Transitional regime takes place in case of absence of conditions for bubble, slug and annular-mist regimes. Integral method of steam-water flow description is used (two-velocities). Theoretical basis for calculation of flow parameters of transitional regime is developed. Criterions of this regime existence are determined.

Press the Back button in your browser, or search again.

Copyright 2000, Stanford Geothermal Program: Readers who download papers from this site should honor the copyright of the original authors and may not copy or distribute the work further without the permission of the original publisher.