• 한국환경과학회지
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• 제32권4호
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• pp.267-276
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• 2023

In this study, we analyzed seasonal variations in carbon dioxide fluxes, concentrations, and soil temperatures over three years in unvegetated tidal flats in the Beolgyo area. We also investigated the correlations between carbon dioxide fluxes and influencing factors. The average carbon dioxide flux was positive in summer and autumn but negative in winter and spring. A positive correlation was observed between carbon dioxide flux and soil temperature in spring whereas a negative correlation was noted in summer. In summer and autumn, as the soil temperature increased, the carbon dioxide flux decreased. In contrast, in spring and winter, as the soil temperature decreased, the carbon dioxide flux increased. Overall, this study reveals the significant influence of soil temperatures on carbon dioxide fluxes between the surface layer of the tidal flat and atmosphere.

• 한국환경과학회지
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• 제28권9호
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• pp.785-795
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• 2019

In order to analyze the sensitivity of carbon dioxide flux by soil temperature in the grassplot, carbon dioxide flux and soil temperature were observed 24 times from March, 2010 to March, 2011 at nine sites in the grassplot. The average of $CO_2$ in the grassplot is $2.2{\sim}36.7^{\circ}C$, the highest in August, the lowest in January, and the average of carbon dioxide flux is $12{\sim}1479mgCO_2{\cdot}m^{-2}{\cdot}hr^{-1}$, and the carbon dioxide emission from the grassplot to the atmosphere was 10 times higher in summer than in winter. The temperature response coefficient estimated by the exponential function of carbon dioxide flux according to soil temperature was ranged from 0.1065 to 0.1274, and the increase tendency of $CO_2$ flux with soil temperature was linear at $0{\sim}20^{\circ}C$ and exponential at $20{\sim}40^{\circ}C$. The $Q_{10}$ values for each of nine observation sites on the grassplot was in the range of 2.901 ~ 3.575, and the $Q_{10}$ value using the total data observed in the lawn was estimated to be 3.374. In the homogeneous grassplot area, the average of $Q_{10}$ values by observation point and the $Q_{10}$ value by the total data were estimated similarly.

• 한국습지학회지
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• 제21권4호
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• pp.257-266
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• 2019

본 연구에서는 함평만에 속하는 무안 지역의 갯벌에서 갈대가 서식하는 식생 지역과 갈대가 없는 비식생 지역을 6개 지점씩 선정하여 저조시에 계절별로 이산화탄소 농도와 플럭스 및 지온의 변화를 관측하였다. 관측은 2012년 5월 30일(봄)과 8월 8일(여름), 2013년 1월 31일(겨울)에 각각 수행되었다. 관측 결과, 식생 지역의 이산화탄소 평균농도는 전체적으로 겨울에 가장 높았고 봄, 여름 순으로 나타났으며, 비식생 지역도 식생 지역과 같은 농도변화를 보였다. 식생 지역의 이산화탄소 플럭스는 봄과 여름에 모두 양(+)의 값으로 방출(emission)의 형태를 보이나, 겨울에는 반대로 흡수(uptake)하는 음(-)의 값으로 나타났다. 이산화탄소 플럭스의 평균값은 봄이 가장 높았으나 여름과 거의 유사하였고, 겨울은 낮은 음의 값으로 나타났다. 비식생 지역은 봄에 양의 값으로 방출의 형태를 보였고, 여름과 겨울에는 흡수하는 음의 값으로 나타났다. 평균값은 봄이 가장 높았고, 여름과 겨울의 차는 작게 나타났다. 연구지역 이산화탄소 플럭스의 계절적인 변화특성은 봄의 경우 식생과 비식생 지역 모두 호흡에 의한 방출이 우세하였으며, 여름은 식생 지역에서 방출이 우세하였고 비식생 지역은 식물플랑크톤의 광합성에 의한 흡수가 확인되었으나 매우 미미하였다. 겨울은 식생 지역에서 이산화탄소 플럭스의 변화가 거의 나타나지 않았으며, 비식생 지역은 흡수가 일부 확인되었으나 매우 미미하였다.

• 한국화재소방학회논문지
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• 제26권4호
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• pp.18-23
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• 2012

이산화탄소 주조법에서 사용되고 있는 방법을 응용하여 목질내에 규산겔과 탄산소다, 이산화규소가 석출된 목재를 제조한 후 외부 복사열원(20, 25, 35 및 50 $kW/m^2$)에 따른 점화시간, 점화온도, 질량감소속도, 임계열유속을 측정하였다. 연구결과, 물유리와 이산화탄소를 이용한 가압함침 처리된 목재는 Pre-Flashover 단계에서의 복사열원(20 $kW/m^2$ 이하)에서 난연성능이 있음을 확인할 수 있었다. 향후 지속적인 연구를 통해 우수한 배합비율을 찾는다면 난연목재로서의 활용가능성이 있다고 판단된다.

• 대한기계학회논문집B
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• 제29권9호
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• pp.979-987
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• 2005

Numerical simulations were performed at atmospheric pressure in order to understand the effect of additives on flame speed, flame temperature, radical concentrations, $NO_x$ formation, and heat flux in freely propagating $CH_4-Air$ flames. The additives were both carbon dioxide and hydrogen chloride which had a combination of physical and chemical behavior on hydrocarbon flame. In the flame established with the same mole of methane and additive, hydrogen chloride significantly contributed toward the reduction of flame speed, flame temperature, $NO_x$ formation and heat flux by the chemical effect, whereas carbon dioxide mainly did so by the physical effect. The impact of hydrogen chloride on the decrease of the radical concentration was about $1.4\~3.0$ times as large as that of carbon dioxide. Hydrogen chloride had higher effect on the reduction of $EI_{NO}$ than carbon dioxide because of the chemical effect of hydrogen chloride. The reaction, $OH+HCl{\rightarrow}Cl+H_2O$, played an important role in the heat flux from flames added by hydrogen chloride instead of the reaction, $OH+H_2{\rightarrow}H+H_2O$ which was an important reaction in hydrocarbon flames.

• The Korean Journal of Ecology
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• 제23권1호
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• pp.39-43
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• 2000

1996년 7월 하순부터 9월 하순에 걸쳐 동경농공대학 농학부 부속부중농장(동경도 부중시)의 대두(Glycine max)개체군을 대상으로 미기상학적 플럭스측정방법의 하나인 열수지법을 이용하여 CO₂ 플럭스와 O₃ 플럭스를 측정하였다. CO₂ 플럭스와 O₃ 플럭스는 엽면적지수(LAI)의 변화에 영향을 받았으며, LAI가 2.0이상일 경우 CO₂ 플럭스는 광합성유효발사량(PAR)과 정비례관계가 있었다. O₃ 플럭스는 측정 기간 중 항상 양의 수치를 나타냈으며, 평균치는 0.5 mol m/sup -2/S/sup -1/이었다. 또한 CO₂와 O₃ 침착속도사이에는 정비례관계가 있었다 (LAI>2.0).

• 한국환경과학회지
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• 제23권6호
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• pp.1131-1142
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• 2014

In this study, the variations of the carbon dioxide fluxes were investigated with soil temperatures in the grassplot and seasonal variations of carbon dioxide concentrations and fluxes were analysed. Soil temperatures, carbon dioxide concentrations and fluxes were measured on the grassplot in Pukyong National University. Field measurements were carried out 25 times from March in 2010 to March in 2011 with nine points on the grassplot. Seasonal variations of carbon dioxide concentrations and fluxes showed an inverse relation. In summer, carbon dioxide concentrations are lower and carbon dioxide fluxes are higher. In winter, carbon dioxide concentrations are higher and carbon dioxide fluxes are lower. On the grassplot, carbon dioxide emission rate increase when the soil temperature is more than $20^{\circ}C$ and the emission rate decrease when the soil temperatures are less than $10^{\circ}C$. When the accumulated rainfall for five days before measurement day is 20~100 mm, it is showed that the more rainfall, the more carbon dioxide emissions. Carbon dioxide emission rate from the grassplot to the upper atmosphere was increased or decreased by the factors such as soil temperature, growth and wither of grass and rainfall. The results of this study showed that the emission of carbon dioxide in the grassplot is dominantly controlled by seasonal factors (especially soil temperature and rainfall).

• International Journal of Air-Conditioning and Refrigeration
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• 제14권1호
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• pp.19-27
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• 2006

The characteristics of heat transfer and pressure drop have been investigated experimentally during gas-cooling process of carbon dioxide. The results of this study are useful information in the design of a heat exchanger of $CO_2$ refrigerator. The test section consists of 6 series of copper tube, 4.15 and 2.18mm ID, respectively. The inlet temperature, the operating pressure, and the mass flux are varied in the range of $80{\sim}120^{\circ}C,\;{7\sim}10MPa,\;and\;400{\sim}1,900kg/m^2s$, respectively. The heat transfer coefficient of $CO_2$ is affected by temperature, inlet pressure, and mass flux of $CO_2$. At the maximum HTC, the temperature of $CO_2$ nearly accords with the psuedocritical temperature. It is found that the pressure drop is substantially affected by mass flux and inlet pressure of $CO_2$ . The results have been compared with those of previous work. The heat transfer correlation at the gas-cooling process has been also suggested which predicts within the error of 20%.

• 한국전자통신학회논문지
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• 제16권1호
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• pp.157-164
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• 2021

순천만 갯벌에서 3차원 초음파풍속계로 바람과 기온을 측정하고, 적외선 센서를 이용하여 이산화탄소 농도를 측정하였다. 일반적으로 기온이 증가하면 대기 중의 이산화탄소 농도가 증가하고, 기온이 감소하면 이산화탄소도 감소한다. 그러나 일몰 직후에는 광합성이 줄어들기 때문에, 기온이 감소함에도 이산화탄소 농도는 증가하였다. 또한 갯벌이 해수로 덮이게 되는 고조기에는 기온 증가에도 불구하고 대기 난류가 강하게 나타나 이산화탄소 농도가 감소하였다. 이산화탄소의 농도 변화에 미치는 갯벌 생태계의 광합성과 호흡 그리고 대기 난류의 영향에 대한 정량적 평가가 필요하다.

• 한국철도학회:학술대회논문집
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• 한국철도학회 2005년도 추계학술대회 논문집
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• pp.1190-1195
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• 2005

Biomass burning is a source of greenhouse gases, carbon dioxide, methane, and nitrous oxide. Under the ideal conditions of complete combustion, the burning of biomass produces carbon dioxide and water vapor. Since complete combustion is not achieved under any conditions of biomass burning, other carbon species, including carbon monoxide, methane, non-methane hydrocarbons and particulate carbon are produced. In this study, we analyze the combustion characteristics of rice-husk, such as heat release rate, smoke production rate, the percentage variation of CO and $CO_2$, oxygen consumption rate, and mass loss under different heat fluxes (20, 50 and 70kW). As a result, at 20kW incomplete combustion is occurred so that the percentage of CO is high in initial burning and total smoke release is higher than the others. At 50kW and 70kW, the combustion behaviors is very similar except the variation of CO percentage.