Microscopic Investigation of Rate Dependence on Three-Point Notched-Tip Bending Sandstone

The cracking process in rock or concrete is usually characterized by the formation of microcracks that eventually form a propagating macrocrack. A series of three-point bending experiments were performed on sandstone containing Mode I crack under different loading rates. The microscopic monitoring s...

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Main Authors: Wenshuai Li, Faiz U. A. Shaikh, Lianguo Wang, Yinlong Lu, Kai Wang, Zhaolin Li
Format: Article
Language:English
Published: Hindawi Limited 2019-01-01
Series:Shock and Vibration
Online Access:http://dx.doi.org/10.1155/2019/4525162
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spelling doaj-9d91aebbf6e146cb92d1287e5ce9c3eb2020-11-25T01:13:42ZengHindawi LimitedShock and Vibration1070-96221875-92032019-01-01201910.1155/2019/45251624525162Microscopic Investigation of Rate Dependence on Three-Point Notched-Tip Bending SandstoneWenshuai Li0Faiz U. A. Shaikh1Lianguo Wang2Yinlong Lu3Kai Wang4Zhaolin Li5State Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xuzhou, Jiangsu 221116, ChinaDepartment of Civil Engineering, Curtin University, Perth, WA 6102, AustraliaState Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xuzhou, Jiangsu 221116, ChinaState Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xuzhou, Jiangsu 221116, ChinaState Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xuzhou, Jiangsu 221116, ChinaState Key Laboratory for Geomechanics and Deep Underground Engineering, China University of Mining and Technology, Xuzhou, Jiangsu 221116, ChinaThe cracking process in rock or concrete is usually characterized by the formation of microcracks that eventually form a propagating macrocrack. A series of three-point bending experiments were performed on sandstone containing Mode I crack under different loading rates. The microscopic monitoring system was established to capture the cracking process at notch tip. The loading rate dependence of microcracking behaviour was analysed based on load-time curves, acoustic emission (AE), microscopic images, and micrograph-based digital image correlation (DIC) technology. Results showed that the specimens underwent a short period of compression and elastic deformation stage under high loading rate, and the peak loads increased with the increase in loading rate. The AE results revealed that the fracturing process can be divided into elastic stage, damage stage, and postpeak stage, and more extensive damage occurred before the peak under low loading rate. It can be observed from microscopic images that the crack was initiated during the elastic stage, which was earlier than that determined from the AE monitoring. In addition, the microcracks were initiated at multiple locations and were mainly located at the interfaces between dense grains under low loading rate, while microcracks were observed inside the grains under high loading rate. Furthermore, the DIC results showed that the crack opening displacement (COD) of 0.6 mm/min at the peak was almost twice than that of 3.0 mm/min. The COD under the same loading rate at the peak can be considered as the material property of sandstone.http://dx.doi.org/10.1155/2019/4525162
collection DOAJ
language English
format Article
sources DOAJ
author Wenshuai Li
Faiz U. A. Shaikh
Lianguo Wang
Yinlong Lu
Kai Wang
Zhaolin Li
spellingShingle Wenshuai Li
Faiz U. A. Shaikh
Lianguo Wang
Yinlong Lu
Kai Wang
Zhaolin Li
Microscopic Investigation of Rate Dependence on Three-Point Notched-Tip Bending Sandstone
Shock and Vibration
author_facet Wenshuai Li
Faiz U. A. Shaikh
Lianguo Wang
Yinlong Lu
Kai Wang
Zhaolin Li
author_sort Wenshuai Li
title Microscopic Investigation of Rate Dependence on Three-Point Notched-Tip Bending Sandstone
title_short Microscopic Investigation of Rate Dependence on Three-Point Notched-Tip Bending Sandstone
title_full Microscopic Investigation of Rate Dependence on Three-Point Notched-Tip Bending Sandstone
title_fullStr Microscopic Investigation of Rate Dependence on Three-Point Notched-Tip Bending Sandstone
title_full_unstemmed Microscopic Investigation of Rate Dependence on Three-Point Notched-Tip Bending Sandstone
title_sort microscopic investigation of rate dependence on three-point notched-tip bending sandstone
publisher Hindawi Limited
series Shock and Vibration
issn 1070-9622
1875-9203
publishDate 2019-01-01
description The cracking process in rock or concrete is usually characterized by the formation of microcracks that eventually form a propagating macrocrack. A series of three-point bending experiments were performed on sandstone containing Mode I crack under different loading rates. The microscopic monitoring system was established to capture the cracking process at notch tip. The loading rate dependence of microcracking behaviour was analysed based on load-time curves, acoustic emission (AE), microscopic images, and micrograph-based digital image correlation (DIC) technology. Results showed that the specimens underwent a short period of compression and elastic deformation stage under high loading rate, and the peak loads increased with the increase in loading rate. The AE results revealed that the fracturing process can be divided into elastic stage, damage stage, and postpeak stage, and more extensive damage occurred before the peak under low loading rate. It can be observed from microscopic images that the crack was initiated during the elastic stage, which was earlier than that determined from the AE monitoring. In addition, the microcracks were initiated at multiple locations and were mainly located at the interfaces between dense grains under low loading rate, while microcracks were observed inside the grains under high loading rate. Furthermore, the DIC results showed that the crack opening displacement (COD) of 0.6 mm/min at the peak was almost twice than that of 3.0 mm/min. The COD under the same loading rate at the peak can be considered as the material property of sandstone.
url http://dx.doi.org/10.1155/2019/4525162
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