Abstract
Introduction and Objective
Calcium phosphates are among the most commonly used bone graft substitute materials. Compositions containing predominantly monetite (∼84.7%) with smaller additions of beta-tricalcium phosphate (β-TCP; ∼8.3%) and calcium pyrophosphate (Ca-PP; ∼6.8%) have previously been demonstrated to exhibit osteoinductive properties. Such a multi-component calcium phosphate bioceramic was fashioned in the form of hollowed-out, dome-shaped devices (15 mm diameter, 4 mm height), each reinforced with a 3D printed Ti6Al4V ELI frame. With the aim to induce bone formation beyond the skeletal envelope, these devices were investigated in vivo using a sheep (Ovis aries) occipital bone model.
Materials and Methods
The bioceramic composition was prepared from a mixture of β-TCP/dicalcium pyrophosphate and monocalcium phosphate monohydrate powders mixed with glycerol. The Ti6Al4V ELI frame was positioned into a dome-shaped mould and bioceramic paste was poured over the frame and allowed to set, in sterile water, prior to removal from the mould. In adult female sheep (n=7), the devices were positioned directly over the bone and stabilised using self-drilling screws. After 52 weeks, the devices were retrieved, resin embedded, and used for X-ray micro-computed tomography (micro-CT), histology, backscattered electron scanning electron microscopy (BSE-SEM), energy dispersive X-ray spectroscopy (EDX), micro-Raman spectroscopy, and Fourier transform infrared spectroscopy (FTIR).
Results
The bioceramic composition (Ca/P: ∼0.85 at. %) transforms to carbonated apatite (Ca/P: ∼1.2 at. %, Mg/Ca: ∼0.03 at. %), in vivo, largely at the expense of monetite and Ca-PP whereas β-TCP remains detectable. Discrete particles of Ca-PP are identified by correlative BSE-SEM and micro-Raman spectroscopy. Together with chemical transformation, physical degradation is evident within the bulk of the bioceramic. Beyond the confines of the skeletal envelope, de novo bone occupies ∼53–84% (∼73 ± 11%; mean ± standard deviation) of the hollowed-out space. Low porosity and the arrangement of remodelled bone into a concentric lamellar pattern is indicative of cortical-like structure. Such areas are typically surrounded by yet unremodelled, and microstructurally disordered, woven bone that stains intensely with blue cationic dyes, owing to relatively higher acid phosphate content. This pattern indicates a recurring sequence of woven bone formation followed by remodelling. Bone formation is also visible within the bioceramic. Recently remodelled and areas of ongoing remodelling are identified by relatively lower mineral density than the surrounding woven bone. Dendritic extensions of osteocytes appear to extend into the bioceramic surface. Both micro-Raman spectroscopy and FTIR reveal little, if any, detectable difference between the mineral and organic phases of the extracellular matrix, between de novo and native bone.
Conclusions
The bioceramic composition undergoes physical degradation, but remains largely intact by 52 weeks in vivo, and only partially transforms to carbonated apatite. In addition to very high bone volume within the hollowed-out bioceramic device, the overall composition and microstructure of de novo bone are similar to native bone. Notably, the mineral phase of bone in response to, and in direct contact with the β-TCP, monetite, and Ca-PP, remains exclusively carbonated apatite.
