• 대한기계학회논문집B
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• 제32권4호
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• pp.255-265
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• 2008

This paper presents the optimization process of evaporator for a vapor compression cooling system for high heat flux CPU. The CPU thermal capacity was given by 300W. Evaporating temperature and mass flow rate were $18^{\circ}C$ and 0.00182kg/s respectively. R134a was used as a working fluid. Channel width(CW) and height(CH) were selected as design factors. And thermal resistance, surface temperature of CPU, degree of superheat, and pressure drop were taken as objective responses. Fractional factorial DOE was used in screening phase and RSM(Response Surface Method) was used in optimization phase. As a result, CW of 2.5mm, CH of 2.5mm, and CL of 484mm were taken as an optimum geometry. Surface temperature of CPU and thermal resistance were $33^{\circ}C\;and\;0.0502^{\circ}C/W$ respectively. Thermal resistance of evaporator designed in this study was significantly lower than that of other cooling systems such as water cooling system and thermosyphon system. It was found that the evaporator considered in this work can be a excellent candidate for a high heat flux CPU cooling system.

• 대기
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• 제28권1호
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• pp.53-67
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• 2018

This study examined the lake effect of the Yellow Sea which was induced by the Siberian High pressure system moving over the open waters. The development mechanism of the convective cells over the ocean was studied in detail using the Weather Research and Forecasting model. Numerical experiments consist of the control experiment (CTL) and an experiment changing the yellow sea to dry land (EXP). The CTL simulation result showed distinct high area of relative vorticity, convergence and low-level atmospheric instability than that of the EXP. The result indicates that large surface vorticity and convergence induced vertical motion and low level instability over the ocean when the arctic Siberian air mass moved south over the Yellow Sea. The sensible heat flux at the sea surface gradually decreased while latent heat flux gradually increased. At the beginning stage of air mass modification, sensible heat was the main energy source for convective cell generation. However, in the later stage, latent heat became the main energy source for the development of convective cells. In conclusion, the mechanism of the west coast heavy snowfall caused by modification of the Siberian air mass over the Yellow Sea can be explained by air-sea interaction instability in the following order: (a) cyclonic vorticity caused by diabatic heating induce Ekman pumping and convergence at the surface, (b) sensible heat at the sea surface produce convection, and (c) this leads to latent heat release, and the development of convective cells. The overall process is a manifestation of air-sea interaction and enhancement of convection from positive feedback mechanism.

• 열처리공학회지
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• 제5권3호
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• pp.171-178
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• 1992

The effect of nozzle characterristics on the mist-cooling heat transfer was investigated under the various flow conditions. Two different types of twin fluid nozzle were used, one is a $90^{\circ}$ angle tip nozzle with needle and the other is a $90^{\circ}$ angle tip non-needle nozzle. The cooling rate from the heated surface was measured and obtained the boiling curve as a function of surface temperature. An immersion sampling was employed for the measurement of droplet size of the spray. As a result of this experiment, the liquid sheet type nozzle shows better atomization when the mass ratio Mr>2.0, and collects more liquid droplets on the heated surface that results in better cooling effect. It was found that the maximum heat flux and heat transfer coefficient increased with increase in the volumetric flow rate, whereas the maximum heat flux decreased with increase in spray distance. The cooling effect depends upon the amount of collected droplet and droplet size, but it strongly depends upon the amount of collected droplet.

• Journal of the Korean Wood Science and Technology
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• 제36권2호
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• pp.1-8
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• 2008

This study was performed to evaluate the burning characteristics of wood-based materials and the effect of surface treatment of fire retardant using cone calorimeter. Four types of wood-based materials, such as Plywood, Oriented Strand Board (OSB), Particle Board (PB) and Medium Density Fiberboard (MDF), were tested at a constant heat flux of $50kW/m^2$ to investigate the time to ignition, mass loss rate, heat release rate, effective heat of combustion, etc. In addition, each type of wood-based material was tested at the same heat flux after fire retardant treatment on the surface to evaluate the effect of this treatment on the burning characteristics. The surface treatment of fire retardant, by the amount of $110g/m^2$, delayed the time to ignition almost twice. However, it was indicated that heat release rate, mass loss rate, and effective heat of combustion were not significantly affected by fire retardants treatment for all types of wood-based materials.

• Nuclear Engineering and Technology
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• 제45권3호
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• pp.335-346
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• 2013

The Critical Heat Flux (CHF) of water with dispersed alumina nanoparticles was measured for the geometry and flow conditions relevant to the In-Vessel Retention (IVR) situation which can occur during core melting sequences in certain advanced Light Water Reactors (LWRs). CHF measurements were conducted in a flow boiling loop featuring a test section designed to be thermal-hydraulically similar to the vessel/insulation gap in the Westinghouse AP1000 plant. The effects of orientation angle, pressure, mass flux, fluid type, boiling time, surface material, and surface state were investigated. Results for water-based nanofluids with alumina nanoparticles (0.001% by volume) on stainless steel surface indicate an average 70% CHF enhancement with a range of 17% to 108% depending on the specific flow conditions expected for IVR. Experiments also indicate that only about thirty minutes of boiling time (which drives nanoparticle deposition) are needed to obtain substantial CHF enhancement with nanofluids.

• 한국습지학회지
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• 제15권4호
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• pp.509-518
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• 2013

지표와 대기간의 에너지 및 수문기상인자들의 교환에 대한 이해는 수자원분야의 연구에 있어서 기초라 할 수 있으며 이를 위하여 Land Surface Mode(LSM)을 활용한 연구가 활발히 진행되고 있다. Noah Land Surface Model (Noah LSM)은 에너지 방정식과 물수지 방정식을 기반으로 한 지면모형으로 수문기상인자들에 대한 모의가 가능하다. 국외에는 Noah LSM을 이용한 다양한 연구사례들이 있으나, 국내에서는 적용사례가 매우 부족하며, 특히 단독으로 Noah LSM을 적용한 사례는 전무한 실정이다. 본 연구에서는 Noah LSM의 국내 적용성을 평가하기 위해 해남(HFK)과 광릉(GDK) Korea Flux Network (KoFlux)에서 제공하는 자료를 입력자료로 활용하여 모형 결과를 산출하고, 순 복사량, 잠열, 현열의 결과를 관측자료와 비교 검증하였다. 모형 결과와 관측치를 비교한 결과 회귀분석에서의 상관계수 값이 각 인자 별로 해남은 0.83~099, 광릉은 0.64~0.99로 신뢰할 만한 수준인 것으로 나타났다.

• 한국해양학회지:바다
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• 제19권3호
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• pp.169-179
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• 2014

황해 남동부 해역에 설치한 해양부이(YSROB)에서 약 27개월간 관측된 장파, 단파 복사량을 포함한 대기, 해양 변수와 COARE 3.0 알고리즘을 이용하여 월평균 해양-대기간 열속을 산출하고 기존 연구결과와 비교하였다. YSROB 위치에서 열속은 순 단파복사(Qi)에 의해 해양은 대기로부터 열을 얻고 순 장파복사($Q_b$), 현열($Q_h$), 잠열($Q_e$)에 의해서 열손실이 일어난다. 전체 열손실 중 $Q_e$에 의한 손실이 51%로 가장 크게 나타났으며 $Q_b$와 $Q_h$에 의한 손실은 각각 34%, 15% 이다. 순열속($Q_n$)은 $Q_i$가 최대인 5월에 최대($191.4W/m^2$)이며 모든 열속 성분이 최소인 12월에 최소($-264.9W/m^2$)이다. 연평균 $Q_n$은 $1.9W/m^2$ 이지만 관측기기의 정확도에 의한 오차산정 결과(최대 ${\pm}19.7W/m^2$)를 고려하면 무시할 정도로 작다. YSROB과 동일한 위치에서의 기존 월별 열속 산출 결과는 YSROB에서 실측값에 기반한 열속에 비해 여름철 $Q_i$가 약 $10{\sim}40W/m^2$ 과소 평가된 반면에 겨울철에는 $Q_e$와 $Q_h$에 의한 열 손실이 각각 약 $50W/m^2$, $30{\sim}70W/m^2$ 과다하게 산출되었다. 이로 인하여 해양이 열을 얻는 4월~8월에는 기존 연구에서의 열 획득량이 본 연구 결과보다 적게 나타나며, 해양이 열을 잃는 겨울철에는 기존 연구에서의 해양으로부터의 열 손실이 본 연구 결과에 비해 크게 나타난다. 특히, 12월과 1월의 $Q_n$ 차이는 약 $70{\sim}130W/m^2$에 달한다. 장기적인 재분석장(MERRA) 분석 결과에 의하면 이와 같은 월평균 열속의 차이는 연변동 등 시간 변동에 의한 것이 아니라 열속 산출 시 사용된 자료의 부정확성에 기인하는 것으로 판단된다. 본 연구 결과로부터 기존의 기후적인 열속을 연구에 활용하거나 수치모델에 사용함에 있어 주의가 요망된다.

• Applied Science and Convergence Technology
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• 제23권5호
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• pp.248-253
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• 2014

Air Gap Membrane Distillation (AGMD) is one of several technologies that can be used to solve problems fresh water availability. AGMD exhibits several advantages, including low conductive heat loss and higher thermal efficiency, due to the presence of an air gap between the membrane and condensation wall. A previous study by Bhardwaj found that the condensation surface properties (materials and contact angle) affected the total collected fresh water in the solar distillation process. However, the process condition differences between solar distillation and AGMD might result in different condensation phenomena. In contrast, N. Miljkovic showed that a hydrophobic surface has higher condensation heat transfer. Moreover, to the best of our knowledge, there is no study that investigates the effect of condensation surface properties in AGMD to overall process performance (i.e. flux and thermal efficiency). Thus, in this study, we treated the AGMD condensation surface to make it hydrophobic or hydrophilic. The condensation surface could be made hydrophilic by immersing and boiling plate in deionized (DI) water, which caused the formation of hydrophilic aluminum hydroxide (AlOOH) nanostructures. Afterwards, the treated plate was coated using hexamethyldisiloxane (HMDSO) through plasma-enhanced chemical vapor deposition (PECVD). The result indicated that condensation surface properties do not affect the permeate flux or thermal efficiency significantly. In general, the permeate flux and thermal efficiency for the treated plates were lower than those of the non-treated plate (pristine). However, at a 1 mm and 3 mm air gap, the treated plate outperformed the non-treated plate (pristine) in terms of permeate flux. Therefore, although surface wettability effect was not significant, it still provided a little influence.

• 한국전자통신학회논문지
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• 제13권1호
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• pp.265-276
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• 2018

지상에 고정된 기기로 감시하기 어려운 대기 하층의 관측 사각 지역에서 유용한 관측 및 자료 분석 기술을 개발하였다. 상층 기상 관측에 사용되는 UHF 라디오존데를 UAV에 탑재하여 기온과 상대습도의 연직 자료를 원격 수집하여 10 m 기상 타워에서 측정한 자료와 비교하였다. 검증된 연직 분포로부터 외삽된 지표 기온과 총체 전달 방법을 이용하여 대기 안정도 변화에 따른 현열 플럭스를 추정하였다. 지상에서 3차원 초음파 풍속계로 측정한 현열 플럭스와 비교한 결과는 원격탐사로 산출되는 현열 플럭스에 허용되는 오차 범위 30%보다 작은 23% 이내의 오차를 보였다. UAV 관측 현열 플럭스로부터 추정한 대기경계층 고도는 대기 오염 확산 모델에 유용한 자료를 실시간, 경제적으로 제공할 수 있다.

• Ocean and Polar Research
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• 제26권2호
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• pp.145-154
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• 2004

Surface energy and $CO_2$ fluxes have been measured over an ocean at Ieodo Ocean Research Station of KORDI since May 2003. Eddy covariance technique, which is a direct flux measurement, is used to quantitatively understand the interaction between the ocean surface and the atmospheric boundary layer. Although fluxes were continuously measured during the period from May 2003 to February 2004, the quality control of these data yielded <20% of data retrieval. The atmospheric stability did not show any distinct dirunal patterns and remained near-neutral to stable from May to June but mostly unstable during fall and winter in 2003. Sensible heat flux showed a good correlation with the difference between the sea water temperature and the air temperature. The maximum fluxes of sensible heat and latent heat were $120Wm^{-2}$ and $350Wm^{-2}$ respectively, with an averaged Bowen ratio of 0.2. The ocean around the tower absorbed $CO_2$ from the atmosphere and the uptake rates showed seasonal variations. Based our preliminary results, the daytime $CO_2$ flux was steady with an average of $-0.1 mgCO_2m^{-2}s^{-1}$ in summer and increased in winter. The nighttime $CO_2$ uptake was greater and fluctuating, reaching up to $-0.1 mgCO_2m^{-2}s^{-1}$ but these data require further examination due to weak turbulent mixing at nighttime. The magnitude of $CO_2$ flux was positively correlated with the half hourly changes in horizontal mean wind speed. Due to the paucity of quality data, further data collection is needed for more detailed analyses and interpretation.