DISSOLUTION KINETICS OF BIOAPATITE FROM PH 2 TO 8 AT 4° TO 38°C
R = k1(H+)n + k2
in which R is the dissolution rate (mol bioapatite m-2 s-1) based on the bioapatite stoichiometry, n = 1.01 ± 0.15, k1 = 1.84 x 10-6 mol m-2 s-1, and k2 =4.29 x 10-10 mol m-2 s-1, and H+ is the hydrogen ion activity. From 2 < pH < 4, the dissolution rate is dependent on pH and becomes independent of pH from 4 < pH < 8. These results for modern bone may be compared with previous investigations of igneous (FAP) and phosphorite-derived sedimentary carbonate fluorapatites (CFA)(e.g., Guidry and Mackenzie, 2003). At pH = 6, in the pH-independent region, dissolution of the modern bioapatite was ca. 7 times faster than FAP and 100 times faster than CFA. The acid transition pH of the bioapatite is lower than that for FAP. The apparent activation energy of bioapatite dissolution, 18.1 kJ mol-1, suggests a diffusion-controlled reaction. Previous studies of dissolution reactions for other forms of apatite have yielded higher activation energies, indicating that their dissolution reactions are surface controlled. BET surface area analyses of bioapatite particles are approximately 5 orders of magnitude greater than calculated geometric surface areas. BET surface areas are therefore critical for calculating accurate bioapatite dissolution rates. Bioapatite has been suggested for use as reactive barriers to control pollutants and nuclear waste isolation and as a feedstock mineral in CO2 sequestration processes. Modeling the dissolution of bioapatite is necessary to determine its potential for these uses.