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Spectral whitening based seismic data preprocessing technique to improve the quality of surface wave's velocity spectra 基于频谱白化的地震数据预处理技术,提高面波速度谱的质量
IF 4.2 2区 地球科学 Q1 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS Pub Date : 2024-11-19 DOI: 10.1016/j.cageo.2024.105784
Tarun Naskar , Mrinal Bhaumik , Sayan Mukherjee , Sai Vivek Adari
A high-quality surface wave velocity spectrum, also known as a dispersion image, is paramount for any MASW survey to accurately predict subsurface earth properties. The presence of diversified noise during field acquisition and dissimilar attenuation due to mechanical and radial damping makes it challenging for any wavefield transformation technique to produce a detailed and precise velocity spectrum. Standard surface wave data preprocessing techniques, such as trace normalization and bandpass filtering, along with postprocessing techniques like frequency-wise amplitude normalization, fail to address all these issues appropriately. In this paper, we present a spectral whitening-based data preprocessing technique that can adequately eradicate most of the shortcomings associated with different wavefield transformation techniques. Instead of normalizing each trace, it normalizes the amplitude of every frequency present in the seismogram. The spectral whitening can regain the relative amplitude losses due to both radial and mechanical damping, thus improving the signal-to-noise ratio. Along with diversified field data including Love and Rayleigh wave surveys, a synthetic dataset is used to demonstrate the efficacy of the proposed technique. Furthermore, field noise is added to random traces to test the ability of the proposed technique to filter asymmetric noise. Overall, the spectral whitening procedure significantly improves the quality of the velocity spectrum and produces a sharper dispersion image with well-separated modes. The work presented here enhances our ability to interpret surface wave velocity spectra precisely and helps explore accurate properties of the subsurface earth. It can help avoid the need for repeated field tests in cases of extremely noisy data, thereby significantly reducing costs and saving time.
高质量的面波速度频谱(也称为频散图像)对于任何 MASW 勘测准确预测地下土层属性都至关重要。由于现场采集过程中存在多种噪声,以及机械和径向阻尼导致的不同衰减,任何波场转换技术都很难生成详细而精确的速度频谱。标准的面波数据预处理技术,如轨迹归一化和带通滤波,以及后处理技术,如频率范围内的振幅归一化,都无法适当地解决所有这些问题。在本文中,我们提出了一种基于频谱白化的数据预处理技术,它能充分消除与不同波场变换技术相关的大部分缺点。它不是对每个地震道进行归一化处理,而是对地震图中每个频率的振幅进行归一化处理。频谱白化可以恢复由于径向阻尼和机械阻尼造成的相对振幅损失,从而提高信噪比。除了包括洛夫波和瑞利波勘测在内的各种现场数据外,还使用了一个合成数据集来证明所建议技术的有效性。此外,还在随机迹线中添加了现场噪声,以测试建议技术过滤非对称噪声的能力。总体而言,频谱白化程序大大提高了速度频谱的质量,并生成了具有良好分离模式的更清晰的频散图像。本文介绍的工作增强了我们精确解释面波速度频谱的能力,有助于探索地下地球的精确特性。在数据噪声极高的情况下,它有助于避免重复现场测试,从而大大降低了成本,节省了时间。
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引用次数: 0
Heterogeneous layer effects on mining-induced dynamic ruptures 异质层对采矿引起的动态断裂的影响
IF 4.2 2区 地球科学 Q1 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS Pub Date : 2024-11-17 DOI: 10.1016/j.cageo.2024.105776
Yatao Li
The risk of dynamic disasters increases with the trend toward deeper mining, highlighting an urgent need to better understand induced seismicity. To address this need, we developed custom code to implement the open-source software PyLith in the study of induced seismicity for the first time. We examined the effects of heterogeneous geological conditions on dynamic ruptures induced by deep mining operations. Our focus was on the dynamic ruptures and their effects on the nearby working face, analyzing parameters such as peak slip rates and rupture velocities. Our results show that rupture duration ranges from 255 ms to 676 ms and peak slip rates vary between 1.3 m/s and 5.0 m/s, with rupture velocities decreasing from 1.29 km/s to 0.17 km/s as the critical slip distance (Dc) increases. The relationship between peak slip rate and rupture velocity is consistent with Bizzarri's (2012) findings. A linear relationship between the times of peak slip rate (Tpv) and breakdown time (Tb) was observed, with a ratio of 1.0. In examining the induced seismic waves at the working face, we found that heterogeneous models exhibited more irregular slip distributions and higher peak particle acceleration (PPA) and peak particle velocity (PPV) compared to homogeneous models, indicating amplified seismic responses due to material heterogeneity. The study also identified potential risks to the working face's structural integrity, with more pronounced effects observed in hanging wall mining compared to footwall mining. These findings underscore the importance of considering geological heterogeneity in seismic hazard assessments and support the development of more accurate predictive models for mining-induced seismic events. It is important to note that our comparison of heterogeneous and homogeneous modeling is based on the assumption of identical initial traction, focusing on the effects of heterogeneous layers.
随着采矿向深部发展的趋势,动态灾害的风险也随之增加,因此迫切需要更好地了解诱发地震。为了满足这一需求,我们开发了自定义代码,首次将开源软件 PyLith 用于诱发地震的研究。我们研究了异质地质条件对深部采矿作业诱发的动态破裂的影响。我们的重点是动态破裂及其对附近工作面的影响,分析了峰值滑移率和破裂速度等参数。结果表明,随着临界滑移距离(Dc)的增加,破裂持续时间从 255 毫秒到 676 毫秒不等,峰值滑移率从 1.3 米/秒到 5.0 米/秒不等,破裂速度从 1.29 千米/秒下降到 0.17 千米/秒。峰值滑移率与破裂速度之间的关系与 Bizzarri(2012 年)的研究结果一致。峰值滑移速率(Tpv)和破裂时间(Tb)之间呈线性关系,比率为 1.0。在研究工作面诱发的地震波时,我们发现与均质模型相比,异质模型的滑移分布更不规则,峰值颗粒加速度 (PPA) 和峰值颗粒速度 (PPV) 也更高,这表明材料异质会放大地震反应。研究还发现了工作面结构完整性的潜在风险,与底壁采矿相比,悬壁采矿的影响更为明显。这些发现强调了在地震灾害评估中考虑地质异质性的重要性,并支持开发更准确的采矿诱发地震事件预测模型。值得注意的是,我们对异质和均质模型的比较是基于相同初始牵引力的假设,重点是异质层的影响。
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引用次数: 0
Robust frequency-domain acoustic waveform inversion using a measurement of smooth radical function derived from compressive sensing 利用测量压缩传感得出的平滑激波函数进行稳健的频域声波反演
IF 4.2 2区 地球科学 Q1 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS Pub Date : 2024-11-17 DOI: 10.1016/j.cageo.2024.105778
Chao Lang, Ning Wang, Shi-Li Pang
A smooth radical function derived from compressive sensing is introduced, aiming to measure the misfit in frequency-domain acoustic waveform inversion. The purpose of employing this function is to improve inverse accuracy and reliability. With a novel approximation of L1 norm, the objective function constructed by this measurement can exhibit favorable robustness throughout the inverse iteration. By exploiting the smoothness property, the misfit can be minimized through a cost-effective approach of taking derivatives. The inverse framework of the smooth radical function is derived which indicates comparable computing complexity per iterative step to L2 case, theoretically. The experiential data with outliers are employed for inversion and compared with the traditional optimization-based L1 norm and L2 norm. The obtained results are consistent with theoretical analysis and demonstrate the superiority of the proposed measurement.
本文介绍了一种源自压缩传感的平滑基函数,旨在测量频域声波反演中的不匹配度。使用该函数的目的是提高反演精度和可靠性。通过对 L1 准则的新颖近似,利用该测量方法构建的目标函数在整个反演迭代过程中表现出良好的鲁棒性。利用平滑特性,可以通过求导的低成本方法使误差最小化。推导出的平滑基函数逆框架表明,理论上每个迭代步骤的计算复杂度与 L2 情况相当。利用带有异常值的经验数据进行反演,并与传统的基于优化的 L1 准则和 L2 准则进行比较。得到的结果与理论分析一致,证明了所提出的测量方法的优越性。
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引用次数: 0
Augmented formulation for a Bayesian approach for frequency-domain full-waveform inversion to estimate the material properties of a layered half-space 贝叶斯频域全波形反演方法的增强公式,用于估算层状半空间的材料特性
IF 4.2 2区 地球科学 Q1 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS Pub Date : 2024-11-16 DOI: 10.1016/j.cageo.2024.105782
Hieu Van Nguyen, Jin Ho Lee
Seismic full-waveform inversion (FWI) facilitates the generation of high-resolution subsurface images using wavefield measurements. Seismic FWI in the frequency domain is preferable because it allows consideration of the multiscale nature of FWI, controls the numerical dispersion of the media, and represents the hysteretic damping of the material. The Bayesian approach can be considered for FWI problems to alleviate the ill-posedness of inverse problems and quantify the uncertainty of the estimated parameters. This study rigorously formulates a Bayesian approach for seismic FWI in the frequency domain, assuming Gaussian probability distributions for the prior information of parameters to be estimated and the likelihood functions of observations. Conventional and augmented formulations are provided. In the augmented formulation, complex dynamic responses in the frequency domain are augmented by their complex conjugates. Rigorous expressions are derived for the posterior covariance matrix of estimated parameters to assess the uncertainty in these parameters. The proposed augmented formulation is demonstrated using various elastic inverse problems to estimate the shear-wave velocities of layered half-spaces. Excellent inverted profiles for the shear-wave velocities are obtained, and their posterior probability distributions are estimated using the Bayesian approach.
地震全波形反演(FWI)有助于利用波场测量生成高分辨率的地下图像。频域地震全波形反演比较可取,因为它可以考虑全波形反演的多尺度性质,控制介质的数值色散,并表示材料的滞后阻尼。对于 FWI 问题,可以考虑采用贝叶斯方法来缓解逆问题的拟合不良性,并量化估计参数的不确定性。本研究假设待估算参数的先验信息和观测值的似然函数为高斯概率分布,严格制定了频域地震 FWI 的贝叶斯方法。研究提供了传统公式和增强公式。在增强公式中,频域中的复杂动态响应由其复杂共轭物增强。为估算参数的后验协方差矩阵导出了严格的表达式,以评估这些参数的不确定性。利用各种弹性反演问题来估算层状半空间的剪切波速度,证明了所提出的增强公式。获得了剪切波速度的出色反演剖面,并利用贝叶斯方法估算了它们的后验概率分布。
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引用次数: 0
ProbShakemap: A Python toolbox propagating source uncertainty to ground motion prediction for urgent computing applications ProbShakemap:为紧急计算应用传播地动预测源不确定性的 Python 工具箱
IF 4.2 2区 地球科学 Q1 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS Pub Date : 2024-11-16 DOI: 10.1016/j.cageo.2024.105748
Angela Stallone , Jacopo Selva , Louise Cordrie , Licia Faenza , Alberto Michelini , Valentino Lauciani
Seismic urgent computing enables early assessment of an earthquake’s impact by delivering rapid simulation-based ground-shaking forecasts. This information can be used by local authorities and disaster risk managers to inform decisions about rescue and mitigation activities in the affected areas. Uncertainty quantification for urgent computing applications stands as one of the most challenging tasks. Present-day practice accounts for the uncertainty stemming from Ground Motion Models (GMMs), but neglects the uncertainty originating from the source model, which, in the first minutes after an earthquake, is only known approximately. In principle, earthquake source uncertainty can be propagated to ground motion predictions with physics-based simulations of an ensemble of earthquake scenarios capturing source variability. However, full ensemble simulation is unfeasible under emergency conditions with strict time constraints. Here we present ProbShakemap, a Python toolbox that generates multi-scenario ensembles and delivers ensemble-based forecasts for urgent source uncertainty quantification. The toolbox implements GMMs to efficiently propagate source uncertainty from the ensemble of scenarios to ground motion predictions at a set of Points of Interest (POIs), while also accounting for model uncertainty (by accommodating multiple GMMs, if available) along with their intrinsic uncertainty. ProbShakemap incorporates functionalities from two open-source toolboxes routinely implemented in seismic hazard and risk analyses: the USGS ShakeMap software and the OpenQuake-engine. ShakeMap modules are implemented to automatically select the set and weights of GMMs available for the region struck by the earthquake, whereas the OpenQuake-engine libraries are used to compute ground shaking over a set of points by randomly sampling the available GMMs. ProbShakemap provides the user with a set of tools to explore, at each POI, the predictive distribution of ground motion values encompassing source uncertainty, model uncertainty and the inherent GMMs variability. Our proposed method is quantitatively tested against the 30 October 2016 Mw 6.5 Norcia, and the 6 February 2023 Mw 7.8 Pazarcik earthquakes. We also illustrate the differences between ProbShakemap and ShakeMap output.
地震紧急计算通过提供基于模拟的快速地震动预报,能够对地震的影响进行早期评估。地方当局和灾害风险管理者可以利用这些信息为灾区的救援和减灾活动提供决策依据。紧急计算应用的不确定性量化是最具挑战性的任务之一。目前的做法考虑了地震动模型 (GMM) 带来的不确定性,但忽略了震源模型带来的不确定性,而震源模型在地震发生后的最初几分钟内只能大致知道。原则上,地震源的不确定性可以通过捕捉震源变异性的地震场景集合物理模拟传播到地动预测中。然而,在时间紧迫的紧急情况下,完全的集合模拟是不可行的。在此,我们介绍一个 Python 工具箱 ProbShakemap,该工具箱可生成多场景集合,并为紧急震源不确定性量化提供基于集合的预测。该工具箱实现了 GMM,可有效地将源头不确定性从场景集合传播到一组兴趣点 (POI) 的地动预测,同时还考虑了模型的不确定性(如果有的话,可通过容纳多个 GMM)及其固有的不确定性。ProbShakemap 融合了两个开源工具箱的功能,这两个工具箱通常用于地震灾害和风险分析:USGS ShakeMap 软件和 OpenQuake-engine。ShakeMap 模块用于自动选择地震灾区可用的 GMMs 集和权重,而 OpenQuake-engine 库则用于通过随机抽样可用的 GMMs 来计算一组点上的地震动。ProbShakemap 为用户提供了一套工具,用于在每个 POI 探索地震动值的预测分布,包括震源不确定性、模型不确定性和 GMMs 固有的可变性。我们提出的方法针对 2016 年 10 月 30 日发生的 Mw 6.5 Norcia 地震和 2023 年 2 月 6 日发生的 Mw 7.8 Pazarcik 地震进行了定量测试。我们还说明了 ProbShakemap 和 ShakeMap 输出之间的差异。
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引用次数: 0
Functional multiple-point simulation 功能多点模拟
IF 4.2 2区 地球科学 Q1 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS Pub Date : 2024-11-14 DOI: 10.1016/j.cageo.2024.105767
Oluwasegun Taiwo Ojo , Marc G. Genton
We present a new paradigm, called functional multiple-point simulation, in which multiple-point geostatistical simulation can be performed when functions or curves are observed at each location of a random field. Multiple-point simulation is a non-parametric method used for conditional geostatistical simulation of complex spatial patterns by inferring multiple-point statistics from a training image, rather than from a two-point variogram or covariance model. When the observable at each spatial location is a functional random variable, such multiple-point simulation must take into account not only the spatial correlation among locations but also the similarity of functions or curves observed at each location. The data events to be compared in this case are now functional, in the sense that they consist of spatial arrangements of functions. Consequently, we propose four distances, inspired by the functional data analysis literature, for measuring similarities between functional data events and use these to extend the direct sampling method to perform multiple-function geostatistical simulation with functional fields. We coin the new method Functional Direct Sampling and carry out extensive qualitative and quantitative performance comparison between the four proposed distances using simulation techniques on two well-known applications of multiple-point simulation: simulating copies of a functional random field and gap-filling of locations in a functional random field. We apply the proposed method to a gap-filling task of simulated wind profiles spatial functions over the Arabian Peninsula.
我们提出了一种新的范例,称为函数多点模拟,当在随机场的每个位置观测到函数或曲线时,就可以进行多点地理统计模拟。多点模拟是一种非参数方法,通过从训练图像中推断多点统计数据,而不是从两点变异图或协方差模型中推断多点统计数据,从而对复杂的空间模式进行有条件的地质统计模拟。当每个空间位置上的观测对象都是函数随机变量时,这种多点模拟不仅要考虑位置之间的空间相关性,还要考虑在每个位置上观测到的函数或曲线的相似性。在这种情况下,需要比较的数据事件现在是函数性的,因为它们由函数的空间排列组成。因此,受函数数据分析文献的启发,我们提出了四种距离来衡量函数数据事件之间的相似性,并利用这些距离来扩展直接采样方法,以执行具有函数场的多重函数地理统计模拟。我们将新方法命名为 "功能直接采样法",并利用仿真技术在两个众所周知的多点仿真应用中对所提出的四种距离进行了广泛的定性和定量性能比较:仿真功能随机场的副本和功能随机场中位置的间隙填充。我们将提出的方法应用于阿拉伯半岛上空模拟风廓线空间函数的间隙填充任务。
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引用次数: 0
Multimodal feature integration network for lithology identification from point cloud data 从点云数据中识别岩性的多模态特征集成网络
IF 4.2 2区 地球科学 Q1 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS Pub Date : 2024-11-13 DOI: 10.1016/j.cageo.2024.105775
Ran Jing , Yanlin Shao , Qihong Zeng , Yuangang Liu , Wei Wei , Binqing Gan , Xiaolei Duan
Accurate lithology identification from outcrop surfaces is crucial for interpreting geological 3D data. However, challenges arise due to factors such as severe weathering and vegetation coverage, which hinder achieving ideal identification results with both accuracy and efficiency. The integration of 3D point cloud technology and deep learning methodologies presents a promising solution to address these challenges. In this study, we propose a novel multimodal feature integration network designed to distinguish various rock types from point clouds. Our network incorporates a multimodal feature integration block equipped with multiple attention mechanisms to extract representative deep features, along with a hierarchical feature separation block to leverage these features for precise segmentation of points corresponding to different lithologies. Furthermore, we introduce a specialized loss function tailored for rock type identification to enhance network training. Through experiments involving point cloud sampling strategies and loss function evaluation, we identify the optimal network configuration. Comparative analyses against baseline methods demonstrate the superiority of our proposed network across diverse study areas reconstructed from UAV images and laser scanner data, exhibiting improved visual appearance and metric values (Accuracy = 0.978, mean Accuracy = 0.895, mean IoU = 0.857). These findings underscore the efficacy of the multimodal feature integration network as a promising approach for lithology identification tasks in various digital outcrop models derived from heterogeneous data sources.
从露头表面准确识别岩性对于解释地质三维数据至关重要。然而,由于严重风化和植被覆盖等因素,实现理想的识别结果的准确性和效率都受到了阻碍。三维点云技术与深度学习方法的结合为应对这些挑战提供了一种前景广阔的解决方案。在本研究中,我们提出了一种新型多模态特征集成网络,旨在从点云中区分各种岩石类型。我们的网络包含一个多模态特征集成块,配备多种注意机制以提取具有代表性的深度特征,以及一个分层特征分离块,利用这些特征精确分割对应不同岩性的点。此外,我们还为岩石类型识别引入了专门的损失函数,以加强网络训练。通过点云采样策略和损失函数评估实验,我们确定了最佳网络配置。与基线方法的对比分析表明,我们提出的网络在由无人机图像和激光扫描仪数据重建的不同研究区域中具有优势,显示出更好的视觉外观和度量值(准确度 = 0.978,平均准确度 = 0.895,平均 IoU = 0.857)。这些发现强调了多模态特征集成网络的功效,它是一种很有前途的方法,可用于从异构数据源获得的各种数字露头模型中的岩性识别任务。
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引用次数: 0
A two-dimensional magnetotelluric deep learning inversion approach based on improved Dense Convolutional Network 基于改进型密集卷积网络的二维磁图谱深度学习反演方法
IF 4.2 2区 地球科学 Q1 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS Pub Date : 2024-11-12 DOI: 10.1016/j.cageo.2024.105765
Nian Yu , Chenkai Wang , Huang Chen , Wenxin Kong
Magnetotelluric (MT) inversion is an important means of MT data interpretation. The use of deep learning technology for MT inversion has attracted much attention because it is not limited to the initial model, avoids falling into local optimal solutions, and has the strong ability to process large amounts of data. However, obtaining highly reliable deep learning inversion results remains a challenge. In this paper, we have proposed a two-dimensional (2-D) MT inversion method based on the improved Dense Convolutional Network (DenseNet), with the aim of improving the reliability of the 2-D deep learning MT inversion results. First, the MARE2DEM is used to compute the 2-D MT forward responses when establishing the sample set. Then, an improved DenseNet is proposed by incorporating depthwise separable convolution in lieu of standard convolution within dense connection blocks, and embedding the attention mechanism. Depthwise separable convolution splits the standard convolution operation into depthwise and pointwise convolution, effectively capturing spatial features of input data and correlations between channels. Meanwhile, attention mechanism allows the network to assign varying degrees of importance (or attention) to different elements in a sequence of data, thus enhancing its ability of key feature extraction. This design not only retains the inherent feature reuse and alleviates gradient vanishing of DenseNet but also further enhances network performance. The optimized network parameters for the improved DenseNet are obtained by training on the training set, while the validation set is used to adjust hyperparameters and evaluate model performance. Finally, the proposed 2-D deep learning approach is verified by using both synthetic and field data. Experimental results with synthetic data show that the reliability of inversion results obtained by using the proposed algorithm is improved, and the inversion results obtained by using both TE- and TM-mode data is more accurate than those obtained by using the single mode data. The inversion results of field data show that the proposed 2-D MT deep learning inversion approach can effectively detect the subsurface resistivity structure and has a good application prospect.
磁电反演(MT)是MT数据解释的重要手段。利用深度学习技术进行MT反演因其不局限于初始模型、避免陷入局部最优解以及处理海量数据的强大能力而备受关注。然而,如何获得高度可靠的深度学习反演结果仍是一个挑战。本文提出了一种基于改进型密集卷积网络(DenseNet)的二维(2-D)MT反演方法,旨在提高二维深度学习MT反演结果的可靠性。首先,在建立样本集时,使用 MARE2DEM 计算二维 MT 前向响应。然后,通过在密集连接块中采用深度可分离卷积代替标准卷积,并嵌入注意力机制,提出了改进的 DenseNet。深度可分离卷积将标准卷积操作分为深度卷积和点卷积,从而有效捕捉输入数据的空间特征和通道之间的相关性。同时,注意力机制允许网络对数据序列中的不同元素赋予不同程度的重要性(或注意力),从而增强了关键特征提取能力。这种设计不仅保留了 DenseNet 固有的特征重用功能,缓解了 DenseNet 的梯度消失问题,还进一步提高了网络性能。改进后的 DenseNet 的优化网络参数通过在训练集上的训练获得,而验证集则用于调整超参数和评估模型性能。最后,利用合成数据和现场数据对所提出的二维深度学习方法进行了验证。合成数据的实验结果表明,使用所提算法得到的反演结果的可靠性得到了提高,使用 TE 和 TM 模式数据得到的反演结果比使用单一模式数据得到的反演结果更准确。野外数据反演结果表明,所提出的二维 MT 深度学习反演方法能有效探测地下电阻率结构,具有良好的应用前景。
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引用次数: 0
Removing atmospheric noise from InSAR interferograms in mountainous regions with a convolutional neural network 利用卷积神经网络去除山区 InSAR 干涉图中的大气噪声
IF 4.2 2区 地球科学 Q1 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS Pub Date : 2024-11-08 DOI: 10.1016/j.cageo.2024.105771
George Brencher , Scott T. Henderson , David E. Shean
Atmospheric noise in interferometric synthetic aperture radar (InSAR)-derived estimates of surface deformation often obscures real displacement signals, especially in mountainous regions. As climate change disproportionately impacts the mountain cryosphere, a reliable technique for atmospheric correction in high-relief terrain is increasingly important. We developed and implemented a statistical machine learning atmospheric correction approach that relies on the differing spatial and topographic characteristics of slow-moving periglacial features and atmospheric noise. Our correction is applied at the native spatial and temporal resolution of the InSAR data, does not require external atmospheric reanalysis data, and can correct both stratified and turbulent atmospheric noise.
Using Sentinel-1 data from 2017 to 2022, we trained a convolutional neural network (CNN) on observed atmospheric noise from 330 short-baseline interferograms and observed displacement signals from time series inversion of 1322 interferograms. We applied our trained CNN to correct 251 additional interferograms over an out-of-region application area, which were inverted to create displacement time series. We used the Rocky Mountains in New Mexico, Colorado, and Wyoming as our training, validation, testing, and application areas. When applied to our testing dataset, our correction offered performance improvements of 131%, 208%, and 68% in structural similarity index measure over corrections using atmospheric reanalysis data, phase correlation with topography, and high-pass filtering, respectively. The CNN-corrected time series reveals previously obscured kinematic behavior of rock glaciers and other features in the application dataset. Our flexible, robust approach can be used to correct arbitrary InSAR data to analyze subtle surface deformation signals for a range of science and engineering applications.
在干涉合成孔径雷达(InSAR)得出的地表形变估算值中,大气噪声往往会掩盖真实的位移信号,尤其是在山区。由于气候变化对山区冰冻圈的影响尤为严重,因此在高折射地形中采用可靠的大气校正技术变得越来越重要。我们开发并实施了一种统计机器学习大气校正方法,该方法依赖于缓慢移动的冰川地貌和大气噪声的不同空间和地形特征。我们的校正应用于 InSAR 数据的原始空间和时间分辨率,不需要外部大气再分析数据,并且可以校正分层和湍流大气噪声。利用 2017 年至 2022 年的哨兵-1 号数据,我们对来自 330 张短基线干涉图的观测到的大气噪声和来自 1322 张干涉图的时间序列反演的观测到的位移信号训练了一个卷积神经网络(CNN)。我们将训练有素的 CNN 应用于校正区域外应用区域的另外 251 张干涉图,并对这些干涉图进行反演,以创建位移时间序列。我们将新墨西哥州、科罗拉多州和怀俄明州的落基山脉作为训练区、验证区、测试区和应用区。与使用大气再分析数据、与地形的相位相关性和高通滤波进行校正相比,我们的校正方法在测试数据集上的性能分别提高了 131%、208% 和 68%。经过 CNN 校正的时间序列揭示了应用数据集中以前被掩盖的岩石冰川运动学行为和其他特征。我们灵活、稳健的方法可用于校正任意 InSAR 数据,以分析一系列科学和工程应用中的微妙地表形变信号。
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引用次数: 0
Curvilinear lineament extraction: Bayesian optimization of Principal Component Wavelet Analysis and Hysteresis Thresholding 曲线线性提取:贝叶斯优化主成分小波分析和滞后阈值法
IF 4.2 2区 地球科学 Q1 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS Pub Date : 2024-11-07 DOI: 10.1016/j.cageo.2024.105768
Bahman Abbassi, Li-Zhen Cheng
Understanding deformation networks, visible as curvilinear lineaments in images, is crucial for geoscientific explorations. However, traditional manual extraction of lineaments is expertise-dependent, time-consuming, and labor-intensive. This study introduces an automated method to extract and identify geological faults from aeromagnetic images, integrating Bayesian Hyperparameter Optimization (BHO), Principal Component Wavelet Analysis (PCWA), and Hysteresis Thresholding Algorithm (HTA). The continuous wavelet transform (CWT), employed across various scales and orientations, enhances feature extraction quality, while Principal Component Analysis (PCA) within the CWT eliminates redundant information, focusing on relevant features. Using a Gaussian Process surrogate model, BHO autonomously fine-tunes hyperparameters for optimal curvilinear pattern recognition, resulting in a highly accurate and computationally efficient solution for curvilinear lineament mapping. Empirical validation using aeromagnetic images from a prominent fault zone in the James Bay region of Quebec, Canada, demonstrates significant accuracy improvements, with 23% improvement in Fβ Score over the unoptimized PCWA-HTA and a marked 300% improvement over traditional HTA methods, underscoring the added value of fusing BHO with PCWA in the curvilinear lineament extraction process. The iterative nature of BHO progressively refines hyperparameters, enhancing geological feature detection. Early BHO iterations broadly explore the hyperparameter space, identifying low-frequency curvilinear features representing deep lineaments. As BHO advances, hyperparameter fine-tuning increases sensitivity to high-frequency features indicative of shallow lineaments. This progressive refinement ensures that later iterations better detect detailed structures, demonstrating BHO's robustness in distinguishing various curvilinear features and improving the accuracy of curvilinear lineament extraction. For future work, we aim to expand the method's applicability by incorporating multiple geophysical image types, enhancing adaptability across diverse geological contexts.
了解变形网络(在图像中表现为曲线线状)对于地球科学勘探至关重要。然而,传统的人工提取线状物的方法依赖于专业知识,耗时耗力。本研究结合贝叶斯超参数优化(BHO)、主成分小波分析(PCWA)和磁滞阈值算法(HTA),介绍了一种从航空磁场图像中提取和识别地质断层的自动化方法。在不同尺度和方向上使用的连续小波变换 (CWT) 可提高特征提取质量,而 CWT 中的主成分分析 (PCA) 则可消除冗余信息,集中处理相关特征。利用高斯过程代理模型,BHO 可自主微调超参数,以实现最佳的曲线模式识别,从而为曲线线状图绘制提供高精度和计算效率的解决方案。利用加拿大魁北克詹姆斯湾地区一个突出断层带的航空磁场图像进行的经验验证表明,该方法的精确度有了显著提高,与未优化的 PCWA-HTA 相比,Fβ 得分提高了 23%,与传统 HTA 方法相比,Fβ 得分明显提高了 300%,这突出表明了在曲线线状提取过程中融合 BHO 与 PCWA 的附加价值。BHO 的迭代特性可逐步完善超参数,增强地质特征检测。早期的 BHO 迭代可广泛探索超参数空间,识别代表深层线状的低频曲线特征。随着 BHO 的发展,超参数微调提高了对指示浅层线状的高频特征的灵敏度。这种逐步完善的过程确保了以后的迭代能更好地检测到细节结构,证明了 BHO 在区分各种曲线特征方面的鲁棒性,并提高了曲线线状提取的准确性。在未来的工作中,我们希望通过结合多种地球物理图像类型来扩展该方法的适用性,从而增强其在不同地质环境下的适应性。
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引用次数: 0
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