纸质出版:2015
移动端阅览
[1]孙冰,郭闪闪,曾晟,马艾阳,邓显石.应力波在层状节理岩体中的透反射与衰减规律[J].防灾减灾工程学报,2015,35(06):828-832.
孙冰, 郭闪闪, 曾晟, et al. Transmission and Reflection and the Attenuation Law of Stress Wave in Layered Joint Rock Mass[J]. 2015, 35(6): 828-832.
[1]孙冰,郭闪闪,曾晟,马艾阳,邓显石.应力波在层状节理岩体中的透反射与衰减规律[J].防灾减灾工程学报,2015,35(06):828-832. DOI: 10.13409/j.cnki.jdpme.2015.06.019.
孙冰, 郭闪闪, 曾晟, et al. Transmission and Reflection and the Attenuation Law of Stress Wave in Layered Joint Rock Mass[J]. 2015, 35(6): 828-832. DOI: 10.13409/j.cnki.jdpme.2015.06.019.
为了研究应力波在穿越层状节理岩体发生透射和反射作用后能量的衰减规律
基于Froude相似比例法制作了层状节理岩体模型
并对模型进行瞬时冲击实验研究。通过对不同位置的加速度时程信号的分析
得出应力波因在节理结构面之间的透反射波的叠加作用形成增强信号
使得穿过节理后的时程信号峰值均未在刚起跳时达到最大
而是起跳后的一段时间先后出现峰值。通过离散快速傅里叶变换对时域信号进行频谱特性分析
得出规律:节理对应力波的阻隔作用使节理前后信号的主频和频率内最大振幅均呈非线性降低趋势
信号的高频部分迅速衰减、能量逐渐被吸收。
In order to research the attenuation law of energy in the process that stress wave crosses the rock mass with layered joint forms transmission and reflection.The model of the rock mass with layered joint was made according to the Froude proportion method
and then the instantaneous impact experiment was conducted on the model.Based on the analysis of the time-domain signal of the acceleration in different locations
it shows that the peaks of time-history signals which passed the joint are maximum during the time after its jumping instead of at the beginning of its jumping because the enhanced signals formed due to the superposition effect of the transmission and reflection wave which formed between each two of the layers.According to the analysis of the frequency spectrum characteristic of the time-domain signal with the discrete fast Fourier transformation
the results show that the dominant frequency and the maximum amplitude of the signals before and after the joint decrease in a nonlinear way
the high frequency part of signal attenuate rapidly
energy is absorbed gradually which are caused by blocking effect of the joint on the stress wave.
应力波通过非线性平行节理的能量分析 [J]. 刘婷婷,李建春,李海波,柴少波. 岩石力学与工程学报 . 2013(08)
纵波垂直入射层状非线性节理岩体的半数值时域解 [J]. 郭力群,俞缙,张亚洲,蔡燕燕,彭兴黔. 土木工程学报 . 2013(S2)
斜入射线弹性节理应力波传播特征的数值模拟 [J]. 杨风威,李海波,李建春,郝亚飞,王秒. 岩土力学 . 2013(03)
含单组节理的双重非线性弹性岩石介质中的P波传播规律 [J]. 俞缙,宋博学,钱七虎. 岩石力学与工程学报 . 2012(12)
层理对爆破振动传播规律的影响 [J]. 宋全杰,李海波,李俊如,姚文生,杨风威,王秒. 岩石力学与工程学报 . 2012(10)
应力波在节理岩体中的传播特性探析 [J]. 宋林,邵珠山,吴敏哲. 煤炭学报 . 2011(S2)
An extended displacement discontinuity method for analysis of stress wave propagation in viscoelastic rock mass [J]. L.F.Fan1,F.Ren1,G.W.Ma2 1 School of Civil and Environmental Engineering,Nanyang Technological University,Singapore,639798,Singapore 2 School of Civil and Resource Engineering,The University of Western Australia,Crawley,WA 6009,Australia. Journal of Rock Mechanics and Geotechnical Engineering . 2011(01)
应力波穿越岩石节理时能量耗散规律的实验研究 [J]. 李业学,刘建锋,秦丽. 实验力学 . 2011(01)
不同应力波在张开节理处的能量传递规律 [J]. 王卫华,李夕兵,周子龙,张义平. 中南大学学报(自然科学版) . 2006(02)
岩石节理经历不同变形历史的剪切试验研究 [J]. 杜守继,朱建栋,职洪涛. 岩石力学与工程学报 . 2006(01)
Obliquely incident wave propagation across rock joints with virtual wave source method [J] . J.B. Zhu,J. Zhao. Journal of Applied Geophysics . 2013
A time‐domain recursive method to analyse transient wave propagation across rock joints [J] . J. C.Li,H.B.Li,G. W.Ma,J.Zhao. Geophysical Journal International . 2012 (2)
Normally incident wave propagation across a joint set with the virtual wave source method [J] . J.B. Zhu,X.B. Zhao,J.C. Li,G.F. Zhao,J. Zhao. Journal of Applied Geophysics . 2011 (3)
An equivalent viscoelastic model for rock mass with parallel joints [J] . Li, Jianchun,Ma, Guowei,Zhao, Jian. Journal of Geophysical Research. Solid Earth . 2010 (3)
Analysis of Blast Wave Interaction with a Rock Joint [J] . Jianchun Li,Guowei Ma. Rock Mechanics and Rock Engineering . 2010 (6)
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