New approach for describing reactor and containment pressure change after loss of core cooling at Fukushima meltdown accident

Tsuyoshi Matsuoka
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Abstract

The purpose of this comment is to clarify the whole history of reactor and containment pressure change during the Fukushima meltdown accident. It is based on a new approach for film boiling, which is sustained after the Zr – H 2 O reaction. As the reaction rate is proportional to the reactor or containment vessel pressure under film boiling, it increases rapidly and stops abruptly while sustaining film boiling. The containment vessel pressure change consists of three phases, namely, pressurization, holding a high pressure and depressurization. The containment vessel is pressurized with H 2 gas and steam produced by the Zr – H 2 O reaction and depressurized by heat removal by heatsinks such as the containment vessel wall and inner concrete after the reaction stops. The high pressure between these pressure changes is sustained by balancing the amount of H 2 gas produced by the reaction and that of gas leaking from the gap of the top hat of the containment vessel. The amount of core decay heat is large, but the change of this is negligible. Thus, pressurization is calculated from the amounts of H 2 gas and steam produced by the Zr – H 2 O reaction. The amount removed by the heatsink balances with that produced by the reaction during the high-pressure phase. Depressurization occurs after the reac tion is over, so the reaction heat rate can be calculated from the heat removal rate of the heatsink, which is equal to the condensation rate during depressurization. The rate of gas leakage can be calcu lated from the reaction rate. It is very important that the reaction rate was slow owing to the insuffi cient steam supply, as the melted core in the Fukushima accident was covered with H 2 gas and steam at a pressure of 0.8 MPa or lower. This is different from the rate ( at approximately 7 MPa ) in the Three Mile Island accident, as the specific volume of steam at 0.8 MPa is ten times larger than that at 7 MPa. The calculation results based on this assumption show that almost all the Zr in each core of Units 1, 2 and 3 reacted with water. The location of a small penetration hole produced by the contact of the high-temperature H 2 gas with the suppression chamber wall, is estimated in Unit 2.
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描述福岛堆芯冷却失效后反应堆和安全壳压力变化的新方法
这个评论的目的是澄清整个历史的反应堆和安全壳压力变化在福岛事故。它是基于一种新的膜沸腾方法,这种方法是在Zr - h2o反应后持续的。在膜沸腾状态下,反应速率与反应器或容器压力成正比,在维持膜沸腾状态下,反应速率迅速增加,并突然停止。安全壳压力变化包括增压、保高压和降压三个阶段。安全壳由Zr - h2o反应产生的h2气体和蒸汽加压,反应停止后由诸如安全壳壁和内部混凝土等散热器散热减压。这些压力变化之间的高压是通过平衡反应产生的h2气体的量和从安全壳顶帽间隙泄漏的气体的量来维持的。堆芯衰变热的量很大,但其变化可以忽略不计。因此,压力是由Zr - h2o反应产生的h2气体和蒸汽的量来计算的。由散热器去除的量与高压阶段反应产生的量相平衡。减压是在反应结束后发生的,所以反应的热速率可以通过散热器的排热速率来计算,它等于减压过程中的冷凝速率。气体泄漏率可由反应速率计算出来。很重要的一点是,由于蒸汽供应不足,反应速度较慢,因为福岛事故中熔化的堆芯被压力为0.8 MPa或更低的h2气体和蒸汽覆盖。这与三里岛事故中的速率(约7兆帕)不同,因为0.8兆帕时的蒸汽比容是7兆帕时的十倍。基于这一假设的计算结果表明,1、2、3号机组各堆芯中Zr几乎全部与水发生反应。在单元2中估计了高温h2气体与抑制室壁接触产生的小穿透孔的位置。
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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来源期刊
Transactions of the Atomic Energy Society of Japan
Transactions of the Atomic Energy Society of Japan Energy-Nuclear Energy and Engineering
CiteScore
0.50
自引率
0.00%
发文量
16
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