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CORE MELT SOLIDIFICATION CHARACTERISTICS IN RPV LOWER HEAD- EXPERIMENTAL RESULTS FROM LIVE-TESTS

机译:实时测试的RPV较低头颅实验结果中的核心熔体凝固特征

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Core melt solidification phenomena during external reactor vessel cooling is investigated in LIVE tests with different external cooling conditions and melt pouring positions. A non-eutectic simulant melt (80-20 mole% KNO_3-NaNO_3) is used in the LIVE tests. It is found out that when the vessel is cooled with water at the beginning of the melt pouring, the cooling is more effective than in the case of delayed water cooling condition, in which the vessel is first cooled with air and then flooded by water. The initial water cooling leads to a faster growth of crust layer, lower crust thermal conductivity and thinner crust layer than those under the delayed water cooling condition. The initial water cooling leads also to higher heat flux through the vessel wall during the steady state and shorter crust growth period in comparison with the delayed water cooling condition. The solidification of the melt is probably under supercooling condition. The pouring position near the vessel wall results in considerable asymmetric heat flux distribution at one latitude. The heat flux at the position of melt pouring is higher than the one at other locations.
机译:在带不同外部冷却条件和熔体浇注位置的LIVE测试中研究了外部反应堆容器冷却期间的堆芯熔体凝固现象。 LIVE测试中使用非共晶模拟熔体(80-20摩尔%KNO_3-NaNO_3)。已经发现,当在熔体浇注开始时用水冷却容器时,冷却比延迟水冷却条件更有效,在延迟水冷却条件下,首先用空气冷却容器,然后用水淹没。初始水冷比延迟水冷条件下的结冰层生长更快,结皮热导率较低,结壳层更薄。与延迟的水冷条件相比,初始水冷还导致稳态期间通过容器壁的热通量更高,并且结壳生长时间更短。熔体的凝固可能是在过冷条件下进行的。靠近容器壁的倾倒位置导致在一个纬度上相当大的不对称热通量分布。熔体浇注位置的热通量高于其他位置的热通量。

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