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ORIGINAL RESEARCH article
Front. Earth Sci.
Sec. Geohazards and Georisks
Volume 13 - 2025 | doi: 10.3389/feart.2025.1544660
This article is part of the Research Topic Understanding Geomaterial Instability: Physics and Mechanics of Landslides and Seismic Events View all 13 articles
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Seismic activities often trigger catastrophic events including collapses and rockfalls on rocky slopes. This research endeavors to understand the dynamic behavior and damage modes in uniform rocky slopes with unstable rock masses. To achieve this objective, the paper constructs a physical model of uniform rocky slope with unstable rock mass and performs triaxial loading shaking table tests. Subsequently, the seismo-dynamic responses and associated damage modes of the slope are scrutinized, and the initiation and deformation mechanisms of the hazardous rock are revealed. Further, we obtained the marginal spectral energy evolution characteristics of measurement points of both the unstable rock and bedrock. This deciphers the damage evolution characteristics of the weak structural plane. The results indicate that there are distinct elevation and surface amplification effects within the rock slopes, which systematically lessened with increasing seismic intensity. The vertical deformation of unstable rock mass is more sensitive to high seismic intensity. The seismic-induced initiation process of unstable rock masses is split into three stages: trailing edge tension cracking, sliding damage of structural planes, and a complete failure of structural plane shear capacity. It is also established that the Hilbert and marginal spectra effectively identified the damage process of unstable rock masses containing weak structural planes.
Keywords: HHT transformation, Shaking table tests, Marginal spectrum, Rocky slope, Unstable rock mass
Received: 13 Dec 2024; Accepted: 17 Feb 2025.
Copyright: © 2025 Wang and Wen. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
* Correspondence:
Hao Wen, Southwest Jiaotong University, Chengdu, China
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