Coal
is one of the major fuels for power generation, and it will
continue in this capacity for the next several decades. Two types
of coal are mainly used: lignite and bituminous coals. When exposed
to air, post-mining, the coal surface undergoes LTO (low-temperature
oxidation) at RT-150 °C according to the atmospheric oxygen level.
The LTO process decreases the calorific value of the coal, and consequently,
different gases are released [mainly carbon oxides (CO, CO2), water vapor, hydrogen (H2), and also some low molecular-weight
organic gases (C1–5)]. Some of these gases are toxic
and flammable. In extreme cases, fires erupt. The mechanism by which
the molecular oxygen oxidizes the coal macromolecule at the temperature
range of 30–150 °C (LTO process) is complex and also involves
a chain of radical reactions that take place; however, the exact underlying
mechanism is not yet clear. The LTO process was studied in detail
by simulating the processes occurring in the coal piles by using two
coal types: an American Bailey coal, used in Israeli coal-fired utilities
and a German Hambach lignite, used in German utilities. The mechanism
underlying the LTO process and the radical reactions that are involved
are discussed in detail.