• 전자공학회논문지B
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• 제33B권3호
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• pp.38-46
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• 1996

In this paper, a multi-velocity log system which uses ultrasonic pulsed doppler signal is developed. The output of the system is the absoluted velcocity of the ship. By using digitral signal processing, we get the vector velocity which displays the ship's speed about fore, aft, port and starboard. And this system give us the information about depth. This multi-velocity system has a large merit that is bottom and water track velocity. In addition, this has the high accuracy and can measure the water-depth according to the deep mode. And the fish finder, echo sounder or docking system will be made by applying the speed log system.

• 한국항만학회지
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• 제6권2호
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• pp.25-31
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• 1992

Herein we investigate the mass transport velocity caused by the viscosity near the ocean structure such as circular pile and inclined breakwaters. The mass transport velocity which is represented by the sum of the Eulerian velocity and the stokes drift were derived by Carter, Liu and Mei(1973). The tangential components of the inviscid velocity field at the bottom needed in the calculation of the mass transport velocity is obtained by solving the scattering problem due to breakwaters. The matched asymptotic expansion technique is employed to obtain the inviscid flow fields scattered by inclined breakwaters. The numerical results show that heary sediments tends to be deposited near the center of breakwaters and that the narrowing of the entrance width results in reduction of the magnitude of mass transport.

• 미생물학회지
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• 제29권5호
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• pp.329-338
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• 1991

From July 1985 to December 1986, 28 variables of phycal-chemical factors, bacteria and heterotrophic activity were investigated 17 times at 3 stations in the estuary of Naktong River and the influences of environmental factors to bacterial population and heterotrophic activity were analyzed through multiple regression. The results of multiple regression were as follows. At station 1, total bacteria and heterotrophic bacteria(Z-25) could explain 57% of the variation of maximum uptake velocity for glucose and 54% of turnover time for glucose was explained by total coliform bacteria and MBOD, Sixty four percent of the variation of Kt+SN was accounted for salinity, MBOD-N and inorganic phosphate. Turnover rate for acetate was also accounted for the change of MBOD-P by 56%. At station 2 maximum uptake velocity for glucose depends on MBOD-N by 81%; turnover time on bacteria by 50%; Kt+Sn on avilable nutrient by 61%. More than 50% of maximum uptake velocity and turnover time for glucose were influenced by bacteria and that of Kt+Sn by the change of nutrient in the surface water of station 3. In the bottom water of station 3, the change of maximumuptake velocity, turnover time and Kt+Sn for glucose was controlled by total bacteria and available nutrient, bacteria, the change of nutrient salts respectively. On the whole, more than 50% of maximum uptake velocity and turnover time for glucose could be due to the change in the number of bacetria and the value of Kt+Sn was affected by the change of nutrient salts. Turnover rate for acetate was controlled by available phosphate at station 1 and by bacteria at station 2 and 3, which showed a distinct difference between the environmental factors which govern the rate of glucose and acetate uptake in the Naktong esturine ecosystem. And bacterial communities were controlled by available nutrients at station 1, by nutrient salts and salinity at station 2 and in the surface water of station 3 and by salinity in the bottom water of station 3.

• 한국해안해양공학회지
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• 제15권3호
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• pp.151-158
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• 2003

잠제 주변의 유속장과 와의 발생에 대한 이해는 잠제의 소파메커니즘과 표사 및 구조물의 안정과 관련하여 중요한 기초자료로 활용될 수 있다. 본 연구에서는 일정한 경사수역에 설치된 불투과잠제 주변의 유속장의 해석과 와(vortex)서 발생을 수치적으로 모의하기 위해 자유수면의 추적기법인 VOF법에 기초하고 있는 김 등(2001, 2002)이 제안한 2차원 수치파동수로를 이용하였다. 특히, 잠제 주변의 정상류의 해석을 통해 잠제의 기하형상 및 파랑의 입사조건에 따른 와의 발생형태를 고찰하였다. 수치모의 결과 잠제 전면에서는 반시계 방향의 와가 발생하였고 잠제 후면에서는 시계방향의 와가 발생하였으며 와의 크기는 입사파고와 주기에 가장 민감하였다.

• 한국지열·수열에너지학회논문집
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• 제12권4호
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• pp.40-46
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• 2016

In order to improve air quality of indoor environment, studies of the underfloor air distribution (UFAD) system for application in buildings are actively in progress based on temperature and air flow distribution. However, although the age of air is the major evaluation parameter, there has been very little study on this parameter for the UFAD system. In this study, we investigated the age of air to reach the air diffuser, which is installed at the bottom of the interior by the UFAD system. Computational fluid dynamics simulations showed no regular pattern to the maximum value of the age of air in accordance with air flow rate and the velocity at air diffuser. These factors can be deduced from air movement by considering that air emitted from air conditioners was rotated according to the bottom shape of the floor, and then, the age of air in the rotation center was increased. The average age of air of internal interior was reduced considerably as the flow velocity at the underfloor air diffuser was increased from 0.5 m/s to 1.0 m/s However, the age of air was not substantially affected with change in the air volume. Moreover, when the flow velocity at the underfloor air diffuser was higher than 1.0 m/s, the age of air showed no significant difference with change in air volume or height of measurement. These results imply that indoor air quality is more substantially influenced by flow velocity than air volume, and the appropriate flow velocity is 1 m/s or more.

• The Journal of the Acoustical Society of Korea
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• 제26권2E호
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• pp.44-49
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• 2007

Donghae City - Ulleung Island Line (DC-UI Line) is a representative line for underwater and geoacoustic modeling in the middle western East Sea. In this line, an integrated model of P-wave velocity is proposed for a low-frequency range target (<200 Hz), based on high-resolution seismic profiles (2 - 7 kHz sonar and air-gun), shallow and deep cores (grab, piston, and Portable Remote Operated Drilling), and outcrop geology (Tertiary rocks and the basement on land). The basement comprises 3 geoacoustic layers of P-wave velocity ranging from 3750 to 5550 m/s. The overlying sediments consist of 7 layers of P-wave velocities ranging from 1500 to 1900 m/s. The bottom model shows that the structure is very irregular and the velocity is also variable with both vertical and lateral extension. In this area, seabed and underwater acousticians should consider that low-frequency acoustic modeling is very range-dependent and a detailed geoacoustic model is necessary for better modeling of acoustic propagation such as long-range surveillance of submarines and monitoring of currents.

• 한국수자원학회논문집
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• 제44권9호
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• pp.731-740
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• 2011

본 연구에서는 국내 기술로 개수로 흐름 측정에 활용할 수 있는 초음파 유속 프로파일러를 개발하였다. 이 유속 프로파일러는 초음파의 도플러 효과로 유속을 측정하는 원리에 기반을 두고 있으며, 도플러 주파수는 펄스반복주파수(Pulse Repetition Frequency) 기법에 의해 산정된다. 개발된 유속 프로파일러의 성능을 검증하기 위해 실내 실험 및 현장 테스트를 수행하였다. 실험 결과 개발된 유속 프로파일러는 바닥에서부터 약 0.1 cm 이상의 수심에서는 정상적인 유속 분포를 측정하며, 상용 유속센서 등과 비교하여 유사한 측정 성능을 가진 것으로 확인되었다.

• Wind and Structures
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• 제18권1호
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• pp.69-82
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• 2014

Flow around a small white fir tree was investigated with varying the length of the bottom trunk (hereafter referred to as bottom gap). The velocity fields around the tree, which was placed in a closed-type wind tunnel test section, were quantitatively measured using particle image velocimetry (PIV) technique. Three different flow regions are observed behind the tree due to the bottom gap effect. Each flow region exhibits a different flow structure as a function of the bottom gap ratio. Depending on the gap ratio, the aerodynamic porosity of the tree changes and the different turbulence structure is induced. As the gap ratio increases, the maximum turbulence intensity is increased as well. However, the location of the local maximum turbulence intensity is nearly invariant. These changes in the flow and turbulence structures around a tree due to the bottom gap variation significantly affect the shelter effect of the tree. The wind-speed reduction is increased and the height of the maximum wind-speed reduction is decreased, as the gap ratio decreases.

• 자원환경지질
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• 제44권3호
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• pp.229-238
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• 2011

가스하이드레이트 부존량 평가에 있어서 해당 부존 지역의 S파 속도 정보는 암상과 공극유체의 정보를 파악하는데 결정적인 역할을 한다. 만일 퇴적층 내에 가스하이드레이트가 존재한다면 이 층에서의 P파 속도와 S파 속도는 동시에 증가하게 되며, 그 하부에 자유가스가 존재하는 경우 P파의 속도는 감소한다. 하지만 S파의 경우 공극을 채우고 있는 유체의 영향을 받지 않고 순수하게 매질을 통해서 진행하므로 하이드레이트 층의 하부에 자유가스층이 존재한다고 해도 그 속도가 변하지 않거나 오히려 매질의 영향으로 그 속도가 증가한다. 본 연구에서는 이러한 특성을 확인하기 위해 울릉분지의 가스하이드레이트 유망지역 중 탄성파 단면상에서 BSR(해저변 모방 반사면)이 강하게 분포하는 한 지점에서 한국지질자원연구원이 2009년 5월에 OBS(해저면 탄성파 기록계)를 이용하여 취득한 해저면 다성분 탄성파 자료를 이용하여 가스하이드레이트 부존 심도 부근의 P파 빛 모드전환 S파의 속도를 구하였다.OBS의 하이드로폰(hydrophone) 성분에 기록된 P파 자료를 이용하여 탄성파 주시 역산법을 수행하여 P파 속도 및 섬도 구조를 도출하였다. 해당지역에 취득한 2차원 반사법 탐사 자료는 기본 전산처리를 통해 구한 탐사지역의 기본 층서모델을 초기모델로 삼았다. 여기에 수평 2성분 지오폰(geophone)에 기록된 자료의 극성 분석을 통해 S파의 에너지가 최대로 모인 radial 성분 단면도를 생성하고 여기서 발췌한 주요 S파 이벤트의 주시를 이용해 포아송 비 정모델링을 수행하여 OBS가 위치한 지점에서의 포아송 비와 S파 속도구조를 최종적으로 도출하였다. 본 연구를 통해 탐사지역의 가스하이드레이트 존재로 인한 BSR 상하부 층의 P파 속도 역전 현상과 P파와는 달리 BSR 상부에서 히부로 갈수록 S파의 속도가 약간 증가하는 경향을 보여 결과적으로 자유가스층의 존재로 인한 BSR 하부에서 포아송 비 감소현상이 뚜렷함을 확인하였다.

• 대한기계학회논문집
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• 제18권10호
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• pp.2675-2685
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• 1994

A study has been conducted to provide the experimental information for the velocity and temperature profiles of steam-air mixutre and to investigate their roles on the film condensation with wavy interface. Saturated gas mixture of steam-air was made to flow through the nearly horizontal$(4.1^{\circ})$ square duct of 0.1m width and 1.56m length at atmospheric pressure, and was condensated on the bottom cold plate. The air mass fraction in the gas mixture was changed from zero(W =0, pure steam) to one(W =1, pure air), and the bulk velocity was varied from 2 to 4 m/s. Water film was injected concurrently to investigate the effect of wavy interface on the condensation. The velocity and temperature profiles were measured by LDA system and thermocouples along the three parameters ; air mass fraction, mixture velocity and film flow rate. The profiles moved toward the interface with increasing steam mass fraction, mixture velocity and film flow rate. The Prandtl and Schmidt numbers were near one in the present experimental range, however there was no complete similarity between the velocity and temperature profiles of gas mixture. And the heat transfer characteristics and interfacial structure were coupled with each other.