Refractories made from raw materials that contain 41-42% AI203 are used in linings of blast-furnace shafts and the critical parts of other furnaces. They provide higb_ly resistant linings in heating units compared with firebrick [1][2][3]. The heating and cooling cycles and the body and gaseous-media compositions are important in the formation of the structure and phase composition of the refractories.The raw material for our investigation consisted of Polozhe and Novoselits kaolins (see Table 1). Analysis of the grain-size composition shows that with a rise in the amount of coarse fractions from 0.02 to 0.06 ram, the SiO 2 content increases sharply, while the proportion of A1203 diminishes (Fig. 1). In the Novoselits kaolin, besides the main materialkaolinite and quartz --there is some hydrargillite, marcasite, pyrites, futile, epidote, leucoxene, biotite, muscovite, microcline, and iron hydrated micas. The total refractive index of the kaolinite is 1.562 +__ 0.003. The marcasite and pyrite bond the main mass of iron impurities. The iron in both kaolins is distributed as oxides, hydroxides, low-solubility silicates, and hydrated micas; and it is bonded with the kaolinite in the form of isomorphous impurities.Thermal analysis of the Novoselits kaolin shows that at 310-315~ there is an endothermic effect, indicating the decomposition of the hydrargillite, at 410~ an exothermic effect for the oxidation of pyrite (FeS 2) and pyrrhotine (FeS 1 -x). Oxidation of the sulfides commences at 380~ with heat evolution according to the reaction FeS 2 + 1.50 2 = leO + SO 2, 2SO 2 + 0 2 ~ 2SO 3.The oxidation process occurs in two stages: adsorption of molecular oxygen and dissociation into atomic oxygen; then diffusion of the oxygen atoms deep into the lattice of the sulfide, and reverse diffusion of SO 3. With enlargement of the grains of FeS 2 we note an extension of the exothermic effects towards the higher temperatures. The magnitude of the exothermic effect for the decomposition of hydrargiUite at 430~ is affected by the exothermic effect for the oxidation of FeO, which is noted at 250-375~ its rate also depends on the particle sizes. The thermogram for pyrite shows an endothermic effect at 700-715~ with a high peak in reducing conditions, which is due to the polymorphic inversion of the pyrrhotine from the monoclinic to hexagonal modification. This indicates the preservation of sulfur compounds of iron at temperatures above 700~The two kaolins were used to press specimens, and these were then fired at 1600~ in oxidizing (air) and reducing (coke filling) conditions. The fired specimens were treated with a water solution of HF, and we then measured the amount of HF-insoluble residues (IR). It is shown that in reducing conditions the mullite-forming reaction in the kaolin begins earlier than in the specimens fired in oxidizing media, and the reaction shifts toward the lower temperatures by 100-200~ This is connected with the earlier formation of the liquid phase in reducing conditions (Fig. 2). A more marked influence is ex...