• 제목/요약/키워드: Kelvin wave

검색결과 79건 처리시간 0.022초

Experimental research on the mechanisms of condensation induced water hammer in a natural circulation system

  • Sun, Jianchuang;Deng, Jian;Ran, Xu;Cao, Xiaxin;Fan, Guangming;Ding, Ming
    • Nuclear Engineering and Technology
    • /
    • 제53권11호
    • /
    • pp.3635-3642
    • /
    • 2021
  • Natural circulation systems (NCSs) are extensively applied in nuclear power plants because of their simplicity and inherent safety features. For some passive natural circulation systems in floating nuclear power plants (FNPPs), the ocean is commonly used as the heat sink. Condensation induced water hammer (CIWH) events may appear as the steam directly contacts the subcooled seawater, which seriously threatens the safe operation and integrity of the NCSs. Nevertheless, the research on the formation mechanisms of CIWH is insufficient, especially in NCSs. In this paper, the characteristics of flow rate and fluid temperature are emphatically analyzed. Then the formation types of CIWH are identified by visualization method. The experimental results reveal that due to the different size and formation periods of steam slugs, the flow rate presents continuous and irregular oscillation. The fluid in the horizontal hot pipe section near the water tank is always subcooled due to the reverse flow phenomenon. Moreover, the transition from stratified flow to slug flow can cause CIWH and enhance flow instability. Three types of formation mechanisms of CIWH, including the Kelvin-Helmholtz instability, the interaction of solitary wave and interface wave, and the pressure wave induced by CIWH, are obtained by identifying 67 CIWH events.

비선형 조파현상의 수치해법 (A Numerical Method for Nonlinear Wave-Making Phenomena)

  • 김장환;배광준
    • 대한조선학회논문집
    • /
    • 제30권1호
    • /
    • pp.65-72
    • /
    • 1993
  • 본 논문에서는 비선형 자유표면파 문제에 대한 수치해법을 개발하였다. 궁극적인 물리적 모델은 수조시험에서의 조파저항 실험으로서 이를 모사하는 수치실험을 위한 수치해법을 개발하는데 그 목적이 있다. 수치해법으로서는 선형 문제에서 이미 수치방사조건의 효율성이 입증된 국소유한요소법을 비선형 문제에 응용하였다. 수치 계산과정에서는 교란원인 압력 분포면으로부터 멀리 떨어진 곳에서는 선형해를 이용하고 교란원 근처에서는 엄밀한 비선형 조건을 만족시켰다. 비선형 영역과 선형 영역 사이에는 비선형-선형 천이 완충영역을 수치 계산영역 내에 도입하여 적절히 수치 정합을 하였다. 수치 계산 과정중 각 축차 단계에서의 모드 해석을 이용하여 계산 시간을 월등히 줄일 수 있었다. 수치 계산 모형으로는 수조 실험을 모사한 자유표면 압력 분포면이 균일한 속도로 전진하는 문제를 택하였다. 본 수치계산 방법의 효율성으로 인하여 기존의 수치 계산 방법에 비해 월등이 큰 계산영역을 사용 수치계산을 수행할 수 있었다. 교란원에서 먼 하류에서 채택된 비선형 자유표면파를 선형 계산 결과와 비교하여 그동안 부분적으로 연구된 비선형파의 특성을 규명할 수 있었다. 비선형 효과에 의해 캘빈각이 증가하며, 캘빈각 근처의 파고와 파수가 증가하는 것을 확인하였다.

  • PDF

횡단류를 이용한 액체제트의 분무 및 분열 특성 실험 (Experimental Study of Spray Characteristics of Liquid jet in Cross-flow)

  • 고정빈;이관형;문희장;구자예
    • 한국추진공학회:학술대회논문집
    • /
    • 한국추진공학회 2005년도 제24회 춘계학술대회논문집
    • /
    • pp.155-158
    • /
    • 2005
  • The spray characteristics of liquid jet minted in subsonic cross-flow were investigated numerically and experimentally. The behaviors of column, penetration and breakup of plain liquid jet in non-swirling cross-flow of air have been studied. Numerical and physical models are based on a modified KIVAII code. The primary atomization is represented by a wave model based on the KH(Kelvin-Helmholtz) instability that is generated by a high interface relative velocity between the liquid and gas flows. CCD camera has been utilized in oder to capture the spray trajectory. The nozzle diameter was 0.5 mm and its L/D ratios were between 1 and 5. Numerical and experimental results indicate that the breakup point is delayed by increasing gas momentum ratio, the penetration decreases by increasing Weber number and the turbulent or nonturbulent liquid jet is obtained at different L/D ratio.

  • PDF

EUNHA: A NEW COSMOLOGICAL HYDRODYNAMIC SIMULATION CODE

  • Shin, Jihye;Kim, Juhan;Kim, Sungsoo S.;Park, Changbom
    • 천문학회지
    • /
    • 제47권3호
    • /
    • pp.87-98
    • /
    • 2014
  • We develop a parallel cosmological hydrodynamic simulation code designed for the study of formation and evolution of cosmological structures. The gravitational force is calculated using the TreePM method and the hydrodynamics is implemented based on the smoothed particle hydrodynamics. The initial displacement and velocity of simulation particles are calculated according to second-order Lagrangian perturbation theory using the power spectra of dark matter and baryonic matter. The initial background temperature is given by Recfast and the temperature uctuations at the initial particle position are assigned according to the adiabatic model. We use a time-limiter scheme over the individual time steps to capture shock-fronts and to ease the time-step tension between the shock and preshock particles. We also include the astrophysical gas processes of radiative heating/cooling, star formation, metal enrichment, and supernova feedback. We test the code in several standard cases such as one-dimensional Riemann problems, Kelvin-Helmholtz, and Sedov blast wave instability. Star formation on the galactic disk is investigated to check whether the Schmidt-Kennicutt relation is properly recovered. We also study global star formation history at different simulation resolutions and compare them with observations.

Interaction among the East Asian Summer and Winter Monsoons, the Tropical Western Pacific and ENSO Cycle

  • Huang, Rong-Hui;Lu, Ri-Yu;Chen, Wen;Chen, Ji-Rong
    • 대기
    • /
    • 제13권2호
    • /
    • pp.47-68
    • /
    • 2003
  • Recent advances in the studies on the interaction between Asian monsoon and ENSO cycle are reviewed in this paper. Through the recent studies, the East Asian summer monsoon circulation system and the East Asian climate system have proposed. Moreover, different responses of the (winter and summer) monsoon circulation and summer rainfall anomalies in East Asia to ENSO cycle during its different stages have been understood further. Recently, the studies on the dynamical effect of East Asian monsoon on the thermal variability of the tropical western Pacific and ENSO cycle have been greatly advanced. These studies demonstrated further that ENSO cycle originates from the tropical western Pacific, and pointed out that the dynamical effect of East Asian winter and summer monsoons on ENSO cycle may be through the atmospheric circulation and zonal wind anomalies over the tropical western Pacific, which can excite the oceanic Kelvin wave and Rossby waves in the equatorial Pacific. Besides, the scientific problems in the interaction between Asian monsoon and ENSO cycle, which should be studied further in the near future, are also pointed out in this paper.

횡단류에 분사되는 액체 제트의 분무 및 연소 특성 (Spray and Combustion Characteristics of Liquid Jet in Cross Flow)

  • 이관형;김두만;구자예;황진석
    • 한국항공우주학회지
    • /
    • 제34권12호
    • /
    • pp.48-58
    • /
    • 2006
  • 횡단류에 분사되는 액체 제트의 분무 및 연소 특성에 대한 수치적 연구를 수행하였다. 수치 계산을 위해 3차원의 분무 및 화학반응 유동 해석에 유용한 KIVA 코드를 횡단류에서의 분무 해석에 적합하도록 수정하여 사용하였다. 액주의 분열과 리거먼트 및 액적의 분열 현상을 해석하기 위하여 wave 모델과 KH-RT hybrid 모델이 사용되었다. 침투길이는 유입공기의 속도가 감소하거나 분사속도가 증가함에 따라 증가하였다. 유입공기의 속도가 증가할수록 계산결과의 오차가 크게 발생함을 알 수 있었다. 연소 특성에 대한 수치 해석으로 연소실 내부의 화염전파 형상과 국부지역에서의 온도및 공해 배출량에 대한 결과를 얻었다.

Rankine 소오스 패널법을 이용한 소수선면 쌍동선의 조파저항계산 (Calculation of the Wave Resistance of SWATH Ships using Rankine Source Panel Methods)

  • 전호환;이명휘;주영렬;장학수
    • 대한조선학회논문집
    • /
    • 제34권2호
    • /
    • pp.27-38
    • /
    • 1997
  • 본 논문에서는 Rankine Source 분포법에 의해 SWATH선의 조파저항 계산을 시도하였다. 자유표변조건은 이중모형근사형(Dawson형)의 자유표면조건과 free stream에 의한 근사형(Kelvin형)을 사용하고, 각각의 경우에 유한 차분법이 아닌 해석적인 방법을 사용하여 수치해석을 하였다. 위 두 가지 패널방법에 의한 수치계산결과, 얇은배 이론과 수정 세장체이론에 의한 계산결과 및 시험 탠값과의 비교를 통하여 각 방법의 특성을 논하였다. 저항실험은 단독형 스트러스와 탠덤값(tendem) 스트러트 SWATH선에 대해서 하였으며, 두 선체간의 거리변화에 따른 결과도 포함시켰다. 개발된 프로그램의 검증을 위해서 Wigley 단독선형 및 쌍동선형에 대해서 계산을 수행하여 발표된 시험결과와 비교하였다. Wigley 단독선형, 쌍동선형 및 SWATH 선형에 대해서 계산한 조파저항 값과 시험값, 관측한 파형과 계산한 파형을 비교하였다.

  • PDF

An Analytical Model with Three Sub-Regions for $M_2$ Tide in the Yellow Sea and the East China Sea

  • Jung, Kyung-Tae;Park, Chang-Wook;Oh, Im-Sang;So, Jae-Kwi
    • Ocean Science Journal
    • /
    • 제40권4호
    • /
    • pp.191-200
    • /
    • 2005
  • In this study an analytical tide model of uniform width with three sub-regions is presented. The three-subregions model takes into account step-like variations in depths in the direction of the channel as a way to examine the $M_2$ tide of the East China Sea (ECS) as well as the Yellow Sea (YS). A modified Proudman radiation condition has been applied at the northern open head, while the sea surface elevation is specified at the southern open boundary. It is seen that, due to the presence of an abrupt change in depth, co-amplitude lines of the $M_2$ tide are splitted to the east and west near the end of the ECS shelf region. Variations in depths, bottom friction and the open head boundary conditions all contribute to the determination of formation of amphidromes as well as overall patterns of $M_2$ tidal distribution. It is seen that increasing water depth and bottom friction in the ECS shelf results in the westward shift of the southern amphidrome. There is however no hint at all of the well-known degenerated tidal pattern being formed. It is inferred that a lateral variation of water depth has to be somehow incorporated to represent the tidal patterns in ECS in a realistic manner. Regarding the radiation factor introduced by Fang et al. (1991), use of a value larger than one, possibly with a phase shift, appears to be a proper way of incorporating the reflected waves from the northern Yellow Sea (NYS).

Global Coupled 모델 2와 3.1의 MJO 모의성능 평가 (Assessment of MJO Simulation with Global Coupled Model 2 and 3.1)

  • 문자연;김기영;조정아;양영민;현유경;김백조
    • 대기
    • /
    • 제32권3호
    • /
    • pp.235-246
    • /
    • 2022
  • A large number of MJO skill metrics and process-oriented MJO simulation metrics have been developed by previous studies including the MJO Working Group and Task Force. To assess models' successes and shortcomings in the MJO simulation, a standardized set of diagnostics with the additional set of dynamics-oriented diagnostics are applied. The Global Coupled (GC) model developed for the operation of the climate prediction system is used with the comparison between the GC2 and GC3.1. Two GC models successfully capture three-dimensional dynamic and thermodynamic structure as well as coherent eastward propagation from the reference regions of the Indian Ocean and the western Pacific. The low-level moisture convergence (LLMC) ahead of the MJO deep convection, the low-level westerly and easterly associated with the coupled Rossby-Kelvin wave and the upper-level divergence are simulated successfully. The GC3.1 model simulates a better three-dimensional structure of MJO and thus reproduces more realistic eastward propagation. In GC2, the MJO convection following the LLMC near and east of the Maritime Continent is much weaker than observation and has an asymmetric distribution of both low and upper-level circulation anomalies. The common shortcomings of GC2 and GC3.1 are revealed in the shorter MJO periods and relatively weak LLMC as well as convective activity over the western Indian Ocean.