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Cryogenic boiling and two-phase chilldown process under terrestrial and microgravity conditions.

机译:在地面和微重力条件下的低温沸腾和两相冷却过程。

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摘要

Chilldown or quenching is a complicated process that initiates the cryogenic fluids transport, and it involves unsteady two-phase heat and mass transfer. To advance understanding of this process, we conducted both experimental and modeling investigations.;An experimental apparatus was designed and fabricated to investigate the cryogenic chilldown process under both 1-g and microgravity conditions. Liquid nitrogen was used as the working fluid. We found that the chilldown process can be generally divided into three regions: film boiling region, transition boiling region and nucleate boiling region, and each region is associated with a different flow regime and heat transfer mechanism.;Under low flow conditions, we observed that the two-phase flow regime is dispersed flow in the film boiling region. The dispersed liquid phase is in the form of long filaments as the tube is chilled down, and the vapor phase is generally superheated. Statistic feature of the liquid filaments was studied and a phenomenological model, in which the heat transfer at the bottom is considered as a sum of vapor and liquid components, was developed.;Microgravity tests were conducted for chilldown in the film boiling region. Bottom wall heat flux was found to decrease under microgravity condition. Under current experimental conditions, the gravity effect does not show a strong dependence on wall temperature and inlet flow rate.;A cryogenic chilldown model was also developed. The model focuses on both vertical tube chilldown and microgravity chilldown. In this model, the chilldown process is characterized as four distinct regions, which are fully vapor region, dispersed flow film boiling region, inverted annular film boiling region, and nucleate boiling region. Two-fluid equations were applied to the dispersed flow film boiling region and the inverted annular film boiling region, while the fully vapor region and nucleate boiling region are depicted by single-phase correlations. The model results show a good agreement with previous experimental data.
机译:急冷或急冷是引发低温流体传输的复杂过程,涉及不稳定的两相传热和传质。为了进一步了解这一过程,我们进行了实验和模型研究。;设计并制造了一种实验装置,以研究1-g和微重力条件下的低温冷却过程。液氮用作工作流体。我们发现冷却过程通常可分为三个区域:薄膜沸腾区域,过渡沸腾区域和核沸腾区域,每个区域都具有不同的流态和传热机制。在低流量条件下,我们观察到两相流态是在膜沸腾区域中的分散流。随着管的冷却,分散的液相呈长丝状,气相通常会过热。研究了液体长丝的统计特性,建立了以底部传热为蒸气和液体总和的现象学模型。进行了微重力试验,研究了薄膜沸腾区的冷却过程。发现底壁热通量在微重力条件下降低。在当前的实验条件下,重力效应对壁温和入口流速没有显着依赖性。;还建立了低温冷却模型。该模型着重于垂直管冷却和微重力冷却。在该模型中,冷却过程的特征是四个不同的区域,分别是完全蒸气区域,分散流膜沸腾区域,倒置环形膜沸腾区域和成核沸腾区域。将二流体方程式应用于分散流膜沸腾区域和倒置环形膜沸腾区域,而全蒸汽区域和成核沸腾区域则通过单相相关来描述。模型结果与以前的实验数据吻合良好。

著录项

  • 作者

    Yuan, Kun.;

  • 作者单位

    University of Florida.;

  • 授予单位 University of Florida.;
  • 学科 Engineering Mechanical.
  • 学位 Ph.D.
  • 年度 2006
  • 页码 179 p.
  • 总页数 179
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 机械、仪表工业;
  • 关键词

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