• 제목/요약/키워드: vertical temperature structure

검색결과 215건 처리시간 0.025초

가열된 원주후류의 열성층 영향에 대한 연구 (A Study on the Effect of Thermal Stratification of a Heated Cylinder Wake)

  • 김경천;정양범
    • 대한기계학회논문집
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    • 제18권9호
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    • pp.2454-2462
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    • 1994
  • The effects of thermal stratification on the flow of a stratified fluid past a heated circular cylinder were examined in a wind tunnel. Turbulent intensities, rms values of temperature and turbulent convective heat flux distributions in the heated cylinder wake with and without thermal stratification were measured by using a hot-wire and cold-wire combination probe. A phase averaging method was also used to estimated coherent motion in the near wake. It is found that the vertical turbulent motion in the stably stratified flow case dissipates faster than that of the neutral case, i.e., vertical growth of vortical structure is suppressed under the strongly stratified condition. The coherent motion of temperature makes a large contribution like velocity coherent motion. However, the coherent motions of temperature fluctuation become very different with the change of experimental conditions, though the velocity coherent motions are quite similar in all experimental conditions.

지하수정호와 결합한 복합지열시스템의 열교환 효율에 대한 실험적 연구 (Experimental Study on Heat Exchange Efficiency of Combined Well & Open-Closed Loops Geothermal System)

  • 송재용;이근춘;박남서
    • 대한건축학회논문집:구조계
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    • 제34권5호
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    • pp.43-50
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    • 2018
  • The temperature of underground water generally remains constant regardless of the season. therefore, it is possible to get plenty of energy if we use characteristics of underground water for both cooling and heating. This study evaluates efficiency of real size coaxial and U-tube type complex geothermal system which is combined with underground water well. This study also evaluates relative efficiency/adaptability through comparison with existing geothermal systems(vertical closed loop system, open loop system(SCW)). The heat exchange capacity of complex geothermal system according to temperature difference between circulating water and underground water shows very high significance by increasing proportionally. The temperature change of underground water according to injection energy, shows very high linear growth aspect as injection thermal volume heightens. As a result of evaluation of heat exchange volume between complex geothermal system and comparative geothermal system, coaxial type has 26.1 times greater efficiency than comparative vertical closed type and 2.8 times greater efficiency than SCW type. U-tube type has 26.5 tims greater efficiency than comparative vertical closed type and 2.8 times greater than SCW type as well. This means complex geothermal system has extremely outstanding performance.

Experimental research on vertical mechanical performance of embedded through-penetrating steel-concrete composite joint in high-temperature gas-cooled reactor pebble-bed module

  • Zhang, Peiyao;Guo, Quanquan;Pang, Sen;Sun, Yunlun;Chen, Yan
    • Nuclear Engineering and Technology
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    • 제54권1호
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    • pp.357-373
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    • 2022
  • The high-temperature gas-cooled reactor pebble-bed module project is the first commercial Generation-IV NPP(Nuclear Power Plant) in China. A new joint is used for the vertical support of RPV(Reactor Pressure Vessel). The steel corbel is integrally embedded into the reactor-cabin wall through eight asymmetrically arranged pre-stressed high-strength bolts, achieving the different path transmission of shear force and moment. The vertical monotonic loading test of two specimens is conducted. The results show that the failure mode of the joint is bolt fracture. There is no prominent yield stage in the whole loading process. The stress of bolts is linearly distributed along the height of corbel at initial loading. As the load increases, the height of neutral axis of bolts gradually decreases. The upper and lower edges of the wall opening contact the corbel plate to restrict the rotation of the corbel. During the loading, the pre-stress of some bolts decreases. The increase of the pre-stress strength ratio of bolts has no noticeable effect on the structure stiffness, but it reduces the ultimate bearing capacity of the joint. A simplified calculation model for the elastic stage of the joint is established, and the estimation results are in good agreement with the experimental results.

Fiber network with superhydrophilic Si-DLC coating

  • 김성진;문명운;이광렬;김호영
    • 한국진공학회:학술대회논문집
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    • 한국진공학회 2009년도 제38회 동계학술대회 초록집
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    • pp.363-363
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    • 2010
  • The high capillarity of a plastic fiber network having superhydrophilic Si-DLC coating is studied. Although the superhydrophilic surface maximize wetting ability on the flat surface, there remains a requirement for the more wettable surface for various applications such as air-filters or liquid-filters. In this research, the PET non-woven fabric surface was realized by superhydrophilic coating. PTE non-woven fabric network was chosen due to its micro-pore structure, cheap price, and productivity. Superhydrophobic fiber network was prepared with a coating of oxgyen plasma treated Si-DLC films using plasma-enhanced chemical vapor deposition (PECVD). We first fabricated superhydrophilic fabric structure by using a polyethylene terephthalate (PET) non-woven fabric (NWF) coated with a nanostructured films of the Si-incorporated diamond-like carbon (Si-DLC) followed by the plasma dry etching with oxygen. The Si-DLC with oxygen plasma etching becomes a superhydrophilic and the Si-DLC coating have several advantages of easy coating procedure at room temperature, strong mechanical performance, and long-lasting property in superhydrophilicity. It was found that the superhydrophobic fiber network shows better wicking ability through micro-pores and enables water to have much faster spreading speed than merely superhydrophilic surface. Here, capillarity on superhydrophilic fabric structure is investigated from the spreading pattern of water flowing on the vertical surface in a gravitational field. As water flows on vertical flat solid surface always fall down in gravitational direction (i.e. gravity dominant flow), while water flows on vertical superhydrophilic fabric surface showed the capillary dominant spreading.

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생태계모델을 이용한 황해투기해역에서의 춘계 식물플랑크톤 대증식 연구 (Ecological Model Experiments of the Spring Bloom at a Dumping Site in the Yellow Sea)

  • 송규민;이상룡;이석;안유환
    • Ocean and Polar Research
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    • 제29권3호
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    • pp.217-231
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    • 2007
  • To explore limiting factors of spring bloom caused by waste disposal after dumping activity commenced in the Yellow Sea, we used a 1-dimensional temperature-ecological coupled model. The vertical structure of temperature and vertical diffusivity (Kh) are calculated by the temperature model with sea surface temperature using the 2.5 layers turbulence closure scheme. The ecological model applied results at the temperature model consisted of five state variables (DIN, DIP, phytoplankton, zooplankton, and detritus) forced by photosynthetically available radiation. We simulate year-to-year variations of plankton and nutrients using the coupled model from 1998 to 2000 and compare results of the model with observed data. It turned out that temperature is the growth factor of spring bloom in dumping area. During the winter the weak stratification made sufficient supply of the accumulated nutrients from the sea bed into the upper water column and led to the bloom in the coming spring. Radiation also turned out to be another important factor of spring bloom in the study area. Insufficient radiation of March 1999 showed low chlorophyll-a concentration despite sufficient nutrients in the surface.

목포항 수질의 계절적 변화 특성 I. 물리 환경과 유기 오염 (The Characteristics of Seasonal Variations of Water Quality in Mokpo Harbour 1. Physical Environment and Organic Pollution)

  • 김광수
    • 해양환경안전학회지
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    • 제5권2호
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    • pp.57-65
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    • 1999
  • The in situ observations and the seawater analyses were conducted at all seasons from July 1996 to April 1999 for the purpose of describing the characteristics of seasonal variations of water quality in Mokpo harbour, Korea. Vertical stratification started to be formed in water column in spring, developed in summer and disappeared in fall. In summer, vertical density distribution of water column was found to be in stable structure with lower temperature and higher salinity of bottom water, and the vertical mixing of water between surface and bottom layers was restricted. In winter, however, surface water was found to be similar to bottom water in temperature and salinity, and water column was in unstable structure and in well-mixed condition between surface and bottom waters. The saturation percentage of dissolved oxygen(DO) in bottom water of inner part of Mokpo harbour at all seasons was shown to be decreased to the third grade or under the third grade of Korean standards of seawater quality. In particular, dissolved oxygen was oversaturated in surface water and undersaturated in bottom water in summer, due to stratification and organic pollution. The difference of DO concentration between surface and bottom waters was found to be greater in spring and summer than in fall and winter, due to stratification and photosynthesis of phytoplankton. The concentrations of chemical oxygen demand(COD) over the entire waters of Mokpo harbour were found to fluctuate from below the third grade to the first grade of Korean standards through all seasons and COD concentrations of same seasons were shown to be different year after year. In particular, in view of COD, the annual average seawater quality of Mokpo harbour was evaluated to be in third grade of Korean standards, due to organic pollution. The average COD of surface water was greater than that of bottom water in spring and summer, due to the autochthonous COD caused by production of phytoplankton in surface waters, while the average COD of surface water was similar to that of bottom water in fall and winter, due to the vertical mixing of water between surface and bottom layers.

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부산연안역의 대기경계층내 잔류 오존의 연직하향혼합에 의한 지표 오존농도의 변화 특성 (Variations of Surface Ozone Concentration by Vertical Downward Mixing of Ozone in the Residual Layer of the Atmospheric Boundary Layer at the Busan Coastal Area)

  • 전병일
    • 한국환경과학회지
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    • 제10권6호
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    • pp.417-422
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    • 2001
  • The vertical structure of atmosphere was observed In investigate the variation of surface ozone concentration by vertical downward mixing of residual ozone in the atmospheric boundary layer at the Busan coastal area. Airsonde and pilot balloon measurements were made at Gamcheondong and the Kimhae airport for April 26~27, 1996. The vertical potential of potential temperature showed a residual layer between 510m and 1800m from 2100LST April 26 to 0900LST April 27. The downward mixing of ozone in the residual layer of the atmospheric boundary layer was confirmed from vertical profile of mixing ratio near 600m in the morning. The thickness of the sea breeze layer was 900m at 1500LST April 26. Thereafter, it become to be lowered with time A low level jet was measured near 900m at 0300LST on April 27 from a pibal measurement. Early morning sharp increase of surface ozone concentration at the Busan coastal area was caused by vertical downward mixing of ozone concentration rather than by photochemical reaction In the atmospheric boundary layer.

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옥정호의 연직 수온분포에 관한 시변화 모델 연구 (A Time Variable Modeling Study of Vertical Temperature Profiles in the Okjung Lake)

  • 박옥란;박석순
    • 생태와환경
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    • 제35권2호통권98호
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    • pp.79-91
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    • 2002
  • 섬진강 상류에 위치한 옥정호의 연직 수온 분포 계절 변화에 대한 시변화 모델 연구를 수행하였다. 미공병단에서 개발한 CE-QUAL-W2모델 구조에 기초하여 호수를 3개의 지류, 50개의 상하류 구획 그리고 49개의 수층으로 구성하였으며 일년동안의 연직 수온 및 유속 분 포를 시뮬레이션하였다. 호수내 5개 지점에서 매월 측정된 연직 수온 분포 자료를 이용하여 보정하고 검증하였다. 또한, 시뮬레이션한 연중 수위 자료 변화를 관측된 자료와 비교하여 호수내 물수지를 확인하였다. 모델 예측값은 실측값과 적절한 일치를 보였으나 7월 관측 자료에서 다소 차이를 보였다. 이것은 우리나라에서 여름 장마동안 급격한 수리 현상 변화를 모델이 표현할 수없는 점과 이 기간동안 사용된 기온자료의 정확성이 부족하였기 때문인 것으로 사료된다. 모델 결과는 옥정호대부분 수역에서 연중 $4^{\circ}C$ 이상을 유지하여 계절에 따른 전도현상이 없는 것을 보여준다. 그러나 상류 얕은 수역 (수심 20미터 이내)에서는 수온이 $4^{\circ}C$ 이하로 떨어지며 겨울에 물이 얼어 흔합이 일어나는 것으로 나타났다. 본 연구로부터 옥정호는 빈혼합 호수라는 결론을 얻었다. 이러한 결론은 위도 $20^{\circ}C$ 부터 $40^{\circ}C$ 사이에 위치한 호수는 일회혼합이라는 일반적 경향과는 크게 다르다. 시뮬레이션한 유속 분포를 검토한 결과 여름 장마기간동안 상류에서 유입되는 물은 수온에 의한 밀도 차이로 인하여 호수 중층으로 유입되는 것이 확인되었다.

Fabrication and Characterization of Silicon Probe Tip for Vertical Probe Card Using MEMS Technology

  • Kim, Young-Min;Yu, In-Sik;Lee, Jong-Hyun
    • KIEE International Transactions on Electrophysics and Applications
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    • 제4C권4호
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    • pp.149-154
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    • 2004
  • This paper presents a silicon probe tip for vertical probe card application. The silicon probe tip was fabricated using MEMS technology such as porous silicon micromachining and deep- RIE (reactive ion etching). The thickness of the silicon epitaxial layers was 5 ${\mu}{\textrm}{m}$ and 7 ${\mu}{\textrm}{m}$, respectively. The width and length were 40 ${\mu}{\textrm}{m}$ and 600 ${\mu}{\textrm}{m}$, respectively. The probe structure was a multilayered structure and was composed of Au/Ni-Cr/Si$_3$N$_4$/n-epi layers. The height of the curled probe tip was measured as a function of the annealing temperature and time. Resistance characteristics of the probe tip were measured using a touchdown test.

Terra/MODIS 자료를 이용한 연안 대기경계층의 연직구조 (Vertical Structure of the Coastal Atmospheric Boundary Layer Based on Terra/MODIS Data)

  • 김동수;권병혁
    • 대기
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    • 제17권3호
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    • pp.281-289
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    • 2007
  • Micrometeorlogical and upper air observation have been conducted in order to determine the atmospheric boundary layer depth based on data from satellite and automatic weather systems. Terra/MODIS temperature profiles and sensible heat fluxes from the gradient method were used to estimate the mixed layer height over a coastal region. Results of the integral model were in good agreement with the mixed layer height observed using GPS radiosonde at Wolsung ($35.72^{\circ}N$, $129.48^{\circ}E$). Since the variation of the mixed layer height depends on the surface sensible heat flux, the integral model estimated properly the mixed layer height in the daytime. The buoyant heat flux, which is more important than the sensible heat flux in the coastal region, must be taken into consideration to improve the integral model. The vertical structure of atmospheric boundary layer can be analyzed only with the routine data and the satellite data.