Thermodynamic Stability of Ettringite Formed by Hydration of Ye'elimite Clinker

被引:31
作者
Fridrichova, Marcela [1 ]
Dvorak, Karel [1 ]
Gazdic, Dominik [1 ]
Mokra, Jana [1 ]
Kulisek, Karel [1 ]
机构
[1] Brno Univ Technol, Veveri 331-95, Brno 60200, Czech Republic
关键词
THERMAL-DECOMPOSITION; GYPSUM;
D O I
10.1155/2016/9280131
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
In order to save limited natural resources by utilising industrial by-products, this paper focuses on an entirely new application of fluidized bed combustion fly ash (FBCFA) into Portland composite cements. It is not currently used because undesirable ettringite, 3CaO center dot Al2O3 center dot 3CaSO(4)center dot 32H(2)O, is formed during the hydration of FBCFA. Although the stability of ettringite has been the subject of much research, the solution is not yet fully clear. Ettringite is generally considered to be stable up to a temperature of 110 degrees C; however, some investigators claimed that ettringite may already decompose at even ambient temperatures. To prove these statements, ettringite was prepared by the hydration of ye'elimite, 3CaO center dot 3Al(2)O(3)center dot CaSO4, and the systemstored at laboratory temperature in two environments: in laboratory settings and in an environment of saturated water vapour. The mineralogical composition of ettringite was long term (up to 160 days of hydration) and was analysed by X-ray diffraction (XRD) and differential thermal analysis (DTA). The hydration of ye'elimite is a relatively complex process. Only approximately 30% of ettringite was formed under laboratory conditions that appeared to gradually convert into metaettringite. Within an environment of saturated water vapour, we observed the conversion of ettringite into monosulfate. Original ye'elimite was indicated as the dominant phase of both storages.
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页数:7
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