1980
DOI: 10.13182/nse80-a18945
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A Nonequilibrium Vapor Production Model for Critical Flow

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Cited by 75 publications
(8 citation statements)
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“…Coincidentally, this value of N falls within the range of values for ordinary water (no precipitate particles) containing natural impurities (dust, etc. ), namely 10 to 10 /m (Richter 1981;Abdollahian et al 1982;Ardon 1978;and Rivard and Travis 1980). Some indication of the validity of equation (B-13) can be given by considering the Lipkis et al (1956) experimental study of boiling in a volumetrically-heated aqueous KOH solution pool.…”
Section: @-2)mentioning
confidence: 99%
“…Coincidentally, this value of N falls within the range of values for ordinary water (no precipitate particles) containing natural impurities (dust, etc. ), namely 10 to 10 /m (Richter 1981;Abdollahian et al 1982;Ardon 1978;and Rivard and Travis 1980). Some indication of the validity of equation (B-13) can be given by considering the Lipkis et al (1956) experimental study of boiling in a volumetrically-heated aqueous KOH solution pool.…”
Section: @-2)mentioning
confidence: 99%
“…1 Les auteurs qui choisissent r [11,14] considèrent qu'une bulle croît jusqu'à la taille critique où son fractionnement en deux bulles est dû à la turbulence du liquide. Le rayon maximum rmax, donné par un nombre de Weber critique, est 1.25 fois le rayon des 2 bulles résultantes ce qui incite les auteurs cités à prendre: (12) r < es où l'expression entre crochet est par définition le nombre de Jakob Ja.…”
Section: Solutions éLémentaîl'es R (A R)unclassified
“…Nonequilibrium mechanistic models based on the numerical solution of the two-fluid conservation equations represent an advanced group of two-phase critical flow models and can account for the integral flow effects on local flow properties at the critical cross section [7][8][9][10][11][12][13][14][15]. In these models the one-dimensional (I-D) phasic conservation equations are numerically solved for flow through a channel and by iteratively varying the channel discharge rate, the flow rate leading to the critical conditions at the channel throat, i.e., an infinitely large pressure gradient [10,12,IS]; a vanishing determinant of the coefficient matrix for the system of I-D, quasi-linear first-order differential equations representing the phasic conservation equations [11,13,16]; or a flow rate independent of downstream pressure [8,14] is specified.…”
Section: Introductionmentioning
confidence: 99%
“…In these models the one-dimensional (I-D) phasic conservation equations are numerically solved for flow through a channel and by iteratively varying the channel discharge rate, the flow rate leading to the critical conditions at the channel throat, i.e., an infinitely large pressure gradient [10,12,IS]; a vanishing determinant of the coefficient matrix for the system of I-D, quasi-linear first-order differential equations representing the phasic conservation equations [11,13,16]; or a flow rate independent of downstream pressure [8,14] is specified. The major difficulty, which also accounts for the disagreement among these models, is the treatment of the poorly understood bubble nucleation processes.…”
Section: Introductionmentioning
confidence: 99%
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