四川盆地不同埋深页岩力学特性差异与水力裂缝扩展特征

    DIFFERENCES IN MECHANICAL PROPERTIES AND HYDRAULIC FRACTURE PROPAGATION CHARACTERISTICS OF SHALE WITH DIFFERENT BURIAL DEPTHS IN THE SICHUAN BASIN

    • 摘要: 四川盆地页岩气资源潜力巨大,川南—渝西是勘探开发热点地区之一。受多期改造影响,五峰组-龙马溪组页岩埋深跨度大,地应力和地层产状复杂,矿物成分和天然裂缝发育程度不同,导致页岩力学特性和储层压裂改造效果存在显著差异,亟须明确不同埋深页岩力学特性差异和水力裂缝扩展规律。本文以昭通地区浅层页岩和大安地区深层页岩为研究对象,开展了井下页岩样品循环加载三轴压缩力学试验和水力压裂试验,对比了龙一1亚段不同小层页岩力学特性和水力裂缝扩展规律。结果表明:(1)受地层抬升影响,浅层页岩层理缝更为发育,脆性矿物含量和三轴抗压强度明显低于深层页岩。浅层页岩三轴压缩形成单一剪切裂缝,伴随层理缝的激活,深层页岩三轴压缩形成多条拉张裂缝。(2)基于CT扫描,重构和对比了浅层页岩与深层页岩三维水力裂缝形态。浅层页岩水力裂缝垂向扩展受层理缝影响较为显著,新生裂缝主要集中在射孔周围,形态较为曲折,裂缝起裂后泵压降幅较小。深层页岩层理缝发育程度明显小于浅层页岩,水力压裂能够形成垂向主裂缝,破裂压力高,裂缝起裂后泵压降幅较大。(3)对比了观音桥泥质灰岩与龙马溪页岩破裂压力,发现泥质灰岩破裂压力低于页岩,表明页岩储层压裂裂缝具备穿过观音桥段泥质灰岩的条件。研究成果为川南—渝西不同埋深页岩储层改造方案设计和靶层选层提供支撑。

       

      Abstract: The shale gas resource potential of Sichuan Basin is huge, and the South Sichuan and West Chongqing area is one of the hot exploration and development areas. Under the influence of multi-stage reconstruction, the shale gas reservoir of Wufeng-Longmaxi Formation exhibits considerable variation in burial depth, complex in-situ stress state and structural characteristics, and the mineral composition and natural fracture development vary correspondingly, resulting in significant differences in shale mechanical properties and stimulation efficiency. It is urgent to clarify the differences in mechanical properties and hydraulic fracture propagation characteristics in shale cores of different burial depths. Taking shallow shale in Zhaotong exploration area and deep shale in Da'an exploration area as research objects, this paper carried out cyclic loading triaxial compression and hydraulic fracturing tests on reservoir shale cores, and the distinctions of mechanical strength and hydraulic fracture propagation characteristics of different sublayer shale in Long-1 submember were analyzed. The results showed that: (1) Affected by stratum uplift, bedding fractures are relatively developed in shallow shale, and the brittle mineral content and triaxial compressive strength of shallow shale are significantly lower than those of deep shale. The triaxial compression of shallow shale forms a single shear fracture, while with the activation of bedding fractures, the triaxial compression of deep shale forms multiple tensile fractures. (2) Based on CT scans, the three-dimensional hydraulic fracture morphology of shallow shale and deep shale was reconstructed and compared. The vertical propagation of hydraulic fractures in shallow shale is significantly affected by bedding fractures, and the newly created fractures are mainly concentrated around the perforation, with the magnitude of fluid pressure decrease after fracture initiation being relatively small. The bedding fracture development degree of deep shale is obviously smaller than that of shallow shale. Vertical main fractures could be created during fracturing, and the breakdown pressure and the magnitude of fluid pressure decrease after fracture initiation are higher than those of shallow shale samples. (3) By comparing the fracture pressure of Guanyinqiao argillaceous limestone and Longmaxi shale, it is found that the fracturing pressure of argillaceous limestone is lower than that of shale, which indicates that the hydraulic fractures initiated from the shale reservoir meet the condition of passing through the argillite of Guanyinqiao section. The research results could provide experimental support for the fracturing scheme and target layer selection of shale reservoirs with different burial depths in South Sichuan and West Chongqing.

       

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