1. Definition of Free Convection Terms 549
IVc
.
. Free Convection
Free or natural convection is that mode of heat transfer where fluid flows only due
to the presence of buoyancy forces. This in turn is the result of the action of body
forces, most notably gravity, in the presence of density gradient, generally due to a
temperature gradient. Although the rate of heat transfer by free convection is gen-
erally smaller than that of forced convection, the most notable advantage associ-
ated with free convection is in its passive nature, which in turn increases system
reliability. Since the lower rate of heat transfer results in higher thermal resis-
tance, making the application of this mode of heat transfer essential in enhancing
insulation. Free convection in flow loops results in the circulation of the working
fluid, referred to as natural circulation, which plays a major role in nuclear plants
during shutdown. Free convection does not always lead to natural circulation as
the latter requires the heat source to be located at a lower elevation than the heat
sink. Even in such case, the buoyancy force must be sufficient to overcome the
friction force caused by the fluid shear stresses. As shown in Section 2 of this
chapter, the interesting feature of free convection heat transfer is the fact that the
thermal and the hydrodynamic aspects are intertwined.
1. Definition of Free Convection Terms
Volumetric expansion coefficient (
β
) for a fluid, as defined in Chapter II, is
the change of fluid volume with temperature at constant pressure. The volumetric
expansion coefficient is given by
β
= (∂V/∂T)
P
/V and has units of inverse tem-
perature. We may approximately express the volumetric expansion coefficient as:
≅ [(V
1
− V
2
)/(T
1
− T
2
)]/V
1
= [(
ρ
1
−
ρ
2
)/(T
1
− T
2
)]/
ρ
1
. For ideal gases,
β
= 1/T
where T is the gas absolute temperature in degrees K or R.
Characteristic length is the length over which free convection is established.
For vertical flat plates and cylinders, this is the height of the plate. For horizontal
cylinders and sphere, this is the diameter. Finally, for horizontal plates, L = A
s
/P
where A
s
and P are the plate surface area and perimeter, respectively.
Grashof number, after Franz Grashof, is a measure of buoyancy as compared
with the viscous forces in the hydrodynamic boundary layer. Due to the appear-
ance of the buoyancy forces, the Grashof number plays an important role in heat
transfer by free convection. For flow of fluid over a plate, the Grashof number is:
Gr = g
β
(T
s
– T
f
)x
3
/v
2
The Gr number is used to determine relative importance of the modes of heat
transfer by convection. If Gr << Re
2
, then the forced convection mode is domi-
nant. For Gr >> Re
2
, the free convection mode is dominant.
Mixed Convection is that mode of convection heat transfer for which Gr
≈ Re
2
.