Definition and classification of rockburst

IF 8
Rock Mechanics Bulletin Pub Date : 2025-07-01 Epub Date: 2025-04-26 DOI:10.1016/j.rockmb.2025.100206
Manchao He , Ismet Canbulat , Fidelis T. Suorineni , Murat Karakus , Wen Nie , Dongqiao Liu , Chengguo Zhang , Alexey Nagibin , Bauyrzhan Rustembek
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Abstract

The rockburst is a violent failure in rock during mining and tunneling operations. Since tunnel constructions for hydropower and transportation purposes and mining operations in deep rock masses have been increasing recently, more frequent rockburst cases have been reported. This paper proposes a new definition for rockburst, considering the main components of the rockburst along with triggering mechanisms and reasons. For this purpose, the historical definitions of rockburst and its related classifications have been reviewed. In terms of triggering mechanisms, a rockburst must be induced by excavation resulting from three effects arising from the transition of stress state from 3- to 1-dimension, such as the transient radial stress loss, the time-dependent tangential stress increase, and the peak strength drop, which are explained by examining the stress transition in the shear stress vs normal stress space and energy transition in the stress-strain space. Based on the understanding of the three effects of excavation, a new definition of rockburst is proposed: “A rockburst is a sudden failure of rock mass surrounding the excavations caused by the rapid release of stored energy when induced stresses exceed the rock strength”. Additionally, rockbursts are classified according to transitions in the static and dynamic stress fields, with further subclassifications into instantaneous and delayed bursts based on the timing of occurrences relative to radial stress drop and tangential stress increase. Rockburst management strategies are also proposed to address stress and energy transitions in excavations.
岩爆的定义和分类
岩爆是在采矿和隧道施工过程中岩石发生的剧烈破坏。近年来,随着水电、交通等隧洞建设和深部岩体采矿作业的增加,岩爆事故也越来越多。本文从岩爆的主要组成、触发机制和原因出发,提出了岩爆的新定义。为此,本文回顾了岩爆的历史定义及其相关分类。在触发机制上,应力状态从三维向一维转变所产生的径向瞬态应力损失、随时间变化的切向应力增加和峰值强度下降三种效应必然会导致开挖诱发岩爆,这可以通过考察剪应力-法向应力空间的应力转变和应力-应变空间的能量转变来解释。在认识开挖三种效应的基础上,提出了岩爆的新定义:“岩爆是指当诱导应力超过岩石强度时,由于储存的能量迅速释放而引起的开挖周围岩体的突然破坏”。此外,岩爆根据静态和动态应力场的转变进行分类,并根据相对于径向应力下降和切向应力增加的发生时间进一步细分为瞬时岩爆和延迟岩爆。针对开挖过程中的应力和能量转换,提出了岩爆管理策略。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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CiteScore
2.40
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