Ec. Moreno et al., ADSORPTION OF PEROXYDIPHOSPHATE ONTO HYDROXYAPATITE - KINETICS, THERMODYNAMICS, AND CRYSTAL-GROWTH INHIBITION, Journal of colloid and interface science, 168(1), 1994, pp. 173-182
Peroxydiphosphate ion, P2O84-, PDP, a potential agent to control miner
alization in biological systems, adsorbs readily onto hydroxyapatite,
HA, the prototype of the mineral in bones and teeth. The apatite cryst
als, however, catalyze the hydrolysis of PDP, which is faster at 37 de
grees C than at 4 degrees C. Hydrolysis at the lower temperature is a
first order reaction; at 37 degrees C the process is more complex and
may be limited by surface diffusion. Orthophosphate in solution repres
ses the hydrolysis of PDP. Adsorption isotherms were determined in the
presence of orthophosphate at the two temperatures mentioned. The exp
erimental data were best described by a model involving two adsorption
sites at which PDP adsorbs in competition with orthophosphate ions. T
he adsorption bond at one of the sites is more than 10 times stronger
but its capacity is from 1/4 (at 37 degrees) to 1/8 (at 4 degrees) the
capacity of the site displaying the weaker bond. The inhibition of cr
ystal growth by PDP is related only to its adsorption onto one of the
adsorption sites, which represents only 18% of the maximal PDP adsorpt
ion. It is inferred that crystal growth occurs (or is initiated) on a
relatively small fraction of the crystal surface. Calculation of the t
hermodynamic functions for adsorption shows that the reaction is endot
hermic and, therefore, that adsorption of PDP is entropically driven;
the gain in entropy is probably associated with changes in the locatio
n of water molecules on the adsorbate and the adsorbent. The reported
thermodynamic properties of the two adsorption sites are distinctly di
fferent. (C) 1994 Academic Press, Inc.