Ye'elimite


Ye'elimite is the naturally occurring form of calcium sulfoaluminate, Ca46SO3. 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 by Shulamit Gross.
The mineral is cubic, with 16 formula units per unit cell, and a cell dimension of 1.8392 nm, and is readily detected and quantified in mixtures by powder x-ray diffraction.

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, and/or monosulfoaluminate, and aluminium hydroxide.
It is manufactured by heating the appropriate quantities of finely-ground alumina, calcium carbonate and calcium sulfate to between 1100-1300°C, preferably in the presence of small quantities of fluxing materials, such as Fe2O3. On heating above 1350°C, ye'elimite will begin to decompose to tricalcium aluminate, calcium oxide, sulfur dioxide and oxygen.