In the process of geothermal energy exploitation and utilization, effective
heat extraction, natural recovery and other key issues are affected and
restricted by the thermal conductivity process of geothermal reservoirs, and
the relevant thermal conductivity model research is not very comprehensive
at present. In this paper, the deep heat storage in pore structure is
divided into development zone, wave zone and original zone according to
their thermal conductivity characteristics. Based on the Representative
Elementary Volume description analysis method, the thermal conductivity
analysis model of pore structure of deep heat storage is established,
including simplified thermal conductivity model and fine thermal
conductivity model. Taking granite as an example, numerical calculation was
carried out to analyze the effects of porosity, impurity content, water
content and channel composition coefficient on heat storage and thermal
conductivity. The model established in this paper lays a foundation for
controlling thermal storage and thermal conductivity mechanism, accurately
analyzing thermal conductivity characteristics, reserve estimation and
mining dynamic changes.