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Titlebook: Advances in Two-Phase Flow and Heat Transfer; Fundamentals and App S. Kaka?,M. Ishii Book 1983 Springer Science+Business Media Dordrecht 19

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31#
發(fā)表于 2025-3-26 21:06:00 | 只看該作者
32#
發(fā)表于 2025-3-27 01:19:37 | 只看該作者
https://doi.org/10.1007/BFb0008607 liquid-solid mass transfer to the film flow phenomena. Surface wettability and film breakdown at various liquid rates, physical properties and surface inclinations are presented. Conditions for the formation of uniform films are established, and the transitions from a smooth film upstream to a dist
33#
發(fā)表于 2025-3-27 08:31:43 | 只看該作者
,The ‘Academic War’: A Case Study, data and prediction methods, notably for transition boiling, inverted annular film boiling and the minimum film boiling point. This paper reports on the more recent experimental and analytical post-CHF studies. An assessment of the available prediction methods is made and recommendation for use in
34#
發(fā)表于 2025-3-27 13:08:30 | 只看該作者
35#
發(fā)表于 2025-3-27 15:58:36 | 只看該作者
36#
發(fā)表于 2025-3-27 20:24:19 | 只看該作者
37#
發(fā)表于 2025-3-27 22:48:57 | 只看該作者
https://doi.org/10.1007/978-94-010-2220-0 for the vapour-phase. For their solution one has to know the fraction . of the total heat flux, which causes the evaporation of the liquid, and the fraction ., produced by the recondensation of the vapour-bubbles. In this paper it will be shown how it is possible to determine these two heat-flux fr
38#
發(fā)表于 2025-3-28 02:05:25 | 只看該作者
Jerzy Neyman,Elizabeth L. Scottured quantities. Therefore, in the first part, the advances are described which can be achieved by the use of single techniques only. Combinations of several methods are discussed next, and mass flow rate results are presented, which were obtained in different experimental facilities for steady-stat
39#
發(fā)表于 2025-3-28 08:29:23 | 只看該作者
40#
發(fā)表于 2025-3-28 11:17:22 | 只看該作者
Confronting Capitalism in the 21st Centuryces of the homogeneous diffusion model when coupled with the standard closure equation for shearing stress and the equation of state for water in the two-phase region. Two cases are analyzed: upward flow in which the gravity and shearing-stress vectors are codirectional, and downward flow when the t
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