Study on the pattern of hydraulic fracture propagation andfracture conductivity of conglomerate with different lithologiesin Ma'nan area

Authors

  • Shuiqing Hu Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, P. R. China
  • Chunlei Wei School of Mechanical Engineering, Beijing Institute of Petrochemical Technology, Beijing 102617, P. R. China
  • Yiqun Yan Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, P. R. China
  • Daobing Wang School of Mechanical Engineering, Beijing Institute of Petrochemical Technology, Beijing 102617, P. R. China https://orcid.org/0000-0003-3579-7227
  • Yiping Ye Xinjiang Oilfield Company, PetroChina, Karamay 834000, P. R. China
  • Xiaoshan Li Xinjiang Oilfield Company, PetroChina, Karamay 834000, P. R. China
  • Jing Zhang Xinjiang Oilfield Company, PetroChina, Karamay 834000, P. R. China
  • Zhongchen Ba Xinjiang Oilfield Company, PetroChina, Karamay 834000, P. R. China

Keywords:

Conglomerate, True triaxial, Hydraulic fracturing, Fracture conductivity, Fracture propagation

Abstract

The Ma’nan Fengcheng Formation in Xinjiang is rich in oil and gas resources, offering significant exploration potential. The reservoir’s lithology is diverse, comprising dolomitic, tuffaceous, and sandy conglomerates. However, the patterns of hydraulic fracture propagation and variations in fracture conductivity in these formations are not well understood. To address this, we conducted experiments using a true triaxial hydraulic fracturing physical modeling system and a fracture conductivity testing system. Our key findings are as follows: (1) In sandy conglomerate reservoirs, fractures tend to propagate along the direction of maximum horizontal stress. The presence of gravel causes these fractures to develop into a complex network of narrower microfractures. The breakdown pressure hierarchy is Dolomitic > Tuffaceous > Sandy conglomerate. Increased confining pressure raises the fracture pressure across all lithologies. (2) Fracture conductivity decreases with increasing confining pressure, particularly during the initial stages of pressure loading, and this loss is irreversible. The conductivity hierarchy is Sandy > Dolomitic > Tuffaceous conglomerate. Additionally, increasing the proppant concentration from 2 to 6 kg/m2 enhances fracture conductivity by approximately 1.5 times. These findings provide valuable insights and technical support for the efficient development of conglomerate reservoirs in China.

Cited as: Hu, S., Wei, C., Yan, Y., Wang, D., Ye, Y., Li, X., Zhang, J., Ba, Z. Study on the pattern of hydraulic fracture propagation and fracture conductivity of conglomerate with different lithology in Ma’nan area. Computational Energy Science, 2024, 1(2): 69-85. https://doi.org/10.46690/compes.2024.02.02

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Published

2024-06-09

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