• 조명전기설비학회논문지
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• 제18권2호
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• pp.44-48
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• 2004

수표면을 전극으로 사용한 무성방전형 오존발생기를 제안하고 수중의 전도도 변화가 수표면 방전에 미치는 영향을 실험적으로 조사하였다. 수표면 방전에 중요한 영향을 줄 수 있는 요소로 방전공간내의 이온과 수중의 이온 및 극성분자등이 있다. 본 연구에서는 전도도를 변화시켜 수중에 존재하는 이온의 수를 조절함으로써 방전특성을 변화시키고자 하였다. 이를 위해 증류수내에 각각 다른양의 NaCl을 투입함으로써 전도도를 변화시켰고 이때의 전류-전압특성과 오존발생특성을 비교 조사하였다. 결과적으로 순수한 증류수를 사용한 경우보다 NaCl을 투입한 경우 안정된 방전을 발생시킬 수 있었고 투입하는 NaCl의 양을 늘여감에 따라 방전개시전압을 낮출 수 있었다.

• 대한전기학회:학술대회논문집
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• 대한전기학회 2002년도 하계학술대회 논문집 C
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• pp.1763-1765
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• 2002

A silent discharge type ozone generator using a water surface as an electrode has been proposed and investigated experimentally. A water surface has many Taylor cones when the ac voltage is applied on its surface, which increase the discharge surface greatly. In this paper, it was studied about the effect of the water conductivity. As increasing the water conductivity, the amount of generated ozone was increased and the silent discharge on the water surface took place steadily and calmly.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2002년도 Proceedings of International Symposium on Remote Sensing
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• pp.728-733
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• 2002

The measurement of river discharge is among the most fundamental observations and is necessary for understanding many water-related issues, such as flooding hazards, sediment transportation, and nutrient movement. Traditionally river discharge is estimated by measuring the water stage and converting the measurement to discharge using a stage-discharge rating curve. The possibility of monitoring river discharge from satellites has been largely ignored, because it is difficult to measure water surface information from space with sufficient precision. In this paper, an efficient approach to discharge estimation using mainly satellite data is developed and described. The proposed method, which focuses on the measurement of water-surface width coupled with river width-stage and stage-discharge relationships, is applied to the Yangtze River with good results.

• 상하수도학회지
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• 제25권5호
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• pp.627-634
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• 2011

In the present study, the flow behaviors of square jets surface discharged and submerged discharged into shallow water were each simulated using computational fluid dynamics, and the results were compared. As for the verification of the models, the results of the hydraulic experiment conducted by Sankar, et al. (2009) were used. According to the results of the verification, the present application of computational fluid dynamics to the flow analysis of square jets discharged into shallow water was valid. As for the wall jet, which is one form of submerged discharges, at the bottom wall boundary, the peak velocity of the jet rapidly moved from the center of the jet to the bottom wall boundary due to the restriction of jet entrainment and the no-slip condition of the bottom wall boundary, and, as for the surface discharge, because jet entrainment is limited on the free water surface, the peak velocity of the jet moved from the center of the jet to the free water surface. This is because jet entrainment is restricted at the bottom wall boundary and the surface so that the momentum of the central core of the jet is preserved for considerable time at the bottom wall boundary and the surface. In addition, due to the effect of the bottom wall boundary and the free water surface, the jet discharged into shallow water had a smaller velocity diminution rate near the discharge outlet than did the free jet; at a location where it was so distant from the discharge outlet that the vertical profile of the velocity was nearly equal (b/x =20~30), moreover, it had a far smaller velocity diminution rate than did the free jet due to the effect of the finite depth.

• 한국콘텐츠학회논문지
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• 제17권2호
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• pp.535-542
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• 2017

우리나라는 갈수기와 홍수기의 유량차이가 극심하여 수자원 관리에 대한 중요성이 대두되고 있는 실정이다. 하천의 특성을 파악하기 위해 정확한 유량을 산정해야 한다. 유량을 산정하기 위해서는 유량을 구하고자 하는 하도의 단면적을 산정하고, 해당 단면에서의 유속을 측정해 연속방정식을 이용하여 유량을 산출해야 한다. 보편적으로 수위-유량관계식으로부터 유량을 산정하지만, 이 경우에는 동일한 수심 동일한 유량만을 산출할 수밖에 없다는 단점이 있다. 그래서 본 연구에서는 낙동강 교량 강창교 지점의 성서관측소의 수심과 ADVM를 이용하여 측정된 수심을 이용한 수면경사와 ADVM지점의 수심을 이용하여 유량산정식을 개발하였다. 자연하천의 흐름은 정류나 등류가 아닌 부정류 흐름이기 때문에 하상경사가 아닌 수면경사를 반영하고자 본 연구에서는 두 지점의 측정된 수심으로부터 손쉽게 유량을 산정하는 방법을 제안하였다.

• 대한전기학회:학술대회논문집
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• 대한전기학회 2005년도 제36회 하계학술대회 논문집 C
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• pp.2193-2195
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• 2005

The hybrid discharge reactor was designed for the application of wastewater treatment and the removal of hazardous volatile organic substances in water. This discharge type was similar to the barrier discharge, and the surface discharge on the dielectric surface was propagated to the water surface. That caused the heterogeneous chemical reaction strongly at the interface between the working gases and the water surface. Changes of the conductivity, acidity, and the dissolved ozone with respect to the treatment time and water quantities were studied as the fundamental experiment. The concentration of hydrogen ions largely increased with increasing the treatment time and the conductivity increased with respect to the increase of water quantities under the constant other discharge parameters.

• 대한전기학회논문지:전기물성ㆍ응용부문C
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• 제50권7호
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• pp.334-339
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• 2001

A silent type ozone generator using water surface has been studied and improved its ozone generation characteristics by the controlling the height of Taylor cone by installing a mesh electrode, a dielectric bed of glass beads in the just under th surface of the water. The current-voltage characteristics and characteristics of ozone generation quantity of the test system were investigated and discharge current oscillograms of the each cases of the mesh electrode and the beds were observed and compared each other to analyze the discharge conditions. The Taylor cone height could be the cause of the discharge bridge to decrease the ozone generation on the discharge spacing. In this study, the hight of Taylor cone could be reduced greatly by installing the mesh and the glass beads bed just under the water surface. Therefore a higher ozone generation also could be obtained.

• 조명전기설비학회논문지
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• 제20권4호
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• pp.37-42
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• 2006

본 논문에서는$CO_2$를 발생시키지 않고 물로부터 직접 수소를 제조하기 위하여 비열플라즈마를 이용하였다. 다중침-평판형(Multineedle-plate electrode geometry reacto: MPER)과 단일침-평판형(Needle-plate electrode geometry reactor: NPER) 두종류의 수소제조 반응기를 설계 제작하여 수소 발생에 미치는 영향에 대하여 실험하였다. 수소발생을 높이기 위해서는 강한 아크성 스트리머 방전 발생과 효과적인 수표면 방전을 위한 수표면 조건을 고려해야만 된다.

• 조명전기설비학회논문지
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• 제17권3호
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• pp.56-63
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• 2003

수표면을 전극으로 사용한 부성방전형 오존발생기를 제안하고 수표면의 바로 아래에 유전체구를 설치함으로써 오존발생특성을 향상시킬 수 있었다. 이때, 서로 다른 유전율을 갖는 유전체구를 사용하여 수표면에 형성되는 방전조건을 변화시키고자 하였다. 전류-전압특성과 오존발생특성을 조사하였고 방전현상을 관찰하기 위해 유리구슬 유전체를 사용한 경우의 방전모양을 사진 촬영하여 분석하였다. 수표면에 발생되는 수돌기의 크기는 교락현상(breakdown)의 원인이 될 수 있고 따라서 오존발생량을 감소시킨다. 본 연구에서는 수표면 바로 아래에 서로 다른 유전율을 갖는 유전체구를 투입함으로써 과도한 크기의 수돌기(Tayler cone)의 놀이를 제한할 수 있었다. 이에 따라, 유전체구를 사용하지 않은 경우보다 많은 양의 오존을 발생시킬 수 있었다. 수중에 투입되는 유전체의 유전율이 증가함에 따라 방전이 시작되는 전압을 앞당길 수 있었고 강유전체구를 사용한 경우 최대 110[ppmv]의 오존발생량을 얻을 수 있었다.

• 한국해양공학회지
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• 제21권6호
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• pp.87-94
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• 2007

This study used POM (Princeton ocean model) improved for applying to coastal area in order to predict the distribution of thermal waste water. This model was applied to the coastal circulation and the effect of thermal waste water of Cheonsu-Bay. So this study compared the discharge of thermal waste water with each layer and section. The tidal current was about 1.5 m/sec at surface level and 0.9 m/sec on bottom level at flood tide; tidal current was about 1.3 m/sec on surface level and 0.8 m/sec on bottom level at ebb tide. The method discharging the thermal waste water in the nearshore region (case 1) accelerates the diffusion of the thermal waste water in the north-south direction(longshore direction). However, the method discharge the thermal waster water in the offshore region (case 2) reduced the diffusion of the thermal waste water over the coastal region. According th the diffusion region of the thermal waste water with case 1 and case 2 at three different layers (surface, middle, bottom), the diffusion region by case 1 discharge method generally influenced wider region (twice) than the one by case 2 discharge method with lower temperature between $1^{\circ}C\;and\;2^{\circ}C$, whereas the case 2 discharge method influenced the deeper region (middle and botton layers) with higher change of the water temperature ($1{\sim}3^{\circ}C$).