Atomic positional disorder of a single-phase natural carbonate fluorapatite
(francolite) is revealed from analysis of the atomic displacement paramete
rs (ADPs) refined from neutron powder diffraction data as a function of tem
perature and carbonate content. The ADPs of the francolite show a strong di
sturbance at the P, O3, and F sites. When it is heat treated to partially o
r completely remove the carbonate, the ADPs as well as the other structural
parameters resemble those of a fluorapatite (Harding: pegmatite) that was
measured under the same conditions. The various structural changes are cons
istent with a substitution mechanism whereby-the planar carbonate group rep
laces a phosphate group and lies on the mirror plane of the apatite structu
re.