• Journal of Biosystems Engineering
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• 제23권1호
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• pp.21-30
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• 1998

A theoretical model was developed to evaluate the effects of soil and airflow characteristics on the soil-air heat exchanger performances. The model, which includes three-dimensional transient energy and mass equilibrium-equation, was solved by using a computer program that uses Finite Difference Methods and Gauss-Seidel iteration computation. Energy gains, heat exchange efficiencies, and outlet air temperature are presented including the effects of soil moisture content, soil conductivity, soil thermal diffusivity, and soil initial temperature. Also, data related to the effects of airflow rate and inlet air temperature on the thermal performance of the system are presented. The results indicated that energy gains depend on soil conductivity, soil thermal diffusivity, and soil initial temperature. Heat exchange efficiencies relied on air mass flow rate and soil moisture content.

• Journal of Biosystems Engineering
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• 제21권4호
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• pp.436-448
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• 1996

An earth tube soil air heat exchange system was designed, installed and operated as a single pass heat exchanger to utilize the geothermal energy as an natural energy source. This study was undertaken to investigate the potential of the heating and cooling, energy gain, heat exchange efficiency and coefficient of performance of the system. The system consisted of 30m in length and 30cm in diameter polyethylene pipes buried 2m deep in soil. Maximum heating and cooling performance were 2.51㎾ and 1.26㎾ at the air mass rate of 21cmm. Energy gain and coefficient of performance were the function of temperature difference between outside air and soil temperature. They were expressed as Q=0.33$ imes$$Delta T_{max}$+0.134(㎾) for energy gain and COP=0.44$ imes$$Delta T_{max}$+0.178 for coefficient of performance with correlation factor of 0.95. The mean of heat exchange efficiencies was 85.6%.

• 한국대기환경학회지
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• 제19권3호
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• pp.275-284
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• 2003

The soil -air exchange processes of CH$_4$ were investigated in Hari district of Kang Hwa Island, Korea during the late April 2002. In the course of our field experiments, we measured the concentration, concentration gradients (between two different heights of 1 and 5 m), and the fluxes of CH$_4$ using the surface layer gradient microm-eteorological methods. If the relationships between CH$_4$ fluxes and the relevant environmental parameters are examined, CH$_4$ fluxes were found to be affected most significantly by parameters like wind speed. The results of our study indicate that the study area behaved as a net source of CH$_4$ to the atmosphere with a net daily emission rate of 3.6 mg m￣$^2$ The findings of relatively low exchange rate observed at our study site suggest that the rice paddy area investigated prior to planting period can behave as a moderate source of methane.

• 한국대기환경학회지
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• 제12권2호
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• pp.189-198
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• 1996

Mercury (Hg) is ubiquitous throughout the earth's atmosphere. The uniqueness of its atmospheric geochemistry is well-known with the high environmental mobility and relatively long atmospheric residence time (c.a., 1 year) associated with its high chemical stability. Despite a growing recognition of the environmental significance of its global cycling, the prexisting Korean database for atmospheric Hg is extremely rare and confined to a number of concentration measurements conducted under relatively polluted urban atmospheric environments. To help activate the research on this suvject, an in-depth analysis on the current development in the measurements of atmospheric mercury and the associated fluxes has been made using the most using the most updated data ests reported worldwide. As a first step toward this purpose, the most reliable techniques commonly employed in the measurements of its concentration in the background atmosphere are introduced in combination with the flux measurement techniques over soil surface such as: dynamic enclosure (or field flux chamber) method and field micrometeorological method. Then the results derived using these measurement techniques are discussed and interpreted with an emphasis on its mobilization across the terrestrial biosphere and atmosphere interface. A unmber of factors including air/soil temperature, soil chemical composition, soil water content, and barometric pressure are found out to be influential to the rate and amount of such exchange processes. Although absolute magnitude of such exchange processes is insignificant relative to that of the major component like the oceanic environment, this exchange process is thought to be the the predominant natural pathway for both the mobilization and redistribution of atmospheric Hg on a local or regional scale.

• 한국대기환경학회지
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• 제26권2호
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• pp.107-117
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• 2010

The atmospheric geochemistry of mercury is generalls represented by gaseous elemental phase that exhibits the high environmental mobility and relatively long atmospheric residence time (c.a., 1 year) with its high chemical stability. In the recognition of the environmental significance of its global cycling, enormous efforts have been devoted to the measurements of Hg exchange across air-soil boundary. To be able to describe the fundamental aspects on this subject, the current development in the measurements of atmospheric exchange rates of mercury has been summarized using the current database reported worldwide. As a first step, different techniques commonly employed in its measurements are introduced with the discussions on their merits and disadvantages. Then, the results derived from various field measurement campaigns are also compared and discussed. The direction for the future study of mercury is presented at last.

• 한국산림과학회지
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• 제87권2호
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• pp.188-193
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• 1998

토양의 pH 변화는 토양의 화학적 특성을 결정하는 중요한 요인이며 도시의 환경오염이 토양과 식물생장에 미치는 영향을 평가할 수 있는 지표가 되기도 한다. 서울지역의 대기오염이 도시림 토양에 미치는 영향을 파악하기 위하여 조사지역을 도심에서 외곽방향으로 5km 간격의 동심원으로 구분하고 도시 외곽지역에서 토양산성화에 차이가 있는지 조사하였다. 각 구역의 도시림에서 토양시료를 A, B층에서 채취하여 토양 pH, 토양완충능력, 양이온치환능력 및 염기포화도를 측정하였다. 토양 pH는 A층에서 3.96~5.08, B층에서 4.10~5.25의 분포를 나타냈다. 도심에서 외곽방향으로 구역간 토양 pH 차이에는 통계적인 유의성이 없었으나 외곽 구역에 비하여 도심 구역에서 토양 pH가 비교적 낮은 경향을 보였다. 토양완충능력은 도심 구역 (0-5km와 5-10km)이 외곽 구역(10-15km와 15-20km)에 비하여 현저히 낮은 값을 나타내었다. 양이온치환능력과 이와 관련있는 염기포화도는 구역간 차이에 유의성이 없었다. 대기오염물질의 도시의 외곽 방향으로의 확산을 따라 서울지역 도시림의 토양 산성화가 유사한 진행을 보이고 있는 것으로 나타났다. 토양완충능력이 도심 구역에서 낮은 것은 서울지역에서 대기 중 산성강하물의 유입에 대하여 나타난 토양 반응의 척도로 볼 수 있다.

• Journal of Biosystems Engineering
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• 제22권4호
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• pp.459-468
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• 1997

To optimize the design and operation of a soil- air heat exchanger system, the effects of variables characterizing system design and operation on the performance of the system were analyzed by a theoretical model which included the three-dimensional transient heat conduction equation. The solution of the theoretical model was acquired by a computer program that uses Finite Difference Methods and Gauss-Seidel iteration computation, in which the time discretization scheme was an implicit difference appoximation. The computer program was validated first by comparison of the results for different grid sizes. Air outlet temperature, energy gain, and heat exchange efficiency of the system were analyzed based upon the tube diameter, tube length, tube thickness, and tube thermal diffusivity.

• 한국건축시공학회:학술대회논문집
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• 한국건축시공학회 2020년도 봄 학술논문 발표대회
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• pp.189-190
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• 2020

The importance of indoor air quality management has recently been highlighted due to environmental problems such as indoor air pollution. Among indoor air pollutants, carbon dioxide occurs in cooking, heating, burning, and causes forgetfulness, dementia and amnesia. Radon, which occurs in building materials, soil and ground, is a type 1 carcinogen that causes lung cancer in the body through breathing. These substances can be released from the room through ventilation, but there is a limit to reducing the amount of indoor activity due to reduced ventilation conditions due to increased indoor activity time. However, these substances can be removed from the gas by adsorption. The purpose of this study was to identify the properties of granular active and powdered active white soil and mix them to make cement-based active white soil adsorbent matrix for carbon dioxide, fine dust and radon gas adsorption, and to evaluate indoor air improvements according to the mixing scale. The results of the experiment showed that active carbon dioxide adsorption performance increased for carbon dioxide and radon as the exchange rate increased through physical adsorption. In particular, the higher the replacement rate of the granular active bag, the better adsorption performance was shown.

• Asian Journal of Atmospheric Environment
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• 제9권2호
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• pp.173-186
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• 2015

In Bangladesh, increases in the tropospheric ozone ($O_3$) concentration and in soil salinization may lead to crop damage. To clarify the effects of $O_3$ and/or soil salinity on Bangladeshi wheat cultivars, BAW1059 (salt-tolerant) and Shatabdi (salt-sensitive) were exposed to 70-day treatments with $O_3$ (charcoal-filtered air (CF), $1.0{\times}O_3$, and $1.5{\times}O_3$) and different levels of soil salinity (0, 4, and $8dS\;m^{-1}$). In both cultivars, the whole-plant dry mass and grain yield were significantly reduced by exposure to $O_3$. Increased soil salinity caused significant reductions in whole-plant growth and yield in Shatabdi, but the reductions were negligible in BAW1059. No significant interactions between $O_3$ and salinity were detected for growth, yield, and leaf gas exchange parameters in both cultivars. We concluded that the effects of $O_3$ are not ameliorated by soil salinity in two Bangladeshi wheat cultivars, regardless of their salinity tolerance.

• 환경생물
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• 제41권4호
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• pp.439-446
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• 2023

맹그로브는 육지와 바다 사이 조간대에 서식하는 식물집단으로, 전지구 탄소 순환에서 중요한 역할을 한다. 그러나 국내에 자생하는 맹그로브 관련 수종의 탄소 순환에 관한 연구는 진행된 바가 없다. 본 연구는 준맹그로브인 황근(Hibiscus hamabo) 자생지 3곳(김녕, 성산, 위미)에서 토양호흡과 잎의 기체 교환을 주기적으로 측정하고 이에 영향을 미치는 요인을 파악하고자 하였다. 토양호흡은 2022년 6월부터 10월까지, 잎의 기체 교환은 6월부터 9월까지 각 월1회씩 측정하였다. 8월의 토양호흡(5.7±0.8 μmol CO₂ m^-2 s^-1)은 다른 달에 비해 유의하게 높았으며(p<0.001), 기온이 증가함에 따라 토양호흡이 증가하였다(p<0.01). 7월에 성산에서의 순광합성률은 9.0±0.9 μmol m^-2 s^-1로 다른 시기보다 높게 나타났으며(p<0.001), 전체 기간 동안 모든 대상지에서 순광합성률은 기공전도도와 증산속도가 증가할수록 증가하였다(p<0.001). 토양호흡은 순광합성률과 양의 선형관계(r²=0.12; p<0.01)를 나타내었다. 이러한 결과는 토양호흡이 계절을 동반한 기온뿐만 아니라 광합성에 의한 CO₂ 흡수에 영향을 받기 때문인 것으로 보인다. 본 연구는 향후 준맹그로브 수종의 탄소 동태 분석에 기초 자료로 활용될 수 있을 것이다.