a thermodynamic approach to cement hydration - Eawag-Empa ...
a thermodynamic approach to cement hydration - Eawag-Empa ...
a thermodynamic approach to cement hydration - Eawag-Empa ...
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XAl,<strong>to</strong>tal = 0.5 and XAl,<strong>to</strong>tal = 0.0. The sample XAl,<strong>to</strong>tal = 1.0 showed a slightly higher loss of<br />
weight than the sample XAl,<strong>to</strong>tal = 0.5 and XAl,<strong>to</strong>tal = 0.0. The more iron is present in the solid<br />
phase the “heavier” is the solid phase and the smaller is the proportion of the water in the<br />
solid phase. The theoretical <strong>to</strong>tal weight loss of Al-ettringite is about 45.9 % and of Feettringite<br />
43.9 %. This difference of 2% is almost the same difference as measured in these<br />
experiments (43.7 % and 41.6 %, respectively). The pure Al-containing ettringite showed a<br />
small second peak at approximately 250 °C (Fig. 3.3B). This is in accordance <strong>to</strong> other<br />
findings (Schwiete and Ludwig, 1968; Buhlert and Kuzel, 1971; Perkins and Palmer,<br />
1990). However, for pure Fe-containing ettringite this peak and thus the loss of water at<br />
this temperature, was not observed (Schwiete and Ludwig, 1968; Buhlert and Kuzel,<br />
1971). Hence, this small peak can be taken as indica<strong>to</strong>r of Al-containing ettringite. It can<br />
be assumed that this peak only occurs for ettringite phases where aluminum is the<br />
dominant element. And with a close look at the differentiated relative weight curves (Fig.<br />
3.3B) the peak at ∼ 250 °C decreased from XAl,<strong>to</strong>tal = 1.0 <strong>to</strong> XAl,<strong>to</strong>tal = 0.5 and was not<br />
observable anymore at smaller XAl,<strong>to</strong>tal ratios.<br />
TGA analyses indicated for the ettringite phases in the presence of saturated CaCl2<br />
solutions a <strong>to</strong>tal water content of 29 <strong>to</strong> 30 H2O molecules. From the loss of water of the<br />
solid phases the masses of the different phases were calculated. The results are presented in<br />
Table 3.2.<br />
As discussed in Chapter 2, the formation of Fe-hydroxide at low molar ratio of XAl,<strong>to</strong>tal is<br />
likely and was indicated by the slight reddish color of the these samples. But freshly<br />
precipitated Fe-hydroxide is XRD amorphous and thus difficult <strong>to</strong> detect. TGA reference<br />
curves of Fe(OH)3, lepidocrocite and goethite (Fig. 3.4) showed that the loss of water of Xray<br />
amorphous Fe-hydroxide overlapped with the loss of water of ettringite. Hence, the<br />
formation of Fe-hydroxides could not be excluded, and the molar ratios of XFe,solid, and<br />
XAl,solid respectively, could not be determined exactly. Therefore, always XAl,<strong>to</strong>tal is given in<br />
this article and refers <strong>to</strong> the <strong>to</strong>tal amount of aluminum added <strong>to</strong> the system.<br />
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