The neutron Compton scattering technique (NCS) was utilized for a precise d
etermination of the randomly oriented crystallites fraction in partially or
iented graphite. This was done by measuring the effective temperatures of t
he C-atom along and perpendicular to the graphite planes in a sample of Pap
yex and comparing the results with those obtained from a highly oriented py
rolytic graphite (HOPG) sample. The half-width at half-max of the oriented
fraction of crystallites (mosaic spread) was found to be (11.0 +/- 0.6)degr
ees, while the randomly oriented fraction was found to be (26.2 +/- 1.6)%.
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