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Engineering Fracture Mechanics
journal homepage: www.elsevier.com/locate/engfracmech
Review of unloading tests of dynamic rock failure in compression
Hongyu Wang
a
, Arcady Dyskin
a,
⁎
, Phil Dight
b
, Elena Pasternak
c
, Ariel Hsieh
b
a
Department of Civil, Environmental and Mining Engineering, School of Engineering, University of Western Australia, 35 Stirling Highway, Crawley,
WA 6009, Australia
b
Australian Centre for Geomechanics, University of Western Australia, 35 Stirling Highway, Crawley, WA 6009, Australia
c
Department of Mechanical Engineering, School of Engineering, University of Western Australia, 35 Stirling Highway, Crawley, WA 6009, Australia
ARTICLE INFO
Keywords:
True triaxial unloading test
Shear stress
End friction effect
Fracture growth
Fracture shape
ABSTRACT
Dynamic rock failure at the walls of an opening, so-called rock burst or strain burst is one of the
major types of rock failure capable of causing human and financial loss. Initially the rock at the
place of the future excavation is in a polyaxial stress state. When excavating an opening, the rock
elements at the excavation boundary are overloaded in the tangential (with respect to excavation
wall) direction and unloaded in the radial direction. This situation can be reproduced by the
modified true triaxial test in which only one surface of prismatic rock sample is unloaded. This
paper reviews the tests under true triaxial unloading condition and the corresponding failure
modes and types (static or dynamic). In these tests the violent (dynamic) ejection of rock frag-
ments and arc-shape fractures near the free face are often observed. However these tests are
affected by friction between the sample and the loading platens. We analyse the end friction
effect and show that unlike the conventional end friction effect produced in uniaxial and biaxial
loading tests, the true triaxial unloading test induces additional shear stress needed to prevent
sliding of the rock sample from the loading platens. This additional shear stress is shown to
considerably affect the geometry of fractures.
1. Introduction
The surface failure at the excavation surface can be nonviolent or violent, i.e. spalling (slabbing) and skin (strain) rockburst,
respectively. According to the first analysis by Fairhurst and Cook [1], spalling is the failure process involves extensional splitting/
cracking during the excavation of deep tunnels under high-stress conditions. In the course of skin rockburst or strainburst, fragments
of rock, usually in the form of thin plates with very sharp edges, are violently ejected locally from the rock surface [2,3]. Spalling and
strainburst are more likely to occur in more massive rock types than in significantly jointed and fractured rock masses [4–7]. Spalling
and strainburst represent a significant hazard and a danger to the safety of personnel and infrastructure in civil engineering ex-
cavations and deep underground mines.
Understanding of the rock failure behaviour near the excavation boundary is critical for the design of a tunnelling and under-
ground mining. Excavation of an opening leads to the in-situ stress redistribution. The stress concentration near the excavation
surface manifests itself in the reduction of the radial stress component, which is zero at the surface and a considerable increase of the
tangential stress component, which may lead to slabbing and strainburst [2,6,8]. Many researchers have studied the rock failure
behaviour near the excavation boundary by conducting uniaxial compression tests [9–11], biaxial compression tests [12–14] and
surface instability tests [15–18].
https://doi.org/10.1016/j.engfracmech.2018.12.022
Received 29 August 2018; Received in revised form 27 November 2018; Accepted 18 December 2018
⁎
Corresponding author.
E-mail address: arcady.dyskin@uwa.edu.au (A. Dyskin).
Engineering Fracture Mechanics xxx (xxxx) xxx–xxx
0013-7944/ © 2018 Elsevier Ltd. All rights reserved.
Please cite this article as: Wang, H., Engineering Fracture Mechanics, https://doi.org/10.1016/j.engfracmech.2018.12.022