Abstract
Using a wet method, we have synthesized octacalcium phosphate carbonate, in which HPO42− in octacalcium phosphate is replaced with CO32−. The physical, crystal, and chemical properties of this new material were compared to octacalcium phosphate, Ca-deficient hydroxyapatite, and Ca-deficient carbonate apatite using X-ray diffraction, Fourier-transform infrared spectroscopy, inductively coupled plasma spectroscopy, and scanning electron microscopy. Surface roughness and morphology were also characterized, along with the ability to support proliferation and differentiation of MG63 cells, as measured by MTT and alkaline phosphatase assay. We found that octacalcium phosphate carbonate enhanced osteoblast proliferation more strongly than all other materials tested. Similarly, Ca-deficient carbonate apatite, a hydrolysate of octacalcium phosphate carbonate, stimulated osteoblast differentiation to a better extent than Ca-deficient hydroxyapatite, a carbonate-free hydrolysate of octacalcium phosphate. These results indicate that octacalcium phosphate carbonate has good biocompatibility and osteoconduction, and incorporation of carbonate into octacalcium phosphate and apatite enhances bone regeneration.
Keywords
Introduction
Among bone substitutes, materials based on calcium phosphate are widely used, because of good biocompatibility and osteoconductivity [1–4]. Examples of such materials include hydroxyapatite and β-tricalcium phosphate [2,5,6]. Hydroxyapatite is well established to be osteoconductive, while β-tricalcium phosphate was found to have good biodegradability following nucleation of new bone [5–7]. Recently, octacalcium phosphate (OCP) has attracted increasing attention because of good osteoconductivity, biocompatibility, and biodegradability [7–11]. In particular, OCP is considered to be a better scaffold for bone regeneration in comparison to hydroxyapatite, which is almost non-absorbable, or to β-tricalcium phosphate, which is absorbed too quickly [6,7,9,12]. Thus, the physicochemical properties of OCP have been extensively investigated, with a view to enhancing its biological properties.
OCP was first suggested by Brown et al. [13,14] to be a precursor to bones and teeth. Synthetic OCP may have thin, plate-like, ribbon, strip-like, and acicular morphology, depending on the environment in which the crystals grow, pH, mode of synthesis, and presence of various inorganic ions and organic molecules [15–19]. In any case, the crystal structure of OCP is similar to that of hydroxyapatite, and includes a water and an apatite layer [20]. OCP is converted to apatite by hydrolysis, which decreases HPO42− content, and increases the Ca/P molar ratio [8,21]. Importantly, Suzuki et al. [22,23] found that synthetic OCP enhances osteoblast differentiation and osteoclast formation. Indeed, OCP enhanced bone regeneration better than insoluble unstinted hydroxyapatite or Ca-deficient hydroxyapatite, a product of OCP hydrolysis [12,24]. Moreover, OCP is more resorbable than β-tricalcium phosphate after hydrolysis, a process that may dissolve OCP in situ, and/or deposit hydroxyapatite [7].
Octacalcium phosphate carbonate (OCPC), a kind of octacalcium phosphate that contains carbonate, was first observed by Hayek et al. [16] during a reaction of CaHPO4 with CaCO3 at 37°C, in which CO32− was suggested to replace HPO42− in apatite as the reaction progressed. The final carbonate-substituted product was then considered to be much more similar to bone. Notably, Pellegrino and Biltz [25] detected OCPC during formation of renal calculi in a patient with primary hyperparathyroidism, and proposed that after dicalcium phosphate dihydrate is hydrolyzed to OCP, OCP reacts with CO32− to form OCPC. In addition, Brown et al. [26] concluded that carbonate was incorporated as OCP is hydrolyzed into hydroxyapatite. Indeed, OCP is believed to promote incorporation of impurities into hydroxyapatite [26].
The cellular response to a substrate depends on its physical and chemical characteristics, particularly crystallinity, particle size, surface structure, and chemical composition [27]. For example, formation of new bone around the typical OCP crystal was found to be higher than around a highly elongated OCP crystal [28]. In addition, Suzuki et al. [24] found that low-crystallinity OCP enhanced bone formation better than OCP or fully hydrolyzed OCP. On the other hand, carbonate apatite has been suggested to have significantly greater impact than hydroxyapatite on cell attachment, proliferation, and differentiation. Thus, incorporation of carbonate into OCP may affect its biological activity.
The physical and chemical properties of OCPC, including crystal structure, morphology, and chemical properties, have not been characterized. For instance, the osteoblast response to carbonate apatite has been investigated, but not to OCPC. OCP and hydrolyzed OCPC have also been evaluated, but not the physicochemical and biological effects of CO32− incorporation. We have now synthesized OCPC through a wet method, and characterized its morphology, crystal structure, and chemical composition. We then used MG63 cells to investigate the osteoblastic response to OCPC, OCP, and their corresponding hydrolysates, Ca-deficient carbonate apatite and Ca-deficient hydroxyapatite.
Materials and methods
Synthesis and preparation of substrates
Reagent-grade chemicals were obtained from Wako Pure Chemical Industries, Ltd. OCP was synthesized by dropwise addition of calcium acetate (250 mL, 0.04 mol, and pH 4.8) into sodium dihydrogen phosphate (250 mL, 0.03 mol, and pH 7.4) at 60°C. The resulting mixture was incubated at 60°C for another 3 hours without stirring, and the final pH was 4.9. Ca-deficient hydroxyapatite was synthesized in a similar manner, except that the mixture was stirred at 70°C for 24 hours, and the final pH was 4.5. Calcium hydrogen phosphate dihydrate, calcium carbonate, and sodium hydrogen carbonate were mixed at molar ratio 5:2:1 to prepare OCPC and Ca-deficient carbonate apatite. The aqueous suspension was stirred at 60°C for 2 hours to prepare OCPC with final pH 6.9, or for 24 hours to prepare Ca-deficient carbonate apatite with final pH 7.6. All products were washed 3 times with distilled water, split into 6 tubes, oven-dried at 60°C for 3 days, and finally ground into powder. Pellets (
Physicochemical characterization
Scanning electron microscopy, X-ray diffraction, FTIR, ICP spectroscopy
Powdered products were imaged on an S-3400NX scanning electronic microscope (Hitachi). X-ray diffraction patterns were collected at 3–45° in 0.02° steps using a Ni-filtered
Surface roughness
Pelleted products were washed with 70% ethanol in a 10 cm dish, then with MilliQ water twice, and finally dried at room temperature on a clean bench. Surface roughness was measured 50 times with pitch 0.02 using a VK-8500 laser microscope (KEYENCE). Measurements were obtained in five pellets of each product, at five different spots per pellet.
Conversion test
OCP and OCPC pellets were sterilized, dried, immersed in a 24-well plate containing αMEM (Wako) supplemented with 10% fetal bovine serum and 1% penicillin-streptomycin (Wako), and incubated at 37°C and 5% CO2. Culture media were refreshed every three days. After 11 days, pellets were quickly washed with phosphate-buffered saline and MilliQ water once each, and dried on a clean bench. X-ray diffraction patterns were then collected as described.
Cell culture
The human osteosarcoma cell line MG63 was cultured at 37°C, 95% air, and 5% CO2 in αMEM containing 10% fetal bovine serum and 1% penicillin-streptomycin. Cells were seeded at
Cell proliferation
MTT was dissolved in phosphate-buffered saline at 5 mg/mL, and mixed at 1:10 v:v with αMEM containing 10% fetal bovine serum and 1% penicillin-streptomycin. Cells seeded at
Cell differentiation
Pellets and glass sheets seeded with
Statistical analysis
MTT, alkaline phosphatase, and surface roughness data were collected from five samples of each substrate. Substrates were then compared by one-way ANOVA, with
Results
Surface characterization
Morphology
SEM images of powdered OCP, OCPC, Ca-deficient hydroxyapatite, and Ca-deficient carbonate apatite are shown in Fig. 1. Synthetic OCP powder consists of long, thin crystals (Fig. 1(a)), while synthetic OCPC powder consists of short plates and flakes (Fig. 1(c)). On the other hand, synthetic Ca-deficient hydroxyapatite is composed of aggregated needle-like crystals (Fig. 1(b)). Aggregated needle-like crystals are also observed in synthetic Ca-deficient carbonate apatite powder, along with plate-like crystals (Fig. 1(d)).

Scanning electron micrographs of OCP (a), Ca-deficient hydroxyapatite (b), OCPC (c), and Ca-deficient carbonate apatite (d) powders. Scale bars, 10 µm.
X-ray diffraction patterns collected from powdered samples of OCP (curve a), OCPC (curve b), Ca-deficient hydroxyapatite (curve c), and Ca-deficient carbonate apatite (curve d) are presented in Fig. 2. The diffraction patterns of synthetic OCP and OCPC were identical to the OCP diffraction pattern deposited with the ICDD No. 26-1056, as shown in Fig. 2(B), in which characteristic OCP diffraction peaks are marked with black arrows. However, the relative intensities of diffraction peaks were different between OCP and OCPC. On the other hand, the diffraction patterns of Ca-deficient hydroxyapatite and Ca-deficient carbonate apatite were identical to that of hydroxyapatite (ICDD No. 09-0432), although both seemed to be less crystalline.

X-ray diffraction patterns collected from powdered OCP (curve a), OCPC (curve b), Ca-deficient hydroxyapatite (curve c), and Ca-deficient carbonate apatite (curve d, A). Black arrows mark characteristic peaks of OCP/OCPC, and red arrows mark characteristic peaks of Ca-deficient hydroxyapatite/carbonate apatite. Panel (B) is a zoomed-in view of the red box in (A), encompassing
Main reflections for OCP, OCPC, Ca-deficient hydroxyapatite and Ca-deficient carbonate apatite
OCP∗: Pattern PDF 26-1056 Radiation: 1.54060 Quality: Star.
HA∗: Pattern PDF 09-0432 Radiation: 1.54060 Quality: Indexed.
CDHA: Ca-deficient hydroxyapatite.
CDCA: Ca-deficient carbonate apatite.
The key reflections that separate OCP and OCPC from their Ca-deficient hydrolysates are listed in Table 1. In particular, the intensity of peaks 010, 020, 110, and 070 in OCP and OCPC decreased as hydrolysis progressed, although these peaks were still detectable just before total hydrolysis (Fig. 2). In addition, the doublet peaks 2–21 and 002 in OCP and OCPC transformed into the single peak 002 after hydrolysis. Further, peaks 260, 2–41, and −1–42 in OCP and OCPC disappeared after hydrolysis, while peaks 211, 112, and 300 appeared in the Ca-deficient hydrolysis products (Fig. 2(B)). The lattice constants of OCP were
Lattice constants for OCP, OCPC, Ca-deficient hydroxyapatite and Ca-deficient carbonate apatite
CDHA: Ca-deficient hydroxyapatite.
CDCA: Ca-deficient carbonate apatite.

FTIR spectra of synthetic OCP (a), OCPC (b), Ca-deficient hydroxyapatite (c), and Ca-deficient carbonate apatite (d). Black frames mark vibrations due to HPO4−. Red frames mark vibrations due to CO32−, and black arrows indicate type A and type B CO32−. Blue frames mark vibrations due to OH−.
The FTIR spectra of synthetic OCP, OCPC, and their Ca-deficient hydrolysates are presented in Fig. 3, and all relevant vibrations are listed in Table 3. Characteristic bands at 912 and 1291 cm−1 are due to HPO42− (Fig. 3, black box), which were clearly observed in OCP and OCPC despite low intensity. However, the intensity of HPO42− bands was weaker in OCPC than in OCP. Additionally, bands at 1419 and 1456 cm−1, observed in OCPC and its Ca-deficient hydrolysate, are due to type B CO32− (Fig. 3, red box), while bands at 1540 cm−1 are attributed to type A CO32− (Fig. 3, red box). OH− bands at 3567 cm−1 were also observed in both Ca-deficient hydrolysates (Fig. 3, blue box). In general, spectra were comparable between OCPC and OCP, and between Ca-deficient carbonate apatite and Ca-deficient hydroxyapatite, except that OCPC and its hydrolysate contain carbonate bands. Taken together, these results indicate that OCPC contains type B carbonate within an OCP-like structure, and that Ca-deficient carbonate apatite also contains carbonate (mainly type B and some type A) in a structure that is otherwise similar to Ca-deficient hydroxyapatite.
FT–IR vibrations for OCP, OCPC, Ca-deficient hydroxyapatite and Ca-deficient carbonate apatite
FT–IR vibrations for OCP, OCPC, Ca-deficient hydroxyapatite and Ca-deficient carbonate apatite
vw, very weak; w, weak; m, medium; s, strong; sh, shoulder; b, broad.
CDHA: Ca-deficient hydroxyapatite.
CDCA: Ca-deficient carbonate apatite.
The Ca/P molar ratio in OCP, OCPC, Ca-deficient hydroxyapatite, and Ca-deficient carbonate apatite was 1.32, 1.45, 1.46, and 1.5, respectively. The Ca/P molar ratio of the OCP we synthesized is slightly lower than the theoretical ratio of 1.33. The results also confirm that the OCP/OCPC hydrolysates are calcium deficient, as the theoretical ratio in hydroxyapatite is 1.67. Sodium was not detected. The mean surface roughness ± SD of OCP, OCPC, Ca-deficient hydroxyapatite, and Ca-deficient carbonate apatite was comparable at
Cell proliferation
As shown in Fig. 4, MTT values increased from day 1 to day 6, indicating that pellets of OCP, OCPC, and their Ca-deficient hydrolysates are biocompatible, and did not negatively affect the viability and proliferation of MG63 cells. Results were comparable at day 1 and day 3, but proliferation on OCPC was significantly higher at day 6 than on any other substrate. At this time point, proliferation on Ca-deficient carbonate apatite was higher than on OCP, and also higher on OCP than on Ca-deficient hydroxyapatite (

Proliferation of MG63 cells cultured on OCP (a), OCPC (b), Ca-deficient hydroxyapatite (c), Ca-deficient carbonate apatite (d) pellets, as measured by MTT assay and using glass as control. Error bars are SD (
Cell differentiation was assessed by alkaline phosphatase activity in MG63 cells cultured for 6, 10, and 14 days on pellets of OCP, OCPC, and their Ca-deficient hydrolysates. As shown in Fig. 5, activity increased from day 6 to day 10, and decreased at day 14. At day 10, activity was higher in cultures grown on OCPC than on OCP, but not to a statistically significant extent. However, activity was significantly higher at days 6 and 10 in cells growing on OCP, OCPC, and Ca-deficient carbonate apatite than on Ca-deficient hydroxyapatite, suggesting enhanced MG63 differentiation.

Changes in alkaline phosphatase activity in MG63 cells cultured on OCP (a), OCPC (b), Ca-deficient hydroxyapatite (c), Ca-deficient carbonate apatite (d) pellets, using glass as control. Error bars represent SD (
In this study, we synthesized OCPC, examined cellular proliferation and differentiation on OCP, OCPC, and their Ca-deficient hydrolysates, and compared their physicochemical characteristics. Results (Figs 4 and 5) confirmed that carbonate incorporation into OCP/apatite should promote bone regeneration.
Synthetic OCPC formed short plate-like crystals in powder form (Fig. 1(c)), while OCP formed long, plate-like crystals (Fig. 1(a)). The difference in length is likely due to environmental conditions during synthesis. In particular, OCPC was obtained as an intermediate product during hydrolysis of dicalcium phosphate dihydrate in the presence of a small amount of NaHCO3, which changed the pH of the reaction, and thus altered the environment in which crystals grew, especially at the beginning of the reaction. Indeed, the effects of synthesis conditions on OCP morphology has been reported [29]. Notably, the OCPC crystals were similar to plate-like OCP crystals that have been previously obtained [2,8,29–31], as well as to OCPC described by Hayek [16]. Thus, we conclude that the difference in crystal length between OCPC and OCP is insignificant, and that the crystal morphologies are similar.
Accordingly, X-ray diffraction patterns suggested that the crystal structure of OCPC is similar to that of OCP. As shown in Fig. 2, there were no differences in X-ray diffraction patterns between OCP and OCPC, and between their Ca-deficient hydrolysates. However, reflections 002 and 300 shifted to lower angles in Ca-deficient carbonate apatite, in comparison to Ca-deficient hydroxyapatite. Similar shifts to lower angles from OCP to OCPC were also observed in reflections 010 and 002. These results indicate that incorporation of carbonate into OCP and Ca-deficient hydroxyapatite slightly changes the structure of the lattice. Indeed, a slight expansion of the c-axis and a contraction of the a-axis (Fig. 2) were observed in OCPC, as has been reported when PO43− is replaced with CO32− in crystals of carbonate apatite. Nevertheless, we consider the observed changes in lattice constants to be negligible.
These changes were also detectable by FTIR, through which carbonate bands were observed both in OCPC and its hydrolysate Ca-deficient carbonate apatite (Fig. 3), although absorbance bands at 1419, 1456, and 1540 cm−1 indicate that some HPO42− had been retained (Fig. 3, curve b). In hydroxyapatite, carbonate substitutions are classified as type A (CO32− for PO43−) or type B (CO32− for OH−), which are observed at 1450 and 1540 cm−1 and at 1420 and 1460 cm−1, respectively. As OCP contains apatite and water layers, the results indicate that carbonate may substitute for HPO42− in the water layer or for PO43− in the apatite layer, thereby generating OCPC. Notably, the FTIR spectra of Ca-deficient carbonate apatite (Fig. 3, curve d) contains a carbonate absorbance band at 1540 cm−1 that is more definitive than that of OCPC, as well as an OH− absorbance band less definitive than that of Ca-deficient hydroxyapatite. A similar phenomenon in carbonate apatite has led to the notion of a type AB substitution, in which carbonate substitutions occur not only at PO43− sites but also at OH− sites [32]. Hence, the results indicate that we have successfully synthesized a carbonate-substituted OCPC, as well as a Ca-deficient carbonate apatite with type AB substitutions.
The Ca/P molar ratio of synthetic OCP was 1.32, which is very close to the theoretical ratio of 1.33. Thus, we appear to have obtained a nearly stoichiometric OCP. Similarly, LeGeros et al. [33] synthesized OCP via precipitation, and obtained material with Ca/P molar ratio from 1.325 to
Notably, OCPC enhanced osteoblast proliferation (Fig. 4) and differentiation (Fig. 5) in vitro, in comparison to all other substrates, and especially at day 6. Accordingly, Ca-deficient carbonate apatite was significantly more effective at stimulating cell proliferation than Ca-deficient hydroxyapatite (Fig. 4). Alkaline phosphatase activity was also higher in Ca-deficient carbonate apatite than in Ca-deficient hydroxyapatite, but was comparable between OCPC and OCP at day 6 and 10 (Fig. 5). Notably, cell proliferation is sensitive to surface roughness [36,37]. However, surface roughness was comparable among all materials tested, and surface morphology was comparable between materials with (OCPC and hydrolysate, Fig. 1, curves d and h) or without carbonate (OCP and hydrolysate, Fig. 1, curves b and f). Thus, differences in cell proliferation cannot be attributed to differences in crystal structure, surface roughness, and morphology, but perhaps to differences in chemical composition. For example, incorporation of magnesium and strontium into OCP increased cell proliferation and differentiation, and enhanced ALP activity [38], while carbonate apatite promote osteoblastic differentiation, and enhanced ALP activity earlier than sintered hydroxyapatite [39]. Indeed, various theories have been proposed to explain how carbonate may improve osteoconductivity. For instance, carbonate may increase solubility [40], enhance protein adsorption and early cell attachment [41], or upregulate bone-related genes such as collagen and osteocalcin. In addition, incorporation of CO32− increases the ratio of calcium to phosphate, and thereby regulate osteoblast activity and bone formation [42,43]. Collectively, these observations indicate that carbonate apatite may stimulate bone growth [44]. However, further studies in vivo are necessary to test this hypothesis.
We note that OCPC may transform into Ca-deficient carbonate apatite during synthesis, given that OCP also tends to convert into apatite both in vitro and in vivo [8,45–47]. However, OCPC and OCP immersed in culture media did not appear to convert. This may be due to (1) in situ hydrolysis of OCP into hydroxyapatite, and/or (2) dissolution of OCP, followed by hydroxyapatite precipitation and formation of new bone, as observed in vivo [46–49].
Further, we note that physiological apatite is an ion-substituted nonstoichiometric form of hydroxyapatite, and contains 4–8 wt% carbonate ions. Nevertheless, hydroxyapatite has been widely used in the clinic as bone substitute, and the osteoconductivity and biocompatibility of carbonate apatite have also been investigated. Similarly, OCP has been shown to possess good osteoconductivity and biodegradability, and is thought to be a precursor of mineral crystals in bone and tooth [50]. Based on all data, we anticipate that OCPC will also become a bone substitute to treat bone defects.
Conclusions
We have demonstrated that carbonate incorporation into OCP/apatite may promote bone regeneration. In particular, results indicate that carbonate is not only incorporated into apatite, but is also incorporated into OCP to form the intermediate product OCPC, which enhances osteoblastic proliferation and differentiation in vitro. These studies may help elucidate the effect of carbonates incorporated into OCP/apatite, as well as characterize OCPC as bone substitute.
Footnotes
Acknowledgements
We acknowledge generous assistance from all teachers and students at Department of Inorganic Biomaterials and Department of Pediatric Dentistry at Tokyo Medical and Dental University.
Conflict of interest
The authors have no conflict of interest to report.
