Evaluation of the characterization of acoustic emission of brittle rocks from the experiment to numerical simulation

被引:27
作者
Bu, Fengchang [1 ,2 ,3 ]
Xue, Lei [1 ,2 ,3 ]
Zhai, Mengyang [1 ,2 ,3 ]
Huang, Xiaolin [1 ,2 ,3 ]
Dong, Jinyu [4 ]
Liang, Ning [1 ,2 ,3 ]
Xu, Chao [1 ,2 ,3 ]
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Shale Gas & Geoengn, Beijing 100029, Peoples R China
[2] Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
[3] Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
[4] North China Univ Water Resources & Elect Power, Res Inst Geotech Engn & Hydraul Struct, Zhengzhou 450046, Peoples R China
基金
中国国家自然科学基金;
关键词
PARTICLE MODEL; B-VALUE; FRACTURE; FAILURE; DAMAGE; COMPRESSION; BEHAVIOR; CRACKING; STRAIN; ENERGY;
D O I
10.1038/s41598-021-03910-8
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Acoustic emission (AE) characterization is an effective technique to indirectly capture the failure process of quasi brittle rock. In previous studies, both experiments and numerical simulations were adopted to investigate the AE characteristics of rocks. However, as the most popular numerical model, the moment tensor model (MTM) cannot be constrained by the experimental result because there is a gap between MTM and experiments in principle, signal processing and energy analysis. In this paper, we developed a particle-velocity-based model (PVBM) that enabled direct monitoring and analysis of the particle velocity in the numerical model and had good robustness. The PVBM imitated the actual experiment and could fill in gaps between the experiment and MTM. AE experiments of marine shale under uniaxial compression were carried out, and the results were simulated by MTM. In general, the variation trend of the experimental result could be presented by MTM. Nevertheless, the magnitudes of AE parameters by MTM presented notable differences of more than several orders of magnitude compared with those by the experiment. We sequentially used PVBM as a proxy to analyse these discrepancies and systematically evaluate the AE characterization of rocks from the experiment to numerical simulation, considering the influence of wave reflection, energy geometrical diffusion, viscous attenuation, particle size and progressive deterioration of rock material. The combination of MTM and PVBM could reasonably and accurately acquire AE characteristics of the actual AE experiment of rocks by making full use of their respective advantages.
引用
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页数:16
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