amplitude is expected. In this study set of experiments are conducted on flat bottom and sloped bottom TLD at beach slope $20^{\circ}$, $30^{\circ}$ and $45^{\circ}$, for different types of structures, mass ratio, and depth ratio to investigate the overall effectiveness of TLD and specific effect of TLD parameters on structural response. This experimental study shows that a properly designed TLD reduces structural response. It is also observed that effectiveness of TLD increases with increase in mass ratio. In this experimental study an effectiveness of sloped bottom TLD with beach slope $30^{\circ}$ is investigated and compared with that of flat bottom TLD in reducing the structural response. It is observed from this study that efficiency of sloped bottom TLD in reducing the response of structure is more as compared to that of flat bottom TLD. It is shown that there is good agreement between numerical simulation of flat bottom and sloped bottom TLD and its experimental results. Also an attempt has been made to investigate the effectiveness of sloped bottom TLD with beach slope $20^{\circ}$ and $45^{\circ}$.

• 한국해안해양공학회지
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• 제6권1호
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• pp.72-80
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• 1994

임의의 수심 및 흐름 상 풍파의 변형에 대한 이산형 스펙트럼 모형을 구성하였다. 파랑의 성장 및 역풍감쇠, 저면마찰, 파랑과 흐름간의 상호작용이 고려되었고 제한 수심의 영향을 포함하기 위해 성숙파 스펙트럼에 수심에 의한 감쇠계수를 추가하였다. 이상의 모형을 수심을 고려한 가상풍장에 적용하여 수심 및 저면마찰에 대한 모형의 물리적 거동을 분석해 보았다.

• Transactions on Electrical and Electronic Materials
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• 제12권5호
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• pp.197-199
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• 2011

In this paper, the bottom-gate thin-film transistors (TFTs) were fabricated with an amorphous/microcrystalline Si double layer (DL) as an active layer and the variations of the electrical characteristics were investigated according to the DC bias stresses. Since the fabrication process of DL TFTs was identical to that of the conventional amorphous Si (a-Si) TFTs, it creates no additional manufacturing cost. Moreover, the amorphous/microcrystalline Si DL could possibly improve stability and mass production efficiency. Although the field effect mobility of the typical DL TFTs is similar to that of a-Si TFTs, the DL TFTs had a higher reliability with respect to the direct current (DC) bias stresses.

• Journal of the korean society of oceanography
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• 제39권1호
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• pp.1-13
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• 2004

The Yellow Sea Warm Current (YSWC) and the Yellow Sea Cold Bottom Water (YSCBW) are two protruding features, which have strong influence on the community structure and distribution of zooplankton in the Yellow Sea. Both of them are seasonal phenomena. In winter, strong north wind drives southward flow at the surface along both Chinese and Korean coasts, which is compensated by a northward flow along the Yellow Sea Trough. That is the YSWC. It advects warmer and saltier water from the East China Sea into the southern Yellow Sea and changes the zooplankton community structure greatly in winter. During a cruise after onset of the winter monsoon in November 2001 in the southern Yellow Sea, 71 zooplankton species were identified, among which 39 species were tropical, accounting for 54.9 %, much more than those found in summer. Many of them were typical for Kuroshio water, e.g. Eucalanus subtenuis, Rhincalanus cornutus, Pareuchaeta russelli, Lucicutia flavicornis, and Euphausia diomedeae etc. 26 species were warm-temperate accounting for 36.6% and 6 temperate 8.5%. The distribution pattern of the warm water species clearly showed the impact of the YSWC and demonstrated that the intrusion of warmer and saltier water happened beneath the surface northwards along the Yellow Sea Trough. The YSCBW is a bottom pool of the remnant Yellow Sea Winter Water resulting from summer stratification and occupy most of the deep area of the Yellow Sea. The temperature of YSCBW temperature remains ${\leq}{\;}10^{\circ}C$ in mid-summer. It is served as an oversummering site for many temperate species, like Calanus sinicus and Euphaisia pacifica. Calanus sinicus is a dominant copepod in the Yellow Sea and East China Sea and can be found throughout the year with the year maximum in May to June. In summer it disappears in the coastal area and in the upper layer of central area due to the high temperature and shrinks its distribution into YSCBW.

• 한국전기전자재료학회논문지
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• 제24권12호
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• pp.988-991
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• 2011

We fabricated a copper phthalocyanine (CuPc) based field-effect transistor with different device structure as a bottom and top contact FET. Also, we used a $SiO_2$ as a gate insulator and analyzed using a current-voltage (I-V) characteristics of the bottom and top contact CuPc FET device. In order to discuss the channel formation, we were observed the capacitance-gate voltage(C-V) characteristics of the bottom and top contact CuPc FET device.

• 대한조선학회논문집
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• 제41권6호
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• pp.102-113
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• 2004

A name of 'Sea Ship' and 'River Ship' had been used based on the comprehension for the difference of ship's hull form in Chosun period. We can find a number of literature describing the situation which transferred the cargo from Sea Ship to River Ship because Sea Ship could not go upstream in the river of which the current is fast and the water depth is low. The reason why Sea Ship could not go upstream was that the bottom of Sea Ship was narrow, it means the non-flat bottom. Generally Sea Ship had short length, wide breadth, so L/B of 2.2∼3.0, and high draft and depth. River Ship has long length, narrow breadth, so L/B of 5.0∼6.3, and low draft and the flat bottom in order to adapt to the low water depth of the river.

• 한국수산과학회지
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• 제36권2호
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• pp.187-192
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• 2003

To evaluate the oceanographic conditions for the artificial upwelling we measured vertical stratification coefficients, current speed distribution and grain size distribution of bottom sediment in the vicinity of Gukdo and Somaemuldo near Geojedo. There were a strong stratification between surface and bottom layers in summer, the stratification was weak from autumn to winter, and the water was well mixed during winter. In summer nutrient concentration of the bottom layer was 4 times higher than that of the surface layer. Underwater currents were strong in the bottom layer. We conclude that the oceanographic conditions in the area will meet the basic requirement for the construction of artificial upwelling.

• 대한토목학회논문집
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• 제13권1호
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• pp.105-114
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• 1993

밀도가 큰 유체의 유입으로 인한 소규모저수지의 바닥밀도류에 의한 순환이 수치해에 의하여 해석된다. 밀도류전면이 하류경계에 도달하기전에는 밀도류전면의 이동에 따라 침강점 하류에 형성된 반시계방향 와의 이동에 의하여 저수지내 순환과 혼합이 이루어지며, 밀도류전면이 하류경계에 도달한 후에는 하류경계에서 밀도류의 상승으로 인한 일종의 내부파가 형성되고 이 파의 상 하류 반복 전파됨에 따라 저수지내 혼합이 이루어지면서 밀도층의 두께는 증가한다. 하류경계에서 유출되는 유체의 희석은 유입밀도후르드수 Fre, 저수지길이, 시간의 함수이며 유출유체의 밀도가 일정값에 도달되는 시간은 저수지길이가 길수록, Fre가 작을수록 증가하는 것으로 나타났다.

• 한국정보디스플레이학회:학술대회논문집
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• 한국정보디스플레이학회 2005년도 International Meeting on Information Displayvol.II
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• pp.1025-1028
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• 2005

Microcrystalline Si (${\mu}c-Si$) TFTs were fabricated using a conventional bottom gate amorphous Si (a-Si) process. A unique ${\mu}c-Si$ deposition technique and TFT architecture was proposed to enhance the reliability of the TFTs. This three-mask TFT fabrication process is comparable with existing a-Si TFT procesess. In order to suppress nucleation at the bottom interface of Si, before deposition of the ${\mu}c-Si$ an $N_2$ plasma passivation was conducted. A typical transfer characteristic of the TFTs shows a low off-current with a value of less than 1 pA and a sub threshold slop of 0.7 V/dec. The DC stress was applied to verify the use of ${\mu}c-Si$ TFTs for AMOLED displays. After 10,000 s of application of the stress, the off-current was even lowered and sub-threshold slope variation was less than 5%. For AMOLED displays, OLED pixel simulation was performed. A pixel current of 13 ${\mu}A$ was achieved with $V_{data}$ of 10 V. After the simulation, a linear equation for the pixel current was suggested.