Solid solution between Al-ettringite and Fe-ettringite (Ca6[Al1-xFex(OH)6]2(SO4)3•26H2O)

被引:123
作者
Moeschner, Goeril [1 ]
Lothenbach, Barbara [1 ]
Winnefeld, Frank [1 ]
Ulrich, Andrea [1 ]
Figi, Renato [1 ]
Kretzschmar, Ruben [2 ]
机构
[1] Empa Swiss Fed Inst Mat Testing & Res, CH-8600 Dubendorf, Switzerland
[2] ETH, Inst Biogeochem & Pollutant Dynam, CH-8092 Zurich, Switzerland
关键词
Ettringite; Thermodynamic calculations; Hydration products; TETRACALCIUM ALUMINOFERRITE HYDRATION; AQUEOUS-SOLUTION SYSTEMS; CENTER-DOT 26H(2)O; CRYSTAL-STRUCTURE; NEW-JERSEY; GYPSUM; SOLUBILITY; STURMANITE; 5-75-DEGREES-C; DIFFRACTION;
D O I
10.1016/j.cemconres.2009.03.001
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The solid solution between Al- and Fe-ettringite Ca-6[Al1-xFex(OH)(6)](2)(SO4)(3)center dot 26H(2)O was investigated. Ettringite phases were synthesized at different Al/(Al + Fe)-ratios (=X-Al,X-total), so that X-Al increased from 0.0 to 1.0 in 0.1 unit steps. After 8 months of equilibration, the solid phases were analyzed by X-ray diffraction (XRD) and thermogravimetric analysis (TGA), while the aqueous solutions were analyzed by inductively coupled plasma optical emission spectroscopy (ICP-OES) and inductively coupled plasma mass spectrometry (ICP-MS). XRD analyses of the solid phases indicated the existence of a miscibility gap between X-Al,X-total =0.30-0.6. Some of the XRD reflections showed two overlapping peaks at these molar ratios. The composition of the aqueous solutions, however, would have been in agreement with both, the existence of a miscibility gap or a continuous solid solution between Al- and Fe-ettringite, based on thermodynamic modeling, simulating the experimental conditions. (c) 2009 Elsevier Ltd. All rights reserved.
引用
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页码:482 / 489
页数:8
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