Published March 1978 | Version v1
Journal article

To the elementary theory of critical (maximum) flow rate of two-phase mixture in channels with various sections

  • 1. Moskovskij Gosudarstvennyj Univ. (USSR)

Description

On the basis of the concepts of two-phase dispersive flow with various structures (bubble, vapour-drop etc) in the framework of the two-speed and two-temperature one-dimension stationary model of the current with provision for phase transitions the conditions, under which a critical (maximum) flow rate of two-phase mixture is achieved during its outflowing from a channel with the pre-set geometry, have been determined. It is shown, that for the choosen set of two-phase flow equations with the known parameters of deceleration and structure one of the critical conditions is satisfied: either solution of the set of equations corresponding a critical flow rate is a special one, i.e. passes through a special point locating between minimum and outlet channel sections where the carrying phase velocity approaches the value of decelerated sound speed in the mixture or the determinator of the initial set of equations equals zero for the outlet channel sections, i.e. gradients of the main flow parameters tend to +-infinity in this section, and carrying phase velocity also approaches the value of the decelerated sound velocity in the mixture

Additional details

Additional titles

Original title (Russian)
К элементарной теории критического (максимального) расхода двухфазной смеси в каналах переменного сечения

Publishing Information

Journal Title
Teplofiz. Vys. Temp.
Journal Volume
16
Journal Issue
2
Series
Teplofiz. Vys. Temp.
Journal Page Range
370-376

INIS

Country of Publication
USSR
Country of Input or Organization
USSR
INIS RN
9414755
Subject category
S42: ENGINEERING;
Descriptors DEI
ANALYTICAL SOLUTION; FLOW MODELS; FLOW RATE; NOZZLES; SPATIAL DISTRIBUTION; TWO-PHASE FLOW
Descriptors DEC
DISTRIBUTION; FLUID FLOW; MATHEMATICAL MODELS

Optional Information

Notes
For English translation see the journal High Temp.