Although this material has been generally regarded as prone to exothermic s
elf-decomposition with very rapid release of heat, oxygen and gaseous chlor
ine derivatives it has not been the subject ol an orthodox thermal ignition
study such as that performed on anhydrous calcium hypochlorite(UN 1748), s
tudied in the standard manner in 1978. This paper describes such rests on s
amples varying in mass from 5 g up to 200 kg in cylindrical containers of v
arying aspect ratio and various materials including stainless steel gauze,
high-density polyethylene and coated fibre. The heat transfer coefficients
of all the containers were measured accurately by both steady-state and coo
ling curve procedures and the thermal conductivity of the hypochlorite was
measured independently. These measurements revealed that the Blot numbers o
f the samples tested were: in a range where the critical ambient temperatur
es were sensitive to the values and thus sensitive to the convective air fl
ow around the test bodies. With these factors taken into account the usual
Frank-Kamenetskii (F-K) plot gave a good straight line in the range 115 deg
rees C upwards. However, below this temperature, i.e. in the range 40-115 d
egrees C very strong deviations occur. Nevertheless, the F-K theory still h
olds as the low-temperature points also fall on a good straight line with a
ctivation energy 48.5 kJ/mol which compares with the high-temperature activ
ation energy much greater than this. These results indicate a sharp change
in the rate determining step for heat generation at temperatures around 100
-120 degrees C. In temperature ranges both above and below this area the te
mperature-lime traces for the samples behave classically as would be expect
ed from the F-E; theory but inside this range the traces show much more com
plex behaviour with some oscillatory characteristics, also some evidence of
endothermic behaviour. The consequences of this unexpected behaviour for s
afety (particularly in the bulk; marine shipping context) are serious. The
deviations predicted from simple extrapolation of the high-temperature resu
lts indicate much lower critical ambient temperatures for large quantities
of this material than previously thought. Our low-temperature results obtai
ned by orthodox ignition methods are entirely consistent with independent d
irect isothermal calorimetric measurements already present in the literatur
e but not used quantitatively in this context. (C) 2000 Elsevier Science Lt
d. All rights reserved.