Pulverised New Zealand coal samples have been tested from an initial temper
ature of 40 degreesC and reacted adiabatisally in an oven with oxygen to pr
ovide a full temperature history of auto-oxidation up to the self-sustained
process of combustion. This procedure produces a self-heating rate index,
R-70, calculated as the ratio of the time taken to reach 70 degreesC (degre
esC/h). The R-70 index is a measure of the coal's propensity to spontaneous
combustion. R-70 values for New Zealand coals are much higher than any pre
viously published results. They show a rank dependence, whereby subbitumino
us coals have the highest propensity to spontaneous combustion (14.91-17.23
degreesC/h). A lignite sample has an R-70 value of 7.76 degreesC/h, and hi
gh-volatile bituminous B coals have R-70 values of 0.31-2.23 degreesC/h. Sa
mples stored for 2 years show the same rank trend. The nature of this trend
is most likely a function of the internal surface area of the coal that go
verns the available sites for oxidation. Calculating the Suggate rank; for
any New Zealand coal can be used to rare its propensity to spontaneous comb
ustion. Resin bodies in the subbituminous coal show no propensity to sponta
neous combustion. (C) 2001 Elsevier Science B.V. All rights reserved.