EFFECTS OF DRYING AND OXIDATION OF WYODAK SUBBITUMINOUS COAL ON ITS THERMAL AND CATALYTIC LIQUEFACTION - SPECTROSCOPIC CHARACTERIZATION ANDPRODUCTS DISTRIBUTION
Cs. Song et al., EFFECTS OF DRYING AND OXIDATION OF WYODAK SUBBITUMINOUS COAL ON ITS THERMAL AND CATALYTIC LIQUEFACTION - SPECTROSCOPIC CHARACTERIZATION ANDPRODUCTS DISTRIBUTION, Energy & fuels, 8(2), 1994, pp. 301-312
Drying and oxidation of Wyodak subbituminous coal at 100-150 degrees C
have been shown to have significant effects on its structure and on i
ts catalytic and noncatalytic low-severity liquefaction at 350 degrees
C for 30 min under 6.9 MPa of H-2. Spectroscopic analyses using solid
-state C-13 NMR, pyrolysis-GC-MS, and FT-IR revealed that oxidative dr
ying at 100-150 degrees C causes the transformation of phenolics and c
atechol into other related structures (presumably via condensation) an
d high-severity air drying at 150 degrees C for 20 h leads to disappea
rance of catechol-like structure. Increasing air drying time or temper
ature increases oxidation to form more oxygen functional groups at the
expense of aliphatic carbons. For noncatalytic liquefaction at 350 de
grees C, raw coal gave higher conversion and oil yield than the dried
coals, regardless of the solvent. Compared to the vacuum-dried coal, t
he coal dried in air at 100 degrees C gave a better conversion in the
presence of either a hydrogen-donor tetralin or a nondonor l-methylnap
hthalene (1-MN) solvent, Catalytic runs were performed using impregnat
ed ammonium tetrathiomolybdate (ATTM) precursor. In the presence of ei
ther-tetralin or 1-MN, however, the runs using ATTM impregnated on air
-dried coal (dried at 100 degrees C for 2 h) afford better-conversions
and oil yields than using vacuum-dried coal. Upon drying in air at 15
0 degrees C for 20 h, the conversion of air-dried coal decreased to a
value significantly lower than that of the vacuum-dried coal in both t
he thermal and catalytic runs at 350 degrees C. Such a clearly negativ
e impact of severe oxidation is considered to arise from significantly
increased oxygen functionality which enhances the cross-link formatio
n in the early stage of coal liquefaction. Physical, chemical, and sur
face physicochemical aspects of drying and oxidation and the role of w
ater are also discussed.