TY - JOUR
T1 - Dilatometry of geopolymers as a means of selecting desirable fly ash sources
AU - Provis, John L
AU - Harrex, R.M.
AU - Bernal, Susan A
AU - Duxson, P.
AU - Van Deventer, J.S.J.
PY - 2012/8/15
Y1 - 2012/8/15
N2 - The use of dilatometry as a screening tool for the analysis of fly ash reactivity in geopolymers is presented and validated by testing six fly ash sources across a range of mix designs. In particular, a prediction of geopolymer mechanical performance can be obtained from the temperature at which the high-temperature expansion peak attributed to the release of strongly chemically-bound water is observed; high-strength samples generally display this expansion at a higher temperature than low-strength samples. Samples made either with a poorly reactive fly ash or an excessive SiO2 content in the activating solution also expand by up to 10–15% below 200 °C, which indicates a low extent of crosslinking in the silicate gel phase. The second derivative of the dilatometric data can be helpful in identifying the onset temperature of the high-temperature expansion peak, as it is sometimes overlaid on a shrinkage phenomenon attributed to viscous sintering.
AB - The use of dilatometry as a screening tool for the analysis of fly ash reactivity in geopolymers is presented and validated by testing six fly ash sources across a range of mix designs. In particular, a prediction of geopolymer mechanical performance can be obtained from the temperature at which the high-temperature expansion peak attributed to the release of strongly chemically-bound water is observed; high-strength samples generally display this expansion at a higher temperature than low-strength samples. Samples made either with a poorly reactive fly ash or an excessive SiO2 content in the activating solution also expand by up to 10–15% below 200 °C, which indicates a low extent of crosslinking in the silicate gel phase. The second derivative of the dilatometric data can be helpful in identifying the onset temperature of the high-temperature expansion peak, as it is sometimes overlaid on a shrinkage phenomenon attributed to viscous sintering.
UR - http://www.scopus.com/inward/record.url?eid=2-s2.0-84863314508&partnerID=MN8TOARS
U2 - 10.1016/j.jnoncrysol.2012.06.001
DO - 10.1016/j.jnoncrysol.2012.06.001
M3 - Article
SN - 0022-3093
VL - 358
SP - 1930
EP - 1937
JO - Journal of Non-Crystalline Solids
JF - Journal of Non-Crystalline Solids
IS - 16
ER -