• 한국대기환경학회지
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• 제16권4호
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• pp.363-372
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• 2000

In order to overtake a quantitative analysis of effect of anthropogenic heat and different land-use on urban thermal environment numerical simulation of surface energy budget was carried out under typical summer synoptic condition. It is beneficial to understand surface temperature of complex urban surace. The different land-use types are classified of rice field farm fruit garden residential region forest water and swamp by using map scaled 1/25000 of Pusan metropolitan. The model predicts that maximum heat island intensity in the central part of Pusan is 7$^{\circ}C$ at 2000 LST in summertime. The surface temperature is propotional to the density of constructions. The effect of anthropogenic heat generation on surface temperature is the increase of 0.3$^{\circ}C$ at 1400LST in the central part of Pusan during summertime.

• 한국태양에너지학회:학술대회논문집
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• 한국태양에너지학회 2008년도 추계학술발표대회 논문집
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• pp.85-89
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• 2008

This study carried out field observations of measuring thermal environment, especially evaluating amount of water evaporation at roof Pond by field observations during the summer. Thermal environment measuring was categorized as air temperature, water temperature of roof pond, surface temperature, globe temperature, short and long wave radiation, net radiation, and amount of water evaporation by water level measurement. Results from this study could be used as fundamental for reducing heat Island phenomena.

• 전자공학회논문지A
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• 제32A권8호
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• pp.107-118
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• 1995

Three-dimensional simulator for thermal oxidation process is developed. The simulator is consisted by two individual module, one is analytic-model module and the other is numerical-model module. The analytic-model which uses simple complementary-error function guarantees fast calculation in prediction of multi-dimensional oxidation process. The numerical-model which is based on boundary element method (BEM), has a good accuracy and suitable for various process conditions. The results of this study show that oxide growth is retarded at the corner of hole structure and enhanced at the corner of island structure. These effects are reson of different distribution of oxidant diffusion and mask stress. The utility of models and simulator developed in this study is demonstrated by using it to predict not only traditional shape of LOCOS but also process effects in small geometry.

• 한국농공학회:학술대회논문집
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• 한국농공학회 2005년도 학술발표논문집
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• pp.569-573
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• 2005

Land surface temperature(LST) is one of the key parameters in physics and meteorology of land-surface processes on regional and global scales. Urban Heat Island(UHI), a meteorological phenomenon by which the air temperature in an urban area increases beyond that in the suburbs, grows with the progress of urbanization. Satellite remote sensing has been expected to be effective for obtaining thermal information of the earth's surface with a high resolution. The main purpose of this study is to produce LST map of Cheongju and to analyze the spatial distributions of surface heat fluxes in urban areas. This study, taking Cheongju as the study area, aims to examine relationship between vegetation cover rates and surface temperature, and to clarify a method for calculation surface temperature with Landsat TM thermal images.

• 한국전기전자재료학회:학술대회논문집
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• 한국전기전자재료학회 1996년도 추계학술대회 논문집
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• pp.67-70
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• 1996

In this paper, the three-dimensional stress effect of thermal oxide is simulated. We developed the three-dimensional finite element numerical simulator including three-dimensional adaptive mesh generator that is able to refine and eliminate nearby moving boundary of oxide, and oxidation solver with stress model. The main effect of deformation at the coner area of oxide is due to distribution of oxidant, but the deformation of oxide is affected by the stress in the oxide. In the island structure which is the structure mostly covered with nitride and a coner is opened to oxidation, oxidation is reduced at the coner by compressive stress. In the hole structure which is the structure mostly opened to oxide and a coner is covered with nitride, however, oxidation is increased at the coner by tensile stress.

• 한국태양에너지학회 논문집
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• 제27권2호
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• pp.95-101
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• 2007

The surface changes due to urban expansion and the increase of artificial heat releases have brought significant climate changes such as heat island phenomenon in urban area. Furthermore, these changes also have brought serious problems such as air temperature increase, wind changes, and air pollution in urban area. Comprehensive analytical technologies considering various effects are required to analyse complicated mechanism of climate changes, and review the efficient measures. In this research, the effect of the urban expansion in Tokyo and Bangkok area on urban environment will be discussed. By using CFD, urban development and the mechanism of global warming and wind change are studied in those two cities. As a result of numerical research, the surface changes of city could bring the environmental changes in urban area.

• 한국건축시공학회:학술대회논문집
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• 한국건축시공학회 2019년도 춘계 학술논문 발표대회
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• pp.186-187
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• 2019

In modern times, due to the centralized urban structure, the interval between buildings is narrow and the increase of the heat island phenomenon due to the accumulation of the structure is becoming a social problem. In order to solve these problems, various materials for reducing the surface temperature of buildings are under study. Particularly, in the case of a wall part which is a part directly affected by the outside air of the building, it is a main structural part for determining the room temperature. The purpose of this study was to develop a material that can improve the thermal environment performance of the building by evaluating the temperature control performance of the exterior finishing material using the heat reflecting material as a method for controlling the temperature of the outer wall finishing material.

• 한국지리정보학회지
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• 제18권2호
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• pp.59-74
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• 2015

본 연구는 다양한 토지이용유형별로 도시열섬현상을 완화하기 위한 합리적 녹지율을 분석하고자 하였다. 토지이용유형은 단독주택과 공동주택, 공공시설, 상업지역, 공업지역의 5가지 유형을 고려하였고, 녹지지역은 토지피복도에서 수목 속성을 추출하여 활용하였다. 열섬효과는 주간 및 야간에 촬영된 다중시기의 ASTER TIR 영상의 표면온도를 이용하였다. 주간시간은 야간시간보다 녹지의 표면온도 저감 효과가 큰 것으로 나타났다. 토지이용유형별로는 주간시간에 단독주택에서 녹지율에 따른 표면온도 저감효과가 가장 뚜렷했지만, 야간시간에는 토지이용유형별로 차이가 크지 않았다. 공업지역은 녹지의 표면온도 저감 효과가 낮았다. 토지이용유형별 도시열섬완화를 위한 합리적 녹지율을 산출한 결과, 주간시간은 단독주택과 공동주택, 상업지역에서 녹지율이 40~50% 사이일 때, 표면온도가 가장 낮았고, 야간시간은 녹지율별로 표면온도 변화가 크지 않았다. 따라서 본 연구의 결과는 도시개발계획 단계에서 도시열섬완화를 위해 효과적인 녹지면적을 제시할 수 있을 것으로 판단된다.

• 대한지하수환경학회지
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• 제1권1호
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• pp.33-50
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• 1994

제주도 지하수자원의 산출특성을 규명키 위하여 총 455개 기존관정의 자료를 전산처리하여 지역별 대수성 수리특성을 규명하였다. 제주도는 주로 현무암내에 협재된 화산쇄설층, crinker층과 현무암의 1 및 2차 유효공극이 주 대수대의 역할을 하며 이들은 기저, 준기저 및 상위대수층으로 구성되어 있다. 본도 대수층의 평균 투수량계수는 29,300 $m^2$/일이며 평 균 저유계수는 0.12로써 자유면 대수층을 이루고 있다. 종합적인 물수지 분석을 실시한 바 본도에 부존된 지하수 부존량은 약 440억 ㎥이고, 년평균 강수량은 33.9억 ㎥으로써 이 중 하천유출량은 6.38억㎥/년이며, 증발산량은 12.56억 ㎥/년(37%)이고 지하수함양량은 년평균 강수량의 44.1%에 해당하는 14.94억㎥이다. 본도에 부존된 지하수의 최적 개발가능량(sustainable yield) 을 각 지역별로 정량적으로 계산한 결과 그 양은 함양량의 41%에 해당하는 6.2억㎥/년(1,689,000 ㎥/일) 정도였으며 잔여 8.74억㎥/년(2,404,000㎥/일)은 해안이나 해저용천의 형태로 유출된다. 특히 최근에 실시한 심부 시추조사 자료에 의하면 EL-120$\pm$68m 부근에 저투수성 해성 퇴적층(일명 세화리층)이 분포되어 있는 것으로 판명되었으며 과거 서귀포층군으로 알려진 저투수성 퇴적층이 북서부와 서부 일원에서 EL-70m 부근에 널리 분포되어 있어 서귀포층군과 세화리층의 명확한 구분이 필요하다. 만일 이러한 저투수성 퇴적층이 제주도의 기저층을 이루는 경우 제주도 내에 부존된 지하수는 주로 준기저 지하수일 것이며 이는 제주도 지하수의 산출특성에 결정적인 영향을 미칠 것이다.

• 한국광물학회지
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• 제10권2호
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• pp.148-161
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• 1997

Based on the X-ray powder diffraction (XRD) and M ssbauer spectroscopy, the thermal behavior and phase transformations of two clays are investigated for raw and fired conditions, which are collected from Kwangryeongli and Ildo district in Cheju Island. M ssbauer spectra at room temperature and 20for two clays show that paramagnetic Fe3- is the structural iron of the layer silicate and ferrihydrite, and superparamagnetic goethite has about 50% of total iron contents. The XRD peaks of hematite for the fired clays appear from 80$0^{\circ}C$ in Kwangryeongli clay and from $600^{\circ}C$ in Ildo district clay, respectively. The structural Fe2+ was completely oxidized into Fe3- at 40$0^{\circ}C$ for Kwangryeongli clay and 50$0^{\circ}C$~$600^{\circ}C$ for Ildo district clay, respectively. The structural Fe2+ was completely oxidized into Fe3- at 40$0^{\circ}C$. For the temperature ranging from 40$0^{\circ}C$ to $700^{\circ}C$~80$0^{\circ}C$, two fired clays exhibit the dehydroxylation of the clay mineral. A disintegration of the clay mineral structure is observed from $700^{\circ}C$~80$0^{\circ}C$ to 110$0^{\circ}C$, followed by the onset and spread of vitrification process. It is also shown that well-crystallized hematite phase is formed at the temperature higher than 110$0^{\circ}C$ and the relative absorption area decreases, which might be related to the recrystallization of alluminosilicate matrix.