The conditions necessary for a laboratory-scale separation of the prem
aceral constituents of peat (i.e., the precursor to coal) are investig
ated. The method used is an isopycnic density centrifugation (DGC) tec
hnique aimed at isolating pure premacerals. This method, which is base
d on known density differences of various macerals, has been used succ
essfully in coal separations but never with peats. The technique invol
ved grinding the peats in a planetary ball mill to an approximate 10 m
u m average particle size and conducting dispersion tests using NaCl,
Ca(NO3)(2), CsCl, and TEE as solvents coupled with numerous surfactant
s. The density gradient centrifugation technique was run with both an
aqueous and organic gradient using plain milled peat, demineralized pe
at, and demineralized methylated peat. The best separations were achie
ved in a single run if the peat was demineralized and dispersed with a
wetting agent in an organic gradient. Analytical-scale separations we
re used to choose the most responsive peat to be used in a preparative
-scale separation. A low and high density weight fraction, analyzed by
flash pyrolysis, revealed distinctly different chromatograms, indicat
ing that the pear had reached a reasonable degree of separation. Four
peats of differing constitution are reviewed.