2002
DOI: 10.1016/s0008-8846(01)00750-5
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XRD, EDX and IR analysis of solid solutions between thaumasite and ettringite

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Cited by 146 publications
(55 citation statements)
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“…We assign the sharp absorption at 3634cm -1 as being due to non-hydrogen bonded O-H stretch, the broad absorption at 3422cm -1 as due to hydrogen bonded O-H stretch and free water, the peak at 1674cm -1 as due to O-H bend and the peak at 1108cm -1 as due to S-O stretch from SO 4 2-groups in line with previous assignations [24][25][26][27]. The effect of pressure on the infrared spectrum of ettringite is shown in figure 8 …”
Section: Resultssupporting
confidence: 88%
“…We assign the sharp absorption at 3634cm -1 as being due to non-hydrogen bonded O-H stretch, the broad absorption at 3422cm -1 as due to hydrogen bonded O-H stretch and free water, the peak at 1674cm -1 as due to O-H bend and the peak at 1108cm -1 as due to S-O stretch from SO 4 2-groups in line with previous assignations [24][25][26][27]. The effect of pressure on the infrared spectrum of ettringite is shown in figure 8 …”
Section: Resultssupporting
confidence: 88%
“…Ettringite forms a partial solid solution with thaumasite [Ca 3 Si (OH) 6 with existing data for the ettringite endmember [10] confirms that our sample correspond to almost pure ettringite (Fig. 1).…”
Section: Experimental Methodssupporting
confidence: 87%
“…Hence, the effect of ettringite on thaumasite formation was studied in synthetic OPC materials using this methodology (Kholer et al 2006). It must be highlighted that ettringite and thaumasite form a solid solution that has been extensively studied (Barnett et al 2002;Torres et al 2004). …”
Section: Durability Studiesmentioning
confidence: 99%