S. Borunov et al., HIGH-TEMPERATURE CHEMISTRY IN THE FIREBALLS FORMED BY THE IMPACTS OF COMET P SHOEMAKER-LEVY-9 IN JUPITER/, Icarus, 125(1), 1997, pp. 121-134
High temperature chemistry in the fireballs created by the impacts of
Comet P/Shoemaker-Levy 9 in Jupiter has been studied using thermochemi
cal models of the impacts. Explosions of the fragments at different le
vels in the jovian atmosphere ranging from above the clouds of NH3(s)
to below the clouds of H2O(s) have been considered. The chemical compo
sition of the expanding fireballs is studied, allowing a retrieval of
the distribution of oxygen, carbonaceous, sulfur, nitrogen, and phosph
orus compounds following the impacts. As a result, a list of the most
abundant compounds is derived, which is found to correspond to the com
pounds observed after SL9 impacts. In particular, it is found that the
production of CS by chemical reactions in the fireballs can be compar
able to the production of CS2. The predictions of CO/H2O, CS/CS2, and
other abundance ratios, which can be derived from the models, may help
in the determination of the average depth of the impacts. (C) 1997 Ac
ademic Press