Avalanches in Compressed Sandstone: Crackling Noise under Confinement

The acoustic emission, AE, from avalanches of local cracks and microstructural changes of sandstone under confined compression have been reported. These avalanches soften the underlying minerals and play a key role as indicators for the prediction of geo-engineering disasters, such as mining collaps...

Full description

Bibliographic Details
Main Authors: Yunfeng Zhao, Hanlong Liu, Kainan Xie, Ekhard K.H. Salje, Xiang Jiang
Format: Article
Language:English
Published: MDPI AG 2019-11-01
Series:Crystals
Subjects:
Online Access:https://www.mdpi.com/2073-4352/9/11/582
_version_ 1828353969928273920
author Yunfeng Zhao
Hanlong Liu
Kainan Xie
Ekhard K.H. Salje
Xiang Jiang
author_facet Yunfeng Zhao
Hanlong Liu
Kainan Xie
Ekhard K.H. Salje
Xiang Jiang
author_sort Yunfeng Zhao
collection DOAJ
description The acoustic emission, AE, from avalanches of local cracks and microstructural changes of sandstone under confined compression have been reported. These avalanches soften the underlying minerals and play a key role as indicators for the prediction of geo-engineering disasters, such as mining collapses, rock outbursts caused by high ground stress, and man-made quakes by fracking. Compressed sandstone is a model material for the investigation of avalanches. The avalanche energies, amplitudes, and waiting times show the probability distributions that allow us to distinguish between three compression stages; namely, (I) pre-failure, (II) correlated failure, and (III) post-failure. The energy of stage I and stage II is power-law distributed and scale invariant, while post-failure experiments show power laws with high exponential damping (friction). The scaling behavior is close to the predictions of a mean-field (MF) model (stage II) and a force-integrated mean-field model (stage I). Confinement shifts the value of the energy exponent closer to the MF prediction. Omori’s law and waiting time distributions are independent of stress during the compression; their scaling exponents are very similar to those found in seismological studies.
first_indexed 2024-04-14T02:15:53Z
format Article
id doaj.art-d6cfba05cda643d1807ea6d3c6074282
institution Directory Open Access Journal
issn 2073-4352
language English
last_indexed 2024-04-14T02:15:53Z
publishDate 2019-11-01
publisher MDPI AG
record_format Article
series Crystals
spelling doaj.art-d6cfba05cda643d1807ea6d3c60742822022-12-22T02:18:12ZengMDPI AGCrystals2073-43522019-11-0191158210.3390/cryst9110582cryst9110582Avalanches in Compressed Sandstone: Crackling Noise under ConfinementYunfeng Zhao0Hanlong Liu1Kainan Xie2Ekhard K.H. Salje3Xiang Jiang4School of Civil Engineering, Chongqing University, Chongqing 400044, ChinaSchool of Civil Engineering, Chongqing University, Chongqing 400044, ChinaState Key Laboratory of Coal Mine Disaster Dynamics and Control, Chongqing University, Chongqing 400044, ChinaDepartment of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UKSchool of Civil Engineering, Chongqing University, Chongqing 400044, ChinaThe acoustic emission, AE, from avalanches of local cracks and microstructural changes of sandstone under confined compression have been reported. These avalanches soften the underlying minerals and play a key role as indicators for the prediction of geo-engineering disasters, such as mining collapses, rock outbursts caused by high ground stress, and man-made quakes by fracking. Compressed sandstone is a model material for the investigation of avalanches. The avalanche energies, amplitudes, and waiting times show the probability distributions that allow us to distinguish between three compression stages; namely, (I) pre-failure, (II) correlated failure, and (III) post-failure. The energy of stage I and stage II is power-law distributed and scale invariant, while post-failure experiments show power laws with high exponential damping (friction). The scaling behavior is close to the predictions of a mean-field (MF) model (stage II) and a force-integrated mean-field model (stage I). Confinement shifts the value of the energy exponent closer to the MF prediction. Omori’s law and waiting time distributions are independent of stress during the compression; their scaling exponents are very similar to those found in seismological studies.https://www.mdpi.com/2073-4352/9/11/582sandstoneacoustic emissioncrackling noisemean-field model
spellingShingle Yunfeng Zhao
Hanlong Liu
Kainan Xie
Ekhard K.H. Salje
Xiang Jiang
Avalanches in Compressed Sandstone: Crackling Noise under Confinement
Crystals
sandstone
acoustic emission
crackling noise
mean-field model
title Avalanches in Compressed Sandstone: Crackling Noise under Confinement
title_full Avalanches in Compressed Sandstone: Crackling Noise under Confinement
title_fullStr Avalanches in Compressed Sandstone: Crackling Noise under Confinement
title_full_unstemmed Avalanches in Compressed Sandstone: Crackling Noise under Confinement
title_short Avalanches in Compressed Sandstone: Crackling Noise under Confinement
title_sort avalanches in compressed sandstone crackling noise under confinement
topic sandstone
acoustic emission
crackling noise
mean-field model
url https://www.mdpi.com/2073-4352/9/11/582
work_keys_str_mv AT yunfengzhao avalanchesincompressedsandstonecracklingnoiseunderconfinement
AT hanlongliu avalanchesincompressedsandstonecracklingnoiseunderconfinement
AT kainanxie avalanchesincompressedsandstonecracklingnoiseunderconfinement
AT ekhardkhsalje avalanchesincompressedsandstonecracklingnoiseunderconfinement
AT xiangjiang avalanchesincompressedsandstonecracklingnoiseunderconfinement