Theory of the Fireball
Theory of the Fireball
Theory of the Fireball
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If we assume that <strong>the</strong> radius Ra <strong>of</strong> <strong>the</strong> iso<strong>the</strong>rmal sphere scales with<br />
4 3<br />
p1<br />
(which may be wrong) <strong>the</strong> radius <strong>of</strong> <strong>the</strong> warm sphere is now<br />
where Y is in megatons. Therefore, along a radius, <strong>the</strong> mount <strong>of</strong> warn<br />
material is about<br />
almost independent <strong>of</strong> ambient air density.<br />
Taking pb/po = 10 -2 (which corresponds to pl/po = 10") and an<br />
average temperature <strong>of</strong> 7000°, Meyerott's tables give for <strong>the</strong> visible:<br />
so that <strong>the</strong> radius represents 0.7 optical mean free path at 1 megaton.<br />
Tnis is nearly transparent, and <strong>the</strong> fireball becomes rapidly more trans-<br />
parent as it cools dawn by fur<strong>the</strong>r emission <strong>of</strong> radiation. The emission<br />
<strong>of</strong> radiation is <strong>the</strong>n proportional to <strong>the</strong> opacity; for each material<br />
element,<br />
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