Hydroxyapatite Flashcards
ionic solid
1) salt
- positive and negative charge
2) aggregation
- formation of solid state
- ions attract (electrostatic or ion-ion)
3) dispersion
- attraction between ion and solvent (ion dipole)
4) entropy of interactions with solvent
slightly soluble in water
1) stable in solid state
2) ions with high charge density
- Ca2+, Al3_, PO43-
3) pack to:
- maximize separation of same charge ions
- minimize separation of opposite charge ion
highly soluble
1) low charge density
2) pack relatively poorly
3) NaCl
basic dissolution/precipitation stages
1) dynamic state
2) reaches equilibrium
- when dissolution and aggregation rates are the same
solid-solution transition
1) ions on left side are shown hydrated (aquo ions) with the common coordination of #6 waters
M(H2O)6 + X(H2O)6
2) usually ion’s hydration state is not shown
3) moving to right: precipitation
MX + 12H2O
equations to describe rate of dissolution and precipitation
1) depends on surface area of the solid
2) rate (dsln) = k(dsln)(Area of solid)
3) rate (pptn) = k(dsln)(Area of solid)*[M+][X-]
4) ion product
- [M+][X-]
5) net rate = rate (dsln) - rate (pptn)
at equilibrium
1) net rate = 0
2) so rate dsln = rate pptn
ksp
1) higher Ksp is higher solubility
2) equilibrium constant
Ksp = kdsln/kpptn = [M+]eq*[X-]eq
3) at equilibrium, the product of component ions is equal to a constant (Ksp)
- saturated
- no net dissolution or precipitation
deviation from equilibrium
1) applicable ion product =/= Ksp
2) ion product > Ksp
- precipitation
- mineralization
- (SUPERSATURATED)
3) ion product < Ksp
- dissolution
- demineralization
(UNDERSATURATION)
in an undersaturated solution
1) K(dsln) > K(pptn)[M+][X-]
2) because the rate of dissolution is more than precipitation (there is more solvent, you need more things to dissolve to reach saturation)
hydroxyapatite composition
1) calcium and phosphate
- pH = 7 ( lowest solubility solid)
2) Ca10(PO4)6(OH)2 – dimer
3) in solutions containing physiological concentrations of other ions, solubility is higher
- Ksp = 0.7 mM^2
4) versus salt
- Ksp = 3*10^7 mM^2
Ksp and ions can allow you to calculate:
1) tendency of a fluid to dissolve
2) it is the product of ion concentration that matters
- differing ion concentrations can lead to same Ksp if multiplying it by phosphate (Pi)
conditions where ion product < Ksp
1) pH dependent for hydroxyapatite
2) the Ksp increase when pH<5
- Ksp > ion product
- dissolution
pH dependent solubility
1) for many other salts, solubility pH dependent too
2) because Pi forms are acids/bases with each form being pH dependent
hydroxyapatite crystals have an anion channel on the c-axis
1) inside is OH-, F-, Cl-