Volatile matter evolved during pyrolysis of 20 different rank coals was stu
died by thermogravimetry-photoionization mass spectrometry (TG-PI-MS). The
composition of the TGA effluent revealed several significant trends with co
al rank. First, the relative intensities of peaks due to compounds containi
ng oxygen such as CnH2nO (n = 2, 3, or 4), phenols, and dihydroxybenzenes d
ecreased with increasing coal rank. Also, the relative intensities of peaks
due to aromatic compounds such as naphthalenes, phenanthrenes, and pyrenes
increased with increasing coal rank. Mass signals due to sulfur compounds
evolved from-coal showed qualitative correlations between CS2 (%TIC) and py
ritic sulfur content and between CH3SH (%TIC) and aliphatic sulfur content.
Several of the coals were extracted with a solvent to remove the soluble p
ortion of the coal. TG-PI-MS analysis of the raw coal, extracted material a
nd coal residue remaining after solvent extraction produced very similar ma
ss spectral These results suggest that the majority of the compounds observ
ed by TG-PI-MS are products: of thermal cleavage of bonds within the coal s
tructure. This conclusion is further supported by 337 nm laser desorption m
ass spectrometry of the solvent extracts, The results from these analyses s
uggest that volatile matter, like coal itself, consists of compounds with a
range of molecular weights but with similar molecular structures.