用kupol-m程序计算考虑氢绝热等时完全燃烧的核电厂安全壳内气体参数

Y. Kryglikov, O. Supotnitskaya, L. Yantseva
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引用次数: 0

摘要

氢安全分析的一个重要因素是考虑可能发生的氢燃烧对核电站安全壳气氛参数的影响。为了评价这种影响,建立了氢的绝热等时完全燃烧(AICC)模型,并在KUPOL-M安全壳规范中实现。由于KUPOL-M规范中包含了氢的绝热等时完全燃烧模型,该规范将适用于VVER核电站的安全性分析,目的是估计氢燃烧情况下安全壳可能承受的热机械负荷。这个模型简单、保守,基于质量和能量守恒定律。对氢的绝热等时完全燃烧模型作如下假设:燃烧的体积是恒定的;没有热传递;限制成分(在大多数情况下是氢)完全燃烧;不考虑化学转变的中间阶段。文中给出了该模型在实验数据上的检验结果。在较宽的混合气体氢浓度范围内,计算结果与实验结果吻合较好。试验结果表明,在KUPOL-M代码中实现AICC模型可以在不显著增加计算时间的情况下保守地评估密闭气氛中的参数。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
CALCULATION OF GAS PARAMETERS IN A NPP CONTAINMENT TAKING INTO ACCOUNT THE ADIABATIC ISOCHORIC COMPLETE COMBUSTION OF HYDROGEN BY THE KUPOL-M CODE
An important factor for the analysis of hydrogen safety is to take into account the effect of possible hydrogen combustion on the parameters of NPP containment atmosphere. In order to evaluate this effect a model of adiabatic isochoric complete combustion (AICC) of hydrogen was developed and implemented in the KUPOL-M containment code. With the model of adiabatic isochoric complete combustion of hydrogen included in the KUPOL-M code, this code will become applicable for the VVER NPP safety analysis performed with the aim to estimate possible thermal mechanical loads on the containment in case of hydrogen burning. This model is simple, conservative and based on the laws of conservation of mass and energy. The following assumptions are made in the model of adiabatic isochoric complete combustion of hydrogen: the volume in which burning takes place is constant; there is no heat transfer; the limiting component (in most cases it is hydrogen) burns down completely; intermediate stages of chemical transformations are not considered. The test results of this model on experimental data are presented in the article. There is a good agreement between the data of calculations and experiments in a wide range of hydrogen concentrations in gas mixtures. Based on the test results it can be concluded that implementation of AICC model in the KUPOL-M code allows conservatively evaluating the parameters in the containment atmosphere without significantly increasing the calculation time.
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