In this work, X-ray diffractograms of about 20 coal-based graphites an
d carbons, with different degrees of graphitic order, have been modele
d using the recent computational model of Shi et al. This model relate
s the crystalline parameters c (=2d(002)) and a and the crystallite si
zes L(c) and L(a), to the parameters of the disorder present in carbon
s. These disorder parameters include the probability P for a random di
splacement delta between adjacent layers, the probability P-t for find
ing a 3R stacking fault, the strain parameters, and the preferred orie
ntation. Plots among d(002) L(c), and L(a) lead us to conclude that a
step transition exists in graphites near d(002)=3.37 Angstrom where a
two-fold increase in L(c) is observed for a fixed L(a). This observati
on of a step at 3.37 Angstrom is consistent with the recent observatio
n of Bragg et al. in a graphite where disorder was produced by success
ive grinding, thermal treatments and neutron irradiation. A theoretica
l interpretation of this step-transition is however not yet available.
Plots of d(002) against [delta(2)>], 2P, (2P+P-t) are discussed in te
rms of the disorder models proposed by Franklin and by Ruland. The pre
ferred orientation evaluated from the fit varies systematically with t
he ratio L(c)/L(a) and the experimental X-ray anisotropy ratio. Copyri
ght (C) 1996 Elsevier Science Ltd