• 한국수소및신에너지학회논문집
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• 제7권2호
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• pp.121-128
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• 1996

수소액화를 위한 직접냉각장치를 개발하고, 이의 성능특성을 시험하였다. 직접냉각장치는 액화용기, 복사쉴드, 저온조와 GM냉동기 등으로 구성하였다. 개발된 액화장치의 cool-down 및 warm-up특성이 상세하게 규명되었다. 본 냉각장치에서 냉각이 시작된지 약 45분 후, 액화용기내의 수소가 액화되기 시작함을 확인하였다. 또한 동일한 실험을 기체헬륨에 대하여 수행하였으며, 기체헬륨은 주어진 작동조건에서 액화되지 않으므로 수소의 경우와는 다른 cool-down 및 warm-up 특성을 보였다. 충전된 기체의 자연대류현상의 영향을 고찰하기 위하여 액화용기내에 진공상태를 유지하면서 시험하였다. 이때 진공상태에서의 액화용기의 냉각시간은 현저히 증가함을 보였다.

• 대한원격탐사학회지
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• 제38권6_2호
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• pp.1607-1622
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• 2022

본 연구의 목적은 도시폭염 저감을 위한 기법인 쿨루프를 연구지역에 적용하여 토지피복 객체 간 지표 온도와 흡수일사 간 공간적 상관관계 분석으로 실질적 효과 파악을 목적으로 한다. 이를 위해 실제 쿨루프가 적용된 경상남도 김해시 장유무계동 인근을 연구지역으로 선정하였으며, 드론 DJI Matrice 300 RTK에 열적외 영역센서 FLIR Vue Pro R, 가시광선 영역센서 H20T와 다중분광영역 센서인 Micasense Red-Edge를 활용하여 계측하였다. 계측 일정은 2021년 7월 27일 아침 7시 15분부터 약 1시간 30분 간격으로 총 9장의 열지도와 동일 시간대의 흡수일사 분포도, 쿨루프(113개) 및 일반옥상(367개) 지붕 객체를 추출하였다. 흡수일사 분포도는 ArcGIS의 3D 분석 기능인 Solar Radiation Analysis Tool을 통해 산출한 전천일사 분포도에 Micasense Red Edge를 통해 촬영한 Blue, Green Red, Near Infrared, Red Edge Range 영역대 센서의 조합을 통해 구축한 연구 지역의 알베도 값을 반영하여 구축한다. 전술된 자료를 기반으로 일반옥상과 쿨루프 지붕 객체별 지표온도와 흡수일사 간 Pearson 상관계수를 산출하였다. 분석 결과 일 평균 기준 일반옥상 0.550, 쿨루프 0.387의 상관계수 값을 나타내고 있었다. 하지만, 시간대별 상관성의 변화를 파악한 결과 분석일 기준 태양고도가 높은 시기인 11시 30분과 13시의 경우 일반옥상과 쿨루프 간 상관계수의 차이는 0.022, 0.024 값을 보여 유사한 상관성을 보이고 있다. 그 외 시간대는 일반옥상의 상관계수 값이 쿨루프 보다 약 0.1 이상 높은 값을 보이고 있다. 본 연구는 드론을 통해 취득한 고해상도 영상을 활용하여 쿨루프의 실질적 일사차단 영향의 가능성을 대조군이 되는 일반 옥상과의 상관성 비교를 통해 파악한 사례 연구이다. 향후 본 연구 결과를 기반으로 효율적인 도시열섬 저감기법 적용이 가능할 것으로 사료된다.

• KIEAE Journal
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• 제8권5호
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• pp.11-16
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• 2008

This research has established CFD model on pit's cool-tube system through heat and air movement simulations, of which data was based on experimental and verification. This research work verified the effectiveness of the cool-tube system by analysing temperature, humidity and air current of the actually installed case. Also, we analysed heat transfer through air current simulation and the results are as followings. Firstly, we experiment on temperature, humidity and speed of air currents of the cool tube system with pit space during the month of May (spring). The average exterior temperature was $16.1^{\circ}C$, and $18.2^{\circ}C$ for the pit, $24.7^{\circ}C$ for the compressor room. Secondly, based on measured data of real case, we have analysed heat transfer through air current simulation and verified our proposed model. The actual measurement of average temperature of exhaust air of the pit's area is $19.7^{\circ}C$ with tolerance of $-0.33^{\circ}C{\sim}-0.6^{\circ}C$ compared to above simulations. Thirdly, having verified air current simulation model with formation of 260,000 and 1,000,000 cells, we could get reasonable near values with 260,000 cells. Lastly, the next step of research would be focused on proposing the best possible pit's cool-tube system after analysis of heat transfer of the air current simulation based on verified CFD model.

• 설비공학논문집
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• 제9권3호
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• pp.284-291
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• 1997

A hydrogen liquefaction equipment by direct cooling has been designed and built at KIST. Cool-down characteristics and liquefaction performance of the equipment have been investigated. The hydrogen liquefaction equipment consists of a GM refrigerator, a liquefaction velssel, a radiation shield and a cryostat. It is found that the hydrogen starts to be liquefied in the liquefaction vessel after 40~50 minutes of cool-down from the gas state of 270K. The effect of natural convection phenomena of charged gas in liquefaction vessel on the cool-down characteristics is evaluated by comparing with those in vacuum of liquefaction vessel. It is seen that the cool-down time of a liquefaction vessel is substantially increased in vacuum environment of liquefaction vessel. The experiments have been performed for 1~5 atm of hydrogen pressure to investigate the influence of hydrogen pressure on the liquefaction rate and figure of merit(FOM). It is found that both liquefaction rate and FOM are increased as the charged hydrogen pressure is increased.

• 천문학회보
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• 제45권1호
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• pp.30.2-31
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• 2020

We present the properties of circumnuclear gas associated with the AGN located in the center of Abell 1644-South. A1644-S is the main cluster in a merging system, which is also known for gas sloshing in its core as seen in X-ray. The X-ray emission of A1644-S shows a rapidly declining profile, indicating the presence of cooling gas flow. This flow of cool gas may fuel the supermassive black hole embedded in the brightest cluster galaxy, leading to the activation of the central AGN. Indeed, we find a parsec-scale bipolar jet feature in the center of A1644-S in our recent KaVA observation, which implies that its central AGN is likely to have been (re)powered quite recently. In order to verify the hypothesis that cooling gas flow in the cluster core can (re)activate the central AGN, we probe the cold gas properties of the central 1 kpc region of A1644-S using the archival VLA and ALMA data. Based on the spatially resolved morphology and kinematics of HI and CO gas, we challenge to identify inflow/outflow gas streams and clumps. We study the role of circumnuclear cool gas in fueling the centrally located cluster AGN in the cool-core environment. We also discuss how the feedback due to the (re)powered AGN affects the surrounding medium.

• Asian Journal of Atmospheric Environment
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• 제7권1호
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• pp.17-24
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• 2013

Fog deposition onto the cool-temperate deciduous forest around Lake Mashu in northern Japan was estimated by the inferential method using the parameterizations of deposition velocity and liquid water content of fog (LWC). Two parameterizations of fog deposition velocity derived from field experiments in Europe and numerical simulations using a detailed multi-layer atmosphere-vegetation-soil model were tested. The empirical function between horizontal visibility (VIS) and LWC was applied to produce hourly LWC as an input data for the inferential method. Weekly mean LWC computed from VIS had a good correlation with LWC sampled by an active string-fog collector. By considering the enhancement of fog deposition due to the edge effect, fog deposition calculated by the inferential method using two parameterizations of deposition velocity agreed with that computed from throughfall data. The results indicated that the inferential method using the current parameterizations of deposition velocity and LWC can provide a rough estimation of water input due to fog deposition onto cool-temperature deciduous forests. Limitations of current parameterizations of deposition velocity related to wind speed, evaporation loss of rain and fog droplets intercepted by tree canopies, and leaf area index were discussed.

• Journal of Ceramic Processing Research
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• 제20권spc1호
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• pp.86-91
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• 2019

A solid-state route was used to prepare sodium titanium oxide (NTO, Na2Ti3O7) as a solar heat protecting material with an impressive solar reflectance (TSR = 94.3%) using a high refractive index rutile TiO2. The solar reflectance of the synthesized NTO was measured using UV-Vis-NIR spectrophotometer. Solar reflectance property of the synthesized compound depends on the calcination temperature. The solar reflectance property of the synthesized NTO powder was compared with commercial rutile TiO2. The compound synthesized at 900 ℃ for 24 hrs had remarkable solar reflectance 94.3% than that calcined below 900 ℃. Crystalline nature, structural property, morphology and optical properties of NTO powders were characterized and analyzed using XRD, FE-SEM, EDS and UV-Vis-NIR spectrophotometer. From the results, we guessed that NTO would be a suitable "solar heat protecting candidate" for energy-saving applications in coating industries.

• 대한원격탐사학회지
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• 제37권6_3호
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• pp.1985-1999
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• 2021

본 연구의 목적은 EPA(Environmental Protection Agency)에서 활용하는 도시열섬 저감기법(옥상녹화, 쿨루프, 차열도료포장 및 차열블럭포장 등)을 연구지역에 적용하여 토지피복 객체간 비교 분석으로 실질적 효과 파악을 목적으로 한다. 이를 위해, 경상남도 김해시 장유무계지역을 연구지역으로 선정하고, 드론 DJI Matrice 300 RTK에 열적외선 영역센서 FLIR Vue Pro R과 가시광선 영역센서인 H20T 1/2.3" CMOS, 12 MP를 활용하여 계측하였다. 계측 일정은 7월 27일 아침 7시 15분부터 저녁 7시 15분까지 1시간 30분 간격으로 총 9장의 열지도와 비교군 토지피복 객체(711개) 열섬 저감기법 토지피복 객체(180개) 를 추출하였다. 추출한 180개의 객체 별 효과값 산출 후, 기법 종류별 효과를 종합한 결과 주간시간 기준 쿨루프 4.71℃, 옥상녹화 3.40℃, 차열도료포장 0.43℃, 차열블록포장 -0.85℃의 열섬 저감효과가 있는 것으로 분석되었다. 시간대별 효과 비교 결과 촬영일 기준 남중시각 인근인 13시에서 기법들의 열섬 저감효과가 가장 높은 것으로 나타났으며, 해당 시각을 지난 13시에서 14:30분 사이에 쿨루프 -8.19℃, 옥상녹화 -5.56℃, 차열도료포장 -1.78℃, 차열블록포장 -1.57℃의 온도 저감의 효율이 변화하였다. 본 연구는 드론과 같은 고해상도 영상을 활용하여 도시열섬 저감기법을 검증한 사례 연구이다. 향후, 고정밀 공간해상도를 가지는 초소형 위성 등의 직접적인 활용 예시가 가능할 것으로 사료된다.

• Nuclear Engineering and Technology
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• 제47권6호
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• pp.746-755
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• 2015

To investigate the effect of hydrogen and oxygen contents on hydride reorientations during cool-down processes, zirconium-niobium cladding tube specimens were hydrogen-charged before some specimens were oxidized, resulting in 250 ppm and 500 ppm hydrogen-charged specimens containing no oxide and an oxide thickness of $0.38{\mu}m$ at each surface. The nonoxidized and oxidized hydrogen-charged specimens were heated up to $400^{\circ}C$ and then cooled down to room temperature at cooling rates of $0.3^{\circ}C/min$ and $8.0^{\circ}C/min$ under a tensile hoop stress of 150 MPa. The lower hydrogen contents and the slower cooling rate generated a larger fraction of radial hydrides, a longer radial hydride length, and a lower ultimate tensile strength and plastic elongation. In addition, the oxidized specimens generated a smaller fraction of radial hydrides and a lower ultimate tensile strength and plastic elongation than the nonoxidized specimens. This may be due to: a solubility difference between room temperature and $400^{\circ}C$; an oxygen-induced increase in hydrogen solubility and radial hydride nucleation energy; high temperature residence time during the cool-down; or undissolved circumferential hydrides at $400^{\circ}C$.

• Journal of Ecology and Environment
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• 제34권3호
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• pp.259-267
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• 2011

A pollen analytical study of sediment sequences collected from Yongneup moor (sampling point: $38^{\circ}$12'57.4" N, $120^{\circ}$7'30.2" E) was conducted to understand the vegetation history in the mountainous region of the central Korean peninsula. Carbon dating was carried out to measure five successive samples obtained from the bottom at a depth of 180 cm to the surface. The Yongneup moor sediment revealed four main local pollen zones; that is, four past vegetation phases as follows: Local pollen zone I: Quercus-Pinus zone; estimated age, 5,900-4,800 calibrated years (cal) before present (BP); vegetation type, cool-temperate central/montane deciduous broad-leaved forest. Local pollen zone II: Pinus-Abies-Quercus zone; estimated age, 4,800-3,400 cal BP; vegetation type, cool-temperate northern/alti-montane mixed coniferous and deciduous broad-leaved forest. Local pollen zone III: Quercus-Pinus-Abies zone; estimated age, 3,400-400 cal BP; vegetation type: cool-temperate central/montane deciduous broad-leaved forest. Local pollen zone IV: Pinus-Quercus zone; estimated age, 400-present cal BP; vegetation type, cool-temperate central/montane mixed deciduous broad-leaved and coniferous forest. It was confirmed that subalpine coniferous forests had expanded to the mountainous region of the central Korean peninsula during the period from 4,800-3,400 cal BP and thereafter deciduous forests dominated by Q. mongolica were established. Notably, secondary forests dominated by P. densiflora developed in the lower part of the mountainous region of the central Korean peninsula about 400 cal BP due to human interference.