Experimental study on the variation of P-wave velocity and waveform characteristics during the whole process of water absorption of coal samples
LI Nan1,2,ZHANG Xin1,2,WANG Daxuan2,ZHAO Xingzhi2,LI Song3
(1. State Key Laboratory of Coal Resources and Safe Mining,China University of Mining and Technology,Xuzhou,Jiangsu 221116,China;2. School of Mines,China University of Mining and Technology,Xuzhou,Jiangsu 221116,China;3. School of Safety Engineering,China University of Mining and Technology,Xuzhou,Jiangsu 221116,China)
Abstract:The measurement of P-wave velocity and the waveform analysis of coal samples during the whole process of water absorption were performed to study the variation of P-wave velocity and the characteristics of waveforms. The variation of P-wave velocity with the water saturation and porosity were studied. The amplitude-frequency and time-frequency characteristics of the waveforms under the different water saturations were researched based on the FFT and HHT methods. The results show that the P-wave velocity is influenced by the water saturation and porosity at the same time. The P-wave velocity increases nonlinearly as the water saturation increases. The increasing rate of the P-wave velocity increases significantly when the water saturation reaches about 70%. The properties of water and the uniform existence of pore water in the porous structure of coal are the main causes of the increase of the P-wave velocity. The P-wave velocity decreases linearly with the increasing of the porosity of coal. The higher the water saturation,the less affected the P-wave velocity by porosities. It indicates that the water in the coal samples weakens the influence of coal porosity on the P-wave velocity. The waveform frequency distributions differ dramatically during the whole process of water absorption of coal samples. The main frequency moves towards the low frequency nonlinearly with the increase of water saturation. The higher the water saturation and the porosities of coal,the smaller the maximum amplitudes of waveforms are. The energy distribution of wave frequency bands and the temporal changing characteristics of the waveform signals can be revealed by the three-dimensional Hilbert spectrums of energy. With the increase of the water saturation,the proportion of the high frequency component reduces gradually,and the frequency bands with the high energy move to the low frequency. It means that the pore water in the porous coal structure not only speeds up the energy attenuation of all frequency bands,but also makes the attenuation of high frequency components greater than the low-frequency components.
李 楠1,2,张 新1,2,王达轩2,赵星智2,李 松3. 煤样吸水全过程纵波波速变化规律及波形特征实验研究[J]. 岩石力学与工程学报, 2017, 36(8): 1921-1929.
LI Nan1,2,ZHANG Xin1,2,WANG Daxuan2,ZHAO Xingzhi2,LI Song3. Experimental study on the variation of P-wave velocity and waveform characteristics during the whole process of water absorption of coal samples. , 2017, 36(8): 1921-1929.
[1] GE M C. Efficient mine microseismic monitoring[J]. International Journal of Coal Geology,2005,64(8):44–56.
[2] 窦林名,牟宗龙,陆菜平,等. 采矿地球物理理论与技术[M]. 北京:科学出版社,2014:28–29.(DOU Linming,MU Zonglong,LU Caiping,et al. Mine geophysical theory and technology[M]. Beijing:Science Press,2014:28–29.(in Chinese))
[3] 王贵宾,杨春和,郭应同,等. 川东北地区岩石纵波速度分布特征和影响因素的试验研究[J]. 岩石力学与工程学报,2011, 30(增1):2 834–2 842.(WANG Guibin,YANG Chunhe,GUO Yingtong,et al. Experimental research on distribution characteristic and influential factors of P-wave velocity for rocks in Northeast region of Sichuan province[J]. Chinese Journal of Rock Mechanics and Engineering,2011,30(Supp.1):2 834–2 842.(in Chinese))
[4] 彭苏萍,谢和平,何满潮,等. 沉积相变岩体声波速度特征的试验研究[J]. 岩石力学与工程学报,2005,24(16):2 831–2 837. (PENG Suping,XIE Heping,HE Manchao,et al. Experimental study on velocity characteristic of lithofacies transition rock mass[J]. Chinese Journal of Rock Mechanics and Engineering,2005,24(16):2 831–2 837.(in Chinese))
[5] 孟召平,张吉昌,JOACHIM T. 煤系岩石物理力学参数与声波速度之间的关系[J]. 地球物理学报,2006,49(5):1 505–1 510. (MENG Zhaoping,ZHANG Jichang,JOACHIM T. Relationship between physical and mechanical parameters and acoustic wave velocity of coal measures rocks[J]. Chinese Journal of Geophisics,2006,49(5):1 505–1 510.(in Chinese))
[6] 陈 旭,俞 缙,李 宏,等. 不同岩性及含水率的岩石声波传播规律试验研究[J]. 岩土力学,2013,34(9):2 527–2 533.(CHEN Xu,YU Jin,LI Hong,et al. Experimental study of propagation characteristics of acoustic wave in rocks with different lithologies and water contents[J]. Rock and Soil Mechanics,2013,34(9):2 527–2 533.(in Chinese))
[7] 孟召平,刘常青,贺小黑,等. 煤系岩石声波速度及其影响因素实验分析[J]. 采矿与安全工程学报,2008,25(4):389–393.(MENG Zhaoping,LIU Changqing,HE Xiaohei,et al. Experimental research on acoustic wave velocity of coal measures rocks and its influencing factors[J]. Journal of Mining and Safety Engineering,2008,25(4):389–393.(in Chinese))
[8] 李浩然,杨春和,李佰林,等. 三轴多级荷载下盐岩声波声发射特征与损伤演化规律研究[J]. 岩石力学与工程学报,2016,35(4):682–691.(LI Haoran,YANG Chunhe,LI Bailin,et al. Damage evolution and characteristics of ultrasonic velocity and acoustic emission for salt rock under triaxial multilevel loading test[J]. Chinese Journal of Rock Mechanics and Engineering,2016,35(4):682–691.(in Chinese))
[9] 陈 颙. 声发射技术在岩石力学研究中的应用[J]. 地球物理学报,1977,20(4):312–322.(CHEN Yong. Application of acoustic emission techniques to rock mechanics research[J]. Chinese Journal of Geophysics,1977,20(4):312–322.(in Chinese))
[10] 陈 颙,杨咸武,韩 彪. 变形过程中岩石P波速度场的空间变化[J]. 地震学报,1990,12(1):54–62.(CHEN Yong,YANG Xianwu,HAN Biao. Spatial velocity variations of P waves during rock deformations[J]. Acta Geophysica Sinica,1990,12(1):54–62.(in Chinese))
[11] 郑贵平,赵兴东,刘建坡,等. 岩石加载过程声波波速变化规律实验研究[J]. 东北大学学报:自然科学版,2009,30(8):1 197–1 200.(ZHENG Guiping,ZHAO Xingdong,LIU Jianpo,et al. Experimental study on change in acoustic wave velocity when rock is loading[J]. Journal of Northeastern University:Natural Science,2009,30(8):1 197–1 200.(in Chinese))
[12] 王 赟,许小凯,张玉贵. 六种不同变质程度煤的纵横波速度特征及其与密度的关系[J]. 地球物理学报,2012,55(11):3 754–3 761. (WANG Yun,XU Xiaokai,ZHANG Yugui. Characteristics of P-wave and S-wave velocities and their relationships with density of 6 metamorphic kinds of coal[J]. Chinese Journal of Geophysics,2012,55(11):3 754–3 761.(in Chinese))
[13] WYLLIE M R J,GREGORY A R,GARDNER L W,Elastic wave velocities in heterogeneous and porous media[J]. Geophysics,1956,21(1):41–70.
[14] 杨为民,宋 杰,刘 斌,等. 饱水过程中类岩石材料波速和电阻率变化规律及其相互关系试验研究[J]. 岩石力学与工程学报,2015,34(4):703–712.(YANG Weimin,SONG Jie,LIU Bin,et al. Experimental research on wave velocity and electrical resistivity of rock-like material during saturation process[J]. Chinese Journal of Rock Mechanics and Engineering,2015,34(4):703–712.(in Chinese))
[15] 史 謌,沈文略,杨东全. 岩石弹性波速度和饱和度、孔隙流体分布的关系[J]. 地球物理学报,2003,46(1):138–142.(SHI Ge,SHEN Wenlue,YANG Dongquan. The relationship of wave velocities with saturation and fluid distribution in pore space[J]. Chinese Journal of Geophysics,2003,46(1):138–142.(in Chinese))
[16] 邓华锋,原先凡,李建林,等. 饱水度对砂岩纵波波速及强度影响的试验研究[J]. 岩石力学与工程学报,2013,32(8):1 625–1 631. (DENG Huafeng,YUAN Xianfan,LI Jianlin,et al. Experimental research on influence of saturation degree on sandstone longitudinal wave velocity and strengths[J]. Chinese Journal of Rock Mechanics and Engineering,2013,32(8):1 625–1 631.(in Chinese))
[17] KAHRAMAN S. The correlations between the saturated and dry P-wave velocity of rocks[J]. Ultrasonics,2007,46(4):341–348.
[18] 王 东,张海澜,王秀明. 部分饱和孔隙岩石中声波传播数值研究[J]. 地球物理学报,2006,49(2):524–532.(WANG Dong,ZHANG Hailan,WANG Xiuming. A numerical study of acoustic wave propagation in partially saturated poroelastic rock[J]. Chinese Journal of Geophysics,2006,49(2):524–532.(in Chinese))
[19] 周治国,朱合华,陈 伟. 饱水岩样声波传播规律的试验研究[J]. 岩石力学与工程学报,2006,25(5):911–917.(ZHOU Zhiguo,ZHU Hehua,CHEN Wei. Experimental study on acoustic wave propagation character of water saturated rock samples[J]. Chinese Journal of Rock Mechanics and Engineering,2006,25(5):911–917.(in Chinese))
[20] 王云刚,李满贵,陈兵兵,等.干燥及饱和含水煤样超声波特征的实验研究[J]. 煤炭学报,2015,40(10):2 445–2 450.(WANG Yungang,LI Mangui,CHEN Bingbing,et al.Experimental study on ultrasonic wave characteristics of coal samples under dry and water saturated conditions[J]. Journal of China Coal Society,2015,40(10):2 445–2 450.(in Chinese))
[21] 史 謌. 岩石含水饱和度、频率、流体类型对声波振幅影响规律的探讨[J]. 北京大学学报:自然科学版,1993,29(4):458–465.(SHI Ge. The investigation of the influence of the degree of saturation,frequency and fluid type on the sonic wave amplitude in sandstone [J]. Acta Scientiarum Naturalium Universitatis Pekinensis,1993,29(4):458–465.(in Chinese))
[22] HUANG N E,SHEN Z,LONG S R. A new view of nonlinear water waves:the Hilbert spectrum[J]. Annual Review of Fluid Mechanics,1999,31:417–457.