Ye'elimite (white) intergrown with Hydroxylellestadite (reddish-brown) in grey Anhydrite from Ronneburg, Thuringia, Germany (Picture size 6 mm)
|Crystal class||Gyroidal (432)
H-M Symbol: (432)
|Unit cell||a= 18.392 Å; Z = 16|
Ye'elimite is the naturally occurring form of calcium sulfoaluminate, Ca4(AlO2)6SO4. It gets its name from Har Ye'elim in Israel in the Hatrurim Basin west of the Dead Sea where it was first found in nature.
Occurrence in cement
It is alternatively called "Klein's Compound", after Alexander Klein of the University of California, Berkeley, who experimented with sulfoaluminate cements around 1960, although it was first described in 1957 by Ragozina. Ye'elimite is most commonly encountered as a constituent of sulfoaluminate cements, in which it is manufactured on the million-tonne-per-annum scale. It also occasionally occurs adventitiously in Portland-type cements. On hydration in the presence of calcium and sulfate ions, it forms the insoluble, fibrous mineral ettringite, which provides the strength in sulfoaluminate concretes.
It is manufactured by heating the appropriate quantities of finely-ground alumina, calcium carbonate and calcium sulfate to around 1000-1100°C, preferably in the presence of small quantities of fluxing materials. On heating above 1350°C, it begins to decompose to tricalcium aluminate, calcium oxide, sulfur dioxide and oxygen.
- Handbook of Mineralogy
- H F W Taylor, Cement Chemistry, Academic Press, 1990, ISBN 0-12-683900-X, pp 51-54
- G C Bye, Portland Cement 2nd Ed, Thomas Telford, 1999, ISBN 0-7277-2766-4, p 206
- P C Hewlett (Ed), Lea's Chemistry of Cement and Concrete, 4th Ed, Arnold, 1998, ISBN 0-340-56589-6, pp 447-449
- A E Moore, Cement Technology, 7 (1976) pp 85, 134
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