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AbstractAbstract
[en] Experimental investigation results of iron oxide deposit effect on crytical heat flux are presented at water motion in an annular channel. Experiments were carried out at the pressure of 7 MPa, mass speed of 1250-5000 kg/(m2xc) and relative enthalpy change in the crisis place from -0.2 to +0.15. It is established that crytical heat flux on the surface with deposits is lower than on the pure surface
Original Title
Vliyanie zhelezookisnykh otlozhenij na krizis teplootdachi pri kipenii vody
Primary Subject
Source
For English translation see the journal Therm. Eng.
Record Type
Journal Article
Journal
Teploehnergetika; (no.6); p. 14-16
Country of publication
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