Startseite Geologie und Mineralogie Detection of objects with diverse geometric shapes in GPR images using deep-learning methods
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Detection of objects with diverse geometric shapes in GPR images using deep-learning methods

  • Orhan Apaydın EMAIL logo und Turgay İşseven
Veröffentlicht/Copyright: 10. Oktober 2024
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Abstract

Buried objects with regular geometric shapes appear as hyperbolic structures in ground-penetrating radar (GPR) images. The shapes of these hyperbolic structures differ depending on the geometric shapes of the objects. In this study, current deep learning-based object detection algorithms such as Faster R-CNN, YOLOv5, and single-shot detector are used to detect hyperbolic structures in GPR images and classify the buried object according to its geometric shape. A mixed data set is produced for training the models. A GPR measurement device is designed with a vector network analyzer and Vivaldi antenna pair to be used in laboratory measurements. Objects with rectangular and cylindrical geometric shapes are placed under the table and measurements are performed. The measurement scenarios created in the laboratory are modeled in the gprMax program and synthetic GPR data are produced. Data augmentation techniques such as flipping and resizing are applied to expand the data set. As a result of the training, three models successfully detect the objects and classify them according to their geometric shapes. The Faster R-CNN model gives the most accurate detection and classification with the metrics classification loss = 5.4 × 10−3, localization loss = 9 × 10−3, regularization loss = 5.1 × 10−5, mAP@0.5 = 1, and mAP@0.5:0.95 = 1.

1 Introduction

Ground-penetrating radar (GPR) is a non-destructive geophysical exploration method used in near-surface investigations [1,2]. It is frequently used for detecting and positioning objects buried in the subsurface, such as mines, water pipes, and graves [3,4]. Object detection and classification in GPR images can be implemented using deep learning-based methods [5,6,7,8,9,10,11,12,13,14,15,16,17,18,19,20,21,22,23]. Three of these methods are Faster R-CNN, You Only Look Ones (YOLOv5), and single-shot detector (SSD). These techniques are capable of detecting multiple objects in an image and accurately presenting them within bounding boxes. Near-surface buried objects appear as hyperbola in GPR images. Rectangular and cylindrical-shaped objects create variations in the hyperbolic structures within GPR images. In this study, we investigate the detection and classification of objects with diverse geometric shapes in GPR images. The dataset includes radargrams obtained from real measurements collected by a radar system consisting of a vector network analyzer (VNA) and Vivaldi antenna pair in a laboratory environment, as well as synthetic radargrams created in the gprMax program. Rectangular-shaped aluminum box and cylindrical-shaped iron bar areplaced beneath the table, and GPR measurements are performed. The hyperbolic structures of these objects are detected in GPR images, and it is found that the object is either rectangular or cylindrical. Thus, the studies in the literature have been extended in terms of detecting different geometric-shaped structures in GPR images.

2 Methods

2.1 Faster R-CNN

Most of the object detection algorithms are based on the CNN method [24]. CNN is one of the most popular feature extraction methods according to its remarkable successful results. In a simple CNN structure, it includes a convolution layer, a pooling layer, and a flattening layer [25]. Region-based CNN (R-CNN) is introduced by Girshick et al. [26] to get better results in object detection. In the first step of R-CNN, object proposals are produced by using selective search (SS). In the second step, possible object areas within each proposal are transformed into a feature vector and then passed to a classifier and also to a regressor. Since these operations are performed for each proposal, it causes an intense computational cost [7]. To overcome this problem, SSPnet and Fast R-CNN recommend that all input images pass through CNN once. Ren et al. [27] introduced the Faster R-CNN object detection method, which is based on R-CNN. Faster R-CNN uses the region proposal network (RPN) instead of SS. RPN makes the Faster R-CNN’s performance better than models that use SS because of the most accurate results and fast algorithm speed [11]. Faster R-CNN consists of two main parts (Figure 1): (1) an RPN that extracts information about the possible locations of objects and (2) the Fast R-CNN network where the object is classified and bounding boxes are found. These two parts work as a whole by sharing their parameters. In the classification part, it will output that if the confidence score is greater than 0.7, it is an object, and if it is less than this value, it is not an object.

Figure 1 
                  Network architecture of Faster R-CNN. There are two learnable stages: region proposal network and classification network.
Figure 1

Network architecture of Faster R-CNN. There are two learnable stages: region proposal network and classification network.

In this study, the Faster R-CNN method is applied using TensorFlow Object detection API. Parameters used in network training are tuned as Epoch = 10,000, learning tare = 1 × 10−2, and batch size = 3.

2.2 YOLOv5

Another network mostly used for object detection is YOLO (You Only Look Once) [28]. YOLO is a CNN-based method. YOLOv5 is the fifth version of YOLO [29]. Multiple objects in an image can be detected by using YOLOv5. This method works with faster training and inference time than other detection networks like SSD and Faster R-CNN and makes it more suitable for real-time applications [30]. However, in addition to its fast work, its accuracy rates in detecting small-size objects including handicaps when compared to other object detection methods.

The main idea of the method is to use the whole picture as input data and pass it through the network to generate bounding boxes containing five predictions: x, y, w, h, and confidence values. While the (x, y) coordinates from the estimates describe the center of the boxes according to the grid cell, the width and heightarerelative values to the whole image [28,30,31].

In the method, the image is divided into S × S grid cells and CNN is performed in each region. A confidence score is issued indicating whether the regions contain objects. Generally, it is best if the confidence score is equal to the point of IOU between the predicted box and the ground truth. Each grid cell contains B bounding boxes which have a class probability (C). All predictions are encoded as an S × S × (B × 5 × C) size tensor [28].

The YOLOv5 consists of three main blocks (Figure 2): (1) “Backbone,” part of feature extraction with CNN, (2) “Neck,” at this stage aggregation of image features is performed, and (3) "Head" section, the object detection predictions are made and the results are shown from these predictions [5].

Figure 2 
                  Network architecture of YOLOv5.
Figure 2

Network architecture of YOLOv5.

Hyperparameters used in YOLOv5 network training are tuned as Epoch = 210, learning rate = 1 × 10−2, and batch size = 4.

2.3 SSD

Unlike traditional methods that require multiple passes through an image, SSD performs object detection in a single shot, thanks to its innovative architecture (Figure 3). By utilizing a combination of 1 × 1 and 3 × 3 filters, SSD generates feature maps essential for detecting objects of various sizes and shapes [32,33]. Furthermore, the SSD algorithm incorporates the MultiBox technique, which involves utilizing predefined bounding boxes placed over actual regions within an image. By segmenting the image into grids of varying sizes, SSD effectively detects both large and small objects, enhancing its versatility. Each predicted bounding box is assigned a confidence score for label prediction, with the highest-scoring box being selected.

Figure 3 
                  SSD model architecture.
Figure 3

SSD model architecture.

This process is facilitated by multi-scale feature maps, where convolutional layers of different cell sizes are employed to detect objects across various scales. To train the SSD model, the TensorFlow Object Detection API with the Resnet50 base model is utilized. The training parameters are carefully configured, with a batch size of 3, a learning rate of 1 × 10−4, and 3,000 epochs.

3 Dataset

In this section, the dataset used in object detection algorithms Faster R-CNN, YOLOv5, and SSD is explained. Dataset has a major role in object detection models. The dataset used in this study consists of measurements performed in the laboratory environment and simulated data created by using gprMax. To increase the variety of the dataset and the accuracy of the algorithms, data augmentation is performed with flipping and image resizing methods. The dataset information used in similar object detection studies in the literature is given in Table 1.

Table 1

Dataset information in the literature and this study

GPR object detection studies Total gprMax Lab and field Train Valid. Test
Lei et al. [7] 5,866 5,236 630
Kumlu [10] 55 55 40 10 5
Dewantara and Parnadi [12] 80 78 2 72 8
Kafedziski et al. [17] 157
Pham and Lefèvre [18] 150 50 100
Cui et al. [9] 3,000 2,100 600 300
Xiao et al. [11] 4,688 3,281 1,407
Gong and Zhang [8] 200 200 160 40
In this study 357 300 57 249 72 36

3.1 Laboratory measurements

In the laboratory environment, measurements are performed with a GPR system using a Copper Mountain TR/1,300 brand and model VNA and Vivaldi antenna pair that can operate at the appropriate frequency for measurements. In measurements, cylindrical and rectangular objects are placed beneath the table at different depths (Figure 4).

Figure 4 
                  Laboratory measurement setup: (a) rectangular shape and (b) cylindrical shape object.
Figure 4

Laboratory measurement setup: (a) rectangular shape and (b) cylindrical shape object.

The frequency band of the VNA device used for the measurements is 600–1,300 MHz, the center frequency is 950 MHz, the number of data points in an A-scan is 1,000, the measurement intervals are 2 cm, the total measurement length is 120 cm, and the GPR data length is 20 ns. The depth of the targets from the table varies between 5 and 30 cm. A total of 19 GPR data are collected for 10 rectangular objects (boxes) and 9 cylindrical objects (iron pipes). Attention has been given to enhancing the electromagnetic reflectivity of objects by using metallic materials. To make the hyperbolas of the box more visible in GPR images, it is covered with aluminum foil with high electromagnetic reflectivity. As seen in Figure 5, the hyperbolas formed by the box and the iron bar in the GPR images exhibit distinct differences.

Figure 5 
                  GPR images of (a) rectangular and (b) cylindrical objects.
Figure 5

GPR images of (a) rectangular and (b) cylindrical objects.

Due to the flat surface on the top of the rectangular-shaped box, the apex of the hyperbola it forms is also planar. In contrast, the interaction area on the cylindrical pipe is much narrower, and as a result, this flat area is not visible at the top of its hyperbola.

3.2 Synthetic data

To expand the dataset, synthetic GPR images are generated through simulation. The gprMax program, capable of simulating electromagnetic waves by solving Maxwell’s equations using the finite difference time domain method [34,35], is used to generate synthetic data. It is essential to emphasize that the inclusion of additional simulated data can lead to more accurate and reliable detection results, marked by an increase in successful detections and a reduction in false alarms. This observation supports the scheme’s intended purpose and affirms its effectiveness [18].

The Vivaldi antennas used in the measurements are modeled in the gprMax program with the same size and material properties as the reality and used in the simulation to obtain the closest results to the data obtained in laboratory measurements. The table, aluminum-covered box, and iron bar used in laboratory measurements are modeled similarly and used in the simulation (Figure 6).

Figure 6 
                  Simulation setup in gprMax: (a) rectangular shape aluminum covered box and (b) cylindrical shape iron pipe.
Figure 6

Simulation setup in gprMax: (a) rectangular shape aluminum covered box and (b) cylindrical shape iron pipe.

The center frequency (950 MHz), measurement interval (2 cm), measurement line length (120 cm), and depth values of the objects (5–30 cm) used in the simulation are the same as the values used in laboratory measurements. A total of 100 synthetic GPR images are created. The pixel values of GPR images are 250 × 1,000. An example of a simulation GPR image of the box and the cylinder is shown in Figure 7.

Figure 7 
                  Synthetic GPR images of (a) rectangular and (b) cylindrical objects.
Figure 7

Synthetic GPR images of (a) rectangular and (b) cylindrical objects.

Similar to the laboratory measurements, the hyperbolic shape anomalies of the aluminum-covered box and the iron bar are obtained differently from each other. Additionally, the waveforms of hyperbolas resemble the waveforms obtained in the laboratory measurements.

3.3 Data augmentation

Data augmentation is generally applied in object detection applications to increase detection accuracy, with resizing and flipping being the most well-known and commonly used techniques. The input image of 250 × 1,000 is set to 300 × 1,000 by using resizing. Figure 8 shows a GPR image that has been flipped and resized.

Figure 8 
                  (a) Original GPR image, (b) flipped, and (c) resized GPR images.
Figure 8

(a) Original GPR image, (b) flipped, and (c) resized GPR images.

As a result of augmentation, the total number of laboratory and simulation GPR data increased from 119 to 357 images. The dataset is distributed as 70% for training, 20% for validation, and 10% for testing. The dataset includes two classes, one of which is ‘cylindrical’ with 183 instances, and the other one is ‘rectangular’ with 174 instances.

4 Results and discussion

The Faster R-CNN application is configured with epoch = 10,000, batch size = 3, learning rate = 1 × 10−2, and the training took 68 min. At the end of the training, the mAP@0.5 and mAP@0.75 values are obtained as 1, and the training classification loss, localization loss, and regularization loss values are obtained as 5.4 × 10−3, 9 × 10−3, and 5.1 × 10−5 respectively. We tested the trained model with confidence >0.7. As can be seen in Figure 9(a)–(c), the values giving the lowest loss values are selected in the hyperparameter test performed to select the training parameters of the Faster RCNN application.

Figure 9 
               Results of the hyperparameter test to determine the parameters to be used in Faster RCNN, YOLOv5, and SSD training. The tests are carried out using four different batch sizes and three different learning rates. (a, d, and g) Classification losses, (b, e, and h) localization losses, (c and i) regularization losses, and (f) objectness loss results.”
Figure 9

Results of the hyperparameter test to determine the parameters to be used in Faster RCNN, YOLOv5, and SSD training. The tests are carried out using four different batch sizes and three different learning rates. (a, d, and g) Classification losses, (b, e, and h) localization losses, (c and i) regularization losses, and (f) objectness loss results.”

In the YOLOv5 application, the epoch is set to 210, batch size to 4, and learning rate to 1 × 10−5. The training process took 9.84 min in total. At the end of the YOLOv5 training, the mAP@0.5 and mAP@0.5:0.95 values are obtained as 0.995 and 0.779, respectively, and the classification loss, localization loss, and objectness loss values are obtained as 1.9 × 10−3, 1.5 × 10−2, and 7.2 × 10−3, respectively.

The third network, SSD, is trained with these tuned configuration parameters: epoch = 3,000, batch size = 3, learning rate = 1 × 10−4, and the training took 17 min. The mAP@0.5 and mAP@0.75 values are obtained as 1 and 0.79, respectively. The training classification loss, localization loss, and regularization loss values are obtained as 2.1 × 10−1, 9.4 × 10−3, and 1.9 × 10−1, respectively. The regularization loss of the SSD method (Figure 10(i)) decreased in a different trend compared to the graphs of other models due to the simple structure of the model. Although a similar pattern of regularization loss decrease was observed in the [36] study, the detection results were successful.

Figure 10 
               Train and validation loss values obtained in each epoch as a result of Faster RCNN, YOLOv5, and SSD training. (a, d, and g) Localization losses, (b, e, and h) classification losses, (c and i) regularization losses, and (f) objectness loss results.
Figure 10

Train and validation loss values obtained in each epoch as a result of Faster RCNN, YOLOv5, and SSD training. (a, d, and g) Localization losses, (b, e, and h) classification losses, (c and i) regularization losses, and (f) objectness loss results.

For all three methods, the training and validation loss values decreased smoothly at each epoch throughout the training process (Figure 10). Recall, precision, and F1-score metrics and detection times are given in Table 2.

Table 2

The performance metrics and detection times of Faster R-CNN, YOLOv5, and SSD

Networks Geometrical shape Precision (%) Recall (%) F1 score (%) Detection time (s)
Faster R-CNN Rectangular 100.0 100.0 100.0 2.2
Cylindrical 100.0 100.0 100.0
YOLOv5 Rectangular 70.6 100.0 82.8 0.0028
Cylindrical 82.6 94.8 88.3
SSD Rectangular 74.1 58.9 65.6 1.9
Cylindrical 62.7 77.1 69.2

In this study, hyperbolas are detected and classified based on the geometric shapes of the objects in GPR images with high accuracy rates. Both Faster R-CNN and YOLOv5 give successful results for detection and classification, but SSD has bad performance scores (Figure 11). YOLOv5 is more suitable for real-time detection applications with 2.8 ms detection time. Faster R-CNN, with its high accuracy detection performance, can be used to detect objects in the radargrams obtained after the GPR applications.

Figure 11 
               Some object detection and classification test results in GPR images of (a) Faster R-CNN, (b) YOLOv5, and (c) SSD models. Models output detected and classified objects with a bounding box and confidence score in percentage.
Figure 11

Some object detection and classification test results in GPR images of (a) Faster R-CNN, (b) YOLOv5, and (c) SSD models. Models output detected and classified objects with a bounding box and confidence score in percentage.

In studies [6,7,10,11,12,13,14,15,16], hyperbolas of objects in GPR images are detected and not classified by using only one of the Faster R-CNN and YOLOv5 methods [8]. It successfully detected objects with different geometric shapes, but the model used in the training is Faster R-CNN and the dataset does not consist of laboratory or field data, but only synthetic data. In this study, Faster R-CNN, YOLOv5, and SSD methods are tested separately to find out which method gave better results for detection and classification.

Acknowledgments

We would like to thank Prof. Dr. Selçuk Paker for his ideas and support in laboratory measurements and Prof. Dr. Işın Erer for providing the GPR device.

  1. Funding information: Authors state no funding involved.

  2. Author contributions: Orhan Apaydın: writing – original draft preparation, software visualization, data curation, formal analysis, methodology. Turgay Işseven: conceptualization, methodology, project administration, validation.

  3. Conflict of interest: Authors state no conflict of interest.

  4. Data availability statement: The datasets generated and/or analyzed during the current study are available from the corresponding author upon reasonable request.

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Received: 2023-11-10
Revised: 2024-04-29
Accepted: 2024-06-03
Published Online: 2024-10-10

© 2024 the author(s), published by De Gruyter

This work is licensed under the Creative Commons Attribution 4.0 International License.

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  26. Permian tectonic switch of the southern Central Asian Orogenic Belt: Constraints from magmatism in the southern Alxa region, NW China
  27. Element geochemical differences in lower Cambrian black shales with hydrothermal sedimentation in the Yangtze block, South China
  28. Three-dimensional finite-memory quasi-Newton inversion of the magnetotelluric based on unstructured grids
  29. Obliquity-paced summer monsoon from the Shilou red clay section on the eastern Chinese Loess Plateau
  30. Classification and logging identification of reservoir space near the upper Ordovician pinch-out line in Tahe Oilfield
  31. Ultra-deep channel sand body target recognition method based on improved deep learning under UAV cluster
  32. New formula to determine flyrock distance on sedimentary rocks with low strength
  33. Assessing the ecological security of tourism in Northeast China
  34. Effective reservoir identification and sweet spot prediction in Chang 8 Member tight oil reservoirs in Huanjiang area, Ordos Basin
  35. Detecting heterogeneity of spatial accessibility to sports facilities for adolescents at fine scale: A case study in Changsha, China
  36. Effects of freeze–thaw cycles on soil nutrients by soft rock and sand remodeling
  37. Vibration prediction with a method based on the absorption property of blast-induced seismic waves: A case study
  38. A new look at the geodynamic development of the Ediacaran–early Cambrian forearc basalts of the Tannuola-Khamsara Island Arc (Central Asia, Russia): Conclusions from geological, geochemical, and Nd-isotope data
  39. Spatio-temporal analysis of the driving factors of urban land use expansion in China: A study of the Yangtze River Delta region
  40. Selection of Euler deconvolution solutions using the enhanced horizontal gradient and stable vertical differentiation
  41. Phase change of the Ordovician hydrocarbon in the Tarim Basin: A case study from the Halahatang–Shunbei area
  42. Using interpretative structure model and analytical network process for optimum site selection of airport locations in Delta Egypt
  43. Geochemistry of magnetite from Fe-skarn deposits along the central Loei Fold Belt, Thailand
  44. Functional typology of settlements in the Srem region, Serbia
  45. Hunger Games Search for the elucidation of gravity anomalies with application to geothermal energy investigations and volcanic activity studies
  46. Addressing incomplete tile phenomena in image tiling: Introducing the grid six-intersection model
  47. Evaluation and control model for resilience of water resource building system based on fuzzy comprehensive evaluation method and its application
  48. MIF and AHP methods for delineation of groundwater potential zones using remote sensing and GIS techniques in Tirunelveli, Tenkasi District, India
  49. New database for the estimation of dynamic coefficient of friction of snow
  50. Measuring urban growth dynamics: A study in Hue city, Vietnam
  51. Comparative models of support-vector machine, multilayer perceptron, and decision tree ‎predication approaches for landslide ‎susceptibility analysis
  52. Experimental study on the influence of clay content on the shear strength of silty soil and mechanism analysis
  53. Geosite assessment as a contribution to the sustainable development of Babušnica, Serbia
  54. Using fuzzy analytical hierarchy process for road transportation services management based on remote sensing and GIS technology
  55. Accumulation mechanism of multi-type unconventional oil and gas reservoirs in Northern China: Taking Hari Sag of the Yin’e Basin as an example
  56. TOC prediction of source rocks based on the convolutional neural network and logging curves – A case study of Pinghu Formation in Xihu Sag
  57. A method for fast detection of wind farms from remote sensing images using deep learning and geospatial analysis
  58. Spatial distribution and driving factors of karst rocky desertification in Southwest China based on GIS and geodetector
  59. Physicochemical and mineralogical composition studies of clays from Share and Tshonga areas, Northern Bida Basin, Nigeria: Implications for Geophagia
  60. Geochemical sedimentary records of eutrophication and environmental change in Chaohu Lake, East China
  61. Research progress of freeze–thaw rock using bibliometric analysis
  62. Mixed irrigation affects the composition and diversity of the soil bacterial community
  63. Examining the swelling potential of cohesive soils with high plasticity according to their index properties using GIS
  64. Geological genesis and identification of high-porosity and low-permeability sandstones in the Cretaceous Bashkirchik Formation, northern Tarim Basin
  65. Usability of PPGIS tools exemplified by geodiscussion – a tool for public participation in shaping public space
  66. Efficient development technology of Upper Paleozoic Lower Shihezi tight sandstone gas reservoir in northeastern Ordos Basin
  67. Assessment of soil resources of agricultural landscapes in Turkestan region of the Republic of Kazakhstan based on agrochemical indexes
  68. Evaluating the impact of DEM interpolation algorithms on relief index for soil resource management
  69. Petrogenetic relationship between plutonic and subvolcanic rocks in the Jurassic Shuikoushan complex, South China
  70. A novel workflow for shale lithology identification – A case study in the Gulong Depression, Songliao Basin, China
  71. Characteristics and main controlling factors of dolomite reservoirs in Fei-3 Member of Feixianguan Formation of Lower Triassic, Puguang area
  72. Impact of high-speed railway network on county-level accessibility and economic linkage in Jiangxi Province, China: A spatio-temporal data analysis
  73. Estimation model of wild fractional vegetation cover based on RGB vegetation index and its application
  74. Lithofacies, petrography, and geochemistry of the Lamphun oceanic plate stratigraphy: As a record of the subduction history of Paleo-Tethys in Chiang Mai-Chiang Rai Suture Zone of Thailand
  75. Structural features and tectonic activity of the Weihe Fault, central China
  76. Application of the wavelet transform and Hilbert–Huang transform in stratigraphic sequence division of Jurassic Shaximiao Formation in Southwest Sichuan Basin
  77. Structural detachment influences the shale gas preservation in the Wufeng-Longmaxi Formation, Northern Guizhou Province
  78. Distribution law of Chang 7 Member tight oil in the western Ordos Basin based on geological, logging and numerical simulation techniques
  79. Evaluation of alteration in the geothermal province west of Cappadocia, Türkiye: Mineralogical, petrographical, geochemical, and remote sensing data
  80. Numerical modeling of site response at large strains with simplified nonlinear models: Application to Lotung seismic array
  81. Quantitative characterization of granite failure intensity under dynamic disturbance from energy standpoint
  82. Characteristics of debris flow dynamics and prediction of the hazardous area in Bangou Village, Yanqing District, Beijing, China
  83. Rockfall mapping and susceptibility evaluation based on UAV high-resolution imagery and support vector machine method
  84. Statistical comparison analysis of different real-time kinematic methods for the development of photogrammetric products: CORS-RTK, CORS-RTK + PPK, RTK-DRTK2, and RTK + DRTK2 + GCP
  85. Hydrogeological mapping of fracture networks using earth observation data to improve rainfall–runoff modeling in arid mountains, Saudi Arabia
  86. Petrography and geochemistry of pegmatite and leucogranite of Ntega-Marangara area, Burundi, in relation to rare metal mineralisation
  87. Prediction of formation fracture pressure based on reinforcement learning and XGBoost
  88. Hazard zonation for potential earthquake-induced landslide in the eastern East Kunlun fault zone
  89. Monitoring water infiltration in multiple layers of sandstone coal mining model with cracks using ERT
  90. Study of the patterns of ice lake variation and the factors influencing these changes in the western Nyingchi area
  91. Productive conservation at the landslide prone area under the threat of rapid land cover changes
  92. Sedimentary processes and patterns in deposits corresponding to freshwater lake-facies of hyperpycnal flow – An experimental study based on flume depositional simulations
  93. Study on time-dependent injectability evaluation of mudstone considering the self-healing effect
  94. Detection of objects with diverse geometric shapes in GPR images using deep-learning methods
  95. Behavior of trace metals in sedimentary cores from marine and lacustrine environments in Algeria
  96. Spatiotemporal variation pattern and spatial coupling relationship between NDVI and LST in Mu Us Sandy Land
  97. Formation mechanism and oil-bearing properties of gravity flow sand body of Chang 63 sub-member of Yanchang Formation in Huaqing area, Ordos Basin
  98. Diagenesis of marine-continental transitional shale from the Upper Permian Longtan Formation in southern Sichuan Basin, China
  99. Vertical high-velocity structures and seismic activity in western Shandong Rise, China: Case study inspired by double-difference seismic tomography
  100. Spatial coupling relationship between metamorphic core complex and gold deposits: Constraints from geophysical electromagnetics
  101. Disparities in the geospatial allocation of public facilities from the perspective of living circles
  102. Research on spatial correlation structure of war heritage based on field theory. A case study of Jinzhai County, China
  103. Formation mechanisms of Qiaoba-Zhongdu Danxia landforms in southwestern Sichuan Province, China
  104. Magnetic data interpretation: Implication for structure and hydrocarbon potentiality at Delta Wadi Diit, Southeastern Egypt
  105. Deeply buried clastic rock diagenesis evolution mechanism of Dongdaohaizi sag in the center of Junggar fault basin, Northwest China
  106. Application of LS-RAPID to simulate the motion of two contrasting landslides triggered by earthquakes
  107. The new insight of tectonic setting in Sunda–Banda transition zone using tomography seismic. Case study: 7.1 M deep earthquake 29 August 2023
  108. The critical role of c and φ in ensuring stability: A study on rockfill dams
  109. Evidence of late quaternary activity of the Weining-Shuicheng Fault in Guizhou, China
  110. Extreme hydroclimatic events and response of vegetation in the eastern QTP since 10 ka
  111. Spatial–temporal effect of sea–land gradient on landscape pattern and ecological risk in the coastal zone: A case study of Dalian City
  112. Study on the influence mechanism of land use on carbon storage under multiple scenarios: A case study of Wenzhou
  113. A new method for identifying reservoir fluid properties based on well logging data: A case study from PL block of Bohai Bay Basin, North China
  114. Comparison between thermal models across the Middle Magdalena Valley, Eastern Cordillera, and Eastern Llanos basins in Colombia
  115. Mineralogical and elemental analysis of Kazakh coals from three mines: Preliminary insights from mode of occurrence to environmental impacts
  116. Chlorite-induced porosity evolution in multi-source tight sandstone reservoirs: A case study of the Shaximiao Formation in western Sichuan Basin
  117. Predicting stability factors for rotational failures in earth slopes and embankments using artificial intelligence techniques
  118. Origin of Late Cretaceous A-type granitoids in South China: Response to the rollback and retreat of the Paleo-Pacific plate
  119. Modification of dolomitization on reservoir spaces in reef–shoal complex: A case study of Permian Changxing Formation, Sichuan Basin, SW China
  120. Geological characteristics of the Daduhe gold belt, western Sichuan, China: Implications for exploration
  121. Rock physics model for deep coal-bed methane reservoir based on equivalent medium theory: A case study of Carboniferous-Permian in Eastern Ordos Basin
  122. Enhancing the total-field magnetic anomaly using the normalized source strength
  123. Shear wave velocity profiling of Riyadh City, Saudi Arabia, utilizing the multi-channel analysis of surface waves method
  124. Effect of coal facies on pore structure heterogeneity of coal measures: Quantitative characterization and comparative study
  125. Inversion method of organic matter content of different types of soils in black soil area based on hyperspectral indices
  126. Detection of seepage zones in artificial levees: A case study at the Körös River, Hungary
  127. Tight sandstone fluid detection technology based on multi-wave seismic data
  128. Characteristics and control techniques of soft rock tunnel lining cracks in high geo-stress environments: Case study of Wushaoling tunnel group
  129. Influence of pore structure characteristics on the Permian Shan-1 reservoir in Longdong, Southwest Ordos Basin, China
  130. Study on sedimentary model of Shanxi Formation – Lower Shihezi Formation in Da 17 well area of Daniudi gas field, Ordos Basin
  131. Multi-scenario territorial spatial simulation and dynamic changes: A case study of Jilin Province in China from 1985 to 2030
  132. Review Articles
  133. Major ascidian species with negative impacts on bivalve aquaculture: Current knowledge and future research aims
  134. Prediction and assessment of meteorological drought in southwest China using long short-term memory model
  135. Communication
  136. Essential questions in earth and geosciences according to large language models
  137. Erratum
  138. Erratum to “Random forest and artificial neural network-based tsunami forests classification using data fusion of Sentinel-2 and Airbus Vision-1 satellites: A case study of Garhi Chandan, Pakistan”
  139. Special Issue: Natural Resources and Environmental Risks: Towards a Sustainable Future - Part I
  140. Spatial-temporal and trend analysis of traffic accidents in AP Vojvodina (North Serbia)
  141. Exploring environmental awareness, knowledge, and safety: A comparative study among students in Montenegro and North Macedonia
  142. Determinants influencing tourists’ willingness to visit Türkiye – Impact of earthquake hazards on Serbian visitors’ preferences
  143. Application of remote sensing in monitoring land degradation: A case study of Stanari municipality (Bosnia and Herzegovina)
  144. Optimizing agricultural land use: A GIS-based assessment of suitability in the Sana River Basin, Bosnia and Herzegovina
  145. Assessing risk-prone areas in the Kratovska Reka catchment (North Macedonia) by integrating advanced geospatial analytics and flash flood potential index
  146. Analysis of the intensity of erosive processes and state of vegetation cover in the zone of influence of the Kolubara Mining Basin
  147. GIS-based spatial modeling of landslide susceptibility using BWM-LSI: A case study – city of Smederevo (Serbia)
  148. Geospatial modeling of wildfire susceptibility on a national scale in Montenegro: A comparative evaluation of F-AHP and FR methodologies
  149. Geosite assessment as the first step for the development of canyoning activities in North Montenegro
  150. Urban geoheritage and degradation risk assessment of the Sokograd fortress (Sokobanja, Eastern Serbia)
  151. Multi-hazard modeling of erosion and landslide susceptibility at the national scale in the example of North Macedonia
  152. Understanding seismic hazard resilience in Montenegro: A qualitative analysis of community preparedness and response capabilities
  153. Forest soil CO2 emission in Quercus robur level II monitoring site
  154. Characterization of glomalin proteins in soil: A potential indicator of erosion intensity
  155. Power of Terroir: Case study of Grašac at the Fruška Gora wine region (North Serbia)
  156. Special Issue: Geospatial and Environmental Dynamics - Part I
  157. Qualitative insights into cultural heritage protection in Serbia: Addressing legal and institutional gaps for disaster risk resilience
Heruntergeladen am 28.12.2025 von https://www.degruyterbrill.com/document/doi/10.1515/geo-2022-0685/html
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