Suppr超能文献

从实验到数值模拟对脆性岩石声发射特性的评估。

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

作者信息

Bu Fengchang, Xue Lei, Zhai Mengyang, Huang Xiaolin, Dong Jinyu, Liang Ning, Xu Chao

机构信息

Key Laboratory of Shale Gas and Geoengineering, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China.

Innovation Academy for Earth Science, Chinese Academy of Sciences, Beijing, 100029, China.

出版信息

Sci Rep. 2022 Jan 11;12(1):498. doi: 10.1038/s41598-021-03910-8.

Abstract

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.

摘要

声发射(AE)表征是间接捕捉准脆性岩石破坏过程的一种有效技术。在以往的研究中,采用实验和数值模拟相结合的方法来研究岩石的声发射特性。然而,作为最常用的数值模型,矩张量模型(MTM)无法受实验结果的约束,因为MTM与实验在原理、信号处理和能量分析方面存在差距。在本文中,我们开发了一种基于粒子速度的模型(PVBM),该模型能够在数值模型中直接监测和分析粒子速度,并且具有良好的鲁棒性。PVBM模拟了实际实验,能够填补实验与MTM之间的差距。开展了海相页岩单轴压缩下的声发射实验,并采用MTM对结果进行了模拟。总体而言,MTM能够呈现实验结果的变化趋势。然而,MTM得到的声发射参数幅值与实验结果相比存在显著差异,相差几个数量级。我们依次用PVBM来分析这些差异,并系统地评估从实验到数值模拟过程中岩石的声发射表征,同时考虑波反射、能量几何扩散、粘性衰减、颗粒尺寸和岩石材料的渐进劣化等因素的影响。MTM和PVBM相结合,充分利用各自的优势,可以合理、准确地获取岩石实际声发射实验的声发射特性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1884/8752740/c5d7f339d804/41598_2021_3910_Fig1_HTML.jpg

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验