1.01
An explosion, in general, results from the very rapid release of a large
amount of energy within a limited space. This is true for a conventional
"high explosive," such as TNT, as well as for a nuclear (or
atomic) explosion, [1]
although the energy is produced in quite different ways (§ 1.11).
The sudden liberation of energy causes a considerable increase of temperature
and pressure , so that all materials present are converted into hot,
compressed gases. Since these gases are at very high temperatures and
pressures, they expand rapidly and thus initiate a pressure wave , called
a "shock wave," in the surrounding medium - air, water or
earth. The characteristic of a shock wave is that there is (ideally)
a sudden increase of pressure at the front, with a gradual decrease
behind it as shown in figure 1.01. A shock wave in
air is generally referred to as a "blast wave" because it
resembles and is accompanied by a very strong wind. In water or in the
ground , however, the term "shock" is used, because the effect
is like that of a sudden impact. |
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