Important Insights on Fracturing Interference in Tight Conglomerate Reservoirs
Accurate understanding of natural fractures, faults, in situ stress, and mechanical properties of reservoir rocks is a prerequisite for evaluating well interference. During hydraulic fracturing, hydraulic fractures may connect with natural fractures or fault zones, leading to communication with adjacent wells and resulting in cross-well interference. Additionally, horizontal well spacing is a critical factor influencing the occurrence and severity of interference. The Mahu tight oil reservoir experiences severe fracturing interference issues, presenting multiple challenges. This study employs numerical simulation methods to quantitatively assess the influence of geological and engineering factors, including reservoir depletion volume, well spacing, natural fractures, and fracturing operation parameters on fracturing interference intensity. By integrating geological data, engineering parameters, and production data with microseismic monitoring and pressure information, this research aims to clarify key influencing factors and elucidate the fundamental mechanisms governing fracturing-driven interference occurrences. Through production performance analysis and microseismic monitoring, it has been established that well spacing, fracturing intensity, and natural fracture networks are the primary factors affecting interference in hydraulically fractured horizontal wells.
Authors
- Kun Liu (ORCID: https://orcid.org/0000-0003-0168-9172)
- Yiping Ye (ORCID: https://orcid.org/0000-0002-1383-4296)
- Zhemin Zhou (ORCID: https://orcid.org/0000-0003-0604-1885)
- Tao Wan (ORCID: https://orcid.org/0000-0002-7623-9398)
- Kaixin Liu (ORCID: https://orcid.org/0000-0001-6778-1591)
Institutions
- China University of Petroleum, Beijing (CN)
Publication Details
- Journal
- Processes
- Published
- 2025-06-11
- DOI
- https://doi.org/10.3390/pr13061842
- Primary Topic
- Hydraulic Fracturing and Reservoir Analysis
- Type
- article
- Field-Weighted Citation Impact
- 0.00