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Barbieri Thesis - BioMedical Materials program (BMM)

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Chapter 6 – Fluid uptake as instructive factor<br />

larger heterotopic bone formation. As seen earlier, fluid uptake could favor various<br />

phenomena such as biomolecule adsorption and it accelerated the degradation<br />

facilitating the release of calcium and phosphate ions. These processes could later<br />

trigger osteogenic differentiation and bone formation by differentiated cells. Further to<br />

this, degradation leads to the formation of available space for bone ingrowth.<br />

However, when bone formation is slow (i.e. the case of composites) a too fast<br />

degradation might be detrimental as a framework for bone formation would no longer<br />

exist (i.e. the case of MDL). On the contrary, a fast degradation of the ceramic did not<br />

inhibit bone formation because the rate of bone growth was quite high (i.e. the case of<br />

TCPS). It is interesting to observe that both ceramics had a higher fluid uptake, with<br />

consequent larger protein adsorption and faster dissolution/degradation rate, as<br />

compared to the composites. Based on these considerations, we could explain a<br />

higher bone induction potential in both ceramics than the composites. However,<br />

MLDL and MDL composites triggered and supported larger heterotopic bone<br />

formation than TCPB ceramic which gave no bone formation. At the same time, TCPS<br />

induced most bone amongst all the materials analyzed. These discrepancies might be<br />

explained by the presence of multiple physicochemical factors between the two<br />

classes of materials. In fact, as mentioned earlier, composite materials differed only in<br />

their monomer chemistry, while the two ceramics differed in their surface grain size.<br />

On the contrary, when comparing the two classes of materials, they differ in chemistry<br />

(i.e. polymer and calcium phosphate) and surface topography (i.e. nano– and micro–<br />

texture), which have various implications on ion release, protein adsorption and,<br />

ultimately, bone induction potential. Therefore, applying the same principle, in this<br />

case the role of fluid uptake in driving bone formation, is feasible when considering<br />

materials belonging to the same class (i.e. composites and ceramics), but not in a<br />

more general view to compare materials of different classes due to the multi–<br />

factorial issue.<br />

6.5. Conclusion<br />

We have reported that the capacity to uptake fluids influences the bone forming<br />

ability of calcium phosphate based biomaterials, where the materials absorbing more<br />

fluids induced larger heterotopic bone formation. This principle might be applied to all<br />

biomaterials as it held true for two different kinds of material (i.e. composites and<br />

ceramics). However, it cannot be applied to compare the osteoinductive potential<br />

between biomaterials from different families.<br />

145

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