Shear characteristics and shear strength model of rock mass structural planes.


Journal

Scientific reports
ISSN: 2045-2322
Titre abrégé: Sci Rep
Pays: England
ID NLM: 101563288

Informations de publication

Date de publication:
10 Aug 2022
Historique:
received: 13 02 2022
accepted: 03 08 2022
entrez: 10 8 2022
pubmed: 11 8 2022
medline: 11 8 2022
Statut: epublish

Résumé

Accurately determining the shear strength of structural planes is crucial for evaluating the stability of rock masses. The shear test using the sawtooth structural plane usually captures the main influencing factors of its shear characteristics. In this study, the two-dimensional particle flow code (PFC2D) numerical simulation method was used to conduct shear tests on the sawtooth structural planes of rock masses with undulant angles of 10°, 20°, and 30°, respectively. With the increase in normal stress and the undulant angle, the shear failure of the structural planes was found to no longer be pure slip failure or shear failure but accompanied by a compression-induced fracture phenomenon. Based on the analysis of the shear test results, a peak shear strength model considering different undulant angles and normal stresses was proposed, and the hyperbolic function post-peak shear strength model was improved. The peak shear strength obtained from the physical direct shear tests was compared with those calculated using the proposed model, Parton model, and Shen model. The calculation error under low and high normal stress of the proposed method was found to be within an acceptable range. Additionally, when calculating the peak shear strength of a structural plane under high normal stress, applying the calculation method proposed in this study is a better option than applying the other models. Furthermore, although the variation trend of the post-peak shear strength was similar to that of the experimental results, the values obtained using the hyperbolic variation model were too large. The variation trend of the post-peak shear strength obtained using the improved function was essentially consistent with the experimental results, and the calculated values were close to the experimental results. The systematic research on the shear strength calculation model of rock mass structural planes contributes to the theoretical research of rock mass mechanics, and this study can act as a guide for landslide prediction and control projects.

Identifiants

pubmed: 35948621
doi: 10.1038/s41598-022-17998-z
pii: 10.1038/s41598-022-17998-z
pmc: PMC9365770
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

13637

Subventions

Organisme : the open fund of state key laboratory of geohazard prevention and geoenvironment protection
ID : SKLGP2020K015
Organisme : the open fund of state key laboratory of geohazard prevention and geoenvironment protection
ID : SKLGP2020K015
Organisme : the open fund of state key laboratory of geohazard prevention and geoenvironment protection
ID : SKLGP2020K015
Organisme : the open fund of state key laboratory of geohazard prevention and geoenvironment protection
ID : SKLGP2020K015
Organisme : the open fund of state key laboratory of geohazard prevention and geoenvironment protection
ID : SKLGP2020K015
Organisme : the open fund of state key laboratory of geohazard prevention and geoenvironment protection
ID : SKLGP2020K015
Organisme : Chongqing Geological Disaster Prevention and Control Center of China
ID : 20C0023
Organisme : Chongqing Geological Disaster Prevention and Control Center of China
ID : 20C0023
Organisme : Chongqing Geological Disaster Prevention and Control Center of China
ID : 20C0023
Organisme : Chongqing Geological Disaster Prevention and Control Center of China
ID : 20C0023
Organisme : Chongqing Geological Disaster Prevention and Control Center of China
ID : 20C0023
Organisme : Chongqing Geological Disaster Prevention and Control Center of China
ID : 20C0023

Informations de copyright

© 2022. The Author(s).

Références

Nature. 2006 Jan 5;439(7072):64-7
pubmed: 16397496

Auteurs

Shan Dong (S)

Badong National Observation and Research Station of Geohazards, China University of Geosciences, Wuhan, 430074, China. 529417548@qq.com.
Three Gorges Research Center for Geohazards, China University of Geosciences, Wuhan, 430074, China. 529417548@qq.com.

Yulin Peng (Y)

Badong National Observation and Research Station of Geohazards, China University of Geosciences, Wuhan, 430074, China.
Three Gorges Research Center for Geohazards, China University of Geosciences, Wuhan, 430074, China.

Zhichun Lu (Z)

Badong National Observation and Research Station of Geohazards, China University of Geosciences, Wuhan, 430074, China.
Three Gorges Research Center for Geohazards, China University of Geosciences, Wuhan, 430074, China.

Heng Zhang (H)

Badong National Observation and Research Station of Geohazards, China University of Geosciences, Wuhan, 430074, China.
Three Gorges Research Center for Geohazards, China University of Geosciences, Wuhan, 430074, China.

Weihua Hou (W)

Badong National Observation and Research Station of Geohazards, China University of Geosciences, Wuhan, 430074, China.
Three Gorges Research Center for Geohazards, China University of Geosciences, Wuhan, 430074, China.

Aijun Su (A)

Badong National Observation and Research Station of Geohazards, China University of Geosciences, Wuhan, 430074, China.
Three Gorges Research Center for Geohazards, China University of Geosciences, Wuhan, 430074, China.

Classifications MeSH