Coal is intensively
used worldwide as a main fuel source. However,
it may undergo oxidation processes [i.e., low-temperature oxidation
(LTO)] when stored under an air atmosphere in piles post-mining at
low temperatures ranging from 300 to 425 K, specifically, a surface
gas/solid reaction with molecular oxygen. Therefore, it is of major
importance to prevent or appreciably slow down such reactions, which
result in a loss in the energy content (calorific value) of coal.
Previously, we showed that radicals are formed during the LTO process.
In this work, the dependence of radical formation on coal rank as
a function of heating (temperature) and the presence of oxygen gas
were studied using electron paramagnetic resonance spectroscopy. It
was shown that lignite coals are more sensitive than bituminous coals
to the atmospheric environment (i.e., molecular oxygen and nitrogen
content) and to temperature, as reflected by the formation of surface
carbon-centered radicals. Moreover, this is the first publication
showing the effects of LTO on micro- and macro-pores by assessing
how these structures affect O
2
diffusion. The LTO process
blocks the micro-pores, such that radicals form mainly at the surface
of the coal macromolecules, in both bituminous and lignite coals.