“…The dissolution of bone mineral, known as biological apatite, has been difficult to characterize due to the complexity of the system (structurally diverse mixture of inorganic apatite mineral, organic macromolecules, , extracellular matrix, cells, and ions) and the technological limitations associated with attaining a well-defined system for gathering precise measurements. To overcome these issues, dissolution of biological apatites as well as hydroxyapatite , (HAP), a close synthetic analog of biological apatite, have been studied under simplified acidic conditions in vitro. − Several dissolution mechanisms have been proposed based on solution phase kinetic data by measuring transient calcium and phosphate ion concentrations from bulk solutions. − However, bone resorption occurs on the apatite surfaces. Recent microscopic kinetic studies based on scanning probe microscopes have shown that the reactions taking place at the solid/liquid (or gas) interface, such as dissolution, nucleation, diffusion and catalytic reactions are significantly affected by local surface structural and stoichiometric environments. − Therefore, the direct observation of atomically well-defined apatite surfaces can provide a fundamental understanding of how the inorganic components of bone and tooth resorb, which cannot be obtained from bulk solution experiments.…”