层理面遇天然裂隙的页岩储层水力裂缝网络复杂性研究

    STUDY ON THE COMPLEXITY OF HYDRAULIC FRACTURE NETWORK IN SHALE RESERVOIRS CONSIDERING THE BEDDING PLANES ENCOUTERING THE NATURAL FRACTURES

    • 摘要: 水力压裂形成复杂裂缝网络是页岩气高效开发的前提条件,其中层理面和天然裂隙的空间展布直接影响着水力裂缝扩展过程及其裂缝网络形成的复杂性。论文结合软件COMSOL Multiphysics和MATLAB,考虑页岩储层非均质性建立渗流-应力-损伤耦合模型,引入基于盒数法的网格覆盖法测定其复杂裂缝网络的分形维数,评价数值模拟的压裂效果,揭示层理面与天然裂隙共同作用的水力裂缝网络复杂性。研究结果表明:(1)层理抗拉强度和角度对水力裂缝网络复杂程度的影响显著,表现为抗拉强度较低或较高时,都不易形成复杂的水力裂缝网络;而较大角度层理的页岩储层更易形成复杂的水力裂缝网络。(2)天然裂隙抗拉强度较低时,容易被激活并诱发水力裂缝的扩展路径改变,增大裂缝网络的分形维数及复杂性。特别是天然裂隙与最大主应力方向的夹角较大时,显著改变水力裂缝的扩展路径,形成分形维数较高的更复杂的裂缝网络。(3)大小适中的应力比更易形成复杂的裂缝网络,论文提出的应力比1.5时,形成的裂缝网络分形维数最大,其复杂程度最高。其研究成果可为页岩储层水力压裂效果评价及压裂技术优化提供科学依据。

       

      Abstract: The formation of a complex fracture network through hydraulic fracturing is a prerequisite for the efficient development of shale gas. The spatial distribution of bedding planes and natural fractures directly influences the propagation of hydraulic fractures and the complexity of corresponding networks. Combinations of the software COMSOL Multiphysics and MATLAB are used to establish a coupled seepage-stress-damage model, considering the heterogeneity of shale reservoirs. A grid coverage method based on the box counting method is introduced to determine the fractal dimension of its complex fracture network, evaluate the hydraulic fracturing effectiveness in numerical simulations, and reveal the complexity of the hydraulic fracture networks resulting from the interactions of bedding planes and natural fractures. It can be concluded from the numerical simulations and discussions that:(1)The bedding plane tensile strength and angle significantly influence the complexity of hydraulic fracture networks. This is evident as both lower and higher tensile strengths of bedding planes make it more difficult to form complex hydraulic fracture networks. In contrast, shale reservoirs with larger angle bedding planes are more prone to form complex hydraulic fracture networks. (2)Considering the lower tensile strength of natural fractures, the propagation path of hydraulic fractures is easily activated and changed, resulting in greater fractal dimensions and more complex fracture networks. In particular, natural fractures with larger angles are along with the maximum principal stress direction, the propagation path of hydraulic fractures is significantly changed, resulting in higher fractal dimensions and more complex fracture networks. (3)Moderate stress ratios are more likely to form complex fracture networks. A stress ratio of 1.5 has been analyzed to represent the highest fractal dimensions and the most complex hydraulic fracturing networks. These investigations can provide scientific support for the assessment of hydraulic fracturing effectiveness and optimization of fracturing techniques in shale reservoirs.

       

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