posted on 2017-01-30, 00:00authored byErik A.
B. Hughes, Richard L. Williams, Sophie C. Cox, Liam M. Grover
Calcium
phosphate (CaPO4) tubes with features comparable
to mineralized biological microstructures, such as Haversian canals,
were grown from a calcium gel/phosphate solution chemical garden system.
A significant difference in gel mass in response to high and low solute
phosphate equivalent environments existed within 30 min of solution
layering upon gel (p = 0.0067), suggesting that the nature of advective movement
between gel and solution is dependent on the solution concentration.
The transport of calcium cations (Ca2+) and phosphate anions
(PO43–) was quantified and changes in
pH were monitored to explain the preferential formation of tubes within
a PO43– concentration range of 0.5–1.25
M. Ingress from the anionic solution phase into the gel followed by
the liberation of Ca2+ ions from the gel was found to be
essential for acquiring self-assembled tubular CaPO4 structures.
Tube analysis by scanning electron microscopy (SEM), X-ray diffraction
(XRD), and micro X-ray florescence (μ-XRF) revealed hydroxyapatite
(HA, Ca10(PO4)6(OH)2)
and dicalcium phosphate dihydrate (DCPD, CaHPO4·2H2O) phases organized in a hierarchical manner. Notably, the
tubule diameters ranged from 100 to 150 μm, an ideal size for
the permeation of vasculature in biological hard tissue.