Abstract
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.
| Original language | English |
|---|---|
| Pages (from-to) | 2059-2067 |
| Number of pages | 8 |
| Journal | Langmuir |
| Volume | 33 |
| Issue number | 8 |
| DOIs | |
| Publication status | Published - 30 Jan 2017 |
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