深层煤层气储层压裂裂缝扩展与支撑剂耦合机理

Coupling mechanisms of fracture propagation and proppant transport indeep coalbed methane reservoirs

  • 摘要:
    目的和方法 深层煤层气储层普遍具有层理发育、力学非均质性强和地应力梯度高等特征,其压裂裂缝呈现出显著的非线性扩展行为和多场耦合效应。针对传统裂缝力学模型难以刻画深层煤储层裂缝复杂化机理的问题,基于2.0 m × 2.0 m × 1.0 m 超大型真三轴水力压裂物理模拟系统,开展不同排量与黏度条件下的水力压裂物理模拟实验,结合断裂力学与能量守恒理论,建立了裂缝扩展能量平衡方程、支撑剂迁移−沉积对流扩散方程及 “排量−黏度−复杂度”耦合模型,系统揭示了裂缝演化的动力学机制与裂缝网络复杂化规律。
    结果  (1) 裂缝扩展过程受地应力场、流体压力场及层理结构共同作用,为非稳态能量转换过程,裂缝扩展速率与能量释放率满足幂律关系。(2) 排量主要决定能量输入速率与裂缝传播速度,高排量导致能量集中于主缝前缘,裂缝趋于贯通但分支数量减少,裂缝复杂度降低;低排量条件下能量分布更均匀,增强能量蓄积与横向扩散,利于多点起裂与分支形成,裂缝复杂度提升25%~35%。(3) 压裂液黏度影响流体–固体间能量传递与支撑剂沉降行为,高黏度(45 mPa·s)条件下支撑剂沉降速度显著减小,与低黏度(15 mPa·s)条件相比,高黏度下携砂性能提高约40%,促进支撑剂向远井段均匀铺置,有利于形成连续导流通道。
    结论 实验拟合获得的经验关系表明,裂缝复杂度与排量及黏度呈幂律耦合关系,低排量–高黏度组合更有利于形成立体裂缝网络,其分形维数可达1.46。建立的理论与实验耦合框架揭示了深层煤储层裂缝扩展–支撑剂运移的内在能量传递规律,为深层非常规储层压裂参数优化及裂缝复杂度预测提供了定量化理论基础。

     

    Abstract:
    Objectives and Methods Deep coalbed methane (CBM) reservoirs commonly exhibit well-developed beddings, strong mechanical heterogeneity, and high in-situ stress gradients. These characteristics result in pronounced nonlinear fracture propagation and strong multi-field coupling effects during hydraulic fracturing. Consequently, it is challenging to accurately describe the mechanisms governing fracture complexity in deep coal reservoirs using conventional mechanical models for fractures. Using a super-large true triaxial system with dimensions of 2.0 m × 2.0 m × 1.0 m, this study conducted physical simulation experiments on hydraulic fracturing under varying injection rates and viscosities of fracturing fluids. In combination with fracture mechanics and energy conservation theory, this study established an energy balance equation for fracture propagation, a convection-diffusion equation for proppant transport and settling, and a model for the coupling relationships among fracture complexity and the injection rate and viscosity of fracturing fluids. Accordingly, both the dynamic mechanisms behind fracture evolution and the pattern governing the fracture network complexity were systematically elucidated.
    Results  The results indicate that fracture propagation is jointly controlled by the in-situ stress field, fluid pressure field, and bedding structures, representing a unsteady energy conversion process. The fracture propagation rate exhibits a power-law relationship with the energy release rate. The injection rate of fracturing fluids primarily determines the energy input rate and fracture propagation velocity. A high injection rate results in energy concentration in the front of the primary fracture, promoting fracture interconnectivity while suppressing branch development. Accordingly, fracture complexity is reduced. In contrast, a low injection rate corresponds to a more uniform energy distribution, enhancing the accumulation and lateral diffusion of energy. This facilitates multi-point initial cracking and fracture branching, increasing fracture complexity by approximately 25%–35%. Fracturing fluid viscosity significantly influences the energy transfer between fluids and solids, as well as proppant settling behavior. A high viscosity (45 mPa·s) is associated with a significant decrease in the proppant settling velocity. Compared to a low viscosity of 15 mPa·s, the high viscosity increases the proppant transport capacity by approximately 40%, promoting more uniform proppant placement in far-wellbore zones and creating favorable conditions for the formation of continuous hydraulically conductive pathways.
    Conclusions Empirical relationships derived from experiments and fitting indicate that the fracture complexity exhibits power-law coupling relationships with the injection rate and viscosity of fracturing fluids. Notably, the low-injection-rate and high-viscosity combination is more favorable for the development of 3D fracture networks, with a fractal dimension reaching up to 1.46. The proposed theoretical-experimental coupling framework reveals the energy transfer mechanisms governing fracture propagation and proppant transport in deep coal reservoirs, providing a quantitative theoretical basis for optimizing hydraulic fracturing parameters and predicting fracture complexity in deep unconventional reservoirs.

     

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