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Creep behavior and microstructural evolution of unsaturated red-bed mudstone under coupled matric suction-stress effects 基质吸力-应力耦合作用下非饱和红层泥岩蠕变行为及微观结构演化
IF 8.4 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-03-01 Epub Date: 2026-01-12 DOI: 10.1016/j.enggeo.2026.108558
Guoqing Cai , Fengjie Yin , Hengshuo Liu , Yanlin Su , Rui Yang
Red-bed mudstone is a widely distributed sedimentary fill material in western China and exhibits pronounced moisture sensitivity, making it susceptible to long-term creep deformation under unsaturated conditions. To elucidate its time-dependent mechanical behavior and underlying microstructural control mechanisms, a series of multi-stage creep tests was conducted using a GDS double-cell unsaturated triaxial apparatus under controlled matric suctions of 100, 200, and 300 kPa. The microstructural evolution before and after creep was systematically investigated through scanning electron microscopy (SEM) and mercury intrusion porosimetry (MIP). The results indicate that red-bed mudstone exhibits strongly nonlinear, time-dependent deformation characteristics under coupled matric suction-stress conditions. At high creep loading levels, increasing matric suction markedly suppresses pore collapse and compressive deformation, leading to a progressive transition in the creep mechanism from compression-dominated to shear-dominated behavior. Matric suction primarily inhibits creep deformation by enhancing structural stability, whereas higher stress levels intensify structural rearrangement and compaction. Microstructural analyses further reveal that increasing suction reduces pore connectivity and promotes face-to-face contacts between platy minerals, thereby effectively slowing the creep rate. In addition, the regulatory effect of matric suction on creep stiffness shows a pronounced dependence on stress level, and creep stiffness exhibits a characteristic time-dependent softening behavior. These findings provide new insights into the long-term creep deformation mechanisms of unsaturated red-bed mudstone and offer valuable reference information for evaluating the long-term stability of high-fill station-yard subgrades under complex geological conditions.
红层泥岩是中国西部地区广泛分布的沉积填充物,具有明显的水分敏感性,在非饱和条件下易发生长期蠕变变形。为了阐明其随时间变化的力学行为和潜在的微观结构控制机制,使用GDS双室非饱和三轴仪在100,200和300 kPa的受控基质吸力下进行了一系列多阶段蠕变试验。采用扫描电镜(SEM)和压汞孔隙法(MIP)对蠕变前后的微观组织演变进行了系统研究。结果表明,红层泥岩在基质吸力-应力耦合作用下表现出强烈的非线性、时变变形特征。在高蠕变加载水平下,增加基质吸力可显著抑制孔隙坍塌和压缩变形,导致蠕变机制由压缩主导向剪切主导逐步转变。基质吸力主要通过增强结构稳定性来抑制蠕变变形,而较高的应力水平会加剧结构重排和压实。微观结构分析进一步表明,吸力的增加降低了孔隙连通性,促进了板状矿物之间的面对面接触,从而有效地减缓了蠕变速率。此外,基质吸力对蠕变刚度的调节作用明显依赖于应力水平,蠕变刚度表现出典型的随时间变化的软化行为。这些研究结果为研究非饱和红层泥岩的长期蠕变变形机制提供了新的认识,为评价复杂地质条件下高填方站场路基的长期稳定性提供了有价值的参考信息。
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引用次数: 0
Capturing the hole effect in Qiantang River alluvial silt by cone penetration test 用锥贯试验捕捉钱塘江冲积粉土的孔效应
IF 8.4 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-03-01 Epub Date: 2026-01-14 DOI: 10.1016/j.enggeo.2026.108564
Yuguo Su , Tiantian Ying , Qiaokan Wang , Xiaodong Pan
Soil spatial variability exhibits significant regional characteristics arising from various geological processes, weathering effects, and stress history during sedimentation. The spatial variability can influence the performance of geotechnical systems, and accurately capturing it is essential for effective reliability analysis. This study first compares the performance of the auto-correlation function and variance reduction function under different fitting strategies. Subsequently, the sampling strategies that yield the best performance in estimating the scale of fluctuation (SOF) are identified. After that, cone penetration test data are collected from sites along the Qiantang River to quantify the spatial variability parameters of the alluvial silt. Analysis reveals that the SOF and its associated uncertainty generally increase with expanding investigation domain length. The mean SOF rises from 0.691 m to 1.225 m across scales from 5 m to 15 m. The hole effect describes a spatial autocorrelation function that exhibits a non-monotonic, cyclical pattern as lag distance increases. A significant hole effect, identified in 75.6% of cases with SOF values ranging from 0.190 m to 1.135 m, may be associated with rhythmic tidal sedimentation processes. The cosine Whittle-Matérn model successfully captures the finer features of the spatial correlation structure, including the SOF, smoothness, and hole effect.
土壤空间变异性表现出明显的区域特征,这是由不同的地质过程、风化作用和沉积过程中的应力历史引起的。空间变异性会影响岩土系统的性能,准确捕捉空间变异性是进行可靠度分析的必要条件。本研究首先比较了自相关函数和方差缩减函数在不同拟合策略下的性能。随后,确定了在估计波动尺度(SOF)时产生最佳性能的采样策略。然后,在钱塘江沿岸各站点采集圆锥体穿透试验数据,量化冲积粉土的空间变异性参数。分析表明,随着研究范围的扩大,soff及其相关不确定性普遍增加。在5米至15米的尺度上,平均sofm从0.691米上升到1.225米。空穴效应描述了一种空间自相关函数,随着滞后距离的增加,该函数呈现出非单调的周期性模式。在sofm值为0.190 ~ 1.135 m范围内,75.6%的案例中发现了明显的孔效应,这可能与有节奏的潮汐沉积过程有关。余弦whittle - mat模型成功地捕获了空间相关结构的更精细的特征,包括柔度、平滑度和空穴效应。
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引用次数: 0
3D seismic response and disaster performance of T-shaped intersecting valley fault sites: A case study of a simply supported beam bridge across fault t形相交谷断层位的三维地震反应与灾害性能——以跨断层简支梁桥为例
IF 8.4 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-03-01 Epub Date: 2026-01-13 DOI: 10.1016/j.enggeo.2026.108563
Ke Yin , Zhiping Hu , Rui Wang , Xianglong Xu , Boyu Wang , Chao Zhang
Irregular topography and faults significantly affect seismic responses, causing notable variations that may show within 1 km2. This study investigates a simply supported bridge site in the Tianshan region, which features a fault and T-shaped intersecting valley topography. The site's actual topography is simulated to establish 3D finite element models, either considering or neglecting the influence of the fault, with 25 seismic waves input from different directions. The seismic response characteristics and mechanisms of the site and their impact on the simply supported beam bridge were analyzed. The results show that irregular topography and faults mainly affect the site's short-period (0.1–0.5 s) spectral acceleration. Short-period spectral acceleration at the peak is approximately twice that at the valley. In terms of the influence of the fault, seismic motion parallel or perpendicular to the fault strike enhances the short-period response near the fault by 1.6 or 4.9 times, respectively. When the seismic motion is parallel to the fault, the footwall response increases slightly, while the hanging wall undergoes no significant change. When the seismic motion is perpendicular to the fault, both the footwall and hanging wall responses increase, with a greater enhancement in the hanging wall response. This is likely related to the dynamic behavior of the fault zone and the seismic wave propagation mechanism. Considering the influence of the fault, energy dissipation, damage, and deformation of the bridge piers on both sides of the fault increase, especially when the seismic motion is perpendicular to the fault strike. The seismic resistance of the bridge in the direction perpendicular to the fault strike should be enhanced.
不规则地形和断层对地震反应有显著影响,在1平方公里范围内可能出现显著变化。本研究以天山地区某简支桥址为研究对象,该桥址具有断层和t型相交山谷地形。模拟场地实际地形,建立三维有限元模型,考虑或忽略断层的影响,从不同方向输入25个地震波。分析了场地的地震反应特征、机理及其对简支梁桥的影响。结果表明,不规则地形和断层主要影响场地的短周期(0.1 ~ 0.5 s)谱加速。峰处的短周期谱加速度大约是谷处的两倍。在断层影响方面,平行或垂直于断层走向的地震运动对断层附近的短周期响应分别提高了1.6倍和4.9倍。当地震运动与断层平行时,下盘响应略有增加,而上盘响应变化不明显。当地震运动垂直于断层方向时,下盘和上盘响应均增大,且上盘响应增强较大。这可能与断裂带的动力特性和地震波传播机制有关。考虑断层的影响,断层两侧桥墩的能量耗散、破坏和变形增加,特别是当地震运动垂直于断层走向时。在与断层走向垂直的方向上,应加强桥梁的抗震能力。
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引用次数: 0
Force distribution due to impact of bidisperse granular avalanches against a retention barrier 由于双分散颗粒雪崩对保留屏障的冲击而产生的力分布
IF 8.4 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-03-01 Epub Date: 2026-01-23 DOI: 10.1016/j.enggeo.2026.108585
Francisco Martínez , Tomás Trewhela , Simón Guerra , Bastián Araya
Landslides, rock, debris, and snow avalanches are frequent disasters characterized by their destructive power. Retention structures are therefore essential for mitigating their effects, particularly near urban areas. Although widely studied, the role of grain-size polydispersity remains poorly addressed, even for the simplified case of bidisperse mixtures. In this work, we experimentally investigate the force histories generated by dense, dry, bidisperse granular flows impacting a rigid barrier at different relative concentrations C of the finer fraction. Experiments were conducted in an inclined flume, where a granular mass collided with a downstream rigid wall. A central strip of load cells measured the local force simultaneously under varying conditions. Time series of the force distribution, peak values, and the net force on the barrier were analyzed, showing a strong dependence on particle concentration, with maximum values often occurring near C=20%. This behavior is interpreted as the outcome of size segregation and its inherent asymmetry, which can be incorporated into dynamic force predictions using a Bagnold velocity scaling. Deposit profiles were also characterized, showing significant morphological variability with respect to C. Finally, we propose empirical relations linking maximum loads to deposit properties, providing scaling laws that may be applied to the design and assessment of real retention structures.
山崩、岩石、碎石和雪崩是经常发生的灾害,其特点是破坏力大。因此,保留结构对于减轻其影响至关重要,特别是在城市地区附近。尽管研究广泛,但即使对于双分散混合物的简化情况,粒径多分散性的作用仍然很少得到解决。在这项工作中,我们通过实验研究了致密、干燥、双分散颗粒流在不同相对浓度C下撞击刚性屏障所产生的力历史。实验是在一个倾斜水槽中进行的,其中颗粒体与下游刚性壁碰撞。测压元件的中心条带在不同条件下同时测量局部力。通过对力分布、峰值和作用在屏障上的净力的时间序列分析,发现其与颗粒浓度有很强的依赖性,最大值往往出现在C=20%附近。这种行为被解释为尺寸偏析及其固有的不对称性的结果,可以使用Bagnold速度标度将其纳入动态力预测中。最后,我们提出了将最大载荷与沉积物性质联系起来的经验关系,提供了可应用于实际保留结构的设计和评估的标度定律。
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引用次数: 0
An implicit feature learning approach for automatic digital twinning of three-dimensional subsurface stratigraphy from limited boreholes 有限钻孔三维地下地层自动数字孪生的隐式特征学习方法
IF 8.4 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-03-01 Epub Date: 2026-01-19 DOI: 10.1016/j.enggeo.2026.108568
Zehang Qian, Chao Shi
Digital twinning of underground space is a transformative paradigm for life-cycle risk assessment, management, and operation of geotechnical infrastructure. A prerequisite for this transformation is the automated construction of subsurface geological domains from sparse borehole data with quantified stratigraphic uncertainty. However, most three-dimensional (3D) stratigraphic modelling methods are categorical variable (CaV)-based models and primarily rely on site-specific prior geological knowledge or calibration of geological settings to replicate intricate 3D spatial features. This inevitably involves significant computational burdens and frequent human intervention, which impede real-time data transmission and model updating. In this study, a continuous variable (CoV)-based 3D stratigraphic modelling method leveraging multiple Signed Distance Functions (MSDFs) and Bayesian Compressive Sensing (BCS) is proposed to address these challenges. MSDFs and a spatial partitioning technique are introduced to accelerate the transformation of borehole CaVs into CoVs before leveraging BCS for spatial interpolation of CoVs. Subsequently, random field samples of predicted CoVs are transformed back into the most probable geological domain with quantified uncertainty. The proposed implicit method is applied to both synthesized stratigraphy and real Nan-Chang Urban Rail project. Results demonstrate MSDF-BCS-3D excels in reconstructing 3D stratigraphy, comprising multiple interlayers and folded stratification, with uncertainty quantification in a non-parametric and near real-time manner.
地下空间的数字孪生是岩土基础设施生命周期风险评估、管理和运营的变革范式。实现这种转变的先决条件是利用具有量化地层不确定性的稀疏钻孔数据自动构建地下地质域。然而,大多数三维(3D)地层建模方法是基于分类变量(CaV)的模型,主要依赖于特定地点的先验地质知识或地质环境校准来复制复杂的三维空间特征。这不可避免地带来了巨大的计算负担和频繁的人为干预,阻碍了实时数据传输和模型更新。在这项研究中,提出了一种基于连续变量(CoV)的三维地层建模方法,利用多个签名距离函数(msdf)和贝叶斯压缩感知(BCS)来解决这些挑战。在利用BCS对cov进行空间插值之前,引入了msdf和空间分区技术来加速井眼cav向cov的转换。随后,将预测冠状病毒的随机场样本转换回最可能的地质区域,并量化不确定性。本文提出的隐式方法应用于综合地层和实际的南昌城市轨道工程。结果表明,MSDF-BCS-3D能够以非参数和接近实时的方式进行不确定度量化,在重建包括多夹层和褶皱层的三维地层方面表现出色。
{"title":"An implicit feature learning approach for automatic digital twinning of three-dimensional subsurface stratigraphy from limited boreholes","authors":"Zehang Qian,&nbsp;Chao Shi","doi":"10.1016/j.enggeo.2026.108568","DOIUrl":"10.1016/j.enggeo.2026.108568","url":null,"abstract":"<div><div>Digital twinning of underground space is a transformative paradigm for life-cycle risk assessment, management, and operation of geotechnical infrastructure. A prerequisite for this transformation is the automated construction of subsurface geological domains from sparse borehole data with quantified stratigraphic uncertainty. However, most three-dimensional (3D) stratigraphic modelling methods are categorical variable (CaV)-based models and primarily rely on site-specific prior geological knowledge or calibration of geological settings to replicate intricate 3D spatial features. This inevitably involves significant computational burdens and frequent human intervention, which impede real-time data transmission and model updating. In this study, a continuous variable (CoV)-based 3D stratigraphic modelling method leveraging multiple Signed Distance Functions (MSDFs) and Bayesian Compressive Sensing (BCS) is proposed to address these challenges. MSDFs and a spatial partitioning technique are introduced to accelerate the transformation of borehole CaVs into CoVs before leveraging BCS for spatial interpolation of CoVs. Subsequently, random field samples of predicted CoVs are transformed back into the most probable geological domain with quantified uncertainty. The proposed implicit method is applied to both synthesized stratigraphy and real Nan-Chang Urban Rail project. Results demonstrate MSDF-BCS-3D excels in reconstructing 3D stratigraphy, comprising multiple interlayers and folded stratification, with uncertainty quantification in a non-parametric and near real-time manner.</div></div>","PeriodicalId":11567,"journal":{"name":"Engineering Geology","volume":"363 ","pages":"Article 108568"},"PeriodicalIF":8.4,"publicationDate":"2026-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146001416","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
Comparing geological process-based and engineering data-based approaches to characterizing rock mass heterogeneities: Insights from the Great Glen Fault, Scotland 比较基于地质过程和基于工程数据的方法来表征岩体非均质性:来自苏格兰大格伦断层的见解
IF 8.4 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-02-13 Epub Date: 2025-12-25 DOI: 10.1016/j.enggeo.2025.108529
Namgwon Kim , Zoe K. Shipton , Yannick Kremer , Christopher D. Jack
In rock engineering, understanding variability in rock mass properties is essential for planning engineering mitigations. The differences between engineering and geological approaches to characterizing rock masses can result in varying estimates of mechanical and/or hydraulic properties. This study applies these approaches in parallel: mapping geological domains, fracture traces and Q-values. The aim is to reveal the relationship between variability in geological and engineering parameters at a case study site in the Torcastle block, a fault-bounded sliver within the Great Glen Fault (GGF) that has a complex internal architecture. Distinct geological domains are defined based on lithology (including two generations of dyke intrusion), foliation, faults, and fracture pattern. Fractures are classified into several geometrical categories mainly based on geometrical relationships with local faults and foliations: foliation-parallel, foliation-bounded, foliation-crossing, and ladder-like fractures. Their spatial distribution correlates with the local trend of pre-existing foliations and dykes. For the engineering characterisation we used Q-value mapping, modified for surface conditions, with a moving window approach. Low Q-value zones are spatially heterogeneous but concordant with areas of high fracture density and intersections (topological X and Y nodes), typically associated with: (1) major shear or fault strands and embedded blocks; (2) intruded igneous dykes; (3) areas where faults with different orientations abut; and (4) highly rotated blocks showing re-oriented local foliations. Cross-plots of Q-value against geological fracture and engineering parameters notably reveal that increased fracture connectivity and orientation variability contribute to low Q-values, resulting from abundant foliation-crossing fractures in highly rotated blocks with relatively low fracture density. The geological and engineering variabilities in the Torcastle block highlight the close interplay between the geological deformation history and resultant rock mass conditions. We argue that combining detailed structural geological insight into engineering rock mass characterisation will result in more robust forecasting of engineering properties in rock masses, thereby reducing geotechnical risks.
在岩石工程中,了解岩体性质的可变性对于规划工程缓解措施至关重要。描述岩体的工程和地质方法之间的差异可能导致对力学和/或水力特性的不同估计。这项研究将这些方法并行应用:绘制地质域、裂缝迹和q值。目的是揭示Torcastle地块的地质和工程参数变化之间的关系。Torcastle地块是大格伦断层(GGF)内的一个断层带,具有复杂的内部结构。根据岩性(包括两代岩脉侵入)、片理、断层和断裂模式,定义了不同的地质域。裂缝主要根据与局部断裂和片理的几何关系划分为几类几何类型:片理平行裂缝、片理界裂缝、片理交叉裂缝和梯状裂缝。它们的空间分布与局部先存叶理和脉的走向有关。对于工程特性,我们使用了q值映射,根据表面条件进行了修改,并采用了移动窗口方法。低q值带在空间上不均匀,但与高断裂密度和交叉点(拓扑X和Y节点)区域一致,通常与:(1)主要剪切或断层链和嵌套块体有关;(2)侵入火成岩岩脉;(3)断层方向不同的地区;(4)高度旋转的块体显示重新定向的局部叶理。q值与地质裂缝和工程参数的交叉图明显显示,裂缝连通性和方向可变性的增加导致了低q值,这是由于在高旋转块体中存在大量的片理交叉裂缝,裂缝密度相对较低。Torcastle地块的地质和工程变异性突出了地质变形历史与形成的岩体条件之间的密切相互作用。我们认为,将详细的构造地质见解与工程岩体特征相结合,将导致对岩体工程特性的更可靠预测,从而降低岩土工程风险。
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引用次数: 0
Probabilistic characterization of 3D geotechnical variability by fusion of multi-fidelity measurements using Gaussian Process Regression 基于高斯过程回归的多保真度测量融合三维岩土变异性的概率表征
IF 8.4 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-02-13 Epub Date: 2025-12-30 DOI: 10.1016/j.enggeo.2025.108514
Tengyuan Zhao , Yatong Qi , Zi-Jun Cao , Ling Xu , Dong Wang , Wei Li
Characterization of three-dimensional (3D) subsurface geotechnical properties is essential for the safe design and analysis of geotechnical infrastructures. Due to the complex geological formation process, these properties exhibit strong spatial variability. However, because of time and budget constraints and/or limited technical access, high-fidelity measurements (e.g., standard penetration test, SPT) are typically sparse. Directly interpreting a 3D subsurface profile from such sparse high-fidelity data can lead to significant statistical uncertainty, which may propagate and compromise project safety. Meanwhile, although various low-fidelity measurements (e.g., geophysical data, measurements at similar geotechnical sites) are often available, they are not fully utilized in practice. This study proposes a Gaussian Process Regression (GPR)–based framework to fuse information from multi-fidelity measurements to facilitate the accurate characterization of site-specific 3D variability. The proposed method first trains separate Gaussian process models on each low-fidelity dataset and uses their combined predictions in a linear regression to approximate high-fidelity values. Next, a new GPR is used to fit the residuals to correct remaining discrepancy, producing a final calibrated estimate. The method is demonstrated on a synthetic 3D subsurface case and a real-world case. The results show the proposed method yields much lower prediction errors and uncertainty compared to using only the high-fidelity measurements, with R2 values improved by approximately 50%/443% and MSE reduced by about 36%/72% in the numerical/real-life case. A sensitivity study further verifies the robustness of the proposed framework, showing that the method proposed in this study is capable of accurately and efficiently characterizing 3D geotechnical variability by fusing of multi-fidelity measurements.
三维地下岩土特性的表征对于岩土基础设施的安全设计和分析至关重要。由于复杂的地质形成过程,这些性质表现出强烈的空间变异性。然而,由于时间和预算的限制和/或有限的技术访问,高保真度测量(例如,标准渗透测试,SPT)通常是稀疏的。直接从这种稀疏的高保真数据解释三维地下剖面可能会导致显著的统计不确定性,这可能会传播并危及项目安全。同时,虽然经常有各种低保真度的测量(例如地球物理数据、类似岩土工程地点的测量),但它们在实践中没有得到充分利用。本研究提出了一种基于高斯过程回归(GPR)的框架来融合来自多保真度测量的信息,以促进准确表征特定地点的三维变异性。该方法首先在每个低保真度数据集上训练单独的高斯过程模型,并在线性回归中使用它们的组合预测来近似高保真度值。接下来,使用新的探地雷达来拟合残差以纠正剩余的差异,产生最终的校准估计。该方法在一个合成三维地下案例和一个实际案例中进行了验证。结果表明,与仅使用高保真度测量值相比,该方法的预测误差和不确定性要低得多,在数值/实际情况下,R2值提高了约50%/443%,MSE降低了约36%/72%。灵敏度研究进一步验证了所提出框架的鲁棒性,表明本文提出的方法能够通过融合多保真度测量准确有效地表征三维岩土变化。
{"title":"Probabilistic characterization of 3D geotechnical variability by fusion of multi-fidelity measurements using Gaussian Process Regression","authors":"Tengyuan Zhao ,&nbsp;Yatong Qi ,&nbsp;Zi-Jun Cao ,&nbsp;Ling Xu ,&nbsp;Dong Wang ,&nbsp;Wei Li","doi":"10.1016/j.enggeo.2025.108514","DOIUrl":"10.1016/j.enggeo.2025.108514","url":null,"abstract":"<div><div>Characterization of three-dimensional (3D) subsurface geotechnical properties is essential for the safe design and analysis of geotechnical infrastructures. Due to the complex geological formation process, these properties exhibit strong spatial variability. However, because of time and budget constraints and/or limited technical access, high-fidelity measurements (e.g., standard penetration test, SPT) are typically sparse. Directly interpreting a 3D subsurface profile from such sparse high-fidelity data can lead to significant statistical uncertainty, which may propagate and compromise project safety. Meanwhile, although various low-fidelity measurements (e.g., geophysical data, measurements at similar geotechnical sites) are often available, they are not fully utilized in practice. This study proposes a Gaussian Process Regression (GPR)–based framework to fuse information from multi-fidelity measurements to facilitate the accurate characterization of site-specific 3D variability. The proposed method first trains separate Gaussian process models on each low-fidelity dataset and uses their combined predictions in a linear regression to approximate high-fidelity values. Next, a new GPR is used to fit the residuals to correct remaining discrepancy, producing a final calibrated estimate. The method is demonstrated on a synthetic 3D subsurface case and a real-world case. The results show the proposed method yields much lower prediction errors and uncertainty compared to using only the high-fidelity measurements, with <span><math><msup><mrow><mi>R</mi></mrow><mrow><mn>2</mn></mrow></msup></math></span> values improved by approximately 50%/443% and MSE reduced by about 36%/72% in the numerical/real-life case. A sensitivity study further verifies the robustness of the proposed framework, showing that the method proposed in this study is capable of accurately and efficiently characterizing 3D geotechnical variability by fusing of multi-fidelity measurements.</div></div>","PeriodicalId":11567,"journal":{"name":"Engineering Geology","volume":"362 ","pages":"Article 108514"},"PeriodicalIF":8.4,"publicationDate":"2026-02-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145881857","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
Seismic site characterization using satellite-derived terrain morphometry and geological data: A machine learning approach for predominant frequency prediction 利用卫星衍生的地形形态测量学和地质数据进行地震现场表征:一种用于主要频率预测的机器学习方法
IF 8.4 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-02-13 Epub Date: 2026-01-02 DOI: 10.1016/j.enggeo.2025.108541
Harish Thakur, P. Anbazhagan
<div><div>Predominant frequency (<em>fo</em>) characterization across large seismically active regions remains challenging due to limited field measurements and cost constraints. Existing <em>fo</em> mapping approaches rely exclusively on spatial interpolation methods (kriging, inverse distance weighting, natural neighbor) that redistribute measured values without incorporating terrain morphometry, geological context, or subsurface parameters as predictors. This study develops a DEM-based machine learning methodology for regional-scale <em>fo</em> prediction in the Himalayan region and Indo-Gangetic Plains, addressing critical data scarcity in earthquake-prone developing countries. We compiled 4400 <em>fo</em> measurements from 26 published HVSR studies using systematic georeferencing procedures to ensure spatial consistency. The methodology employs a two-stage regression kriging framework: (1) stacked ensemble machine learning models trained on 20 predictor variables using GLO-30 DEM morphometric parameters (elevation, slope, curvature indices), geological classifications, and bedrock depth information to capture nonlinear terrain-frequency relationships; and (2) ordinary kriging of model residuals to account for spatial correlation patterns. Cross-validation partitioning ensures unbiased residuals, while Bayesian optimization determines optimal hyperparameters for base model selection. Feature importance analysis reveals that valley bottom identification (MRVBF), geological formation characteristics, and bedrock depth provide primary predictive capability (Shapley values ∼0.15–0.18), demonstrating that terrain morphometry and subsurface parameters effectively control <em>fo</em> variation at regional scales. The stacked ensemble achieves R<sup>2</sup> = 0.516 and RMSE = 0.634 log units, with variogram analysis revealing spatial correlation extending 7.3 km and structured variance accounting for 52 % of model residuals. High-resolution <em>fo</em> maps (50 m grid) generated for Delhi, Kathmandu, and Dhaka differentiate site response zones: low frequencies (<1.0 Hz) in deep sedimentary basins versus high frequencies (>3.0 Hz) in bedrock-controlled areas.</div><div>This work represents the first regional-scale application of DEM-derived terrain morphometry for direct <em>fo</em> prediction, utilizing a much larger compiled dataset for this purpose than previous basin-scale studies. Unlike previous studies that employed purely interpolation techniques without predictive parameters, this hybrid framework integrates physical predictors (terrain morphometry, geology, bedrock depth) with spatial modelling to produce more robust <em>fo</em> maps. Results demonstrate that incorporating satellite-derived morphometric and geological parameters—readily available globally—significantly enhances prediction reliability beyond interpolation-only approaches. This cost-effective methodology enables preliminary seismic hazard assessment in data-sparse mounta
由于有限的现场测量和成本限制,大型地震活跃区域的主要频率(fo)表征仍然具有挑战性。现有的测绘方法完全依赖于空间插值方法(克里格法、逆距离加权法、自然邻域法),这些方法重新分配测量值,而没有将地形形态、地质背景或地下参数作为预测因素。本研究开发了一种基于dem的机器学习方法,用于喜马拉雅地区和印度恒河平原的区域尺度预测,解决了地震多发发展中国家的关键数据短缺问题。我们使用系统的地理参考程序,从26项已发表的HVSR研究中收集了4400个测量值,以确保空间一致性。该方法采用两阶段回归克里格框架:(1)利用gloo -30 DEM形态参数(高程、坡度、曲率指数)、地质分类和基岩深度信息,训练20个预测变量的堆叠集成机器学习模型,捕捉非线性地形-频率关系;(2)对模型残差进行普通克里格,以解释空间相关模式。交叉验证分区确保残差无偏,贝叶斯优化确定最优超参数,用于基础模型选择。特征重要性分析表明,谷底识别(MRVBF)、地质构造特征和基岩深度提供了主要的预测能力(Shapley值~0.15 ~ 0.18),表明地形形态和地下参数在区域尺度上有效控制了变化。叠加集合的R2 = 0.516,RMSE = 0.634 log units,方差分析显示空间相关延伸7.3 km,结构方差占模型残差的52. %。为德里、加德满都和达卡制作的高分辨率地图(50 m网格)区分了场地响应区域:深沉积盆地的低频(<1.0 Hz)与基岩控制区的高频(>3.0 Hz)。
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引用次数: 0
Multiscale damage mechanisms of reservoir bank sandstone under prolonged immersion in pumped-storage hydropower projects: From microscale processes to macroscopic fracture 抽水蓄能水电站长时间浸没下库岸砂岩多尺度损伤机理:从微观过程到宏观断裂
IF 8.4 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-02-13 Epub Date: 2025-12-28 DOI: 10.1016/j.enggeo.2025.108532
Hexing Zhang , Qiang Xie , Jiwei Jia , Kunpeng Lu , Fubo Yang , Weichen Sun
The long-term stability of pumped-storage reservoir banks is strongly governed by damage evolution induced by prolonged water immersion. In this study, reservoir bank sandstone from the Laowuji pumped-storage site in Guizhou, China, was examined using computerized tomography (CT), nuclear magnetic resonance (NMR), scanning electron microscopy (SEM), and molecular dynamics (MD) simulations to systematically characterize damage evolution from the mesoscopic to microscopic scales and to elucidate cascade effects across multiple scales. After 360 days of immersion, the mineral cement interface dissolution area increased from 12.51 μm2 to 139.83 μm2. Porosity rose from 9.45 % to 10.95 %, the small-pore fraction decreased to 80.11 %, and medium-to-large pores increased significantly, enhancing pore connectivity and heterogeneity. Concurrently, the P-wave velocity decreased cumulatively by 45.99 %, indicating a high sensitivity to microstructural degradation. MD simulations revealed that mineral interfaces weaken chemical bonding while providing lubricated and dilatable pathways, thereby facilitating early microcrack initiation and rapid propagation, ultimately compromising reservoir bank integrity and reducing seepage safety margins. The three-dimensional fracture spatial inhomogeneity index (FSI3D) increased by more than an order of magnitude over 360 days, capturing the transition of fracture patterns from relatively simple through-going cracks to a complex, interconnected fracture network. On this basis, a zoned management strategy consisting of “shallow-sealing and deep-infiltration control” and a multi-parameter dynamic early warning system is proposed. These findings provide theoretical support and engineering guidance for long-term stability control of reservoir bank sandstone in pumped-storage systems.
抽水蓄能库岸的长期稳定性受长期浸水损伤演化的强烈影响。本研究利用计算机断层扫描(CT)、核磁共振(NMR)、扫描电镜(SEM)和分子动力学(MD)模拟技术,对贵州老五集抽水蓄能区储层砂岩进行了研究,系统地表征了从细观到微观尺度的损伤演化过程,并阐明了跨多个尺度的级联效应。浸泡360 d后,矿物水泥界面溶解面积由12.51 μm2增加到139.83 μm2。孔隙度由9.45%上升至10.95%,小孔隙率下降至80.11%,中大型孔隙显著增加,孔隙连通性和非均质性增强。同时,纵波速度累计下降45.99%,表明其对微观结构降解具有较高的敏感性。MD模拟显示,矿物界面在提供润滑和可膨胀通道的同时削弱了化学键,从而促进了早期微裂缝的形成和快速扩展,最终损害了储层的完整性,降低了渗流安全裕度。三维裂缝空间不均匀性指数(FSI3D)在360天内增加了一个多数量级,捕捉到了裂缝模式从相对简单的贯通裂缝到复杂、相互连接的裂缝网络的转变。在此基础上,提出了“浅封深控”分区治理策略和多参数动态预警系统。研究结果为抽水蓄能系统库岸砂岩的长期稳定控制提供了理论支持和工程指导。
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引用次数: 0
Forecasting CO2 injection-induced fault reactivation: A hybrid approach and its application to the Illinois Basin–Decatur Project 预测二氧化碳注入引起的断层再活化:一种混合方法及其在伊利诺斯盆地-迪凯特项目中的应用
IF 8.4 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2026-02-13 Epub Date: 2026-01-02 DOI: 10.1016/j.enggeo.2025.108536
Yao Zhang , Qi Li , Jianhua Zhang , Haodong Cui , Yiyan Zhong , Yongsheng Tan , Meng Jing , Xiaying Li
Geological CO2 storage (GCS) is an effective method for reducing carbon emissions. However, as more such projects are deployed in the future, the associated risks of injection-induced fault reactivation require comprehensive assessment to ensure long-term and effective CO2 storage. This study presents an integrated assessment of the Illinois Basin–Decatur Project (IBDP) through a hybrid approach combining physics-based modeling and probabilistic forecasting. A coupled CO2-geomechanical model is developed to simulate CO2 injection at CCS1 well. The fault reactivation risks have been systematically evaluated by analyzing near-well and far-field fault slip tendency indices, spatiotemporal evolution of Coulomb failure stress (CFS), seismogenic index (Σ), and magnitude probability distributions. Results demonstrate that while permeability-controlled pore pressure diffusion dominates fault reactivation for both near-well and far-well faults, poroelastic stresses may induce localized fault slip and provide stabilization during shut-in periods. The reactivation state is significantly controlled by fault geometry. Higher initial injection rates substantially facilitate fault instability compared to constant or gradually increasing injection schemes. Based on field data, the applicability of the seismogenic index for carbon storage sites has been validated. The low seismogenic index (Σ ≈ −4) for this site confirms limited seismic potential, and the probability of seismic magnitude below 2.27 exceeds 50%. Probabilistic modeling further indicates that a controlled injection rate ramp-up preferentially induces seismicity with low magnitudes. The proposed hybrid forecasting approach enables a more comprehensive evaluation of fault reactivation risks at carbon storage sites.
地质CO2封存是减少碳排放的有效方法。然而,随着未来更多此类项目的部署,需要对注入引起的断层重新激活的相关风险进行全面评估,以确保长期有效的二氧化碳储存。本研究通过结合物理建模和概率预测的混合方法,对伊利诺斯盆地-迪凯特项目(IBDP)进行了综合评估。建立了模拟CCS1井CO2注入过程的CO2-地质力学耦合模型。通过分析近井和远场断层滑动趋势指数、库仑破坏应力(CFS)时空演化、发震指数(Σ)和震级概率分布,系统评价了断层再激活风险。结果表明,虽然渗透率控制的孔隙压力扩散主导着近井和远井断层的恢复,但孔隙弹性应力可能会导致局部断层滑动,并在关井期间提供稳定。再激活状态在很大程度上受断层几何形状的控制。与恒定或逐渐增加的注入方案相比,较高的初始注入速率大大促进了断层的不稳定性。根据实测资料,验证了孕震指数在碳库选址上的适用性。本区孕震指数(Σ≈−4)较低,地震潜力有限,发生2.27级以下地震的概率超过50%。概率模型进一步表明,控制注入速度的增加优先诱发低震级的地震活动。提出的混合预测方法能够更全面地评估碳储存地点的断层再激活风险。
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引用次数: 0
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Engineering Geology
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