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Search Results (161)

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24 pages, 11349 KiB  
Article
Multi-Size Voxel Cube (MSVC) Algorithm—A Novel Method for Terrain Filtering from Dense Point Clouds Using a Deep Neural Network
by Martin Štroner, Martin Boušek, Jakub Kučera, Hana Váchová and Rudolf Urban
Remote Sens. 2025, 17(4), 615; https://doi.org/10.3390/rs17040615 - 11 Feb 2025
Viewed by 336
Abstract
When filtering highly rugged terrain from dense point clouds (particularly in technical applications such as civil engineering), the most widely used filtering approaches yield suboptimal results. Here, we proposed and tested a novel ground-filtering algorithm, a multi-size voxel cube (MSVC), utilizing a deep [...] Read more.
When filtering highly rugged terrain from dense point clouds (particularly in technical applications such as civil engineering), the most widely used filtering approaches yield suboptimal results. Here, we proposed and tested a novel ground-filtering algorithm, a multi-size voxel cube (MSVC), utilizing a deep neural network. This is based on the voxelization of the point cloud, the classification of individual voxels as ground or non-ground using surrounding voxels (a “voxel cube” of 9 × 9 × 9 voxels), and the gradual reduction in voxel size, allowing the acquisition of custom-level detail and highly rugged terrain from dense point clouds. The MSVC performance on two dense point clouds, capturing highly rugged areas with dense vegetation cover, was compared with that of the widely used cloth simulation filter (CSF) using manually classified terrain as the reference. MSVC consistently outperformed the CSF filter in terms of the correctly identified ground points, correctly identified non-ground points, balanced accuracy, and the F-score. Another advantage of this filter lay in its easy adaptability to any type of terrain, enabled by the utilization of machine learning. The only disadvantage lay in the necessity to manually prepare training data. On the other hand, we aim to account for this in the future by producing neural networks trained for individual landscape types, thus eliminating this phase of the work. Full article
(This article belongs to the Special Issue New Perspectives on 3D Point Cloud (Third Edition))
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Figure 1
<p>A 2D illustration of the point cloud (profile) and its voxelization to 2 × 2 × 2 m voxels. Individual dots represent the centers of the voxels, color-coded to represent the number of points in the voxel (see the color bar). The central red square indicates the evaluated voxel, and the large orange square indicates the entire area used for its evaluation (2D representation of the voxel cube). (<b>a</b>) shows the overall view, (<b>b</b>) detail.</p>
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<p>A 2D illustration of the progressive reduction in vegetation with a gradual reduction in the voxel size (color-coding indicates the number of points in the voxel relative to the most populated voxel; grey indicates voxels with no points; and the greyed-out part of the point cloud indicates the points removed in previous steps). (<b>a</b>) A voxel size of 3.38 m; (<b>b</b>) A voxel size of 1.90 m; (<b>c</b>) A voxel size of 1.42 m; (<b>d</b>) A voxel size of 0.6 m.</p>
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<p>(<b>a</b>) The misclassification of voxels with low numbers of points (marked with red arrows) as non-ground and (<b>b</b>) the solution to this problem through the use of the additional shifted grid (blue lines); voxels classified as ground in any of the grids (thick lines) are considered ground and carried forward to the next step.</p>
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<p>Gradual filtering with stepwise reduction in the voxel size: (<b>a</b>) Original point cloud; (<b>b</b>) Step 2 (voxel size 4.5 m); (<b>c</b>) Step 5 (voxel size 1.9 m); (<b>d</b>) Step 15—final result (voxel size 0.11 m).</p>
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<p>Flowchart of the multi-size voxel cube (MSVC) algorithm.</p>
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<p>Data 1 with the vegetation color-coded according to the vegetation height: (<b>a</b>) Training data, (<b>b</b>) Test data; note that the training data contain all types of terrain as well as the vegetation character present in the test data.</p>
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<p>Data 2—training area (<b>a</b>,<b>b</b>) and the testing areas Boulders (<b>c</b>,<b>d</b>), Tower (<b>e</b>,<b>f</b>), and Rugged (<b>g</b>,<b>h</b>).</p>
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<p>Data 1—best classification results: (<b>a</b>) CSF (cloth resolution 2.5 cm; threshold 25 cm); (<b>b</b>) MSVC (voxel size 6 cm); (<b>c</b>) detail of the CSF classification; (<b>d</b>) detail of the same area classified by MSVC; the color-coded points indicate erroneously preserved vegetation, along with its height.</p>
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<p>Classification success for Data 2—Boulder: (<b>a</b>) CSF classification and (<b>b</b>) MSVC classification, with points erroneously classified as ground highlighted in red; (<b>c</b>) CSF classification, with points correctly identified by CSF but not by MSVC highlighted in green (<b>d</b>) MSVC classification, with points correctly identified by MSVC but not by CSF highlighted in green.</p>
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<p>Classification success for Data 2—Tower: (<b>a</b>) CSF classification and (<b>b</b>) MSVC classification, with points erroneously classified as ground highlighted in red; (<b>c</b>) CSF classification, with points correctly identified by CSF but not by MSVC highlighted in green (<b>d</b>) MSVC classification, with points correctly identified by MSVC but not by CSF highlighted in green. Blue ovals indicate areas with the biggest differences in the performance of the filters, where CSF identified more points falsely as ground.</p>
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<p>Classification success for Data 2—Rugged: (<b>a</b>) CSF classification and (<b>b</b>) MSVC classification, with points erroneously classified as ground highlighted in red; (<b>c</b>) CSF classification, with points correctly identified by CSF but not by MSVC highlighted in green (<b>d</b>) MSVC classification, with points correctly identified by MSVC but not by CSF highlighted in green. Colored ovals indicate areas with the biggest differences in the performance of the filters.</p>
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<p>The terrain model of the Data 2—Tower area with buildings shown; note that no buildings were present in the training data.</p>
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<p>Data 2—location of individual data in the area (<b>a</b>) Data 2 Training (<b>b</b>) Data 2 Boulders (<b>c</b>) Data 2 Tower (<b>d</b>) Data 2 Rugged.</p>
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26 pages, 13415 KiB  
Article
A Methodology for the Multitemporal Analysis of Land Cover Changes and Urban Expansion Using Synthetic Aperture Radar (SAR) Imagery: A Case Study of the Aburrá Valley in Colombia
by Ahmed Alejandro Cardona-Mesa, Rubén Darío Vásquez-Salazar, Juan Camilo Parra, César Olmos-Severiche, Carlos M. Travieso-González and Luis Gómez
Remote Sens. 2025, 17(3), 554; https://doi.org/10.3390/rs17030554 - 6 Feb 2025
Viewed by 550
Abstract
The Aburrá Valley, located in the northwestern region of Colombia, has undergone significant land cover changes and urban expansion in recent decades, driven by rapid population growth and infrastructure development. This region, known for its steep topography and dense urbanization, faces considerable environmental [...] Read more.
The Aburrá Valley, located in the northwestern region of Colombia, has undergone significant land cover changes and urban expansion in recent decades, driven by rapid population growth and infrastructure development. This region, known for its steep topography and dense urbanization, faces considerable environmental challenges. Monitoring these transformations is essential for informed territorial planning and sustainable development. This study leverages Synthetic Aperture Radar (SAR) imagery from the Sentinel-1 mission, covering 2017–2024, to propose a methodology for the multitemporal analysis of land cover dynamics and urban expansion in the valley. The novel proposed methodology comprises several steps: first, monthly SAR images were acquired for every year under study from 2017 to 2024, ensuring the capture of surface changes. These images were properly calibrated, rescaled, and co-registered. Then, various multitemporal fusions using statistics operations were proposed to detect and find different phenomena related to land cover and urban expansion. The methodology also involved statistical fusion techniques—median, mean, and standard deviation—to capture urbanization dynamics. The kurtosis calculations highlighted areas where infrequent but significant changes occurred, such as large-scale construction projects or sudden shifts in land use, providing a statistical measure of surface variability throughout the study period. An advanced clustering technique segmented images into distinctive classes, utilizing fuzzy logic and a kernel-based method, enhancing the analysis of changes. Additionally, Pearson correlation coefficients were calculated to explore the relationships between identified land cover change classes and their spatial distribution across nine distinct geographic zones in the Aburrá Valley. The results highlight a marked increase in urbanization, particularly along the valley’s periphery, where previously vegetated areas have been replaced by built environments. Additionally, the visual inspection analysis revealed areas of high variability near river courses and industrial zones, indicating ongoing infrastructure and construction projects. These findings emphasize the rapid and often unplanned nature of urban growth in the region, posing challenges to both natural resource management and environmental conservation efforts. The study underscores the need for the continuous monitoring of land cover changes using advanced remote sensing techniques like SAR, which can overcome the limitations posed by cloud cover and rugged terrain. The conclusions drawn suggest that SAR-based multitemporal analysis is a robust tool for detecting and understanding urbanization’s spatial and temporal dynamics in regions like the Aburrá Valley, providing vital data for policymakers and planners to promote sustainable urban development and mitigate environmental degradation. Full article
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<p>The Aburrá Valley (white line) between the valleys of the Magdalena and Cauca rivers. Data were acquired from ALOS PALSAR Terrain Corrected and data from IGAC.</p>
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<p>Region of interest (yellow bounding box) selected from the interior of the Aburrá Valley (red line) and the municipalities that are part of it (green lines). Data were acquired from IGAC.</p>
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<p>Proposed methodology for the multitemporal analysis <math display="inline"><semantics> <mrow> <mi>S</mi> <mi>M</mi> <msub> <mi>A</mi> <mn>1</mn> </msub> </mrow> </semantics></math>.</p>
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<p>Proposed methodology for kurtosis multitemporal analysis, <math display="inline"><semantics> <mrow> <mi>S</mi> <mi>M</mi> <msub> <mi>A</mi> <mn>2</mn> </msub> </mrow> </semantics></math>.</p>
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<p>Proposed methodology for analysis of zonal land cover changes.</p>
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<p>Samples of resulting images of the multitemporal analysis methodology proposed in <math display="inline"><semantics> <mrow> <mi>S</mi> <mi>M</mi> <msub> <mi>A</mi> <mn>1</mn> </msub> </mrow> </semantics></math> (<b>a</b>) <math display="inline"><semantics> <mrow> <mi>M</mi> <msub> <mi>F</mi> <mrow> <mi>M</mi> <mi>d</mi> <mi>n</mi> </mrow> </msub> </mrow> </semantics></math>, (<b>b</b>) <math display="inline"><semantics> <mrow> <mi>M</mi> <msub> <mi>F</mi> <mi>σ</mi> </msub> </mrow> </semantics></math>, (<b>c</b>) <math display="inline"><semantics> <mrow> <mi>M</mi> <msub> <mi>F</mi> <mi>M</mi> </msub> </mrow> </semantics></math>, (<b>d</b>) <math display="inline"><semantics> <mrow> <mi>M</mi> <msub> <mi>F</mi> <mrow> <mi>C</mi> <mi>V</mi> </mrow> </msub> </mrow> </semantics></math>, (<b>e</b>) <math display="inline"><semantics> <mrow> <mi>M</mi> <msub> <mi>F</mi> <mi>C</mi> </msub> </mrow> </semantics></math> for the year 2018, and (<b>f</b>) <math display="inline"><semantics> <mrow> <mi>M</mi> <msub> <mi>F</mi> <mi>K</mi> </msub> </mrow> </semantics></math> of <math display="inline"><semantics> <mrow> <mi>S</mi> <mi>M</mi> <msub> <mi>A</mi> <mn>2</mn> </msub> </mrow> </semantics></math> for 2017–2014. Scale, coordinate frame (grid), and north correspond to the region described in the Study area section.</p>
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<p>Areas of analysis of the results by the SMA1 methodological route and kurtosis. (<b>A</b>). Central Park in Bello (<b>B</b>). Parques del Río Medellín (<b>C</b>). Arkadia Shopping center; (<b>D</b>). Peldar Plant (<b>E</b>). La García water supply reservoir (<b>F</b>). Conasfaltos dam (<b>G</b>). La Ayurá stream basin in Envigado (<b>H</b>). Central Park in Bello (<b>I</b>). Avenida Regional Norte (<b>J</b>). Vía Distribuidora Sur.</p>
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<p>Side-by-side comparison of the Aburrá Valley. (<b>a</b>) Division into 9 geographical zones. (<b>b</b>) The corresponding correlation coefficients for 5 different land cover change types of the 9 zones.</p>
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<p>Color maps for every change class in the Aburrá Valley’s nine geographical zones.</p>
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21 pages, 1865 KiB  
Review
Sustainable Active Travel in Environmentally Challenging Cities: A Systematic Review of Barriers and Strategies
by Muhammad Tsaqif Wismadi, Yngve Karl Frøyen and Adil Rasheed
Sustainability 2025, 17(3), 1276; https://doi.org/10.3390/su17031276 - 5 Feb 2025
Viewed by 730
Abstract
Active travel modes, such as walking and cycling, are essential for fostering sustainable urban transportation. However, their adoption in environmentally challenging areas—characterised by steep slopes, extreme weather, and rugged terrain—presents significant obstacles. This study addresses these challenges by conducting a systematic literature review [...] Read more.
Active travel modes, such as walking and cycling, are essential for fostering sustainable urban transportation. However, their adoption in environmentally challenging areas—characterised by steep slopes, extreme weather, and rugged terrain—presents significant obstacles. This study addresses these challenges by conducting a systematic literature review of studies published between 2000 and 2024 to identify strategies that promote active travel in such contexts. Using a structured five-step methodology, 62 relevant articles were selected and analysed to explore common challenges and propose tailored solutions. The findings highlight critical barriers, including topographical difficulties, harsh climatic conditions, and adverse weather, all of which hinder walking and cycling. To address these barriers, this study identifies a range of solutions, including infrastructure enhancements such as bike lifts, e-bike systems, shaded walkways, and heated pavements, as well as policy measures like financial incentives and disincentive regulations. Importantly, this study makes a deliberate effort to avoid overgeneralised solutions by emphasising the need for interventions that are context-sensitive and tailored to specific environmental challenges, urban scales, and local conditions. By providing options for actionable strategies, this research offers a comprehensive foundation for developing inclusive and sustainable policies that encourage active travel in diverse and environmentally constrained urban settings. Full article
(This article belongs to the Section Sustainable Transportation)
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<p>The systematic framework of the literature review process.</p>
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<p>The systematic literature review search query based on PICON keywords.</p>
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<p>Pathway of selection in PRISMA diagram (red: excluded records, green: included records).</p>
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<p>Number of studies based on the travel mode.</p>
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<p>Number of studies based on the data type.</p>
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<p>The number of studies and geographical spreads based on the environmental challenge (bubble size represents the number of studies).</p>
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<p>The heatmap table of environmental challenge and intervention type.</p>
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<p>The boxplot of city population density against intervention type.</p>
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20 pages, 15815 KiB  
Article
Characterizing Surface Deformation of the Earthquake-Induced Daguangbao Landslide by Combining Satellite- and Ground-Based InSAR
by Xiaomeng Wang, Wenjun Zhang, Jialun Cai, Xiaowen Wang, Zhouhang Wu, Jing Fan, Yitong Yao and Binlin Deng
Sensors 2025, 25(1), 66; https://doi.org/10.3390/s25010066 - 26 Dec 2024
Viewed by 434
Abstract
The Daguangbao landslide (DGBL), triggered by the 2008 Wenchuan earthquake, is a rare instance of super-giant landslides globally. The post-earthquake evolution of the DGBL has garnered significant attention in recent years; however, its deformation patterns remain poorly characterized owing to the complex local [...] Read more.
The Daguangbao landslide (DGBL), triggered by the 2008 Wenchuan earthquake, is a rare instance of super-giant landslides globally. The post-earthquake evolution of the DGBL has garnered significant attention in recent years; however, its deformation patterns remain poorly characterized owing to the complex local topography. In this study, we present the first observations of the surface dynamics of DGBL by integrating satellite- and ground-based InSAR data complemented by kinematic interpretation using a LiDAR-derived Digital Surface Model (DSM). The results indicate that the maximum line-of-sight (LOS) displacement velocity obtained from satellite InSAR is approximately 80.9 mm/year between 1 January 2021, and 30 December 2023, with downslope displacement velocities ranging from −60.5 mm/year to 69.5 mm/year. Ground-based SAR (GB-SAR) enhances satellite observations by detecting localized apparent deformation at the rear edge of the landslide, with LOS displacement velocities reaching up to 1.5 mm/h. Our analysis suggests that steep and rugged terrain, combined with fragile and densely jointed lithology, are the primary factors contributing to the ongoing deformation of the landslide. The findings of this study demonstrate the effectiveness of combining satellite- and ground-based InSAR systems, highlighting their complementary role in interpreting complex landslide deformations. Full article
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<p>(<b>a</b>) The geographical location of the DGBL and the coverage of the SAR image. The rectangular window indicates the coverage of Sentinel-1 data, and the red pentagram marks the location of the DGBL. (<b>b</b>) The UAV equipped with the AU20 multi-platform laser scanning system is primarily used to collect external auxiliary data such as DSM and DOM. (<b>c</b>) Ground-based radar field monitoring site (from 15 October to 17 October 2024).</p>
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<p>Zoning map of DGBL based on satellite imagery. I1 represents the Northern Scarp Zone; I2 is the Rear Scarp Zone; and I3 is the Southern Scarp Zone. II1 and II2 correspond to the Baiguolin and Chuanlin Gully Barrier Lake Zones, respectively. II3 and II4 are the Huangdongzi and Menkanshi Gully Accumulation Zones. II5 represents the Main Accumulation Zone. III1 refers to the Secondary Slide Mass, while III2 is the Collapse Accumulation Zone.</p>
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<p>Aerial LiDAR remote sensing interpretation map of the DGBL. (<b>a</b>) High-resolution Digital Elevation Model (DEM). (<b>b</b>) Hillshade map, with red triangles indicating the locations of GB-SAR monitoring sites. (<b>c</b>) Slope map. (<b>d</b>) Aspect map.</p>
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<p>Data processing flow diagram.</p>
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<p>InSAR downslope displacement transformation model of landslide and SAR imaging geometry.</p>
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<p>Deformation rate along the LOS direction in the radar coordinate system. (<b>a</b>) LOS direction deformation of path 128 (ascending). (<b>b</b>) LOS direction deformation of path 62 (descending). The areas within the white rectangular frames highlight regions with significant deformation changes. II1 represents the Northern Scarp Zone, composed of dolomite and slate, with substantial rockfall deposits. II2 refers to a barrier lake formed by rock debris along the Chuanlin Gully. II3 is primarily composed of black limestone fragments, which flowed downward along the Huangdongzi Gully, forming an accumulation zone. II5 serves as the Main Accumulation Zone, functioning as the primary deposition site for landslide materials.</p>
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<p>(<b>a</b>) The DOM of the DGBL. (<b>b</b>) The LOS displacement rate map of the DGBL obtained from the GB-SAR data (negative values indicate that the ground surface is moving away from the sensor). The areas Z1, Z2, and Z4 are located in the northern fault scarp area. Z3 is a slope rock detritus area, with the lithology mainly consisting of gray-black limestone, which flows downward along the Menkanshi Gully to form an accumulation area. The triangle marks the location of the GB-SAR monitoring site.</p>
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<p>(<b>a</b>) Cumulative LOS displacement map of DGBL obtained from GB-SAR data. (<b>b</b>–<b>d</b>) Correspond to the deformation maps of regions I1, III1, and II4. I1 represents the Northern Scarp Zone, III1 represents the Secondary Slide Mass, and II4 represents the Menkanshi Gully Accumulation Zone. (<b>e</b>–<b>g</b>) Hillshaded Lidar DSM; red arrows indicate the maximum topographical gradient, and the white dashed line marks the gully boundary.</p>
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<p>Time series of LOS displacement of three feature points (T1–T3).</p>
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<p>(<b>a</b>) Ascending orbit annual downslope deformation rate. (<b>b</b>) Descending orbit annual downslope deformation rate (areas within rectangular frames indicate regions with significant deformation changes). (<b>c</b>–<b>e</b>) Hillshaded LiDAR DSM, with red arrows indicating the maximum topographical gradient. I1 represents the Northern Scarp Zone, while II2 corresponds to the Chuanlin Gully Barrier Lake Zone. II3 denotes the Huangdongzi Gully Accumulation Zone, and II5 represents the Main Accumulation Zone.</p>
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<p>(<b>a</b>) The Q1 and Q2 regions, which are located in areas of significant deformation. (<b>b</b>,<b>c</b>) Correspond to the deformation rate maps of Q1–Q2, respectively.</p>
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<p>GB-SAR rate plots for the Q1 and Q2 regions. The solid line in the figure represents the cumulative displacements of Q1 and Q2.</p>
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17 pages, 7698 KiB  
Article
An Analysis and Interpretation of Magnetic Data of the Qing-Chengzi Deposit in Eastern Liaoning (China) Area: Guide for Structural Identification and Mineral Exploration
by Jianyu Li, Jun Wang, Xiaohong Meng, Yuan Fang, Weichen Li and Shunong Yang
Minerals 2024, 14(12), 1272; https://doi.org/10.3390/min14121272 - 13 Dec 2024
Viewed by 606
Abstract
Qing-Chengzi (QCZ) is an important silver-gold mining area in the eastern part of the Northeast China Craton. The shallow minerals in this area are almost completely depleted, leading to a demand for exploration to find deeper, concealed deposits. However, due to the rugged [...] Read more.
Qing-Chengzi (QCZ) is an important silver-gold mining area in the eastern part of the Northeast China Craton. The shallow minerals in this area are almost completely depleted, leading to a demand for exploration to find deeper, concealed deposits. However, due to the rugged terrain, few high-precision ground surveys have been executed in this area, resulting in an insufficient understanding of the unexposed ores. To address this issue, this study implemented a high-precision ground magnetic survey to identify faults and potential rocks in this area. To achieve these goals, remanence was analyzed to reduce its adverse effect on processing. Then, lineament enhancement with directional derivatives was conducted on the pre-processed magnetic anomalies to highlight structural features. Based on the results, eight major and twenty-one minor faults were identified, among which three major faults correspond well to the known faults. Most of the major faults run N–S, and the others run NW/NE. Furthermore, 3D inversion was conducted to locate potential rocks. Our inversion results indicate that there are six hidden rocks in the underground, extending from a depth of a few hundred meters to no more than three km. Two of the rocks correspond well to the already mined areas. This study provides support for subsequent exploration in the QCZ area. Full article
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<p>Geological map of the study area (modified after Yang [<a href="#B13-minerals-14-01272" class="html-bibr">13</a>]; An et al., [<a href="#B2-minerals-14-01272" class="html-bibr">2</a>]). (<b>a</b>) Tectonic background of the North China Craton. The black rectangular box marks the Liaodong gold district. (<b>b</b>) Sketch map and main ore fields in the Liaodong Peninsula, including three main gold deposits. The research area is within the black circle (the detailed parts in (<b>a</b>)).</p>
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<p>Geological map of the QCZ ore-concentrated district showing the location of major deposits. (The area delimited by the black square is the research area of this article. The blue square is the QCZ lead–zinc mining area.).</p>
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<p>(<b>a</b>) Original magnetic anomaly map; (<b>b</b>) Upward continuation of (<b>a</b>) by 60 m; (<b>c</b>) Magnetic amplitude map; (<b>d</b>) Analytic signal map (use (<b>b</b>)); (<b>e</b>) Reduction to magnetic pole map; (<b>f</b>) Neural network stripping remanence anomaly map.</p>
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<p>Regional separation of the data in <a href="#minerals-14-01272-f003" class="html-fig">Figure 3</a>d. (<b>a</b>) Optimized filter spectrogram; (<b>b</b>) Low-frequency regional magnetic anomaly; (<b>c</b>) Mid frequency filter residual magnetic anomaly map.</p>
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<p>(<b>a</b>) Primary and secondary faults on the original magnetic anomaly map; (<b>b</b>) N–S directional derivative map; (<b>c</b>) NE–SW directional derivative.</p>
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<p>3D inversion map of rock masses and magnetic susceptibility (section depth = 180 m).</p>
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<p>Comparison of rock masses and original magnetic magnetic anomaly (<a href="#minerals-14-01272-f003" class="html-fig">Figure 3</a>a).</p>
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<p>Depth slices maps and east–west slices of rock mass ①–③ and its surrounding area.</p>
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15 pages, 3260 KiB  
Article
Comparative Analysis of CNNs and Vision Transformers for Automatic Classification of Abandonment in Douro’s Vineyard Parcels
by Danilo Leite, Igor Teixeira, Raul Morais, Joaquim J. Sousa and Antonio Cunha
Remote Sens. 2024, 16(23), 4581; https://doi.org/10.3390/rs16234581 - 6 Dec 2024
Viewed by 952
Abstract
The Douro Demarcated Region is fundamental to local cultural and economic identity. Despite its importance, the region faces the challenge of abandoned vineyard plots, caused, among other factors, by the high costs of maintaining vineyards on hilly terrain. To solve this problem, the [...] Read more.
The Douro Demarcated Region is fundamental to local cultural and economic identity. Despite its importance, the region faces the challenge of abandoned vineyard plots, caused, among other factors, by the high costs of maintaining vineyards on hilly terrain. To solve this problem, the European Union (EU) offers subsidies to encourage active cultivation, with the aim of protecting the region’s cultural and environmental heritage. However, monitoring actively cultivated vineyards and those that have been abandoned presents considerable logistical challenges. With 43,843 vineyards spread over 250,000 hectares of rugged terrain, control of these plots is limited, which hampers the effectiveness of preservation and incentive initiatives. Currently, the EU only inspects 5 per cent of farmers annually, which results in insufficient coverage to ensure that subsidies are properly used and vineyards are actively maintained. To complement this limited monitoring, organisations such as the Instituto dos Vinhos do Douro e do Porto (IVDP) use aerial and satellite images, which are manually analysed to identify abandoned or active plots. To overcome these limitations, images can be analysed using deep learning methods, which have already shown great potential in agricultural applications. In this context, our research group has carried out some preliminary evaluations for the automatic detection of abandoned vineyards using deep learning models, which, despite showing promising results on the dataset used, proved to be limited when applied to images of the entire region. In this study, a new dataset was expanded to 137,000 images collected between 2018 and 2023, filling critical gaps in the previous datasets by including greater temporal and spatial diversity. Subsequently, a careful evaluation was carried out with various DL models. As a result, the ViT_b32 model demonstrated superior performance, achieving an average accuracy of 0.99 and an F1 score of 0.98, outperforming CNN-based models. In addition to the excellent results obtained, this dataset represents a significant contribution to advancing research in precision viticulture, providing a solid and relevant basis for future studies and driving the development of solutions applied to vineyard monitoring in the Douro Demarcated Region. These advances not only improve efficiency in detecting abandoned plots, but also contribute significantly to optimising the use of subsidies in the region. Full article
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<p>Different vineyard planting systems. Patamares (<b>top left</b>), vertical planting (<b>top right</b>), terraces (<b>bottom left</b>), and naturally sloping planting (<b>bottom right</b>). Source: Instituto dos Vinhos do Douro e do Porto (IVDP).</p>
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<p>Examples of aerial images of active and abandoned vineyard plots. The upper part (<b>A</b>) shows active vineyards, with organised rows of vines and clear signs of cultivation. The lower part (<b>B</b>) shows examples of abandoned vineyards, characterised by vegetation and lack of maintenance [<a href="#B5-remotesensing-16-04581" class="html-bibr">5</a>,<a href="#B6-remotesensing-16-04581" class="html-bibr">6</a>].</p>
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<p>Pipeline of the image classification models of this work.</p>
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<p>Process of image extraction using a GIS polygon. The polygon shape is created to encompass the desired region of the image, and the software then extracts the image corresponding to the area defined by the mask (polygon).</p>
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<p>Confusion matrix for the ViT_b32 model using images resized to 384 × 384 pixels, showing the distribution of correct and incorrect classifications in the ‘Baresoil’, ‘NoVineyard’, and ‘Vineyard’ categories.</p>
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<p>Examples of images misclassified by the ViT-B32 model. Image (<b>A</b>) was classified as ‘Baresoil’ with 99% confidence, and image (<b>B</b>) with 81% confidence. Both were originally labelled as ‘Vineyard’.</p>
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14 pages, 3527 KiB  
Article
Enhanced Foot Proprioception Through 3-Minute Walking Bouts with Ultra-Minimalist Shoes on Surfaces That Mimic Highly Rugged Natural Terrains
by Andrea Biscarini, Andrea Calandra, Alberto Marcucci, Roberto Panichi and Angelo Belotti
Biomimetics 2024, 9(12), 741; https://doi.org/10.3390/biomimetics9120741 - 5 Dec 2024
Viewed by 1211
Abstract
The use of minimalist shoes can lead to enhanced foot somatosensory activation and postural stability but can also increase the incidence of overuse injuries during high-impact or prolonged activities. Therefore, it appears useful to explore new strategies that employ minimalist shoes to effectively [...] Read more.
The use of minimalist shoes can lead to enhanced foot somatosensory activation and postural stability but can also increase the incidence of overuse injuries during high-impact or prolonged activities. Therefore, it appears useful to explore new strategies that employ minimalist shoes to effectively facilitate the somatosensory activation of the foot while minimizing acute and cumulative joint stress and risk of injury. To this purpose, this study introduces a novel exercise paradigm: walking for three minutes in ultra-minimalist shoes on artificial flat surfaces designed to mimic highly rugged natural terrains. The activity of foot muscles and lumbar multifidus, pain perception level, and stabilometric parameters were recorded and analyzed to characterize the novel exercise, comparing it to walking barefoot or in conventional shoes on the same rugged surface. Compared to being barefoot, ultra-minimalist shoes effectively filter nociceptive stimuli from the rugged surface, while compared to conventional shoes, they enhance the somatosensory input supporting static stability. Walking with ultra-minimalist and conventional shoes yielded higher gastrocnemius activity and lower tibialis anterior and multifidus activity compared to barefoot walking. This study highlights a practical and safe framework for enhancing foot somatosensory activation and postural stability. The new intervention is suitable for people of all ages, requires minimal time commitment, and can be performed in controlled environments such as homes, gyms, and healthcare facilities. Full article
(This article belongs to the Section Biomimetic Design, Constructions and Devices)
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Graphical abstract

Graphical abstract
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<p>Ultra-minimalist FiveFingers<sup>®</sup> shoes used in the three walking trials (<b>a</b>). Rectangular rigid slabs (35 cm length, 20 cm width, 2 cm thickness) with small, irregularly shaped protrusions simulating rough natural terrain (<b>b</b>). The slabs were arranged in series to form a straight path 10 m long.</p>
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<p>Schematic diagram of the testing area.</p>
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<p>Flowchart showing the stages of the testing session.</p>
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<p>CoP mean velocity (<b>a</b>), equivalent radius (<b>b</b>), and longitudinal and transverse standard deviation (<b>c</b>) recorded during the stabilometric tests conducted before the walking trials and after each of the three walking trials (with conventional shoes, ultra-minimalist shoes, and barefoot). * Significant difference with the reference test (before walking trials).</p>
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<p>Mean level of tibialis anterior (<b>a</b>), gastrocnemius medialis (<b>b</b>), peroneus longus (<b>c</b>) and lumbar multifidus (<b>d</b>) muscle activation during the three walking trials (with conventional shoes, ultra-minimalist shoes, and barefoot). * <span class="html-italic">p</span> &lt; 0.05.</p>
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<p>Perceived regional pain in the plantar area of the foot during the three walking trials (conventional shoes, ultra-minimalist shoes, and barefoot), assessed using a 100 mm VAS scale. * <span class="html-italic">p</span> &lt; 0.001.</p>
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18 pages, 7848 KiB  
Article
Effects of Climate Change and Human Activities on Streamflow in Arid Alpine Water Source Regions: A Case Study of the Shiyang River, China
by Honghua Xia, Yingqing Su, Linshan Yang, Qi Feng, Wei Liu and Jian Ma
Land 2024, 13(11), 1961; https://doi.org/10.3390/land13111961 - 20 Nov 2024
Cited by 1 | Viewed by 776
Abstract
Climate change and human activities were identified as the primary drivers of streamflow in arid alpine regions. However, limitations in observational data have resulted in a limited understanding of streamflow changes in these water sources, which hinders efforts to adapt to ongoing climate [...] Read more.
Climate change and human activities were identified as the primary drivers of streamflow in arid alpine regions. However, limitations in observational data have resulted in a limited understanding of streamflow changes in these water sources, which hinders efforts to adapt to ongoing climate change and to formulate effective streamflow management policies. Here, we use the four main tributaries in the upper reach of the Shiyang River in China as a case study to investigate the long-term trends in streamflow within arid alpine water sources, quantifying the individual contributions of climate change and human activities to these changes. The findings revealed that temperatures and precipitation in arid alpine regions have risen over the past 40 years. Although the warming trend has been significant, it has slowed in recent years. Nevertheless, three-quarters of the rivers are experiencing a decline in streamflow. The land types within the watershed remain relatively stable, with land use and cover change (LUCC) primarily occurring in the Gulang River watershed. Climate change has significantly affected streamflow change in high and rugged terrains, with an influence exceeding 70%. For example, Jingta River showed an impact of 118.79%, Zamu River 84.00%, and Huangyang River 71.43%. Human-driven LUCC, such as the expansion of cultivated and urban land, have led to increased water consumption, resulting in reduced streamflow. This effect is particularly pronounced in the low-lying and gently undulating areas of the Gulang River, where LUCC account for 78.68% of the change in streamflow. As human activities intensify and temperatures continue to rise, further declines in streamflow are projected, highlighting the urgent need for effective water resource management. These insights highlight the urgent need for targeted mitigation and adaptation strategies to confront the water scarcity challenges faced by these vulnerable regions. Full article
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<p>Location of the study area. (<b>a</b>) The geographical position of the watershed in China. (<b>b</b>) The environmental background. The abbreviations featured in the figure are listed in <a href="#app1-land-13-01961" class="html-app">Supplementary Material Table S1</a>.</p>
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<p>Research framework on the effects of climate change and human activities on streamflow.</p>
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<p>Comparison of streamflow simulated by SWAT model with monthly observation data of hydrologic stations during 1980–2016 in the JTR (<b>a</b>), ZMR (<b>b</b>), HYR (<b>c</b>), and GLR (<b>d</b>).</p>
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<p>LUCC from 1990 to 2010. (<b>a</b>) and (<b>b</b>) represent the LUCC of the four basins for 1990 and 2010, respectively. (<b>c</b>) indicates the land use dynamic degree of the four basins. (<b>d</b>) refers to the comprehensive land use dynamic degree of the four basins. Note: The abbreviations CL, FL, WB, UrL, UnL, HCG, MCG, and LCG represent cultivated land, forest land, water body, urban land, unutilized land, high-coverage grassland, medium-coverage grassland, and low-coverage grassland, respectively.</p>
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<p>The 1990–2010 land use transition matrix in the JTR (<b>a</b>), ZMR (<b>b</b>), HYR (<b>c</b>), and GLR (<b>d</b>). The unit of LUCC transfer area is km<sup>2</sup>.</p>
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<p>Changing trends in temperature, precipitation, and streamflow. Note: β1 and β2 represent Sen’s slope during 1985–2000 and 2001–2016, respectively. “β” in bold denotes the trends for the entire period 1980–2009 (per decade). The single asterisk (“*”) and two asterisks (“**”), represent statistical significance levels of <span class="html-italic">p</span> &lt; 0.1and <span class="html-italic">p</span> &lt; 0.05, respectively.</p>
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<p>Sen’s slope of temperature (<b>a</b>), precipitation (<b>b</b>), and streamflow (<b>c</b>). Note: The single asterisks (“*”), two asterisks (”**”), and three asterisks (”***”) represent statistical significance levels of <span class="html-italic">p</span> &lt; 0.1, <span class="html-italic">p</span> &lt; 0.05, and <span class="html-italic">p</span> &lt; 0.01, respectively.</p>
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<p>Changes in monthly streamflow impacted by climate change and LUCC in the JTR (<b>a</b>), ZMR (<b>b</b>), HYR (<b>c</b>), and GLR (<b>d</b>).</p>
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<p>Streamflow suitability management in arid alpine regions.</p>
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28 pages, 31167 KiB  
Article
Optimizing GEDI Canopy Height Estimation and Analyzing Error Impact Factors Under Highly Complex Terrain and High-Density Vegetation Conditions
by Runbo Chen, Xinchuang Wang, Xuejie Liu and Shunzhong Wang
Forests 2024, 15(11), 2024; https://doi.org/10.3390/f15112024 - 17 Nov 2024
Cited by 1 | Viewed by 1295
Abstract
The Global Ecosystem Dynamics Investigation (GEDI) system provides essential data for estimating forest canopy height on a global scale. However, factors such as complex topography and dense canopy can significantly reduce the accuracy of GEDI canopy height estimations. We selected the South Taihang [...] Read more.
The Global Ecosystem Dynamics Investigation (GEDI) system provides essential data for estimating forest canopy height on a global scale. However, factors such as complex topography and dense canopy can significantly reduce the accuracy of GEDI canopy height estimations. We selected the South Taihang region of Henan Province, China, as our study area and proposed an optimization framework to improve GEDI canopy height estimation accuracy. This framework includes correcting geolocation errors in GEDI footprints, screening and analyzing features that affect estimation errors, and combining two regression models with feature selection methods. Our findings reveal a geolocation error of 4 to 6 m in GEDI footprints at the orbital scale, along with an overestimation of GEDI canopy height in the South Taihang region. Relative height (RH), waveform characteristics, topographic features, and canopy cover significantly influenced the estimation error. Some studies have suggested that GEDI canopy height estimates for areas with high canopy cover lead to underestimation, However, our study found that accuracy increased with higher canopy cover in complex terrain and dense vegetation. The model’s performance improved significantly after incorporating the canopy cover parameter into the optimization model. Overall, the R2 of the best-optimized model was improved from 0.06 to 0.61, the RMSE was decreased from 8.73 m to 2.23 m, and the rRMSE decreased from 65% to 17%, resulting in an accuracy improvement of 74.45%. In general, this study reveals the factors affecting the accuracy of GEDI canopy height estimation in areas with complex terrain and dense vegetation cover, on the premise of minimizing GEDI geolocation errors. Employing the proposed optimization framework significantly enhanced the accuracy of GEDI canopy height estimates. This study also highlighted the crucial role of canopy cover in improving the precision of GEDI canopy height estimation, providing an effective approach for forest monitoring in such regions and vegetation conditions. Future studies should further improve the classification of tree species and expand the diversity of sample tree species to test the accuracy of canopy height estimated by GEDI in different forest structures, consider the distortion of optical remote sensing images caused by rugged terrain, and further mine the information in GEDI waveforms so as to enhance the applicability of the optimization framework in more diverse forest environments. Full article
(This article belongs to the Section Forest Inventory, Modeling and Remote Sensing)
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<p>In the figure, (<b>a</b>) shows the location of Henan Province in China, (<b>b</b>) illustrates the study area’s location within Henan Province, and (<b>c</b>) presents the DEM of the study area, with each individual area number corresponding to the ALS aerial flight areas.</p>
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<p>CHM raster maps based on ALS acquisition: bottom images are true color images of Sentinel-2 in May 2023; black dots are GEDI footprints.</p>
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<p>The distribution of slope and canopy cover within the aerial flight zone after cropping based on ALS slope and canopy cover raster maps. Panel (<b>a</b>) shows the slope distribution following the cropping of the ALS airspace slope raster map using the extent of forested land from the Land Use Survey. Panel (<b>b</b>) shows the slope distribution across ALS airspace. Panels (<b>c</b>,<b>d</b>) show the canopy cover, where the vertical axis represents the number of raster pixels and the horizontal axis indicates the canopy cover (0-1).</p>
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<p>A square fishing net with a length and width of 5 m was used to calculate statistics of the DEM and slope within each grid, and the mean value, range, standard deviation, and mean slope of the DEM were calculated. Due to the huge amount of data, the data of all grids were not counted, but 5000 grids were randomly selected in each ALS region for statistics. The change from blue to red means the density goes from small to large.</p>
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<p>The principle of geolocation error correction is illustrated as follows: (<b>a</b>) displays the displacement mode of the footprint, where the red circle in the center represents the original GEDI location, and the cyan spot indicates the position after displacement. The angular step is set at 30°, while the distance step is 2 m. (<b>b</b>) shows the waveform corresponding to the GEDI location. (<b>c</b>) depicts the simulated waveform from ALS, and (<b>d</b>) presents the aligned GEDI waveform and ALS simulated waveform.</p>
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<p>Overall frame flowchart.</p>
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<p>The effect of geolocation error correction for a single footprint. Toploc and botloc refer to the start and end positions of the signal, respectively. Panels (<b>a</b>,<b>b</b>) display the original and corrected geolocation waveforms of the complex footprint, while panels (<b>c</b>,<b>d</b>) show the original and corrected geolocation waveforms of the simple footprint.</p>
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<p>The statistics of all R averages after displacing footprints to the same location for the same acquisition date. Each polar plot represents the average correction effect of geolocation errors for all footprints corresponding to the same acquisition date. The top label of each polar plot indicates the data acquisition date in the format YYYYDDD.</p>
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<p>R-values between individual features and GEDI canopy height estimation error, All feature parameters in the figure are significantly correlated (<math display="inline"><semantics> <mrow> <mi>p</mi> <mo>≤</mo> <mn>0.05</mn> </mrow> </semantics></math>), with a positive correlation in blue and a negative correlation in orange.</p>
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<p>Box plots of error distribution in different intervals of each feature with the absolute value of R above 0.3. The left vertical axis is the error (m) and the right vertical axis is the RMSE (m) of RH96 and CHM96.</p>
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<p>This figure shows the importance of each feature parameter with respect to the residuals: the upper figure shows the top 30 feature parameters in terms of importance, and the lower figure shows the thumbnail of the importance distribution of all feature parameters, where the blue part is the detailed distribution of the importance of the top 30 features in the upper figure.</p>
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<p>Box plots of error distribution in different intervals of each feature with the absolute value of RF importance above 1%. The left vertical axis is error (m) and the right vertical axis is the RMSE (m) of RH_96 and CHM_96.</p>
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<p>In the case of selecting different numbers of features, the model effects of various combinations of regression models and feature extraction methods are presented. The results are organized in the vertical coordinates from top to bottom in the order of <math display="inline"><semantics> <msup> <mi>R</mi> <mn>2</mn> </msup> </semantics></math>, <math display="inline"><semantics> <mrow> <mi>R</mi> <mi>M</mi> <mi>S</mi> <mi>E</mi> </mrow> </semantics></math> (m), and <math display="inline"><semantics> <mrow> <mi>r</mi> <mi>R</mi> <mi>M</mi> <mi>S</mi> <mi>E</mi> </mrow> </semantics></math> (%). The horizontal coordinates indicate the number of feature parameters used in the model.</p>
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<p>The left and right panels show the data distribution of RH_96 and RHT_96 with CHM96, respectively.</p>
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<p>The upper panel is a localized thumbnail of the remote sensing image, the blue part is the non-shadowed area, the white part is the shadowed area, and the lower two panels are the reflectance distributions of the red, green, and blue bands in the shadowed and non-shadow areas, respectively.</p>
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18 pages, 1660 KiB  
Article
Evaluating the Soil Properties of Different Land Use Types in the Deviskel Watershed in the Hilly Region of Northeast Türkiye
by Esin Erdoğan Yüksel and Gökhan Yavuz
Sustainability 2024, 16(22), 9732; https://doi.org/10.3390/su16229732 - 8 Nov 2024
Viewed by 1028
Abstract
Land use is a remarkable human-induced change that has redesigned the Earth’s surface since the beginning of civilization. Due to the combination of rugged terrain and low-income levels in rural areas, people in watershed regions often resort to overexploiting forests, agricultural land, and [...] Read more.
Land use is a remarkable human-induced change that has redesigned the Earth’s surface since the beginning of civilization. Due to the combination of rugged terrain and low-income levels in rural areas, people in watershed regions often resort to overexploiting forests, agricultural land, and grasslands beyond their capacity. As a result of these spatio-temporal changes in land use, various soil properties undergo changes. This study aims to determine the changes in some physical (texture, bulk weight, particle density, total porosity), hydro-physical (water holding capacity, permeability, field capacity, wilting point), physico-chemical (organic matter, pH, electrical conductivity), and erodibility (dispersion ratio, colloid–moisture equivalent ratio, erosion ratio, clay ratio, aggregate stability and K-factor of Universal Soil Loss Equation-USLE) properties of soil depending on land use in the Deviskel Watershed in the city of Artvin in Türkiye. For this purpose, disturbed (composite) and undisturbed (cylinder) soil samples were taken from a 0 to 20 cm depth at 108 different points in the determined areas (36 from forests, 36 from agricultural areas, and 36 from grassland areas). It was determined that 15 of the 19 soil properties examined showed statistical differences depending on the change in land use. All the examined soil properties, except for clay content, particle density, dispersion ratio, and aggregate stability, were found to be statistically significantly affected by the change in land use, and the reasons behind these changes were discussed. The particle density had the lowest coefficient of variation value (15.26%) while electrical conductivity had the highest coefficient of variation value (91.25%). According to erosion tendencies, all watershed soils were found to be susceptible to erosion. The average aggregate stability was 88.52% in forest soils, 84.84% in agricultural soils, and 85.48% in grassland soils. The average USLE-K factor was determined to be 0.22 for forests, while it was determined to be 0.17 and 0.18 for agriculture and grassland areas, respectively. According to the USLE-K factor, 68.37% of the watershed was dominated by moderately erodible soils, while 31.63% consisted of highly erodible soils. Based on the colloid–moisture equivalent ratio, erosion ratio, and clay ratio, which are statistically different erodibility features, the grassland soils of the research area were found to be more susceptible to erosion than forest and agricultural soils. In terms of aggregate stability, which indicates resistance to water erosion, forest areas had higher values, while agricultural lands were more prone to erosion. Full article
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<p>Location of Deviskel Watershed.</p>
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<p>The land use map and soil sampling points of the Deviskel Watershed.</p>
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<p>Erodibility map of the study area.</p>
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<p>Distribution of the range of K-factors grouped in percentages.</p>
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25 pages, 2178 KiB  
Article
User Sentiment Analysis of the Shared Charging Service for China’s G318 Route
by Mei Wang, Siva Shankar Ramasamy, Xi Yu, Mutong Liu, Ahmad Yahya Dawod and Huayue Chen
Electronics 2024, 13(22), 4335; https://doi.org/10.3390/electronics13224335 - 5 Nov 2024
Viewed by 819
Abstract
Shared charging services have gained popularity for their contribution to green travel. Accurately identifying the core factors that influence user experience (UX) not only enhances service quality and optimizes user satisfaction, but also promotes the dissemination of green travel concepts. However, the influencing [...] Read more.
Shared charging services have gained popularity for their contribution to green travel. Accurately identifying the core factors that influence user experience (UX) not only enhances service quality and optimizes user satisfaction, but also promotes the dissemination of green travel concepts. However, the influencing factors and their mechanisms vary significantly across regions, particularly along the Chengdu–Lhasa (G318) route, which features large elevation changes, diverse climatic conditions, rugged terrain, and frequent geological disasters, making the influencing factors particularly complex. This study analyzes comment texts from 38 shared charging stations along the G318 route in the e-Charging APP, totaling 15,214 comments. A comprehensive approach is employed, including high-frequency word analysis, term frequency–inverse document frequency (TF-IDF) comparison, co-occurrence semantic network and co-word matrix feature correlation analysis, Latent Dirichlet Allocation (LDA) topic modeling, and sentiment analysis. This multifaceted analysis explores core themes, user viewpoints, and sentiments in the comments, focusing on users’ perspectives on service quality, usage experience, and environmental impact of the charging stations. The findings indicate that charging speed, service attitude, environment, operational status of hardware and software, and pricing are key factors influencing user sentiment. Users have a high demand for the perfection of supporting facilities of shared charging stations, directly affecting user satisfaction and indirectly influencing the brand image and market competitiveness of enterprises. Full article
(This article belongs to the Special Issue Intelligent Data Analysis and Learning)
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<p>Route map of the South Route of G318.</p>
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<p>Distribution map of 38 shared charging stations.</p>
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<p>Overall evaluation chart of 38 shared charging stations.</p>
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<p>Word cloud diagram.</p>
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<p>Co-occurrence semantic network diagram.</p>
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<p>The distribution of emotion value and quantity.</p>
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18 pages, 4951 KiB  
Article
Combining Remote Sensing Data and Geochemical Properties of Ultramafics to Explore Chromite Ore Deposits in East Oltu Erzurum, Turkey
by Amr Abd El-Raouf, Fikret Doğru, Özgür Bilici, Islam Azab, Sait Taşci, Lincheng Jiang, Kamal Abdelrahman, Mohammed S. Fnais and Omar Amer
Minerals 2024, 14(11), 1116; https://doi.org/10.3390/min14111116 - 2 Nov 2024
Viewed by 856
Abstract
The present research’s main objective was to apply thorough exploration approaches that combine remote sensing data with geochemical sampling and analysis to predict and identify potential chromitite locations in a complex geological site, particularly in rugged mountainous terrain, and differentiate the ultramafic massif [...] Read more.
The present research’s main objective was to apply thorough exploration approaches that combine remote sensing data with geochemical sampling and analysis to predict and identify potential chromitite locations in a complex geological site, particularly in rugged mountainous terrain, and differentiate the ultramafic massif containing chromitite orebodies from other lithologies. The ultramafic massif forming the mantle section of the Kırdağ ophiolite, located within the Erzurum–Kars Ophiolite Zone and emerging in the east of Oltu district (Erzurum, NE Turkey), was selected as the study area. Optimum index factor (OIF), false-color composite (FCC), decorrelation stretch (DS), band rationing (BR), minimum noise fraction (MNF), and principal and independent component analyses (PCA-ICA) were performed to differentiate the lithological features and identify the chromitite host formations. The petrography, mineral chemistry, and whole-rock geochemical properties of the harzburgites, which are the host rocks of chromitites in the research area, were evaluated to verify and confirm the remote sensing results. In addition, detailed petrographic properties of the pyroxenite and chromitite samples are presented. The results support the existence of potential chromitite formations in the mantle section of the Kırdağ ophiolite. Our remote sensing results also demonstrate the successful detection of the spectral anomalies of this ultramafic massif. The mineral and whole-rock geochemical features provide clear evidence of petrological processes, such as partial melting and melt–peridotite interactions during the harzburgite formation. The chromian spinels’ Cr#, Mg#, Fe3+, Al2O3, and TiO2 concentrations indicate that the harzburgite formed in a fore-arc environment. The Al2O3 content and Mg# of the pyroxenes and the whole-rock Al2O3/MgO ratio and V contents of the harzburgite are also compatible with these processes. Consequently, the combined approaches demonstrated clear advantages over conventional chromitite exploration techniques, decreasing the overall costs and supporting the occurrence of chromite production at the site. Full article
(This article belongs to the Section Mineral Exploration Methods and Applications)
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<p>(<b>a</b>) Illustration depicting the overall distribution of ophiolite belts and prominent tectonic suture areas across Turkey, with modifications derived from [<a href="#B21-minerals-14-01116" class="html-bibr">21</a>,<a href="#B22-minerals-14-01116" class="html-bibr">22</a>]. (<b>b</b>) Geological map specifically detailing the Kırdağ ophiolite, adapted from [<a href="#B23-minerals-14-01116" class="html-bibr">23</a>].</p>
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<p>A flow chart showing the methodology of the combined approach applied in the investigated area.</p>
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<p>(<b>a</b>) False-color composite image in the RGB of ASTER bands (2, 3, 5). Ultra = ultramafic and Gab = gabbro; (<b>b</b>) false-color composite image in the RGB of ASTER bands (8, 3, 1); (<b>c</b>) false-color composite image in the RGB of ASTER bands (1, 2, 3); and (<b>d</b>) false-color composite image in the RGB of the ASTER band ratio (4/8, 4/1, and 3/2 × 4/3).</p>
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<p>(<b>a</b>) Grayscale image of the ASTER band ratio (3/4), (<b>b</b>) false-color composite image in the RGB of ASTER MNF (1, 2, 3), and (<b>c</b>) false-color composite image in the RGB of ASTER MNF (9, 6, 4).</p>
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<p>(<b>a</b>) False-color composite image in the RGB of ASTER PCs (1, 2, 3), (<b>b</b>) false-color composite image in the RGB of ASTER ICs (1, 2, 3), (<b>c</b>) false-color composite image in the RGB of ASTER PCs (5, 4, 2), and (<b>d)</b> false-color composite image in the RGB of ASTER (b4, PC1, PC2).</p>
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<p>(<b>a</b>) Field snapshot exhibiting the juxtaposition between the host harzburgite and adjacent lithologies (including dunite, pyroxenite, and chromitite) within the research locale. (<b>b</b>–<b>h</b>) Detailed close-up images showcasing the characteristics of the harzburgite, dunite, pyroxenite, and chromitite pod within the mantle section of the Kırdağ ophiolite.</p>
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<p>Thin-section photomicrographs of the harzburgite (<b>a</b>,<b>b</b>), dunite (<b>c</b>,<b>d</b>), pyroxenite (<b>e</b>), and chromitite (<b>f</b>). Microphotos (<b>a</b>,<b>c</b>,<b>e</b>) were taken under cross-polarized light, (<b>b</b>,<b>d</b>) were taken under plane-polarized light, and (<b>f</b>) was taken using a reflecting microscope for a chromitite ore sample. In the figure, spnl = chromian spinel, ol = olivine, opx = orthopyroxene, cpx = clinopyroxene, and srpn = serpentine.</p>
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<p>Graphical representations (<b>a</b>,<b>b</b>) illustrating the relationship between the Cr-number, Mg-number, and Cr-number and TiO<sub>2</sub> for chromian spinels within the harzburgite. Abyssal, fore-arc peridotite, and boninite fields are derived from [<a href="#B68-minerals-14-01116" class="html-bibr">68</a>], whereas the reaction fields and partial melting trend are referenced from [<a href="#B66-minerals-14-01116" class="html-bibr">66</a>,<a href="#B69-minerals-14-01116" class="html-bibr">69</a>], respectively. The diagram (<b>c</b>) presents the relationship between TiO<sub>2</sub> and Fe<sup>3+</sup>-number for chromian spinels. The fields representing the Mid-Ocean Ridge (MOR) and Supra-Subduction Zone (SSZ) contexts are based on data from [<a href="#B64-minerals-14-01116" class="html-bibr">64</a>]. Diagram (<b>d</b>) illustrates the correlation between Al<sub>2</sub>O<sub>3</sub> and Mg-number for orthopyroxene. In addition, (<b>e</b>) depicts the exact correlation for clinopyroxene. The fields representing abyssal and SSZ peridotites are based on data from [<a href="#B67-minerals-14-01116" class="html-bibr">67</a>]. The diagram (<b>f</b>) illustrates the relationship between V (ppm) and Al<sub>2</sub>O<sub>3</sub>/MgO for the harzburgites from the Kırdağ ophiolite. The fields representing the fore-arc and abyssal peridotites are derived from data compiled by [<a href="#B65-minerals-14-01116" class="html-bibr">65</a>,<a href="#B67-minerals-14-01116" class="html-bibr">67</a>], respectively.</p>
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<p>Sentinel-2-L2A True Color B4, B3, B2 showing the location of high-potential chromite-bearing mineralized zones based on integrating remote sensing and geochemical results with field validation.</p>
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17 pages, 11423 KiB  
Article
Spatiotemporal Variability of Soil Erosion in the Pisha Sandstone Region: Influences of Precipitation and Vegetation
by Zhenqi Yang, Jianying Guo, Fucang Qin, Yan Li, Xin Wang, Long Li and Xinyu Liu
Sustainability 2024, 16(21), 9313; https://doi.org/10.3390/su16219313 - 26 Oct 2024
Viewed by 1041
Abstract
The Pisha sandstone area, situated in the upper and middle reaches of the Yellow River in China, is characterized by severe soil and water erosion, making it one of the most critical regions on the Loess Plateau. The rugged terrain and exposed bedrock [...] Read more.
The Pisha sandstone area, situated in the upper and middle reaches of the Yellow River in China, is characterized by severe soil and water erosion, making it one of the most critical regions on the Loess Plateau. The rugged terrain and exposed bedrock complicate management efforts for this area, posing challenges for accurate forecasting using soil erosion models. Through an analysis of terrain, vegetation, and precipitation impacts on soil erosion, this study offers theoretical support for predicting soil erosion within the exposed Pisha sandstone area of the Loess Plateau. This has substantial implications for guiding water and soil conservation measures in this region. Focusing on China’s exposed sandstone area within the Geqiugou watershed, temporal and spatial changes in vegetation cover and land use from 1990 to 2020 were analyzed. The result shows that, from 1990 to 2020, the grassland area has exhibited a consistent downward trend, with successive reductions of 64.86% to 59.46%. The area of low vegetation cover witnessed a significant decline of 59.29% in 2020 compared to that in 1990. The moderate erosion area decreased from 84.52 to 57.17 km2. The significant reduction in soil and water loss can be attributed to the expansion of forest and grassland areas, with the implementation of the Grain for Green project serving as a key policy driver for facilitating this expansion. This study provided a good example of combining rainfall with vegetation coverage to fast estimation soil erosion. A mathematical relationship between the vegetation rainfall coupling index (RV) and soil erosion was established with strong fitting effects, enabling estimation of the soil erosion volume under varying slope conditions within Pisha sandstone areas. The main focus of future soil and water conservation in the Pisha sandstone area should be on effectively managing the channel slope and minimizing exposed bedrock areas through a combination of slope cutting, the application of anticorrosive materials, and the implementation of artificial vegetation planting. Full article
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<p>Geographical location of the study site.</p>
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<p>The field for monitoring soil and water loss in Ordos City.</p>
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<p>Interannual change characteristics of ground utilization form in the study area from 1990 to 2020.</p>
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<p>Spatial distribution map of <span class="html-italic">VC</span> in the watershed.</p>
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<p>Spatial distribution map of the hydraulic erosion modulus.</p>
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<p>Relationship between vegetation coverage and soil erosion under different slopes. (<b>a</b>) The vegetation coverage of various slopes from 1990 to 2020. (<b>b</b>) The soil erosion amount of various slopes from 1990 to 2020. (<b>c</b>) The correlation between vegetation coverage and soil erosion under varying slope conditions.</p>
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<p>Relationship between vegetation coverage and soil erosion under different slopes. (<b>a</b>) The vegetation coverage of various slopes from 1990 to 2020. (<b>b</b>) The soil erosion amount of various slopes from 1990 to 2020. (<b>c</b>) The correlation between vegetation coverage and soil erosion under varying slope conditions.</p>
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<p>Relationship between annual rainfall and soil erosion at different gradients.</p>
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<p>Relationship between RV and soil erosion at different gradients.</p>
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15 pages, 3362 KiB  
Article
Assessing Atlantic Kelp Forest Restoration Efforts in Southern Europe
by Alexandre F. S. Marques, Álvaro Sanchéz-Gallego, Rodrigo R. Correia, Isabel Sousa-Pinto, Silvia Chemello, Inês Louro, Marco F. L. Lemos and João N. Franco
Sustainability 2024, 16(21), 9176; https://doi.org/10.3390/su16219176 - 23 Oct 2024
Cited by 1 | Viewed by 1494
Abstract
Kelp forests are essential marine ecosystems increasingly compromised by human activities. Effective reforestation strategies are urgently needed, and the “green gravel” method is a viable tool already used in some European regions. This study aimed to assess the success of this method using [...] Read more.
Kelp forests are essential marine ecosystems increasingly compromised by human activities. Effective reforestation strategies are urgently needed, and the “green gravel” method is a viable tool already used in some European regions. This study aimed to assess the success of this method using the native Kelp species Laminaria ochroleuca on the Portuguese coastline. Cultures of green gravel were reared until the specimens reached a size of approximately 3 cm. The gravel was then deployed at selected sites in Peniche, Berlengas, and Cascais. Over an eight-month period, scientific scuba divers monitored the integration of Kelp, along with associated fish, invertebrate, and algae communities. Nutrient availability, temperature, water movement, substrate type, and Rugosity Index (RI) were also measured. The highest success rate was 12% in Consolação, with Elefante and Galos (Berlengas) reaching 7% and 4%, respectively. By the end of the monitoring period, Cascais had no remaining Kelp on green gravel. Present data suggest that higher success is dependent on less rugged and higher RI topography. Higher grazing pressure, rougher terrain, and unexpected sedimentation appear to be the main obstacles to deployment success. Solid knowledge (biologic and topographic) on the restoration site, starting restoration actions near already established Kelp forests, and significantly scaling up restoration efforts could substantially improve the success of the green gravel method in future reforestation campaigns. Full article
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<p>(<b>A</b>) Section of the western continental Portuguese coast where the deployments took place. Three distinct zones were selected: (<b>B</b>) The coast of Peniche, with Marques-Neves as the reference Kelp forest (I) and Consolação (II); (<b>C</b>) In the Berlengas Islands at the sites Elefante (III) and Galos (IV); (<b>D</b>) and in the Cascais area at Boca do Inferno (V).</p>
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<p>(<b>A</b>) Technique used to deploy the gravel from the surface; (<b>B</b>) Scientific divers deployed buoys marking the area for deployment (100 m<sup>2</sup>) in Berlengas at the Galos site; (<b>C</b>) close-up of the deployed green gravel.</p>
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<p>Percentage of each bottom substratum category (reef plateau, boulders, and sand) measured in 25 m transects at the different studied sites (<span class="html-italic">n</span> = 5). Numbers within each bar indicate the site’s Rugosity Index (RI) achieved (<span class="html-italic">n</span> = 5).</p>
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<p>(<b>A</b>) Average seawater temperature (measured in situ); (<b>B</b>) sea surface temperature—SST; (<b>C</b>) near surface chlorophyll <span class="html-italic">a</span> level—Chla <span class="html-italic">a</span>, and (<b>D</b>) absolute average water movement in all monitored sites. Statistically significant different groups (a, b, and c) are shown (Tukey’s HSD; <span class="html-italic">p</span> ≤ 0.05). Error bars are ±2 sd of means (n.a. = not assessed).</p>
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<p>(<b>A</b>) Concentration of phosphates, (<b>B</b>) nitrates, and (<b>C</b>) nitrites at depth at all monitored sites. Statistically significant different groups (a and b) are shown (Tukey’s HSD; <span class="html-italic">p</span> ≤ 0.05). Error bars are ±2 sd of means. (<span class="html-italic">n</span> = 9 per site).</p>
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<p>(<b>A</b>) Gravel retention and (<b>B</b>) deployment success at the four deployment sites in the three monitoring moments after 3, 6, and 8 months of deployment.</p>
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<p>Coefficient plot of the first component of the PLS regression model. The model included data from all the deployment sites to explain the green gravel success index. Importance was deemed as high if the coefficient was higher than 0.15 (<span class="html-italic">n</span> = 80).</p>
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22 pages, 25663 KiB  
Article
Trade-Off and Coordination between Development and Ecological Protection of Urban Agglomerations along Rivers: A Case Study of Urban Agglomerations in the Shandong Section of the Lower Yellow River
by Anbei Liu, Tingting Yan, Shengxiang Shi, Weijun Zhao, Sihang Ke and Fangshu Zhang
Land 2024, 13(9), 1368; https://doi.org/10.3390/land13091368 - 26 Aug 2024
Viewed by 785
Abstract
Urban development of clusters situated along rivers significantly affects the health of the river ecosystems, the quality of urban environments, and the overall well-being of local communities. Ecosystem service supply value (ESSV) measures the delivery of ecosystem goods and services within a specific [...] Read more.
Urban development of clusters situated along rivers significantly affects the health of the river ecosystems, the quality of urban environments, and the overall well-being of local communities. Ecosystem service supply value (ESSV) measures the delivery of ecosystem goods and services within a specific timeframe in a particular area. Using the lower Yellow River urban agglomeration (Shandong section) as a case, we comprehensively applied land use structure and intensity change analysis, quantitative calculation of ESS, and geographical probe methods to unveil ESS and its mechanism of response to the spatio-temporal evolution of the intensity of land use in urban agglomeration along the river. The key results were as follows: (1) Over the past two decades, farmland and construction land areas have continued to decrease and increase, respectively, with the intensity of land use change being highest from 2005 to 2010. (2) ESS has continued to rise over the past 20 years, with the income in 2020 being 11.142 billion yuan, an increase of 31.13%. The “low-value areas” are mainly concentrated in Liaocheng City, Dezhou City, and Tai’an City, which are characterized by predominantly flat terrains where farmland constitutes the principal land use type. Conversely, “high-value areas” are largely in the counties bordering the Yellow River, including the upper estuary in the north and the rugged, southeastern terrains. (3) Areas with concentrated ESSV were primarily localized in the northern estuary area and along the Yellow River in a scattered point-like pattern. The spatial distribution of hotspots has become increasingly concentrated, transitioning from points to planes. Conversely, cold spots initially increased in number before subsequently decreasing. Waterbody was the most sensitive ESSV-determining factor. (4) The spatial heterogeneity of ESSV emerges as a consequence of the interaction of multiple factors, and among these interactions, those involving NDVI and POP contain the greatest explanatory power. Our findings are expected to offer a scientific foundation for optimizing land spatial patterns and enhancing ecological management in the lower Yellow River region. Full article
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<p>Location of the study area.</p>
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<p>Land use in the study area in 2000–2020.</p>
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<p>Land use in the study area in 2000–2020.</p>
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<p>Sankey map depicting the change in land use from 2000 to 2020.</p>
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<p>Time-intensity analysis of four time intervals: 2000–2005, 2005–2010, 2010–2015, and 2015–2020.</p>
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<p>The category intensities in 2000–2005, 2005–2010, 2010–2015, and 2015–2020 are shown in figures (<b>a</b>–<b>d</b>), respectively.</p>
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<p>Transition intensity of the given category gains during the four time intervals. The green lines and orange lines in the figures represent the intensity of the transition from M to other categories, and from other categories to M, respectively.</p>
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<p>Transition intensity of the given category gains during the four time intervals. The green lines and orange lines in the figures represent the intensity of the transition from M to other categories, and from other categories to M, respectively.</p>
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<p>Characteristics of the spatial distribution of ESSV from 2000 to 2020. The blue and red colors indicate the low-value and high-value areas, respectively.</p>
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<p>Land use type transfer and distribution of ESSV hot spots in the study area.</p>
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<p>Results of the spatial differentiation of factors driving ESSV in the study area.</p>
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<p>Interactive effect of driving factors from 2000 to 2020. Note: X<sub>1</sub>: population; X2: per capita GDP; X3: precipitation; X4: temperature; X5: normalized difference vegetation index; X6: night light index; X7: distance from the Yellow River.</p>
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