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Title: Low temperature chemical fragmentation of coal

Technical Report ·
DOI:https://doi.org/10.2172/5291898· OSTI ID:5291898

Trifluoroperoxyacetic acid chemically fragments coals at 25 to 80/sup 0/. The reagent is so selective for oxidizing aromatic rings and is so inert towards benzylic hydrogen that isopropylbenzene, tetralin, indan, and dihydrophenanthrene have their benzene ring(s) totally destroyed without any evidence of oxidation at the benzylic hydrogen. The fragments contain more and different structural information relative to conventional oxidations with Mn VII, Cr VI, HNO/sub 3/, and O/sub 2/. These latter selectively oxidize benzylic hydrogen. Products from 37 selected coals show that 9,10-dihydroanthracene and 9,10-dihydrophenanthrene units are prominent features in most bituminous coals in accord with Given's structure of coal. Their frequency accounts for the fact that no continuous fused ring structure or graphite structure exists. The only simple alkyl substituent is methyl. Liquefaction (solvent refining) sharply increases the amount of arylmethyl and aromatic structure and causes the appearance of unsubstituted phenyl groups. Nitric acid degradations have been reinvestigated and are developed into a premier method for analyzing the amounts and lengths of linear alkane chains in coals. Generally the amounts of such chains represents 0 to 2% of the carbon in coal, but in one Utah coal they account for about 42% of the carbons.

Research Organization:
Pennsylvania State Univ., University Park, PA (United States)
Sponsoring Organization:
USDOE
DOE Contract Number:
AS01-78ET13381
OSTI ID:
5291898
Report Number(s):
DOE/ET/13381-T1
Country of Publication:
United States
Language:
English