Nicole L.
Morozowich‡
,
Jordan O.
Lerach‡
,
Tomasz
Modzelewski‡
,
Lauren
Jackson
,
Nicholas
Winograd
* and
Harry R.
Allcock
*
The Pennsylvania State University, Department of Chemistry, University Park, PA 16802, USA. E-mail: hra@chem.psu.edu; nxw@psu.edu
First published on 15th April 2014
Synthetic bone grafts that promote the natural mineralization process are excellent candidates for the repair and replacement of bone defects. In this study, a series of phosphoester and phosphonic acid containing polyphosphazenes were examined for their ability to mineralize hydroxyapatite (HAp) during exposure to a solution of simulated body fluid (SBF) for a period of four weeks. Although all the polymers showed an initial mineralization response, the amount of deposition and the time scale were dependent upon the side group chemistry of the polymers. After exposure to SBF for one week, all polymers mineralized HAp. After three weeks in SBF, polymers containing phosphoester substituents showed no significant change, with a weight gain of <1%, while polymers containing phosphonic acid substituents underwent a significant increase in the amount of mineralized HAp, with weight gains between 5–10%. The morphology of mineralized features was observed with Environmental Scanning Electron Microscopy (ESEM). However, due to the structural complexity of the mineralized polymers, the identity of the mineralized phase could not be definitively identified using traditional characterization techniques such as energy dispersive spectroscopy (EDS), X-ray diffraction (XRD), Fourier-transform infrared spectroscopy (FTIR), or X-ray photoelectron spectroscopy (XPS). Time-of-flight secondary ion mass spectrometry (ToF-SIMS), a technique not previously explored for this type of application, successfully reveals details of the chemistry associated with the mineralized phase not possible to achieve with XRD analysis.
Several synthetic and natural polymers have been investigated for this application, including poly(lactic-co-glycolic acid) (PLGA),4 poly(L-lactic acid) (PLA),4–6 polycaprolactone (PCL),4,7,8 bacterial cellulose,9 chitosan,10,11 and silk.12 While many of these polymers show promising results, there are still a number of limitations preventing their use as implantable scaffolds. One of the main limitations is their lack of osteoinductive properties. Methods have been developed to improve these properties by means of incorporating growth factors13 or other additives, such as autographic fillers and hydroxyapatite (Ca10(PO4)6(OH)2), into the polymer matrix by a physical mixing of the two components.14–18 The incorporation of hydroxyapatite allows the materials to better mimic the chemical and physical properties of natural bone, as it comprises nearly 70 wt% of dry bone. Although the osteoinductive properties of these materials are enhanced, the mechanical properties suffer due to poor dispersion of the particles in the bulk polymer.14,19
One alternative to the use of particulate hydroxyapatite fillers to improve the osteoinductive properties of a material is to coat the sample with calcium phosphates, or to functionalize polymers with acidic (negatively charged) substituents to allow them to coordinate calcium and phosphate ions, thus promoting the mineralization of hydroxyapatite.3,20,21 Many different types of polymers have been investigated for their ability to mineralize hydroxyapatite (HAp) using this method, and in most cases some type of biological apatite was deposited on the surface.8,9,22 Studies have shown that these polymer scaffolds coated with hydroxyapatite had improved osteoinduction in vivo.23,24 Moreover, these functional polymers should have better mechanical properties because of their ability to chemically bond to the hydroxyapatite.25,26
Traditional techniques used to characterize the mineralized phase rely heavily on scanning electron microscopy (SEM) coupled with energy dispersive spectroscopy (EDS), X-ray diffraction (XRD), and Fourier transform infrared spectroscopy (FTIR).5,8,27 X-ray photoelectron spectroscopy (XPS) is also used but to a much lesser extent.28 These techniques may be suitable for proper characterization of most polymer systems; however more complex systems may require alternative characterization methods, especially when the sample size is small and/or more than one phase is present on the sample.
An alternative analytical tool that is utilized to study such complex polymer systems is time-of-flight secondary ion mass spectrometry (ToF-SIMS). ToF-SIMS can provide excellent sensitivity, detecting attomolar concentrations for a variety of analytes,29 as well as having the ability to generate chemical images of a surface with submicron spatial resolution. Chemical imaging capabilities can yield the location of specific analytes within a system. This is particularly advantageous in a situation where complementary ESEM images can be correlated. By collecting ToF-SIMS spectra over the same 2D array, the accurate location of specific features can be determined with chemical specificity. ToF-SIMS has been utilized previously for exceedingly complex systems, such as differentiation between multiple biologically-relevant apatite phases,30 and for the chemical imaging of eukaryotic cells.31,32 Furthermore, advancements in primary ion sources, specifically the shift towards cluster ions, such as C60+, allows researchers to investigate a multitude of sample varieties including both polymeric33,34 and inorganic35,36 substances, whereas, some atomic sources have proven much less effective.37–39
Recently, a number of polyphosphazene-based polymers have been developed and evaluated for their potential use in tissue engineering applications. Polyphosphazenes are tunable inorganic–organic hybrid polymers consisting of a backbone of alternating nitrogen and phosphorus atoms, with each phosphorus atom bearing two organic side groups.40,41 The synthetic flexibility of this system has provided access to biocompatible and biodegradable polymers that show good osteocompatibility42,43 both in vitro44,45 and in vivo,44–46 with little acute inflammatory response47 and mineral deposition.27 More recently, a number of phosphonic acid containing polyphosphazenes have been synthesized and characterized48 in order to generate bioactive polymers capable of inducing in situ hydroxyapatite mineralization. In this work, their ability to mineralize hydroxyapatite from a simulated body fluid (SBF) solution was examined. The use of SBF to predict the in vivo bioactivity of a material has been well-established in the literature.49
Due to the complex nature of the mineralized polymers, their chemical composition was characterized by ToF-SIMS and morphologically by ESEM. As a means to confirm the presence of HAp detected by ToF-SIMS, XRD was used. To provide a unique and thorough characterization using ToF-SIMS, complete phase identification and relative quantification of HAp was accomplished using a QSTAR® XL ToF-MS which possesses both high mass accuracy and high mass resolution, while 2D chemical images that show distinct HAp localization were obtained on a Bio-ToF MS. With C60+ primary ion bombardment a number of characteristic and non-coincidental ions from HAp and the polymer are observed. Utilizing these ions as a marker, the location of HAp can be determined with chemical specificity, and in the case of the relative quantitation scheme, a relative amount of HAp within a sample. The identities of the HAp ions are confirmed with high mass resolution measurements and with MS/MS analyses. The information obtained identifies HAp features and the relative amounts on the surface of the samples.
When compared to the as-prepared clean sample which was not exposed to SBF, all of the polymers showed evidence of small inorganic crystalline deposits after 1 and 2 week exposure to SBF, as detected by ESEM and shown in Fig. 2, with all samples showing a heterogeneous distribution of particles along their surface. These samples were further analyzed using EDS. Calcium and phosphorus signatures were found for all mineralized samples using EDS, indicating that some type of apatite was present (Fig. 3A). However, the specific apatite phase was not determined by the Ca/P ratio due to the presence of phosphorus in the polyphosphazene backbone. Based on the tendency of dissolved phosphate ions to mineralize HAp because of their high chemical affinity for calcium ions,50,51 coupled with HAp being the most thermodynamically stable phase precipitated from SBF under the conditions used,52 HAp is the most likely candidate.
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Fig. 2 ESEM images of polymer samples before mineralization (clean PEA film shown as a representative of all polymers), and after 2 and 4 weeks exposure to simulate body fluid (SBF). |
After 3 and 4 weeks in SBF, PEA and PEPA underwent no significant changes from the results at weeks 1 and 2. However, PAA and PAPA showed a strikingly different behavior, with 3 morphologies of mineral deposits detected on their surfaces. The first deposit type was the same as those observed at weeks 1 and 2, with small inorganic deposits distributed homogeneously on the surface. The second and third were clusters of inorganic deposits distributed heterogeneously across the surface, with one cluster type possessing an irregular shape and the other exhibiting a globular morphology. Using EDS, both clusters were found to be apatite phases showing intense calcium signatures, and were probably the same phase, but in two different morphologies. The morphology of both the globular clusters22,27,53 and the irregularly-shaped clusters7,54 have been identified as HAp in previous literature reports. This behavior was not found for PEA and PEPA, which is a direct result of the difference in side group chemistry, shown in Fig. 1. Because the mineralization process begins with the initial binding of calcium ions to the free phosphonic acid groups, the availability of these groups to the SBF solution becomes the limiting factor, and ultimately determines the mineralization behaviors.3,53 Based on this, PAA and PAPA which contain phosphonic acid substituents with six P-OH groups per site available for calcium binding, should perform better than PEA and PEPA which contain phosphoester derivatives that contain only two free P-OH groups per site available for calcium binding. An increase in the number of P-OH linkages increases the number of binding modes available to calcium, thus increasing the probability of mineralization. This hypothesis is supported by the weight gain data provided in the following section. The presence of HAp was later confirmed by ToF-SIMS and XRD. To date, this is the first reported, fully characterized polyphosphazene that mineralized HAp from SBF.
With C60+ primary ion bombardment, a large number of characteristic, non-coincidental ions from HAp and the polymer are detected from the collected spectra. This diversity in ion identity allows for the differentiation of HAp ions due to any number of characteristic ions that cannot be generated from the polymeric species. The ion identities were compared to HAp reference material and ions [CaO]+, [Ca2O]+, [Ca2O2]+, [Ca2PO3]+, [Ca2PO4]+, [Ca3PO5]+, and [Ca4PO6]+ well represent the HAp moiety. Also, polymeric samples which had no exposure to SBF yielded characteristic ions of [C7H7]+ and [C6H5]+ due to fragmentation of the functionalized polymer side-groups. Furthermore, identification is aided by utilizing instrumentation which possess high mass accuracy and tandem MS capabilities (Fig. 6). It should be noted that polydimethylsiloxane (PDMS) was also detected at the surface of all polymers. The most intense ions in the polymer spectra at m/z 73 and 147 are due to PDMS contamination. In light of this information the characteristic ions chosen to represent the polyphosphazenes and HAp phase are non-isobaric with the PDMS ions. It was found that solvent washes in hexanes diminish the PDMS signal from the polymer surface (ESI†). Given the current capabilities of ToF-SIMS instruments, chemical images can be created using mass spectra obtained at various points across a sample, allowing for the generation of a 2D representation of the distribution of analytes on a sample (Fig. 5). Also, by examining the relative ion signal strength among a group of samples, the amount of HAp present at each time point may be relatively quantified (Fig. 7).
Imaging work was performed on a Bio-ToF mass spectrometer.55 Control spectra for HAp and of the unexposed polymers were analyzed and compared to identify unique, abundant ions for both species.
PAA and PAPA were examined first since they showed evidence for the most apatite deposition by ESEM and weight gain analyses. Spectra were obtained for PAA and PAPA after mineralization in SBF for 1, 2, 3, and 4 weeks. Before ToF-SIMS imaging analysis, the mineralized samples were mapped using ESEM due to the heterogeneous deposition of HAp. By imaging the entire sample with ESEM, the HAp regions were identified, and then samples with abundant HAp localization were subsequently transferred to the mass spectrometer. Analysis of the pre-mapped ESEM samples allowed a comparison of the ToF-SIMS images with the ESEM images, to allow chemical identification of coincidental features. The HAp had characteristic peaks at m/z 56, 96, 112, 159, 175, 231, and 287 which were assigned as [CaO]+, [Ca2O]+, [Ca2O2]+, [Ca2PO3]+, [Ca2PO4]+, [Ca3PO5]+, and [Ca4PO6]+ respectively. The polymer had unique ions at m/z 77 and 91 which are indicative of the [C6H5]+ and [C7H7]+ ions. These unique identifiers allow characterization of complex samples.
After analysis, the intensities of the ions listed for HAp and the polymer were utilized to generate 2D chemical images. Mass spectra were collected over a 2008 × 2008 μm2 field-of-view (FOV) for PAA and PAPA at before and after exposure to SBF for 2 and 4 weeks, where the peaks previously mentioned were used to create the 2D images. The integrated intensity for the mass spectra at each pixel in a 256 × 256 array was summed together for each respective ion, then the intensities were summed together for each pixel. The 2D chemical image for PAA showing the HAp signal as yellow pixels and polymer in purple is compared to the same area analyzed by ESEM in Fig. 5. The figure clearly shows localization of the HAp signal to the surface features on the polymer in the ESEM images. Analysis of other polymer samples shows no distinguishable surface features after 1 and 2 weeks of SBF exposure. However, in samples with 3 to 4 weeks of SBF exposure surface features were observed. This localization is believed to be a consequence of the PDMS detected which would have changed the surface chemistry based on the local PDMS content, allowing only portions of the sample to effectively interact with the SBF and coordinate the necessary ions to allow for the growth of HAp on the surface.
Confirmatory results which differentiate HAp signal from the polymer signal are shown in Fig. 6. In this figure mass spectra from regions of interest of the provided SIMS image (Fig. 5 bottom) of PAA week 3 are exhibited. In Fig. 6 (bottom) characteristic mass regions of the HAp feature are plotted along with HAp reference material. In Fig. 6 (top) exposed polymer regions are plotted with PAA reference before and after hexane washes, which show an increase in the characteristic [C7H7]+ and [C6H5]+ fragments. Full spectra and highlighted regions of interest are provided in the supporting materials. From these spectra the ion signatures from each region uniquely identify HAp compared to polymeric regions allowing for differentiation based on ion signatures.
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Fig. 6 Select polymer region compared to PAA reference and PAA reference after triplicate hexane washes (top). Select regions of mass spectra from regions of interest from PAA week 3 for HAp feature as compared to HAp reference (bottom). Characteristic ions are observed in the respective spectra. Complete spectra and region of interest are presented in ESI.† |
As shown in Fig. 6, there is a direct overlap between the HAp phase detected by ToF-SIMS and the surface features observed by ESEM. The areas of high electron density in the ESEM images correlate in the ToF-SIMS image to HAp (yellow). The chemical image provided for polymer PAA at week 3 provides clear evidence for HAp mineralization. However, identification of HAp after 1 and 2 weeks mineralization in SBF for polymers PAA and PAPA was not possible using the Bio-ToF due to low or no HAp signal detected.
The signal to noise ratio for the ToF-SIMS spectra obtained for PAA and PAPA after 1 and 2 weeks of SBF treatment was not sufficient to distinguish background from small quantities of HAp. To overcome this limitation the samples were analyzed using a QSTAR® XL triple quadrupole ToF-MS modified with a 20 keV C60+ primary ion source to enable SIMS analysis. This system possesses higher mass accuracy (10 ppm) and mass resolution (m/Δm > 12000) than the Bio-ToF instrument albeit with less reliable imaging capabilities. Empirical masses were compared to their calculated exact mass values and their subsequent assignments verified.
Because the exact masses of several ions that relate to HAp were identified and separated from interfering signals, a relative quantitation study was performed to determine the amount of HAp deposition as a function of exposure to SBF. The abundance of several HAp ions were compared and all were found to increase in intensity during the exposure time to SBF.
Relative quantitation data are shown in Fig. 7 for the [Ca2O2]+, [Ca2PO3]+, [Ca2PO4]+ and [Ca4PO6]+ ions. The overall trend is toward an increase in HAp signal compared to each individual group. These results support the weight gain data (Fig. 4), which showed a progressive increase in the weight of the samples with increasing exposure time to SBF. It also supports the data presented in Fig. 2, where PAA and PAPA mineralized significantly more HAp than PEA and PEPA.
The magnitude of the standard deviation is not surprising considering the heterogeneous deposition of HAp on the polymer surface, as shown by SIMS and ESEM imaging. Also, SIMS relative quantitation can be accomplished more readily on samples with a lower surface roughness56 than that observed for the mineralized samples. Despite this, an increase in the HAp signal as a function of SBF exposure time for each polymer was clearly established. In some instances, the specific ion signal was detected before SBF exposure, but was attributed to be background noise.
XRD patterns of polymers PAA and PAPA were also obtained before and after mineralization. Before mineralization, both polymers contained two predominant amorphous peaks centered at 2θ = 6.87° and 19.26°. After incubation in SBF for 1 and 2 weeks, the XRD patterns did not change, even though mineralized deposits were detected on their surface by ESEM. However, after incubation in SBF for 3 and 4 weeks, a new peak appeared at 2θ = 31.7°, as shown in Fig. 3B. The reflection at 31.7° (211) is characteristic of the strongest reflection from hydroxyapatite [HAp, Ca10(PO4)6(OH)2, FIZ 97849, major 2θ = 31.7° (211 hkl), 32.2° (112 hkl), and 32.9° (300 hkl)]. Like many examples in the literature, the 2θ peaks for nucleated HAp are broad.6–8,22 For example, the three intense peaks for HAp listed above usually appear as one broad peak, centered at 31.7°, representing nano-crystalline HAp.57
High Mass Resolution and Accuracy ToF-MS and Relative Quantitation with QSTAR® XL ToF-SIMS Instrument. The QSTAR® XL (Applied Biosystems/MDS Sciex) was modified in-house to incorporate a 20 keV C60+ source (Ionoptika Ltd.) for SIMS analysis.62,63 The QSTAR® XL system is a tandem quadrupole orthogonal time-of-flight mass spectrometer. For all aforementioned samples, an approximately 15 pA current beam of C60+ was produced by a 20 keV Ionoptika C60+ source operated in direct current mode. The relative quantitation scheme was adapted from previously reported research56 and briefly described here, as used on the QSTAR®XL system. While collecting each surface spectrum, the sample stage was rastered continuously across the surface of the samples in 10 μm steps. The samples used for analysis each had a surface area of approximately 5 × 5 mm2. Three trials for each polymer at each time point were collected. For each trial, 180 successive scans were collected by multi-channel acquisition, thus, all aforementioned scans are summed in a running total of intensities from the first to the last scan. Each multi-channel acquisition scan lasted 0.33 seconds. Peak assignments are determined with <10 ppm accuracy. The average intensity and the standard deviation of the three trials per sample are calculated to enable a more accurate and precise measurement of the yield of the ions of interest from each sample.
Footnotes |
† Electronic supplementary information (ESI) available: Characterization data and hydrolysis profiles for all polymers examined along with ToF-SIMS quantification data for the mineralized polymers. See DOI: 10.1039/c3ra47205a |
‡ These authors contributed equally to this manuscript. |
This journal is © The Royal Society of Chemistry 2014 |