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基质-裂隙相互作用对煤渗透率的影响:考虑煤的软化

程先振, 陈连军, 栾恒杰, 王春光, 蒋宇静

程先振, 陈连军, 栾恒杰, 王春光, 蒋宇静. 基质-裂隙相互作用对煤渗透率的影响:考虑煤的软化[J]. 岩土工程学报, 2022, 44(10): 1890-1898. DOI: 10.11779/CJGE202210015
引用本文: 程先振, 陈连军, 栾恒杰, 王春光, 蒋宇静. 基质-裂隙相互作用对煤渗透率的影响:考虑煤的软化[J]. 岩土工程学报, 2022, 44(10): 1890-1898. DOI: 10.11779/CJGE202210015
CHENG Xian-zhen, CHEN Lian-jun, LUAN Heng-jie, WHANG Chun-guang, JIANG Yu-jing. Influences of softening behaviour of coal on evolution of its permeability by considering matrix-fracture interactions[J]. Chinese Journal of Geotechnical Engineering, 2022, 44(10): 1890-1898. DOI: 10.11779/CJGE202210015
Citation: CHENG Xian-zhen, CHEN Lian-jun, LUAN Heng-jie, WHANG Chun-guang, JIANG Yu-jing. Influences of softening behaviour of coal on evolution of its permeability by considering matrix-fracture interactions[J]. Chinese Journal of Geotechnical Engineering, 2022, 44(10): 1890-1898. DOI: 10.11779/CJGE202210015

基质-裂隙相互作用对煤渗透率的影响:考虑煤的软化  English Version

基金项目: 

国家自然科学基金重点项目 51934004

山东省自然科学基金项目 ZR2018ZA0602

详细信息
    作者简介:

    程先振(1990—),男,博士研究生,主要从事煤层气开采基础理论方面的研究。E-mail: lbs_cxz@163.com

    通讯作者:

    陈连军, E-mail: skdclj@sdust.edu.cn

  • 中图分类号: TE319

Influences of softening behaviour of coal on evolution of its permeability by considering matrix-fracture interactions

  • 摘要: 瞬态渗透率是提高煤层气产量的重要依据。为了得到基质-裂隙压力相互作用出现煤的软化行为对渗透率演化的影响。基于理论分析建立含模量软化系数的双重孔隙介质渗透率模型,并基于脉冲瞬态试验与COMSOL有限元数值模拟软件进行渗透率模型的验证。结果表明:根据曲线变化特征,将应变分为初始,快速增长和平衡阶段。在快速增长阶段,注气压力从1 MPa增大到3 MPa应变曲线的斜率分别为83.77,270.54,440.92 m/s。模量软化系数是应变的函数,其值也增大;其次,通过提出张开型和闭合型裂隙几何概念模型,得到含模量软化系数的双孔渗透率模型;最后,试验数据与改进的渗透率模型结果一致,证明模量软化系数主导了渗透率的动态演化。与试验方法相比,数值模拟方法能够监测煤基质的压力,基质与裂隙之间气体压力的变化揭示了煤渗透率演化机理。
    Abstract: The evolution of dynamic permeability is an important basis for improving the production of coal bed methane. In order to obtain the influences of the softening behavior of coal from matrix-fracture pressure interactions on the evolution of its permeability, a dual-pore permeability model with modulus reduction ratio from differential pressure is obtained through theoretical analysis and is validated based on the permeability transient method tests and the finite element numerical simulation software COMSOL. The experimental results show that the strain is divided into the initial, rapid growth and equilibrium phases based on the characteristics of the curve change. During the rapid growth phase, the slope of the strain curve increases from 1 to 3 MPa with slopes of 83.77, 270.54, 440.92 m/s respectively. The modulus-softening coefficient is a function of the strain and its value increases. Furthermore, a dual-pore permeability model with modulus-softening coefficient is obtained by proposing a conceptual model for open and closed fractures. The experimental data are consistent with the results of the improved permeability model, demonstrating that the modulus-softening coefficient dominates the dynamic evolution of the permeability. Finally, the numerical simulation method can be used to monitor the pressure in the coal matrix compared to the experimental method. Thus, the pressure difference between the matrix and the fracture reveals the mechanism of permeability evolution in coal samples.
  • 随着中国交通行业的不断发展,中国桥梁建设水平得到大幅提升,对桥梁跨越能力的要求也不断增长,悬索桥作为所有桥型中跨越能力最大的桥型,越来越成为跨越大江、大河的主要解决方案。但是随着悬索桥跨度的不断增加,锚碇规模急剧扩大,造成锚碇建设成本过高。因此研究锚碇沉井基础的受力变形特性对于悬索桥的锚碇优化设计显得尤为重要。

    Alampalli[1]在1994年研究了沉井在承受竖向和水平向荷载时的结构响应;李永盛[2]和李家平等[3]分别在1995年和2005年通过模型试验探讨了沉井基础的变形机制和破坏失稳形式;穆保岗等[4]在2017年通过模型试验研究了水平荷载长期作用下沉井变位的特性;Liu等[5]在2019年通过模型试验结合数值模拟分析研究了重力式锚碇的稳定性。

    本文首先进行了在分级水平荷载下的沉井在砂箱中的模型试验,然后基于PLAXIS 3D软件建立了有限元模型,并分析了沉井的位移及沉井前侧和沉井底部的土压力,研究了水平荷载条件下沉井的受力变形规律。

    本文依托南京仙新路大桥北锚碇沉井工程,沉井长度为70 m,宽度为50 m,高度为49.5 m。该工程地基土以粉砂和中砂为主。

    本试验采用的模型槽平面尺寸为4.0 m×2.0 m,高1.0 m。地基土采用中砂,其相对密度为2.68,最大孔隙比0.881,最小孔隙比0.463,不均匀系数3.89,曲率系数0.92。模型试验分层填筑地基土,控制每层填土的厚度为0.1 m,最终得到地基土的干密度为1.55 g/cm3,含水率0.63%,相对密实度为59.61%,内摩擦角为34.5°(快剪)。

    沉井模型平面尺寸为0.7 m×0.5 m,高0.495 m,由厚度为22 mm的钢板焊接而成,试验过程将沉井看成刚体,不考虑沉井自身的变形,为模拟沉井与土体相互作用的界面,通过在沉井表面黏2~3 mm的砂粒实现[6],如图1所示。

    图  1  沉井界面的处理
    Figure  1.  Surface treatment for cassion

    模型试验中设计荷载为62kg,本文中水平荷载分级施加,每级荷载为设计荷载的~0.5倍,试验过程中每级荷载施加持续15 min直至土体破坏(土体破坏表现为沉井盖板处的位移急剧增大),沉井加载示意图如图2所示。

    图  2  沉井加载示意图
    Figure  2.  Schematic diagram of cassion under loading

    本研究建立的有限元模型完全基于模型试验,土体及沉井的单元形状均为四面体十节点实体单元,数值模型的网格如图3所示。

    图  3  有限元模型网格
    Figure  3.  Mesh of finite element model

    砂土的本构模型采用土体硬化(HS)模型,土层参数[7]取值见表1

    表  1  土层参数
    Table  1.  Soil parameters
    土层γ/(kN·m-3)eEs/MPaErefoed/MPaEref50/MPaErefur/MPacφ/(°)ψ/(°)m
    砂土15.60.72310.210.210.230.6034.500.5
    注:γ为砂土的重度;e为砂土的孔隙比;Es为砂土的压缩模量;Erefoed为砂土的主固结加载切线刚度;Eref50为砂土的标准三轴排水试验割线刚度;Erefur为砂土的卸载重加载刚度;c为砂土的有效黏聚力;φ为砂土的有效摩擦角;ψ为砂土的膨胀角;m为砂土的刚度应力水平相关幂值。
    下载: 导出CSV 
    | 显示表格

    在沉井盖板顶部设置3个位移测量点A、B、C。在位移测量点上放置位移靶标,采用TH-ISM-ST机器视觉测量仪对靶标位移进行测量,分辨率为0.01 mm,靶标布置如图4

    图  4  靶标布置图
    Figure  4.  Layout of targets

    模型试验和数值模拟的位移对比如图5所示,由图易知,模型试验和数值模拟的靶标位移较为一致,本文中取水平位移随设计荷载增加而不断增加的线弹性阶段为水平承载力极限值[4],即安全系数取值为4。

    图  5  模试验和数值模拟的位移对比
    Figure  5.  Comparison of displacements between model tests and numerical simulations

    在沉井前侧设置8个土压力盒,布置如图6所示,由于土压力盒对称分布,且沉井左右侧完全对称,因此取沉井左右两侧土压力盒平均值作为最终结果,结果如图7所示,其中模型试验中3号及3'号土压力盒数据较差,本文中已舍弃,余下的沉井前侧土压力盒数据和数值模拟结果较吻合。

    图  6  沉井前侧土压力盒布置图
    Figure  6.  Layout of earth pressure cells on front side of caisson
    图  7  模试验和数值模拟的沉井前侧土压力对比
    Figure  7.  Comparison of soil pressures on front side of caisson between model tests and numerical simulations

    在沉井底部设置12个土压力盒,布置如图8所示,同理,取沉井左右两侧土压力盒平均值作为最终结果,结果如图9所示,其中8号及8'号土压力盒数据较差,本文中已舍弃,余下的沉井底部土压力盒数据和数值模拟结果对比,发现当施加荷载/设计荷载的值小于等于4时较一致,当其值大于4之后,二者的结果相差较大。

    图  8  沉井底部土压力盒布置图
    Figure  8.  Layout of earth pressure cells on bottom of caisson
    图  9  模型试验和数值模拟的沉井前侧土压力对比
    Figure  9.  Comparison of soil pressures on bottom of the caisson between model tests and numerical simulations

    本文在已有的研究基础上,通过开展模型试验和数值模拟计算,得到水平荷载下沉井的受力变位特性,主要得出以下结论:

    (1)对锚碇沉井基础在砂土中的受力变位特性进行了试验研究和有限元分析,结果显示,水平荷载下锚碇沉井基础在砂土中的破坏模式为倾覆破坏,且安全系数远大于2,说明现阶段规范[8]中锚碇设计较为保守,有进一步的优化空间。

    (2)通过PLAXIS 3D软件建立了锚碇沉井基础的有限元模型,采用应变硬化的本构模型,结果表明模型试验的结果和有限元模型计算的结果较为一致,说明数值建模过程中的土体本构模型及参数取值可靠,表明PLAXIS 3D软件能够较好的模拟锚碇沉井在砂土中的受力变形行为。

    上述模型试验和有限元分析,只是针对水平荷载条件下锚碇沉井基础在砂土中的受力特性开展的研究,只考虑了单层干砂的地基土层,尚需更近一步探索。

  • 图  1   裂隙分布特征

    Figure  1.   Distribution characteristics of fracture

    图  2   试验系统图

    Figure  2.   Schematic diagram of experimental system

    图  3   煤样上、下游压力演化图

    Figure  3.   Gas pressures of upstream and downstream

    图  4   煤样应变曲线

    Figure  4.   Curves of coal strain

    图  5   煤渗透率演化与应变对比图

    Figure  5.   Evolution of coal permeability versus strain

    图  6   裂隙几何概念模型图

    Figure  6.   Conceptual model for fractures

    图  7   数值计算几何模型

    Figure  7.   Geometric model for numerical calculation

    图  8   改进渗透率模型验证

    Figure  8.   Comparison of numerical results with experimental data

    图  9   基质-裂隙压差演化图

    Figure  9.   Evolution of pressure difference of matrix-fracture

    表  1   不同边界条件下的试验方案

    Table  1   Experimental schemes of different boundary conditions

    方案 围压/MPa 注气压力/MPa 边界条件
    1 7 1 恒围压
    2 7 3 恒围压
    3 7 5 恒围压
    4 5 3 恒压差
    5 6 4 恒压差
    6 7 5 恒压差
    下载: 导出CSV

    表  2   模拟采用的物理力学参数

    Table  2   Physical and mechanical parameters in simulations

    参数 取值
    煤杨氏模量Et/ GPa 3.766
    裂隙杨氏模量Ef/GPa 1.461
    基质杨氏模量Em/ GPa 6.366
    泊松比ν 0.339
    气体黏度μ/(pas) 1.84×10-5
    形状因子f/m-2 1
    初始渗透率k0/m2 1.80×10-18
    煤的密度ρc/(kg·m-3) 1250
    初始孔隙压力p0/MPa 0.1
    裂隙的初始孔隙率ϕf0/% 2
    基质的初始孔隙率ϕm0/% 2.6
    下载: 导出CSV
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  • 收稿日期:  2021-08-11
  • 网络出版日期:  2022-12-11
  • 刊出日期:  2022-09-30

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