MOLECULAR CHARACTERIZATION OF FLASH PYROLYSATES OF 2 CARBONIFEROUS COALS AND THEIR CONSTITUTING MACERAL FRACTIONS

Citation
Wa. Hartgers et al., MOLECULAR CHARACTERIZATION OF FLASH PYROLYSATES OF 2 CARBONIFEROUS COALS AND THEIR CONSTITUTING MACERAL FRACTIONS, Energy & fuels, 8(5), 1994, pp. 1055-1067
Citations number
72
Categorie Soggetti
Engineering, Chemical","Energy & Fuels
Journal title
ISSN journal
08870624
Volume
8
Issue
5
Year of publication
1994
Pages
1055 - 1067
Database
ISI
SICI code
0887-0624(1994)8:5<1055:MCOFPO>2.0.ZU;2-R
Abstract
Two high-volatile bituminous Upper Carboniferous coals from the Argonn e Premium Coal Set and their constituting liptinite, vitrinite, and in ertinite fractions, obtained by density gradient centrifugation (DGC), were characterized by Curie point pyrolysis-gas chromatography-mass s pectrometry. A detailed analysis of the pyrolysis products was perform ed to relate individual macerals to their (plant-derived) precursors. Liptinite fractions were found to be mainly composed of sporinite, the diagenetic product of sporopollenin. Its aliphatic character was refl ected in its pyrolysate by the abundance and characteristic distributi on of n-alk-1-enes and n-alkanes showing maxima at C-11 and C-25 Moreo ver, a selective enrichment of aromatic components derived from linear carbon skeletons via cyclization and aromatization of functionalized, linear precursors was observed. In the sulfur-rich Illinois No. 6 coa l, the addition of abiotic inorganic sulfur species to functional grou ps was reflected by a selective enrichment of organic sulfur compounds in the liptinite maceral. Diagenetically altered lignin derived from gymnospermous wood is the most likely precursor for vitrinite, the maj or constituent of both coals. Flash pyrolysates of vitrinite fractions were dominated by alkylbenzenes and alkylphenols. Inertinite fraction s exhibited relatively high amounts of(poly)aromatic pyrolysis product s. Thermal extraction experiments revealed that these components were mainly present as such adsorbed to or entrapped in the pore system of the maceral matrix.