Home > Research > Publications & Outputs > Magnesium analogues of aluminosilicate inorgani...
View graph of relations

Magnesium analogues of aluminosilicate inorganic polymers (geopolymers) from magnesium minerals

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Published

Standard

Magnesium analogues of aluminosilicate inorganic polymers (geopolymers) from magnesium minerals. / Mackenzie, Kenneth J. D.; Bradley, Siobhan; Hanna, John V. et al.
In: Journal of Materials Science, Vol. 48, No. 4, 01.02.2013, p. 1787-1793.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Mackenzie, KJD, Bradley, S, Hanna, JV & Smith, ME 2013, 'Magnesium analogues of aluminosilicate inorganic polymers (geopolymers) from magnesium minerals', Journal of Materials Science, vol. 48, no. 4, pp. 1787-1793. https://doi.org/10.1007/s10853-012-6940-y

APA

Mackenzie, K. J. D., Bradley, S., Hanna, J. V., & Smith, M. E. (2013). Magnesium analogues of aluminosilicate inorganic polymers (geopolymers) from magnesium minerals. Journal of Materials Science, 48(4), 1787-1793. https://doi.org/10.1007/s10853-012-6940-y

Vancouver

Mackenzie KJD, Bradley S, Hanna JV, Smith ME. Magnesium analogues of aluminosilicate inorganic polymers (geopolymers) from magnesium minerals. Journal of Materials Science. 2013 Feb 1;48(4):1787-1793. Epub 2012 Oct 16. doi: 10.1007/s10853-012-6940-y

Author

Mackenzie, Kenneth J. D. ; Bradley, Siobhan ; Hanna, John V. et al. / Magnesium analogues of aluminosilicate inorganic polymers (geopolymers) from magnesium minerals. In: Journal of Materials Science. 2013 ; Vol. 48, No. 4. pp. 1787-1793.

Bibtex

@article{6cdbaf8c4b1b421e810671451a8f5852,
title = "Magnesium analogues of aluminosilicate inorganic polymers (geopolymers) from magnesium minerals",
abstract = "Attempts to synthesise magnesium-containing analogues of aluminosilicate geopolymers from the 1:1 and 2:1 layer magnesiosilicate minerals chrysotile and talc, as well as the magnesium mineral sepiolite are reported. The effect of pre-treating these starting minerals by grinding and/or dehydroxylation was also investigated by XRD, 29Si and natural-abundance 25Mg solid-state magic angle spinning (MAS) NMR spectroscopy. The products from sepiolite most closely resembled an aluminosilicate geopolymer, setting at 40 °C to an X-ray amorphous product containing a broad characteristic 29Si MAS NMR resonance at −90 ppm. The 25Mg MAS NMR spectrum of this product also showed evidence that some of the Mg was located in tetrahedral sites, as expected for a conventional geopolymer. A similar 25Mg MAS NMR result was obtained for chrysotile, but talc proved to be extremely resistant to geopolymer synthesis, requiring treatment at 120 °C for 3 days to set to a friable material retaining the XRD and NMR characteristics of the original talc or its crystalline dehydroxylation products. This lack of reactivity may be related to the 2:1 layer-lattice talc structure, or to the fact that a suitably reactive amorphous product is not formed upon dehydroxylation.",
author = "Mackenzie, {Kenneth J. D.} and Siobhan Bradley and Hanna, {John V.} and Smith, {Mark E.}",
note = "Date of Acceptance: 05/10/2012",
year = "2013",
month = feb,
day = "1",
doi = "10.1007/s10853-012-6940-y",
language = "English",
volume = "48",
pages = "1787--1793",
journal = "Journal of Materials Science",
issn = "0022-2461",
publisher = "Springer Netherlands",
number = "4",

}

RIS

TY - JOUR

T1 - Magnesium analogues of aluminosilicate inorganic polymers (geopolymers) from magnesium minerals

AU - Mackenzie, Kenneth J. D.

AU - Bradley, Siobhan

AU - Hanna, John V.

AU - Smith, Mark E.

N1 - Date of Acceptance: 05/10/2012

PY - 2013/2/1

Y1 - 2013/2/1

N2 - Attempts to synthesise magnesium-containing analogues of aluminosilicate geopolymers from the 1:1 and 2:1 layer magnesiosilicate minerals chrysotile and talc, as well as the magnesium mineral sepiolite are reported. The effect of pre-treating these starting minerals by grinding and/or dehydroxylation was also investigated by XRD, 29Si and natural-abundance 25Mg solid-state magic angle spinning (MAS) NMR spectroscopy. The products from sepiolite most closely resembled an aluminosilicate geopolymer, setting at 40 °C to an X-ray amorphous product containing a broad characteristic 29Si MAS NMR resonance at −90 ppm. The 25Mg MAS NMR spectrum of this product also showed evidence that some of the Mg was located in tetrahedral sites, as expected for a conventional geopolymer. A similar 25Mg MAS NMR result was obtained for chrysotile, but talc proved to be extremely resistant to geopolymer synthesis, requiring treatment at 120 °C for 3 days to set to a friable material retaining the XRD and NMR characteristics of the original talc or its crystalline dehydroxylation products. This lack of reactivity may be related to the 2:1 layer-lattice talc structure, or to the fact that a suitably reactive amorphous product is not formed upon dehydroxylation.

AB - Attempts to synthesise magnesium-containing analogues of aluminosilicate geopolymers from the 1:1 and 2:1 layer magnesiosilicate minerals chrysotile and talc, as well as the magnesium mineral sepiolite are reported. The effect of pre-treating these starting minerals by grinding and/or dehydroxylation was also investigated by XRD, 29Si and natural-abundance 25Mg solid-state magic angle spinning (MAS) NMR spectroscopy. The products from sepiolite most closely resembled an aluminosilicate geopolymer, setting at 40 °C to an X-ray amorphous product containing a broad characteristic 29Si MAS NMR resonance at −90 ppm. The 25Mg MAS NMR spectrum of this product also showed evidence that some of the Mg was located in tetrahedral sites, as expected for a conventional geopolymer. A similar 25Mg MAS NMR result was obtained for chrysotile, but talc proved to be extremely resistant to geopolymer synthesis, requiring treatment at 120 °C for 3 days to set to a friable material retaining the XRD and NMR characteristics of the original talc or its crystalline dehydroxylation products. This lack of reactivity may be related to the 2:1 layer-lattice talc structure, or to the fact that a suitably reactive amorphous product is not formed upon dehydroxylation.

U2 - 10.1007/s10853-012-6940-y

DO - 10.1007/s10853-012-6940-y

M3 - Journal article

VL - 48

SP - 1787

EP - 1793

JO - Journal of Materials Science

JF - Journal of Materials Science

SN - 0022-2461

IS - 4

ER -