• 한국가스학회지
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• 제19권1호
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• pp.51-56
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• 2015

To assess downward positions of water spray for the small-scale release of chlorine gas, dispersion coefficients for the Gaussian dispersion model were validated at the small-scale release experiment. And the downwind distances of water spray were assessed with the simulated results. As results, the Gaussian plume model using the Briggs' dispersion coefficient well estimated the dispersed characteristics for small-scale release of chlorine gas. The best adequate downwind position of water spray is the position of the maximum concentration of chlorine at the ground level. And the adequate vertical and horizontal dimensions of water spray consider the maximum width and height of cloud.

• 한국추진공학회지
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• 제13권3호
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• pp.34-40
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• 2009

카본슬러리 연료 제조 시 카본의 분산안정성에 미치는 공정변수의 영향을 조사하였다. 카본슬러리연료의 분산안정성은 위치별 입도분석, 카본함량 분석, 그리고 원심분리 후 분산상태 관찰을 통해서 측정하였다. 여러 종류의 첨가제를 적용한 결과, NB463S84 사용시 분산성과 분산안정성이 가장 우수한 것을 알 수 있었다. NB463S84와 비슷한 작용기를 가지는 PIBSI를 합성하였으며, 이를 카본슬러리 연료에 적용하여 유사한 분산안정도를 얻었다. 끝으로 g 규모에서 얻은 제조 조건을 kg 규모 제조에 적용하여 카본슬러리 연료의 실용화 가능성을 확인하였다.

• 한국가스학회지
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• 제8권1호
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• pp.13-17
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• 2004

무거운 독성가스의 소규모 누출에 대한 가우시안 연속모델의 적용성을 평가하기 위하여 염소가스의 소규모 누출에서 염소농도의 실험값과 여러 가지 분산계수를 사용한 가우시안 연속모델에 의해 산출한 이론값을 비교하였다. 그 결과, 염소가스 분산은 분산계수와 대기안정도에 따라 상당히 차이가 있었으며, 염소농도는 Briggs의 분산계수와 유효 누출높이를 사용한 가우시안 연속모델에 의해 비교적 정확하게 산출할 수 있었다.

• 대한기계학회:학술대회논문집
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• 대한기계학회 2001년도 춘계학술대회논문집E
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• pp.94-99
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• 2001

The numerical simulation of the particle dispersion in the vortical flows provides insight into the mechanism of particle-fluid interaction. The simulation results show that the mixing layers are characterized by the large-scale vortical structures undergoing pairing process. The particle dispersion is strongly influenced by the large-scale structures and the particle sizes. The analysis shows that the mixing layers grows like a step-function.

• 한국가스학회지
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• 제8권2호
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• pp.8-14
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• 2004

본 연구는 염소가스의 소규모 연속누출에서 분산특성과 독성영향을 해석하였다. 염소 농도의 실험값과 이론값을 비교한 결과, Briggs의 분산계수와 유효누출높이를 사용한 가우시안 모델이 BM 모델보다 적용성이 우수하였다. 또한 가우시안 모델에 의해 염소농도를 산출하고 해석한 결과, 염소분산은 누출속도 보다 대기안정도와 바람속도에 크게 영향을 받으며, 독성영향은 염소분산에 미치는 매개변수의 영향과 유사한 경향을 나타내었다. 이때, 여러 독성기준에 의해 산출된 피해범위로부터 인명을 보호하기 위한 위험지역을 파악할 수 있었다.

• 한국추진공학회:학술대회논문집
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• 한국추진공학회 2008년도 제31회 추계학술대회논문집
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• pp.459-462
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• 2008

슬러리 연료 제조 시 카본의 분산안정성에 미치는 공정변수의 영향을 조사하였다. 슬러리연료 저장용기의 세군데(위, 중간, 아래) 위치별로 채취된 시료에서 평균입도와 탄소함량을 분석하여 Jet A-1에서 카본의 분산안정성을 측정하였다. 여러 종류의 첨가제를 적용한 결과, NB463S84 사용 시 분산성과 증가된 중력 가속도하에서 안정성이 가장 우수하였다. 동일 조건에서 카본층 높이 변화와 카본의 평균입도 측정을 통하여 혼합장비의 성능을 비교하였고, 실험실 규모에서 얻은 제조조건을 bench 규모 제조에 적용하여 본 연구의 실용 가능성을 확인하였다.

• 한국대기환경학회지
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• 제20권1호
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• pp.47-58
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• 2004

The $textsc{k}$-$\varepsilon$ algebraic stress model (KEASM) was applied to atmospheric dispersion simulation using the Lagrangian particle dispersion model and was compared with the most popular turbulence closure model in the field of atmospheric simulation, the Mellor-Yamada (MY) model. KEASM has been rarely applied to atmospheric simulation, but it includes the pressure redistribution effect of buoyancy due to heat and momentum fluxes. On the other hand, such effect is excluded from MY model. In the simulation study, the difference in the two turbulence models was reflected to both the turbulent velocity and the Lagrangian time scale. There was little difference in the vertical diffusion coefficient $\sigma$$_{z}$. However, the horizontal diffusion coefficient or calculated by KEASM was larger than that by MY model, coincided with the Pasquill-Gifford (PG) chart. The applicability of KEASM to atmospheric simulations was demonstrated by the simulations.s.

• Journal of Radiation Protection and Research
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• 제48권1호
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• pp.28-43
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• 2023

Background: High-fidelity meteorological data is a prerequisite for the realistic simulation of atmospheric dispersion of radioactive materials near nuclear power plants (NPPs). However, many meteorological models frequently overestimate near-surface wind speeds, failing to represent local meteorological conditions near NPPs. This study presents a new high-resolution (approximately 1 km) meteorological downscaling method for modeling short-range (< 100 km) atmospheric dispersion of accidental NPP plumes. Materials and Methods: Six considerations from literature reviews have been suggested for a new dynamic downscaling method. The dynamic downscaling method is developed based on the Weather Research and Forecasting (WRF) model version 3.6.1, applying high-resolution land-use and topography data. In addition, a new subgrid-scale topographic drag parameterization has been implemented for a realistic representation of the atmospheric surface-layer momentum transfer. Finally, a year-long simulation for the Kori and Wolsong NPPs, located in southeastern coastal areas, has been made for 2016 and evaluated against operational surface meteorological measurements and the NPPs' on-site weather stations. Results and Discussion: The new dynamic downscaling method can represent multiscale atmospheric motions from the synoptic to the boundary-layer scales and produce three-dimensional local meteorological fields near the NPPs with a 1.2 km grid resolution. Comparing the year-long simulation against the measurements showed a salient improvement in simulating near-surface wind fields by reducing the root mean square error of approximately 1 m/s. Furthermore, the improved wind field simulation led to a better agreement in the Eulerian estimate of the local atmospheric dispersion. The new subgrid-scale topographic drag parameterization was essential for improved performance, suggesting the importance of the subgrid-scale momentum interactions in the atmospheric surface layer. Conclusion: A new dynamic downscaling method has been developed to produce high-resolution local meteorological fields around the Kori and Wolsong NPPs, which can be used in short-range atmospheric dispersion modeling near the NPPs.

• 한국대기환경학회지
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• 제19권3호
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• pp.249-261
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• 2003

A three-dimensional mesoscale atmospheric dispersion modeling system consisting of the Lagrangian particle dispersion model (LPDM) and the meteorological mesoscale model (MM5) was employed to simulate the transport and dispersion of non-reactive pollutant during the nuclear spill event occurred from Sep. 31 to Oct. 3, 1999 in Tokaimura city, Japan. For the comparative analysis of numerical experiment, two more sets of foreign mesoscale modeling system; NCEP (National Centers for Environmental Prediction) and DWD (Deutscher Wetter Dienst) were also applied to address the applicability of air pollution dispersion predictions. We noticed that the simulated results of horizontal wind direction and wind velocity from three meteorological modeling showed remarkably different spatial variations, mainly due to the different horizontal resolutions. How-ever, the dispersion process by LPDM was well characterized by meteorological wind fields, and the time-dependent dilution factors ($\chi$/Q) were found to be qualitatively simulated in accordance with each mesocale meteorogical wind field, suggesting that LPDM has the potential for the use of the real time control at optimization of the urban air pollution provided detailed meteorological wind fields. This paper mainly pertains to the mesoscale modeling approaches, but the results imply that the resolution of meteorological model and the implementation of the relevant scale of air quality model lead to better prediction capabilities in local or urban scale air pollution modeling.

• 상하수도학회지
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• 제21권2호
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• pp.187-193
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• 2007

Reynolds and Froude numbers, along with tracer tests, have been widely used to estimate hydrodynamics in full-scale horizontal sedimentation basin in water treatment plants (WTPs). In spite of this, the former numbers do not reflect actual operating conditions, instead most often being based on the dimensions of the structures. The index and graphic analyses most often used were found to be too subjective to accurately analyze tracer test results. In order to overcome these limitations, dispersion number was applied for analysis of tracer test results. Tracer tests were conducted in eight full-scale sedimentation basins in six WTPs, and then analyzed by index and graphic analyses as well as by dispersion number. The dispersion number was more useful as an indicator of the hydrodynamic behavior in the basin. It was also found that as dispersion number decreased, flow approached the ideal for plug flow in which case, higher sedimentation efficiency could be expected.