Physico-mathematical modeling and experimental studies of the thermal conductivity coefficient of oil-and-gas-bearing rocks
To describe the process of thermal conductivity in oil-and-gas-bearing rocks, which are multicomponent macroscopically disordered environments (MDE), the following hypothesis is used: the MHE's structure is considered as a set of interpenetrating percolation (in nite) clusters (PC), consolidated from the phases of the same-named components, and isolated clusters of elements not included in the PC, and MHE's e ective thermal conductivity depends on the volume fractions, ratios of components conductivity and relative conductivities of PC (RCPC).