Abstract
Zinc whitlockite (Zn-WH, Ca18Zn2(HPO4)2(PO4)12) is a new synthetic analog of the second most abundant biomineral - magnesium whitlockite (Mg-WH, Ca18Mg2(HPO4)2(PO4)12), which is considered as a potential material for bone regeneration. In the present work, the formation of Zn-WH via a dissolution-precipitation process under hydrothermal conditions was investigated in detail. The influence of medium pH, reaction time, temperature and concentration of precursors on the formation of the single-phase material was studied. It was demonstrated that the phase-pure material can be obtained in the pH range from 5.6 to 6.2 in a very short period of time - 1 h. Variation of chemical composition in terms of the Ca-to-Zn ratio was determined to be possible in a narrow range. The structural properties of the synthesized Zn-WH were investigated by powder X-ray diffraction analysis along with 1H and 31P solid-state NMR spectroscopy, FTIR spectroscopy, Raman spectroscopy and XPS. Rietveld refinement confirmed that the synthesized material has a rhombohedral structure with the R3c space group. The NMR study confirmed the presence of three inequivalent phosphorus atoms in the crystal structure, whereas only one PO43− tetrahedron was determined to be protonated. The size and shape of the particles can be controlled by the concentration of the precursors as well as by the initial Ca-to-Zn ratio in the reaction mixture.
| Original language | English |
|---|---|
| Pages (from-to) | 5068-5079 |
| Number of pages | 12 |
| Journal | CrystEngComm |
| Volume | 24 |
| Issue number | 28 |
| DOIs | |
| Publication status | Published - 2 Jun 2022 |
| Externally published | Yes |
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