• 한국진공학회지
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• 제20권2호
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• pp.100-105
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• 2011

이온을 Si(100) 기판에 주입할 때 조사량과 에너지, 빔 전류가 면저항에 영향을 미치는 원인을 규명하기 위해 여러 연구자가 행하였던 실험과 동일한 조건으로 Crystal TRIM 프로그램을 이용하여 컴퓨터 시뮬레이션을 실행하였다. 주입한 $As^+$이온의 조사량을 $1{\times}10^{15}/cm^2$로 일정하게 하고 에너지를 5, 10, 15 keV로 변화시켜 계산한 결과 에너지가 커질수록 Rp값은 표면에서 깊어지는 반면에, 표면근방에 축적되는 격자손상은 증가하였다. 20keV의 B+이온을 $5{\times}10^{15}/cm^2$의 동일한 조사량으로 1mA와 7 mA의 빔 전류에 해당하는 값을 이용하여 계산한 결과 빔 전류가 커질수록 표면근방 100 nm 이내에서 격자손상이 증가하였다. 20 keV의 일정한 에너지로 B+이온을 $1{\times}10^{15}$, $3{\times}10^{15}/cm^2$ 조사량과 0.8 mA와 8 mA의 빔 전류로 각각 계산한 결과 조사량이 많아질수록, 빔 전류가 커질수록 표면 근방에 축적되는 격자손상의 양이 증가하였다. 이러한 에너지, 조사량과 빔 전류증가에 의한 시료표면의 격자손상 증가는 시료표면의 면저항을 감소시킨다.

• 대한전기학회:학술대회논문집
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• 대한전기학회 1999년도 하계학술대회 논문집 D
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• pp.1971-1973
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• 1999

Monolayers of azo-benzene group containing fatty acids(8A5H) were made by spreading and compressing on the water surface. These monolayers were optically stimulated by illuminating the lights of 365[nm] and 450[nm] from X-non lamp, and the structural changes of the molecules were measured by the displacement current method. Also, the dynamic behaviors of these monolayers were measured by the $\pi-A$ isotherms when changing the temperatures of the water surface. As results, when the monolayers were stimulated by 365[nm] light, the positive currents which were generated by the structural changes from trans to cis were measured. But the negative currents of the structural changes from cis to trans were too weak to detect. When the temperatures of the water surface were increased, surface pressures of the monolayers increased early because of the thermal activations of the molecules, and the double liquid film phase were disappeared upon $40[^{\circ}C]$.

• 한국물환경학회지
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• 제23권3호
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• pp.385-390
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• 2007

Reliable flow measurement for dry season is very important to set up the in-stream flow exactly and total maximum daily load control program in the basin. Especially, in the points which tidal current effects are dominant because reliability of the low measurement decrease. The reliable measuring methods are needed. In this study, we analysis the water surface elevation difference of water surface elevation. Quantity relationship to consider tidal currents in these regions. It is known that tidal current effects from Nakdong river barrage are dominant in Samrangjin measuring station. We developed multiple regression equation with water surface elevation, quantity, and difference of water surface elevation and compared these results water measured rating curve. All of these regression equation including linear regression equation and log regression equation fits better measured data them existing water surface elevation quantity line and Among three equations, the log regression equation is best to represent the measured the rating curve in Samrangjin point. The log regression equation is useful method to obtain the quantity in the regions which tidal currents are dominant.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume I
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• pp.352-355
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• 2006

In this study, the seasonal and inter-annual variation of sea surface current in the Gulf of Thailand were revealed through the use of WOD temperature and salinity data and monthly sea surface dynamic heights (SSDH) from TOPEX/Poseidon and ERS-2 altimetry data during 1995-2001. The mean dynamic height and mean geostrohic current were derived from the climatological data while SSDH data gave monthly dynamic heights and their geopstrophic currents. The mean geostrophic current showed strong southward and westward flow of South China Sea water along the gulf entrance. Counterclockwise eddy in the inner gulf and the western side of the gulf entrance associated with upwelling in the area. Seasonal geostrophic currents show basin-wide counterclockwise circulation during the southwest monsoon season and clockwise circulation during the northeast monsoon season. Upwelling was enhanced during the southwest monsoon season. The circulation patterns varied seasonally and inter-annually probably due to the variation in wind regime. And finally we found that congregation, spawning, and migration routes of short-bodied mackerel conform well with coastal upwelling and surface circulation in the gulf.

• Journal of information and communication convergence engineering
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• 제2권1호
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• pp.58-60
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• 2004

Sea level variations and sea surface circulations in the Korean seas were observed by Topex/Poseidon altimeter data from 1993 through 1997. In sea level variations, the West and South Sea showed relatively high variations with comparison to the East Sea. Then, the northern and southern area in the West Sea showed the range of 20∼30cm and 18∼24cm, and the northern west of Jeju island and the southern west of Tsushima island in the South Sea showed the range of 15∼20cm and 10∼15cm, respectively. High variations in the West Sea were results to the inflow in sea surface of Yellow Sea Warm Current (YSWC) and bottom topography. Sea level variations in the South Sea were due to two branch currents (Jeju Warm Current and East Korea Warm Current) originated from Kuroshio Current (KC). In sea surface circulations, there existed remarkably three eddies circulations in the East Sea that are mainly connected with North Korea Cold Current (NKCC), East Korea Warm Current (EKWC) and Tushima Warm Current (TWC). Their eddies are caused basically to the influence of currents in sea surface circulations; Cyclone (0.03 cm/see) in the Wonsan bay off shore with NKCC, and anticyclone (0.06 cm/see) in the southwestern area of Ulleung island with EKWC, and cyclone (0.01 cm/see) in the northeastern area of Tushima island with TWC, respectively.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2003년도 Proceedings of ACRS 2003 ISRS
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• pp.879-881
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• 2003

Sea level variations and sea surface circulations in the Korean seas were observed by Topex/Poseidon altimeter data from 1993 through 1997. In sea level variations, the West and South Sea showed relatively high variations with comparison to the East Sea. Then, the northern and southern area in the West Sea showed the range of 20${\sim}$30cm and 18${\sim}$24cm, and the northern west of Jeju island and the southern west of Tsushima island in the South Sea showed the range of 15${\sim}$20cm and 10${\sim}$15cm, respectively. High variations in the West Sea was results to the inflow in sea surface of Yellow Sea Warm Current (YSWC) and bottom topography. Sea level variations in the South Sea was due to two branch currents(Jeju Warm Current and East Korea Warm Current) originated from Kuroshio Current (KC). In sea surface circulations, there existed remarkably three eddies circulations in the East Sea that are mainly connected with North Korea Cold Current (NKCC), East Korea Warm Current (EKWC) and Tushima Warm Current(TWC). Their eddies are caused basically to the influence of currents in sea surface circulations; Cyclone (0.03 cm/sec) in the Wonsan bay off shore with NKCC, and anticyclone (0.06 cm/sec) in the southwestern area of Ulleung island with EKWC, and cyclone (0.01 cm/sec) in the northeastern area of Tushima island with TWC, respectively.

• International Journal of Aeronautical and Space Sciences
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• 제16권3호
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• pp.339-346
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• 2015

Aerodynamic flow control phenomena were investigated with a low-current DC surface discharge plasma actuator. The plasma actuator was found to operate in three different discharge modes with similar discharge currents of about 1 mA or less. Stable continuous DC discharge without audible noise was obtained at higher ballast resistances and lower discharge currents. However, even with continuous DC power input, a low-frequency self-pulsed discharge was obtained at lower ballast resistances, and a high-frequency self-pulsed discharge was obtained at higher set-point currents and higher ballast resistances, both with audible noise. The Schlieren image reveals that the low-frequency self-pulsed mode produces a synthetic jet-like flow implying that a gas heating effect plays a role, even though the discharge current is small. The high-frequency self-pulsed mode produces pulsed jets in a tangent direction, and the continuous DC mode produces a steady straight pressure wave. Particle image velocimetry (PIV) images reveal that the induced flow field by the low-frequency self-pulsed mode has flow propagating in the radial direction and centered between the electrodes. The high-frequency self-pulsed mode and continuous DC mode produce flow from the anode to the cathode. The perturbed region downstream of the cathode is larger in the high-frequency self-pulsed mode with similar maximum speeds.

• 건축사
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• 제3권7호통권7호
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• pp.21-29
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• 1968

It is axiomatic that all living things on the earth's surface are enveloped by an ocean of air at all times. An architecture meant to serve these creatures must naturally take into account problems posed by the currents in this ocean of air. Because air space is necessary to human life, it is a central concern of good architecture. In studying how to manipulate these spaces architecturally to best advantage, problems concerning the fluctuation of air currents should be a primary concern.

• 대한토목학회논문집
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• 제29권1B호
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• pp.73-81
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• 2009

본 연구에서는 개수로 흐름에서 오염물질 이동 현상에 대한 이차흐름의 영향을 분석하였다. 운동량 방정식과 스칼라 수송 방정식에서의 난류 폐합을 위해 레이놀즈응력 모형 및 GGDH 모형을 사용하였다. 개발된 모형을 이용하여 조 세립상의 횡방향 연속구조를 갖는 개수로 흐름에서의 오염물질 이동에 대한 이차흐름의 영향을 분석하였다. 그 결과, 이차흐름의 영향으로 인해 최대 농도 값의 발생 위치가 이동하는 것으로 나타났으며, 농도 분포 역시 정규 분포에서 거리에 따라 점차 왜곡 되는 것으로 확인되었다. 또한, 이차흐름의 영향으로 자유수면 근처에서는 매끄러운 하상에 비해 거친 하상에서의 오염물질 농도가 더 크게 발생되었으며, 스칼라-흐름률을 계산한 결과, 오염물질의 수직방향 확산은 매끄러운 하상에 비해 거친 하상에서 더 빨리 진행되는 것으로 확인되었다. 한편, 농도 분포 변화에 대한 이차흐름 및 스칼라-흐름률의 영향을 살펴보기 위하여 스칼라 수송률 분석을 수행하였다.

• 한국해양학회지:바다
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• 제13권1호
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• pp.56-66
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• 2008

서해 중부에 위치한 새만금 연안역에서 HF radar를 이용하여 2002년 7월과 2004년 9월부터 11월 초까지 표층해류를 관측하였다. 관측 자료로부터 조하주기대(subtidal) 표층해류가 해안선 변화, 바람과 담수 방류량의 변화에 대하여 시 공간적으로 어떻게 변동하는지 조사하였다. 2002년 7월 관측 기간 동안 바람이 약 0.5 m/s로 불었으며, 일 평균 금강 담수 방류량이 $0.88{\times}10^7$ 톤이었다. 시간평균된 표층해류($\overline{U}$)는 금강하구입구에서 $7{\sim}10\;cm/s$의 크기로 북서쪽으로, 방조제 개방구간에서 13 cm/s 이상의 크기를 갖고 서쪽으로, 고군산군도 북측에서는 북서방향의 분포를 보였다. 이는 금강 담수와 새만금 방조제 개방구간에서 유출된 조석 잔차류에 의해 형성된 흐름이다. 또한 를 제거한 표층해류의 공간평균치(<$U-\overline{U}$>)의 방향변화가 바람방향변화와 상대적으로 높은 상관관계(r=0.98)를 보였다. 2004년 9월부터 11월에는 북북서풍이 2.5 m/s로 불었으며, 일평균 담수 방류량이 $11.9{\times}10^7$ 톤이었다. 표층해류($\overline{U}$)는 대부분의 연안에서 크기가 작았고, 새만금 방조제와 고군산군도가 이루는 해안선을 따라서 약 10 cm/s의 상대적으로 빠른 해류가 남서방향으로 흘렀다. 이는 강한 북서풍이 금강 담수를 새만금 방조제 쪽으로 이동시켜 형성된 흐름이다. 2004년도에는 방조제 개방구간에서 유출되는 조석 잔차류가 없어졌으며, 공간평균()된 표층해류의 방향변화가 바람방향변화와 0.69의 상관관계를 보였다.