Oxidation produces important transformations in the chemical composition an
d textural properties of bituminous coals. A higher-rank coal - semianthrac
ite, 14.7% volatile matter - was oxidised in an oven with a forced air circ
ulation, at 473 and 543 K, for periods of 1-7 days. The pyrolysis of fresh
and oxidised coal samples was performed under nitrogen up to 1123 K at a he
ating rate of 60 K min(-1) without a soaking time. As oxidation progressed,
increases in volatile matter and oxygen content were observed for all the
coals. Preoxidation led to a densification of carbonaceous matter with an i
ncrease in the true and apparent densities, the increase being most pronoun
ced for the series oxidised at 543 K. The pyrolysis of raw material and oxi
dised coals caused a decrease in oxygen and hydrogen contents and an increa
se of up to 93% in carbon content. The true density of the chars was higher
than that of the oxidised coals. Total pore volume and porosimetry values
show that oxidation has a strong influence on pore-size distribution in the
chars, a longer oxidation favouring a pronounced microporous character. Bo
th BET-N-2 and DR-CO2 surface areas of the chars increase correspondingly,
showing the positive effect of oxidation on the evolution of the solid text
ure. (C) 2001 Elsevier Science B.V. All rights reserved.