Mixing and Stratification Phenomena Under Natural Convection in the Multi-Openings Compartment

Jinghua Jiang, Ying Li, Tianlin Wang, L. Tong, Xuewu Cao
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Abstract

The mixing and stratification of hydrogen-vapor-air in the compartment is extensively studied under inertia jets and turbulent buoyant jets. The characteristics of buoyancy-driven flows during fission and fusion reactor accidents need to be further studied to provide a benchmark for the validation of computational procedures. In this paper, a large-scale facility of a vessel with multiple openings is established to study the mixing and stratification of the mixture driven by buoyancy under natural convection. The test is carried out with well-controlled boundary conditions, in which, a mixture of helium and vapor with a volume fraction of 1:10 is injected in the compartment filled with air. As the injection begins, the gas mixture is driven by the injection source and the buoyancy of the light gas. The gas is released through the top and bottom openings with the flow velocity of 5 m/s and 7.5 m/s, respectively. When the injection is stopped at 4600s, the density gradient induces the natural convection, air enters the vessel through the bottom opening with a relatively low velocity, and the low-density mixture is discharged through the top opening at the same time. During this period, the velocity of the mixture at the opening decreases due to the reduction of the drive force of natural convection.
多开口舱室自然对流下的混合和分层现象
在惯性射流和湍流浮力射流作用下,对舱内氢气-蒸汽-空气的混合和分层进行了广泛的研究。需要进一步研究裂变和聚变反应堆事故中浮力驱动流动的特性,为计算程序的验证提供基准。本文建立了大型多开口容器装置,研究了自然对流条件下浮力驱动下的混合和分层过程。试验在控制良好的边界条件下进行,在边界条件下,将体积分数为1:10的氦气和蒸汽的混合物注入充满空气的隔间中。当喷射开始时,气体混合物由喷射源和轻气体的浮力驱动。气体从顶部开口和底部开口分别以5 m/s和7.5 m/s的流速释放。在4600s停止喷射时,密度梯度诱导自然对流,空气以较低的速度从底部开口进入容器,同时低密度混合物从顶部开口排出。在此期间,由于自然对流的驱动力减少,混合物在开口处的速度降低。
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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