长江科学院院报 ›› 2018, Vol. 35 ›› Issue (10): 115-119.DOI: 10.11988/ckyyb.20170309

• 岩土工程 • 上一篇    下一篇

不同静应力作用下砂岩应力波波速及幅值衰减规律

程昀1,2, 宋战平1, 金解放3, 昌晓旭3, 袁伟3   

  1. 1.西安建筑科技大学 土木工程学院,西安 710055;
    2.贺州学院 建筑工程学院,广西 贺州 542899;
    3.江西理工大学 建筑与测绘工程学院,江西 赣州 341000
  • 收稿日期:2017-03-22 出版日期:2018-10-01 发布日期:2018-10-22
  • 作者简介:程 昀(1991-),男,安徽界首人,博士研究生,主要从事岩土动力学及岩体稳定性分析方面的研究工作。E-mail: chengyunedu@163.com
  • 基金资助:
    国家自然科学基金项目(51578447, 51664017); 2017年贺州学院(自然科学类)科研项目(2017ZZZK04)

Variation of P-wave Velocity and Stress WaveAmplitude in Sandstone under Static Stress

CHENG Yun1,2, SONG Zhan-ping1, JIN Jie-fang3, CHANG Xiao-xu3, YUAN Wei3   

  1. 1.School of Civil Engineering,Xi’an University of Architecture and Technology, Xi’an 710055, China;
    2.School of Civil Engineering, Hezhou University, Hezhou 542899, China;
    3.School of Architectural andSurveying Engineering, Jiangxi University of Science and Technology, Ganzhou 341000, China
  • Received:2017-03-22 Online:2018-10-01 Published:2018-10-22

摘要: 为研究轴向应力对大长径比砂岩中应力波传播特性的影响,利用动静组合加载试验装置,对砂岩进行了小扰动冲击试验,研究了轴向应力对砂岩中应力波波形、纵波波速、应力波幅值衰减规律的影响。研究表明:同一轴向应力下,不同测点的应力波波形变化不大,而轴向应力的改变对应力波波形变化影响较大;存在轴向应力时,应力波中同时出现压缩波和拉伸波,且轴向应力越大,拉伸波越长;轴向应力对纵波波速变化影响较大,波速与轴向应力呈线性变化,而与传播距离呈指数函数衰减;轴向应力对幅值变化有明显影响,随着传播距离增加,应力波起跳时间点逐渐滞后,应力波幅值呈不同程度的衰减,这与波携带的能量被砂岩中孔隙吸收程度有关。结果表明轴向应力通过改变砂岩密度进而影响了应力波传播特性。

关键词: 砂岩, 轴向应力, 应力波, 纵波波速, 传播特性, 幅值衰减

Abstract: To study the influence of static stress on propagation characteristics of stress wave in sandstone with large length-diameter ratio, impact test of small disturbance is conducted by dynamic and static combined testing system. The variation of stress wave, P-wave velocity and stress wave amplitude attenuation under different static stresses are obtained. Research results imply that stress wave curves of different test points remain approximately the same when static stress is constant; stress wave curves vary remarkably when static stress changes. Compressional wave and tensile wave both exist in the presence of static stress, and tensile wave increases with the increase of static stress. In addition, static stress has a great impact on P-wave velocity in a linear relationship, and P-wave velocity decays exponentially with propagation distance. Moreover, static stress also has obvious influence on stress wave amplitude. With the increase of propagation distance, the jump of stress wave delays gradually and stress wave amplitude tends to attenuate as wave energy is absorbed by sandstone fractures. The results suggest that static stress affects stress wave propagation in sandstone by changing the internal pores or fractures of sandstone.

Key words: sandstone, axial static stress, stress wave, P-wave velocity, propagation feature, amplitude attenuation

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