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-
ion exchange of HA
1) even when there is no net precipitation or dissolution, exchange of ions occurs
2) depends on location
a) hydration shell (very fast)
b) surface (slow)
c) crystal interior (very slow)
HA ions substituted
1) because bulk solutions in contact with HA vary in ion content
- biological HA contains other ions
2) most substitutions increase HA solubility
- ex. carbonated apatite
3) exception
- F- (fluoridated HA)
- makes it more stable