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Modeling for Evaluation of Debris Coolability in Lower Plenum of Reactor Pressure Vessel

机译:反应堆压力容器下部夹杂物冷却性评估模型

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摘要

Effectiveness of debris cooling by water that fills a gap between the debris and the lower head wall was estimated through steady calculations in reactor scale. In those calculations, the maximum coolable debris depth was assessed as a function of gap width with combination of correlations for critical heat flux and turbulent natural convection of a volumetrically heated pool. The results indicated that the gap with a width of 1 to 2 mm was capable of cooling the debris under the conditions of the TMI-2 accident, and that a significantly larger gap width was needed to retain a larger amount of debris within the lower plenum. Transient models on gap growth and water penetration into the gap were developed and incorporated into CAMP code along with turbulent natural convection model developed by Yin, Nagano and Tsuji, categorized in low Reynolds number type two-equation model. The validation of the turbulent model was made with the UCLA experiment on natural convection of a volumetrically heated pool. It was confirmed that CAMP code predicted well the distribution of local heat transfer coefficients along the vessel inner surface. The gap cooling model was validated by analyzing the in-vessel debris coolability experiments at JAERI, where molten Al_2O_3 was poured into a water-filled hemispherical vessel. The temperature history measured on the vessel outer surface was satisfactorily reproduced by CAMP code.
机译:通过对反应堆规模进行稳定计算,估算了填充残渣和下端盖壁之间间隙的水进行残渣冷却的有效性。在这些计算中,将最大可冷却碎片深度评估为间隙宽度的函数,并结合了体积加热池的临界热通量和湍流自然对流的相关性。结果表明,在TMI-2事故条件下,宽度为1到2毫米的间隙能够冷却碎屑,并且需要较大的间隙宽度以在下气室中保留更多的碎屑。 。开发了关于间隙增长和水渗透到间隙中的瞬态模型,并将其与阴,长野和Tsuji开发的湍流自然对流模型一起纳入了CAMP代码中,归类于低雷诺数类型的两方程模型。湍流模型的验证是通过对容积加热池的自然对流进行的UCLA实验进行的。证实了CAMP代码很好地预测了沿容器内表面的局部传热系数的分布。通过分析JAERI的船内碎屑可冷却性实验验证了间隙冷却模型,其中将熔融的Al_2O_3倒入充满水的半球形容器中。通过CAMP代码令人满意地再现了在容器外表面上测得的温度历史。

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