4.7 Article

An Experimental and Numerical Study on Cracking Behavior of Brittle Sandstone Containing Two Non-coplanar Fissures Under Uniaxial Compression

期刊

ROCK MECHANICS AND ROCK ENGINEERING
卷 49, 期 4, 页码 1497-1515

出版社

SPRINGER WIEN
DOI: 10.1007/s00603-015-0838-3

关键词

Brittle sandstone; Two non-coplanar fissures; Crack initiation; Crack coalescence; Tensile crack

资金

  1. Program for New Century Excellent Talents in University [NCET-12-0961]
  2. National Natural Science Foundation of China [51179189]
  3. Fundamental Research Funds for the Central Universities (China University of Mining and Technology) [2014YC10]
  4. Outstanding Innovation Team Project in China University of Mining and Technology [2014QN002]
  5. Team Project - Jiangsu Innovation and Entrepreneurship Program
  6. Natural Science Foundation of Jiangsu Province for Distinguished Young Scholars [BK20150005]

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To understand the fracture mechanism in all kinds of rock engineering, it is important to investigate the fracture evolution behavior of pre-fissured rock. In this research, we conducted uniaxial compression experiments to evaluate the influence of ligament angle on the strength, deformability, and fracture coalescence behavior of rectangular prismatic specimens (80 x 160 x 30 mm) of brittle sandstone containing two non-coplanar fissures. The experimental results show that the peak strength of sandstone containing two non-coplanar fissures depends on the ligament angle, but the elastic modulus is not closely related to the ligament angle. With the increase of ligament angle, the peak strength decreased at a ligament angle of 60A degrees, before increasing up to our maximum ligament angle of 120A degrees. Crack initiation, propagation, and coalescence were all observed and characterized from the inner and outer tips of pre-existing non-coplanar fissures using photographic monitoring. Based on the results, the sequence of crack evolution in sandstone containing two non-coplanar fissures was analyzed in detail. In order to fully understand the crack evolution mechanism of brittle sandstone, numerical simulations using PFC2D were performed for specimens containing two non-coplanar fissures under uniaxial compression. The results are in good agreement with the experimental results. By analyzing the stress field, the crack evolution mechanism in brittle sandstone containing two non-coplanar fissures under uniaxial compression is revealed. These experimental and numerical results are expected to improve the understanding of the unstable fracture mechanism of fissured rock engineering structures.

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