When clayey rocks are heated, the decomposition of organic matter is accompanied by the release of Н 2, СО and СО 2, which create a reducing nature of the gaseous environment. Burnout of residual carbon occurs in the temperature range 250 - 500 ° C and is extreme due to oxygen diffusion into the inner layers of the heat-treated material. To exclude the black core, it is recommended to provide exposure in the temperature range of 700 - 800 ° C to complete the oxygen burnout process, as well as to mold hollow products with the minimum permissible thickness of the outer and inner walls. Tab. 2, ill. 2, bibliography: 6 titles.