首页 > 最新文献

International Journal of Rock Mechanics and Mining Sciences最新文献

英文 中文
Modeling the thermo-mechanical behavior of porous lava under reservoir conditions 储层条件下多孔熔岩热-力学行为模拟
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-15 DOI: 10.1016/j.ijrmms.2025.106383
Ghassan Shahin , Michael J. Heap , Marie Violay
Harnessing geothermal energy and storing carbon dioxide in volcanic systems require reliable constitutive models to predict rock deformation and failure under extreme pressure and temperature. However, existing models are limited, especially when compared to the more advanced predictive tools available for sedimentary rocks. In this study, we integrate elastoplasticity, strain hardening, nonassociative plasticity, phenomenological thermomechanics, and bifurcation analysis to establish a novel constitutive model for porous lava. The model is calibrated against a unique dataset that provides the stress–strain and strain localization responses of porous andesite deformed at temperatures ranging from room temperature up to 800 °C and at effective confining pressures from room pressure to 50 MPa. These mechanical and thermal conditions are representative of deep geothermal reservoirs. Finite element simulations of laboratory experiments are used to demonstrate the model’s capabilities in terms of reproducing key mechanical characteristics, including the differential stress required for the first stress drop and deformation mechanisms, across varying pressure and temperature conditions. Further validation via full-field finite element computations, simulating borehole excavation in low- to high-temperature systems, underscores the model’s predictive capabilities. In particular, the field-scale simulations demonstrate the model’s efficacy in reproducing variable forms of deformation structures and deformation modes around boreholes with capabilities to provide more information about the displacement in the borehole walls. The proposed modeling framework can be integrated into commercial numerical tools and used to facilitate the engineering of safe and cost-effective geothermal energy production and carbon geostorage, as well as numerical models designed to better understand the stability and therefore the hazard potential of volcanic structures.
利用地热能和在火山系统中储存二氧化碳需要可靠的本构模型来预测岩石在极端压力和温度下的变形和破坏。然而,现有的模型是有限的,特别是与更先进的沉积岩预测工具相比。在本研究中,我们综合了弹塑性、应变硬化、非联想塑性、现象学热力学和分岔分析,建立了一个新的多孔熔岩本构模型。该模型是根据一个独特的数据集进行校准的,该数据集提供了多孔安山岩在室温至800°C和室温至50 MPa有效围压下变形的应力-应变和应变局部化响应。这些力学和热条件是深层地热储层的代表性条件。实验室实验的有限元模拟用于证明模型在再现关键机械特性方面的能力,包括在不同压力和温度条件下第一次应力下降和变形机制所需的差应力。通过模拟低至高温系统中钻孔开挖的现场有限元计算,进一步验证了该模型的预测能力。特别是,现场规模的模拟证明了该模型在再现井眼周围不同形式的变形结构和变形模式方面的有效性,并能够提供有关井眼壁位移的更多信息。所提出的建模框架可以集成到商业数值工具中,用于促进安全且具有成本效益的地热能生产和碳地质储存工程,以及旨在更好地了解火山结构稳定性和潜在危害的数值模型。
{"title":"Modeling the thermo-mechanical behavior of porous lava under reservoir conditions","authors":"Ghassan Shahin ,&nbsp;Michael J. Heap ,&nbsp;Marie Violay","doi":"10.1016/j.ijrmms.2025.106383","DOIUrl":"10.1016/j.ijrmms.2025.106383","url":null,"abstract":"<div><div>Harnessing geothermal energy and storing carbon dioxide in volcanic systems require reliable constitutive models to predict rock deformation and failure under extreme pressure and temperature. However, existing models are limited, especially when compared to the more advanced predictive tools available for sedimentary rocks. In this study, we integrate elastoplasticity, strain hardening, nonassociative plasticity, phenomenological thermomechanics, and bifurcation analysis to establish a novel constitutive model for porous lava. The model is calibrated against a unique dataset that provides the stress–strain and strain localization responses of porous andesite deformed at temperatures ranging from room temperature up to 800 °C and at effective confining pressures from room pressure to 50 MPa. These mechanical and thermal conditions are representative of deep geothermal reservoirs. Finite element simulations of laboratory experiments are used to demonstrate the model’s capabilities in terms of reproducing key mechanical characteristics, including the differential stress required for the first stress drop and deformation mechanisms, across varying pressure and temperature conditions. Further validation via full-field finite element computations, simulating borehole excavation in low- to high-temperature systems, underscores the model’s predictive capabilities. In particular, the field-scale simulations demonstrate the model’s efficacy in reproducing variable forms of deformation structures and deformation modes around boreholes with capabilities to provide more information about the displacement in the borehole walls. The proposed modeling framework can be integrated into commercial numerical tools and used to facilitate the engineering of safe and cost-effective geothermal energy production and carbon geostorage, as well as numerical models designed to better understand the stability and therefore the hazard potential of volcanic structures.</div></div>","PeriodicalId":54941,"journal":{"name":"International Journal of Rock Mechanics and Mining Sciences","volume":"199 ","pages":"Article 106383"},"PeriodicalIF":7.5,"publicationDate":"2026-01-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145980631","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Coalescence of a subcritical crack pair in carbonate rocks upon acidizing 碳酸盐岩酸化过程中亚临界裂纹对的聚并
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-14 DOI: 10.1016/j.ijrmms.2026.106414
Xiao-Jie Tang , Si-Han Zhou , Man-Man Hu
For chemically assisted cracking in tight low-permeable carbonate-rich reservoirs, crack growth and coalescence are driven by a complex interplay between stress redistribution, mineral dissolution, elasto-viscoplastic deformation, damage-enhanced specific surface area, and evolving permeability. Albeit that extensive research exists on crack initiation and growth, little has been found focusing on the underlying mechanism of how two adjacent cracks interact and coalesce through their tips - driven by a combined effect of chemical erosion and internal pressurization. Here we adopt a fully coupled reactive chemo-mechanical model for investigating the coalescence of the propagating plasticity zones around two adjacent crack-tips that precede the subcritical growth of the cracks. The constitutive framework captures time-dependent processes including proton diffusion, dissolution-induced stiffness degradation, damage evolution, chemical alteration of the yield limits, and micro-cracking feedback. The implemented formulation is applied to a pair of internally pressurized blunt-tip collinear cracks exposed to a weak-acidic solution. Our results show that the crack pair coalescence undergoes a multi-stage subcritical development: (i) a quasi-linear mechanically dominated initial (incubation) phase, (ii) a dissolution-enhanced softening phase once an accumulated mass-removal threshold is reached, and (iii) a secondary acceleration phase upon the onset when the two propagating plasticity zones coalesce in the ligament between the crack-tips. It is illustrated that an intensified acidity, or a higher rock susceptibility to micro-cracking, amplifies positive feedback between damage evolution and chemical dissolution, markedly enhancing crack growth. Mild intrinsic heterogeneity seeds further accelerate the process zone interaction and crack coalescence, through forming networks of orthogonal micro-deformation bands in front of the crack-tips.
对于致密低渗透富碳酸盐岩储层的化学辅助裂缝,裂缝的扩展和合并是由应力重分布、矿物溶解、弹粘塑性变形、损伤增强比表面积和渗透率变化等复杂的相互作用驱动的。尽管对裂纹的产生和扩展进行了广泛的研究,但很少有人关注两个相邻裂纹如何在化学侵蚀和内部加压的共同作用下通过其尖端相互作用和合并的潜在机制。在这里,我们采用一个完全耦合的反应化学-力学模型来研究在裂纹亚临界扩展之前,两个相邻裂纹尖端周围扩展塑性区的合并。本构框架捕获了与时间相关的过程,包括质子扩散、溶解引起的刚度退化、损伤演化、屈服极限的化学变化和微裂纹反馈。所实施的配方适用于一对暴露于弱酸性溶液中的内部加压钝尖共线裂纹。我们的研究结果表明,裂纹对合并经历了一个多阶段的亚临界发展:(i)准线性机械主导的初始(孵化)阶段,(ii)一旦达到累积质量去除阈值,溶解增强的软化阶段,以及(iii)当两个扩展塑性区域在裂纹尖端之间的韧带中合并时开始的二次加速阶段。结果表明,酸性的增强或岩石对微裂纹的敏感性的提高,放大了损伤演化与化学溶解之间的正反馈,显著促进了裂纹的扩展。温和的本征非均质种子通过在裂纹尖端前形成正交微变形带网络,进一步加速了过程区相互作用和裂纹合并。
{"title":"Coalescence of a subcritical crack pair in carbonate rocks upon acidizing","authors":"Xiao-Jie Tang ,&nbsp;Si-Han Zhou ,&nbsp;Man-Man Hu","doi":"10.1016/j.ijrmms.2026.106414","DOIUrl":"10.1016/j.ijrmms.2026.106414","url":null,"abstract":"<div><div>For chemically assisted cracking in tight low-permeable carbonate-rich reservoirs, crack growth and coalescence are driven by a complex interplay between stress redistribution, mineral dissolution, elasto-viscoplastic deformation, damage-enhanced specific surface area, and evolving permeability. Albeit that extensive research exists on crack initiation and growth, little has been found focusing on the underlying mechanism of how two adjacent cracks interact and coalesce through their tips - driven by a combined effect of chemical erosion and internal pressurization. Here we adopt a fully coupled reactive chemo-mechanical model for investigating the coalescence of the propagating plasticity zones around two adjacent crack-tips that precede the subcritical growth of the cracks. The constitutive framework captures time-dependent processes including proton diffusion, dissolution-induced stiffness degradation, damage evolution, chemical alteration of the yield limits, and micro-cracking feedback. The implemented formulation is applied to a pair of internally pressurized blunt-tip collinear cracks exposed to a weak-acidic solution. Our results show that the crack pair coalescence undergoes a multi-stage subcritical development: (i) a quasi-linear mechanically dominated initial (incubation) phase, (ii) a dissolution-enhanced softening phase once an accumulated mass-removal threshold is reached, and (iii) a secondary acceleration phase upon the onset when the two propagating plasticity zones coalesce in the ligament between the crack-tips. It is illustrated that an intensified acidity, or a higher rock susceptibility to micro-cracking, amplifies positive feedback between damage evolution and chemical dissolution, markedly enhancing crack growth. Mild intrinsic heterogeneity seeds further accelerate the process zone interaction and crack coalescence, through forming networks of orthogonal micro-deformation bands in front of the crack-tips.</div></div>","PeriodicalId":54941,"journal":{"name":"International Journal of Rock Mechanics and Mining Sciences","volume":"199 ","pages":"Article 106414"},"PeriodicalIF":7.5,"publicationDate":"2026-01-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145980633","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Exclusion-dependent percolation threshold of non-convex pores and permeability of porous media 非凸孔的非排斥性渗流阈值与多孔介质渗透率
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-13 DOI: 10.1016/j.ijrmms.2026.106417
Wenxiang Xu , Li Wang , Dingcheng Dai , Jiaping Liu , Jinyang Jiang
Intricate morphologies of pores have great influences on the percolation threshold of pore space and even the permeability of porous media. Despite extensive efforts to numerically explore the large design space for continuum percolation models of pore space constituted by overlapping objects with rich convexities and their impacts on the permeability, there is a critical knowledge gap on our understanding of the effect of nature of non-convex pore on the percolation threshold and permeability of porous media. This missing understanding hinders the precise evaluation of sewage transport in marine and soil, the durability optimization of hydropower dam, and the fast development of oil and shale gas exploitation. In this work, we develop and validate a high-fidelity numerical description to bridge this knowledge gap. Our description contains three major powerful models. Starting from a 3D morphology reconstruction of realistic surface of non-convex pore, we propose a mathematically-controllable parameterized method to realize arbitrary-shaped pore. Accordingly, the excluded volume of non-convex pore and its dependence on non-convex morphologies are obtained using large-scale Monte Carlo simulations (LSMCs). Then, we combine LSMCs and finite-size scaling method to accurately determine the long-range percolation threshold of non-convex pore space. By analyzing 311 statistical data for the percolation threshold affected by excluded volume of convex/non-convex objects, a generic exclusion-dependent percolation threshold model is proposed that does not only demonstrate the universality of the excluded-volume theory but is capable of estimating the percolation threshold of overlapping arbitrary-shaped objects from convexity to non-convexity. We also develop a multi-relaxation-time lattice Boltzmann method to precisely capture the permeability of porous media over the entire range of porosities, specifically its non-linear saltation behavior near the percolation threshold of non-convex pore space. Altogether, these results shed fresh light on non-convex pore morphologies that dominate the excluded volume, percolation threshold and permeability. Our description illuminates the universal relationship of “excluded volume-percolation threshold-permeability” in porous media, which in turn can guide the design of geological materials and the pore-level optimization in ways previously unattainable for critical water/gas/oil-energy applications.
孔隙的复杂形态对孔隙空间的渗透阈值甚至多孔介质的渗透率都有很大的影响。尽管大量研究人员在数值上探索了由具有丰富凸度的重叠物体构成的连续渗流模型的大设计空间及其对渗透率的影响,但我们对非凸孔性质对多孔介质渗透阈值和渗透率的影响的理解仍存在关键的知识空白。这种认识的缺失阻碍了污水在海洋和土壤中运移的精确评价、水电大坝的耐久性优化以及石油和页岩气开发的快速发展。在这项工作中,我们开发并验证了一个高保真的数值描述,以弥合这一知识差距。我们的描述包含三个主要的强大模型。从非凸孔真实表面的三维形态重建出发,提出了一种数学可控的参数化方法来实现任意形状的孔。据此,利用大规模蒙特卡罗模拟(LSMCs)得到了非凸孔的排除体积及其与非凸形貌的依赖关系。然后,我们将LSMCs与有限尺寸标度法相结合,精确地确定了非凸孔空间的远程渗透阈值。通过分析311个凸/非凸物体的排除体积影响渗透阈值的统计数据,提出了一个通用的排除依赖渗透阈值模型,该模型不仅证明了排除体积理论的通用性,而且能够估计重叠任意形状物体从凸到非凸的渗透阈值。我们还开发了一种多松弛时间晶格玻尔兹曼方法来精确捕获多孔介质在整个孔隙度范围内的渗透率,特别是其在非凸孔隙空间渗透阈值附近的非线性跃变行为。总之,这些结果为非凸孔形态提供了新的视角,这些形态在排除体积、渗透阈值和渗透率方面占主导地位。我们的描述阐明了多孔介质中“排除体积-渗透阈值-渗透率”的普遍关系,这反过来又可以指导地质材料的设计和孔隙水平的优化,这在以前的关键水/气/油能源应用中是无法实现的。
{"title":"Exclusion-dependent percolation threshold of non-convex pores and permeability of porous media","authors":"Wenxiang Xu ,&nbsp;Li Wang ,&nbsp;Dingcheng Dai ,&nbsp;Jiaping Liu ,&nbsp;Jinyang Jiang","doi":"10.1016/j.ijrmms.2026.106417","DOIUrl":"10.1016/j.ijrmms.2026.106417","url":null,"abstract":"<div><div>Intricate morphologies of pores have great influences on the percolation threshold of pore space and even the permeability of porous media. Despite extensive efforts to numerically explore the large design space for continuum percolation models of pore space constituted by overlapping objects with rich convexities and their impacts on the permeability, there is a critical knowledge gap on our understanding of the effect of nature of non-convex pore on the percolation threshold and permeability of porous media. This missing understanding hinders the precise evaluation of sewage transport in marine and soil, the durability optimization of hydropower dam, and the fast development of oil and shale gas exploitation. In this work, we develop and validate a high-fidelity numerical description to bridge this knowledge gap. Our description contains three major powerful models. Starting from a 3D morphology reconstruction of realistic surface of non-convex pore, we propose a mathematically-controllable parameterized method to realize arbitrary-shaped pore. Accordingly, the excluded volume of non-convex pore and its dependence on non-convex morphologies are obtained using large-scale Monte Carlo simulations (LSMCs). Then, we combine LSMCs and finite-size scaling method to accurately determine the long-range percolation threshold of non-convex pore space. By analyzing 311 statistical data for the percolation threshold affected by excluded volume of convex/non-convex objects, a generic exclusion-dependent percolation threshold model is proposed that does not only demonstrate the universality of the excluded-volume theory but is capable of estimating the percolation threshold of overlapping arbitrary-shaped objects from convexity to non-convexity. We also develop a multi-relaxation-time lattice Boltzmann method to precisely capture the permeability of porous media over the entire range of porosities, specifically its non-linear saltation behavior near the percolation threshold of non-convex pore space. Altogether, these results shed fresh light on non-convex pore morphologies that dominate the excluded volume, percolation threshold and permeability. Our description illuminates the universal relationship of “excluded volume-percolation threshold-permeability” in porous media, which in turn can guide the design of geological materials and the pore-level optimization in ways previously unattainable for critical water/gas/oil-energy applications.</div></div>","PeriodicalId":54941,"journal":{"name":"International Journal of Rock Mechanics and Mining Sciences","volume":"199 ","pages":"Article 106417"},"PeriodicalIF":7.5,"publicationDate":"2026-01-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145962149","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Multi-method constrained stress states in the Qiabuqia geothermal field, NW China: Insights from basin-basement contrasts 中国西北恰布恰地热田多方法约束应力状态:盆地-基底对比的启示
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-13 DOI: 10.1016/j.ijrmms.2026.106422
Zijuan Hu , Shengsheng Zhang , Chongyuan Zhang , Shian Zhang , Derek Elsworth , Wen Meng , Xianghui Qin
We applied anelastic strain recovery (ASR), hydraulic fracturing (HF), and acoustic image logging to determine the full three-dimensional stress state in the Qiabuqia geothermal field, northeastern Tibetan Plateau. ASR measurements from twenty-five core samples across five boreholes in the geothermal field reveal a pronounced stress contrast between the sedimentary basin fill and the underlying granite basement. The sediments exhibit a normal faulting stress regime (Sv > SHmax > Shmin), primarily governed by gravitational loading. In contrast, the granite basement exhibits a strike-slip regime (SHmax > Sv > Shmin), indicating a dominant tectonic compression. Horizontal differential stress increases with depth in the sediments but decreases within the granite. We interpret these contrasts as resulting from variations in basement topography and mechanical properties between sedimentary and crystalline rocks. Acoustic image logs from borehole DR-8S indicate a mean SHmax orientation of approximately N47° ± 21°E, aligning with regional stress indicators derived from focal mechanisms and GPS data. Weak alteration minerals on fractures and faults may facilitate reactivation, promoting stress release and local reorientation. Our results demonstrate that the present-day stress field is controlled by northeastward expansion of the Tibetan Plateau, with direct implications for the development and stability of the Qiabuqia geothermal reservoir.
采用非弹性应变恢复(ASR)、水力压裂(HF)和声波成像测井等方法对青藏高原东北部恰布恰地热田进行了全三维应力状态测定。对地热田5个钻孔的25个岩心样本进行的ASR测量显示,沉积盆地填充物与花岗岩基底之间存在明显的应力对比。沉积物表现为正常的断裂应力状态(Sv > SHmax > Shmin),主要受重力载荷控制。花岗岩基底则表现为走滑构造(SHmax > Sv > Shmin),以构造挤压为主。水平差应力在沉积物中随深度增加而减小,而在花岗岩中随深度增加而减小。我们将这些对比解释为沉积岩和结晶岩之间基底地形和力学性质的差异。DR-8S井眼的声波图像测井显示,平均最大震源方向约为N47°±21°E,与震源机制和GPS数据得出的区域应力指标一致。裂缝和断层上的弱蚀变矿物可能促进再活化,促进应力释放和局部定向。研究结果表明,青藏高原东北向扩张控制了现今应力场,这对恰布恰地热储层的发育和稳定具有直接影响。
{"title":"Multi-method constrained stress states in the Qiabuqia geothermal field, NW China: Insights from basin-basement contrasts","authors":"Zijuan Hu ,&nbsp;Shengsheng Zhang ,&nbsp;Chongyuan Zhang ,&nbsp;Shian Zhang ,&nbsp;Derek Elsworth ,&nbsp;Wen Meng ,&nbsp;Xianghui Qin","doi":"10.1016/j.ijrmms.2026.106422","DOIUrl":"10.1016/j.ijrmms.2026.106422","url":null,"abstract":"<div><div>We applied anelastic strain recovery (ASR), hydraulic fracturing (HF), and acoustic image logging to determine the full three-dimensional stress state in the Qiabuqia geothermal field, northeastern Tibetan Plateau. ASR measurements from twenty-five core samples across five boreholes in the geothermal field reveal a pronounced stress contrast between the sedimentary basin fill and the underlying granite basement. The sediments exhibit a normal faulting stress regime (S<sub>v</sub> &gt; S<sub>Hmax</sub> &gt; S<sub>hmin</sub>), primarily governed by gravitational loading. In contrast, the granite basement exhibits a strike-slip regime (S<sub>Hmax</sub> &gt; S<sub>v</sub> &gt; S<sub>hmin</sub>), indicating a dominant tectonic compression. Horizontal differential stress increases with depth in the sediments but decreases within the granite. We interpret these contrasts as resulting from variations in basement topography and mechanical properties between sedimentary and crystalline rocks. Acoustic image logs from borehole DR-8S indicate a mean S<sub>Hmax</sub> orientation of approximately N47° ± 21°E, aligning with regional stress indicators derived from focal mechanisms and GPS data. Weak alteration minerals on fractures and faults may facilitate reactivation, promoting stress release and local reorientation. Our results demonstrate that the present-day stress field is controlled by northeastward expansion of the Tibetan Plateau, with direct implications for the development and stability of the Qiabuqia geothermal reservoir.</div></div>","PeriodicalId":54941,"journal":{"name":"International Journal of Rock Mechanics and Mining Sciences","volume":"199 ","pages":"Article 106422"},"PeriodicalIF":7.5,"publicationDate":"2026-01-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145961726","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Ultrasonic sensing of the mechanical fingerprint of reactive transport in rock 岩石反应输运力学指纹的超声检测
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-13 DOI: 10.1016/j.ijrmms.2026.106404
Ali Aminzadeh , Prasanna Salasiya , Joseph F. Labuz , Mohammad Nooraiepour , Bojan B. Guzina
Mineral carbon storage in rock formations has gained significant interest in recent years. In principle, changes in mechanical rock properties driven by carbon mineralization could be quantified using seismic methods, opening the door toward field monitoring of carbon storage. However, these changes may vary spatially within a rock mass when reactive transport occurs. In this vein, full-field ultrasonic characterization of reacted specimens can help shed light on the process. We use a 3D Scanning Laser Doppler Vibrometer to perform full-field monitoring of one-dimensional (1D) ultrasonic waves in rod-shaped sandstone specimens exposed to NaCl-rich fluid. Our initial experiments were conducted on intact sandstone specimens with high aspect ratio (length/diameter15) to cater for 1D axial wave propagation. To investigate the evolution of the Young’s modulus and attenuation of rock due to reactive transport, we exposed the specimens to an under-saturated NaCl solution, achieving supersaturation – and so mineralization – through evaporation. The upward movement of the fluid, supplied at the bottom of each specimen, was achieved through capillary action. We deploy an elastography-type approach to back-analysis, known as modified-error-in-constitutive-relation (MECR) approach, to expose the spatially-heterogeneous evolution of mechanical rock properties due to reactive transport. Our results consistently demonstrate (i) an approximately 30% degradation of the Young’s modulus and (ii) 7-fold increase in ultrasonic attenuation due to mineralization. To better understand the root causes of these changes, we made use of the X-ray micro-computed tomography and scanning electron microscopy of selected cross-sections. The grain-scale information suggests that pore filling with powder-like participate is responsible for the increase in attenuation, while microcracking – observed by acoustic emission monitoring – is behind the observed damage of rock.
近年来,矿物碳在岩层中的储存引起了人们极大的兴趣。原则上,碳矿化驱动的岩石力学性质变化可以用地震方法量化,为现场监测碳储量打开了大门。然而,当反应性输运发生时,这些变化可能在岩体内的空间上有所不同。在这种情况下,反应样品的全场超声表征可以帮助阐明这一过程。我们使用3D扫描激光多普勒振动仪对暴露于富盐流体中的棒状砂岩试样进行一维(1D)超声波的全方位监测。我们的初步实验是在高长径比(长径/直径)的完整砂岩样品上进行的,以满足一维轴向波的传播。为了研究杨氏模量的演化和岩石因反应输运而产生的衰减,我们将样品暴露在不饱和的NaCl溶液中,通过蒸发实现过饱和,从而实现矿化。在每个样品的底部提供的流体的向上运动是通过毛细管作用实现的。我们采用弹性学类型的方法进行反分析,称为修正误差本构关系(MECR)方法,以揭示由于反应性输运导致的岩石力学性质的空间非均质演化。我们的结果一致表明:(1)杨氏模量下降了约30%,(2)由于矿化,超声波衰减增加了7倍。为了更好地了解这些变化的根本原因,我们使用了x射线显微计算机断层扫描和扫描电子显微镜选择的截面。颗粒级信息表明,孔隙中粉状物质的填充是导致衰减增加的原因,而声发射监测观测到的微裂纹是导致岩石损伤的原因。
{"title":"Ultrasonic sensing of the mechanical fingerprint of reactive transport in rock","authors":"Ali Aminzadeh ,&nbsp;Prasanna Salasiya ,&nbsp;Joseph F. Labuz ,&nbsp;Mohammad Nooraiepour ,&nbsp;Bojan B. Guzina","doi":"10.1016/j.ijrmms.2026.106404","DOIUrl":"10.1016/j.ijrmms.2026.106404","url":null,"abstract":"<div><div>Mineral carbon storage in rock formations has gained significant interest in recent years. In principle, changes in mechanical rock properties driven by carbon mineralization could be quantified using seismic methods, opening the door toward field monitoring of carbon storage. However, these changes may vary spatially within a rock mass when reactive transport occurs. In this vein, full-field ultrasonic characterization of reacted specimens can help shed light on the process. We use a 3D Scanning Laser Doppler Vibrometer to perform full-field monitoring of one-dimensional (1D) ultrasonic waves in rod-shaped sandstone specimens exposed to NaCl-rich fluid. Our initial experiments were conducted on intact sandstone specimens with high aspect ratio (<span><math><mrow><mtext>length/diameter</mtext><mo>≃</mo><mn>15</mn></mrow></math></span>) to cater for 1D axial wave propagation. To investigate the evolution of the Young’s modulus and attenuation of rock due to reactive transport, we exposed the specimens to an under-saturated NaCl solution, achieving supersaturation – and so mineralization – through evaporation. The upward movement of the fluid, supplied at the bottom of each specimen, was achieved through capillary action. We deploy an elastography-type approach to back-analysis, known as modified-error-in-constitutive-relation (MECR) approach, to expose the spatially-heterogeneous evolution of mechanical rock properties due to reactive transport. Our results consistently demonstrate (i) an approximately 30% degradation of the Young’s modulus and (ii) 7-fold increase in ultrasonic attenuation due to mineralization. To better understand the root causes of these changes, we made use of the X-ray micro-computed tomography and scanning electron microscopy of selected cross-sections. The grain-scale information suggests that pore filling with powder-like participate is responsible for the increase in attenuation, while microcracking – observed by acoustic emission monitoring – is behind the observed damage of rock.</div></div>","PeriodicalId":54941,"journal":{"name":"International Journal of Rock Mechanics and Mining Sciences","volume":"199 ","pages":"Article 106404"},"PeriodicalIF":7.5,"publicationDate":"2026-01-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145957139","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Numerical study on pillar stress distribution in room-and-pillar hard rock mines using stress concentration factor based on tributary area: Bridging to pressure arch effect 基于分支面积应力集中系数的房柱硬岩矿山矿柱应力分布数值研究:桥接至压力拱效应
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-13 DOI: 10.1016/j.ijrmms.2025.106198
Dong-Ho Yoon , Jae-Joon Song
This study analyzes how the stress distribution in panel pillars of room-and-pillar mining systems deviates from Tributary Area Theory (TAT) under changes in key design parameters, such as overburden height, pillar array size, opening width-to-pillar width ratio, and pillar width. The Stress Concentration Factor based on Tributary Area (SCFT) was employed to visualize the stress disturbance profile, known as the pressure arch effect, and provide a clearer understanding of load distribution while facilitating individual pillar stress calculations. Numerical analysis revealed that SCFT profiles converge to stable shapes with increasing depth, and as panel width grows, central pillars exhibit SCFT values closer to TAT predictions, while discrepancies persist at peripheral pillars. This observation suggests the possibility of controlled peripheral pillar trimming to enhance production without excessively increasing stress levels. Sensitivity analysis further indicated that the horizontal-to-vertical stress ratio (k) and pillar height, often overlooked, are critical factors for accurate stress estimation. These findings demonstrate the potential of SCFT as a practical tool for realistic pillar stress estimation and its applicability for optimizing room-and-pillar mining system designs.
分析了在覆岩高度、矿柱阵列尺寸、开孔宽与矿柱宽比、矿柱宽度等关键设计参数变化的情况下,房柱联合开采系统盘状矿柱应力分布偏离支路区理论(TAT)的规律。采用基于支路面积的应力集中系数(SCFT)将应力扰动曲线(即压力拱效应)可视化,从而更清晰地了解荷载分布,同时便于各矿柱的应力计算。数值分析表明,随着深度的增加,SCFT曲线趋于稳定,随着面板宽度的增加,中心柱的SCFT值更接近TAT预测值,而外围柱的SCFT值仍然存在差异。这一观察结果表明,在不过度增加应力水平的情况下,控制外围矿柱修剪以提高产量的可能性。敏感性分析进一步表明,水平-垂直应力比(k)和矿柱高度是准确估计应力的关键因素,但往往被忽视。这些发现证明了SCFT作为实际矿柱应力估计的实用工具的潜力,以及它在优化房柱采矿系统设计中的适用性。
{"title":"Numerical study on pillar stress distribution in room-and-pillar hard rock mines using stress concentration factor based on tributary area: Bridging to pressure arch effect","authors":"Dong-Ho Yoon ,&nbsp;Jae-Joon Song","doi":"10.1016/j.ijrmms.2025.106198","DOIUrl":"10.1016/j.ijrmms.2025.106198","url":null,"abstract":"<div><div>This study analyzes how the stress distribution in panel pillars of room-and-pillar mining systems deviates from Tributary Area Theory (TAT) under changes in key design parameters, such as overburden height, pillar array size, opening width-to-pillar width ratio, and pillar width. The Stress Concentration Factor based on Tributary Area (SCF<sub>T</sub>) was employed to visualize the stress disturbance profile, known as the pressure arch effect, and provide a clearer understanding of load distribution while facilitating individual pillar stress calculations. Numerical analysis revealed that <span><math><mrow><msub><mrow><mi>S</mi><mi>C</mi><mi>F</mi></mrow><mi>T</mi></msub></mrow></math></span> profiles converge to stable shapes with increasing depth, and as panel width grows, central pillars exhibit <span><math><mrow><msub><mrow><mi>S</mi><mi>C</mi><mi>F</mi></mrow><mi>T</mi></msub></mrow></math></span> values closer to TAT predictions, while discrepancies persist at peripheral pillars. This observation suggests the possibility of controlled peripheral pillar trimming to enhance production without excessively increasing stress levels. Sensitivity analysis further indicated that the horizontal-to-vertical stress ratio (<em>k</em>) and pillar height, often overlooked, are critical factors for accurate stress estimation. These findings demonstrate the potential of <span><math><mrow><msub><mrow><mi>S</mi><mi>C</mi><mi>F</mi></mrow><mi>T</mi></msub></mrow></math></span> as a practical tool for realistic pillar stress estimation and its applicability for optimizing room-and-pillar mining system designs.</div></div>","PeriodicalId":54941,"journal":{"name":"International Journal of Rock Mechanics and Mining Sciences","volume":"199 ","pages":"Article 106198"},"PeriodicalIF":7.5,"publicationDate":"2026-01-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145961727","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Dynamic response analysis of three-layer anchorage under radial P-wave loading: wave-function expansion for optimal thickness 径向纵波荷载作用下三层锚固动力响应分析:波函数展开式最优厚度
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-12 DOI: 10.1016/j.ijrmms.2026.106416
Jian Ouyang , Xiuzhi Shi , Xianyang Qiu , Chengxing Zong , Zongguo Zhang
Blasting-induced dynamic loads are a primary risk factor for failure in underground support structures. Based on the wave-function expansion method, this study develops a dynamic response model of a surrounding rock-anchoring agent-bolt system subjected to cylindrical P-wave incidence. A dimensionless dynamic stress concentration factor (DSCF) is introduced to characterize the stress within the system. The influences of blasting source frequency, impact distance, anchoring agent thickness, and material impedance mismatch on the evolution of DSCF are systematically analyzed. Parametric analyses reveal that low-frequency excitation leads to lower and more uniformly distributed DSCF. The thickness and shear modulus of the anchoring agent significantly affect the magnitude and directional distribution of DSCF. The LS-DYNA simulations validate the model's ability to capture wave propagation, interface reflections, and stress concentration, confirming that reflected shear waves govern circumferential stress and make the 90° direction most prone to tensile failure. Physical model tests further verify this trend, with higher 90° strain and stronger internal interface response, supporting the model's engineering applicability. A three-dimensional response surface is established, incorporating frequency, impedance, and thickness. Based on this surface, a quantitative optimization strategy is proposed: within the parameter space examined here, thickness ratios in the range of 1.4–1.8 reduce DSCF, combined with suitable impedance matching, can effectively minimize DSCF under multi-frequency excitation under the adopted model assumptions. This study establishes an analytical framework and validated failure mechanism for radial dynamic stress concentration, and proposes a quantifiable design criterion that enables more reliable optimization of anchorage systems under blasting loads.
爆破动荷载是地下支护结构破坏的主要危险因素。基于波函数展开法,建立了柱面纵波作用下围岩-锚固剂-锚杆体系的动力响应模型。引入无量纲动态应力集中因子(DSCF)来表征系统内的应力。系统分析了爆破源频率、冲击距离、锚固剂厚度、材料阻抗失配等因素对DSCF演化的影响。参数分析表明,低频激励导致的离散流场更小且分布更均匀。锚固剂的厚度和剪切模量对DSCF的大小和方向分布有显著影响。LS-DYNA模拟验证了该模型捕捉波传播、界面反射和应力集中的能力,证实了反射剪切波控制周向应力,并使90°方向最容易发生拉伸破坏。物理模型试验进一步验证了这一趋势,具有更高的90°应变和更强的内部界面响应,支持了模型的工程适用性。建立了包含频率、阻抗和厚度的三维响应面。基于该曲面,提出了一种定量优化策略:在所选取的参数空间内,在采用的模型假设下,厚度比在1.4 ~ 1.8范围内减小DSCF,并结合合适的阻抗匹配,可以有效地减小多频激励下的DSCF。本研究建立了径向动应力集中的分析框架,验证了破坏机理,提出了可量化的设计准则,使爆破荷载作用下锚固体系的优化更加可靠。
{"title":"Dynamic response analysis of three-layer anchorage under radial P-wave loading: wave-function expansion for optimal thickness","authors":"Jian Ouyang ,&nbsp;Xiuzhi Shi ,&nbsp;Xianyang Qiu ,&nbsp;Chengxing Zong ,&nbsp;Zongguo Zhang","doi":"10.1016/j.ijrmms.2026.106416","DOIUrl":"10.1016/j.ijrmms.2026.106416","url":null,"abstract":"<div><div>Blasting-induced dynamic loads are a primary risk factor for failure in underground support structures. Based on the wave-function expansion method, this study develops a dynamic response model of a surrounding rock-anchoring agent-bolt system subjected to cylindrical P-wave incidence. A dimensionless dynamic stress concentration factor (DSCF) is introduced to characterize the stress within the system. The influences of blasting source frequency, impact distance, anchoring agent thickness, and material impedance mismatch on the evolution of DSCF are systematically analyzed. Parametric analyses reveal that low-frequency excitation leads to lower and more uniformly distributed DSCF. The thickness and shear modulus of the anchoring agent significantly affect the magnitude and directional distribution of DSCF. The LS-DYNA simulations validate the model's ability to capture wave propagation, interface reflections, and stress concentration, confirming that reflected shear waves govern circumferential stress and make the 90° direction most prone to tensile failure. Physical model tests further verify this trend, with higher 90° strain and stronger internal interface response, supporting the model's engineering applicability. A three-dimensional response surface is established, incorporating frequency, impedance, and thickness. Based on this surface, a quantitative optimization strategy is proposed: within the parameter space examined here, thickness ratios in the range of 1.4–1.8 reduce DSCF, combined with suitable impedance matching, can effectively minimize DSCF under multi-frequency excitation under the adopted model assumptions. This study establishes an analytical framework and validated failure mechanism for radial dynamic stress concentration, and proposes a quantifiable design criterion that enables more reliable optimization of anchorage systems under blasting loads.</div></div>","PeriodicalId":54941,"journal":{"name":"International Journal of Rock Mechanics and Mining Sciences","volume":"199 ","pages":"Article 106416"},"PeriodicalIF":7.5,"publicationDate":"2026-01-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145956878","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
A microplane-enhanced quasi-bond method with a dual-mechanism fracture criterion for mixed-mode failure in rock-like materials 基于双机制断裂准则的类岩材料混合模式破坏微平面增强准粘结方法
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-12 DOI: 10.1016/j.ijrmms.2025.106396
Wei-Tong Li , Qi-Zhi Zhu , Wei-Jian Li , Xing-Guang Zhao
This paper presents an enhanced quasi-bond method for modeling mixed-mode fracture in rock-like materials. By integrating concepts from microplane theory, the proposed approach incorporates strain decomposition and projection onto bond directions, establishing bond-level stiffness through energy equivalence with classical elasticity. The formulation accommodates arbitrary Poisson’s ratios and preserves consistency across two-dimensional/three-dimensional settings. A novel dual-mechanism fracture criterion is introduced, incorporating both a bond-breakage rule based on energy thresholds and microstress states to differentiate tensile and shear cracks, and a complementary bond-level softening model that concurrently captures tensile and shear strength degradation. To improve numerical accuracy, a smoothed strain technique synchronizes strain updates with bond failure, and a hybrid finite element/quasi-bond coupling strategy enables efficient localized fracture resolution. Validations against notched beams and multi-flawed specimens under compression demonstrate the accuracy of the proposed model in solving mixed-mode fracture in rock-like materials. Engineering-scale extensions to jointed rock slopes reveal step-path fracture network evolution governed by flaw interaction-driven coalescence patterns, advancing geohazard predictions through explicit linkage between discrete fracturing and macro-scale instability.
本文提出了一种改进的类岩石材料混合模式断裂模拟准键方法。该方法结合微平面理论,结合应变分解和键向投影,通过与经典弹性力学的能量等效建立键级刚度。该公式适用于任意泊松比,并保持二维/三维设置的一致性。引入了一种新的双机制断裂准则,结合了基于能量阈值和微应力状态的粘结破坏规则来区分拉伸和剪切裂纹,以及同时捕获拉伸和剪切强度退化的互补粘结级软化模型。为了提高数值精度,一种平滑应变技术将应变更新与粘结破坏同步,一种混合有限元/准粘结耦合策略可以实现有效的局部断裂分辨率。对缺口梁和多缺陷压缩试样的验证表明了该模型在求解类岩石材料混合模式断裂中的准确性。对节理岩质边坡的工程尺度扩展揭示了由缺陷相互作用驱动的聚结模式控制的阶梯裂缝网络演化,通过离散压裂与宏观尺度失稳之间的明确联系,推进了地质灾害预测。
{"title":"A microplane-enhanced quasi-bond method with a dual-mechanism fracture criterion for mixed-mode failure in rock-like materials","authors":"Wei-Tong Li ,&nbsp;Qi-Zhi Zhu ,&nbsp;Wei-Jian Li ,&nbsp;Xing-Guang Zhao","doi":"10.1016/j.ijrmms.2025.106396","DOIUrl":"10.1016/j.ijrmms.2025.106396","url":null,"abstract":"<div><div>This paper presents an enhanced quasi-bond method for modeling mixed-mode fracture in rock-like materials. By integrating concepts from microplane theory, the proposed approach incorporates strain decomposition and projection onto bond directions, establishing bond-level stiffness through energy equivalence with classical elasticity. The formulation accommodates arbitrary Poisson’s ratios and preserves consistency across two-dimensional/three-dimensional settings. A novel dual-mechanism fracture criterion is introduced, incorporating both a bond-breakage rule based on energy thresholds and microstress states to differentiate tensile and shear cracks, and a complementary bond-level softening model that concurrently captures tensile and shear strength degradation. To improve numerical accuracy, a smoothed strain technique synchronizes strain updates with bond failure, and a hybrid finite element/quasi-bond coupling strategy enables efficient localized fracture resolution. Validations against notched beams and multi-flawed specimens under compression demonstrate the accuracy of the proposed model in solving mixed-mode fracture in rock-like materials. Engineering-scale extensions to jointed rock slopes reveal step-path fracture network evolution governed by flaw interaction-driven coalescence patterns, advancing geohazard predictions through explicit linkage between discrete fracturing and macro-scale instability.</div></div>","PeriodicalId":54941,"journal":{"name":"International Journal of Rock Mechanics and Mining Sciences","volume":"199 ","pages":"Article 106396"},"PeriodicalIF":7.5,"publicationDate":"2026-01-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145956879","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Capturing dynamic rockburst behaviors of deep rock masses with a novel nonlocal general particle dynamic method 用一种新的非局部一般粒子动力学方法捕捉深部岩体的动态岩爆行为
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-10 DOI: 10.1016/j.ijrmms.2026.106403
Jin-Hu Pan , Xiao-Ping Zhou
Understanding rockburst mechanism has always been a fundamental challenge in the field of geotechnical engineering. The nonlocal methods have excellent potential to simulate fragment problems such as rockburst. However, early researches employing nonlocal methods primarily focused on the static process of rockburst, their capabilities in simulating the full dynamic fracture propagation and fragment ejection processes remain to be further explored. To reproduce the dynamic rockburst process in deep tunnel, the present work proposes a novel nonlocal general particle dynamic method. Firstly, four types of contact behaviors in rockburst are identified and a contact model based on the theorem of momentum is proposed to determine the contact force. Secondly, we establish a joint model that distinguishes the tensile, compressive and shear deformation features of bonds to characterize the joints in rock masses. Thirdly, the Holmquist-Johnson-Cook constitutive model is modified to consider the features of high pressure and high strain rate in rockburst process and to simulate the damage evolution by incorporating the critical stretch criterion and critical equivalent strain criterion. The first three examples, oedometric test, block sliding on an inclined plane and wave propagation in a one-dimensional bar with a joint, are conducted to verify the proposed numerical framework. The final three examples simulate the rockburst phenomenon induced by excavation. The numerical results obtained by the developed approach are in high agreement with the experimental results and the field observations. The several typical features in rockburst, particle spalling, particle ejection and V-shaped rockburst pit, are successfully reproduced, which demonstrate that the proposed method possesses excellent ability to model the dynamic rockburst process and can provide a theoretical basis for hazard assessment and prevention strategies in deep underground engineering.
了解岩爆机理一直是岩土工程领域的一个基本挑战。非局部方法在模拟岩爆等破片问题上具有很好的潜力。然而,早期采用非局部方法的研究主要集中在岩爆的静态过程,其模拟全动态裂缝扩展和破片喷射过程的能力有待进一步探索。为了再现深埋隧道岩爆的动态过程,提出了一种新的非局部一般颗粒动力学方法。首先,识别了岩爆中的四种接触行为,并提出了基于动量定理的接触模型来确定接触力。其次,建立了区分粘结体拉伸、压缩和剪切变形特征的节理模型,对岩体中的节理进行了表征。第三,对Holmquist-Johnson-Cook本构模型进行修正,考虑岩爆过程中高压、高应变率的特点,引入临界拉伸准则和临界等效应变准则,模拟岩爆过程的损伤演化;通过测量试验、斜面上的块体滑动和带节理的一维杆体中的波传播三个算例验证了所提出的数值框架。最后三个算例模拟了开挖引起的岩爆现象。该方法的数值计算结果与实验结果和现场观测结果吻合较好。成功再现了岩爆中颗粒剥落、颗粒抛射和v型岩爆坑等典型特征,表明该方法具有良好的岩爆动态过程建模能力,可为深埋地下工程灾害评价和防治策略提供理论依据。
{"title":"Capturing dynamic rockburst behaviors of deep rock masses with a novel nonlocal general particle dynamic method","authors":"Jin-Hu Pan ,&nbsp;Xiao-Ping Zhou","doi":"10.1016/j.ijrmms.2026.106403","DOIUrl":"10.1016/j.ijrmms.2026.106403","url":null,"abstract":"<div><div>Understanding rockburst mechanism has always been a fundamental challenge in the field of geotechnical engineering. The nonlocal methods have excellent potential to simulate fragment problems such as rockburst. However, early researches employing nonlocal methods primarily focused on the static process of rockburst, their capabilities in simulating the full dynamic fracture propagation and fragment ejection processes remain to be further explored. To reproduce the dynamic rockburst process in deep tunnel, the present work proposes a novel nonlocal general particle dynamic method. Firstly, four types of contact behaviors in rockburst are identified and a contact model based on the theorem of momentum is proposed to determine the contact force. Secondly, we establish a joint model that distinguishes the tensile, compressive and shear deformation features of bonds to characterize the joints in rock masses. Thirdly, the Holmquist-Johnson-Cook constitutive model is modified to consider the features of high pressure and high strain rate in rockburst process and to simulate the damage evolution by incorporating the critical stretch criterion and critical equivalent strain criterion. The first three examples, oedometric test, block sliding on an inclined plane and wave propagation in a one-dimensional bar with a joint, are conducted to verify the proposed numerical framework. The final three examples simulate the rockburst phenomenon induced by excavation. The numerical results obtained by the developed approach are in high agreement with the experimental results and the field observations. The several typical features in rockburst, particle spalling, particle ejection and V-shaped rockburst pit, are successfully reproduced, which demonstrate that the proposed method possesses excellent ability to model the dynamic rockburst process and can provide a theoretical basis for hazard assessment and prevention strategies in deep underground engineering.</div></div>","PeriodicalId":54941,"journal":{"name":"International Journal of Rock Mechanics and Mining Sciences","volume":"199 ","pages":"Article 106403"},"PeriodicalIF":7.5,"publicationDate":"2026-01-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145956889","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Analysis of seismic potential in a depleted chalk reservoir subject to CO2 injection 注二氧化碳作用下枯竭白垩储层地震潜力分析
IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-01-09 DOI: 10.1016/j.ijrmms.2025.106394
M.R. Hajiabadi, F. Amour, B. Hosseinzadeh, A.C. Cheriki, H. Nick
This study presents a multi-scale modelling framework to evaluate fault reactivation risks and seismic potential during CO2 injection into a highly depleted and deformable chalk reservoir, using the Harald East field in the northern part of the Danish North Sea as a case study. A robust multi-scale Thermo-Hydro-Mechanical (THM) modeling approach is developed to bridge field- and fault-scale processes, supporting fault stability and seismic risk assessment in CO2 storage. A field-scale coupled flow-geomechanical model is used to screen for critically-stressed faults, while fault-scale simulations investigate slip behaviour using a Mohr-Coulomb frictional model, combined with a rate-dependent frictional model to assess specific potential seismic events. THM analysis under realistic CO2 injection scenarios reveals that faults remain stable with friction coefficients of 0.6. However, simulations with reduced initial friction coefficients (e.g., 0.27 and 0.36) indicate localized slip risks during both production and injection phases along the plane of one single fault out of a total of 30 faults analysed. As the reservoir repressurizes, the stress regime transitions from normal to reverse faulting, accompanied by a significant reorientation in principal stress. This shift of stress regime causes a progressive rise in shear stress on the fault plane as repressurization continues, resulting in higher slip tendency values and a greater likelihood of seismic reactivation. Besides, the results demonstrate the benefit of a combined field- and fault-scale approach that enhances computational efficiency by restricting detailed analyses to critical faults and critical time throughout the injection period. This work provides a framework for fault stability and seismic risk assessments, offering key insights for the safe implementation of underground CO2 storage projects.
本研究以丹麦北海北部Harald East油田为例,提出了一个多尺度建模框架,以评估向高度枯竭和可变形的白垩油藏注入二氧化碳期间断层再激活风险和地震潜力。开发了一种鲁棒的多尺度热-水-机械(THM)建模方法,以桥接现场和断层尺度过程,支持二氧化碳储存中的断层稳定性和地震风险评估。现场尺度的耦合流动-地质力学模型用于筛选临界应力断层,而断层尺度的模拟使用Mohr-Coulomb摩擦模型来研究滑动行为,并结合速率相关的摩擦模型来评估特定的潜在地震事件。在实际CO2注入场景下的THM分析表明,断层保持稳定,摩擦系数为0.6。然而,降低初始摩擦系数(例如0.27和0.36)的模拟表明,在分析的30条断层中,沿单个断层的平面,在生产和注入阶段都存在局部滑动风险。随着储层增压,应力状态由正断层向逆断层转变,主应力方向发生明显改变。随着再增压的继续,这种应力状态的转变导致断面上的剪应力逐渐上升,导致更高的滑动倾向值和更大的地震再激活可能性。此外,研究结果还证明了现场和断层尺度相结合的方法的优势,该方法将详细分析限制在整个注入周期的关键断层和关键时间,从而提高了计算效率。这项工作为断层稳定性和地震风险评估提供了一个框架,为地下二氧化碳储存项目的安全实施提供了关键见解。
{"title":"Analysis of seismic potential in a depleted chalk reservoir subject to CO2 injection","authors":"M.R. Hajiabadi,&nbsp;F. Amour,&nbsp;B. Hosseinzadeh,&nbsp;A.C. Cheriki,&nbsp;H. Nick","doi":"10.1016/j.ijrmms.2025.106394","DOIUrl":"10.1016/j.ijrmms.2025.106394","url":null,"abstract":"<div><div>This study presents a multi-scale modelling framework to evaluate fault reactivation risks and seismic potential during CO<sub>2</sub> injection into a highly depleted and deformable chalk reservoir, using the Harald East field in the northern part of the Danish North Sea as a case study. A robust multi-scale Thermo-Hydro-Mechanical (THM) modeling approach is developed to bridge field- and fault-scale processes, supporting fault stability and seismic risk assessment in CO<sub>2</sub> storage. A field-scale coupled flow-geomechanical model is used to screen for critically-stressed faults, while fault-scale simulations investigate slip behaviour using a Mohr-Coulomb frictional model, combined with a rate-dependent frictional model to assess specific potential seismic events. THM analysis under realistic CO<sub>2</sub> injection scenarios reveals that faults remain stable with friction coefficients of 0.6. However, simulations with reduced initial friction coefficients (e.g., 0.27 and 0.36) indicate localized slip risks during both production and injection phases along the plane of one single fault out of a total of 30 faults analysed. As the reservoir repressurizes, the stress regime transitions from normal to reverse faulting, accompanied by a significant reorientation in principal stress. This shift of stress regime causes a progressive rise in shear stress on the fault plane as repressurization continues, resulting in higher slip tendency values and a greater likelihood of seismic reactivation. Besides, the results demonstrate the benefit of a combined field- and fault-scale approach that enhances computational efficiency by restricting detailed analyses to critical faults and critical time throughout the injection period. This work provides a framework for fault stability and seismic risk assessments, offering key insights for the safe implementation of underground CO<sub>2</sub> storage projects.</div></div>","PeriodicalId":54941,"journal":{"name":"International Journal of Rock Mechanics and Mining Sciences","volume":"199 ","pages":"Article 106394"},"PeriodicalIF":7.5,"publicationDate":"2026-01-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145941325","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
期刊
International Journal of Rock Mechanics and Mining Sciences
全部 Acc. Chem. Res. ACS Applied Bio Materials ACS Appl. Electron. Mater. ACS Appl. Energy Mater. ACS Appl. Mater. Interfaces ACS Appl. Nano Mater. ACS Appl. Polym. Mater. ACS BIOMATER-SCI ENG ACS Catal. ACS Cent. Sci. ACS Chem. Biol. ACS Chemical Health & Safety ACS Chem. Neurosci. ACS Comb. Sci. ACS Earth Space Chem. ACS Energy Lett. ACS Infect. Dis. ACS Macro Lett. ACS Mater. Lett. ACS Med. Chem. Lett. ACS Nano ACS Omega ACS Photonics ACS Sens. ACS Sustainable Chem. Eng. ACS Synth. Biol. Anal. Chem. BIOCHEMISTRY-US Bioconjugate Chem. BIOMACROMOLECULES Chem. Res. Toxicol. Chem. Rev. Chem. Mater. CRYST GROWTH DES ENERG FUEL Environ. Sci. Technol. Environ. Sci. Technol. Lett. Eur. J. Inorg. Chem. IND ENG CHEM RES Inorg. Chem. J. Agric. Food. Chem. J. Chem. Eng. Data J. Chem. Educ. J. Chem. Inf. Model. J. Chem. Theory Comput. J. Med. Chem. J. Nat. Prod. J PROTEOME RES J. Am. Chem. Soc. LANGMUIR MACROMOLECULES Mol. Pharmaceutics Nano Lett. Org. Lett. ORG PROCESS RES DEV ORGANOMETALLICS J. Org. Chem. J. Phys. Chem. J. Phys. Chem. A J. Phys. Chem. B J. Phys. Chem. C J. Phys. Chem. Lett. Analyst Anal. Methods Biomater. Sci. Catal. Sci. Technol. Chem. Commun. Chem. Soc. Rev. CHEM EDUC RES PRACT CRYSTENGCOMM Dalton Trans. Energy Environ. Sci. ENVIRON SCI-NANO ENVIRON SCI-PROC IMP ENVIRON SCI-WAT RES Faraday Discuss. Food Funct. Green Chem. Inorg. Chem. Front. Integr. Biol. J. Anal. At. Spectrom. J. Mater. Chem. A J. Mater. Chem. B J. Mater. Chem. C Lab Chip Mater. Chem. Front. Mater. Horiz. MEDCHEMCOMM Metallomics Mol. Biosyst. Mol. Syst. Des. Eng. Nanoscale Nanoscale Horiz. Nat. Prod. Rep. New J. Chem. Org. Biomol. Chem. Org. Chem. Front. PHOTOCH PHOTOBIO SCI PCCP Polym. Chem.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1