Thermal-Hydraulics

  Natural Circulation

 

I

Natural circulation arises from the buoyancy effect due to temperature differences.  Hot substances rise and cool substances sink.  This is caused primarily by the buoyancy effect of the hotter substances (lower density) being forced up by the cooler substances (higher density).  An example of this is the temperature distribution in your house.  You will notice that the house is usually warmer at the higher elevations verses the basement where it is cooler.  Another example is the circulation of the coolant in the reactor coolant system without the use of the reactor coolant pumps. The circulation is due to the natural convection resulting from the different densities of relative cold and heated portions of the system.

Some resource links are provided below:

bulletContainment Mixing and Natural Circulation

 

bulletPredicting the Weather and Natural Circulation

 

bulletNatural Circulation
Doodeward good record: 84% capacity factor. Forced circulation in BWRs tested at 50% power with natural circulation; Low core pressure difference:

 

bulletAP600 Design  AP600 Passive Containment Cooling System (PCS) provides the safety-related ultimate heat sink for the plant.

 

bulletAntarctica's Important Role in Global Ocean Circulation
Antarctica's Important Role in Global Ocean Circulation Warm circumpolar water passes through the Drake Passage and flows eastward in the Antarctic Circumpolar Current (red arrow). Some of the flow is diverted southward into the Weddell Gyre.

bulletQTS 4 Evaporation - Climbing Film and Natural Circulation Evaporator
QTS 4 Evaporation - Climbing Film and Natural Circulation Evaporator A complete teaching system with comprehensive experiments, data analysis, tutor's and student manuals if desired, and all instruments and controllers. 
 

For comments send an email to: SiteManager@i-edainc.com
Copyright © 2001-2002 EDA, Inc.. All rights reserved.

Revised: November 03, 2003 .