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A Volumetric Approach to Natural Convection |
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Introduction
Natural convection was widely used a couple of decades ago.
Nowadays it is different. The heat densities are often so high
that fan cooling must be used. There are nevertheless still
several applications for which natural convection is the best
choice, mainly because it is simple and safe.
The subject has been treated before in this magazine. There are
also several other web publications about it, so there is no
lack of information. Here are some references:
Estimating Natural Convection Heat Transfer for Arrays of
Vertical Parallel Flat Plates
Heat Sinks in
Natural Convection: Optimum Fin Spacing
Natural convection modelling of heat sinks
using web-based tools
The purpose of this article is not to repeat the content of
those excellent publications. It is to deal with a concept
that probably is new to most readers: the volumetric efficiency
for natural convection. The background needed will also be
rapidly scanned.
Conventional heat transfer theory is based on defining a heat
transfer coefficient that operates on surfaces. This approach
is always correct and it has also been considerably refined
over the years. There are however cases when it does not
really provide a good overview. Natural convection is one
example. It can then be an advantage to use a more volume
oriented approach.
Figure 1
Typical velocity profiles.
Some basics
Figure 1 shows some typical velocity profiles for natural
convection. There are clearly two distinct cases. One in which
the velocity profile does not interact with any nearby surface
and one in which this is indeed the case. All heat transfer
correlations for natural convection between parallel plates
are based on this observation and they can all simply be said
to map a weighted average between these two extremes.
Figure 2
Typical heat transfer coefficient.
A typical case is shown in Figure 2. The heat transfer
coefficient increases sharply with the spacing when it is
small but it then levels out and approaches the one for
single plates. The slope of a straight line drawn from any
point on that curve to the origin is a measure of the heat
transfer coefficient per spacing unit. The optimum spacing is
found where this line has its maximum slope. If a given volume
is filled with heated plates this is also the spacing for
which the dissipated heat has its maximum value.
Figure 3
Some basic equations put in an applied format.
|
Air temp [C]
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Kl
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Kq
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Kt
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Ks
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Kv
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-20
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1.51
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1.39
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1.73
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0.0226
|
116
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-10
|
1.50
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1.38
|
1.69
|
0.0236
|
109
|
|
0
|
1.48
|
1.37
|
1.65
|
0.0247
|
104
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10
|
1.47
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1.36
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1.61
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0.0257
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98.5
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20
|
1.46
|
1.35
|
1.58
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0.0268
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93.9
|
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30
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1.44
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1.34
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1.54
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0.0279
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89.3
|
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40
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1.43
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1.33
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1.51
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0.0290
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85.2
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50
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1.42
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1.32
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1.48
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0.0301
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81.5
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60
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1.41
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1.32
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1.45
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0.0311
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78.0
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