The present study examined changes in surface shape and pore size observed in carbon black particles isothermally oxidized in an air atmosphere according to their burn-off ratio. Carbon black materials were fed into a horizontal tubular furnace in an air atmosphere when the inside temperature reached 600 °C. Subsequently, while changing the isothermal oxidation time, carbon black samples with different burn-off ratios were obtained, i.e., 10.5, 20.0, 30.4, 41.0, 49.9, 59.8, 71.1, and 81.0%. The scanning electron microscope analysis revealed that the observed carbon black particles were in the form of aggregated primary particles, and that there was no change in the particle size of these primary particles as the burn-off process proceeded. The latter observation supported the observation that pores were formed in the carbon black samples during the burn-off process. Notably, the Brunauer–Emmett–Teller analysis exhibited hysteresis curves, indicating that the corresponding adsorption isotherms were of IV-type. It was also found that the area of the hysteresis curves increased as the burn-off process proceeded. The specific surface area of the raw carbon black sample was 58.00 m2/g, while that of the 81.0% sample was about 4.1 times the figure at 240.27 m2/g. The total pore volume VT was 0.17 cm3/g for the raw sample, and it was much higher for the 81.0% sample at 0.58 cm3/g. The transmission electron microscope analysis showed that the raw carbon black particles had a spherical shape with a smooth surface, but inner pores were not observed. In the 49.9% sample, pores with a size of about 5 nm were observed inside carbon black particles. Notably, the size of the pores observed in the 81.0% sample was about 20 nm and the large pores were created by the collapsing and merging of the smaller pores by oxidation.

본 연구에서는 지역 기상-해양 접합모델을 이용하여 2018년 8월 28일부터 30일까지 한반도 서울-경기지역에 내린 강수에 대해 대기-해양 상호작용의 효과를 분석하였다. 지역 기상-해양 접합모델에서 기상모델은 WRF (Weather Research Forecasts)가 사용되었으며, 해양모델은 ROMS (Regional Oceanic Modeling System)가 사용되었다. 단일 기상 모델은 WRF모델만 이용되었으며, ECMWF Re-Analysis Interim 의 해수면온도자료가 바닥경계자료로 사용되었다. 관측자료와 비교하여, 대기-해양 상호작용의 효과가 고려된 접합모델은 서울-경기지역의 강수 및 황해 해수면온도에 대해 공간상관계수가 각각 0.6과 0.84로 이는 지역 기상모델보다 높게 나타났다. 또한, 평균편향오차(MBE, Mean Bias Error)은 각각 −2.32와 −0.62로 지역 기상모델 보다 낮은 오차율을 보였다. 상당온위와 해수면온도 및 역학적 수렴장으로 분석한 대기-해양 상호작용의 효과는 황해 해수면온도의 변화를 유도하였고, 그 변화는 하층대기에서 열적 불안정과 운동학적 수렴대의 차이를 발생시켰다. 열적 불안정과 수렴대는 결과적으로 서울-경기 지역에서 상승운동을 유도하였고, 결과적으로 기상-해양 접합모델에서 모의된 강수가 관측과 더 유사한 공간분포를 나타냈다. 그러나 복잡한 관계에 있는 대기-해양 상호작용의 효과를 더 명확히 파악하기 위해서는 다양한 사례연구와 장기적인 분석이 필요하지만, 본 연구는 기상-해양 상호작용이 강수 예보에 중요성에 대한 또 다른 증거를 제시한다.

The present study intends to investigate the transient response of an atmosphere/ocean general circulation model to a gradual increase of atmospheric carbon dioxide. To detect the climatic change of the surface air temperature due to gradual increasing carbon dioxide for 100 years, two runs of GFDL CGCM for 1 % CO_2 run with increasing CO_2 and the control run with fixed CO_2 are compared. From results it is noted that the transient response of surface air temperature is more increased over the Northern Hemisphere than the Southern Hemisphere. However, in Northern Hemisphere the transient response of the surface air temperature due to the gradual increase of atmospheric carbon dioxide is slowly increased with latitudes and is clearly larger over continents than oceans. The annual global mean temperature is continuously increased with 0.03552 per one year with strong S/N ratio and distinguished from the natural variability. The time dependent response of the gradual increasing CO_2 has the strong seasonal variability with small change in summer and large change in winter, and the strong regionality in the Asian and the American continents. It has been suggested that the direct and the feedback processes in the climate systems should be investigated by the detailed sensitivity runs to get the meaningful estimate of the CO_2 forced variability.

In the Atmosphere under the various physical and chemical condition different chemical reactions occur and there are a number of air pollutants which are generated by photochemical reaction by absorbing solar energy. Therefor various testing simulation was done as foundation work to develop the numerical model for the prediction of concentration of air pollutants. It was shown change of major air pollutants concentration in according to variation of photodissociation speed constant, K_1 and initial condition of air pollutants concentration which plays major role in photochemical reaction. The photochemical reaction model which was used in this study is found to be useful for understanding relationship among the concentration of reacting air pollutants and the prediction of concentration of air pollutants in urban atmosphere