The inelastic neutron-scattering (INS) spectra from 30 to 4000 cm(-1)
of four coal samples of different rank (subbituminous A, low-volatile
bituminous, semianthracite and anthracite) at 20 K are reported. For e
ach coal, rather broad bands superimposed on a continuum with almost c
onstant intensity over the whole frequency range are observed. This co
ntinuum is assigned to recoiling free protons located between the grap
hite-like planes. Band frequencies are compared with those observed in
the infrared for the same samples in KBr matrices at room temperature
, and consistent assignments in terms of chemical-grouping vibrations
are proposed. The INS spectra of the coals are also compared with that
of perylene (C20H12) The spectrum of anthracite is dominated by CH an
d skeletal modes of polyaromatic entities. Coals of lower rank show ba
nds due to alkyl and vinyl CH2 and CH3 groups. A comparison of INS int
ensities in the CH stretching region for coals and perylene gives an e
stimate of the concentration of bound protons which ranges from simila
r to 40% to similar to 80%. A simple model is proposed to estimate the
mean size of the graphite-like domains in the coals.