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Theory of the Fireball

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toward a .second maximum. This stage has been very little considered<br />

<strong>the</strong>oretically, except in numerical calculations, and forms <strong>the</strong> subject<br />

<strong>of</strong> this report.<br />

We shall show that for some time In Stage Cy <strong>the</strong> radiation comes<br />

fm <strong>the</strong> air between iso<strong>the</strong>rmal sphere and shock front (Stage C I) .<br />

During this time, <strong>the</strong> radiation can be calculated essentially from <strong>the</strong><br />

temperature distribution which is set up by <strong>the</strong> adiabatic expansion <strong>of</strong><br />

<strong>the</strong> material behind <strong>the</strong> shock (Secs 3 and 5f ,g) The temperature and<br />

total intensity <strong>of</strong> <strong>the</strong> radiation increase with time toward <strong>the</strong> larger,<br />

second maximum.<br />

The energy for<strong>the</strong> radiation is largely sqplied by a cooling wave<br />

(Sec. 5) which gradually eats into <strong>the</strong> hot interior. When this coollng<br />

wave reaches <strong>the</strong> iso<strong>the</strong>rmal sphere, <strong>the</strong> radiation temperature reaches<br />

its maximum (Sec. 5e); it <strong>the</strong>n declines again as <strong>the</strong> cooling wave eats<br />

more deeply into <strong>the</strong> iso<strong>the</strong>rmal sphere (Stage C 11). This process ends<br />

by <strong>the</strong> iso<strong>the</strong>rmal sphere being comgletely eaten away (Sec. 6) .<br />

mer this has happened, <strong>the</strong> entire fireball, iso<strong>the</strong>rmal sphere and<br />

cooler envelope, is transparent to its own <strong>the</strong>rmal. radiation (Stage D) .<br />

The molecular bands, which previously appeared in absorption, now appear<br />

in emission (Stage D I) . Emission w ill lead to fur<strong>the</strong>r coollng <strong>of</strong> <strong>the</strong><br />

fireball, though more slowly than before. Soon, when <strong>the</strong> temperature<br />

falls below about 6000°, <strong>the</strong> emission becomes very weak, and stibsequent<br />

cooling is almost entirely adiabatic (Stage D 11) . A t sea level, <strong>the</strong><br />

pressure may go down to 1 bar before <strong>the</strong> temperature falls belaw 6000~;<br />

c

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