Failure Mechanisms in Rock and Soil Masses Research

A Special Issue of Geotechnics (ISSN 2673-7094).

Deadline for manuscript submissions: 1 July 2027 | Viewed by 378

Editors

College of Geological Engineering and Geomatics, Chang’an University, Xi’an 710054, China
Interests: heterogeneous rocks; crack initiation and propagation; strength loss and mobilization; micro fracture mechanisms

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Guest Editor
School of Architecture and Civil Engineering, Xi’an University of Science and Technology, Xi’an, China
Interests: special geomechanics and engineering applications—frozen soil mechanics; loess mechanics; subgrade engineering; foundation pit engineering

Special Issue Information

Dear Colleagues,

The reliable prediction and control of failure in rock and soil masses remain central challenges in geotechnical engineering, spanning a vast range of scales—from microcrack initiation in laboratory specimens to massive landslides and collapses that threaten communities. Today, we are witnessing a surge in large‑scale human activities—such as high‑altitude railways, deep open‑pit mines, energy tunnels, and water diversion schemes—in environmentally fragile zones like the Qinghai–Tibet Plateau, where complex geological histories, active tectonics, and extreme climates interact with engineering disturbances in unpredictable ways. As infrastructure projects become more complex and extend into increasingly diverse geological settings, the spectrum of failure mechanisms continues to broaden. These include time-dependent creep, brittle fracture, strain softening, liquefaction, progressive slope deterioration, and coupled thermal–hydro-mechanical–chemical instabilities, to name but a few. Advances in experimental techniques, field instrumentation, numerical modeling, and data science now offer unprecedented opportunities to observe, simulate, and understand these processes in greater depth than ever before.

This Special Issue invites original contributions that expand our fundamental knowledge of how rock and soil masses deform and fail under various loading and environmental conditions. We aim to create a comprehensive collection that bridges theoretical analyses, laboratory experiments, long-term field observations, and advanced computational methods. While all high-quality submissions on failure mechanisms are welcome, we particularly encourage studies that address topics including (but not limited to) the following broad themes:

  • Fundamental mechanical behavior: constitutive modeling, strength and deformation characteristics, fracture toughness, damage evolution, and size effects in both rock and soil.
  • Experimental techniques and characterization: novel laboratory testing (including true triaxial, dynamic, and ultra-low-temperature tests), advanced imaging (CT, SEM, DIC), and in situ geophysical methods.
  • Multi-field coupling processes: hydro-mechanical, thermal–hydro-mechanical, and chemo-mechanical interactions; effects of pore pressure, freeze–thaw, wet–dry, and saline intrusion.
  • Natural and climate-driven geohazards: landslides, debris flows, slope instability under extreme rainfall, permafrost degradation, coastal erosion, and ice-related hazards.
  • Anthropogenic impacts and infrastructure: tunneling and excavation-induced ground movements, rock bursts and micro-seismicity, foundation instability, and large-scale mining or quarrying activities. This includes, as particular cases, projects in environmentally fragile regions (e.g., the Qinghai–Tibet Plateau), where high-altitude engineering, water diversion, and transport corridors impose unique stresses on sensitive geomaterials.
  • Failure of problematic and special geomaterials: collapsible soils (loess), frozen soils, saline soils, expansive clays, and residual soils—with emphasis on their moisture- and temperature-dependent failure modes.
  • Field monitoring and long-term observational studies: case histories, real-time sensor networks, fiber-optic sensing, InSAR, and automated warning systems that capture precursory deformation and enable the validation of predictive models.
  • Multi-scale and multi-physics modeling: continuum and discontinuum numerical methods (FEM, DEM, XFEM, hybrid approaches), machine learning-enhanced simulations, digital twins, probabilistic reliability analysis, and uncertainty quantification.

We strongly encourage submissions that combine two or more of these perspectives—for instance, linking long-term monitoring data with advanced constitutive models, or integrating laboratory findings with field-scale hazard assessments. By presenting a diverse and inclusive view of failure mechanisms across different geomaterials, loading conditions, and environmental contexts, this Special Issue aims to foster interdisciplinary dialogue and translate fundamental insights into safer, more resilient engineering practices.

We look forward to receiving your contributions.

Dr. Shijie Liu
Dr. Pan Wang
Guest Editors

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Keywords

  • failure mechanisms
  • rock and soil mechanics
  • multi-field coupling (hydro-mechanical–thermal–chemical)
  • natural and anthropogenic geohazards
  • special geomaterials (frozen soil, loess, saline soil)
  • long-term field monitoring and in situ observation
  • large-scale engineering in fragile environments
  • numerical and experimental modeling
  • progressive failure and time-dependent behaviour
  • risk assessment and early warning

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Published Papers (1 paper)

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Research

19 pages, 15967 KB  
Article
Coupled Effects of Confining Pressure and Freeze–Thaw Cycles on Shear Strength and Deformation Characteristics of Moraine Soil
by Yuanyong Zeng and Xiewen Hu
Geotechnics 2026, 6(3), 87; https://doi.org/10.3390/geotechnics6030087 - 4 Sep 2026
Viewed by 141
Abstract
The mechanical properties of moraine soil in cold regions are significantly influenced by freeze–thaw cycles (FTCs). However, current understanding of the quantitative characteristics of its shear behavior under the coupled effect of FTCs and confining pressure is still insufficient. To address this, a [...] Read more.
The mechanical properties of moraine soil in cold regions are significantly influenced by freeze–thaw cycles (FTCs). However, current understanding of the quantitative characteristics of its shear behavior under the coupled effect of FTCs and confining pressure is still insufficient. To address this, a series of triaxial unconsolidated-undrained shear tests were conducted on saturated moraine soil, with different numbers of FTCs (N = 0, 1, 4, 8, 10, 12, 15, 20) and various confining pressures (σ3 = 100, 200, 300, 400 kPa). The experimental results reveal that: (1) With an increase in the number of FTCs, the stress–strain curves gradually change from strain-softening to strain-hardening types. Correspondingly, the pore water pressure development shifts gradually from a peak-decay pattern to a growth-stabilization pattern. The peak pore water pressure rises linearly with increasing confining pressure, whereas it decays linearly with an increasing number of FTCs. (2) Both the secant modulus E50 and the shear strength increase with higher confining pressure and decrease with more FTCs. Confining pressure exerts a significant inhibitory and compensatory effect on freeze–thaw-induced damage, markedly reducing the deterioration rate under high confining pressure. (3) Quantitative prediction models for E50 and qmax were established, effectively capturing the coupled effect of confining pressure and FTCs. It can be inferred that confining pressure mitigates structural damage by compressing frost-induced cracks and enhancing interparticle contacts, while FTCs exacerbate the degradation of soil mechanical properties because of ice crystal expansion or contraction and weakening of cementation. This study quantifies the coupled effect of confining pressure and FTCs, and the proposed prediction model provides a useful reference or preliminary estimation for relevant geotechnical engineering designs. Full article
(This article belongs to the Special Issue Failure Mechanisms in Rock and Soil Masses Research)
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