Disks made of hydroxyapatite, p-tricalcium phosphate, carbonate apatite, te
tracalcium phosphate, a-tricalcium phosphate, dicalcium phosphate dihydrate
, and octacalcium phosphate were incubated in osteoclastic cell cultures fo
r 2 days. The first five salts were sintered and the last two were compress
ed before incubation. Osteoclasts resorbed only the sintered carbonate apat
ite disks. However, osteoclasts were able to resorb octacalcium phosphate d
isks that were preincubated for 1 day in medium without cells, indicating t
hat surface conditioning was important for osteoclastic resorption of this
calcium phosphate. Although resorption did not occur, medium calcium and ph
osphorus changed to an appreciable extent after a 2-day incubation of p-tri
calcium phosphate, tetracalcium phosphate, ol-tricalcium phosphate, and dic
alcium phosphate dihydrate. These changes in the medium calcium and phospha
te concentrations could explain why osteoclasts appeared to have lost their
activity on these calcium phosphate disks and were not capable of resorbin
g them. With hydroxyapatite disks no changes were observed in the medium ca
lcium and phosphorus before and after incubation. Moreover, the osteoclasts
appeared to be essentially the same as with the sintered carbonate apatite
disks and with bone slices used as a control. Nevertheless, no pits or lac
unae were observed on the hydroxyapatite disks, indicating that sintered ca
rbonate apatite should be superior to sintered hydroxyapatite as a bioresor
bable bone substitute. (C) 1999 John Wiley & Sons, Inc.