Natural Convection - horizontal cylinder

MET In summary, the Churchill/Thelen correlation is commonly used for the Nusselt number in the range of natural convection. However, there are concerns about the characteristic length and Nuo value. Alternative correlations, such as those developed by Churchill and Chu and by Gebhart and Pera, have been proposed for the Grasshof range of 0.01<Gr<50 and air (Pr=0.7), taking into account the aspect ratio and orientation of the heated surface. Further clarification on the characteristic length and Nuo value may be needed for more accurate results.
  • #1
MET
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Nusselt number:

1) The only correlation I could find so far is the one described here http://en.wikipedia.org/wiki/Natural_convection which seems to be from Churchill/Thelen. There seem however to exist some questions regarding the characteristic length and the value to use for Nuo (see discussion). Could someone here may be clarify these points?

2) Does someone know of an alternative correlation which could be used instead of the one from Chruchill/Thelen for the Grasshof range 0.01<Gr<50 and air (Pr=0.7)?

3) Does someone know of such a correlation which considers also the length to diameter ratio of the cylinder?

Thanks in advance.

Regrads MET
 
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  • #2


Dear MET,

Thank you for bringing up these questions regarding the Nusselt number correlation for natural convection. The Churchill/Thelen correlation is commonly used in this range, but as you mentioned, there are some concerns about the characteristic length and Nuo value.

To clarify, the characteristic length in this correlation is typically taken as the diameter of the cylinder or the length of the heated surface. However, some researchers have suggested using the height of the cylinder or the average of the diameter and height as the characteristic length. The Nuo value, which is the Nusselt number at the onset of natural convection, has been found to vary depending on the geometry of the cylinder and the orientation of the heated surface.

In terms of alternative correlations for the Grasshof range of 0.01<Gr<50 and air (Pr=0.7), there are a few options that have been proposed. One is the correlation developed by Churchill and Chu, which takes into account the aspect ratio of the cylinder. Another is the correlation by Gebhart and Pera, which includes the aspect ratio and also considers the orientation of the heated surface.

I hope this information helps and provides some alternatives for your research. If you have any further questions, please don't hesitate to ask.


 

FAQ: Natural Convection - horizontal cylinder

What is natural convection?

Natural convection is a type of heat transfer that occurs due to the density differences caused by temperature variations in a fluid. When a fluid is heated, it becomes less dense and rises, while cooler fluid sinks. This creates a circular motion known as convection currents.

What is a horizontal cylinder?

A horizontal cylinder is a three-dimensional shape that has a circular cross-section and a constant diameter along its entire length. It is oriented horizontally, meaning that its length is perpendicular to the force of gravity.

How does natural convection affect a horizontal cylinder?

Natural convection affects a horizontal cylinder by causing heat transfer between the cylinder and the surrounding fluid. As the cylinder is heated, the fluid near its surface becomes less dense and rises, carrying heat away from the cylinder. This creates a cooling effect on the cylinder, which can be beneficial in some applications.

What factors influence the rate of natural convection on a horizontal cylinder?

The rate of natural convection on a horizontal cylinder is influenced by several factors, including the temperature difference between the cylinder and the surrounding fluid, the fluid properties (such as viscosity and thermal conductivity), and the size and shape of the cylinder.

How is natural convection on a horizontal cylinder different from other types of heat transfer?

Natural convection on a horizontal cylinder differs from other types of heat transfer, such as conduction and forced convection, in that it does not require an external force or a temperature gradient to occur. It is driven solely by the density differences created by temperature variations in the fluid.

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