Dolomite from the gavadovsk deposits is a promising material for use in metallurgy [1][2][3]. The concentration of basic component equals 88-98%; the impurities consist of calcite, quartz, clay particles, and iron oxides [3].Systematic studies were carried out on the influence of the method of p~eparing these dolomites for firing, the addition of slags, and the firing temperature on the sintering and hydration resistance. Samples of domomites from the Zavadovsk area were provided by the Pravoberezhe geological expedition of the Kiev Geological Commission; batches were taken from the trenches (Nos. 1-4); and the core of the boring (Nos. 5-17).The domomite was calcined in periodic furnaces in the granular form (fractions 5-25 mm), and also in the form of pellets made from finely milled material (cylinders of diameter and height 25 mm). The addition consisted of slag (scale) contain ing the following, %: Fe203 (total) 85.05, Si02 9.66, AI20~ 3.10, CaO 0.13, MgO 5.03. The chemical composition of the calcined dolomite is shown in Table I, and the main experimental data are given in Tables 2-4. The degree of sintering of the dolomite was established visually be examining the external appearance of the specimens, and with respect to the capacity to absorb water applied to the surface of the fracture, and also according to data for open porosity and apparent density measured in kerosene.With an increase in temperature we note an improvement in the sintering, both of the granular and also the pelletized material.In this case for the majority of the specimens satisfactory sintering is provided at 1750"C; with the addition of the scale a higher density is obtained. In terms of the degree of sintering the dolomites can tentatively be classified into three groups. With a weak degree of sintering all the grains are white, light gray, or light brown; and a drop of water is absorbed instantly. With an average degree of sintering some of the fired grains are light brown, a drop of water is absorbed, and some of the grains are brown, and the drop of water is not absorbed. With good sintering all the fired grains of dolomite are brownish and the water is not absorbed.