How Nuclear Power Works
Summary
In simple terms, a radioactive material such
as uranium spontaneously breaks apart. As it does so, it gives out energy
and this energy, in the form of heat, can be used to drive an electricity
generator. (Other forms of fuel such as coal, oil and gas also use heat
to drive a generator, although they are burned rather than use radioactivity.)
Although far less uranium is needed to supply a power station than fossil
fuels, the process still consumes material and the uranium eventually
has to be replaced.
The uranium releases its heat to a primary coolant,
usually water, and this is then transferred to a secondary coolant which
drives the turbines to produce electricity. Because the two coolants
are kept apart, the radioactivity is contained within a substantial shield.
In detail
Radioactivity is the spontaneous disintegration of the atomic
nucleus of a material, giving out subatomic particles or electromagnetic
rays. The energy that occurs when this happens can be used to provide
heat which, in turn, can drive a generator to produce electricity. There
are many radioactive elements but the one which is used in all existing
power nuclear stations is uranium.
One reason why uranium is used in nuclear power is that it has
the advantage of being 'fissile' - that means that some of the particles
that are emitted by radioactivity hit other atoms which force them to
release particles in turn. A chain reaction is thus created.
Uranium does not occur naturally but has to be retrieved from an ore
such as pitchblende or carnotite. Pure uranium
consists of the isotope* uranium-238 (U238) which makes up over 99%,
0.7% of uranium-235 and a trace of uranium-234. Because U238 is non-fissile,
the natural uranium has to be enhanced or enriched to provide enough
of the fissile U235 to be useable as a fuel.
|