• The Korean Journal of Quaternary Research
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• v.24 no.2
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• pp.1-11
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• 2010

Energy Balance Model (EBM) was used to experiment the distribution of surface equilibrium temperature which responds to external forcing associated with the surface characteristics. Surface equilibrium temperature is calculated as sum of incoming solar radiation and latitudinal transport is balanced with outgoing infrared radiation. To treat incoming solar radiation, the source of the earth energy, significantly for energy balance, the experiment for surface equilibrium temperature distribution was performed considering the energy balance with the latitudinal albedo change as well as land and sea distribution. In addition, linear albedo change experiment, arctic albedo 5%, 10%, 15% change experiments and the opposite albedo change experiments between arctic and mid-latitudes were performed using incoming solar radiation as an external forcing. Moreover, with and without ice-albedo feedback experiments were performed. Increasing of arctic albedo is blocked out the incoming solar radiation so that it induces decreasing of latitudinal heat transport. It is strengthened energy transport from low latitudes by keeping arctic low energy states. Therefore the temperature change in the mid-latitudes exhibits larger response than that of arctic due to the difference of transport. The land which has lower heat capacity than sea can be reach to equilibrium temperature shortly. Also land is more sensitive to temperature change with respects to albedo. Thus it induces the thermal difference between land and sea. As a result, the equilibrium temperature exhibits differently as the difference of albedo and heat capacity which are the one of surface characteristics. Surface equilibrium temperature decreases as albedo increase and the ratio of temperature change is large as heat capacity is small. The decreasing of surface equilibrium temperature with respects to increasing of linear albedo is accelerated by ice-albedo feedback. However local change of surface equilibrium temperature decreases non-linearly.

• Journal of the Korean Geophysical Society
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• v.9 no.1
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• pp.27-36
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• 2006

The radiative convective equilibrium (RCE) temperature was calculated for the climate change study at King Sejong Station in West Antarctica. As a result of RCE model sensitivity test, the increases of surface albedo, solar zenith angle, and cloud optical thickness decrease surface temperature. On the other hand, the increases of carbon dioxide and cirrus cloud amount are caused by surface warming due to the greenhouse effect. According to the model calculation result, annual mean surface temperature shows a upward trend of 0.012oC/year during the period of 1958-2001. During the period of 1989∼2001, the trend of monthly mean surface temperature by model calculation is 0.01oC/month and the observation trend is 0.005oC/month.

• Food Science and Preservation
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• v.15 no.1
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• pp.74-78
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• 2008

Desorption experiments were carried out on soybean (Taegwang) at 5, 15, 25, 35, $45^{\circ}C$ for moisture contents between 6.74 and 28.87%(db). The method employed was to measure the equilibrium relative humidity (ERH) of air in contact with the grain under static conditions, using an electronic hygrometer. The effects of temperature and moisture contents were investigated, and the measured values were fitted to the modified Henderson, the modified Chung-Pfost, the modified Halsey, the modified Oswin and the modified GAB model. The ERHs of soybean under the moiture content of 16.67%(db) decreased with an decrease in moisture content and temperature, but the ERH of the moisture content of 28.87%(db) material decreased with an increase of temperature. The modified GAB model was the best in describing the EMC/ERH of soybean.

• Environmental Analysis Health and Toxicology
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• v.17 no.3
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• pp.187-195
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• 2002

다환방향족탄화수소류 화합물의 증기상-입자상간의 분배평형의 설명을 위해 흔히 입자상의 흡착지점이 균질하고 총흡착면적은 TSP에 비례한다는 가정을 사용하는데 본 연구의 목적은 이러한 가정의 타당성을 평가하는 것이다. 본 연구를 위해 도심에서 6단의 다단계 대기중입자채집기를 사용하여 대기 중의 입자를 포집하였으며 이들 입자에 흡착된 phenanthrene, anthracene, fluoranthene, pyrene을 분석하여 입경별 분포를 측정하였다. 특히 연구기간 중에 황사현상이 일어나 입경분포나 입자의 기원이 매우 다른 경우에 대한 연구가 가능하였다. 주요연구결과로서 우선 야마사키가 제안한 분배평형의 온도 의존식은 제한된 범위에서 사용되어야 한다는 것이 관측되었다. 즉, 황사현상이 일어나는 경우와 같이 입자의 흡착특성과 입경분포가 보통때와 다른 경우에는 log Kp와 l/T의 관계에서 선형성이 상당히 저하되었다. 또한 특히 낮은 온도에서는 입자의 입경분포가 달라지면 전체적인 분배평형이 달라지게 되는 것으로 평가되었으며 입자의 흡착특성도 분배평형의 온도의존성에 결정적인 영향을 줄 수 있는 것으로 나타났다. 따라서 입자의 기원이 다양하거나 입경분포가 달라지면 흡착평형이 바뀌기 때문에 흡착특성의 균질성과 단순한 TSP를 전제로 하는 분배평형의 평가나 예측은 실제 대기조건에서는 정확하지 않을 수가 있으며 제한적인 조건에서 사용되어야 할 것이다.

• Proceedings of the KAIS Fall Conference
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• 2009.05a
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• pp.863-866
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• 2009

Ethanol/3-methyl-1-butanol 계에 대하여 정온하 즉 50, 55, 60, 65, 70, 75 및 $80^{\circ}C$에서 2성분 기-액 평형측정치를 측정하였다. 측정된 기-액평형치의 액조성과 비휘발도의 대수치와의 관계를 직교좌표에 plot하면 직선이 이루어지고 온도변화에 대한 각각의 직선이 평형임을 확인하였다. Ethanol/3-methyl-1-butanol 계에 대한 추산식은 각각의 온도변화에 따라 나타내었고 이식들을 이용하여 추산식을 구하였다. 추산식으로부터 구한 추산치와 측정치를 비교 검토한 결과 Ethanol/3-methyl-1-butanol 계에서는 기상조성의 몰분율은 ${\pm}0.00051$[-]의 오차 범위에서 잘 일치하는 것으로 나타났고, modified UNIFAC방법은 실측치와 비교한 평균오차는 ${\pm}0.0022$[-]에서 추산하였다. 따라서 본 연구에서 제안한 추산법이 2성분계 기-액평형치를 추산하는 방법으로 타당함을 확인하였다.

• Proceedings of the Petrological Society of Korea Conference
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• 1998.09a
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• pp.29-29
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• 1998

• Proceedings of the Korean Vacuum Society Conference
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• 2012.02a
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• pp.521-521
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• 2012

공정용 유도 결합 플라즈마에서 강자성체 페라이트를 이용하여 평형전력 공급 변압기를 사용하여 안정적인 고밀도 플라즈마 발생원 개발에 관한 연구를 수행하였다. 실험에서는2개의 평형전력 공급 변압기를 이중 구조 안테나에 설치하였다. 20-100 mTorr 압력 범위의 아르곤 기체에 30-150 W범위의 전력을 인가하여 반응용기의 중앙에서 부유 탐침법을 이용하여 플라즈마 밀도와 전자 온도를 측정하였다. 동일한 압력과 전력이 인가되었을 때, 평형전력 공급 변압기의 연결 유무에 따른 플라즈마 밀도를 비교하였으며, 본 연구에서 제시한 플라즈마 발생원에서의 플라즈마 밀도가 더욱 높음을 보였다. 또한 전자 온도와 부유 전위는 평행전력 공급방식을 이용한 플라즈마 발생원이 상대적으로 낮은 값을 가졌다. 이는 플라즈마 전위의 감소를 나타내며, 챔버 벽으로 빠져나가는 이온과 전자의 손실이 줄어들었음을 알 수 있다.

• Journal of the East Asian Society of Dietary Life
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• v.11 no.6
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• pp.479-484
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• 2001

The absorption characteristics of persimmon powder related to different drying methods and various storage temperatures was investigated. The physical properties of persimmon powder by different drying methods displayed the largest amount of porosity in the freeze-dried sample, and the smallest in hot air dried sample. Equilibrium moisture was reached in 6 days. Monolayer moisture contents were predicted to 0.09687~0.19712(freeze drying), 0.07820~0.18617(vacuum drying) and 0.07715~0.18056(hot air drying) g H2O/g solid respectively using the BET equation. BET equation for isothermal absorption curve showed over 0.95 R-square for all dried methods. Monolayer moisture contents were increased as storage temperature was incremented because water molecular movement was more active and there was a greater chance to clash with the absorption surface area.

• Journal of Korean Society of Forest Science
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• v.83 no.4
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• pp.540-544
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• 1994

Equilibrium moisture contents(EMC) were calculated based on temperature and relative humidity of atmosphere and actual EMCs were measured at intervals of ten days in previous air-dried wood samples for seven different species including Douglas fir and oaks in four indoor locations in central region for one year. Mean annual air temperature and relative humidity were $23.3^{\circ}C$ and 54.9% in bedroom, $22.4^{\circ}C$ and 59.5% in living room of apartment, $20.1^{\circ}C$ and 57.0% in office room and 19.4 and 64.0% in living room of tile-roofed house, respectively. Mean annual calculated and actual EMCs were 10.2 and 9.7% in bedroom, 11.1 and 10.2% in living room of apartment, 10.7 and 10.4% in office room, and 12.1 and 12.5% in living room of tile-roofed, house, respectively. Actual EMC of kasai were higher than average value of EMC for seven species. However, those of sycamore and apitong were lower than average value.

• Korean Journal of Food Science and Technology
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• v.16 no.1
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• pp.108-112
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• 1984

The sorption characteristics of red pepper powder stored at various relative humidity and temperature were studied. At low relative humidity below RH 57%, the sorption equilibrium was easily attained, whereas at higher relative humidity above RH 75%, the powder was browned by higher equilibrium moisture content. The moisture content of monolayer value for the powder was ranging from 11.32% to 12.13% with temperature. First order regression equation of equilibrium moisture content for relative humidity was determined.