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10
Flow with Heat Transfer
Introduction
Most of the previous chapters in this book have been devoted to a discussion of ows in
which the effects of viscosity could be neglected over most of the ow eld and to ows that
could be assumed to be adiabatic. However, the effects of viscosity and heat transfer can
be of dominant importance in some ow situations. In this chapter, consideration will be
given to some illustrative situations involving compressible ows in which heat transfer has
a signicant effect. This heat transfer to the ow may be the result of heat transfer from the
walls over which the uid is owing or it may be the result of chemical reactions in the ow.
This chapter is basically broken down into three sections. The rst section is predomi-
nantly concerned with external ows, i.e., ows over the surface of a body, and deals with
so-called aerodynamic heating and with the factors that affect the heat transfer rate in
such situations. Only a brief introduction to the topic is given. The second section is con-
cerned with heat transfer effects in internal ows of the type dealt with in the previous
chapter except that here the ows considered are not adiabatic. The third section deals
very briey with two types of shock wave in which heat generation or release plays a very
important role.
Aerodynamic Heating
When a gas ows over a surface, the gas in contact with the surface is brought to rest as
a result of viscosity. A rise in temperature is associated with this decrease in velocity at a
surface. If the gas velocity over the surface is high, this temperature rise, associated with the
slowing of the ow near a surface, can become quite large. This, basically, is what is referred
to as the “aerodynamic heating” of a surface. The phenomena is illustrated in Figure 10.1.
The velocity is zero at the surface because of the action of viscosity, and the temperature
rise across the boundary layer is the result of the work done on the ow by the viscous
forces, i.e., the temperature rise is produced by the dissipation of kinetic energy into heat
as the result of the work done by the viscous forces. The temperature rise, i.e., the aerody-
namic heating, is therefore said to be the result of “viscous dissipation.”
Aerodynamic heating is particularly important in hypersonic ows. However, in such
ows, as will be discussed in Chapter 12, changes in the specic heats and the chemi-
cal nature of the gas can occur due to the very high temperatures arising in such ows.
Further, because the temperature rises that occur at the surface are so high in hypersonic