The non-stoichiometric dissolution of hydroxyapatite (HAP) in aqueous solutions of NaCl, Na
2SO
4, and sodium dodecyl sulfate (SDS) was studied. Molar ratios of Ca
2+ to phosphate ion (Pi) released from HAP varied depending on species and concentration of an added salt. The order of salts inc reasing [Pi] was SDS >Na
2SO
4>NaCl, while that increasing [Ca
2+] was NaCl> Na
2SO
4 > SDS, where the concentration of SDS was lower than its cmc (critical micellization concentration). These results were explained as follows: Pion the surface of HAP is more easily replaced by SO
42- than Cl- through a mechanism of ion exchange with isomorphic substitution, because the ion size of SO
42- is quite similar to that of PO
43--. On the other hand, the chemical structure of dodecyl sulfate ion (DS-) is made u p by a covalent bond between -SO
4- and a hydrocarbon chain (-C
12H
25). The adsorption of organic DS-, therefore, was enhanced more than that of inorganic SO
42- by both the hydrophobic/cooperative e ffect of the hydrocarbon chains and the isomorphous replacement of the terminal -SO
4- with PO
43- on the surface of HAP. Excess amounts of negative charge due to the adsorbed DS- accelerate the release of Pi from HAP in order to relax the high electrochemical potential of the surface. This mechanism result s in more release of Pi in the presence of SDS than in the presence of Na
2SO
4. The sequence of th e salts for the Ca
2+ releasing was in t he reverse of that for the Pi releasing by virtue of restriction of the solu bility product of HAP.
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