Ignition temperatures of plutonium and the pyrophoric potential of plutoniu
m-containing pyrochemical salt residues are determined from differential th
ermal analysis (DTA) data and by modeling of thermal behavior. Exotherms ob
served at 90-200 degrees C for about 30% of the residues are attributed to
reaction of plutonium with water from decomposition of hydrated salts. Exot
herms observed near 300 degrees C are consistent with ignition of metal par
ticles embedded in the salt. Onset of self-sustained reaction at temperatur
es as low as 90 degrees C is not precluded by these results and heat-balanc
e models are developed and applied in predicting the static ignition point
of massive metal and in evaluating salt pyrophoricity. Results show that am
bient temperatures in excess of 200 degrees C are required for ignition of
salt residues and that the most reactive salts cannot ignite at low tempera
tures because diffusion of oxidant to embedded metal is limited by low salt
porosity. (C) 2000 Elsevier Science B.V. All rights reserved.