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Local structures of mesoporous bioactive glasses and their surface alterations in vitro : inferences from solid-state nuclear magnetic resonance
Author(s) -
Philips N. Gunawidjaja,
Renny Mathew,
Andy Y. H. Lo,
Isabel IzquierdoBarba,
Ana García,
Daniel Arcos,
Maria ValletRegí,
Mattias Edén
Publication year - 2012
Publication title -
philosophical transactions of the royal society a mathematical physical and engineering sciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.074
H-Index - 169
eISSN - 1471-2962
pISSN - 1364-503X
DOI - 10.1098/rsta.2011.0257
Subject(s) - mesoporous material , magic angle spinning , silicate , solid state nuclear magnetic resonance , simulated body fluid , materials science , magic angle , nuclear magnetic resonance spectroscopy , magnetization , ion , spectroscopy , chemical engineering , nuclear magnetic resonance , analytical chemistry (journal) , chemistry , scanning electron microscope , composite material , organic chemistry , magnetic field , physics , quantum mechanics , engineering , catalysis
We review the benefits of using (29)Si and (1)H magic angle spinning (MAS) nuclear magnetic resonance (NMR) spectroscopy for probing the local structures of both bulk and surface portions of mesoporous bioactive glasses (MBGs) of the CaO-SiO(2)-(P(2)O(5)) system. These mesoporous materials exhibit an ordered pore arrangement, and are promising candidates for improved bone and tooth implants. We discuss experimental MAS NMR results from three MBGs displaying different Ca, Si and P contents: the (29)Si NMR spectra were recorded either directly by employing radio-frequency pulses to (29)Si, or by magnetization transfers from neighbouring protons using cross polarization, thereby providing quantitative information about the silicate speciation present in the pore wall and at the MBG surface, respectively. The surface modifications were monitored for the three MBGs during their immersion in a simulated body fluid (SBF) for intervals between 30 min and one week. The results were formulated as a reaction sequence describing the interconversions between the distinct silicate species. We generally observed a depletion of Ca(2+) ions at the MBG surface, and a minor condensation of the silicate-surface network over one week of SBF soaking.

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