• 한국환경과학회지
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• 제10권6호
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• pp.417-422
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• 2001

The vertical structure of atmosphere was observed In investigate the variation of surface ozone concentration by vertical downward mixing of residual ozone in the atmospheric boundary layer at the Busan coastal area. Airsonde and pilot balloon measurements were made at Gamcheondong and the Kimhae airport for April 26~27, 1996. The vertical potential of potential temperature showed a residual layer between 510m and 1800m from 2100LST April 26 to 0900LST April 27. The downward mixing of ozone in the residual layer of the atmospheric boundary layer was confirmed from vertical profile of mixing ratio near 600m in the morning. The thickness of the sea breeze layer was 900m at 1500LST April 26. Thereafter, it become to be lowered with time A low level jet was measured near 900m at 0300LST on April 27 from a pibal measurement. Early morning sharp increase of surface ozone concentration at the Busan coastal area was caused by vertical downward mixing of ozone concentration rather than by photochemical reaction In the atmospheric boundary layer.

• 한국군사과학기술학회지
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• 제11권3호
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• pp.169-175
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• 2008

A fine carbon fibers dispersion model is implemented to calculate the scattering range and ground level concentration of carbon fibers emitted at certain altitudes of atmospheric boundary layer. This carbon fibers dispersion model was composed by coupling a commonly used atmospheric dispersion model and an atmospheric boundary layer model. The atmospheric boundary layer model, applying the Monin-Obukov Similarity Rule obtained from measurement input data at ground level, was used to create the atmospheric boundary layer structure. In the atmospheric dispersion model, the Lagrangian Particle Model and the Markov Process were applied to calculate the trajectory of scattered carbon fibers relative to gravity and aerodynamic force, as well as carbon fibers specification.

• 한국환경과학회지
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• 제21권7호
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• pp.815-824
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• 2012

The purpose of this study was to analyze the meteorological characteristics of wintertime high PM10 concentration episodes in Busan. $PM_{10}$ concentration has been reduced for the past four years and recorded near or exceeded 100 ${\mu}g/m^3$ (national standard of $PM_{10}$). High concentration episodes in Busan were 6 case, $PM_{2.5}/PM_{10}$ ratio was 0.36~0.39(mean 0.55). High $PM_{10}$ concentration occurred during higher air temperature, more solar radiation and sunshine, lower relative humidity, and smaller cloud amount. Synoptically, it also occurred when Busan was in the center or the edge of anticyclone and when sea breeze intruded. An analysis of upper air sounding showed that high $PM_{10}$ concentration occurred when surface inversion layer and upper subsidence inversion layer existed, and when boundary layer depth and vertical mixing coefficient were low. An analysis of backward trajectory of air mass showed that high $PM_{10}$ concentration was largely affected by long range transport considering that it occurs when air mass is intruded from China.

• Asian Journal of Atmospheric Environment
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• 제4권3호
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• pp.141-149
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• 2010

Aerosol size and number concentration were observed in the atmospheric boundary layer over Beijing (from near the ground to 1,200 m) on March 15 (a clear day) and 16 (a dusty day), 2005. The results were further compared with lidar measurements in order to understand the dependency of extinction on the particle size distribution and their vertical changes. The boundary layer atmosphere was composed of several sub-layers, and a dry air layer appeared between 400 and 1,000 m under the influence of dust event. In this dry air layer, the concentration of the fine-mode particles (diameter smaller than $1.0\;{\mu}m$) was slightly lower than the value on the clear day, while the concentration of coarse-mode particles (diameter larger than $1.0\;{\mu}m$) was remarkably higher than that on the clear day. This situation was attributed to the inflow of an air mass containing large amounts of Asian dust particles and a smaller amount of fine-mode particles. The results strongly suggest that the fine-mode particles affect light extinction even in the dusty atmosphere. However, quantitatively the relation between extinction and particle concentration is not satisfied under the dusty atmospheric conditions since laser beam attenuates in the atmosphere with high concentration of particles. Laser beam attenuation effect becomes larger in the relation between extinction and coarse particle content comparing the relation between extinction and fine particle content. To clarify this problem technically, future in situ measurements such as balloon-borne lidar are suggested. Here extinction was measured at 532 nm wavelength. Measurements of extinction at other wavelengths are desired in the future.

• Nuclear Engineering and Technology
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• 제53권1호
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• pp.244-252
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• 2021

Wind plays an important role in cases of unexpected radioactive pollutant dispersion, deciding distribution and concentration of the leaked substance. The accurate prediction of wind has been challenging in numerical weather prediction models, especially near the surface because of the complex interaction between turbulent flow and topographic effect. In this study, we investigated the characteristics of atmospheric dispersion of radioactive material (i.e. ¹³⁷Cs) according to the simulated boundary layer around the HANARO research nuclear reactor in Korea using the Weather Research and Forecasting (WRF)-Mesoscale Model Interface (MMIF)-California Puff (CALPUFF) model system. We examined the impacts of orographic drag on wind field, stability calculation methods, and planetary boundary layer parameterizations on the dispersion of radioactive material under a radioactive leaking scenario. We found that inclusion of the orographic drag effect in the WRF model improved the wind prediction most significantly over the complex terrain area, leading the model system to estimate the radioactive concentration near the reactor more conservatively. We also emphasized the importance of the stability calculation method and employing the skillful boundary layer parameterization to ensure more accurate low atmospheric conditions, in order to simulate more feasible spatial distribution of the radioactive dispersion in leaking scenarios.

• Ocean and Polar Research
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• 제32권4호
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• pp.439-448
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• 2010

CTD를 이용하여 용존산소의 농도에 대한 연속적인 관측이 이루어지면서 용존산소 농도 분포의 fine structure에 대한 연구가 가능해졌다. 뿐만 아니라 altimeter로부터 해저 퇴적물 표면에 최대한 가까이 까지 관측이 가능해짐에 따라 해저 경계면에서의 용존산소 농도 분포에 대한 정보를 얻을 수 있게 되었다. 지금까지 동해 울릉분지의 용존 산소 농도의 수직 분포는 동해 북부의 일본 분지와는 수심 300 m 이하에서는 수심에 따라 지속적으로 감소하는 형태를 보이는 것으로 알려져 있다. 그러나 2005년부터 2006년까지 6회에 걸쳐 수심이 1000 m보다 깊은 지역에서 해저퇴적물 상부 100 m 이내의 수심까지 용존산소를 관측한 결과, 울릉분지 내의 용존 산소 농도의 수직분포형태는 3가지로 분류된다. 첫 번째는 지금까지 알려진 바와 같이 수심에 따라 지속적으로 감소하는 형태(Type-1), 두 번째는 Type-1과 같은 형태를 보이다가 해저 경계면 근처에서 급격히 산소의 농도가 줄어드는 형태(Type-2), 세 번째는 해저 경계면 상층에 용존산소 농도의 최소층이 존재하는 형태(Type-3)이다. 울릉분지 수심 1000 m 이상되는 지역에서는 분지 전반에 걸쳐 Type-2 형태로 분포하고 Ulleung Interplane Gap을 포함하여 일본 분지와 가까운 지역에서는 Type-1, 독도 인근 해역에서는 Type-3 형태의 분포를 보인다. 표층 퇴적물에서 유기물 분해를 전제로 해저 경계면의 용존 산소 분포를 이용하여 계산된 표층 퇴적물의 산소 소모율은 $0.2{\sim}5.8\;mmol\;m^{-2}d^{-1}$로 실제 퇴적물 배양을 통해 얻은 산소 소모율 약 $1{\sim}9\;mmol\;m^{-2}d^{-1}$(정 등 2009; 이 등 2010b)와 일치하는 것으로 미루어 볼 때, 울릉분지의 전반에 걸쳐 Type-2와 같은 형태의 분포를 보이는 것은 울릉분지의 표층 퇴적물에서 높은 농도를 보이는 유기물의 분해가 일차적으로 중요한 역할을 하는 것으로 판단된다.

• Journal of Pharmaceutical Investigation
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• 제31권1호
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• pp.13-18
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• 2001

This study was to investigate the relationship between the gel layer thickness and swelling boundary via strength measurements using texture analysis. The novel texture analysis approach was used to examine the dynamics of swelling behavior in a ternary polymeric matrix tablet. The method permitted the characterization of the changes occurring at the peripheral as well as within interior boundary of the swelling during water ingress. The increase in gel strength for pectin, HPMC, and a ternary mixture with gelatin was found to depend on polymer concentration. Therefore, this method is further applicable to characterize the swelling behavior and provide opportunity to differentiate the gel-layer from that of swelling boundary.

• Nuclear Engineering and Technology
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• 제38권8호
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• pp.763-778
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• 2006

Injection of microbubbles within the turbulent boundary layer has been investigated for several years as a method to achieve drag reduction. However, the physical mechanism of this phenomenon is not yet fully understood. Experiments in a channel flow for single phase (water) and two phase (water and microbubbles) flows with various void fraction values are studied for a Reynolds number of 5128 based on the half height of the channel and bulk velocity. The state-of-the art Particle Tracking Velocimetry (PTV) measurement technique is used to measure the instantaneous full-field velocity components. Comparisons between turbulent statistical quantities with various values of local void fraction are presented to elucidate the influence of the microbubbles presence within the boundary layer. A decrease in the Reynolds stress distribution and turbulence production is obtained with the increase of microbubble concentration. The results obtained indicate a decorrelation of the streamwise and normal fluctuating velocities when microbubbles are injected within the boundary layer.

• 멤브레인
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• 제11권2호
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• pp.74-82
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• 2001

실리콘(PDM)막을 통한 휘발성유기화합물(VOCs)과 질소 혼합물의 증기투과시 공급부 경계층에서 발생하는 VOCs의 농도분극 현상을 정량적인 평가를 위하여 저항직렬연결의 개념을 바탕으로 한 수학적인 모델식을 확립하였다. feed속도를 변화시키면서 여러 VOCs 혼합물에 대한 증기투과를 시행하였는데 본 연구에 사용한 VOCs는 염소화 탄화수소계 중에서 응축도가 다른 methylene chloride, chloroform, 1,2-dichloroethane, 1,1,2-trichloroethane 등을 선정하여 사용하였다. 확립한 모델식에 각 혼합물의 투과 실험치들의 frtting 및 regression을 통하여 각 모델 파라메타들을 구하고 물질전달계수 및 농도분극탄성률 등을 결정하였다. 결정한 모델 파라메타를 분석한 결과 VOCs의 응축도가 클수록 경계층 저항이 현저함을 관찰할 수 있었으며 또한 모델링을 통해서 고 투과성 고 선택성막을 통한 증기투과에서 경계층저항의 중요성을 확인할 수 있었다.

• 환경영향평가
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• 제20권4호
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• pp.557-564
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• 2011

This study was conducted to investigate the sudden rise of fine particle concentration after the passage of typhoon USAGI and NARI in Busan. Nocturnal inversion layer was formed at atmospheric boundary layer and wind direction changed from southerly wind to northeasterly wind after USAGI passed through Busan. Fine particle concentration in Busan rapidly increased by subsidence of air pollutants released from sources and dust transported from in the vicinity of industrial regions. Wind direction changed from northeasterly wind to southeasterly wind, wind velocity increased and lower atmosphere became extremely unstable after NARI passed through Busan. $PM_{10}$ concentration of Busan increased sharply because of surface dust dispersed by strong wind. Fine particle concentration generally decreases by precipitation and wind after typhoon passes through. However, the concentration can also go up not only by subsidence and transportation in nocturnal inversion layer but also by surface dust which temporarily occurs by strong wind.