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HEATING
PRINCIPLES
The
transfer of heat from a warm object to a cooler one takes place by one of
three methods or a combination thereof. These methods are: conduction,
convection or radiation.
CONDUCTION
Conduction of heat occurs when faster moving molecules pass on some of their
energy to adjacent molecules which are slower-moving, i.e. at a lower
temperature. This may occur within a solid or between a solid and an
adjacent fluid such as air. In any heated building or enclosure, heat is
conducted or transmitted from the warm inside air to the inside surfaces,
then through the wall or roof, to the cooler outside surface and on to the
outside air.
CONVECTION
Convection transfer of heat involves the mixing of warm and cool particles
of fluid. The mixing may come as a result of density differences due to
temperature differences which is natural convection, or, if the mixing is
produced by mechanical means, forced convection.
In a heated building, convection losses occur when cold outside air enters a
building, mixes with the warmer inside air, and then exits through an
exhauster or through doors, cracks, etc.
RADIATION
Heat transfer by radiation differs from the transfer of heat by conduction
or convection in that it does not need matter to accomplish the transfer.
Radiated heat is usually termed infra-red. This is just one of the several
forms of radiation. Infra-red is transmitted at the speed of light, 186,000
miles per second, in a straight line with minimal loss to the air. It can
be aimed, reflected or focused by materials that have a highly reflective
surface, bright aluminum, for example. When infra-red strikes an absorptive
object such as concrete, wood, water, paint, skin or clothing it is
converted into heat at the surface. Surrounding air is then warmed by
conduction and convection. The best example of this transfer of heat is
from the sun to the earth without loss of heat to outer space.
Radiation or infra-red energy is emitted by all matter that is above
absolute zero (-460°F). The net transfer of heat is from one object to a
cooler object.
Warm objects, including people inside a heated building lose or radiate heat
to the cooler inside surfaces of the walls. The walls conduct heat to the
outside surface and then lose heat by radiation, conduction and convection
to the outside. |
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