Effect of mineral morphology of the dolomitic binding material on strength

The peculiarities of mineral morphology of oxychloride cement obtained from the dolomite burning adding intensifiers are considered. It’s revealed that periclase and calcite are formed as fine-crystalline, periclase has a distorted lattice. It’s suggested that these peculiarities of the morphology provide the oxychloride cement from dolomite with strength that is similar to the strength of binding substances made of magnesite and brucite.