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    夹层发育陆相页岩水力压裂物理模型实验研究

    Experimental study of hydraulic fracturing in interbedded lacustrine shales using physical models

    • 摘要: 陆相页岩中复杂的夹层结构显著影响着水力裂缝的起裂扩展规律。以四川盆地侏罗系凉高山组陆相页岩储层为研究对象,选取相应层段中代表性夹层的半直径岩心,开展连续划痕与冲击锤高分辨率力学测试。在获得页岩基质及介壳、砂质、泥质3类夹层抗压强度、杨氏模量等关键力学参数差异分布特征的基础上,以硅酸盐水泥为胶结材料并调控骨料配比,制备了具有不同力学参数值的人工岩板,依据物理模型相似比原理,构建了具有夹层发育特征的立方体层状物理模型。对3类夹层发育模型开展真三轴条件下的水力压裂模拟实验,结果表明不同夹层物理模型中水力裂缝的展布特征存在明显差异。进一步分析3种夹层样品的莫尔圆及抗剪强度参数差异显示,夹层发育对水力裂缝扩展路径与缝网复杂度具有显著控制作用。

       

      Abstract: The complex sandwich construction of lacustrine shales significantly influences the initiation and propagation of hydraulic fractures. The case study deals with lacustrine shale reservoirs of the Jurassic Lianggaoshan Formation in the Sichuan Basin. It uses half-diameter core samples with typical interlayers for high-resolution mechanical characterization via continuous scratch and impulse hammer tests. Based on the distinct distribution characteristics of key mechanical parameters (including uniaxial compressive strength and Young’s modulus) for the shale matrix and three interlayer types (shell, sandy, and argillaceous), artificial rock slabs with different mechanical properties are prepared using Portland cement as the binder with adjusted aggregate proportions. Following the similarity principle of physical modeling, cubic layered physical models with sandwich structures are constructed. True triaxial hydraulic fracturing experiments on physical models with three interlayer types show markedly different spatial distributions of hydraulic fractures. Further analysis of Mohr's circles and shear strength suggests that interlayers significantly control hydraulic fracture propagation pathways and fracture network complexity.

       

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