A sampling of data on the density of dolomites fired at 1750°C as a function of their chemical composition and structure is presented, and the coefficients of linear correlation are calculated. The most significant coefficients were obtained for the apparent density after firing, the sums of mass fractions CaO+MgO and Fe2O3+Al2O3, and the fraction of SiO2 in the dolomite.
Refractories and Industrial Ceramics – Springer Journals
Published: Nov 26, 2007
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