4.7 Article

Bulk modulus of basic sodalite, Na-8[AlSiO4](6)(OH)(2)center dot 2H(2)O, a possible zeolitic precursor in coal-fly-ash-based geopolymers

Journal

CEMENT AND CONCRETE RESEARCH
Volume 41, Issue 1, Pages 107-112

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.cemconres.2010.09.012

Keywords

Geopolymer; Fly ash; Basic sodalite; Bulk modulus; High pressure

Funding

  1. King Abdullah University of Science and Technology (KAUST) [KUS-l1-004021]
  2. NIST [60NANB10D014]
  3. Office of Science, Office of Basic Energy Sciences, of the U.S. Department of Energy [DE-AC02-05CH11231]

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Synthetic basic sodalite, Na-8[AlSiO4](6)(OH)(2)center dot 2H(2)O, cubic, P43n, (also known as hydroxysodalite hydrate) was prepared by the alkaline activation of amorphous aluminosilicate glass, obtained from the phase separation of Class F fly ash. The sample was subjected to a process similar to geopolymerization, using high concentrations of a NaOH solution at 90 degrees C for 24 hours. Basic sodalite was chosen as a representative analogue of the zeolite precursor existing in Na-based Class F fly ash geopolymers. To determine its bulk modulus, high-pressure synchrotron X-ray powder diffraction was applied using a diamond anvil cell (DAC) up to a pressure of 4.5 GPa. A curve-fit with a truncated third-order Birch-Murnaghan equation of state with a fixed K'(o) = 4 to pressure-normalized volume data yielded the isothermal bulk modulus, K-o = 43 +/- 4 GPa, indicating that basic sodalite is more compressible than sodalite, possibly due to a difference in interactions between the framework host and the guest molecules. (C) 2010 Elsevier Ltd. All rights reserved.

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