Nothing Special   »   [go: up one dir, main page]

You seem to have javascript disabled. Please note that many of the page functionalities won't work as expected without javascript enabled.
 
 
Sign in to use this feature.

Years

Between: -

Subjects

remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline

Journals

remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline

Article Types

Countries / Regions

remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline

Search Results (2,866)

Search Parameters:
Keywords = flood processes

Order results
Result details
Results per page
Select all
Export citation of selected articles as:
17 pages, 8008 KiB  
Article
An Exploratory Study of Quartz Grain Surface Microtextures in Dam-Break Flood Deposits from the Middle Reaches of the Yarlung Tsangbo River
by Zhihang Lu, Mengying He, Jinying Xu, Xilin Cao, Jingran Zhang, Zhigang Zhang, Xinggong Kong and Zhijun Zhao
Minerals 2025, 15(2), 183; https://doi.org/10.3390/min15020183 (registering DOI) - 16 Feb 2025
Abstract
This study focused on the surface microtextures of quartz grains deposited by dam-break floods in Jiacha Gorge, situated in the middle reaches of the Yarlung Tsangpo River. Utilizing a scanning electron microscope (SEM), 200 quartz grains were observed and analyzed based on their [...] Read more.
This study focused on the surface microtextures of quartz grains deposited by dam-break floods in Jiacha Gorge, situated in the middle reaches of the Yarlung Tsangpo River. Utilizing a scanning electron microscope (SEM), 200 quartz grains were observed and analyzed based on their microtextural features. Our findings reveal specific microtextures—such as angular outlines, high relief, flat cleavage surfaces, conchoidal fractures, and steps—that serve as clear indicators of the extreme energy associated with dam-break floods in Jiacha Gorge, distinguishing them from meteorological floods and smaller-scale dam-break events. These features also facilitate the differentiation of dam-break flood deposits from those of other sedimentary environments. This research demonstrates that quartz microtextures are a valuable tool for reconstructing sediment transport processes during extreme flood events. We recommend integrating microtextural analysis with complementary methods to refine interpretations and address methodological uncertainties in future studies. Full article
Show Figures

Figure 1

Figure 1
<p>(<b>A</b>) Locations of the Yarlung Tsangpo River drainage and other flood deposit sites compared to this study [<a href="#B31-minerals-15-00183" class="html-bibr">31</a>,<a href="#B32-minerals-15-00183" class="html-bibr">32</a>]; (<b>B</b>) topographic map of the Yarlung Tsangpo River drainage and the major paleo-dammed lakes and gorges in the middle reaches; (<b>C</b>) tectonic background of the Yarlung Tsangpo River. YZS: Yarlung Tsangpo suture; STD: South Tibetan detachment; MCT: main central thrust; MBT: main boundary thrust.</p>
Full article ">Figure 2
<p>(<b>A</b>) Topographic map of dam-break flood deposit profiles in this study and existing studies [<a href="#B26-minerals-15-00183" class="html-bibr">26</a>,<a href="#B40-minerals-15-00183" class="html-bibr">40</a>,<a href="#B41-minerals-15-00183" class="html-bibr">41</a>,<a href="#B71-minerals-15-00183" class="html-bibr">71</a>] within the Jiacha Gorge section in the Yarlung Tsangpo River; (<b>a</b>–<b>g</b>) the lithological column for each profile; (<b>B</b>–<b>F</b>) representative photos of the sampling profiles.</p>
Full article ">Figure 3
<p>Frequency of quartz surface microtextures. High-frequency features are marked in red font, while moderately common features are marked in light red font.</p>
Full article ">Figure 4
<p>Typical microtextures in Jiacha Gorge sample. (<b>A</b>) High relief and angular outline. (<b>B</b>) Low relief and angular outline. (<b>C</b>) Low relief and subangular outline. (<b>D</b>) Medium relief and angular outline. (<b>E</b>) Medium relief and angular outline. (<b>F</b>) High relief and angular outline. (<b>G</b>) Medium relief and angular outline. (<b>H</b>) Medium relief and subrounded outline. (<b>I</b>) Frequent occurrence of conchoidal fractures near a flat cleavage surface. (<b>J</b>) V-shaped percussion marks on a flat cleavage surface. (<b>K</b>) Frequent occurrence of both arcuate and straight steps. (<b>L</b>) Conchoidal fractures coexist with steps. (<b>M</b>) A mechanical curved crack and clearly visible upturned plates. (<b>N</b>) Large V-shaped percussion marks on a pre-weathered surface. The left part is a newly formed fresh surface. (<b>O</b>) A straight groove on a fresh surface. (<b>P</b>) A fresh surface covered with grooves and V-shaped percussion marks. (<b>Q</b>) Frequent occurrence of solution pits. Notice that solution pits overlap fresh surfaces, indicating these chemical features formed later than mechanical features. (<b>R</b>) Silica precipitation on flat cleavage surface. (<b>S</b>) Oriented etch pits in a depression on the grain, indicating a diagenesis process. (<b>T</b>) The grain surface is covered with silica precipitation. Some curved cracks can be seen, which are more likely to have originated from chemical processes. Abbreviations: SS—straight step; AS—arcuate step; VPM—V-shaped percussion mark; CC—curved crack; FCS—flat cleavage surface; SG—straight groove; CG—curved groove; UP—upturned plate; SCF—small conchoidal fracture; MCF—medium conchoidal fracture; LCF—large conchoidal fracture; SOP—solution pit; SIP—silica pellicle; OEP—oriented etch pit.</p>
Full article ">Figure 5
<p>The mean values and coefficients of variation for quartz surface microtextures from the Jiacha Gorge.</p>
Full article ">Figure 6
<p>Typical inherited microtextures. (<b>A</b>) The upper part of the grain has undergone extensive chemical alteration, while other parts remain fresh surfaces. This clearly indicates that these chemical microtextures are inherited. (<b>B</b>) The left side of the grain has a fresh surface with straight steps, while the rest has undergone extensive chemical rework. (<b>C</b>) The lower part of the grain is a newly formed fresh surface, while the flat cleavage surface on the upper part has been weathered and has numerous marks on it. (<b>D</b>) Details of the flat cleavage surface on grain G show numerous V-shaped percussion marks and impact grooves. (<b>E</b>) Abrasion fatigue and chatter marks on the flat cleavage surface, with chatter marks indicating glacial modification. (<b>F</b>) Parallel striations indicate glacial work. (<b>G</b>) A bulbous edge showing a very rounded outline. The rest of the grain is angular and has fresh surfaces resulting from grain fragmentation. (<b>H</b>) Details of bulbous edges on grain A. Abbreviations: BE—bulbous edge; CPM—crescentic percussion mark; SOP—solution pit; AS—arcuate step; AF—abrasion fatigue; PS—parallel striation; OEP—oriented etch pit; FCS—flat cleavage surface; SG—straight groove.</p>
Full article ">Figure 7
<p>Contrast between dam-break flood deposits and those from other sedimentary environments. Data for other sedimentary environments are sourced from Vos et al. [<a href="#B46-minerals-15-00183" class="html-bibr">46</a>].</p>
Full article ">
27 pages, 7459 KiB  
Article
Flood Modelling of the Zhabay River Basin Under Climate Change Conditions
by Aliya Nurbatsina, Zhanat Salavatova, Aisulu Tursunova, Iulii Didovets, Fredrik Huthoff, María-Elena Rodrigo-Clavero and Javier Rodrigo-Ilarri
Hydrology 2025, 12(2), 35; https://doi.org/10.3390/hydrology12020035 (registering DOI) - 15 Feb 2025
Abstract
Flood modelling in snow-fed river basins is critical for understanding the impacts of climate change on hydrological extremes. The Zhabay River in northern Kazakhstan exemplifies a basin highly vulnerable to seasonal floods, which pose significant risks to infrastructure, livelihoods, and water resource management. [...] Read more.
Flood modelling in snow-fed river basins is critical for understanding the impacts of climate change on hydrological extremes. The Zhabay River in northern Kazakhstan exemplifies a basin highly vulnerable to seasonal floods, which pose significant risks to infrastructure, livelihoods, and water resource management. Traditional flood forecasting in Central Asia still relies on statistical models developed during the Soviet era, which are limited in their ability to incorporate non-stationary climate and anthropogenic influences. This study addresses this gap by applying the Soil and Water Integrated Model (SWIM) to project climate-driven changes in the hydrological regime of the Zhabay River. The study employs a process-based, high-resolution hydrological model to simulate flood dynamics under future climate conditions. Historical hydrometeorological data were used to calibrate and validate the model at the Atbasar gauge station. Future flood scenarios were simulated using bias-corrected outputs from an ensemble of General Circulation Models (GCMs) under Representative Concentration Pathways (RCPs) 4.5 and 8.5 for the periods 2011–2040, 2041–2070, and 2071–2099. This approach enables the assessment of seasonal and interannual variability in flood magnitudes, peak discharges, and their potential recurrence intervals. Findings indicate a substantial increase in peak spring floods, with projected discharge nearly doubling by mid-century under both climate scenarios. The study reveals a 1.8-fold increase in peak discharge between 2010 and 2040, and a twofold increase from 2041 to 2070. Under the RCP 4.5 scenario, extreme flood events exceeding a 100-year return period (2000 m3/s) are expected to become more frequent, whereas the RCP 8.5 scenario suggests a stabilization of extreme event occurrences beyond 2071. These findings underscore the growing flood risk in the region and highlight the necessity for adaptive water resource management strategies. This research contributes to the advancement of climate-resilient flood forecasting in Central Asian river basins. The integration of process-based hydrological modelling with climate projections provides a more robust framework for flood risk assessment and early warning system development. The outcomes of this study offer crucial insights for policymakers, hydrologists, and disaster management agencies in mitigating the adverse effects of climate-induced hydrological extremes in Kazakhstan. Full article
(This article belongs to the Section Hydrological and Hydrodynamic Processes and Modelling)
Show Figures

Figure 1

Figure 1
<p>Location of the study area—Zhabay River basin.</p>
Full article ">Figure 2
<p>Interannual variation of seasonal values of air temperature and precipitation.</p>
Full article ">Figure 2 Cont.
<p>Interannual variation of seasonal values of air temperature and precipitation.</p>
Full article ">Figure 3
<p>SWIM model structure diagram (PIK, User Manual, 2024).</p>
Full article ">Figure 4
<p>Maps of land use and soil types of the Zhabay River catchment area.</p>
Full article ">Figure 5
<p>Difference-integral curve of maximum water runoff of the Zhabay-Atbasar region.</p>
Full article ">Figure 6
<p>Cumulative distribution function for maximum water discharge for 1984–2010 in the Zhabay-Atbasar region.</p>
Full article ">Figure 7
<p>Average water discharge for the period April–September in the Zhabay-Atbasar region.</p>
Full article ">Figure 8
<p>Seasonal distribution of water runoff in the Zhabay-Atbasar region during the historical period.</p>
Full article ">Figure 9
<p>Seasonal dynamics of runoff at the Atbasar gauge according to the RCP 4.5 and RCP 8.5 scenarios.</p>
Full article ">Figure 10
<p>Cumulative distribution function for maximum water discharge from 2011 to 2099 in the Zhabay-Atbasar region according to the GFDL-ESM2M RCP 4.5 and GFDL-ESM2M RCP 8.5 scenarios.</p>
Full article ">Figure 11
<p>Flood area estimation map using the FastFlood app on a 40 m grid.</p>
Full article ">
26 pages, 13040 KiB  
Article
A Historical Overview of Methods for the Estimation of Erosion Processes on the Territory of the Republic of Serbia
by Ivan Malušević, Ratko Ristić, Boris Radić, Siniša Polovina, Vukašin Milčanović and Petar Nešković
Land 2025, 14(2), 405; https://doi.org/10.3390/land14020405 (registering DOI) - 15 Feb 2025
Abstract
Erosion is a significant environmental challenge in Serbia, shaped by natural and human factors. Pronounced relief, fragile geological substrate, a developed hydrographic network, and a climate characterized by an uneven distribution of precipitation throughout the year make this area prone to activating erosion [...] Read more.
Erosion is a significant environmental challenge in Serbia, shaped by natural and human factors. Pronounced relief, fragile geological substrate, a developed hydrographic network, and a climate characterized by an uneven distribution of precipitation throughout the year make this area prone to activating erosion processes and flash floods whenever there is a significant disruption in ecological balance, whether due to the removal of vegetation cover or inadequate land use. Researchers have recorded approximately 11,500 torrents in Serbia, most of which were activated during the 19th century, a period of significant social and political change, as well as intensive deforestation and the irrational exploitation of natural resources. By the mid-19th century, the effects of land degradation were impossible to ignore. As the adequate assessment of soil erosion intensity is the initial step in developing a prevention and protection strategy and the type and scope of anti-erosion works and measures, this article presents the path that the anti-erosion field in Serbia has taken from the initial observations of erosion processes through the first attempts to create the Barren Land Cadastre and Torrent Cadastre to the creation of the Erosion Potential Method (EPM) and its modification by Dr. Lazarević that resulted in the creation of the first Erosion Map of SR Serbia in 1971 (published in 1983). In 2020, a new Erosion Map of Serbia was created with the application of Geographic Information System (GIS) technologies and based on the original method by Professor Slobodan Gavrilović—the EPM—without the modifications introduced by Lazarević. We compared the 1983 and 2020 erosion maps in a GIS environment, where the change in soil erosion categories was analyzed using a confusion matrix. The updated erosion maps mirror the shift in methodology from a traditional approach (Lazarević’s modification) to the modern GIS-based method (Gavrilović’s original EPM) and reflect technological improvements and changes in land use, conservation practices, and environmental awareness. Full article
(This article belongs to the Section Urban Contexts and Urban-Rural Interactions)
Show Figures

Figure 1

Figure 1
<p>The position and topography of the Republic of Serbia.</p>
Full article ">Figure 2
<p>The algorithm of the process of creating an erosion map according to the EPM [<a href="#B36-land-14-00405" class="html-bibr">36</a>].</p>
Full article ">Figure 3
<p>The Erosion Map of the Republic of Serbia from 1983, using the EPM modified by Lazarević [<a href="#B36-land-14-00405" class="html-bibr">36</a>].</p>
Full article ">Figure 4
<p>The Erosion Map of the Republic of Serbia from 2020, using the original EPM by Gavrilović [<a href="#B36-land-14-00405" class="html-bibr">36</a>].</p>
Full article ">
26 pages, 13339 KiB  
Article
An Enhanced Framework for Assessing Pluvial Flooding Risk with Integrated Dynamic Population Vulnerability at Urban Scale
by Xinyi Shu, Chenlei Ye, Zongxue Xu, Ruting Liao, Pengyue Song and Silong Zhang
Remote Sens. 2025, 17(4), 654; https://doi.org/10.3390/rs17040654 - 14 Feb 2025
Abstract
Under the combined influence of climate change, accelerated urbanization, and inadequate urban flood defense standards, urban pluvial flooding has become an increasingly severe issue. This not only poses significant challenges to social stability and economic development but also makes accurate flood risk assessment [...] Read more.
Under the combined influence of climate change, accelerated urbanization, and inadequate urban flood defense standards, urban pluvial flooding has become an increasingly severe issue. This not only poses significant challenges to social stability and economic development but also makes accurate flood risk assessment crucial for improving urban flood control and drainage capabilities. This study uses Jinan, a typical foothill plain city in Shandong Province, as a case study to compare the performance of differential evolution (DE), genetic algorithm (GA), and particle swarm optimization (PSO) in calibrating the SWMM. By constructing a hydrological–hydrodynamic coupled model using the SWMM and LISFLOOD-FP, this study evaluates the drainage capacity of the pipe network and surface inundation characteristics under both historical and design rainfall scenarios. An agent-based model (ABM) is developed to analyze the dynamic risks and vulnerabilities of population and building agents under different rainfall scenarios, capturing macroscopic emergent patterns from individual behavior rules and analyzing them in both time and space dimensions. Additionally, using multi-source remote sensing data, dynamic population vulnerability, and flood hazard processes, a quantitative dynamic flood risk analysis is conducted based on cloud models. The results demonstrated the following: (1) PSO performed best in calibrating the SWMM in the study area, with Nash–Sutcliffe efficiency (NSE) values ranging from 0.93 to 0.69. (2) Drainage system capacity was low, with over 90% of the network exceeding capacity in scenarios with return periods of 1 to 100 years. (3) The vulnerability of people and buildings increased with higher flood intensity and duration. Most affected individuals were located on roads. In Event 6, 11.41% of buildings were at risk after 1440 min; in the 20-year flood event, 26.69% of buildings were at risk after 180 min. (4) Key features influencing vulnerability included the DEM, PND, NDVI, and slope. High-risk areas in the study area expanded from 36.54% at 30 min to 38.05% at 180 min. Full article
Show Figures

Figure 1

Figure 1
<p>Overview of the study area.</p>
Full article ">Figure 2
<p>Technology roadmap.</p>
Full article ">Figure 3
<p>Dynamic population vulnerability mobility strategy.</p>
Full article ">Figure 4
<p>The iterative process of different parameter optimization algorithms.</p>
Full article ">Figure 5
<p>Simulations and observation comparison within calibration and validation flood events: (<b>a</b>) Event 1, (<b>b</b>) Event 2, (<b>c</b>) Event 4, (<b>d</b>) Event 5, (<b>e</b>) Event 3, and (<b>f</b>) Event 6.</p>
Full article ">Figure 6
<p>Assessment of the drainage capacity of the pipeline system under different historical rainfall events: (<b>a</b>) node overflow condition, and (<b>b</b>) pipeline overload condition.</p>
Full article ">Figure 7
<p>Surface inundation depth distribution under different historical rainfall events: (<b>a</b>) Event 1 rainfall, (<b>b</b>) Event 2 rainfall, (<b>c</b>) Event 3 rainfall, (<b>d</b>) Event 4 rainfall, (<b>e</b>) Event 5 rainfall, and (<b>f</b>) Event 6 rainfall.</p>
Full article ">Figure 8
<p>Assessment of the drainage capacity of the pipeline system under different rainfall return periods: (<b>a</b>) node overflow condition, and (<b>b</b>) pipeline overload condition.</p>
Full article ">Figure 9
<p>Surface inundation depth distribution under different return period rainfall events. (<b>a</b>) 1-year return period rainfall, (<b>b</b>) 20-year return period rainfall, (<b>c</b>) 50-year return period rainfall, (<b>d</b>) 100-year return period rainfall.</p>
Full article ">Figure 10
<p>Changes in population vulnerability risk during the flooding process under different rainfall events: (<b>a</b>) Event 6 rainfall, and (<b>b</b>) 20-year return period rainfall.</p>
Full article ">Figure 11
<p>Changes in the vulnerability risk of the population in road areas during the flooding process under different rainfall events: (<b>a</b>) Event 6 rainfall, and (<b>b</b>) 20-year return period.</p>
Full article ">Figure 12
<p>Changes in the vulnerability risk of the population in building areas during the flooding process under different rainfall events: (<b>a</b>) Event 6 rainfall, and (<b>b</b>) 20-year return period.</p>
Full article ">Figure 13
<p>Changes in building vulnerability risk during the flooding process under different rainfall events: (<b>a</b>) Event 6 rainfall, and (<b>b</b>) 20-year return period rainfall.</p>
Full article ">Figure 14
<p>Dynamic spatial changes in the population during the flooding process of rainfall for Event 6: (<b>a</b>) at 240 min, (<b>b</b>) at 480 min, (<b>c</b>) at 720 min, (<b>d</b>) at 960 min, (<b>e</b>) at 1200 min, and (<b>f</b>) at 1440 min.</p>
Full article ">Figure 15
<p>Dynamic spatial changes in the population during the flooding process under a 20-year return period rainfall event: (<b>a</b>) at 30 min, (<b>b</b>) at 60 min, (<b>c</b>) at 90 min, (<b>d</b>) at 120 min, (<b>e</b>) at 150 min, and (<b>f</b>) at 180 min.</p>
Full article ">Figure 16
<p>Attribution of the explanatory factors under different rainfalls.</p>
Full article ">Figure 17
<p>The dynamic changes in flood risk during a 20-year return period rainfall and flooding event: (<b>a</b>) at 30 min, (<b>b</b>) at 60 min, (<b>c</b>) at 90 min, (<b>d</b>) at 120 min, (<b>e</b>) at 150 min, and (<b>f</b>) at 180 min.</p>
Full article ">
24 pages, 11294 KiB  
Article
Innovative Flood Impact Monitoring and Harvest Analysis in Oil Palm Plantations Utilizing Geographic Information Systems and Deep Learning
by Supattra Puttinaovarat, Supaporn Chai-Arayalert, Wanida Saetang, Kanit Khaimook, Sasikarn Plaiklang and Paramate Horkaew
AgriEngineering 2025, 7(2), 44; https://doi.org/10.3390/agriengineering7020044 - 13 Feb 2025
Abstract
Floods, as a form of disaster, significantly affect individuals and farmers in impacted areas, particularly through crop damage and the inability to harvest due to prolonged and extensive flooding. Among the most severely affected agricultural sectors are oil palm plantations, which regularly experience [...] Read more.
Floods, as a form of disaster, significantly affect individuals and farmers in impacted areas, particularly through crop damage and the inability to harvest due to prolonged and extensive flooding. Among the most severely affected agricultural sectors are oil palm plantations, which regularly experience such disruptions annually. Current methods of assistance and relief during flooding rely on field surveys conducted manually by personnel, a process constrained by its time-intensive nature. Moreover, existing applications or platforms do not support the classification and inspection of oil palm plantations affected by floods during harvesting. This research aims to develop a method and application for inspecting oil palm plantations impacted by floods during harvesting. The approach utilizes deep learning and geographic information systems (GIS) to classify and analyze flood-affected areas and determine the ripeness of oil palm bunches on trees, enabling accurate and rapid identification of flood-affected areas. The study results demonstrate that the proposed method achieves a flood classification accuracy ranging from 96.80% to 98.29% and ripeness classification accuracy for oil palm bunches on trees ranging from 97.60% to 99.75%. These findings indicate that the proposed model effectively and efficiently monitors flood-affected areas. Additionally, the developed application serves as a valuable tool for flood management, facilitating timely assistance and relief for farmers impacted by flooding. Full article
Show Figures

Figure 1

Figure 1
<p>Research framework.</p>
Full article ">Figure 2
<p>Study area, highlighting flood-affected areas (blue) and oil palm plantations with different conditions. The images illustrate flooded and non-flooded plantations, as well as ripe and unripe oil palm bunches on trees.</p>
Full article ">Figure 3
<p>Use case diagram.</p>
Full article ">Figure 4
<p>Confusion matrix for model evaluation of oil palm ripeness classification.</p>
Full article ">Figure 5
<p>Confusion matrix for model evaluation of flood classification.</p>
Full article ">Figure 6
<p>User account creation and authentication interface.</p>
Full article ">Figure 7
<p>Farmers’ interface for flood reporting.</p>
Full article ">Figure 8
<p>Farmers’ interface for data visualization.</p>
Full article ">Figure 9
<p>Oil palm plantation flood classification module.</p>
Full article ">Figure 10
<p>Oil palm bunches ripeness classification module.</p>
Full article ">Figure 11
<p>Flood-affected oil palm plantations or plots during harvest.</p>
Full article ">Figure 12
<p>Flooded areas with unripe oil palm bunches on trees.</p>
Full article ">Figure 13
<p>Oil palm plantations not affected by flooding (Ripe).</p>
Full article ">Figure 14
<p>Oil palm plantations not affected by flooding (Unripe).</p>
Full article ">Figure 15
<p>Dashboard visualization.</p>
Full article ">
23 pages, 299 KiB  
Article
Co-Creating Educational Action to Protect Children After DANA Floods in Spain
by Esther Roca-Campos, Sara Carbonell-Sevilla, Josep M. Canal-Barbany, Mireia Barrachina-Sauri, Sandra Girbés-Peco, Elisenda Giner-Gota and Ramón Flecha
Sustainability 2025, 17(4), 1542; https://doi.org/10.3390/su17041542 - 13 Feb 2025
Abstract
On 29 October 2024, Spain suffered the impact of an Isolated Depression at High Levels (DANA) that caused severe human and material damage. As seen in cases of natural disasters of similar magnitudes, the impact on children requires sustained interventions, with educational communities [...] Read more.
On 29 October 2024, Spain suffered the impact of an Isolated Depression at High Levels (DANA) that caused severe human and material damage. As seen in cases of natural disasters of similar magnitudes, the impact on children requires sustained interventions, with educational communities being key settings for providing protection and accompaniment. Although numerous studies highlight the role of schools in preventing and mitigating the socio-emotional impact of natural disasters on children, the literature on concrete educational actions to address the consequences of flood disasters is limited. This study analyses the co-creation process of six actions developed between researchers and teachers from 18 schools in the most affected areas of Valencia. For this purpose, a communicative research methodology was used. The techniques used to co-create actions were six dialogic focus groups, one dialogical scientific gathering and one WhatsApp community with teachers affected by the DANA. The results provide information on the redevelopment of the following six evidence-based actions and their impacts in the first weeks after the DANA: (1) the mapping of educational communities; (2) the planning of dialogic gatherings; (3) the creation of solidarity networks; (4) the creation of optimal learning environments; (5) the preservation of violence-free networks; and (6) the giving of specific support to vulnerable groups. The study offers guidelines for educational practises in flood-related disaster interventions, focusing on enhancing community resilience. Full article
20 pages, 8786 KiB  
Article
Experimental Investigation of the Influence of Milling Conditions on Residual Stress in the Surface Layer of an Aerospace Aluminum Alloy
by Magdalena Zawada-Michałowska, Kamil Anasiewicz, Jarosław Korpysa and Paweł Pieśko
Materials 2025, 18(4), 811; https://doi.org/10.3390/ma18040811 - 12 Feb 2025
Abstract
In this study, the correlations between milling conditions—namely, the cutting tool feed direction relative to the rolling direction, the milling type, the coolant application, as well as the cutting speed—and the surface residual stress of a selected aluminum alloy (2024 T351) were investigated. [...] Read more.
In this study, the correlations between milling conditions—namely, the cutting tool feed direction relative to the rolling direction, the milling type, the coolant application, as well as the cutting speed—and the surface residual stress of a selected aluminum alloy (2024 T351) were investigated. Determining the type and magnitude of residual stress is of paramount importance as this stress is among the primary causes of post-machining strain of thin-walled components. On the basis of the experimental results, it was found that all factors analyzed significantly affect the residual stress state. Specifically, milling in the parallel direction induces lower residual tensile stress compared to milling in the perpendicular direction. Analogously, up-milling yields lower tensile residual stress than down-milling, and flood cooling leads to lower tensile residual stress than MQL. It was clearly confirmed that as cutting speed increases, tensile residual stress also increases, but only up to a certain threshold; once the high-speed cutting regime is reached, tensile residual stress begins to decrease. Consequently, the proper selection of milling parameters is a crucial consideration for optimizing machining processes and minimizing machining-induced residual stress. Full article
Show Figures

Figure 1

Figure 1
<p>Research plan.</p>
Full article ">Figure 2
<p>Experimental procedure.</p>
Full article ">Figure 3
<p>Example of the single measurement result of surface residual stress (<span class="html-italic">v<sub>c</sub></span> = 750 m/min, up-milling, MQL, parallel feed direction relative to rolling direction).</p>
Full article ">Figure 4
<p>Comparison of residual stress for parallel and perpendicular cutting tool feed directions relative to rolling direction as a function of cutting speed under up-milling and flood cooling.</p>
Full article ">Figure 5
<p>Comparison of residual stress for parallel and perpendicular cutting tool feed directions relative to rolling direction as a function of cutting speed under down-milling and flood cooling.</p>
Full article ">Figure 6
<p>Comparison of residual stress for parallel and perpendicular cutting tool feed directions relative to rolling direction as a function of cutting speed under up-milling and MQL.</p>
Full article ">Figure 7
<p>Comparison of residual stress for parallel and perpendicular cutting tool feed directions relative to rolling direction as a function of cutting speed under down-milling and MQL.</p>
Full article ">Figure 8
<p>Comparison of residual stress for up and down-milling as a function of cutting speed under perpendicular feed direction relative to rolling direction and flood cooling.</p>
Full article ">Figure 9
<p>Comparison of residual stress for up and down-milling as a function of cutting speed under perpendicular feed direction relative to rolling direction and MQL.</p>
Full article ">Figure 10
<p>Comparison of residual stress for up and down-milling as a function of cutting speed under parallel feed direction relative to rolling direction and flood cooling.</p>
Full article ">Figure 11
<p>Comparison of residual stress for up and down-milling as a function of cutting speed under parallel feed direction relative to rolling direction and MQL.</p>
Full article ">Figure 12
<p>Comparison of residual stress for flood cooling and MQL as a function of cutting speed under perpendicular feed direction relative to rolling direction and up-milling.</p>
Full article ">Figure 13
<p>Comparison of residual stress for flood cooling and MQL as a function of cutting speed under perpendicular feed direction relative to rolling direction and down-milling.</p>
Full article ">Figure 14
<p>Comparison of residual stress for flood cooling and MQL as a function of cutting speed under parallel feed direction relative to rolling direction and up-milling.</p>
Full article ">Figure 15
<p>Comparison of residual stress for flood cooling and MQL as a function of cutting speed under parallel feed direction relative to rolling direction and down-milling.</p>
Full article ">Figure 16
<p>Residual stress as a function of cutting speed with different milling combinations and parallel feed direction of the cutting tool with respect to the rolling direction.</p>
Full article ">Figure 17
<p>Residual stress as a function of cutting speed with different milling combinations and perpendicular feed direction of the cutting tool relative to the rolling direction.</p>
Full article ">Figure 18
<p>Interaction plots for ANOVA.</p>
Full article ">
21 pages, 6975 KiB  
Article
A Real-Time Water Level and Discharge Monitoring Station: A Case Study of the Sakarya River
by Fatma Demir and Osman Sonmez
Appl. Sci. 2025, 15(4), 1910; https://doi.org/10.3390/app15041910 - 12 Feb 2025
Abstract
This study details the design and implementation of a real-time river monitoring station established on the Sakarya River, capable of instantaneously tracking water levels and flow rates. The system comprises an ultrasonic distance sensor, a GSM module (Global System for Mobile Communications), which [...] Read more.
This study details the design and implementation of a real-time river monitoring station established on the Sakarya River, capable of instantaneously tracking water levels and flow rates. The system comprises an ultrasonic distance sensor, a GSM module (Global System for Mobile Communications), which enables real-time wireless data transmission to a server via cellular networks, a solar panel, a battery, and a microcontroller board. The river monitoring station operates by transmitting water level data collected by the ultrasonic distance sensor to a server via a communication module developed on a microcontroller board using an Arduino program, and then sharing these data through a web interface. The developed system performs regular and continuous water level readings without the need for human intervention. During the installation and calibration of the monitoring station, laboratory and field tests were conducted, and the obtained data were validated by comparison with data from the hydropower plant located upstream. This system, mounted on a bridge, measures water levels twice per minute and sends these data to the relevant server via the GSM module. During this process, precipitation data were utilized as a critical reference point for validating measurement data for the 2023 hydrological year, with changes in precipitation directly correlated with river water levels and calculated flow values, which were analyzed accordingly. The real-time river monitoring station allows for instantaneous monitoring of the river, achieving a measurement accuracy of within 0.1%. The discharge values recorded by the system showed a high correlation (r2 = 0.92) with data from the hydropower plant located upstream of the system, providing an accurate and comprehensive database for water resource management, natural disaster preparedness, and environmental sustainability. Additionally, the system incorporates early warning mechanisms that activate when critical water levels are reached, enabling rapid response to potential flood risks. By combining energy-independent operation with IoT (Internet Of Things)-based communication infrastructure, the developed system offers a sustainable solution for real-time environmental monitoring. The system demonstrates strong applicability in field conditions and contributes to advancing technologies in flood risk management and water resource monitoring. Full article
Show Figures

Figure 1

Figure 1
<p>Örencik Bridge and Doğançay HPP I.</p>
Full article ">Figure 2
<p>Real-Time River Monitoring Station Components.</p>
Full article ">Figure 3
<p>Cabin Design.</p>
Full article ">Figure 4
<p>Monitoring Station Integrated Components.</p>
Full article ">Figure 5
<p>Arduino Program Interface and Protocols.</p>
Full article ">Figure 6
<p>Php Functions.</p>
Full article ">Figure 7
<p>Arduino–Sensor Connection Flowchart.</p>
Full article ">Figure 8
<p>Laboratory calibration.</p>
Full article ">Figure 9
<p>Field Calibration.</p>
Full article ">Figure 10
<p>Real-Time Flow Monitoring Station Cabin Installation.</p>
Full article ">Figure 11
<p>Topography of the River and RMS (River Monitoring Station) Location.</p>
Full article ">Figure 12
<p>Schematic Representation of Sensor Placement on Örencik Bridge.</p>
Full article ">Figure 13
<p>Comparison of Hourly Discharge Variations.</p>
Full article ">Figure 14
<p>Comparison of Daily Discharge Variations.</p>
Full article ">Figure 15
<p>Comparison of Monthly Discharge Variations.</p>
Full article ">Figure 16
<p>River Monitoring Station 2023 Hydrological Year Discharge Variation and Daily Total Precipitation.</p>
Full article ">Figure 17
<p>Seasonal Water Level Variation in River Monitoring Station and Daily Total Precipitation.</p>
Full article ">Figure 18
<p>Seasonal Discharge Variation In River Monitoring Station.</p>
Full article ">
24 pages, 6082 KiB  
Article
Research on Joint Operation of Flood Diversion and Storage Measures: A Case Study of Poyang Lake
by Shupan Deng, Zhichao Wang, Longhua Wu, Ting Wu, Yang Xia and Yue Liu
Sustainability 2025, 17(4), 1522; https://doi.org/10.3390/su17041522 - 12 Feb 2025
Abstract
In recent years, flood hazards have occurred increasingly worldwide, posing significant threats to the safety of life and property in lacustrine and riverine environments. To mitigate the devastating impacts of floods, it is crucial to explore optimal strategies for joint flood diversion of [...] Read more.
In recent years, flood hazards have occurred increasingly worldwide, posing significant threats to the safety of life and property in lacustrine and riverine environments. To mitigate the devastating impacts of floods, it is crucial to explore optimal strategies for joint flood diversion of flood diversion and storage measures (FDSM). The FDSM management of Poyang Lake in China focuses on studying semi-restoration polder areas (SR Polders) and flood storage and detention areas (FS Detentions), which are subjects of ongoing research. Existing studies primarily focus on SR Polders or FS Detentions, with limited research on the joint flood diversion potential of these two measures, particularly regarding optimal scheduling. This study takes 185 SR Polders and the Kangshan flood storage and detention area (KS Detention) as the primary research objects. By integrating hydraulic theory, numerical simulation techniques, and survey data, we develop a hydraulic model for the SR Polders and a hydrodynamic model for the KS Detention to carry out flood diversion simulation. The 1998 flood is chosen as a typical case to simulate and analyze their flood diversion processes under various schemes. The results indicate that altering the operation criteria for FDSM influences both the maximum diversion discharge and the timing of the main diversion period. For the SR Polders, under the current flood control scheme, raising the operation water level (OWL) of SR Polders-I by 1.0 m increases the maximum diversion discharge by 894 m3/s. Additionally, raising the OWL of SR Polders-II by 0.37 m delays the main diversion period by one day. For the KS Detention, higher flood diversion water levels correspond to greater discharge capacities. Furthermore, a fuzzy optimization method is applied to optimize nine joint schemes of the SR Polders and KS Detention. The results indicate that the optimal joint flood diversion strategy for Poyang Lake is operating SR Polders-I, SR Polders-II, and KS Detention at a Hukou water level of 21.65 m, 22.05 m, and 22.50 m, respectively. Finally, the study provides insights and recommendations for flood control management at Poyang Lake. The results of this study not only have important guiding significance for flood control management of large plain lakes but also provide references for the joint operation of flood diversion and storage areas in other regions. Full article
(This article belongs to the Special Issue Sustainable Water Management in Rapid Urbanization)
Show Figures

Figure 1

Figure 1
<p>Geographic location of Poyang Lake and relevant hydrological stations [<a href="#B10-sustainability-17-01522" class="html-bibr">10</a>].</p>
Full article ">Figure 2
<p>The Zenglong SR Polder located in Zenglong Village, Jiangyi Town, Gongqingcheng County, Jiujiang City, Jiangxi Province.</p>
Full article ">Figure 3
<p>Statistics of flood diversion facilities of SR Polders in three cities.</p>
Full article ">Figure 4
<p>The physical model of flood diversion gates of KS Detention [<a href="#B10-sustainability-17-01522" class="html-bibr">10</a>].</p>
Full article ">Figure 5
<p>The model testing results about the downstream water level and the flood diversion discharge with the 28 gates fully opened, where orange points indicate test results under two notable conditions.</p>
Full article ">Figure 6
<p>The flood diversion calculation process of hydraulic model for SR Polders.</p>
Full article ">Figure 7
<p>The hydrodynamic model of KS Detention [<a href="#B10-sustainability-17-01522" class="html-bibr">10</a>].</p>
Full article ">Figure 8
<p>The experimental and simulated values of flood diversion discharge under different downstream water levels.</p>
Full article ">Figure 9
<p>The changes in flood diversion discharge of SR Polders in different schemes.</p>
Full article ">Figure 10
<p>The changes in cumulative flood diversion volume of SR Polders in different schemes.</p>
Full article ">Figure 11
<p>The changes in flood diversion discharge of KS Detention in different schemes.</p>
Full article ">Figure 12
<p>The changes in cumulative flood diversion volume of KS Detention in different schemes.</p>
Full article ">Figure 13
<p>The water level of Xingzi Station before the implementation of the SR Polders and KS Detention for different schemes.</p>
Full article ">
29 pages, 13238 KiB  
Article
Spatial Insights for Building Resilience: The Territorial Risk Management & Analysis Across Scale Framework for Bridging Scales in Multi-Hazard Assessment
by Francesca Maria Ugliotti, Muhammad Daud and Emmanuele Iacono
Smart Cities 2025, 8(1), 27; https://doi.org/10.3390/smartcities8010027 - 11 Feb 2025
Abstract
In an era of increasingly abundant and granular spatial and temporal data, the traditional divide between environmental GIS and building-centric BIM scales is diminishing, offering an opportunity to enhance natural hazard assessment by bridging the gap between territorial impacts and the effects on [...] Read more.
In an era of increasingly abundant and granular spatial and temporal data, the traditional divide between environmental GIS and building-centric BIM scales is diminishing, offering an opportunity to enhance natural hazard assessment by bridging the gap between territorial impacts and the effects on individual structures. This study addresses the challenge of integrating disparate data formats by establishing a centralised database as the foundation for a comprehensive risk assessment approach. A use case focusing on flood risk assessment for a public building in northwest Italy demonstrates the practical implications of this integrated methodology. The proposed TErritorial RIsk Management & Analysis Across Scale (TERIMAAS) framework utilises this centralised repository to store, process, and dynamically update diverse BIM and GIS datasets, incorporating real-time IoT-derived information. The GIS spatial analysis assesses risk scores for each hazard type, providing insights into vulnerability and potential impacts. BIM data further refine this assessment by incorporating building and functional characteristics, enabling a comprehensive evaluation of resilience and risk mitigation strategies tailored to dynamic environmental conditions across scales. The results of the proposed scalable approach could provide a valuable understanding of the territory for policymakers, urban planners, and any stakeholder involved in disaster risk management and infrastructure resilience planning. Full article
(This article belongs to the Section Smart Buildings)
Show Figures

Figure 1

Figure 1
<p>Strengthening building resilience through IoT-driven environmental data integration.</p>
Full article ">Figure 2
<p>The “House of Digital Twin”, illustrating the essential components of a DT [<a href="#B17-smartcities-08-00027" class="html-bibr">17</a>].</p>
Full article ">Figure 3
<p>The DT domain: connecting the building detail with world scale for integrated hazard assessment.</p>
Full article ">Figure 4
<p>Conceptual design of the TERIMAAS multi-hazard framework.</p>
Full article ">Figure 5
<p>Natural hazard types mapped by spatial and temporal scales [<a href="#B46-smartcities-08-00027" class="html-bibr">46</a>].</p>
Full article ">Figure 6
<p>Technical framework of TERIMAAS, highlighting software and data management processes.</p>
Full article ">Figure 7
<p>The selected case study building (marked in red) and its related territorial context. The figure highlights how the area is interested by medium-high probability of flood events.</p>
Full article ">Figure 8
<p>(<b>a</b>) The school building used as a case study, and (<b>b</b>) its corresponding BIM model for assessment and visualisation purposes.</p>
Full article ">Figure 9
<p>Integrated database demonstration including all GIS, IoT, and BIM domains.</p>
Full article ">Figure 10
<p>Dynamo script for the vulnerability and exposure assessment calculations of selected BIM model elements, and the colour-coded visualisation of the risk results.</p>
Full article ">Figure 11
<p>Probability-based flooding risk visualisation for building elements on weekdays, accounting for exposure due to building occupancy: room elements (<b>a</b>,<b>b</b>), structural elements (<b>c</b>,<b>d</b>), and door/window elements (<b>e</b>,<b>f</b>) at 06:00 A.M. (<b>a</b>,<b>c</b>,<b>e</b>) and 11:00 A.M. (<b>b</b>,<b>d</b>,<b>f</b>). Increased occupancy during working hours contributes to higher overall risk.</p>
Full article ">
28 pages, 28459 KiB  
Article
Multi-Temporal Remote Sensing Satellite Data Analysis for the 2023 Devastating Flood in Derna, Northern Libya
by Roman Shults, Ashraf Farahat, Muhammad Usman and Md Masudur Rahman
Remote Sens. 2025, 17(4), 616; https://doi.org/10.3390/rs17040616 - 11 Feb 2025
Abstract
Floods are considered to be among the most dangerous and destructive geohazards, leading to human victims and severe economic outcomes. Yearly, many regions around the world suffer from devasting floods. The estimation of flood aftermaths is one of the high priorities for the [...] Read more.
Floods are considered to be among the most dangerous and destructive geohazards, leading to human victims and severe economic outcomes. Yearly, many regions around the world suffer from devasting floods. The estimation of flood aftermaths is one of the high priorities for the global community. One such flood took place in northern Libya in September 2023. The presented study is aimed at evaluating the flood aftermath for Derna city, Libya, using high resolution GEOEYE-1 and Sentinel-2 satellite imagery in Google Earth Engine environment. The primary task is obtaining and analyzing data that provide high accuracy and detail for the study region. The main objective of study is to explore the capabilities of different algorithms and remote sensing datasets for quantitative change estimation after the flood. Different supervised classification methods were examined, including random forest, support vector machine, naïve-Bayes, and classification and regression tree (CART). The various sets of hyperparameters for classification were considered. The high-resolution GEOEYE-1 images were used for precise change detection using image differencing (pixel-to-pixel comparison and geographic object-based image analysis (GEOBIA) for extracting building), whereas Sentinel-2 data were employed for the classification and further change detection by classified images. Object based image analysis (OBIA) was also performed for the extraction of building footprints using very high resolution GEOEYE images for the quantification of buildings that collapsed due to the flood. The first stage of the study was the development of a workflow for data analysis. This workflow includes three parallel processes of data analysis. High-resolution GEOEYE-1 images of Derna city were investigated for change detection algorithms. In addition, different indices (normalized difference vegetation index (NDVI), soil adjusted vegetation index (SAVI), transformed NDVI (TNDVI), and normalized difference moisture index (NDMI)) were calculated to facilitate the recognition of damaged regions. In the final stage, the analysis results were fused to obtain the damage estimation for the studied region. As the main output, the area changes for the primary classes and the maps that portray these changes were obtained. The recommendations for data usage and further processing in Google Earth Engine were developed. Full article
(This article belongs to the Special Issue Image Processing from Aerial and Satellite Imagery)
Show Figures

Figure 1

Figure 1
<p>Map of Libya with the location of Derna (P.C. BBC News after the Flooding).</p>
Full article ">Figure 2
<p>Pre-flood (1 July 2023) and post-flood (13 September 2023) images show damage caused by the collapse of the Derna Dam.</p>
Full article ">Figure 3
<p>Change detection analysis flowchart.</p>
Full article ">Figure 4
<p>Image differencing for Derna region using (<b>a</b>) band 1, (<b>b</b>) band 2, and (<b>c</b>) band 3.</p>
Full article ">Figure 5
<p>Area changes: (<b>a</b>) band 1, (<b>b</b>) band 2, and (<b>c</b>) band 3.</p>
Full article ">Figure 6
<p>Spectral indices and their changes for the Derna area using NDVI (<b>a</b>,<b>b</b>), SAVI (<b>c</b>,<b>d</b>), TNDVI (<b>e</b>,<b>f</b>), and NDMI (<b>g</b>,<b>h</b>).</p>
Full article ">Figure 6 Cont.
<p>Spectral indices and their changes for the Derna area using NDVI (<b>a</b>,<b>b</b>), SAVI (<b>c</b>,<b>d</b>), TNDVI (<b>e</b>,<b>f</b>), and NDMI (<b>g</b>,<b>h</b>).</p>
Full article ">Figure 7
<p>(<b>a</b>) Derna Region Random Forest Classification results for image dated (<b>a</b>) 18 August 2023 and (<b>b</b>) Derna Region Random Forest Classification dated 22 September 2023.</p>
Full article ">Figure 8
<p>Derna Region CART Classification results for image dated (<b>a</b>) 18 August 2023 and (<b>b</b>) Derna Region Random Forest Classification dated 22 September 2023.</p>
Full article ">Figure 9
<p>Derna Region Naïve Bayes Classification for 18 August 2023 (<b>a</b>) and 22 September 2023 (<b>b</b>).</p>
Full article ">Figure 10
<p>SVM hyperparameters and classification ways.</p>
Full article ">Figure 11
<p>Derna Region SVM Classification for 18 August 2023 (<b>a</b>) and 22 September 2023 (<b>b</b>).</p>
Full article ">Figure 12
<p>Derna Region SVM Classification, the polynomial kernel for 18 August 2023 (<b>a</b>) and 22 September 2023 (<b>b</b>).</p>
Full article ">Figure 13
<p>Building footprint extracted using GEOBIA and building damaged due to flash.</p>
Full article ">
17 pages, 3235 KiB  
Article
Toward Sustainable Infrastructure: Advanced Hazard Prediction and Geotechnical Risk Management in the Jiroft Dam Project, Iran
by Sanaz Soltaninejad, Mohammad Sina Abdollahi, Naveen BP, Seyed Morteza Marandi, Marziyeh Abdollahi and Saranaz Abdollahi
Sustainability 2025, 17(4), 1465; https://doi.org/10.3390/su17041465 - 11 Feb 2025
Abstract
The Jiroft Dam, situated in Kerman province, Iran, serves as a crucial infrastructure for water management, flood control, and agricultural development in the region. However, the surrounding mountainous terrain presents considerable geotechnical challenges that threaten the stability of access roads and other essential [...] Read more.
The Jiroft Dam, situated in Kerman province, Iran, serves as a crucial infrastructure for water management, flood control, and agricultural development in the region. However, the surrounding mountainous terrain presents considerable geotechnical challenges that threaten the stability of access roads and other essential infrastructure. This study is based on comprehensive field surveys and mapping, which have revealed significant ground displacements and evidence of slope instabilities in the area. The investigation identifies key factors, including soil composition, rock formations, groundwater flow, and seismic activity, that contribute to these shifts in the terrain. To ensure the accuracy of the elevation data, the study employed Monte Carlo simulation techniques to analyze the statistical distribution of the collected survey data. By simulating various possible outcomes, this study enhanced the precision of the elevation models, allowing for better identification of critical instability zones. Additionally, the Overall Equipment Effectiveness (OEE) was utilized to evaluate the effectiveness of the current monitoring equipment and infrastructure, providing a clearer understanding of operational efficiency and areas for improvement. The findings of this study highlight the immediate need for effective risk management strategies to mitigate the potential hazards of landslides and infrastructure failure. Addressing these challenges is essential to ensure the long-term sustainability of the region’s infrastructure. In response to these observations, this research proposes practical engineering solutions such as slope stabilization techniques and improved drainage systems to address the identified instabilities. Furthermore, this study underscores the necessity of the continuous monitoring and the implementation of early warning systems to detect further ground movements and mitigate associated risks.In addition to technical interventions, this research emphasizes the importance of integrating local knowledge and expertise into the risk management process. Full article
Show Figures

Figure 1

Figure 1
<p>Jiroft Dam and Halil River valley.</p>
Full article ">Figure 2
<p>(<b>A</b>,<b>B</b>) The fracture and weathering zones along the Jiroft Dam path. (<b>C</b>,<b>D</b>) The position of the dam spillway channel among unstable areas. (<b>E</b>) The dam spillway channel runs parallel to the river and is connected to it through a curved path.</p>
Full article ">Figure 3
<p>Impact of seasonal rainfall on road stability, shown from the left and right perspectives of the same section of the road.</p>
Full article ">Figure 4
<p>(<b>A</b>) Survey location and topography and (<b>B</b>) survey pattern.</p>
Full article ">Figure 5
<p>Vertical displacement of various points.</p>
Full article ">Figure 6
<p>Operational flowchart for Jiroft Dam.</p>
Full article ">
15 pages, 2370 KiB  
Article
Mechanisms of Permeability Alteration via Gel Based on Nuclear Magnetic Resonance
by Bin Zou, Chuanzhi Cui, Wangang Zheng, Weiyao Zhu, Haishun Feng, Wei Chu, Tiantian Yu and Zhongping Zhang
Processes 2025, 13(2), 497; https://doi.org/10.3390/pr13020497 - 11 Feb 2025
Abstract
DPR refers to the fact that the reduction in the permeability of the water phase is much greater than the reduction in the permeability of the oil phase when a water-based gel seals porous media. In order to clarify the mechanisms of the [...] Read more.
DPR refers to the fact that the reduction in the permeability of the water phase is much greater than the reduction in the permeability of the oil phase when a water-based gel seals porous media. In order to clarify the mechanisms of the gel-plugging pore pathway and the principle of the oil phase and water-phase permeability change, gel-plugging core replacement experiments and NMR T2 scanning experiments were conducted in this work. Based on the nuclear NMR T2 spectroscopy, the core blocked with Cr (III)–acetate–HPAM gel is divided into five stages (a plug injection and seal gel-formation stage, an oil-phase repulsion stage, a stopping-gel reabsorption stage, an oil-phase reinjection stage, and a subsequent water-drive stage) for displacement and scanning, and the signal changes of various phases in the displacement process are studied. The principle of an oil-phase permeability increase after Cr (III)–acetate–HPAM gel plugging, and the principle of a disproportionate decrease in water-phase permeability in the subsequent water-flooding stage were finally revealed. According to the results, the difference in the permeability leads to some diversity in NMR T2 curves, but the final conclusions for the mechanisms are consistent. They show a significant decrease in core permeability of 3.5 × 10−3 μm2 and 0.8 × 10−3 μm2 after gel plugging. With the injection of the oil phase, the permeability of the oil phase keeps increasing from 0.13 × 10−3 μm2 to 0.76 × 10−3 μm2 in the core permeability of 3.5 × 10−3 μm2. Similarly, the permeability of the oil phase increases from 0.03 × 10−3 μm2 to 0.19 × 10−3 μm2 in the core permeability of 0.8 × 10−3 μm2. During the oil-phase replacement phase, gel replacement in the large pores is the main cause of the increase in oil-phase permeability, and as the replacement process progresses, the mechanism for the increase in oil-phase permeability changes, and gel dehydration becomes the main mechanism for the increase in oil-phase permeability. Full article
(This article belongs to the Special Issue Research Progress of Chemical Flooding for Enhanced Oil Recovery)
Show Figures

Figure 1

Figure 1
<p>Experimental flow diagram.</p>
Full article ">Figure 2
<p>Change in permeability of oil and water phases (3.5 × 10<sup>−3</sup> μm<sup>2</sup>).</p>
Full article ">Figure 3
<p>Change in permeability of oil and water phases (0.8 × 10<sup>−3</sup> μm<sup>2</sup>).</p>
Full article ">Figure 4
<p>Changes in the ratio of oil–water permeability during gel flooding.</p>
Full article ">Figure 5
<p>T2 spectra of different injected fluids at the initial stage.</p>
Full article ">Figure 6
<p>T2 spectra of different oil phase injections (3.5 × 10<sup>−3</sup> μm<sup>2</sup>).</p>
Full article ">Figure 7
<p>T2 spectrum of different oil phases’ injections (0.8 × 10<sup>−3</sup> μm<sup>2</sup>).</p>
Full article ">Figure 8
<p>T2 spectrum of different oil phases’ injections (3.5 × 10<sup>−3</sup> μm<sup>2</sup>).</p>
Full article ">Figure 9
<p>T2 spectrum of different oil and water phases’ injections (3.5 × 10<sup>−3</sup> μm<sup>2</sup>).</p>
Full article ">Figure 10
<p>T2 spectrum of different oil and water phases’ injections (0.8 × 10<sup>−3</sup> μm<sup>2</sup>).</p>
Full article ">
24 pages, 1967 KiB  
Review
Research Status and Trends of Hydrodynamic Separation (HDS) for Stormwater Pollution Control: A Review
by Yah Loo Wong, Yixiao Chen, Anurita Selvarajoo, Chung Lim Law and Fang Yenn Teo
Water 2025, 17(4), 498; https://doi.org/10.3390/w17040498 - 10 Feb 2025
Abstract
Growing urbanization has increased impermeable surfaces, raising and polluting stormwater runoff, and exacerbating the risk of urban flooding. Effective stormwater management is essential to curb sedimentation, minimize pollution, and mitigate urban flooding. This systematic literature review from the Web of Science and Scopus [...] Read more.
Growing urbanization has increased impermeable surfaces, raising and polluting stormwater runoff, and exacerbating the risk of urban flooding. Effective stormwater management is essential to curb sedimentation, minimize pollution, and mitigate urban flooding. This systematic literature review from the Web of Science and Scopus between January 2000 and June 2024 presents hydrodynamic separation (HDS) technologies. It sheds light on the significant issues that urban water management faces. HDS is classified into four categories: screening, filtration, settling, and flotation, based on the treatment mechanisms. The results show a shift from traditional standalone physical separations to multi-stage hybrid treatment processes with nature-based solutions. The great advantage of these approaches is that they combine different separation mechanisms and integrate ecological sustainability to manage urban stormwater better. The findings showed that future research will examine hybrid AI-assisted separation technologies, biochar-enhanced filtration, and green infrastructure systems. When adopting an integrated approach, the treatment system will perform like natural processes to remove pollutants effectively with better monitoring and controls. These technologies are intended to fill existing research voids, especially in removing biological contaminants and new pollutants (e.g., microplastics and pharmaceutical substances). In the long term, these technologies will help to enforce Sustainable Development Goals (SDGs) and orient urban areas in developing countries towards meeting the circular economy objective. Full article
(This article belongs to the Section Urban Water Management)
Show Figures

Figure 1

Figure 1
<p>Flow diagram of overall process.</p>
Full article ">Figure 2
<p>Time variation in the number of publications from 2000 to 2004.</p>
Full article ">Figure 3
<p>Geographical distribution of publications.</p>
Full article ">Figure 4
<p>Time variation in the publications on different types of pollutants (indicates with different colors).</p>
Full article ">Figure 5
<p>Classification of stormwater treatment devices.</p>
Full article ">Figure 6
<p>Percentage of publications for each type of separation.</p>
Full article ">
22 pages, 4242 KiB  
Article
Spatiotemporal Evolution and Determinants of Urban Flood Resilience: A Case Study of Yellow River Basin
by Jie Liu, Xinyu Wang and Gongjing Gao
Sustainability 2025, 17(4), 1433; https://doi.org/10.3390/su17041433 - 10 Feb 2025
Abstract
Global climate change has intensified flood disasters at the local scale. In response, this study constructs a flood resilience indicator system at the urban scale based on the “pressure-state-response” (PSR) model. Indicator weights were determined using the analytic hierarchy process–entropy weight method (AHP-EWM), [...] Read more.
Global climate change has intensified flood disasters at the local scale. In response, this study constructs a flood resilience indicator system at the urban scale based on the “pressure-state-response” (PSR) model. Indicator weights were determined using the analytic hierarchy process–entropy weight method (AHP-EWM), the flood resilience of 35 cities within the Yellow River Basin from 2010 to 2021, and their spatiotemporal evolution patterns, spatial correlations, and determinants were analyzed. The results indicate that flood resilience shows an upward trend over time, with stronger resilience observed in upstream and downstream cities and weaker resilience in midstream cities. The spatial correlation of flood resilience was significantly positive in 2010, 2015, and 2021, while it exhibited non-significant, fluctuating declines in other years. Most cities in Henan and Shandong provinces are characterized as high–high agglomeration type, whereas most cities in Shanxi and Shaanxi provinces are classified as low–low type. Drainage efficiency, municipal investment, resilient planning, and urbanization have significant positive impacts on flood resilience, while the urban registered unemployment rate shows a positive spatial spillover effect. This study analyzed the flood resilience of cities in the Yellow River Basin from a comprehensive and logically coherent perspective and concluded with targeted recommendations aimed at enhancing flood resilience in the region. Full article
(This article belongs to the Section Hazards and Sustainability)
Show Figures

Figure 1

Figure 1
<p>Correlation matrix among indicators. Note: The upper right section represents Pearson correlation coefficients, while the lower left section represents Spearman rank correlation coefficients.</p>
Full article ">Figure 2
<p>Study area.</p>
Full article ">Figure 3
<p>The temporal change of urban flood resilience and each layer’s level for the Yellow River Basin as a whole, 2010–2021.</p>
Full article ">Figure 4
<p>The spatial distribution and change of urban flood resilience in the Yellow River Basin, 2010–2021.</p>
Full article ">Figure 5
<p>Global Moran’s index and local Moran’s index for cities in the Yellow River Basin for the years 2010, 2015, and 2021.</p>
Full article ">
Back to TopTop