SM6.4 | Geophysical imaging of near-surface structures and processes
EDI
Geophysical imaging of near-surface structures and processes
Convener: Florian Wagner | Co-conveners: Ellen Van De Vijver, James Irving, Frédéric Nguyen, Anja Klotzsche
Orals
| Thu, 18 Apr, 14:00–15:45 (CEST)
 
Room -2.47/48
Posters on site
| Attendance Wed, 17 Apr, 10:45–12:30 (CEST) | Display Wed, 17 Apr, 08:30–12:30
 
Hall X1
Posters virtual
| Attendance Wed, 17 Apr, 14:00–15:45 (CEST) | Display Wed, 17 Apr, 08:30–18:00
 
vHall X1
Orals |
Thu, 14:00
Wed, 10:45
Wed, 14:00
Geophysical imaging techniques are widely used to characterize and monitor structures and processes in the shallow subsurface. Methods include active imaging using seismic, (complex) electrical resistivity, electromagnetic, and ground-penetrating radar methods, as well as passive monitoring based on ambient noise or electrical self-potentials. Advances in experimental design, instrumentation, data acquisition, data processing, numerical modeling, open hardware and software, and inversion push the limits of spatial and temporal resolution. Nonetheless, the interpretation of geophysical images often remains ambiguous. Persistent challenges addressed in this session include optimal data acquisition strategies, (automated) data processing and error quantification, spatial and temporal regularization of model parameters, integration of non-geophysical measurements and geological/process realism into the imaging procedure, joint inversion, as well as the quantitative interpretation of tomograms through suitable petrophysical relations.

In light of these topics, we invite submissions concerning a broad spectrum of near-surface geophysical imaging developments and applications at different spatial and temporal scales. Novel developments in the combination of complementary measurement methods, machine learning, and process monitoring applications are particularly welcome.

Solicited speaker: Dr. Sebastian Uhlemann, Berkeley Lab, CA, USA

Orals: Thu, 18 Apr | Room -2.47/48

14:00–14:10
|
EGU24-7978
|
ECS
|
solicited
|
On-site presentation
Sebastian Uhlemann, Luca Peruzzo, Chunwei Chou, Kenneth Williams, Stijn Wielandt, Chen Wang, Nicola Falco, Yuxin Wu, Brad Carr, Philip Meldrum, Jonathan Chambers, and Baptiste Dafflon

Hydrological processes in mountainous watersheds, and how soil, bedrock, and plants interact are still poorly understood. Through a dense network of soil moisture and temperature sensors, high resolution electrical resistivity tomography monitoring, and weather data we assess the above and below-ground processes driving the hydrological response of a hillslope during snowmelt and summer monsoon. The monitoring transect covers different bedrock and vegetation types, with a steep upper part characterized by shallow bedrock and covered by pine trees, and a gentle lower part underlain by colluvium and covered mostly by grass and veratrum. Coupling the monitoring data with a simplified hydrological model, we observe several important hydrological processes that show how variations in bedrock and vegetation type change subsurface flow patterns, allowing us to answer how subsurface flow pathways differ between shallow and deep bedrock units, and to assess the interactions between vegetation, bedrock types and subsurface flow dynamics. 

While on the steep section, characterized by thin soil and shallow bedrock, we observe mostly shallow and rapid lateral flow, on the gentle slope underlain by colluvium vertical flow is prevailing. Timelapse resistivity patterns indicate that for shallow bedrock, fractures and tree roots may provide preferential flow pathways into deeper bedrock units during snowmelt, which may provide means to mitigate summer drought conditions. Shading of the trees seems to further mitigate drought conditions by limiting evaporation of summer monsoon rainfall, leading to less drying of the shallow soil layer. In the lower, gentle part of the profile snowmelt is contributing to vertical flow recharging the aquifer, while in the summer upwelling groundwater is providing moisture to sustain plant growth. 

These observations show that variations in bedrock and vegetation pose a strong control on hillslope hydrology, creating spatially complex flow patterns. These results highlight the spatial heterogeneity of hydrological processes in mountainous watersheds, which need to be understood to predict how watersheds respond to disturbances.

How to cite: Uhlemann, S., Peruzzo, L., Chou, C., Williams, K., Wielandt, S., Wang, C., Falco, N., Wu, Y., Carr, B., Meldrum, P., Chambers, J., and Dafflon, B.: Integrated model-data observations of water flow dynamics across bedrock and vegetation variations of a mountainous hillslope, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-7978, https://doi.org/10.5194/egusphere-egu24-7978, 2024.

14:10–14:20
|
EGU24-14573
|
ECS
|
Virtual presentation
Rolando Carbonari, Rosanna Salone, and Rosa Di Maio

Hydrothermal and natural degassing geological systems present various hazards. Monitoring them is crucial to understanding their behavior, assessing risks comprehensively, and mitigating potential impacts on both the environment and human safety. Electrical resistivity, which is closely related to water content, gas content, and fluid temperature, is a key parameter for studying these systems. However, existing mathematical relationships, such as Archie's law, have limitations, particularly in their applicability to a wide range of petrophysical and thermodynamic properties. Linking the observed variations in measured resistivity to variations in the dynamics of the hydrothermal or natural degassing system under investigation is not straightforward.

 

The aim of this study is to establish a numerical relationship between petrophysical and thermodynamic input variables and resistivity data obtained from geoelectrical field surveys. This numerical relationship could predict changes in the electrical resistivity distribution based on variations in simulated petrophysical and thermodynamic values over time. Comparison between predicted and field resistivity data would ultimately validate the current dynamic state of the system, providing a powerful monitoring tool.

 

To this end, two 3D petrophysical and thermodynamic numerical models for two natural degassing systems were constructed by 3D electrical resistivity tomography surveys using constraints derived from different types of data (e.g., geological, geochemical and/or hydrogeological data). The models were validated through the comparison of predicted temperature, pressure, and gas flow distributions with field survey data. We then trained a Random Forest algorithm to predict the resistivity values for each cell of the models using the petrophysical and thermodynamic parameters of each cell as input and the field resistivity values as the target variable.

 

The results obtained for both models on the test data demonstrate the effectiveness of the Random Forest algorithm in successfully predicting resistivity values. This predictive capability, which allows adjustments to the system’s petrophysical and thermodynamic parameters until the predicted resistivity aligns with newly observed values, could shed light on the ongoing dynamics within the system, thereby enhancing its understanding through geophysical monitoring. The developed methodology could be a powerful addition to resistivity monitoring in active geological systems.  

How to cite: Carbonari, R., Salone, R., and Di Maio, R.:  Predicting Electrical Resistivity in Hydrothermal and Natural Degassing Geological Systems through petrophysical and thermodynamic data: a machine learning approach, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-14573, https://doi.org/10.5194/egusphere-egu24-14573, 2024.

14:20–14:30
|
EGU24-9793
|
ECS
|
On-site presentation
Johannes Hoppenbrock, Malkin Gerchow, Matthias Beyer, Vera Hörmann, Mona Quambusch, Michael Strohbach, and Matthias Bücker

The impact of climate change is increasingly restricting water availability in the soil, posing a significant challenge in urban areas where plants have to deal with limited space and sealed surfaces hinder rainwater infiltration. However, the amount of plant-available soil moisture plays a crucial role in plant vitality and is therefore important for ecosystem health. In urban environments, obtaining information on soil moisture is challenging. Commonly used methods, such as soil-moisture sensors, are often not applicable or do not provide a spatially resolved picture of soil moisture.

Within the context of the interdisciplinary project CliMax, we explore the applicability of geophysical methods to characterize soil moisture in the rhizosphere in urban areas. Over the past year, monthly monitoring Electrical Resistivity Tomography (ERT) measurements were conducted at nine different tree locations in Braunschweig, Germany, characterized by diverse tree species and degrees of sealing of the surface. Additionally, temporally and spatially higher-resolution measurements were selectively taken. Various time-lapse inversion approaches implemented in the open geophysical inversion library pyGIMLi were tested and applied. Furthermore, Time-Domain Reflectometry (TDR) soil-moisture sensor data from different depths are available at each site, allowing calibration of ERT results with respect to soil moisture.

The time-lapse inversion reveals well-resolved variation in soil moisture over the observed period, distinguishing between weather fluctuations and the influence of trees on the water balance. The water uptake is evident through increased resistivity values directly beneath the trees. Our study indicates that, depending on tree species and degree of sealing, the investigated urban trees predominantly extract water from the upper 1-4 meters. This finding is substantiated at specific locations by the data from deployed soil-moisture sensors.

How to cite: Hoppenbrock, J., Gerchow, M., Beyer, M., Hörmann, V., Quambusch, M., Strohbach, M., and Bücker, M.: Geoelectrical monitoring of tree-soil water interactions at urban sites , EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-9793, https://doi.org/10.5194/egusphere-egu24-9793, 2024.

14:30–14:40
|
EGU24-16128
|
ECS
|
On-site presentation
Yannick Forth, Hadrien Michel, David Caterina, Joost Hase, Andreas Kemna, Nils Chudalla, Florian Wellmann, Bjorn Vink, and Frédéric Nguyen

The geophysical investigation of geologic structures is an essential prerequisite for the preparatory phase of large subsurface construction projects like caverns or tunnels and to study structural geology. This type of investigation is crucial to guide boreholes for relevant ground truth, knowledge of the local geology, or to adjust the position of underground constructions.

Typical approaches to image large structures are seismic reflection surveys or Airborne Electromagnetic surveys (AEM). However, seismic surveys might fail due to an absorbing soft top layer or steeply inclined layers. AEM surveys generally are poorly adapted to applications in urbanized areas. To overcome these issues, another method for large-scale subsurface imaging is the application of Deep Electrical Resistivity Tomography (Deep ERT), a recent approach where employing separated injection and measurement systems allows for large injection dipoles that retrieve information from depth.

We conducted a Deep ERT campaign in the framework of the E-TEST project for the investigation for a suitable location for the Einstein Telescope, a gravitational wave observatory consisting of a set of subsurface laser interferometers in a triangular shape at a depth around 300 m. Here, we present the results from a 2D Deep ERT survey in Val Dieu, Belgium with a total length and maximum injection dipoles of 7,5 km and a total of 14040 measured datapoints. We show the challenges during preparation, performance and data processing and discuss its capability in imaging large and deep geological structures.

How to cite: Forth, Y., Michel, H., Caterina, D., Hase, J., Kemna, A., Chudalla, N., Wellmann, F., Vink, B., and Nguyen, F.: Imaging large-scale geological structures using Deep ERT: a case study on the Booze Val-Dieu block in Belgium, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-16128, https://doi.org/10.5194/egusphere-egu24-16128, 2024.

14:40–14:50
|
EGU24-382
|
ECS
|
On-site presentation
Orhan Apaydın and Turgay İşseven

In this study, the detection of buried objects in GPR images using the deep learning-based Faster R-CNN and YOLOv5 methods and their classification according to their geometric shapes are investigated. Buried objects in the near surface may have different geometric shapes. Such objects can be imaged using Ground Penetrating Radar (GPR). As research materials, a rectangular prism-shaped aluminum-coated box and a cylindrical rod are used for laboratory measurements. A simulated underground model has been created in a laboratory environment, and GPR measurements have been performed. A radar device is designed for measurements using a Vector Network Analyzer (VNA) and a Vivaldi antenna pair. The scenarios for the measurements in the laboratory environment are modeled in the gprMax program, and synthetic GPR images are generated. The dataset consists of both actual measurements and synthetic data. Deep learning-based Faster R-CNN and YOLOv5 methods are popular techniques used for object detection in images. The GPR images used for training in these methods are augmented by using flipping and resizing techniques, and the dataset is expanded. Subsequently, hyperbolic structures of objects in GPR images are labeled as "rectangular" and "cylindrical" based on their geometric shapes. The training process is then carried out using these methods, resulting in the detection of buried objects in GPR images with high accuracy and classification based on their geometric shapes as "rectangular" and "cylindrical". The performances of the two different methods are compared, revealing that Faster R-CNN achieved higher accuracy, while the YOLOv5 method exhibited faster detection.

How to cite: Apaydın, O. and İşseven, T.: Detection and classification of near-surface buried objects in GPR images with deep learning-based Faster R-CNN and YOLOv5 methods, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-382, https://doi.org/10.5194/egusphere-egu24-382, 2024.

14:50–15:00
|
EGU24-3609
|
ECS
|
On-site presentation
Albachiara Brindisi, Dario Albarello, Nicolò Carfagna, and Enrico Paolucci

Multiple studies highlight the evidence of a trough within the low-frequency range in HVSRs measurements performed over a gas field and attribute it to the presence of a hydrocarbon reservoir (Lambert et al., 2007; Saenger et al., 2007; Panzera et al., 2016). To explain the natural emission of low-frequency signals Saenger et al. (2007) and Lambert et al. (2007) consider hydrocarbon-reservoir related microtremor, assuming that the reservoir itself acts as a (secondary) source of low-frequency seismic waves by a resonant amplification effect. Furthermore, Panzera et al. (2016) observe that the minimum is identified by an “inverse eye-shaped” feature in the Fourier spectra, related to an amplitude increase in the vertical component of motion due to a velocity inversion. This study focuses on the investigation of the spectral anomaly described above at Nirano mud volcano field, conducted through the analysis of the results obtained by seismic arrays and three directional velocimetric stations (HVSR) deployed in the site. After a cluster analysis carried out on HVSRs have been identified 3 groups of measurements, one of which include HVSRs located in the caldera-like basin area, marked by a minimum in the seismic spectrum at 0.53 Hz. The joint inversion procedure based on Genetic Algorithms of the HVSR curves and the Rayleigh waves dispersion curve shows that the minimum is well reproduced even without a velocity inversion. This proves that it is not uniquely correlated to the mechanisms proposed above and that, therefore, it may be linked to a stratigraphic effect that unites all the measurements concentrated in the group under examination or to the surface wave model used.

References

Lambert M., Schmalholz S. M., Saenger E. H. and Podladchikov Y. Y.; 2007: Low-frequency anomalies in spectral ratios of single-station microtremor measurements: Observations across an oil and gas field in Austria. In SEG Technical Program Expanded Abstracts 2007 (pp. 1352-1356). Society of Exploration Geophysicists.

Panzera F., Sicali S., Lombardo G., Imposa S., Gresta S. and D’Amico S.; 2016: A microtremor survey to define the subsoil structure in a mud volcanoes area: the case study of Salinelle (Mt. Etna, Italy). Environmental Earth Sciences, 75, 1-13.

Saenger E.H., Torres A., Rentsch S., Lambert M., Schmalholz S.M. and Mendez-Hernandez E.; 2007: A hydrocarbon microtremor survey over a gas field: Identification of seismic attributes. 77th SEG meeting, San Antonio, Texas, USA, Expanded Abstracts, 1277–1281.

How to cite: Brindisi, A., Albarello, D., Carfagna, N., and Paolucci, E.: HVSR analysis to investigate a possible correlation to a gas shallow reservoir in a mud volcanic field: the case of Nirano (MO)., EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-3609, https://doi.org/10.5194/egusphere-egu24-3609, 2024.

15:00–15:10
|
EGU24-1014
|
ECS
|
Virtual presentation
Rashi Rashi, Rahul Dehiya, Sudipta Sarkar, and Raymond Duraiswami

Lava-flow structure and morphology provide insights into eruption styles, emplacement mechanisms, and post-emplacement alterations like weathering. However, the challenge lies in quantifying subsurface structures of buried lava flows beneath soil and vegetation cover. We present a case study of lave flow mapping employing seismic methods from the Dive Ghat region of Pune, situated in the Deccan Volcanic Province. Seismic data was collected using a 48-channel engineering seismograph with 1m receiver spacing and 2m shot spacing via a sledgehammer source. The seismic profile is taken parallel (roughly 4 m away) to the approximately 10 m vertical exposed section, which is used for cross-validation of the flow geometry, and it shows the presence of roughly six inches of red bole layer overlaying on a highly weathered basalt. The observed data is analyzed through refraction and multichannel analysis of surface wave (MASW) techniques. The refraction method yielded a high-resolution P-wave velocity model in the near subsurface with P-wave velocity (Vp) ranging from 0.3–4.5 km/s. However, the refraction method fails to image highly weathered basalt, which is expected as no critically refracted wave will be generated from the top of a low-velocity layer. The MASW method delivered a horizontally smeared S-wave velocity model where S-wave velocity (Vs) varies from 0.15–2.2 km/s. The subsurface S-wave model has a low-velocity layer of around 0.7 km/s Vs velocity embedded between 8.5–14m, which correlates to a red bole layer and underlying fractured basalt formed through weathering. Furthermore, a Vp-Vs cross plot is calculated to characterize different seismic units in velocity sections. The results obtained in this study may serve as an analogue to map near-surface flow geometry in unexposed sections in the Deccan Volcanic Province region. The MASW method successfully imaged the buried red bole layer and underlying weathered zone, which is crucial for agriculture due to its organic content. The imaging also holds implications for slope stability studies, emphasizing the importance of seismic characterization for hazard zonation, especially concerning the red bole and fractured basalt.

How to cite: Rashi, R., Dehiya, R., Sarkar, S., and Duraiswami, R.: Mapping basalt lava flows at Dive Ghat (Pune, India) using multichannel analysis of surface wave (MASW) technique, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-1014, https://doi.org/10.5194/egusphere-egu24-1014, 2024.

15:10–15:20
|
EGU24-17357
|
ECS
|
On-site presentation
Xinhua Chen, Jianghai Xia, Yu Hong, and Jingyin Pang

In near-surface investigations, the advent of massive seismic data has ushered in the application of deep learning (DL) techniques for surface wave inversion to attain the shear-wave velocity (Vs). While the efficiency of DL inversion surpasses that of classic physics-driven methods, its broader attributes remain underexplored. Our study delves into a comparative analysis of DL inversion versus physics-driven inversion, focusing on three key aspects: anti-noise ability, stability, and generalization.

In numerical experiments, we employ the neighborhood algorithm (NA) (Wathelet, 2008) as a representative of physics-driven inversion, and a convolutional neural network (CNN) constructed for near-surface investigations (Chen et al., 2022) as a representative of data-driven inversion. In addition to comparing the two methods, we also explore the characteristics of joint inversion using Rayleigh-wave dispersion curves (DCs) and Love-wave DCs in the three above aspects. To quantitatively evaluate inversion results, we calculate the root mean square error and relative error of both DCs and Vs. The assessment of anti-noise performance involves applying NA and CNN to DCs with varying noise levels. To gauge stability, we introduce errors in compressional-wave velocity (Vp) and density, examining their effects on inversion precision. Lastly, to assess generalization, we use NA and CNN to invert DCs whose Vs exceeds the range of the training dataset by different percentages.

Our findings reveal that DL inversion has a higher anti-noise ability compared with NA. Both methods demonstrate high stability, with errors in Vp and density exerting a slight impact on inversion results, aligning with surface wave inversion characteristics. Compared with physics-driven inversion, generalization is a unique feature of data-driven inversion. The experimental results indicate that the CNN can predict Vs models that are not included in the training dataset although this ability is somewhat limited. Furthermore, like physics-driven inversion, joint inversion enhances all three examined aspects for data-driven inversion. This analysis of characteristics can guide the selection of inversion methods for surface wave applications in near-surface investigations.

 

References:

  • Wathelet M., "An improved neighborhood algorithm: parameter conditions and dynamic scaling," Geophysical Research Letters, vol. 35, no. 9, pp. 2008, doi: 10.1029/2008GL033256.
  • Chen X., Xia J., Pang J., Zhou C., and Mi B., "Deep learning inversion of Rayleigh-wave dispersion curves with geological constraints for near-surface investigations," Geophysical Journal International, vol. 231, no. 1, pp. 1-14, 2022, doi: 10.1093/gji/ggac171.

How to cite: Chen, X., Xia, J., Hong, Y., and Pang, J.: Comparison of data-driven and physics-driven surface wave inversion, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-17357, https://doi.org/10.5194/egusphere-egu24-17357, 2024.

15:20–15:30
|
EGU24-17729
|
ECS
|
On-site presentation
Arnaud Mercier and Hansruedi Maurer

Full Waveform Inversion (FWI) has emerged as a groundbreaking tool in geophysics, offering unprecedented resolution in subsurface imaging. However, its broader application is often limited by substantial computational demands, especially in 3D elastic applications. This research addresses this critical barrier by introducing a novel approach that optimizes both data (source-receiver layout) and model (model parameterization) spaces, thereby reducing computational overhead and extending FWI's applicability. The interdependence between data and model spaces is a key factor to optimize FWI. We believe that both spaces must be simultaneously optimized to enhance the efficiency of FWI. This optimization is particularly crucial for intensive FWI problems but is also expected to make FWI accessible to a broader range of users, including those with limited computational resources.

We combine principles from Optimal Experimental Design (OED) and Compact Full Waveform Inversion (CFWI). Selecting only the most relevant source-receiver pair ensures a minimal, yet informative data set. By using a wavelet representation of the model, it is possible to easily tune the compression of the model based on the local resolution. The outcome of our data-model approach is a source-receiver layout that maximize the resolution of a compressed representation of the model.

Initial results with applications focused on synthetic 2D acoustic problems shows that the data-model approach allow for a significant reduction in both source-receiver pairs (≈ 50%) and model parameters (≈ 90%), whilst retaining 90% of the information content. Compare to classical OED criterion, our approach posses a lower time complexity by about 2 order of magnitude (O (m) vs O (mn2)). The significant speed up enables optimizing for sources and receivers independently, leading to further optimized layouts.

The data and model compression enables the use of Gauss-Newton optimization algorithm, leveraging faster convergence and greater flexibility. Benefits of this algorithm includes the possibility to optimize source-receiver layouts not only prior to fieldwork, but also during the inversion. At each stage of the inversion process, the most relevant data points are effectively identified and retained. This selection significantly reduces both computational and memory requirements. An additional benefit of this approach is the straightforward implementation of targeted OED, enabling optimization of the source-receiver layout for specific subsurface targets.

Key aspects to ensure a reliable and efficient data-model approach include evaluating the prior model's influence, examining the effects of compression ratio, resolving ambiguities in survey layout and model parametrization, and refining source and receiver positioning. We will present initial results and  highlight its potential benefits to significantly reduce the computational load of FWI.

How to cite: Mercier, A. and Maurer, H.: Optimizing Full Waveform Inverse Problems: A Combined Data and Model approach, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-17729, https://doi.org/10.5194/egusphere-egu24-17729, 2024.

15:30–15:40
|
EGU24-19778
|
ECS
|
On-site presentation
Hagen Söding, Hansruedi Maurer, and Thomas Fechner

Tomographic techniques have been an indispensable tool for tackling manifold problems in earth and environmental sciences. For wavefield techniques, like seismics and ground penetrating radar, full waveform inversions offer powerful tools for extracting the full waveform information content to obtain high-resolution subsurface images. Although mostly applied to deeper targets (exploration scale), near-surface full waveform information holds a strong potential to analyse the often more complicated subsurface structures both in imaging and monitoring applications. Due to the complexity of the very shallow subsurface, source- and receiver coupling often exhibit substantial variations and can thus not be neglected. Maurer et al. (2012) showed that this problem can be addressed in frequency domain full waveform inversions by including source- and receiver coupling terms as additional unknowns into the inversion workflow. However, there are inherent trade-offs between the source- and receiver coupling factors. This is irrelevant for frequency-domain full waveform inversions, but this problem needs to be addressed for time-domain inversion problems.

In our contribution we present two possible options to make source- and receiver coupling inversions also applicable in time-domain problems, using either a parameterized source wavelet or a sparsity regularisation approach. We demonstrate our novel methodology with a synthetic study and with an application to an acoustic seismic full waveform inversion on a CCS study from the Digimon project from Svelvik, Norway.

 

References:

Hansruedi Maurer, Stewart A. Greenhalgh, Edgar Manukyan, Stefano Marelli, Alan G. Green; Receiver-coupling effects in seismic waveform inversions. Geophysics 2012;; 77 (1): R57–R63. doi: https://doi.org/10.1190/geo2010-0402.1

How to cite: Söding, H., Maurer, H., and Fechner, T.: Source- and receiver-coupling effects for time-domain Full Waveform Inversion, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-19778, https://doi.org/10.5194/egusphere-egu24-19778, 2024.

15:40–15:45

Posters on site: Wed, 17 Apr, 10:45–12:30 | Hall X1

Display time: Wed, 17 Apr, 08:30–Wed, 17 Apr, 12:30
X1.95
|
EGU24-5159
Yan Liu, Yao Huang, and Qingtian Lü

We proposes a method of gravity inversion based on an adaptive mesh-free approach by using a modified radial basis function . It can parametrize the density distribution by using a mesh-free approach. The subsurface space is generally discretized into regular grid cells, while mesh-free methods can avoid the expensive mesh generation and manipulation required in traditional approaches. Scattered points are introduced in most mesh-free methods to discretize the given equations. To deal with the problem of unstructured nodal discretization, we use a mesh-free discretization strategy to establish a mapping of subsurface grid cells to a cloud of discrete points. The nodes are adaptively refined during the inversion process to better recover abnormal bodies. In addition, the hybrid basis function and the modified radial basis function are used to improve the accuracy and stability of the solution. We verify the effectiveness of the proposed method by using several synthetic and empirical tests.

How to cite: Liu, Y., Huang, Y., and Lü, Q.: Adaptive Mesh-free Approach for Gravity Inversion, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-5159, https://doi.org/10.5194/egusphere-egu24-5159, 2024.

X1.96
|
EGU24-12500
|
ECS
Sophie Stephan, Conrad Jackisch, Jens Tronicke, and Niklas Allroggen

High-resolution measurement techniques for distributed and fast soil water dynamics could advance the understanding of subsurface infiltration processes on the plot scale when it can combine high spatial and temporal resolution with a high repeatability of the measured data.

Ground-penetrating radar (GPR) is a promising geophysical tool to image and quantify subsurface flow processes in a non-invasive fashion. In the literature, different strategies to collect time-lapse GPR data have been presented. However, so far, no standardized data acquisition and analysis strategy has been established to monitor subsurface changes related to water infiltration and to compare the outcomes of different experiments.

Here, we present a 4D-GPR measurement strategy to monitor infiltration experiments by combining an irrigation pad (to simulate moderate rain fall events) with a manually operated 3D GPR measurement platform (equipped with a two-channel GPR antenna array and positioning guides). For investigating the repeatability and resolution limits of our measurement strategy, we conducted a systematic field experiment with two recurrent irrigations at two nearby spots at a selected field plot. Our results show that we can reliably monitor non-uniform subsurface flow processes with a spatial resolution < 5 cm and a temporal resolution below 10 minutes.

Because of these so far unreached spatial and temporal resolution capabilities we consider our 4D-GPR measurement strategy as a first step toward a standardized strategy for monitoring infiltration processes. Furthermore, such detailed knowledge about the resolution and repeatability limits of 4D-GPR measurements opens new options for further interpretation approaches, for example without assumptions about a horizontally stratified subsurface model.

How to cite: Stephan, S., Jackisch, C., Tronicke, J., and Allroggen, N.: High-resolution 4D GPR data acquisition strategy to monitor fast and small-scale subsurface flow processes, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-12500, https://doi.org/10.5194/egusphere-egu24-12500, 2024.

X1.97
|
EGU24-4860
|
ECS
Machine Learning-Based Identification of Fault Structures in Seismic Refraction and Resistivity Tomography
(withdrawn after no-show)
Yonatan Garkebo Doyoro, Chih-Ping Lin, Samuel Kebede Gelena, and Ernian Pan
X1.98
|
EGU24-12370
|
ECS
Anton H. Ziegon, Marc S. Boxberg, and Florian M. Wagner

Interpreting independent geophysical data sets can be challenging due to ambiguity and non-uniqueness. To address this, joint inversion techniques have been developed to produce less ambiguous multi-physical subsurface images. Recently, a novel cooperative inversion approach that uses minimum entropy constraints has been proposed. The major feature of this approach is that it can produce sharper boundaries inside the model domain. We implemented this approach in an open-source software framework and systematically investigated its capabilities and applicability on electrical resistivity tomography (ERT), seismic refraction tomography (SRT), and magnetic data.

First, we conducted a synthetic 2D ERT and SRT data study to demonstrate the approach and investigate the influence of the equations’ parameters that must be calibrated as well as to justify extensions of the method. The results show that the use of the joint minimum entropy (JME) stabilizer outclasses separate, conventional smoothness-constrained inversions and provides improved images.

Next, we used the method to analyze 3D ERT and magnetic field data from Rockeskyller Kopf, Germany. Independent inversion of the magnetic field data already suggested a subsurface volcanic diatreme structure, but the joint inversion using JME not only confirmed the expected structure, but also provided improved details in the subsurface image. The multi-physical images of both methods are consistent in many regions of the model as they produce similar boundaries. Due to the sensitivity of the ERT measurements to hydrogeological conditions in the subsurface, some structures are only visible in the ERT data. These features seem not to be enforced on the magnetic susceptibility model, which highlights another advantage and the flexibility of the approach.

However, the results of both the synthetic and field data use cases suggest that careful parameter tests are required prior to cooperative inversion to obtain a suitable hyperparameters and reference model. Our work implies that minimum entropy constrained cooperative inversion is a promising tool for geophysical imaging provided that proper settings are chosen while it also identifies some objectives for future research to improve the approach.

How to cite: Ziegon, A. H., Boxberg, M. S., and Wagner, F. M.: Minimum entropy constrained cooperative inversion with application to electrical resistivity, seismic and magnetic field and synthetic data, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-12370, https://doi.org/10.5194/egusphere-egu24-12370, 2024.

X1.99
|
EGU24-9128
|
ECS
Nino Menzel, Sebastian Uhlemann, and Florian M. Wagner

Electrical resistivity tomography (ERT) offers noninvasive monitoring capabilities for a wide range of environmentally relevant subsurface processes. Its sensitivity to fluid content and temperature changes positions it as an important tool for capturing dynamic processes such as the transport of groundwater pollutants, CO2 or radionuclides. Particularly crucial is its ability to achieve this without intrusively accessing to the site, making it highly valuable in closed repositories like high-level radioactive waste (HLW) storage sites.

In highly sensitive and complex environments, as in the case of closed repositories, it is critical to maximize the information content of the planned (geo)physical measurements while keeping the costs to a minimum. Several past studies presented approaches to optimize both the sensor positions and the measurement configurations of ERT surveys for static or moving targets in the subsurface. This study extends Optimal Experimental Design (OED) strategies for geoelectrical measurements using information of active time-dependent transport processes in the subsurface. We present three different approaches for process monitoring and apply them to a simulated diffusive-advective transport process in a synthetic model over several time steps. The methods aim at focusing the survey only on the relevant part of the model, in this case the model region that is affected by the transport process. All presented approaches account for uncertain model input parameters by introducing an uncertainty factor in the ranking function. We present a purely model-driven and a purely data-driven active time-dependent OED approach. The first method utilizes the already acquired data from previous time steps to create predictive focusing masks for the next data set, the latter purely relies on model predictions to focus the survey. Moreover, we delineate a hybrid approach using both the simulated transport distance and the already acquired datasets. All three OED methods are compared to each other as well as to datasets that were acquired using standard electrode configurations.

The results of our synthetic study show that the adaptively designed, time-dependent OED approaches result in increased image quality compared to both standard surveys as well as time-independent OED methods. For slow transport processes or small monitoring intervals, the purely data-driven approach is most suitable, since no model predictions, and thus no possible model parametrization uncertainties, are incorporated. For faster transport processes or monitoring strategies with larger acquisition intervals, the strategies that (partly) incorporate model predictions provide the most promising results.

How to cite: Menzel, N., Uhlemann, S., and Wagner, F. M.: Optimal Experimental Design strategies for geoelectrical monitoring of fluid transport processes, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-9128, https://doi.org/10.5194/egusphere-egu24-9128, 2024.

X1.100
|
EGU24-18216
|
ECS
Polina Pugacheva and Hussien Allam

The application of Electrical Resistivity Tomography (ERT) for the investigation of architectural heritage has numerous limitations. In most cases, we are referring to historic stone buildings and monuments built from limestone, sandstone, or granite blocks, where many features may complicate the interpretation of electrical resistivity data. First of all, there is incomplete or missing information about principles of building construction and the materials used. Another challenge is the heterogeneity of the masonry as a material due to the presence of many joints between the stone blocks, which may be filled with cementitious materials or be completely or partially empty. For medium-scale studies with limited penetration depth, the presence of air in the joints between stone blocks may affect the electrical resistivity distribution and interfere with the detection of the archaeologically relevant anomalies associated, in particular, with the presence of air cavities. Systematic studies of the applicability of the Electrical Resistivity Tomography in such blocky structures are lacking. In this study, the effect caused by masonry geometry was assessed using numerical 3D modelling of the electrical resistivity distribution in a simplified blocky structure consisting of rows of masonry blocks by incorporating joints between them. The purpose is to study how the presence of air-filled joints affects the ability of the ERT method to detect voids in masonry structures depending on the position and size of these voids. The analysis of numerical models provides insights to facilitate the interpretation of ERT results in historical monuments and other structures constructed from stone blocks.

How to cite: Pugacheva, P. and Allam, H.: Application of 3D Forward Modelling to Improve the Interpretation of Electrical Resistivity Tomography Results in Architectural Heritage Monuments, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-18216, https://doi.org/10.5194/egusphere-egu24-18216, 2024.

X1.101
|
EGU24-2665
|
ECS
Evaluating Hydro Carbon Potential and Estimating Crustal Shortening in Pothohar Area, Punjab, Pakistan
(withdrawn after no-show)
Rizwan Maqsood
X1.102
|
EGU24-8256
Yanru An, Weitao Wang, Wei Yang, Haikun Jiang, Jun Yang, Xiaobin Li, and Rui Pan

Seismic velocity change is a good indicator reflecting the stress state variation of the underground media. Therefore, seismogenic process could be effectively revealed by the velocity change calculation. Based on the seismic ambient noise interferometry, we study the co-seismic velocity change and post-seismic recovery process of the 21 May 2021 MS6.4 Yangbi earthquake using the continuous records from 16 stations within 50km of the epicenter. The results show that the relative velocity changes between the station pairs (dv/vpair) decrease significantly after the mainshock. The amplitude ranges from -0.29% to -0.02% and decreases with the increase of station spacing. The relative velocity changes of each station (dv/vstation) obtained by linear regression range from -0.16% to -0.02%, and are generally negatively correlated with the epicenter distance. It is notable that the measured co-seismic velocity changes are mainly originated from the shallow media (≤2km). Such changes are considered to be caused by both static and dynamic strain, but the primary controlling factor is rock fragmentation and large-scale adjustment of stress produced by strong ground motion. In addition, dv/vstation located at the northern stations far from the epicenter have the largest drop values, demonstrating that they are more sensitive to stress disturbances. This may be related to the distribution of thermal fluids below these stations. The results of velocity changes indicate that around the study area the seismic velocity reached its minimum value within a few days after the mainshock. The value then gradually recovered, reaching the pre-seismic level around August, which characterizes the healing process of broken rocks. In this study, ambient noise interferometry has been effectively applied to measure the velocity changes during and after the Yangbi earthquake, and the results show that co-seismic velocity changes are jointly controlled by various factors including the fracture degree of the fault zone, dynamic strain, and the existence of fluids.

How to cite: An, Y., Wang, W., Yang, W., Jiang, H., Yang, J., Li, X., and Pan, R.: Using ambient noise to study the co-seismic and post-seismic velocity changes of the 2021 Yangbi MS 6.4 earthquake in Yunnan, China, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-8256, https://doi.org/10.5194/egusphere-egu24-8256, 2024.

X1.103
|
EGU24-3801
Christopher Juhlin, Bojan Brodic, Mikael Erlström, Peter Hedin, Daniel Sopher, Zhihui Wang, and Zbigniew Wilczynski

Reflection seismic data were acquired in the Sudret area of Gotland in the time window 6 to 13 November, 2023. Objectives of the survey were to obtain images of the subsurface down to the Precambrian basement in the vicinity of two coreholes that had been drilled earlier down to about 800 m. These images would provide a better understanding of the sedimentary strata and local structure near these holes. For these purposes a sparse 3D survey was acquired that covered a c. 300 m by 700 m rectangular area with high fold, including the locations where the boreholes were drilled. A longer c. 2.8 km 2D profile was also acquired adjacent to the 3D survey that ran roughly in the N-S direction. In addition, distributed acoustic sensing (DAS) measurements were performed in the two coreholes. We report here on some results from the 3D survey and from the DAS measurements.

A Bobcat source with a 500 kg weight drop hammer with base plate was used as a source and 410 5Hz nodal units were available for recording. In total, 704 receiver locations were occupied with acquisition along 19 source lines, implying that 294 units had to be moved during the survey and that the source lines had to be shot twice. DAS data were recorded over the depth interval 17 m above sea level to 475 m below sea level in the Nore-1 corehole. In Nore-2 the depth interval was 17 m above sea level to 720 m below sea level. The fiber optic cable was sampled at 2.45 m intervals and data were recorded at a sampling frequency of 4000 Hz. Due to borehole irregularities it was not possible to get the fiber optic cables all the way to the bottom of the coreholes.

Numerous semi-continuous reflection horizons are observed in the c. upper 500 ms after stacking. A particularly strong reflection at 350 ms likely originates from the top of the Ordovician. Cambrian sandstones are also reflective, as well as shallow sandstone layers in the upper 150 ms. Normal moveout (NMO) velocities are relatively constant at about 3500 m/s. However, depth conversion using this velocity places the reflectivity deeper than what is expected from the cores. The DAS data allow the vertically propagating P-wave velocity to be measured at 3100 m/s. Using this velocity for depth conversion provides more reasonable depths to the main horizons. Since the NMO velocities are largely controlled by the horizontal velocity of the rock the difference between these and the DAS velocity can be explained by the rocks in the area having significant anisotropy (about 10%).

How to cite: Juhlin, C., Brodic, B., Erlström, M., Hedin, P., Sopher, D., Wang, Z., and Wilczynski, Z.: 3D reflection seismic surveying and borehole DAS measurements to image the sedimentary structure in the Sudret area of Gotland, Sweden, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-3801, https://doi.org/10.5194/egusphere-egu24-3801, 2024.

X1.104
|
EGU24-15635
Xu Wang, Ling Chen, and Xin Wang

Exploring the shallow crustal structure of Mars can offer valuable insights into the planet’s geological evolution and climate history. The ambient wavefield data and marsquake records from NASA’s InSight mission have enabled the characterization of both fine-scale near-surface structures (less than 200 meters) and large-scale crustal structures (greater than a few kilometers) on Mars. However, the exploration of intermediate-scale structures has remained limited. In this study, we introduce a novel varying-parameter approach that integrates principal component analysis with receiver function techniques. This method allows for the effective extraction of P-wave particle motions across various frequencies from the InSight low-frequency marsquake data, facilitating the inversion for the S-wave velocity structure within the topfew kilometers beneath the lander. Our resulting models reveal a distinct discontinuity at a depth of approximately 0.7 km, marked by a sharp increase in S-wave velocity from about 1.4 km/s to roughly 1.9 km/s. This discontinuity is characterized by a sharp transition, approximately 0.1 km thick, rather than a wider gradient zone. Our models are generally consistent with existing data on Mars’ near-surface and large-scale crustal structures, effectively bridging these datasets. When combined with previous geological and seismic observations, the newly identified discontinuity may signify the top of less affected basaltic bedrock, and the overlying structures are interpreted as a composite of Noachian- to early Hesperian-aged sediments and Hesperian to Amazonian basalts. These insights provide new perspectives on the stratification at the InSight landing area, enhancing our understanding of Martian geological history.

How to cite: Wang, X., Chen, L., and Wang, X.: Shallow Crustal Structures of Mars Beneath the InSight Landing Site Revealed by Frequency-Dependent P-wave Particle Motions, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-15635, https://doi.org/10.5194/egusphere-egu24-15635, 2024.

X1.105
|
EGU24-19047
Virginie Gaullier, François Schmitt, and Muriel Laurencin

Numerous very high-resolution seismic lines (Sparker/single-channel seismic reflection) were acquired in the Eastern Channel, along the the Opal Coast, between the Bay of Somme and Cape Gris-Nez, during the oceanographic missions GEOBAS (2016-2020), TREMOR 1 (2014), TREMOR 2 (2017) and MARCOPALE (2023). In this sector, numerous sandy banks are observed, especially the Bassure of Baas. These geophysical data were analyzed as part of the TURBODUNES project, by comparing two reflectors, respectively the sea floor and the base of the dunes (corresponding to the top of the deformed Cretaceous and Eocene bedrocks). The difference between the two signals makes it possible to identify areas with dunes and areas where dunes are absent. Assuming a constant boat speed, the extraction of signals provides spatial information on the height of the dunes. We carry out analyzes of these signals using different methods, including Fourier spectral analysis, empirical mode decomposition and structure functions. Empirical mode decomposition is a method which allows a one-dimensional series to be decomposed into a sum of several series, called “modes”, each having a characteristic wavelength. This makes it possible to quantitatively characterize the shape of the dunes via different modes, each having a wavelength ranging between 25 and 400 m. The lines for which dunes are absent nevertheless have profiles with strong multi-scale variability, with scale-invariant Fourier spectra with a slope of -2, for scales between 2.5 m and approximately 1 km.

How to cite: Gaullier, V., Schmitt, F., and Laurencin, M.: Statistical analyzes of the shapes of marine sand dunes off the Opal Coast (Eastern English Channel), EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-19047, https://doi.org/10.5194/egusphere-egu24-19047, 2024.

X1.106
|
EGU24-12013
Ludovic Bodet, Ramon Sanchez Gonzalez, José Cunha Teixeira, Marine Dangeard, Alexandrine Gesret, and Agnès Rivière

Pressure (P) or shear (S)-wave velocity models of the near-surface can be simultaneously estimated along coincident arrays from P-wave refraction tomography and surface-wave (SW) dispersion inversion methods. Over the past decade, this approach has been integrated into the hydrogeophysics toolbox to image spatial variations of VP/VS (or Poisson) ratio, as its evolution is strongly associated with water content (or saturation) contrasts. The relevance of this method has been verified in various Critical Zone (CZ) observatories, each with distinct hydrogeological characteristics such as continuous multi-layered hydrosystems or fractured environments with strong discontinuities. It has also proven successful in other contexts and application scales, including a hydrothermal site or partially saturated glass beads in a laboratory experiment. However, we identified two major issues: (1) the combined use of P-wave traveltime tomography and SW dispersion inversion involves distinct characteristics of the wavefield and different assumptions about the medium, providing VP and VS models with different sensitivity, resolution, investigation depth, and posterior uncertainties; (2) the involved inversion processes use a small number of layers that cannot properly describe the continuous variations of subsurface hydrological properties. In particular, we noted that VP/VS (or Poisson) ratio was only consistent with strong saturation contrasts and often faced difficulties in retrieving water content variations in the unsaturated zone. This underscores the need to use petrophysical approaches to build alternative forward models and improve inversion processes. Adapted rock physics models have thus recently been developed to take capillary suction effects into account in the effective stress of the soil. In this study, we first present several datasets obtained from various contexts in which SW dispersion variations have been observed and related to changes in water content and/or water table depths. We then suggest using the previously cited rock physics models to simulate these data and show how it helps in understanding the involved hydrofacieses and processes. We finally address the relevance of surface-wave dispersion inversion approaches involving such forward models and discuss the possible use of additional attributes of the seismic wavefield to constrain interpretations.

How to cite: Bodet, L., Sanchez Gonzalez, R., Cunha Teixeira, J., Dangeard, M., Gesret, A., and Rivière, A.: Measuring and modelling seismic surface-wave dispersion variations in various hydrogeological contexts, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-12013, https://doi.org/10.5194/egusphere-egu24-12013, 2024.

X1.107
|
EGU24-15191
|
ECS
Caiwang Shi, Xiaofei Chen, and Zhengbo Li

The dispersion curves of surface waves have been widely used for the retrieval of subsurface structures. Because the surface-wave dispersion is not sensitive to Vp, classical dispersion inversion can only retrieve Vs structures. To retrieve Vp, the dispersion of guided-P waves, which belong to leaky waves, should be considered. Due to the difficulty in forward modeling, the quantitative analysis of the leaky-wave dispersion curves has been rarely reported. In this study, we first derive the sensitivity analysis method of the leaky-wave dispersion based on previously proposed the semi-analytical spectral element method. Then the quantitative sensitivity analysis of leaky-wave dispersion curves is carried out, which confirms the ability of guided-P wave dispersion to constrain the velocity structures. With the theoretical analysis, we propose a joint inversion method based on surface and guided-P wave dispersion curves, which can simultaneously retrieve Vp and Vs. To verify the effectiveness, the proposed joint inversion has been applied to different kinds of field data including ocean bottom seismometer data with active sources and the seismic data of Nevada in the United States in 2008. Both of the inversion tests show that the joint inversion of surface- and leaky-wave dispersion can effectively constrain the velocity structure of Vp and Vs at the same time, which helps to obtain more complete and accurate models than the traditional surface wave dispersion inversion.

How to cite: Shi, C., Chen, X., and Li, Z.: Constraining Vp and Vs structures using the dispersion of surface and leaky waves, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-15191, https://doi.org/10.5194/egusphere-egu24-15191, 2024.

X1.108
|
EGU24-7360
Enhancing Dispersion Imaging with the Frequency-Bessel Method Using the Kolmogorov-Smirnov Subarry Partition Test: A Case Study of SGB Dense Array
(withdrawn)
Shuhao Song and Xiaofei Chen
X1.109
|
EGU24-11360
Antonio Schettino, Annalisa Ghezzi, and Luca Tassi

Classical analysis of radar profiles generally relies on a visual inspection and interpretation of profiles and sometimes on inverse modelling of the acquired data. Both methods suffer severe limitations due to the antenna resolution, thereby preventing the identification of tiny structures, especially in forensic applications. Here we describe a forward modelling technique, which allows to reproduce individual traces (A-scans) of radar profiles through superposition of Ricker wavelets. The method allows to detect ultra-thin layers, well beyond the Ricker and Rayleigh vertical resolution of GPR antennas. This approach starts from an estimation of the instrumental uncertainty of common monostatic antennas and takes into account of the frequency-dependent attenuation, which causes spectral shift of the dominant frequency acquired by the receiver antenna. The forward modelling procedure loads a single trace from a radar profile and allows to build a synthetic A-scan by fitting a sequence of Ricker wavelets with user-defined amplitude, polarity, and arrival time to the acquired trace. The resulting synthetic trace can be used to create a reflectivity diagram that plots reflection amplitudes and polarities versus depth. Often a reflectivity diagram shows intervals bounded by reflectors of opposite polarity, associated with layers having higher or lower velocity than the surrounding material, respectively. These intervals may result from very subtle features that represent interesting survey targets, for example buried bones, small cracks, thin lens of liquid contaminants, etc. and could be confused with individual reflectors through the simple visual inspection of a radar profile. Our quantitative approach can be used in several applications of GPR methods, especially in forensic, paleontological, civil engineering, heritage protection, and soil stratigraphy applications.

How to cite: Schettino, A., Ghezzi, A., and Tassi, L.: Trace Modelling: A Quantitative Approach to the Interpretation of Ground Penetrating Radar Profiles, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-11360, https://doi.org/10.5194/egusphere-egu24-11360, 2024.

Posters virtual: Wed, 17 Apr, 14:00–15:45 | vHall X1

Display time: Wed, 17 Apr, 08:30–Wed, 17 Apr, 18:00
vX1.9
|
EGU24-4659
|
ECS
ran cheng

In seismic exploration, three-dimensional near-surface tomography is key to solving complex statics problem and is an important prerequisite for migration imaging. To this end, this paper starts with the principles of ray tracing theory and tomographic inversion methods. Based on a comprehensive comparative analysis of the advantages and disadvantages of traditional ray tracing methods and numerical algorithms for tomographic inversion, using the first arrival times in three-dimensional seismic data, a high-precision three-dimensional ray tracing method based on multi-retracing technology and a tomographic inversion method constrained by prior information such as small refraction and micro logging throughout the process are proposed. First, this paper use near-surface survey information such as micro logging and small refraction to constrain the establishment of an initial velocity model and constrain tomographic inversion to improve the vertical inversion accuracy of the model. Secondly, to address the loss of shallow layer information due to excessive shot-to-detector distances, this paper introduces a virtual detector point technique. By adding one or more virtual detector points between known shot points and detector points within a close offset range, the density of rays at near offsets is increased, thereby improving the lateral tomographic imaging accuracy of the near-surface. At the same time, various constraints are introduced during the inversion process, including the range of velocity restriction, inversion slowness correction size constraints, internal iteration number constraints of tomographic inversion, dual-grid inversion, velocity extrapolating and smoothing, etc., greatly improving the accuracy of inversion and the quality of tomographic imaging. Given the large computational volume of three-dimensional data and the high memory consumption of large sparse matrices, this paper employs compressed storage and tomographic matrix solving techniques, greatly saving memory space and enhancing computational efficiency. The test results on theoretical models and actual data show that the ray tracing method used in this paper provides essentially correct ray propagation paths, consistent with geological laws. The final inversion results effectively reveal the velocity and thickness of near-surface low-speed layers and deceleration layers, demonstrating the correctness and effectiveness of the inversion method proposed in this paper.

Keywords: Velocity modeling, Ray tracing, Tomographic inversion, Micro logging, Small refraction

How to cite: cheng, R.: Method for near-surface three-dimensional velocity modeling based on first-arrival, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-4659, https://doi.org/10.5194/egusphere-egu24-4659, 2024.

vX1.10
|
EGU24-8505
|
ECS
Preliminary investigation of earth dam using multiple geophysical imaging techniques
(withdrawn)
Eslam Roshdy, Mariusz Majdański, Artur Marciniak, Szymon Oryński, Paweł Popielski, Sebastian Kowalczyk, Radosław Mieszkowski, Justyna Cader, Zygmunt Trześniowski, and Ireneusz Ostrzołek