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Theory of the Fireball

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Magee in Report LA-2000) and will <strong>the</strong>refore not be fur<strong>the</strong>r" consid,ered ..<br />

here . During Stage A, temperatures are very high. The Pianck spectrum <strong>of</strong><br />

t <strong>the</strong> air is in <strong>the</strong> x-ray or far ultraviolet region, and hence is irmnedf-<br />

ately absorbed by <strong>the</strong> surrounding air. The very hot air is <strong>the</strong>refore<br />

surrounded by a cooler envelope, and only this envelope is visible to<br />

observers at a distance. The observable temperature <strong>the</strong>refore has little<br />

physical significance. It is observed that <strong>the</strong> size <strong>of</strong> <strong>the</strong> ltrminous<br />

sphere lncreases rapidly, and <strong>the</strong> total emission also .Increases, up to<br />

a first maximum. -<br />

When <strong>the</strong> temperature <strong>of</strong> <strong>the</strong> central sphere <strong>of</strong> air has fallen, by<br />

successive emission and re-absorption <strong>of</strong> x-rays, to about j0O,00O0, a<br />

-hydrodynamic shock forms, The shock now moves faster than <strong>the</strong> tempera-<br />

ture could propagate by radiation transport, The shock <strong>the</strong>refore sepa-<br />

rates from<strong>the</strong> very hot, nearly iso<strong>the</strong>nml sphere at <strong>the</strong> center. This<br />

is Stage 13 in <strong>the</strong> development. The shock mves by simple<br />

Its front obeys <strong>the</strong> Hugoniot relations, <strong>the</strong> density being<br />

Behind <strong>the</strong> front, <strong>the</strong> air expands adiabatically, and at a<br />

<strong>of</strong> <strong>the</strong> shock radius, .<strong>the</strong> density is apt to have fallen. by<br />

or mre compared to <strong>the</strong> shock density, while <strong>the</strong> temperature has risen<br />

by a comparable factor, (3.16) Thus <strong>the</strong> interior is at very low density,<br />

and hence <strong>the</strong> pressure must be neasly constant (o<strong>the</strong>rwise <strong>the</strong>re would be<br />

very large accelerations which soon would equalize <strong>the</strong> pressure) . This<br />

. .<br />

greatly simplifies <strong>the</strong> structure <strong>of</strong> <strong>the</strong> shock, and leads to such simple<br />

13<br />

,

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