ISSN 2096-4498

   CN 44-1745/U

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Discussion on Identification and Classification Standards of High Geostress

  • GUO Limin ,
  • LI Guoliang ,
  • QI Zhanfeng ,
  • LI Fangfang ,
  • ZHANG Jing
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  • (1. State Key Laboratory of Intelligent Geotechnics and Tunnelling, Xi′an 710043, Shaanxi, China; 2. China Railway First Survey and Design Institute Group Co., Ltd., Xi′an 710043, Shaanxi, China)

Online published: 2025-10-20

Abstract

In response to the limited applicability of the currently accepted high-geostress criterion in soft surrounding rocks prone to large deformations and within a rock mass strength range of 15-60 MPa, the authors integrate in-situ testing, case history investigations, theoretical analyses, and finite-element modeling to develop an improved criterion applicable across the entire rock mass strength spectrum. The main conclusions are as follows: (1) The failure pattern of high-geostress tunnels is strongly controlled by the mechanical properties of the associated rock mass; within the 15-60 MPa strength range, relaxation-induced fracturing and excessive convergence predominate. (2) Based on energy principles, nonlinear energy conversion accompanying rock mass fracturing is revealed: energy dissipation during fragmentation initially increases and subsequently decreases with increasing rock mass strength and brittle-ductile transition index. This finding suggests an optimal rock mass strength and brittleness index. (3) A novel high-geostress criterion is proposed that is valid for all rock mass strengths, thereby providing a theoretical basis for hazard prevention and control in tunnel engineering under diverse geological conditions. These findings effectively overcome the limitations of existing criteria and provide clear engineering guidance.

Cite this article

GUO Limin , LI Guoliang , QI Zhanfeng , LI Fangfang , ZHANG Jing . Discussion on Identification and Classification Standards of High Geostress[J]. Tunnel Construction, 2025 , 45(10) : 1919 -1925 . DOI: 10.3973/j.issn.2096-4498.2025.10.010

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