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Tunnel geological forward-prospecting based on an optimized beamforming seismic method 基于优化波束形成地震方法的隧道地质正测
IF 2.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-27 DOI: 10.1016/j.jappgeo.2026.106135
Lei Chen , Zhifei Gong , Long Chen , Chuanwu Wang
Currently, more and more tunnels are being built and designed in urban and mountain areas. To ensure the safe construction of a tunnel, the seismic method is widely applied to estimate the geological conditions ahead of the tunnel face. However, due to the complex environment in the tunnel (narrow observation aperture, strong noise, etc.), it is hard to extract the effective reflected waves with poor energy for imaging geology, especially for the target far away from the tunnel face. In this paper, for the demand of geological detection in the Water Diversion Project from the Songhua River, the tunnel seismic ahead-prospecting was improved by using the adaptive beamforming approach, supporting the extraction of reflected waves with poor energy. As the core of beamforming, the delay time is an important parameter to control the reliability of stacking, especially for the various strata. The relevance analysis-based adaptive beamforming is proposed for the delay-time calculation to obtain the correlation coefficient. Among them, the reflection group composed of several reflections is used to obtain an accurate delay time first. Then, the seismic data are reconstructed and overlapped to improve the SNR based on the obtained delay time. Numerical simulation denotes that the energy of reflected waves can be enhanced significantly. Finally, the improved seismic ahead-prospecting was applied in the Water Diversion Project from the Songhua River; the method successfully predicted the fractured zones ahead of the tunnel face and guaranteed tunnel construction safety.
目前,城市和山区正在建设和设计越来越多的隧道。为了保证隧道的安全施工,地震法被广泛应用于隧道工作面前方地质条件的估算。然而,由于巷道内环境复杂(观测孔径窄、噪声强等),成像地质很难提取出能量较差的有效反射波,特别是对于距离巷道工作面较远的目标。本文针对松花江引水工程地质探测的需要,采用自适应波束形成方法对隧道地震超前勘探进行改进,支持能量较差的反射波提取。延迟时间作为波束形成的核心,是控制波束形成可靠性的重要参数,特别是对于不同的层。提出了基于相关性分析的自适应波束形成算法,计算时延,得到相关系数。其中,利用由多个反射组成的反射组,首先获得准确的延迟时间。然后,根据得到的延迟时间对地震数据进行重构和叠加,提高信噪比。数值模拟结果表明,反射波的能量明显增强。最后,将改进的地震超前勘探技术应用于松花江引水工程;该方法成功地预测了巷道工作面前方的裂隙区,保证了巷道的安全施工。
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引用次数: 0
Frequency-domain fast slant stacking method based on non-uniform fast Fourier transform for dispersion imaging from dense array ambient seismic noise 基于非均匀快速傅立叶变换的频域快速倾斜叠加方法在密集阵列环境地震噪声中色散成像
IF 2.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-26 DOI: 10.1016/j.jappgeo.2026.106136
Chaoqiang Xi , Hao Zhang , Ya Liu , Ling Ning
Ambient-noise interferometry from dense seismic arrays provides rich surface-wave information for dispersion imaging and multiscale shear-wave velocity Vs inversion, but it also produces very large virtual shot gathers that make conventional frequency-domain slant stacking computationally expensive. We present a frequency-domain fast slant-stacking method based on the non-uniform fast Fourier transform NUFFT for dispersion imaging from dense-array ambient seismic noise. Synthetic and field tests show that the NUFFT-based formulation yields same dispersion spectra and picked dispersion curves that are identical to those obtained by conventional direct summation, with an RMS misfit of 0. Benchmarks on three field datasets demonstrate substantial runtime reductions, requiring 1.44–2.23 s and 0.33–0.49 s with parallelization for NUFFT, whereas Numba, PyTorch, and NumPy implementations typically require tens to hundreds of seconds under the same settings, achieving speedups of up to about 60 times relative to the fastest conventional baseline. Comparisons with the widely used CC-FJpy package show consistent dispersion trends while requiring significantly less computation time.
密集地震阵列的环境噪声干涉测量为色散成像和多尺度横波速度v反演提供了丰富的表面波信息,但它也产生了非常大的虚拟射击集,这使得传统的频域倾斜叠加计算成本很高。提出了一种基于非均匀快速傅里叶变换(NUFFT)的频域快速倾斜叠加方法,用于密集阵列环境地震噪声的色散成像。综合和现场试验表明,基于nufft的公式得到的色散光谱和拾取色散曲线与传统直接求和方法得到的色散光谱和拾取色散曲线相同,其RMS失拟值为0。在三个字段数据集上的基准测试显示了大量的运行时间减少,对于NUFFT并行化需要1.44-2.23秒和0.33-0.49秒,而Numba, PyTorch和NumPy实现在相同的设置下通常需要几十到几百秒,相对于最快的传统基准,实现了高达60倍的速度。与广泛使用的CC-FJpy包的比较显示出一致的色散趋势,同时所需的计算时间大大减少。
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引用次数: 0
A new method for reconstructing surface wavefields via cross-correlation of ambient noise from DAS and geophone records 一种利用DAS和检波器记录的环境噪声相互关重建表面波场的新方法
IF 2.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-25 DOI: 10.1016/j.jappgeo.2026.106121
Wenda Sun, Jing Zheng, Suping Peng
Distributed Acoustic Sensing (DAS) is an emerging seismic acquisition technology that offers high spatial sampling density, continuous recording capability, and flexible deployment. These characteristics make it particularly suitable for shallow subsurface exploration in urban environments. However, DAS exhibits limited sensitivity to weak seismic signals and typically captures only the axial component of ground motion. In contrast, conventional geophones offer high signal fidelity and multi-component recordings, but are limited by lower spatial resolution, greater deployment costs, and reduced adaptability in complex terrain conditions. To enhance surface wavefields reconstructed from DAS ambient noise, we propose a method that integrates the complementary strengths of DAS and conventional geophones. The method employs a linear array configuration, where the vertical component of a geophone deployed at the front of the array serves as a virtual source, and the DAS system is deployed along the subsequent positions of the array to serve as receivers. These recordings are combined to form a hybrid ambient noise dataset, which is processed in the frequency domain through normalization and cross-correlation. The acausal parts of the cross-correlation functions (CCFs) are taken as virtual shot gathers (VSGs). This method not only preserves the high spatial resolution of DAS but also incorporates the high signal fidelity of geophones, thereby significantly enhancing the surface wavefields in passive surface wave imaging. By evaluating the signal-to-noise ratio (SNR) of randomly selected traces from the CCFs obtained under various ambient noise stacking durations, the proposed method achieves average SNR improvements of 1.54 dB and 1.00 dB compared to the case where both the virtual source and receivers are derived from DAS data. Under the optimal stacking duration, the extracted dispersion energy shows clearer and more concentrated patterns, with an extended frequency range.
分布式声传感(DAS)是一种新兴的地震采集技术,具有高空间采样密度、连续记录能力和灵活部署的特点。这些特点使其特别适合于城市环境中的浅层地下勘探。然而,DAS对弱地震信号的敏感性有限,通常只捕获地面运动的轴向分量。相比之下,传统检波器可以提供高信号保真度和多分量记录,但受到空间分辨率较低、部署成本较高以及在复杂地形条件下适应性降低的限制。为了增强从DAS环境噪声中重建的表面波场,我们提出了一种融合DAS和传统检波器互补优势的方法。该方法采用线性阵列配置,其中部署在阵列前端的检波器的垂直组件作为虚拟源,DAS系统沿着阵列的后续位置部署作为接收器。将这些记录组合在一起形成混合环境噪声数据集,并通过归一化和相互关联在频域进行处理。将相互关联函数(CCFs)的非因果部分作为虚拟射击集(VSGs)。该方法既保留了DAS的高空间分辨率,又结合了检波器的高信号保真度,从而显著增强了被动表面波成像中的表面波场。通过评估在不同环境噪声叠加时间下随机选择ccf走线的信噪比(SNR),与从DAS数据获取虚拟源和接收源的情况相比,该方法的平均信噪比分别提高了1.54 dB和1.00 dB。在最优叠加时间下,提取的色散能量模式更清晰、更集中,频率范围更广。
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引用次数: 0
Petrophysics and mass balance integration for alteration detection in orogenic gold exploration 造山带金矿蚀变探测中的岩石物理与物质平衡集成
IF 2.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-24 DOI: 10.1016/j.jappgeo.2026.106114
Yasaman Nemati , J. Christian Dupuis , Benoit Quesnel , Bernard Giroux , Richard Smith , Georges Beaudoin
This study explores the integration of petrophysical and geochemical data to characterize hydrothermal alteration in mafic and ultramafic rocks, with a focus on the Augmitto-Bouzan orogenic gold deposit in the Abitibi Greenstone Belt. Employing established mass balance techniques using zirconium (Zr) as the immobile reference element, we quantified element mobility during alteration processes. Due to the absence of original komatiite protolith data, we compiled geochemical compositions from published sources across the Superior Province and applied bootstrapping to derive a representative baseline for mass balance calculations, which were then correlated with petrophysical logs from multiple boreholes to identify modification signatures. The analysis reveals robust correlations: potassium enrichment aligns with elevated gamma-ray responses, carbonate alteration is marked by increased CaO and reduced density, and magnetic susceptibility decreases correspond to Fe-Mg depletion and sulfide mineralization. These observations demonstrate systematic links between geochemical changes and petrophysical data, showing that petrophysical logs can serve as high-resolution, cost-effective proxies for alteration mapping, offering a scalable framework for exploration targeting in orogenic gold systems hosted in ultramafic rocks. The methodology bridges traditional geochemistry and in-situ measurements of physical properties, improving subsurface characterization and supporting the development of data-driven exploration tools while advancing our understanding of processes associated with gold mineralization.
本文以阿比提比绿岩带的Augmitto-Bouzan造山带金矿为研究对象,结合岩石物理和地球化学资料,探讨了基性岩和超基性岩热液蚀变特征。采用已建立的质量平衡技术,以锆(Zr)作为固定参考元素,我们量化了蚀变过程中的元素迁移率。由于缺乏原始的科马地岩原岩数据,我们从苏必利尔省的公开资料中收集了地球化学成分,并应用bootstrapping获得了一个具有代表性的质量平衡计算基线,然后将其与多个井眼的岩石物理测井相关联,以识别变质特征。分析表明,钾的富集与伽马射线响应的升高有关,碳酸盐蚀变的特征是CaO的增加和密度的降低,磁化率的降低与Fe-Mg的耗尽和硫化物矿化有关。这些观测结果证明了地球化学变化与岩石物理数据之间的系统联系,表明岩石物理测井可以作为高分辨率、高成本效益的蚀变填图代理,为超基性岩石中的造山带金系统的勘探目标提供了可扩展的框架。该方法将传统的地球化学和物理性质的原位测量相结合,改善了地下特征,并支持数据驱动勘探工具的开发,同时提高了我们对金矿化过程的理解。
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引用次数: 0
A FFT-based calculation method for third-order gradient tensor of gravity potential from vertical gravity gradient data 基于fft的重力势三阶梯度张量的垂直重力梯度计算方法
IF 2.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-24 DOI: 10.1016/j.jappgeo.2026.106125
Feng Qiu , Zhengwang Hu , Jinsong Du , Songtao Hu
With the same distribution of the observation points, the third-order gravitational gradient tensor is capable of acquiring more comprehensive information pertaining to the geophysical field and its corresponding sources, demonstrates superior sensitivity to changes in the burial depth of field sources, and features enhanced horizontal resolving power. But the current instrumental measurement technology has not yet reached the level of measuring the third-order gradient tensor of gravitational potential directly in the field. In this paper, we provide an alternative technique for calculating the complete third-order gradient tensor of gravitational potential from the pre-existing vertical gravity gradient data by using the fast Fourier transform (FFT). In order to verify the correctness of the transform calculation method, the complete third-order gradient tensor components of gravitational potential are computed from the synthetic vertical gravity gradient data by two different three-dimensional (3-D) theoretical density models. Comparing the FFT-based calculation results with theoretically forward calculated data shows that the root-mean-square (RMS) error for each component, is at most 1.5 pMKS (1 pMKS = 10−12 m−1·s−2). In addition, as a real example, based on the practically measured vertical gravity gradient data over the Vinton salt dome area, the complete third-order gradient tensor is obtained by using the FFT-based calculation method and the results illustrate a better resolution and a richer information for understanding the underground density structures. Then, the determined tensor data is quantitatively interpreted by using the DEXP (i.e., Depth from EXtreme Point) imaging technique. The imaging results show that, the depth and boundaries of anomalous density sources by the DEXP imaging method are consistent with the previous research results, and the third-order gradient tensor-based imaging has a weaker influence of trend component than the traditional gravity and second-order gravity gradient tensor. Both synthetic examples and practical application suggest that our proposed method is not only valid and reliable but also has a high computational efficiency due to the FFT algorithm, and meanwhile the calculated third-order gradient tensor also provides a novel way for exploring the geological structures, ore bodies and hydrocarbon reservoirs, etc.
在观测点分布相同的情况下,三阶重力梯度张量能够获得更全面的地球物理场及其源信息,对场源埋深变化的敏感性更强,水平分辨率更高。但目前的仪器测量技术还没有达到直接在现场测量引力势的三阶梯度张量的水平。本文提出了一种利用快速傅立叶变换(FFT)从已有的垂直重力梯度数据计算重力势完全三阶梯度张量的方法。为了验证变换计算方法的正确性,利用两种不同的三维理论密度模型,利用合成的垂直重力梯度数据计算重力势的完整三阶梯度张量分量。将基于fft的计算结果与理论正演计算数据进行比较,各分量的均方根误差(RMS)不超过1.5 pMKS (1 pMKS = 10−12 m−1·s−2)。此外,以Vinton盐丘地区实测垂直重力梯度数据为例,采用基于fft的计算方法获得了完整的三阶梯度张量,结果表明,该方法对地下密度结构的理解具有更好的分辨率和更丰富的信息。然后,使用DEXP(即极限点深度)成像技术对确定的张量数据进行定量解释。成像结果表明,DEXP成像方法的异常密度源深度和边界与前人的研究结果一致,且基于三阶梯度张量的成像对趋势分量的影响弱于传统重力和二阶重力梯度张量。综合算例和实际应用表明,该方法不仅有效可靠,而且由于采用FFT算法,计算效率高,同时计算得到的三阶梯度张量也为地质构造、矿体、油气藏等勘探提供了新的途径。
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引用次数: 0
Automatic identification and location of underground defects in urban roads via ground penetrating radar and deep learning approaches 基于探地雷达和深度学习方法的城市道路地下缺陷自动识别与定位
IF 2.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-23 DOI: 10.1016/j.jappgeo.2026.106128
Jiwei Zhang , Xiaoyi Ji , Mingzhe Zhao , Yaxiu Li , Haifeng Wang , Ming Zhong , Shuai Li
Underground defects in urban roads endanger driving safety and hinder road usability. These defects are primarily identified using technologies such as ground penetrating radar. The current intelligent algorithms used for identifying underground road defects rely heavily on large datasets of on-site road images. However, the automatic detection of defects remains challenging due to small datasets, limited image availability, and inconsistent on-field image quality. This paper proposes a novel approach to address these challenges through a model based on actual road conditions and forward simulations of road defect images. To improve the quality of both real and simulated field images, we apply a joint denoising method that combines wavelet transform, the K-SVD algorithm, and bilateral filtering. This denoising process enhances both real and simulated field images and expands the image dataset, transforming it into a mixed database, and strengthens the distinctive features of each defect, facilitating more accurate algorithm-based detection. In the first and second stages of the study, we conduct a comparative analysis of various deep learning-based object detection models. We then propose a deep learning model, optimized with the joint denoising model, that is best suited for practical road evaluation projects. The model was trained and validated across 100 km of high-quality field measurement data collected from various districts and counties in Beijing. Experimental results showed that the model can achieve a prediction accuracy of 82.3% for Looseness, 92.6% for Cavities, and 50.9% for Voids, with an overall Mean Average Precision of 75.3%. These results demonstrate that the method proposed in this study can enhance the detection accuracy for various subsurface defects.
城市道路地下缺陷危害行车安全,阻碍道路可用性。这些缺陷主要是通过诸如探地雷达之类的技术来识别的。目前用于地下道路缺陷识别的智能算法严重依赖于现场道路图像的大型数据集。然而,由于数据集小、图像可用性有限以及现场图像质量不一致,缺陷的自动检测仍然具有挑战性。本文提出了一种新的方法,通过基于实际路况的模型和道路缺陷图像的前向模拟来解决这些挑战。为了提高真实和模拟现场图像的质量,我们采用了一种结合小波变换、K-SVD算法和双边滤波的联合去噪方法。这种去噪过程同时增强了真实和模拟的现场图像,扩展了图像数据集,将其转化为混合数据库,并加强了每个缺陷的鲜明特征,便于更准确的算法检测。在研究的第一阶段和第二阶段,我们对各种基于深度学习的目标检测模型进行了比较分析。然后,我们提出了一个深度学习模型,并对联合去噪模型进行了优化,该模型最适合实际的道路评估项目。该模型在北京市各区县采集的100公里高质量野外测量数据中进行了训练和验证。实验结果表明,该模型对松度、空腔和空洞的预测精度分别为82.3%、92.6%和50.9%,总体平均精度为75.3%。结果表明,本文提出的方法可以提高对各种亚表面缺陷的检测精度。
{"title":"Automatic identification and location of underground defects in urban roads via ground penetrating radar and deep learning approaches","authors":"Jiwei Zhang ,&nbsp;Xiaoyi Ji ,&nbsp;Mingzhe Zhao ,&nbsp;Yaxiu Li ,&nbsp;Haifeng Wang ,&nbsp;Ming Zhong ,&nbsp;Shuai Li","doi":"10.1016/j.jappgeo.2026.106128","DOIUrl":"10.1016/j.jappgeo.2026.106128","url":null,"abstract":"<div><div>Underground defects in urban roads endanger driving safety and hinder road usability. These defects are primarily identified using technologies such as ground penetrating radar. The current intelligent algorithms used for identifying underground road defects rely heavily on large datasets of on-site road images. However, the automatic detection of defects remains challenging due to small datasets, limited image availability, and inconsistent on-field image quality. This paper proposes a novel approach to address these challenges through a model based on actual road conditions and forward simulations of road defect images. To improve the quality of both real and simulated field images, we apply a joint denoising method that combines wavelet transform, the <em>K-SVD</em> algorithm, and bilateral filtering. This denoising process enhances both real and simulated field images and expands the image dataset, transforming it into a mixed database, and strengthens the distinctive features of each defect, facilitating more accurate algorithm-based detection. In the first and second stages of the study, we conduct a comparative analysis of various deep learning-based object detection models. We then propose a deep learning model, optimized with the joint denoising model, that is best suited for practical road evaluation projects. The model was trained and validated across 100 km of high-quality field measurement data collected from various districts and counties in Beijing. Experimental results showed that the model can achieve a prediction accuracy of 82.3% for Looseness, 92.6% for Cavities, and 50.9% for Voids, with an overall Mean Average Precision of 75.3%. These results demonstrate that the method proposed in this study can enhance the detection accuracy for various subsurface defects.</div></div>","PeriodicalId":54882,"journal":{"name":"Journal of Applied Geophysics","volume":"247 ","pages":"Article 106128"},"PeriodicalIF":2.1,"publicationDate":"2026-01-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146071109","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Target-oriented full waveform inversion based on optimal transport theory 基于最优输运理论的目标定向全波形反演
IF 2.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-22 DOI: 10.1016/j.jappgeo.2026.106120
Tianjing Shen , Xiaochun Chen , Kai Chen , Yukai Wo , Xuri Huang
Target-oriented full waveform inversion (TOFWI) provides an efficient strategy for high-resolution imaging in local regions of interest, but its effectiveness is often limited by two main challenges: the need for redatuming of the acquisition system and the sensitivity of conventional L2-norm-based TOFWI (L2-TOFWI) to initial models and data quality. In this study, we propose an optimal transport (OT)-based TOFWI framework to overcome these limitations. First, we apply the Marchenko redatuming method to retrieve virtual reflection responses that isolate the target-zone wavefield. Then, we incorporate OT-based misfit functions, including graph-space OT (GSOT) and Kantorovich-relaxed OT (KROT), to enhance the convexity of the inversion landscape and improve robustness against noise and velocity-model inaccuracies. KROT introduces entropy regularization via the Sinkhorn algorithm, leading to smooth transport plans and improved numerical stability, whereas GSOT relies on a discrete assignment formulation that yields sparse transport plans and higher sensitivity to local waveform variations. Numerical experiments demonstrate that the proposed OT-TOFWI framework delivers more accurate and stable reconstructions than conventional L2-TOFWI, particularly under conditions of significant initial-model errors and low signal-to-noise ratio. Furthermore, comparisons with global full waveform inversion highlight that OT-TOFWI achieves better resolution in deeper structures with lower computational cost. These results confirm that integrating Marchenko redatuming with OT-based misfit functions provides a promising pathway for reliable target-oriented seismic imaging in complex geological settings.
面向目标的全波形反演(TOFWI)为局部感兴趣区域的高分辨率成像提供了一种有效的策略,但其有效性通常受到两个主要挑战的限制:需要重新恢复采集系统以及传统的基于l2规范的TOFWI (L2-TOFWI)对初始模型和数据质量的敏感性。在这项研究中,我们提出了一个基于最佳传输(OT)的TOFWI框架来克服这些限制。首先,我们应用Marchenko重数据方法来检索分离目标区波场的虚拟反射响应。然后,我们结合了基于逆拟合函数的逆拟合函数,包括图空间逆拟合函数(GSOT)和kantorovich -relax逆拟合函数(KROT),以增强反演景观的凹凸性,并提高对噪声和速度模型不准确性的鲁棒性。KROT通过Sinkhorn算法引入熵正则化,导致平滑的传输计划和改进的数值稳定性,而GSOT依赖于离散分配公式,产生稀疏的传输计划和对局部波形变化的更高灵敏度。数值实验表明,与传统的L2-TOFWI相比,本文提出的OT-TOFWI框架提供了更精确和稳定的重建,特别是在初始模型误差较大和信噪比较低的情况下。此外,与全局全波形反演的比较表明,OT-TOFWI在更深的结构中获得了更好的分辨率,且计算成本更低。这些结果证实,将Marchenko重建与基于ot的失配函数相结合,为复杂地质环境下可靠的目标导向地震成像提供了一条有希望的途径。
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引用次数: 0
Application of geophysical methods in the assessment of conservation conditions in a small earth dam 地球物理方法在小土坝保护条件评价中的应用
IF 2.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-22 DOI: 10.1016/j.jappgeo.2026.106127
Luiz Filipe Caríssimo Soares , Eduardo Antonio Gomes Marques , Cibele Cláuver
Assessing safety and conservation conditions in earth dams involves the investigation of phenomena that compromise their stability. In this regard, geophysical methods can be combined with direct investigations to enhance the efficiency of geotechnical studies, allowing faster data acquisition at relatively low cost. Therefore, this study aims to evaluate the conservation conditions of a small earth dam through the integrated interpretation of results obtained using the geophysical methods of Electrical Resistivity and Ground-Penetrating Radar, coupled with the results of grain size analyses of samples collected in situ. The results confirmed the efficiency of the proposed methodology, enabling assessment of features associated with the prolonged biological activity and surface water runoff. Among the identified geotechnical properties, a zone affected by the intense presence of ant nests and tree roots was detected, highlighting the need for corrective actions to maintain the structural integrity of the embankment.
评估土坝的安全和保护条件涉及对危及土坝稳定性的现象的调查。在这方面,地球物理方法可以与直接调查相结合,以提高岩土技术研究的效率,从而以相对较低的成本更快地获取数据。因此,本研究旨在通过电阻率和探地雷达地球物理方法综合解释结果,结合现场采集样品的粒度分析结果,对小土坝的保护条件进行评价。结果证实了所提出方法的有效性,能够评估与长期生物活动和地表水径流相关的特征。在已确定的岩土特性中,检测到受蚁巢和树根强烈存在影响的区域,强调需要采取纠正措施以保持路堤的结构完整性。
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引用次数: 0
A proposed brittleness index model based on shale multicomponent digital cores 基于页岩多组分数字岩心的脆性指数模型
IF 2.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-21 DOI: 10.1016/j.jappgeo.2026.106110
Haitao Wang , Fuqiang Lai , Min Wang , Zhaohui Huang , Zhangxiong Zhu , Yuejiao Liu , Xianfeng Tan , Huaimin Dong , Ye Yang
The exploitation of organic shale reservoirs depends on the brittleness affected by lamination, fracture, porosity, and minerals. However, the existing brittleness index for petroleum only considers mineral types and requires comprehensive characterization. Therefore, a multicomponent model was constructed by inserting a planar fracture, planar lamination, and gas saturation model into a multimineral model using the Markov-chain Monte Carlo method. The elastic parameters were calculated using a finite element method, and the sensitivity of the parameters to the brittleness index defined by the Young's modulus and Poisson's ratio was determined using Morris screening and analytical hierarchy process methods. The investigation indicated that the development of brittle minerals and fracture porosity increased the brittleness index and, Young's modulus and decreased the Poisson's ratio, whereas the fracture width decreased the brittleness index, Gas saturation increases the brittleness index. A new comprehensive brittleness index was proposed in which the sensitivity decreased from the dip angle, azimuthal angle of fracture, dip angle of lamination, width and length of fracture, mineral types, width, and azimuthal angle of lamination to gas saturation. The proposed brittleness model was applied to a shale reservoir and is helpful in further identifying zones for hydraulic fracturing.
有机页岩储层的开发取决于层理、裂缝、孔隙度和矿物对其脆性的影响。然而,现有的石油脆性指标只考虑矿物类型,需要综合表征。为此,采用马尔可夫链蒙特卡罗方法,将平面裂缝、平面层合和含气饱和度模型插入到多矿物模型中,构建了多组分模型。采用有限元法计算弹性参数,采用Morris筛选法和层次分析法确定弹性参数对杨氏模量和泊松比定义的脆性指数的敏感性。研究表明,脆性矿物和裂缝孔隙度的发育使脆性指数和杨氏模量增大,泊松比减小,裂缝宽度减小脆性指数,含气饱和度增大脆性指数。提出了一种新的综合脆性指标,其敏感性从倾角、裂缝方位角、层状倾角、裂缝宽度和长度、矿物类型、层状宽度和方位角对含气饱和度的敏感性依次递减。将所提出的脆性模型应用于页岩储层,有助于进一步确定水力压裂区域。
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引用次数: 0
Higher-order total-variation regularization methods for 3D inversion of gravity data 重力数据三维反演的高阶全变分正则化方法
IF 2.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2026-01-20 DOI: 10.1016/j.jappgeo.2026.106123
Mohammad Rezaie
Inverting gravity data is an important geophysical method for imaging underground structures, but it naturally suffers from non-uniqueness. To produce solutions that make geological sense, some form of regularization is necessary. This paper presents an improved methodology for 3D gravity data inversion using higher-order total variation regularization techniques. Traditional first-order TV regularization has proved effective for blocky geological structures with sharp contrasts but often fails when the subsurface features are complex. We propose second and third-order TV regularization schemes that have the strengths of classical TV but provide much greater flexibility in handling more general geological contexts. The optimization problem including these higher-order regularization terms is solved by the reweighted regularized conjugate gradient algorithm, carefully addressing the parameters selection and focusing strategies. We demonstrate the effectiveness of our approach through synthetic examples, including a dipping dyke model and a multiple blocks scenario, where the higher-order TV methods give better performance for the reconstruction of subsurface structures compared to the minimum norm and first-order TV regularization. Then, the methodology was further validated using field data from the Thunderbird V-Ti-Fe deposit, Ontario, Canada, where the inversion of airborne gravity gradiometer data successfully revealed subsurface density distributions well-matched by the known geological and drilling data. The results illustrate that the higher-order TV regularization produces a more focused and geologically plausible model, especially in resolving complex structures at different levels. Current advances in inversion methodology are offering superior performance for applications in mineral exploration and geological studies.
反演重力数据是地下构造成像的重要物探方法,但其存在非唯一性的缺陷。为了产生具有地质学意义的解决方案,某种形式的正则化是必要的。提出了一种利用高阶全变分正则化技术进行三维重力数据反演的改进方法。传统的一阶电视正则化方法对对比强烈的块状地质构造是有效的,但在地下特征复杂的情况下往往失效。我们提出了二阶和三阶电视正则化方案,它们具有经典电视的优点,但在处理更一般的地质背景时提供了更大的灵活性。采用重加权正则化共轭梯度算法求解包含高阶正则化项的优化问题,仔细处理参数选择和聚焦策略。我们通过综合实例证明了该方法的有效性,包括倾斜岩脉模型和多区块场景,其中高阶电视方法与最小范数和一阶电视正则化相比,在地下结构重建方面具有更好的性能。然后,使用加拿大安大略省雷鸟V-Ti-Fe矿床的现场数据进一步验证了该方法,在那里,航空重力梯度数据的反演成功地揭示了地下密度分布,与已知的地质和钻井数据非常匹配。结果表明,高阶电视正则化产生了一个更集中和地质上更合理的模型,特别是在不同层次上解决复杂构造。目前反演方法的发展为矿产勘探和地质研究提供了优越的性能。
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Journal of Applied Geophysics
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