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考虑页岩塑性变形的水力裂缝与天然裂缝相交模拟研究

曹玉玲 何强胜 刘闯

曹玉玲, 何强胜, 刘闯. 考虑页岩塑性变形的水力裂缝与天然裂缝相交模拟研究[J]. 应用数学和力学, 2023, 44(6): 679-693. doi: 10.21656/1000-0887.430300
引用本文: 曹玉玲, 何强胜, 刘闯. 考虑页岩塑性变形的水力裂缝与天然裂缝相交模拟研究[J]. 应用数学和力学, 2023, 44(6): 679-693. doi: 10.21656/1000-0887.430300
CAO Yuling, HE Qiangsheng, LIU Chuang. Numerical Simulation of Hydraulic Fractures Intersecting Natural Fractures in Shale With Plastic Deformation[J]. Applied Mathematics and Mechanics, 2023, 44(6): 679-693. doi: 10.21656/1000-0887.430300
Citation: CAO Yuling, HE Qiangsheng, LIU Chuang. Numerical Simulation of Hydraulic Fractures Intersecting Natural Fractures in Shale With Plastic Deformation[J]. Applied Mathematics and Mechanics, 2023, 44(6): 679-693. doi: 10.21656/1000-0887.430300

考虑页岩塑性变形的水力裂缝与天然裂缝相交模拟研究

doi: 10.21656/1000-0887.430300
基金项目: 

国家自然科学基金项目 12102173

安徽省自然科学基金项目 1908085QA32

江苏省高校自然科学研究面上项目 21KJB130001

详细信息
    作者简介:

    曹玉玲(1996—),女,硕士(E-mail: 1319647425@qq.com)

    何强胜(1999—),男,硕士(E-mail: 1353232771@qq.com)

    通讯作者:

    刘闯(1992—),男,副教授,博士(通讯作者. E-mail: cliu2013@ustc.edu.cn)

  • 中图分类号: TE312

Numerical Simulation of Hydraulic Fractures Intersecting Natural Fractures in Shale With Plastic Deformation

  • 摘要: 水力压裂中,页岩的塑性变形和大量天然弱界面的存在,给水力裂缝扩展形态的预测带来了巨大的挑战.该文基于有限元法建立了一个完全耦合的弹塑性水力压裂数值模型,并考虑了天然裂缝和层理面.数值模型得到了KGD解析解和Blanton曲线的验证.模拟结果显示:与线弹性的水力压裂结果相比,岩石中的塑性变形使得水力裂缝更容易进入天然弱界面;裂缝扩展过程中,岩石塑性变形区域主要集中在储层内;当岩石发生韧性破坏时,水力裂缝更容易贯穿层理面;水力裂缝在高注入速率下,得益于较大驱动力,裂缝能够直接穿过天然裂缝和层理面.研究结果为页岩储藏中水力裂缝的扩展规律提供了新的认识.
  • 图  1  水力裂缝半长-时间的曲线图

    Figure  1.  The hydraulic fracture half length-time curve

    图  2  水力裂缝与天然裂缝交叉角度-地应力差曲线图

    Figure  2.  The approaching angle between the hydraulic fracture and the natural fracture-stress difference curve

    图  3  分层页岩模型的几何形状和边界条件

    Figure  3.  Geometric and boundary conditions of the layered shale model

    图  4  不同注入速率下弹性模型(左)和弹塑性模型(右)裂缝几何形态对比

      为了解释图中的颜色,读者可以参考本文的电子网页版本,后同.

    Figure  4.  Comparison of crack morphologies between the elastic model (left) and the elasto-plastic model (right)at different injection rates

    图  5  分布在裂缝附近的等效塑性应变

    Figure  5.  Equivalent plastic strains distributed in the vicinity of the crack

    图  6  储层和隔层中水力裂缝在不同强度下的断裂机制(方案A)

    Figure  6.  Fracture mechanisms of hydraulic fractures in the pay zone and the barrier at different strengths(plan A)

    图  7  储层和隔层中水力裂缝在不同强度下的断裂机制(方案B)

    Figure  7.  Fracture mechanisms of hydraulic fractures in the pay zone and the barrier at different strengths (plan B)

    图  8  裂缝形态随水力裂缝与层理面的交叉角度的变化

    Figure  8.  Variations of the fracture morphology with the approaching angle between the hydraulic fracture and the bedding plane

    图  9  裂缝扩展随地应力差的变化

    Figure  9.  Variations of the crack extension with the stress difference

    图  10  裂缝扩展随层理面抗拉强度的变化

    Figure  10.  Variations of the crack extension with the tensile strength of the bedding plane

    图  11  裂缝扩展随注入速率的变化

    Figure  11.  Variations of the fracture extension with the injection rate

    图  12  分层页岩中交叉角度-地应力差的散点图

    Figure  12.  The scatter plot of the stress difference vs.the approaching angle in the layered shale

    表  1  分层页岩的输入参数

    Table  1.   The input parameters of the layered shale

    parameter pay zone barrier bedding plane
    height H/m 10 10 -
    elastic modulus E/GPa 15 20 20
    Poisson’s ratio ν 0.25 0.2 -
    permeability k/mD 10 1 -
    rock tensile strength T/MPa 1 2 1.5
    vertical in-situ stress Vmax/MPa 9 9 -
    minimum horizontal in-situ stress hmin/MPa 5 7 -
    maximum horizontal in-situ stress hmax/MPa 8 8 -
    fluid leakoff coefficient (HF & NF) km/(m/(Pa·s)) 1×10-13 1×10-14 1×10-13
    fluid viscosity μ/(Pa·s) 0.001 0.001 0.001
    下载: 导出CSV

    表  2  页岩的塑性参数

    Table  2.   The input plastic parameters of the shale

    parameter value
    hardening constant hr0 0.35
    hardening parameter ξ 0.01
    yield stress c/MPa 11.25
    yield parameter α -0.365
    yield parameter β 1.980 4
    approaching angle θ/(°) 80
    下载: 导出CSV
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  • 收稿日期:  2022-09-29
  • 修回日期:  2023-01-30
  • 刊出日期:  2023-06-01

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