Pub Date : 2025-12-01DOI: 10.1016/j.gete.2025.100776
Yuda Zhang , Jingnan Dong , Guangjie Yuan , Yan Xia , Hong Zhang , Pan Fu
Carbon storage in depleted reservoirs has emerged as a critical technology for mitigating atmospheric CO₂ concentrations, where the sealing integrity of old wells constitutes a pivotal factor in site selection. This study investigates the sealing performance of old wells containing fish and buried by wellbore collapse debris through comprehensive experimental approaches, including full-scale wellbore debris sealing simulations and small-scale core permeability tests. The experimental design systematically examined key variables including debris composition, compaction degree, and permeability characteristics under varying hydraulic pressures. Results demonstrate two distinct failure mechanisms: (1) gas breakthrough occurring at pressure differentials of 1.3–2.7 MPa with approximately 30-second response time, where gas migration predominantly follows interfacial pathways between compacted debris (permeability <0.031 D) and casing/fish structures; and (2) persistent gas leakage through debris pore networks, exhibiting permeability ranges of 0.0024–0.031 D. These findings provide fundamental insights into failure dynamics of debris-sealed abandoned wells, offering critical empirical data for safety assessment of CCS/CCUS reservoir candidates. The experimental methodology establishes a replicable framework for evaluating wellbore sealing integrity under simulated reservoir conditions.
{"title":"Sealing simulation experiment of old well collapse debris in carbon capture and storage (CCS)","authors":"Yuda Zhang , Jingnan Dong , Guangjie Yuan , Yan Xia , Hong Zhang , Pan Fu","doi":"10.1016/j.gete.2025.100776","DOIUrl":"10.1016/j.gete.2025.100776","url":null,"abstract":"<div><div>Carbon storage in depleted reservoirs has emerged as a critical technology for mitigating atmospheric CO₂ concentrations, where the sealing integrity of old wells constitutes a pivotal factor in site selection. This study investigates the sealing performance of old wells containing fish and buried by wellbore collapse debris through comprehensive experimental approaches, including full-scale wellbore debris sealing simulations and small-scale core permeability tests. The experimental design systematically examined key variables including debris composition, compaction degree, and permeability characteristics under varying hydraulic pressures. Results demonstrate two distinct failure mechanisms: (1) gas breakthrough occurring at pressure differentials of 1.3–2.7 MPa with approximately 30-second response time, where gas migration predominantly follows interfacial pathways between compacted debris (permeability <0.031 D) and casing/fish structures; and (2) persistent gas leakage through debris pore networks, exhibiting permeability ranges of 0.0024–0.031 D. These findings provide fundamental insights into failure dynamics of debris-sealed abandoned wells, offering critical empirical data for safety assessment of CCS/CCUS reservoir candidates. The experimental methodology establishes a replicable framework for evaluating wellbore sealing integrity under simulated reservoir conditions.</div></div>","PeriodicalId":56008,"journal":{"name":"Geomechanics for Energy and the Environment","volume":"44 ","pages":"Article 100776"},"PeriodicalIF":3.7,"publicationDate":"2025-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145693074","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-11-19DOI: 10.1016/j.gete.2025.100769
Ahu Zhao , Yinping Li , Xilin Shi , Shefeng Hao , Zengguang Che , Kun Yang , Mingnan Xu , Hongling Ma
Solution mining in salt mine typically induces regional ground subsidence and even localized collapse. However, monitoring data from a large-scale salt mine in eastern China reveal significant ground uplift in peripheral areas, while persistent subsidence occurs in the Internal mining area. This study systematically investigates the mechanisms underlying this anomalous phenomenon through integrated InSAR and first-order leveling surveys, detailed geological exploration, and theoretical modeling approaches. A six-year deformation monitoring campaign identified anomalous surface deformation characterized by internal subsidence and peripheral uplift, exhibiting pronounced spatial heterogeneity and temporal non-stationarity. Field core drilling, hydraulic connectivity testing, borehole inflow monitoring, and dynamic injection-extraction analyses confirmed that the high-pressure aquifer within the Dainan Formation(Ed) is an anthropogenic geological formation resulting from injection-extraction imbalance. The core hypothesis posited in this study is that leakage from injection wells elevates pore pressure in deep sandstone aquifers, triggering poroelastic expansion effects that fundamentally drive the sustained ground uplift around mined-out regions. To quantitatively evaluate this large-scale uplift deformation, the issue was conceptualized as a semi-infinite spatial boundary condition, and a corresponding computational model for surface uplift was developed. Following numerical validation of the model and integration with established subsidence theories associated with solution mining, the spatiotemporal deformation patterns from 2018 to 2023 were successfully inverted. The results indicate that the observed deformation pattern of internal subsidence and peripheral uplift arises from the spatial superposition of ground subsidence induced by salt mining and poroelastic uplift driven by injection-induced leakage. The established model quantitatively assesses the contributions of critical injection-extraction parameters to ground deformation, providing a universally applicable theoretical framework for predicting future surface deformation and facilitating geological hazard mitigation.
{"title":"Mechanism of anomalous “internal subsidence and peripheral uplift” in a salt mine goaf: A multi-source validated superposition of poroelastic uplift and mining-induced subsidence","authors":"Ahu Zhao , Yinping Li , Xilin Shi , Shefeng Hao , Zengguang Che , Kun Yang , Mingnan Xu , Hongling Ma","doi":"10.1016/j.gete.2025.100769","DOIUrl":"10.1016/j.gete.2025.100769","url":null,"abstract":"<div><div>Solution mining in salt mine typically induces regional ground subsidence and even localized collapse. However, monitoring data from a large-scale salt mine in eastern China reveal significant ground uplift in peripheral areas, while persistent subsidence occurs in the Internal mining area. This study systematically investigates the mechanisms underlying this anomalous phenomenon through integrated InSAR and first-order leveling surveys, detailed geological exploration, and theoretical modeling approaches. A six-year deformation monitoring campaign identified anomalous surface deformation characterized by internal subsidence and peripheral uplift, exhibiting pronounced spatial heterogeneity and temporal non-stationarity. Field core drilling, hydraulic connectivity testing, borehole inflow monitoring, and dynamic injection-extraction analyses confirmed that the high-pressure aquifer within the Dainan Formation(Ed) is an anthropogenic geological formation resulting from injection-extraction imbalance. The core hypothesis posited in this study is that leakage from injection wells elevates pore pressure in deep sandstone aquifers, triggering poroelastic expansion effects that fundamentally drive the sustained ground uplift around mined-out regions. To quantitatively evaluate this large-scale uplift deformation, the issue was conceptualized as a semi-infinite spatial boundary condition, and a corresponding computational model for surface uplift was developed. Following numerical validation of the model and integration with established subsidence theories associated with solution mining, the spatiotemporal deformation patterns from 2018 to 2023 were successfully inverted. The results indicate that the observed deformation pattern of internal subsidence and peripheral uplift arises from the spatial superposition of ground subsidence induced by salt mining and poroelastic uplift driven by injection-induced leakage. The established model quantitatively assesses the contributions of critical injection-extraction parameters to ground deformation, providing a universally applicable theoretical framework for predicting future surface deformation and facilitating geological hazard mitigation.</div></div>","PeriodicalId":56008,"journal":{"name":"Geomechanics for Energy and the Environment","volume":"44 ","pages":"Article 100769"},"PeriodicalIF":3.7,"publicationDate":"2025-11-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145578593","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-11-17DOI: 10.1016/j.gete.2025.100767
Janne Yliharju , Tero Harjupatana , Jukka Kuva , Heini Reijonen , Markku Kataja , Arttu Miettinen
X-ray tomography and image analysis were applied to monitor the 4D (3D spatial with time) evolution of partial densities of bentonite and water in compacted Wyoming sodium bentonite under constant volume conditions at elevated temperatures. The experiments were conducted at four temperatures: 21 °C, 50 °C, 90 °C, and 130 °C, in a uniform temperature distribution. The study encompassed the validation of the method, and the applicability and limitations of the methodology for experiments at elevated temperatures were discussed. The results showed that the water uptake in bentonite is sensitive to temperature, and significant changes were observed between all the studied temperatures. Although the impact of temperature on water uptake has been observed before, this study obtained detailed 4D data, which is difficult to acquire using other methods. This methodology provides data for modelling the thermo-hydro-mechanical behaviour of compacted bentonite, which is required in the safety assessment of the geological final disposal of radioactive waste.
{"title":"Observation of water transport in compacted bentonite at elevated temperatures using X-ray tomography and image analysis","authors":"Janne Yliharju , Tero Harjupatana , Jukka Kuva , Heini Reijonen , Markku Kataja , Arttu Miettinen","doi":"10.1016/j.gete.2025.100767","DOIUrl":"10.1016/j.gete.2025.100767","url":null,"abstract":"<div><div>X-ray tomography and image analysis were applied to monitor the 4D (3D spatial with time) evolution of partial densities of bentonite and water in compacted Wyoming sodium bentonite under constant volume conditions at elevated temperatures. The experiments were conducted at four temperatures: 21<!--> <!-->°C, 50<!--> <!-->°C, 90<!--> <!-->°C, and 130<!--> <!-->°C, in a uniform temperature distribution. The study encompassed the validation of the method, and the applicability and limitations of the methodology for experiments at elevated temperatures were discussed. The results showed that the water uptake in bentonite is sensitive to temperature, and significant changes were observed between all the studied temperatures. Although the impact of temperature on water uptake has been observed before, this study obtained detailed 4D data, which is difficult to acquire using other methods. This methodology provides data for modelling the thermo-hydro-mechanical behaviour of compacted bentonite, which is required in the safety assessment of the geological final disposal of radioactive waste.</div></div>","PeriodicalId":56008,"journal":{"name":"Geomechanics for Energy and the Environment","volume":"44 ","pages":"Article 100767"},"PeriodicalIF":3.7,"publicationDate":"2025-11-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145578591","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-11-17DOI: 10.1016/j.gete.2025.100771
Ding Liu , Bowen Cheng , Xinping Li , Mingyang Wang , Yu Wang , Yuliang Zhang
To elucidate the failure mechanism of limestone during excavation-induced unloading in underground engineering, a series of triaxial loading–unloading tests were conducted under various confining pressures(σ₃) and initial unloading levels (n). The results show that increasing σ₃ enhances both the peak strength and plastic deformation capacity of limestone. Although a higher n leads to a strength increase, it remains lower than that under conventional triaxial loading and intensifies the brittleness of failure. In terms of energy evolution, both the maximum elastic strain energy (Ue-max) and the maximum dissipated energy (Ud-max) increase linearly with σ₃. During the unloading path, the dissipated energy exhibits a pronounced hysteresis effect, which becomes more evident at higher n values, revealing the sudden energy release characteristic of highly pre-damaged rock masses. Macro- and micro-scale analyses indicate that the failure mode evolves from tensile–shear mixed failure to shear-dominated failure as σ₃ and n increase. Furthermore, the unloading damage constitutive model, established based on strain equivalence and Weibull distribution, shows good agreement with experimental results, effectively characterizes the damage evolution process of limestone.
{"title":"Fracture evolution and energy dissipation characteristics of limestone under triaxial loading and unloading experiments","authors":"Ding Liu , Bowen Cheng , Xinping Li , Mingyang Wang , Yu Wang , Yuliang Zhang","doi":"10.1016/j.gete.2025.100771","DOIUrl":"10.1016/j.gete.2025.100771","url":null,"abstract":"<div><div>To elucidate the failure mechanism of limestone during excavation-induced unloading in underground engineering, a series of triaxial loading–unloading tests were conducted under various confining pressures(<em>σ</em>₃) and initial unloading levels (<em>n</em>). The results show that increasing <em>σ</em>₃ enhances both the peak strength and plastic deformation capacity of limestone. Although a higher n leads to a strength increase, it remains lower than that under conventional triaxial loading and intensifies the brittleness of failure. In terms of energy evolution, both the maximum elastic strain energy (<em>U</em><sub><em>e-max</em></sub>) and the maximum dissipated energy (<em>U</em><sub><em>d</em></sub><sub><em>-max</em></sub>) increase linearly with <em>σ</em>₃. During the unloading path, the dissipated energy exhibits a pronounced hysteresis effect, which becomes more evident at higher n values, revealing the sudden energy release characteristic of highly pre-damaged rock masses. Macro- and micro-scale analyses indicate that the failure mode evolves from tensile–shear mixed failure to shear-dominated failure as <em>σ</em>₃ and <em>n</em> increase. Furthermore, the unloading damage constitutive model, established based on strain equivalence and Weibull distribution, shows good agreement with experimental results, effectively characterizes the damage evolution process of limestone.</div></div>","PeriodicalId":56008,"journal":{"name":"Geomechanics for Energy and the Environment","volume":"44 ","pages":"Article 100771"},"PeriodicalIF":3.7,"publicationDate":"2025-11-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145578595","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
High-strength hard rock and its complex stress environment are one of the challenges faced by deep underground engineering. Mastering the strength characteristics, such as deformation and failure of rock under a multiaxial compression environment, is the basis for solving such problems. This paper proposed a strength criterion based on energy evolution and multi-scale failure characteristics to describe the failure behavior of granite under multiaxial compression. Firstly, the multiaxial compression test of granite was carried out to analyze its stress-strain curve, macro-meso failure characteristics, and energy evolution law, and its meso-failure characteristics were quantitatively characterized based on fractal theory. Secondly, the relationship between shape change energy density, confining pressure, and mesoscopic failure fractal dimension is established, and the rock's multi-scale failure strength criterion is proposed. Finally, the calculation results of the multi-scale failure strength criterion are compared with the test results, Mohr-Coulomb criterion, and Hoek-Brown criterion, and the sensitivity analysis of the parameters in the multi-scale failure strength criterion is carried out. The results show that the multi-scale failure strength criterion can accurately reflect the deformation and failure behavior of rock, and it is proven that the failure characteristics of rock significantly influence the accuracy of its strength criterion. The multi-scale failure strength criterion considers the influence of meso-damage on rock failure behavior, which makes up for the deficiency of the traditional strength criterion in considering damage characteristics and meso-mechanical parameters. It provides a new idea for analyzing rock failure mechanisms and a more accurate prediction model for engineering practice.
{"title":"Energy evolution law and multi-scale failure strength criterion of granite under multiaxial compression","authors":"Yingqing Lyu, Haijun Wu, Heng Dong, Tianlong Zhang, Meng Li, Fenglei Huang","doi":"10.1016/j.gete.2025.100770","DOIUrl":"10.1016/j.gete.2025.100770","url":null,"abstract":"<div><div>High-strength hard rock and its complex stress environment are one of the challenges faced by deep underground engineering. Mastering the strength characteristics, such as deformation and failure of rock under a multiaxial compression environment, is the basis for solving such problems. This paper proposed a strength criterion based on energy evolution and multi-scale failure characteristics to describe the failure behavior of granite under multiaxial compression. Firstly, the multiaxial compression test of granite was carried out to analyze its stress-strain curve, macro-meso failure characteristics, and energy evolution law, and its meso-failure characteristics were quantitatively characterized based on fractal theory. Secondly, the relationship between shape change energy density, confining pressure, and mesoscopic failure fractal dimension is established, and the rock's multi-scale failure strength criterion is proposed. Finally, the calculation results of the multi-scale failure strength criterion are compared with the test results, Mohr-Coulomb criterion, and Hoek-Brown criterion, and the sensitivity analysis of the parameters in the multi-scale failure strength criterion is carried out. The results show that the multi-scale failure strength criterion can accurately reflect the deformation and failure behavior of rock, and it is proven that the failure characteristics of rock significantly influence the accuracy of its strength criterion. The multi-scale failure strength criterion considers the influence of meso-damage on rock failure behavior, which makes up for the deficiency of the traditional strength criterion in considering damage characteristics and meso-mechanical parameters. It provides a new idea for analyzing rock failure mechanisms and a more accurate prediction model for engineering practice.</div></div>","PeriodicalId":56008,"journal":{"name":"Geomechanics for Energy and the Environment","volume":"44 ","pages":"Article 100770"},"PeriodicalIF":3.7,"publicationDate":"2025-11-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145578594","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-11-13DOI: 10.1016/j.gete.2025.100768
Yingping Xiao , Hong Cao , Hong Pan , Guanyong Luo , Bo Li , Dongfeng Zhu
Backward erosion piping is an internal erosion process that creates shallow pipes at the interface between an impermeable cover layer and a sandy foundation. Shallow pipes develop intermittently towards the riverside. Seepage and pipe flow are the main drivers of pipe erosion. Accurately simulating this coupled system is crucial for revealing the underlying erosion mechanisms, and the pipe depth is a significant parameter in these simulations. The pipe depth is determined by applying the incipient motion condition of bed particles, a method which relies on the pipe being in a limit-state equilibrium. This condition, along with the depth-averaged critical velocity, is derived from a force balance analysis of a single particle at the pipe's bottom under upward seepage. Accordingly, a coupled approach simulating erosion in the pipe, groundwater flow, and pipe flow is proposed. Pipe deepening coupled with groundwater flow and pipe flow are simulated for some available experiments to illustrate this simulation approach.
{"title":"Incipient motion of sands in the pipe and numerical modelling of the pipe depth","authors":"Yingping Xiao , Hong Cao , Hong Pan , Guanyong Luo , Bo Li , Dongfeng Zhu","doi":"10.1016/j.gete.2025.100768","DOIUrl":"10.1016/j.gete.2025.100768","url":null,"abstract":"<div><div>Backward erosion piping is an internal erosion process that creates shallow pipes at the interface between an impermeable cover layer and a sandy foundation. Shallow pipes develop intermittently towards the riverside. Seepage and pipe flow are the main drivers of pipe erosion. Accurately simulating this coupled system is crucial for revealing the underlying erosion mechanisms, and the pipe depth is a significant parameter in these simulations. The pipe depth is determined by applying the incipient motion condition of bed particles, a method which relies on the pipe being in a limit-state equilibrium. This condition, along with the depth-averaged critical velocity, is derived from a force balance analysis of a single particle at the pipe's bottom under upward seepage. Accordingly, a coupled approach simulating erosion in the pipe, groundwater flow, and pipe flow is proposed. Pipe deepening coupled with groundwater flow and pipe flow are simulated for some available experiments to illustrate this simulation approach.</div></div>","PeriodicalId":56008,"journal":{"name":"Geomechanics for Energy and the Environment","volume":"44 ","pages":"Article 100768"},"PeriodicalIF":3.7,"publicationDate":"2025-11-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145578592","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-11-07DOI: 10.1016/j.gete.2025.100765
Gianmario Sorrentino , Andrea Franza
This paper presents an experimental study of sugar as a low-viscosity cementing agent for sand in dry laboratory conditions. Sand was mixed with aqueous sugar solutions of varying concentrations (15%–40% by mass) and oven-cured at different temperatures. Unconfined compressive strength (UCS) tests showed that strength increased with sugar concentration, with UCS values reaching up to 6 MPa —comparable to or exceeding those achieved with conventional bio-cementation methods. Optimal curing occurred at 105 °C, balancing rapid hardening and peak strength, while excessive heating at 170 °C reduced strength due to sugar caramelisation. Nevertheless, all conditions yielded mean UCS values above 1 MPa, demonstrating the method’s reliability. Scanning electron microscopy (SEM) was used to observe the interaction between sugar and sand particles, revealing a substantial sugar coating bonding the grains. These findings reveal some of the fundamental mechanisms of sugar-induced cementation. Finally, research pathways and current shortcomings for field applications are discussed.
{"title":"Experimental study of sugar-induced sand cementation in dry conditions","authors":"Gianmario Sorrentino , Andrea Franza","doi":"10.1016/j.gete.2025.100765","DOIUrl":"10.1016/j.gete.2025.100765","url":null,"abstract":"<div><div>This paper presents an experimental study of sugar as a low-viscosity cementing agent for sand in dry laboratory conditions. Sand was mixed with aqueous sugar solutions of varying concentrations (15%–40% by mass) and oven-cured at different temperatures. Unconfined compressive strength (UCS) tests showed that strength increased with sugar concentration, with UCS values reaching up to 6<!--> <!-->MPa —comparable to or exceeding those achieved with conventional bio-cementation methods. Optimal curing occurred at 105<!--> <!-->°C, balancing rapid hardening and peak strength, while excessive heating at 170<!--> <!-->°C reduced strength due to sugar caramelisation. Nevertheless, all conditions yielded mean UCS values above 1<!--> <!-->MPa, demonstrating the method’s reliability. Scanning electron microscopy (SEM) was used to observe the interaction between sugar and sand particles, revealing a substantial sugar coating bonding the grains. These findings reveal some of the fundamental mechanisms of sugar-induced cementation. Finally, research pathways and current shortcomings for field applications are discussed.</div></div>","PeriodicalId":56008,"journal":{"name":"Geomechanics for Energy and the Environment","volume":"44 ","pages":"Article 100765"},"PeriodicalIF":3.7,"publicationDate":"2025-11-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145528429","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-11-06DOI: 10.1016/j.gete.2025.100759
Wenbo Niu , Chaofa Zhao , Hamza Mhamdi Alaoui , Zhongxuan Yang , Pierre-Yves Hicher
Clayey geomaterials rarely occur in a pure mineralogical state in nature and are more commonly found as mixed-layer clays, such as interstratified illite-smectite. These clays consist of varying proportions of illite and smectite layers, which significantly affect their mechanical properties. Under variable mechanical conditions, the shear behavior of mixed-layer clays exhibits considerable complexity, underscoring the need for in-depth investigations. This paper presents a molecular-scale study on the behavior of interstratified illite-smectite minerals, simulating a geotechnical shear setup at the molecular level. Multiple molecular models were constructed to explore the effects of water content and illite layer proportions, effectively replicating stages of the illitization process. The results reveal that the mixed-layer clays exhibit clear stick–slip behavior during shear simulation. Models with low illite content demonstrated relatively similar shear characteristics, while higher illite content led to a significant reduction in nanoscale cohesion and a slight increase in friction coefficient. Pure illite exhibited the highest shear strength among the studied materials, with a friction coefficient and cohesion of 0.111 and 0.172 GPa, respectively. Furthermore, the illitization process was observed to progressively enhance the shear modulus, ranging from 0.63 GPa to 26.81 GPa under various hydrostatic pressures. A statistical analysis was also performed to further examine the stick–slip behavior of mixed-layer clays. These findings provide essential insights into the nanoscale mechanical properties of mixed-layer clay minerals, contributing to a deeper understanding of geomaterial stability in critical applications.
{"title":"Molecular insights into the shear behavior of interstratified illite-smectite clays: Effects of hydration and illitization","authors":"Wenbo Niu , Chaofa Zhao , Hamza Mhamdi Alaoui , Zhongxuan Yang , Pierre-Yves Hicher","doi":"10.1016/j.gete.2025.100759","DOIUrl":"10.1016/j.gete.2025.100759","url":null,"abstract":"<div><div>Clayey geomaterials rarely occur in a pure mineralogical state in nature and are more commonly found as mixed-layer clays, such as interstratified illite-smectite. These clays consist of varying proportions of illite and smectite layers, which significantly affect their mechanical properties. Under variable mechanical conditions, the shear behavior of mixed-layer clays exhibits considerable complexity, underscoring the need for in-depth investigations. This paper presents a molecular-scale study on the behavior of interstratified illite-smectite minerals, simulating a geotechnical shear setup at the molecular level. Multiple molecular models were constructed to explore the effects of water content and illite layer proportions, effectively replicating stages of the illitization process. The results reveal that the mixed-layer clays exhibit clear stick–slip behavior during shear simulation. Models with low illite content demonstrated relatively similar shear characteristics, while higher illite content led to a significant reduction in nanoscale cohesion and a slight increase in friction coefficient. Pure illite exhibited the highest shear strength among the studied materials, with a friction coefficient and cohesion of 0.111 and 0.172 GPa, respectively. Furthermore, the illitization process was observed to progressively enhance the shear modulus, ranging from 0.63 GPa to 26.81 GPa under various hydrostatic pressures. A statistical analysis was also performed to further examine the stick–slip behavior of mixed-layer clays. These findings provide essential insights into the nanoscale mechanical properties of mixed-layer clay minerals, contributing to a deeper understanding of geomaterial stability in critical applications.</div></div>","PeriodicalId":56008,"journal":{"name":"Geomechanics for Energy and the Environment","volume":"44 ","pages":"Article 100759"},"PeriodicalIF":3.7,"publicationDate":"2025-11-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145528497","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-11-06DOI: 10.1016/j.gete.2025.100766
Xiaoming Shi , Lei Geng , Xuejie Deng , Gustavo Paneiro , Zhide Wu , Yang Li , Hao Liu , Jianye Feng
The mechanical behavior and damage evolution of coal pillars under cyclic loading govern the long-term stability of underground gas storage in abandoned coal mines. Using coal from Ningxia, we conducted uniaxial constant-amplitude cyclic tests and incremental loading-unloading tests, combined with acoustic-emission monitoring, damage-mechanics modeling, and PFC particle-flow simulations, to elucidate a stress-threshold-controlled evolution law. The results show that the first loading cycle dominates damage progression, contributing 36.75 %-75.19 % of the cumulative AE ringing counts and markedly degrading mechanical integrity. Also, macroscopic failure is mainly shear (73.9 %-80.1 %), while the proportion of tensile events rises with stress amplitude. This study also shows that a stress-threshold range of about 89.2 %-95.4 % UCS is identified for the coal specimens, within which sub-threshold damage is self-limiting and the damage variable grows by only 9.3 % after 50 cycles, whereas super-threshold loading induces a three-stage process of compaction, stable accumulation, and accelerated instability. Finally, a damage-evolution model that couples Ashby’s microcrack mechanics with geometric damage predicts a nonlinear link between crack growth and loss of load-bearing capacity and reproduces the measured stress-damage trajectory more accurately than classical formulas. PFC simulations further show that a stress difference of 0.05 MPa can trigger an abrupt transition to instability, confirming the decisive control of the threshold. These findings provide a basis for safety-threshold design and long-term stability assessment of rock masses under cyclic loading.
{"title":"Experimental investigation of damage behavior of coal pillars during injection-production in abandoned coal mine gas storage","authors":"Xiaoming Shi , Lei Geng , Xuejie Deng , Gustavo Paneiro , Zhide Wu , Yang Li , Hao Liu , Jianye Feng","doi":"10.1016/j.gete.2025.100766","DOIUrl":"10.1016/j.gete.2025.100766","url":null,"abstract":"<div><div>The mechanical behavior and damage evolution of coal pillars under cyclic loading govern the long-term stability of underground gas storage in abandoned coal mines. Using coal from Ningxia, we conducted uniaxial constant-amplitude cyclic tests and incremental loading-unloading tests, combined with acoustic-emission monitoring, damage-mechanics modeling, and PFC particle-flow simulations, to elucidate a stress-threshold-controlled evolution law. The results show that the first loading cycle dominates damage progression, contributing 36.75 %-75.19 % of the cumulative AE ringing counts and markedly degrading mechanical integrity. Also, macroscopic failure is mainly shear (73.9 %-80.1 %), while the proportion of tensile events rises with stress amplitude. This study also shows that a stress-threshold range of about 89.2 %-95.4 % UCS is identified for the coal specimens, within which sub-threshold damage is self-limiting and the damage variable grows by only 9.3 % after 50 cycles, whereas super-threshold loading induces a three-stage process of compaction, stable accumulation, and accelerated instability. Finally, a damage-evolution model that couples Ashby’s microcrack mechanics with geometric damage predicts a nonlinear link between crack growth and loss of load-bearing capacity and reproduces the measured stress-damage trajectory more accurately than classical formulas. PFC simulations further show that a stress difference of 0.05 MPa can trigger an abrupt transition to instability, confirming the decisive control of the threshold. These findings provide a basis for safety-threshold design and long-term stability assessment of rock masses under cyclic loading.</div></div>","PeriodicalId":56008,"journal":{"name":"Geomechanics for Energy and the Environment","volume":"44 ","pages":"Article 100766"},"PeriodicalIF":3.7,"publicationDate":"2025-11-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145528428","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2025-11-04DOI: 10.1016/j.gete.2025.100764
Zechen Chang , Pengxiang Zhao , Shugang Li , Diego Maria Barbieri , Xu Guo , Weidong Lu , Quan Jin , Linyue Jie
In this study, the precise layout of the pressure-relief gas drainage boreholes significantly impacted the efficiency of gas drainage and the efficient utilization of gas. This research considered a certain main mining face of the Lutang Coal Mine in Guizhou Province as its research background. The evolution law of the overburden fracture evolution during the mining of high-gas coal seams was analyzed, and a regional division was conducted. A characterization model of the gas migration zone in a high-gas coal seam was constructed. This model was applied to the test working face to perform directional borehole gas drainage and gas utilization. The results showed that the goaf area can be divided into subsidence, rupture, and curved subsidence zones based on the evolutionary trend of the fractures. The goaf area was laterally divided into gas migration and compaction areas based on the density of the fractures. A characterization model of the gas migration zones in high-gas coal seams was established, the stability of rock masses in different regions was analyzed, and the optimal area for directional drilling in the gas migration zone of the fracture was determined. The drilling layout parameters were optimized, and the wellbore gas production, average volume fraction of wellbore gas production, and pure gas production under pressure relief increased by 267 %, 240 %, and 241 %, respectively. The gas-fired power generation increased from 519.3 kWh to 1311.1 kWh. The gas volume fraction in the return air duct and upper corner decreased to between 0.27–0.53 and 0.22–0.43. These results provide theoretical guidance for parameter optimization of extraction boreholes in high-gas coal seams and the utilization of depressurized gas.
{"title":"Pressure relief and zonal extraction and utilization of medium-thick coal seams with high gas content","authors":"Zechen Chang , Pengxiang Zhao , Shugang Li , Diego Maria Barbieri , Xu Guo , Weidong Lu , Quan Jin , Linyue Jie","doi":"10.1016/j.gete.2025.100764","DOIUrl":"10.1016/j.gete.2025.100764","url":null,"abstract":"<div><div>In this study, the precise layout of the pressure-relief gas drainage boreholes significantly impacted the efficiency of gas drainage and the efficient utilization of gas. This research considered a certain main mining face of the Lutang Coal Mine in Guizhou Province as its research background. The evolution law of the overburden fracture evolution during the mining of high-gas coal seams was analyzed, and a regional division was conducted. A characterization model of the gas migration zone in a high-gas coal seam was constructed. This model was applied to the test working face to perform directional borehole gas drainage and gas utilization. The results showed that the goaf area can be divided into subsidence, rupture, and curved subsidence zones based on the evolutionary trend of the fractures. The goaf area was laterally divided into gas migration and compaction areas based on the density of the fractures. A characterization model of the gas migration zones in high-gas coal seams was established, the stability of rock masses in different regions was analyzed, and the optimal area for directional drilling in the gas migration zone of the fracture was determined. The drilling layout parameters were optimized, and the wellbore gas production, average volume fraction of wellbore gas production, and pure gas production under pressure relief increased by 267 %, 240 %, and 241 %, respectively. The gas-fired power generation increased from 519.3 kWh to 1311.1 kWh. The gas volume fraction in the return air duct and upper corner decreased to between 0.27–0.53 and 0.22–0.43. These results provide theoretical guidance for parameter optimization of extraction boreholes in high-gas coal seams and the utilization of depressurized gas.</div></div>","PeriodicalId":56008,"journal":{"name":"Geomechanics for Energy and the Environment","volume":"44 ","pages":"Article 100764"},"PeriodicalIF":3.7,"publicationDate":"2025-11-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145528496","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}