EGU25-8971, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-8971
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Tuesday, 29 Apr, 11:30–11:40 (CEST)
 
Room -2.43
Discussion on the superiority of carbon dioxide geological storage between coal seam bifurcation and coalescence area
Suzhen Shi
Suzhen Shi
  • China University of Mining&Technology-Beijing, Beijing, China (ssz@cumtb.edu.cn)

 China 's energy structure is dominated by coal. The large amount of CO2 emissions leads to a deterioration of the environment. Sequestration of CO2 into coal seams will be an effective measure to reduce emissions. In order to evaluate the potential of CO2 sequestration in complex coal seams, taking the bifurcation and merging area of 15# coal seam in Xinjing mining area as an example, firstly, the spatial distribution characteristics of coal seams are finely characterized on the basis of logging constrained wave impedance inversion and time-depth conversion technology. Then, the intelligent ant body technology is used to realize the effective prediction of the fault system. On this basis, the influence of coal seam thickness, structure, sealing conditions and other factors on CO2 geological storage in the study area is discussed. The results show that the thickness of the bifurcation area of 15 # coal seam in Xinjing mining area is small and there is gangue, which is not conducive to CO2 storage; the thick coal seam in the combined area has large gas storage space, moderate burial, simple structure and good sealing conditions of surrounding rock, which is a good place for CO2 storage. Therefore, the 15 # coal merging area is selected as a favorable area for storage, which provides a reference for the storage and injection of CO2 in deep complex coal seams.

How to cite: Shi, S.: Discussion on the superiority of carbon dioxide geological storage between coal seam bifurcation and coalescence area, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-8971, https://doi.org/10.5194/egusphere-egu25-8971, 2025.