Calcium phosphate hydraulic cements are promising synthetic bone grafting m
aterials. Brushite-based cements were implanted for 6 and 12 months in the
distal condyle of sheep femur, and their in vivo evolution was investigated
by Raman microspectrometry. This new technique can probe small volumes in
the cubic micrometer range. Its resolution allows a very fine analysis of c
rystalline changes in calcium phosphate mixtures at the microscopic level.
First, Raman spectra of pure brushite, monetite, and beta-tricalcium phosph
ate (beta-TCP) were recorded, in order to set a data base for the basic com
ponents of brushite cements. These spectra show significant differences in
the vibration mode v(1) for the phosphate ion (988 and 878 cm(-1) for brush
ite, 988 and 900 cm(-1) for monetite, 968 and 948 cm(-1) for beta-TCP), The
se differences are strong enough as to allow the qualitative and quantitati
ve analysis of these crystalline phases in the cement, Implanted sheep femu
r samples were harvested after 24 and 52 weeks post-op, and prepared for Ra
man analysis in the form of 1-mm-thick sections. Implants at 24 weeks show
a core of residual cement isolated from the surrounding bone by fibroconnec
tive tissue. No trace of brushite was detected by micro-Raman analysis in t
his area, but instead, a mixture of beta-TCP and Type-B carbonated apatite,
the latter being very close in composition and structure to the mineral fr
action of normal bone in the vicinity of the implant. Implants recovered af
ter 52 weeks show a decrease of the bone/residual cement perimeter, whereas
new trabeculations are formed in the implanted zone; the small amounts of
residual cement still present are substantially transformed into Type-Il ca
rbonated apatite containing small amounts of proteins. In the same area, so
me beta-TCP particles are also detected showing that, contrary to brushite,
the excess beta-TCP originally present in the cement is not completely met
abolized. In the implanted zone already converted into trabecular bone, Ram
an microspectrometry shows the characteristic spectrum of normal bone. (Bon
e 25: 81S-84S; 1999) (C) 1999 by Elsevier Science Inc. All rights reserved.