<?xml version="1.0" encoding="UTF-8"?><!DOCTYPE article  PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd"><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" dtd-version="3.0" xml:lang="en" article-type="research article"><front><journal-meta><journal-id journal-id-type="publisher-id">JBiSE</journal-id><journal-title-group><journal-title>Journal of Biomedical Science and Engineering</journal-title></journal-title-group><issn pub-type="epub">1937-6871</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/jbise.2013.63032</article-id><article-id pub-id-type="publisher-id">JBiSE-28643</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Biomedical&amp;Life Sciences</subject></subj-group></article-categories><title-group><article-title>
 
 
  Sol-gel bioceramic material from bentonite clay
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>nobong</surname><given-names>R. Essien</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Luqman</surname><given-names>A. Adams</given-names></name><xref ref-type="aff" rid="aff2"><sup>2</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Rafiu</surname><given-names>O. Shaibu</given-names></name><xref ref-type="aff" rid="aff2"><sup>2</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Aderemi</surname><given-names>Oki</given-names></name><xref ref-type="aff" rid="aff3"><sup>3</sup></xref></contrib></contrib-group><aff id="aff2"><addr-line>Department of Chemistry, Faculty of Science, University of Lagos, Lagos, Nigeria</addr-line></aff><aff id="aff3"><addr-line>Department of Chemistry, Prairie View A &amp;amp; M University, Prairie View, USA</addr-line></aff><aff id="aff1"><addr-line>Department of Chemical Sciences, Bells University of Technology, Ota, Nigeria</addr-line></aff><author-notes><corresp id="cor1">* E-mail:<email>ladams@unilag.edu.ng(LAA)</email>;</corresp></author-notes><pub-date pub-type="epub"><day>12</day><month>03</month><year>2013</year></pub-date><volume>06</volume><issue>03</issue><fpage>258</fpage><lpage>264</lpage><history><date date-type="received"><day>20</day>	<month>December</month>	<year>2012</year></date><date date-type="rev-recd"><day>5</day>	<month>January</month>	<year>2013</year>	</date><date date-type="accepted"><day>15</day>	<month>January</month>	<year>2013</year></date></history><permissions><copyright-statement>&#169; Copyright  2014 by authors and Scientific Research Publishing Inc. </copyright-statement><copyright-year>2014</copyright-year><license><license-p>This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/</license-p></license></permissions><abstract><p>
 
 
   Bioceramic material of the quaternary system; SiO<sub>2</sub>- CaO-Na<sub>2</sub>O-P<sub>2</sub>O<sub>5</sub> that has composition similar to Bio- glass<sup>?</sup> 45S5 was prepared by the sol-gel method from locally obtained bentonite clay (BTC). The monolith obtained was sintered at 1000?C for 2 h to facilitate densification and phase transformation. X-ray diffraction (XRD) analysis revealed the presence of sodium calcium silicate, Na<sub>2</sub>Ca<sub>2</sub>Si<sub>3</sub>O<sub>9</sub> as major crystal phase, and another secondary orthorhombic phase, NaCaPO<sub>4</sub>. Fourier transform infrared (FTIR) spectroscopic investigation confirmed the presence of Si-O-Si bonds and a crystalline phosphate in the glass network. Scanning electron microscopy (SEM) revealed a network of micropores and interconnected macropores. Overall, the material displays features amenable for possible utilization in tissue engineering scaffolds. 
 
</p></abstract><kwd-group><kwd>Bioceramic; Sol-Gel; Monolith; Bentonite Clay; Silica</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. INTRODUCTION</title><p>The number of patients requiring and receiving biomedical implants to correct defects and heal diseases of the skeletal system is constantly increasing [<xref ref-type="bibr" rid="scirp.28643-ref1">1</xref>]. Tissue engineering and regenerative medicine assist with restoration of damaged tissues using both functional cells and biodegradable scaffolds made from engineered biomaterials [2,3]. Significant efforts in the last decades have been devoted to the fabrication of porous and highly interconnected bioceramic scaffolds based on hydroxyapatite (HA), tricalcium phosphate and related composite materials for application in bone tissue engineering [4-6].</p><p>In this regard, Bioglass<sup>&#174;</sup> 45S5 characterised with high amounts of Na<sub>2</sub>O and CaO, and relatively high CaO/P<sub>2</sub>O<sub>5</sub> ratio [<xref ref-type="bibr" rid="scirp.28643-ref7">7</xref>] has shown capacity to induce favourable intracellular and extracellular responses promoting rapid bone formation [8-11] through formation of a hydroxycarbonate apatite (HCA) layer.</p><p>The major approaches to processing bioactive glass materials include; the melting and the sol-gel methods. The melting method utilizes high temperature in the range of 1300˚C - 1400˚C, while a major advantage of the sol-gel method is the much lower processing temperature, coupled with the ability to control the compositional range of the glass [<xref ref-type="bibr" rid="scirp.28643-ref6">6</xref>].</p><p>A major limitation of bioactive glasses, especially in the porous form is that they display low mechanical properties compared to cortical and cancellous bone [12,13], thus restricting their wide range of applications.</p><p>Some previous efforts [14,15] have shown that when sintered under optimal conditions, sodium containing bioglass attains nearly full densification and produces fine crystals of Na<sub>2</sub>Ca<sub>2</sub>Si<sub>3</sub>O<sub>9</sub> having high bioactivity index [<xref ref-type="bibr" rid="scirp.28643-ref16">16</xref>] to give scaffolds with competent mechanical strength.</p><p>The serious challenge to the large scale preparation of bioactive glasses and glass-ceramic materials is the high cost of the widely used alkoxide precursors such as; tetraethyl orthosilicate (TEOS) and tetramethyl orthosilicate (TMOS) [17-20]. Consequently, some authors like Nayak et al. [<xref ref-type="bibr" rid="scirp.28643-ref21">21</xref>], Wu et al. [<xref ref-type="bibr" rid="scirp.28643-ref22">22</xref>] and Zanotto et al. [<xref ref-type="bibr" rid="scirp.28643-ref23">23</xref>] have explored alternative silica sources in their pathway to large scale bioactive glasses.</p><p>Clay minerals are fine grained hydrous silicates of octahedral or tetrahedral layered arrangement. Their chemical composition implies that they may yet serve as an economically viable non-toxic silica source for large scale synthesis of bioactive glasses.</p><p>Bentonite clay; (Na,Ca)(Al,Mg)<sub>6</sub>(Si<sub>4</sub>O<sub>10</sub>)<sub>3</sub>(OH)<sub>6</sub>∙nH<sub>2</sub>O formed from the weathering of volcanic ash is naturally occurring sedimentary clay with the 3-layered clay structure. It displays one aluminium oxide sheet sandwiched by two silicon oxide sheets <xref ref-type="fig" rid="fig1">Figure 1</xref> [<xref ref-type="bibr" rid="scirp.28643-ref24">24</xref>]. Structurally, the internal aluminium and external silicon oxide sheet share oxygen atoms, while Mg<sup>2+</sup> ions often substitute for Al<sup>3+</sup> ions resulting in net negative charge [<xref ref-type="bibr" rid="scirp.28643-ref25">25</xref>]. The charge in the platelet is balanced by counter ions, usually</p><p>Na<sup>+</sup> and Ca<sup>2+</sup> located between the platelets. Clay has a wide origin and is particularly cheap and widely available in Nigeria [<xref ref-type="bibr" rid="scirp.28643-ref26">26</xref>]. The silicon oxide layer can be extracted using alkali at elevated temperature to give the corresponding alkali silicate as possible precursor for glass synthesis.</p><p>In this research work, we focus on the use of sodium bentonite as a source of silica to prepare sodium containing bioceramic material similar in composition to Bioglass<sup>&#174;</sup> 45S5 quaternary system via the sol-gel process. To the best of our knowledge the use of bentonite clay as a precursor for this type of bioceramic has not been previously reported in literature.</p></sec><sec id="s2"><title>2. MATERIALS AND EXPERIMENTAL PROCEDURES</title><sec id="s2_1"><title>2.1. Materials</title><p>The following chemicals were used as obtained for the preparation of the bioceramic material; bentonite clay- (OH)<sub>4</sub>Si<sub>8</sub>Al<sub>4</sub>O<sub>20</sub>∙nH<sub>2</sub>O (obtained locally), nitric acid (Fluka, Germany), phosphorus pentoxide (BDH Laboratory, 98%), sodium nitrate (Sigma-Aldrich, 99%), and calcium nitrate tetrahydrate (LOBA, 98%).</p></sec><sec id="s2_2"><title>2.2. Experimental Procedures</title><p>The bioceramic material with composition (wt%); 45 SiO<sub>2</sub>, 24.5 Na<sub>2</sub>O, 24.5 CaO, 6 P<sub>2</sub>O<sub>5</sub> was prepared through the sol-gel process using bentonite clay as precursor. According to the extraction procedure reported by Essien et al. [<xref ref-type="bibr" rid="scirp.28643-ref26">26</xref>], a mixture of bentonite clay (13.33 g) in 1 M NaOH (250.00 ml) was heated at 120˚C for 2 hours under reflux in a round bottom flask. The filtrate obtained was slowly evaporated to dryness at 130˚C to obtain sodium metasilicate (Na<sub>2</sub>SiO<sub>3</sub>). In a typical gel-derived procedure for preparing Bioglass<sup>&#174;</sup> 45S5 [<xref ref-type="bibr" rid="scirp.28643-ref15">15</xref>], Na<sub>2</sub>SiO<sub>3</sub> (9.00 g) was dissolved in deionised water (15.00 ml) to give a solution that was then added slowly to 1 M HNO<sub>3</sub> (15.50 ml) in a beaker furnished with a magnetic stirrer under ambient temperature for 1 hour to facilitate complete hydrolysis. Thereafter, P<sub>2</sub>O<sub>5</sub> (0.59 g), NaNO<sub>3</sub> (0.37 g) and Ca(NO<sub>3</sub>)<sub>2</sub>∙4H<sub>2</sub>O (10.16 g) were added respectively under constant stirring. Each of those three reagents was allowed 45 minutes to react. After complete addition, the mixture was further stirred for additional 1 h to afford a gel. The resulting gel was aged at room temperature for 5 days, dried at 60˚C, 200˚C, and 600˚C for 72, 40 and 5 hours respectively, followed by sintering at 800˚C for 3 hours and 1000˚C for 2 hours.</p></sec><sec id="s2_3"><title>2.3. Methods of Characterization</title><p>Atomic absorption spectroscopy (AAS) Perkin Elmer A Analyst 200 was used to determine elemental composition of the finally sintered material. Further evaluation was by X-ray diffraction (XRD, X’pert PRO PANalytical) using CuKα radiation (0.154060) source operated at 40 kV and 40 mA. The diffraction patterns were obtained in the 2θ range from 5˚ - 120˚. The morphology of the material was investigated using scanning electron microscopy (SEM, EVO/MAIO). The sample was carboncoated and observed at an accelerating voltage of 10 kV. Fourier transform infrared (FTIR, Perkin Elmer Spectrum X), with the wavenumber range of 4000 - 400 cm<sup>−</sup><sup>1</sup> employing KBr pellets operating in a reflectance mode with a 4 cm<sup>−</sup><sup>1</sup> resolution was used to monitor the nature of bonds present in the glass network.</p></sec></sec><sec id="s3"><title>3. RESULTS AND DISCUSSION</title><sec id="s3_1"><title>3.1. Composition of the Porous BTC-Derived Bioglass Material</title><p>Bentonite clay of the type (OH)<sub>4</sub>Si<sub>8</sub>Al<sub>4</sub>O<sub>20</sub>∙nH<sub>2</sub>O shown in <xref ref-type="fig" rid="fig2">Figure 2</xref>(a) was reacted in strong basic medium to initially afford sodium metasilicate (reaction equation is shown elsewhere [<xref ref-type="bibr" rid="scirp.28643-ref26">26</xref>]) after evaporating the alkaline filtrate slowly to dryness at 120˚C. The waterglass obtained, <xref ref-type="fig" rid="fig2">Figure 2</xref>(b), from this reaction is hydrolysed under acidic conditions to silicic acid which undergoes condensation to disilicic acid and further reaction to a polycondensed hydrogel [26,27]. The elemental composition of the bioceramic material was adjusted to give a ratio similar to Bioglass<sup>&#174;</sup> 45S5 by varying the amount of the following reagents; P<sub>2</sub>O<sub>5</sub>, NaNO<sub>3</sub> and Ca(NO<sub>3</sub>)<sub>2</sub>∙4H<sub>2</sub>O.</p><p>The monolith obtained is shown in <xref ref-type="fig" rid="fig2">Figure 2</xref>(c). The weight percentage analysis by AAS of the monolith was confirmed as; (wt%) 45 SiO<sub>2</sub>, 24.5 Na<sub>2</sub>O, 24.5 CaO, 6 P<sub>2</sub>O<sub>5</sub>.</p></sec><sec id="s3_2"><title>3.2. FTIR Characterisation of the Bioceramic Monolith Similar to Bioglass<sup>&#174;</sup> 45S5</title><p>The FTIR spectrum of the BTC-derived bioglass monolith material is shown in <xref ref-type="fig" rid="fig3">Figure 3</xref>. It is characterised by a very broad OH<sup> </sup>absorption band centred around 3424 cm<sup>−</sup><sup>1</sup> and a weak absorbed water band at 1650 cm<sup>−</sup><sup>1</sup> [<xref ref-type="bibr" rid="scirp.28643-ref28">28</xref>]. Two other absorptions bands observed at 905 and 1011 cm<sup>−</sup><sup>1</sup> correspond to asymmetric Si-O-Si stretching vibration of silanol groups [29,30]. The peak centred at 565 cm<sup>−</sup><sup>1</sup> can be attributed to the P-O bond in crystalline phosphates [<xref ref-type="bibr" rid="scirp.28643-ref31">31</xref>]. Similarly, the weak peak at 1212 cm<sup>−</sup><sup>1</sup> is attributed to the characteristic vibration of P=O bonds. Furthermore, the broad band centred at 1440 cm<sup>−</sup><sup>1</sup> is diagnostic of the vibrations of non-bridging PO<sub>2</sub> in <img src="3-9101591\18c70c24-d1dc-4ce7-a83f-063f94a3bec7.jpg" /> groups or <img src="3-9101591\ef49dcc1-3cad-4a3b-948c-cdbe32265601.jpg" /> originated from air during the sol-gel fabrication [<xref ref-type="bibr" rid="scirp.28643-ref32">32</xref>]. The vibrational modes obtained for the bioceramic monolith compare with those of biomorphic 45S5 bioglass scaffold [<xref ref-type="bibr" rid="scirp.28643-ref32">32</xref>].</p></sec><sec id="s3_3"><title>3.3. XRD Characterisation of the Bioceramic Monolith Similar to Bioglass<sup>&#174;</sup> 45S5</title><p>XRD pattern of the BTC-derived bioceramic sintered at 1000˚C for 2 h is shown in <xref ref-type="fig" rid="fig4">Figure 4</xref>. It can be seen that the material contains both amorphous and crystalline phases. The amorphous phase is characterized by a wave-like tendency in the baseline and diffused peak bottoms caused by the short-range ordering of the silicate structure in the glass [<xref ref-type="bibr" rid="scirp.28643-ref33">33</xref>]. The major crystalline phase Na<sub>2</sub>Ca<sub>2</sub>Si<sub>3</sub>O<sub>9</sub> has hexagonal system based on the angular</p><p>locations and the intensities of the sharp diffraction peaks which match those of the standard PDF #22-1455 [16,34]. The same diffraction pattern was reported by previous studies on sintered 45S5 bioactive glass [14-16,32,34].</p><p>There are two additional peaks observed at 2θ = 23.13˚ and 32.62˚ assigned to the (111) and (211) planes of orthorhombic NaCaPO<sub>4</sub> crystal (PDF #29-1193) [<xref ref-type="bibr" rid="scirp.28643-ref29">29</xref>].</p></sec><sec id="s3_4"><title>3.4. Morphology of the Bioceramic Monolith Similar to Bioglass<sup>&#174;</sup> 45S5</title><p>The porous nature of the BTC-derived bioceramic was investigated using SEM. <xref ref-type="fig" rid="fig5">Figure 5</xref> shows that the material contains prominent macropores, micropores and pore struts. Most of the pores are open and interconnected, with a network of macropores linking the smaller micropores. Many authors agree that a minimum pore size of 100 &#181;m is required for fast cell infiltration inside the scaffold material [<xref ref-type="bibr" rid="scirp.28643-ref27">27</xref>]. However, Figures 6(a)-(d) indicate the presence of seemingly widespread microporosity with an average size range of about 2 - 6 &#181;m, and macropores that range between 20 - 70 &#181;m. Similar morphologies have been reported for 45S5 bioactive glasses sintered up to 1000˚C [14,15].</p><p>Microporosity and the resultant large surface area are crucial to promote diffusion of fluids and nutrients by means of capillary in-growth [<xref ref-type="bibr" rid="scirp.28643-ref29">29</xref>]. The nature of the struts between pores as shown in Figures 6(c) and (d) is evidently thick and dense which is particularly required to enhance the scaffold mechanical strength.</p></sec></sec><sec id="s4"><title>4. CONCLUSION</title><p>Bioceramic monolith with elemental composition similar to Bioglass<sup>&#174;</sup> 45S5 has been prepared by the sol-gel process employing bentonite clay as a cheap source of silica. Strong alkaline medium was used to initially obtain sodium metasilicate from the bentonite clay. The metasilicate was subjected to acidic hydrolysis to give the sol.</p><p>Thereafter, elemental composition of the sol obtained was adjusted by addition of appropriate inorganic reagents to give the gel that underwent polycondensation reaction that gave a monolith after aging and drying. The monolith was subjected to phase transformation during sintering at elevated temperature to give a major crystal phase identified as Na<sub>2</sub>Ca<sub>2</sub>Si<sub>3</sub>O<sub>9</sub> and a secondary crystal phase, orthorhombic NaCaPO<sub>4</sub>. XRD analysis indicated almost complete conversion of the amorphous phase to a new crystalline phase. Sintering also resulted in densification of the pore struts which is envisioned to enhance the mechanical property. FTIR analysis indicated characteristic absorption bands for Si-O-Si and silanol groups in the framework. SEM analysis however reveals that the pore sizes obtained are smaller than the ideal for bone ingrowth which is between 300 - 400 μm. Nevertheless, our results suggest that bentonite clay may serve as low cost raw material for preparing sodium containing bioactive glasses.</p></sec><sec id="s5"><title>5. ACKNOWLEDGEMENTS</title><p>The authors are grateful to Bells University of Technology, Ota, Nigeria for providing funding and their laboratory for this work.</p></sec><sec id="s6"><title>REFERENCES</title></sec><sec id="s7"><title>NOTES</title></sec></body><back><ref-list><title>References</title><ref id="scirp.28643-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">Hench, L.L. (1998) Bioceramics. Journal of American Ceramic Society, 81, 1705-1728. 
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