海水对内加热环空不沸腾换热的影响

Shin-ichiro Uesawa, Wei Liu, Lifang Jiao, T. Nagatake, K. Takase, Mitsuhiko Shibata, H. Yoshida
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引用次数: 4

摘要

在东京电力公司福岛第一核电站的事故中,海水被注入反应堆。然而,海水对燃料棒和燃料碎片冷却性能的影响尚不清楚。作为可能的影响,冷却剂物理性质的变化和海盐在传热表面和冷却剂中的沉积被考虑在内。我们使用内部加热环空进行了热水力实验,以确定海水在不沸腾条件下的影响。为了与人工海水进行比较,还对水和氯化钠溶液进行了相同的实验。在实验中,考虑到人工海水的物理性质,利用Dittus-Boelter对比估算了强制对流条件下(Re > 2300[-])人工海水的热-水力行为,尽管海水中存在海盐沉积。粒子图像测速(PIV)结果表明,人工海水中的速度分布与水中和NaCl溶液中的速度分布没有明显差异。在混合对流条件下,人工海水的Nusselt数由Grasholf数、Reynolds数和Prandtl数以及水和NaCl溶液的Nusselt数的相关性得到。因此,考虑到人工海水的物理性质,可以通过传统的单相流热-水力关系式来估计海水在单相流中的热-水力行为。
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Effect of Seawater on Heat Transfer without Boiling in Internally Heated Annulus
Seawater was injected into the reactors during the accident at TEPCO’s Fukushima Daiichi NPS. However, the effects of the seawater on the cooling performance of the fuel rods and fuel debris are not clear. As possible effects, the change in the physical properties of the coolant and the sea salt de-position on a heat transfer surface and in the coolant are considered. We conducted thermal-hydraulic experiments using an internally heated annulus to determine the effects of seawater under conditions without boiling. The same experiments for water and sodium chloride ( NaCl ) solution were also conducted for the purpose of comparison with the artificial seawater. In these experiments, considering the physical properties of the artificial seawater, the thermal-hydraulic behaviors of the artificial seawater under forced convection ( Re > 2300 [-]) was estimated from the Dittus-Boelter correlation although sea salt was deposited in the fluid. According to the results of particle image velocimetry ( PIV ) , the velocity distribution in the artificial seawater was NOT different from that in the water and the NaCl solution. For a mixed convection regime, the Nusselt number of the artificial seawater was obtained from the correlation of the Grasholf number, Reynolds number and Prandtl number, as well as those for the water and the NaCl solution. Therefore, considering the physical properties of the artificial seawater, the thermal-hydraulic behavior of the seawater in single-phase flow can be estimated from the conventional thermal-hydraulic correlations for a single-phase flow.
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