Heat transfer characteristics of single-layer and two-layer corium pool in elliptical lower head

Y.P. Zhang , D.H. Zhu , K. Ge , Y.W. Wu , W.X. Tian , G.H. Su , S.Z. Qiu
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引用次数: 1

Abstract

In this study, we investigated the characteristics of natural convection heat transfer of single-layer and two-layer corium pool in the elliptical lower head by the numerical method. Numerical simulations were performed using FLUENT software with the WMLES (Wall-Modeled Large Eddy Simulation) turbulence model, solid-liquid phase change model and the VOF (Volume of Fluid) model. The heat transfer characteristics such as pool temperature field, flow velocity field and heat flux distribution were obtained. For the single-layer corium pool, different degrees of melting occurred on the wall surface from about 1712 mm arc length inside the inner wall to the liquid level. The transient velocity field of single-layer corium pool showed that the natural convection first occurs near the wall surface and then gradually forms in the center of the corium pool as the temperature rises. When the quasi-steady state is reached, the upper part of the pool forms strong turbulence, while the lower part has lower velocity and forms transverse flow. For the two-layer corium pool, the lower head wall is more severely melted than the single-layer configuration. Whereas, the crust at the wall near the stratified interface is only slightly melted due to the lower flow rate and weaker heat transfer capacity. The research revealed the flow and heat transfer mechanisms of corium pool, and provided reference for the technology design, system optimization and safety evaluation of the IVR (In-Vessel Retention) – ERVC (External Reactor Vessel Cooling) severe accident mitigation strategy for the large-scale advanced pressurized water reactor.

椭圆下封头单层和双层堆芯池的换热特性
本文采用数值方法研究了椭圆下封头内单层和双层堆芯熔池的自然对流换热特性。采用FLUENT软件对WMLES (wall - modelling Large Eddy Simulation)湍流模型、固液相变模型和VOF (Volume of Fluid)模型进行数值模拟。得到了池温场、流速场和热流密度分布等换热特性。对于单层堆芯熔池,从内壁约1712 mm弧长到液面,其壁面发生了不同程度的熔化。单层堆芯熔池的瞬态速度场表明,随着温度的升高,堆芯熔池壁面附近首先发生自然对流,然后在堆芯熔池中心逐渐形成自然对流。当达到准稳态时,池的上部形成强烈的湍流,而下部流速较低,形成横向流动。对于双层堆芯池,较低的头壁比单层结构的熔化更严重。而靠近分层界面的壁面处,由于流速较低,换热能力较弱,地壳仅发生轻微熔化。研究揭示了堆芯熔池的流动和传热机理,为大型先进压水堆的IVR (In-Vessel Retention) - ERVC (External Reactor Vessel Cooling)严重事故缓解策略的技术设计、系统优化和安全性评估提供了参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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