不同应变率下两种岩石的压缩破碎特征试验研究

卢振宇 李文彬 姚文进 彭航

卢振宇, 李文彬, 姚文进, 彭航. 不同应变率下两种岩石的压缩破碎特征试验研究[J]. 高压物理学报, 2021, 35(1): 014101. doi: 10.11858/gywlxb.20200605
引用本文: 卢振宇, 李文彬, 姚文进, 彭航. 不同应变率下两种岩石的压缩破碎特征试验研究[J]. 高压物理学报, 2021, 35(1): 014101. doi: 10.11858/gywlxb.20200605
LU Zhenyu, LI Wenbin, YAO Wenjin, PENG Hang. Experimental Study on Compression and Fracture Characteristics of Two Kinds of Rocks under Different Strain Rates[J]. Chinese Journal of High Pressure Physics, 2021, 35(1): 014101. doi: 10.11858/gywlxb.20200605
Citation: LU Zhenyu, LI Wenbin, YAO Wenjin, PENG Hang. Experimental Study on Compression and Fracture Characteristics of Two Kinds of Rocks under Different Strain Rates[J]. Chinese Journal of High Pressure Physics, 2021, 35(1): 014101. doi: 10.11858/gywlxb.20200605

不同应变率下两种岩石的压缩破碎特征试验研究

doi: 10.11858/gywlxb.20200605
基金项目: 国家自然科学基金(11972018)
详细信息
    作者简介:

    卢振宇(1996-),男,硕士研究生,主要从事岩石侵彻动力学研究. E-mail:lzy199639@163.com

    通讯作者:

    李文彬(1965-),男,博士,教授,主要从事弹药总体技术研究. E-mail:lwb2000cn@njust.edu.cn

  • 中图分类号: O347.1; TD326

Experimental Study on Compression and Fracture Characteristics of Two Kinds of Rocks under Different Strain Rates

  • 摘要: 为了研究不同岩石在不同应变率下压缩时裂纹的产生规律及破坏模式,将石灰岩和红砂岩制成试件,研究其在不同应变率和受力模式下裂纹的形成模式。开展了两种岩石的准静态压缩和动态压缩试验,采用高速摄影机记录了裂纹的产生和破坏模式。对两种岩石试件的裂纹形态进行对比,基于岩石的物理性质、受力状态、能量演化分析,得到了在不同应变率下压缩时产生差异性的原因。结果表明:准静态压缩下岩石试件受压的破坏模式也会因应变率的不同而存在差异,并且破坏模式的差异对岩石试件的抗压强度将产生显著的影响;从能量演化的角度分析,入射能量的大小将会决定岩石试样动态抗压强度曲线是否出现起伏;动态压缩时,裂纹的周向扩展速度与岩石抗压强度呈正相关。

     

  • 图  岩石试件及岩石微观结构

    Figure  1.  Rock specimens and rock microstructure

    图  准静态试验示意图

    Figure  2.  Schematic diagram of quasi-static test

    图  红砂岩和石灰岩在两种应变率下的真实应力-应变曲线

    Figure  3.  True stress-strain curves of red sandstone and limestone at two strain rates

    图  准静态单轴压缩下试件的破坏模式

    Figure  4.  Failure modes of the specimen under quasi-static uniaxial compression

    图  纺锤形子弹(单位:mm)

    Figure  5.  Spindle bullet (Unit: mm)

    图  整形后入射波的波形

    Figure  6.  Waveform of incident wave after shaping

    图  红砂岩和石灰岩在动态压缩下的应力-应变曲线

    Figure  7.  Stress-strain curves of red sandstone and limestone under dynamic compression

    图  红砂岩在两种应变率下的破坏模式

    Figure  8.  Failure modes of red sandstone at two strain rates

    图  石灰岩在两种应变率下的破坏模式

    Figure  9.  Failure modes of limestone at two strain rates

    图  10  石灰岩在动态压缩下的破坏模式($\dot{\varepsilon }=429\;{\mathrm{s}}^{-1}$

    Figure  10.  Failure mode of limestone under dynamic compression ($\dot{\varepsilon }=429\;{\mathrm{s}}^{-1}$)

    图  11  红砂岩在动态压缩下的破坏模式($\dot{\varepsilon }=312\;{\mathrm{s}}^{-1}$

    Figure  11.  Failure mode of red sandstone under dynamic compression ($\dot{\varepsilon }=312\;{\mathrm{s}}^{-1}$)

    图  12  两种岩石强度与应变能的对比

    Figure  12.  Comparison of strength and strain energy between red sandstone and limestone

    图  13  动态压缩下岩石裂纹周向扩展速度对比

    Figure  13.  Comparison of circumferential velocity of rock cracks under dynamic compression

    表  1  动态压缩试验分组

    Table  1.   Runs of dynamic compression tests

    Rock materialTest No.Total number of trialsBullet speed/(m·s−1)Rock materialTest No.Total number of trialsBullet speed/(m·s−1)
    Red sandstoneH-1314.8LimestoneS-1316.7
    H-2316.5S-2318.6
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  • 收稿日期:  2020-08-20
  • 修回日期:  2020-09-02

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