Bentonite Clay and Water Glass Porous Monoliths via Sol-gel Process.
dc.contributor.author | Adams, L.A. | |
dc.contributor.author | Shaibu, R.O. | |
dc.contributor.author | Essien, R.O. | |
dc.contributor.author | Oki, A. | |
dc.date.accessioned | 2019-08-31T17:25:55Z | |
dc.date.available | 2019-08-31T17:25:55Z | |
dc.date.issued | 2011 | |
dc.description.abstract | Porous silicate glass monoliths were obtained from two inexpensive precursors; sodium metasilicate (waterglass) (Na2SiO3) (SMS) and bentonite clay (BTC) using the sol gel synthesis. The optimal gelation mole ratio for SMS was (Na2SiO3 : H2O : H2SO4 : C2H5OH) of (1 : 13.54 : 0.5 : 1.68); while gelation for BTC was (BTC : H2O : H2SO4 : C2H5OH) of (1 : 13.54 : 1.0 : 1.68). The gels obtained were initially washed with deionised water to free the (Si-O-Si) framework from Na2SO4 as by-product of the hydrolysis, followed by aging, drying at low temperature before finally sintering at 600°C to give the monoliths. The bulk density of the monoliths obtained were determined, and further characterized using Fourier transform infra red (FTIR) spectroscopy, X-ray diffraction (XRD) spectroscopy, Atomic absorption spectroscopy (AAS), and Scanning electron microscopy (SEM). The monoliths show macroporous structure with pore size ranging from 150 – 250 nm, and can be further tailored to give scaffolds for bone tissue repair. | en_US |
dc.identifier.citation | Adams, L. A., Shaibu, R. O., Essien, R. E., & Oki, A. (2011). Bentonite clay and waterglass porous monoliths via the sol-gel process. Journal of Metals, Materials and Minerals, 21(2), 1-6. | en_US |
dc.identifier.uri | https://ir.unilag.edu.ng/handle/123456789/5015 | |
dc.language.iso | en | en_US |
dc.publisher | SEMANTICSCHOLAR | en_US |
dc.subject | Research Subject Categories::NATURAL SCIENCES::Chemistry::Inorganic chemistry::Bio-inorganic chemistry | en_US |
dc.title | Bentonite Clay and Water Glass Porous Monoliths via Sol-gel Process. | en_US |
dc.type | Article | en_US |