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23 pages, 8605 KiB  
Article
Displacement Interval Prediction Method for Arch Dam with Cracks: Integrated STL, MF-DFA and Bootstrap
by Zeyuan Chen, Bo Xu, Linsong Sun, Xuan Wang, Dalai Song, Weigang Lu and Yangtao Li
Water 2024, 16(19), 2755; https://doi.org/10.3390/w16192755 - 27 Sep 2024
Abstract
Displacement prediction models based on measured data have been widely applied in structural health monitoring. However, most models neglect the particularity of displacement monitoring for arch dams with cracks, nor do they thoroughly analyze the non-stationarity and uncertainty of displacement. To address this [...] Read more.
Displacement prediction models based on measured data have been widely applied in structural health monitoring. However, most models neglect the particularity of displacement monitoring for arch dams with cracks, nor do they thoroughly analyze the non-stationarity and uncertainty of displacement. To address this issue, the influencing factors of displacement were first considered, with crack opening displacement being incorporated into them, leading to the construction of the HSCT model that accounts for the effects of cracks. Feature selection was performed on the factors of the HSCT model utilizing the max-relevance and min-redundancy (mRMR) algorithm, resulting in the screened subset of displacement influence factors. Next, displacement was decomposed into trend, seasonal, and remainder components applying the seasonal-trend decomposition using loess (STL) algorithm. The multifractal characteristics of these displacement components were then analyzed by multifractal detrended fluctuation analysis (MF-DFA). Subsequently, displacement components were predicted employing the convolutional neural network-long short-term memory (CNN-LSTM) model. Finally, the impact of uncertainty factors was quantified using prediction intervals based on the bootstrap method. The results indicate that the proposed methods and models are effective, yielding satisfactory prediction accuracy and providing scientific basis and technical support for the health diagnosis of hydraulic structures. Full article
(This article belongs to the Special Issue Water Engineering Safety and Management)
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<p>Structure of CNN-LSTM network.</p>
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<p>Schematic diagram of prediction interval.</p>
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<p>Flow chart of displacement interval prediction method.</p>
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<p>Layout diagram of plumb line measuring points.</p>
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<p>Schematic diagram of the arch dam.</p>
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<p>Process lines of water level, temperature, and displacement.</p>
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<p>Crack opening displacement process lines of 19 measuring points: (<b>a</b>) automatic measuring point and (<b>b</b>) manual measuring point.</p>
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<p>Decomposition results of two monitoring points via STL: (<b>a</b>) PL8−U and (<b>b</b>) PL18−U.</p>
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<p>Variation of Hurst exponent at measuring points: (<b>a</b>) PL8−U and (<b>b</b>) PL18−U.</p>
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<p>Variation of Renyi exponent at measuring points: (<b>a</b>) PL8−U and (<b>b</b>) PL18−U.</p>
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<p>Multifractal spectrum of measuring points: (<b>a</b>) PL8−U and (<b>b</b>) PL18−U.</p>
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<p>Fitting curves and statistical indicators of various models at PL8−U: (<b>a</b>) SSA-ELM, (<b>b</b>) LSTM, and (<b>c</b>) CNN-LSTM.</p>
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<p>Fitting curves and statistical indicators of various models at PL18−U: (<b>a</b>) SSA-ELM, (<b>b</b>) LSTM, and (<b>c</b>) CNN-LSTM.</p>
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<p>Prediction intervals at 95% PINC of various models at PL8−U: (<b>a</b>) STL-SSA-ELM, (<b>b</b>) STL-LSTM, and (<b>c</b>) STL-CNN-LSTM.</p>
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<p>Prediction intervals at 95% PINC of various models at PL18−U: (<b>a</b>) STL-SSA-ELM, (<b>b</b>) STL-LSTM, and (<b>c</b>) STL-CNN-LSTM.</p>
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22 pages, 21487 KiB  
Article
Influence Mechanism of Water Level Variation on Deformation of Steep and Toppling Bedding Rock Slope
by Tiantao Li, Weiling Ran, Kaihong Wei, Jian Guo, Shihua Chen, Xuan Li, Mingyang Chen and Xiangjun Pei
Water 2024, 16(19), 2706; https://doi.org/10.3390/w16192706 - 24 Sep 2024
Abstract
The construction of major hydropower projects globally is challenged by slope deformation in reservoir areas. The deformation and failure mechanisms of large rock slopes are complex and poorly understood, making prevention and management extremely challenging. In order to explore the influence mechanism of [...] Read more.
The construction of major hydropower projects globally is challenged by slope deformation in reservoir areas. The deformation and failure mechanisms of large rock slopes are complex and poorly understood, making prevention and management extremely challenging. In order to explore the influence mechanism of the water level variation on the deformation of steep toppling bedding rock slopes, this paper takes the right bank slope near the dam area of the Longtou Hydropower Station as an example, and field investigations, deformation monitoring, physical simulation tests and numerical analyses are carried out. It is found that the slope deformation response is obvious under the influence of the reservoir water level variation, which is mainly reflected in the change in the slope groundwater level, rock mechanical parameters and seepage field in the slope body. The toe of the slope produces plastic deformation and maximum displacement. With the increase in the reservoir water level, the plastic zone expands and the displacement increases, which leads to the intensification of the slope deformation. This paper puts forward that the deformation and failure modes of the steep and toppling bedding rock slope caused by water level variation are due to shear dislocation, bending deformation and toppling fracture. This study reveals the influence mechanism of the water level variation on the deformation of steep and toppling bedding rock slopes, which can provide theoretical support for the construction of major hydropower projects. Full article
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<p>Location and regional geological map of the research area: (<b>a</b>) Map of China; (<b>b</b>) Map of Sichuan Province; (<b>c</b>) The regional geological map.</p>
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<p>Engineering geological plan.</p>
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<p>Slope panoramic picture.</p>
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<p>Engineering geological profile of typical section 1–1’.</p>
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<p>Sketch of the 1–1 adit.</p>
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<p>Sketch of the 1–2 adit.</p>
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<p>Relationship of rock mass toppling deformation with the dip angle and horizontal depth.</p>
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<p>The toppling deformation degree (with the increase in the toppling deformation degree, the deformable body is divided into the normal rock mass, the toppling zone, the strong toppling–weak loosening fracture zone and the strong toppling–loosening fracture zone).</p>
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<p>Zoning map of the slope. The slope is divided into 3 zones: zone II has 3 small zones and zone III has 2 small zones.</p>
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<p>Monitoring point layout.</p>
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<p>Displacement curve from 1 March 2013 to 1 September 2014.</p>
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<p>Cumulative displacement from 1 March 2013 to 1 September 2014.</p>
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<p>Displacement rate from 1 March 2013 to 1 September 2014.</p>
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<p>Displacement curve from 1 September 2014 to 1 September 2021.</p>
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<p>Cumulative displacement from 1 September 2014 to 1 September 2021.</p>
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<p>Displacement rate from 1 September 2014 to 1 September 2016.</p>
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<p>Slope deformation zone (according to the cumulative displacement, the slope is divided into 5 zones, and they are similar to the engineering geological zoning).</p>
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<p>Displacement vector: (<b>a</b>) Before the first stage of water storage; (<b>b</b>) Stage I water storage to stage II water storage; (<b>c</b>) After the second stage of water storage. The red arrow means the maximum displacement, and the blue arrow means the minimum displacement.</p>
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<p>Rock deterioration curve under the saturation state: (<b>a</b>) Cohesion and friction angle of the fault fracture zone and strong toppling–loosening zone; (<b>b</b>) Cohesion and friction angle of the normal rock mass.</p>
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<p>Rock deterioration curve under the dry–wet cycle state: (<b>a</b>) Cohesion and friction angles of the fault fracture zone and strong toppling–loosening zone; (<b>b</b>) Cohesion and friction angle of the normal rock mass.</p>
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<p>Computational model.</p>
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<p>Volumetric water content and hydraulic conductivity: A: avalanche deposit; B: sand soil layer; C: strong toppling–loosening fracture zone; D: strong toppling–weak loosening fracture zone; E: toppling zone; F: fault-affected zone; G: interbedded sandstone and slate; H: slate.</p>
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<p>Seepage field and seepage curve with different rates of water level increase: (<b>a</b>) Water level increases at a rate of 0.4 m/d; (<b>b</b>) Water level increases at a rate of 0.8 m/d; (<b>c</b>) Water level increases at a rate of 1.6 m/d; (<b>d</b>) Seepage curve at different rates of water level increase.</p>
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<p>Seepage field and seepage curve with different rates of water level decrease: (<b>a</b>) Water level decreases at a rate of 0.4 m/d; (<b>b</b>) Water level decreases at a rate of 0.8 m/d; (<b>c</b>) Water level decreases at a rate of 1.6 m/d; (<b>d</b>) Seepage curve at different rates of water level decrease.</p>
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<p>Zones in the model (the model is divided into the saturation area, fault, water-level-variation area and above-water area).</p>
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<p>Results under a single time of reservoir water level variation: (<b>a</b>) Displacement result; (<b>b</b>) Displacement vector and plastic deformation.</p>
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<p>Results under five times of reservoir water level variations: (<b>a</b>). Displacement result; (<b>b</b>) Displacement vector and plastic deformation.</p>
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<p>The deformation response process of the water level variation: (<b>a</b>) The steep bedding rock mass topples and deforms due to the downward cutting of the valley and the unloading rebound in the early stage; (<b>b</b>) The reservoir water level variation leads to the deterioration of the rock mass, and the rock stratum at the toe of the slope will creep; (<b>c</b>) The strong toppling rock mass at the rear of the slope further topples and deforms, and the shear slide occurs in the middle and lower parts of the slope. The slope toppling deformation is aggravated by the development and evolution of tensile cracks in the rock mass.</p>
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<p>The evolutionary stages of the deformable body: (<b>a</b>). Unloading rebound stage; (<b>b</b>) Toppling creep stage; (<b>c</b>) Partial fracture stage.</p>
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<p>The slide and fracturing deformation phenomena. The arrows mean the direction of slip.</p>
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13 pages, 9816 KiB  
Article
Sustainable Utilization of Stabilized Dredged Material for Coastal Infrastructure: Innovations in Non-Fired Brick Production and Erosion Control
by Thi Thuy Minh Nguyen, Saeed Rabbanifar, Aalok Sharma Kafle, Reid Johnson, Brian Bonner, Dason Fernandez, Fernando Aleman, Jared Defrancis, Chun-Wei Yao, Xianchang Li, Mien Jao and Paul Bernazzani
Appl. Sci. 2024, 14(18), 8544; https://doi.org/10.3390/app14188544 - 23 Sep 2024
Abstract
The deterioration of dams and levees is an increasing concern for both infrastructure integrity and environmental sustainability. The extensive repercussions, including the displacement of communities, underscore the imperative for sustainable interventions. This study addresses these challenges by investigating the stabilization of dredged material [...] Read more.
The deterioration of dams and levees is an increasing concern for both infrastructure integrity and environmental sustainability. The extensive repercussions, including the displacement of communities, underscore the imperative for sustainable interventions. This study addresses these challenges by investigating the stabilization of dredged material (DM) for diverse applications. Seven mixtures incorporating fly ash, lime, and cement were formulated. The Standard Compaction Test was used to determine optimal density–moisture conditions, which helped with brick fabrication. Bricks were tested for compressive strength over various curing periods, and the durability of the 28-day-cured samples was evaluated by performing water immersion tests following the New Mexico Code specifications. Scanning electron microscopy (SEM) was used to assess microstructural bonding. Results confirm that the inclusion of cementitious stabilizers modifies the material’s microstructure, resulting in enhancements of both strength and water resistance. Notably, the stabilized material demonstrates potential for use in non-fired brick manufacturing and as bridge stones for waterway erosion control. This dual-function application offers a sustainable and economically feasible approach to managing dredged materials. Full article
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<p>Location overview of Placement Area 9 (PA9): (<b>A</b>) a GIS map highlighting the location of PA9 within Texas; (<b>B</b>) a detailed GIS map showing the boundaries of PA9; (<b>C</b>) an aerial photograph depicting the surrounding area of PA9; (<b>D</b>) an aerial photograph providing a close-up view of PA9.</p>
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<p>The brick fabrication process involves the drying of DM and the mixing of additives (panel (<b>A</b>)), the ensuring of proper moisture content (panel (<b>B</b>)), and the use of the Auram Press 3000 to make the compressed bricks (panel (<b>C</b>)). The final results: a series of bricks (panel (<b>D</b>)).</p>
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<p>Image of a typical compressed block from stabilized dredged material using mix design 4 (HL/FA/PC ratio of 35/80.5/10).</p>
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<p>Particle size distribution of DM and additives.</p>
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<p>Compaction data for varying contents of HL and FA (for PC = 10%).</p>
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<p>Compaction data for varying contents of HL and FA (for PC = 15%).</p>
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<p>Stabilized mixed at a fixed dosage of HL and FA (for PC = 10, 15, and 20).</p>
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<p>UCS of all stabilized samples.</p>
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<p>Scanning electron microscopy (SEM) image 1000x magnification of (<b>A</b>) fly ash and (<b>B</b>) hydrated lime. The yellow arrows indicate the presence of voids.</p>
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<p>SEM images of the highest dosage (35/84.5/20) at different scales: (<b>A</b>) 1000x highlighting the enveloping of small particles; (<b>B</b>) 1000x highlighting the continuous smooth texture; (<b>C</b>) 2000x, and (<b>D</b>) 3000x. The white arrows highlight the presence of excess fly ash material.</p>
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26 pages, 36184 KiB  
Article
Incorporating Effects of Slope Units and Sliding Areas into Seismically Induced Landslide Risk Modeling in Tectonically Active Mountainous Areas
by Hao Wu, Chenzuo Ye, Xiangjun Pei, Takashi Oguchi, Zhihao He, Hailong Yang and Runqiu Huang
Remote Sens. 2024, 16(18), 3517; https://doi.org/10.3390/rs16183517 - 22 Sep 2024
Abstract
Traditional Newmark models estimate earthquake-induced landslide hazards by calculating permanent displacements exceeding the critical acceleration, which is determined from static factors of safety and hillslope geometries. However, these studies typically predict the potential landslide mass only for the source area, rather than the [...] Read more.
Traditional Newmark models estimate earthquake-induced landslide hazards by calculating permanent displacements exceeding the critical acceleration, which is determined from static factors of safety and hillslope geometries. However, these studies typically predict the potential landslide mass only for the source area, rather than the entire landslide zone, which includes both the source and sliding/depositional areas. In this study, we present a modified Newmark Runout model that incorporates sliding and depositional areas to improve the estimation of landslide chain risks. This model defines the landslide runout as the direction from the source area to the nearest river channel within the same slope unit, simulating natural landslide behavior under gravitational effects, which enables the prediction of the entire landslide zone. We applied the model to a subset of the Minjiang Catchment affected by the 1933 MW 7.3 Diexi Earthquake in China to assess long-term landslide chain risks. The results indicate that the predicted total landslide zone closely matches that of the Xinmo Landslide that occurred on 24 June 2017, despite some uncertainties in the sliding direction caused by the old landslide along the sliding path. Distance-weighted kernel density analysis was used to reduce the prediction uncertainties. The hazard levels of the buildings and roads were determined by the distance to the nearest entire landslide zone, thereby assessing the landslide risk. The landslide dam risks were estimated using the kernel density module for channels blocked by the predicted landslides, modeling intersections of the total landslide zone and the channels. High-risk landslide dam zones spatially correspond to the locations of the knickpoints primarily induced by landslide dams, validating the model’s accuracy. These analyses demonstrate the effectiveness of the presented model for Newmark-based landslide risk estimations, with implications for geohazard chain risk assessments, risk mitigation, and land use planning and management. Full article
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<p>Geomorphic and geological settings of the Diexi Catchment [<a href="#B25-remotesensing-16-03517" class="html-bibr">25</a>]. (<b>a</b>) Topographic map of the Diexi Catchment (black boundary) within the Minjiang Catchment (purple boundary); (<b>b</b>) geological map of the Diexi Catchment. Detailed description of lithological units is shown in <a href="#remotesensing-16-03517-f002" class="html-fig">Figure 2</a>.</p>
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<p>Description of lithological units in the study area. The colors in the figure correspond to the strata in <a href="#remotesensing-16-03517-f001" class="html-fig">Figure 1</a>.</p>
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<p>Sketch illustration of sliding block model. (<b>a</b>) Force balance utilized in Equation (1) is for a block that is sitting on an inclined plane; (<b>b</b>) schematic illustration of the Newmark model.</p>
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<p>Double integral to calculate Newmark’s permanent displacement based on real-time spectral acceleration. (<b>a</b>) Real-time seismic spectral acceleration; (<b>b</b>) velocity versus time; (<b>c</b>) permanent displacement versus time. Points X, Y, and Z are critical state beyond critical acceleration; Earthquake acceleration-time history with critical acceleration (solid line) of 0.20 g superimposed.</p>
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<p>Maps of (<b>a</b>) slope gradients and (<b>b</b>) lithologic groups. (Detailed parameters are shown in <a href="#remotesensing-16-03517-t001" class="html-table">Table 1</a>). The black capitalized letters represent abbreviations for place names as follows: HJZ—Huoji; YNZ—Yini; WEB—Waer; BLZ—Baila; LHK—Lianghe; JC—Jiaochang; LC—Longchi; MND—Manaoding; TP—Taiping.</p>
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<p>Back-calculations of different slopes’ structural types in the Diexi Catchment: (<b>a</b>) total study area; (<b>b</b>) cataclinal slope; (<b>c</b>) orthoclinal slope; (<b>d</b>) anaclinal slope.</p>
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<p>Maps showing the distribution of the amplification factor: (<b>a</b>) topographic amplification; (<b>b</b>) seismically induced strength losses.</p>
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<p>Maps showing the PGA with an exceedance probability of 2%. (<b>a</b>) Location of the Diexi Catchment on the CPSHA map. (<b>b</b>) Distribution of the PGA in the Diexi Catchment.</p>
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<p>The flowchart for the automatic extraction of slope units based on <span class="html-italic">r.slopeunits V1.0</span>.</p>
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<p>Automatically generated slope units in the Diexi Catchment.</p>
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<p>Illustration of landslide runout and relationship between landslide area and runout distance. (<b>a</b>) Sketch of landslide source area, sliding area, and deposit area; (<b>b</b>) landslide runout distance plotted as a function of the landslide source area for the Diexi Catchment.</p>
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<p>Illustration of Newmark Runout to predict landslide-covering areas.</p>
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<p>Slope-unit-based landslide runout hazard prediction: (<b>a</b>) total landslide-covering areas predicted using Newmark Runout for the Diexi Catchment; (<b>b</b>) illustration of distance-based hazard analysis.</p>
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<p>Maps showing the distributions of the hillslope safety factor and critical acceleration: (<b>a</b>) static hillslope safety factor (<span class="html-italic">F<sub>S</sub></span>); (<b>b</b>) critical acceleration (<span class="html-italic">A<sub>C</sub></span>). The lower values indicate high susceptibility to landslides.</p>
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<p>Comparison of entire landslide zones and landslide source areas. (<b>a</b>) Entire landslide zones induced by the Diexi Earthquake; (<b>b</b>) results of landslide source area interpretation.</p>
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<p>Susceptibility of landslide source areas based on CPSHA with an exceedance probability of 2%. The inventory of potentially unstable landslide source areas is marked with black boundaries.</p>
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<p>Risk estimation of buildings in the Diexi Catchment.</p>
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<p>Risk estimation of roads in the Diexi Catchment.</p>
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<p>Earthquake magnitude versus landslide volume based on global empirical regression [<a href="#B54-remotesensing-16-03517" class="html-bibr">54</a>,<a href="#B55-remotesensing-16-03517" class="html-bibr">55</a>].</p>
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<p>Spatial distribution and risk estimations of seismically induced landslide dams. (<b>a</b>) Risk estimations of landslide dams in the Diexi Catchment. (<b>b</b>) Comparison of landslide dam clustering and knickpoints in the Diexi Catchment.</p>
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<p>Risk estimation of landslide dams for the Minjiang River.</p>
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16 pages, 5410 KiB  
Article
Study on the Effects of Influence Factors on the Stress and Deformation Characteristics of Ultra-High CFRDs
by Hongmei Li, Jianxin Wang, Yanyuan Lv and Chengming Feng
Appl. Sci. 2024, 14(18), 8268; https://doi.org/10.3390/app14188268 - 13 Sep 2024
Abstract
A sensitivity analysis was conducted to evaluate several factors, including dam height, bank slope gradient, water storage times, and phased panel filling, on concrete-faced rockfill dams (CFRDs). The analysis identified the three most significant factors to examine their impacts on the stress-deformation characteristics [...] Read more.
A sensitivity analysis was conducted to evaluate several factors, including dam height, bank slope gradient, water storage times, and phased panel filling, on concrete-faced rockfill dams (CFRDs). The analysis identified the three most significant factors to examine their impacts on the stress-deformation characteristics of CFRDs. The results show that the order of influence on the dam body’s stress and deformation characteristics is as follows: dam height > bank slope gradient > water storage times > panel phased construction. From the perspective of stress-deformation of the face slab, water storage times predominantly affect tensile stress, while the bank slope gradient exerts the greatest influence on compressive stress. As the bank slope gradient decreases, the panel’s lateral restraint diminishes, leading to a decrease in the panel’s extrusion efficacy. Consequently, there are notable variations in the panel’s compressive stresses. An increase in dam height correlates with escalating stress and deformation in both the dam and face slab. As the bank slope gradient decreases, the deformation of the dam and face slab, as well as the range of tensile stress of the face slab, also increase. In contrast to a single water storage scenario, the face slab has experienced greater stress and deformation during the initial impoundment under multiple impoundment conditions. Therefore, multiple water storage schemes result in reduced deflection, axial horizontal displacement, and tensile stresses both along the slope and axial in the face slab. Furthermore, the tensile area at the bottom of the face slab transitions into a compressive area. Full article
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<p>Statistical patterns related to the maximum internal settlement of dam body and maximum deflection of panel relative to dam height. (<b>a</b>) Maximum internal settlement of dam [<a href="#B9-applsci-14-08268" class="html-bibr">9</a>,<a href="#B10-applsci-14-08268" class="html-bibr">10</a>]; (<b>b</b>) maximum deflection of panel [<a href="#B11-applsci-14-08268" class="html-bibr">11</a>,<a href="#B12-applsci-14-08268" class="html-bibr">12</a>].</p>
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<p>Standard cross-section of a 250 m CFRD.</p>
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<p>Finite element model of a 250 m CFRD.</p>
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<p>The relative weight distribution of influencing factors on stress and deformation characteristics of the dam body.</p>
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<p>The relative weight distribution of influencing factors on stress and deformation characteristics of the panel.</p>
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<p>Changes in stress and deformation characteristics of the dam body and panel during the storage period under different dam height conditions: (<b>a</b>) internal settlement of the dam body; (<b>b</b>) deflection of the panel; (<b>c</b>) stress along the slope direction of the panel; (<b>d</b>) stress along the axial direction of the panel.</p>
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<p>Distribution of stress along the slope and axial direction in the face slab under different dam height conditions: (<b>a</b>) axial stress in the panel under 200 m/MPa; (<b>b</b>) stress along the slope in the panel under 200 m/MPa; (<b>c</b>) axial stress in the panel under 300 m/MPa; (<b>d</b>) stress along the slope in the panel under 300 m/MPa.</p>
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<p>Changes in deformation and stress characteristics of the dam body and panel under different bank slope gradient conditions during the water storage period: (<b>a</b>) deformation; (<b>b</b>) stress.</p>
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<p>Distribution of stress along the slope and axial direction in the panel under different bank slope gradient conditions: (<b>a</b>) axial stress at a bank slope gradient of 1:0.5/MPa; (<b>b</b>) stress along the slope at a bank slope gradient of 1:0.5/MPa; (<b>c</b>) axial stress at a bank slope gradient of 1:1.5/MPa; (<b>d</b>) stress along the slope at a bank slope gradient of 1:1.5/MPa.</p>
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<p>Changes in stress and deformation characteristics of the panel during completion and storage periods under different water storage conditions: (<b>a</b>) deflection; (<b>b</b>) stress along the slope; (<b>c</b>) stress along the axial.</p>
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<p>Stress contour maps along the slope and axial of the panel under the one-time and three-times water storage schemes: (<b>a</b>) stress contour map along an axial direction/MPa; (<b>b</b>) stress contour map along a slope direction/MPa.</p>
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12 pages, 2564 KiB  
Article
Influence of Infill Patterns on the Shape Memory Effect of Cold-Programmed Additively Manufactured PLA
by Vladimir Barrera-Quintero, Erasmo Correa-Gómez, Alberto Caballero-Ruiz and Leopoldo Ruiz-Huerta
Polymers 2024, 16(17), 2460; https://doi.org/10.3390/polym16172460 - 29 Aug 2024
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Abstract
In four-dimensional additive manufacturing (4DAM), specific external stimuli are applied in conjunction with additive manufacturing technologies. This combination allows the development of tailored stimuli-responsive properties in various materials, structures, or components. For shape-changing functionalities, the programming step plays a crucial role in recovery [...] Read more.
In four-dimensional additive manufacturing (4DAM), specific external stimuli are applied in conjunction with additive manufacturing technologies. This combination allows the development of tailored stimuli-responsive properties in various materials, structures, or components. For shape-changing functionalities, the programming step plays a crucial role in recovery after exposure to a stimulus. Furthermore, precise tuning of the 4DAM process parameters is essential to achieve shape-change specifications. Within this context, this study investigated how the structural arrangement of infill patterns (criss-cross and concentric) affects the shape memory effect (SME) of compression cold-programmed PLA under a thermal stimulus. The stress–strain curves reveal a higher yield stress for the criss-cross infill pattern. Interestingly, the shape recovery ratio shows a similar trend across both patterns at different displacements with shallower slopes compared to a higher shape fixity ratio. This suggests that the infill pattern primarily affects the mechanical strength (yield stress) and not the recovery. Finally, the recovery force increases proportionally with displacement. These findings suggest a consistent SME under the explored interval (15–45% compression) despite the infill pattern; however, the variations in the mechanical properties shown by the stress–strain curves appear more pronounced, particularly the yield stress. Full article
(This article belongs to the Special Issue 3D and 4D Printing of Polymers: Modeling and Experimental Approaches)
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Graphical abstract
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<p>Stress–strain curve for cold programming.</p>
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<p>Infill patterns proposed: (<b>a</b>) criss-cross and (<b>b</b>) concentric patterns.</p>
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<p>Experimental methodology.</p>
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<p>Stress–strain response during compression testing for samples deformed to 15%, 30%, and 45% strain.</p>
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<p>(<b>a</b>) Positions for height measurements, (<b>b</b>) one in the middle of the sample (white arrow), (<b>c</b>) two for the opposite corners (white arrows).</p>
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<p>Shape fixity ratio (SFR) for criss-cross and concentric infill patterns.</p>
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<p>Shape recovery ratio (SRR) for criss-cross and concentric infill patterns.</p>
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<p>Maximum recovery force for criss-cross and concentric infill patterns.</p>
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26 pages, 7267 KiB  
Review
Cracks in Arch Dams: An Overview of Documented Instances
by André Conde, Miguel Á. Toledo and Eduardo Salete
Appl. Sci. 2024, 14(17), 7580; https://doi.org/10.3390/app14177580 - 27 Aug 2024
Viewed by 412
Abstract
It is essential to understand how failure mechanisms work in arch dams and, in particular, their most common manifestation: cracking. In this paper, the different types of cracking are explained in terms of their causes and consequences. Then, an exhaustive literature review is [...] Read more.
It is essential to understand how failure mechanisms work in arch dams and, in particular, their most common manifestation: cracking. In this paper, the different types of cracking are explained in terms of their causes and consequences. Then, an exhaustive literature review is carried out that results in a detailed compilation of the characteristics of 38 cracked arch dams from all over the world, including crack characteristics (zone, position, dimensions and probable cause). This review is restricted to only those dams for which information on the position of the cracks or dam displacements is publicly available. As part of the review, a brief summary of key data for each dam is included, as well as a compilation of published crack diagrams. The positions of the cracks of all the dams are classified using diagrams in relation to the type of dam and the origin of the crack. Finally, the distribution of some dam parameters and crack features is analyzed by studying the relationships between them. Full article
(This article belongs to the Special Issue Latest Research on Geotechnical Engineering)
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<p>Radial displacements of Zeuzier dam measured at the level of gallery 2. Reprinted from [<a href="#B69-applsci-14-07580" class="html-bibr">69</a>].</p>
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<p>Radial displacements of Kariba dam at the crest of the crown cantilever. Reprinted from [<a href="#B68-applsci-14-07580" class="html-bibr">68</a>].</p>
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<p>Part 1 of crack location diagrams. Main cracks highlighted in red. Images reprinted from cited references. * Downstream face. ** Upstream face. [<a href="#B11-applsci-14-07580" class="html-bibr">11</a>,<a href="#B21-applsci-14-07580" class="html-bibr">21</a>,<a href="#B30-applsci-14-07580" class="html-bibr">30</a>,<a href="#B36-applsci-14-07580" class="html-bibr">36</a>,<a href="#B38-applsci-14-07580" class="html-bibr">38</a>,<a href="#B55-applsci-14-07580" class="html-bibr">55</a>,<a href="#B69-applsci-14-07580" class="html-bibr">69</a>,<a href="#B70-applsci-14-07580" class="html-bibr">70</a>,<a href="#B75-applsci-14-07580" class="html-bibr">75</a>,<a href="#B82-applsci-14-07580" class="html-bibr">82</a>,<a href="#B83-applsci-14-07580" class="html-bibr">83</a>].</p>
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<p>Part 2 of crack location diagrams. Main cracks highlighted in red. Images reprinted from cited references. * Downstream face. ** Upstream face. [<a href="#B21-applsci-14-07580" class="html-bibr">21</a>,<a href="#B69-applsci-14-07580" class="html-bibr">69</a>,<a href="#B84-applsci-14-07580" class="html-bibr">84</a>,<a href="#B86-applsci-14-07580" class="html-bibr">86</a>,<a href="#B87-applsci-14-07580" class="html-bibr">87</a>,<a href="#B91-applsci-14-07580" class="html-bibr">91</a>,<a href="#B95-applsci-14-07580" class="html-bibr">95</a>,<a href="#B96-applsci-14-07580" class="html-bibr">96</a>,<a href="#B99-applsci-14-07580" class="html-bibr">99</a>].</p>
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<p>Areas where cracks were found. Dotted lines divide toe, center, abutment and crest areas.</p>
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<p>Areas where cracks were found. Bold: cracks due to chemical effects.</p>
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<p>Areas where cracks were found. Bold: cracks due to inadequate design or execution of the construction and maintenance.</p>
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<p>Areas where cracks were found. Bold: cracks due to thermal effects.</p>
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<p>Areas where cracks were found. Bold: cracks due to external events.</p>
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<p>Distribution of the main characteristics of dams as a percentage of the entire available set of cracked dams.</p>
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<p>Relationship between three main parameters.</p>
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<p>External event cracks.</p>
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23 pages, 9797 KiB  
Article
Enhancing Dam Safety: Statistical Assessment and Kalman Filter for the Geodetic Network of Mosul Dam
by Bashar Alsadik and Hussein Alwan Mahdi
Infrastructures 2024, 9(9), 144; https://doi.org/10.3390/infrastructures9090144 - 26 Aug 2024
Viewed by 348
Abstract
Dams play a pivotal role in providing essential services such as energy generation, water supply, and flood control. However, their stability is crucial, and continuous monitoring is vital to mitigate potential risks. The Mosul Dam is one of the most interesting infrastructures in [...] Read more.
Dams play a pivotal role in providing essential services such as energy generation, water supply, and flood control. However, their stability is crucial, and continuous monitoring is vital to mitigate potential risks. The Mosul Dam is one of the most interesting infrastructures in Iraq because it was constructed on alternating beds of karstified and gypsum which required continuous grouting due to water seepage. Therefore, the ongoing maintenance issues raised international concerns about its stability. For several years the dam indicated a potential for disastrous failure that could cause massive flooding downstream and pose a serious threat to millions of people. This research focuses on comprehensive statistical assessments of the dam geodetic network points across multiple epochs of long duration. Through the systematic application of three statistical tests and the predictive capabilities of the Kalman filter, safety and long-term stability are aimed to be enhanced. The analysis of the dam’s geodetic network points shows a consistent trend of upstream-to-downstream movement. The Kalman filter demonstrates promising outcomes for displacement prediction compared to least squares adjustment. This research provides valuable insights into dam stability assessment, aligns with established procedures, and contributes to the resilience and safety of critical infrastructure. The outcome of this paper can encourage future studies to build upon the foundation presented. Full article
(This article belongs to the Special Issue Advances in Structural Health Monitoring of the Built Environment)
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<p>Aerial view of the Mosul Dam site taken from Google Earth [<a href="#B25-infrastructures-09-00144" class="html-bibr">25</a>].</p>
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<p>The workflow diagram of the Kalman filter.</p>
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<p>The <span class="html-italic">t</span>-distribution curve plot.</p>
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<p>The F-distribution curve plot.</p>
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<p>Different standard deviation limits of the normal distribution curve.</p>
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<p>Part of the horizontal geodetic network of the Mosul Dam. Red triangles are fixed points and yellow circles are the un-fixed pillars of the dam. Arcs indicate measured angles and dashed lines indicate distances.</p>
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<p>The inconsistency and imperfection in the network measurements during epochs affect the quality of the estimated accuracy at the adjusted dam pillars (plot exaggeration scale = 50,000). (<b>a</b>) Epoch 37 (unit variance = 0.64), (<b>b</b>) epoch 49 (unit variance = 1.27).</p>
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<p>The relation between the quality of the adjusted network points and the measurement weight. (<b>a</b>) A priori error of angles = 10”. (<b>b</b>) A priori error of angles = 5” (plot exaggeration scale = 30,000).</p>
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<p>(<b>a</b>) Trilateration net adjustment. (<b>b</b>) Triangulation net adjustment. (<b>c</b>) Free net adjustment of the dam hybrid network. (<b>d</b>) Constrained adjustment where P51 and P55 are fixed. (<b>e</b>) Constrained adjustment where P42 and P44 are fixed (exaggeration scale = 20,000).</p>
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<p>Visual representation of dam pillar displacement directions, showcasing the displacement vectors computed through constrained network adjustment (<b>a</b>) and free network adjustment (<b>b</b>), spanning from epoch 36 (2005) to epoch 50 (2013).</p>
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<p>Compatibility checks where the <span class="html-italic">x</span>-axis shows the dam pillar labels and the <span class="html-italic">y</span>-axis shows the displacement in mm. (<b>a</b>) The compatibility checks using the F-statistic test. (<b>b</b>) The compatibility checks using the <span class="html-italic">t</span>-statistic test. Green indicates compatible points and red indicates incompatible points.</p>
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<p>Compatibility checks where the <span class="html-italic">x</span>-axis shows the dam pillar labels and the <span class="html-italic">y</span>-axis shows the displacement in mm. (<b>a</b>) The compatibility checks using the Z-score (at 3.29). (<b>b</b>) The compatibility checks using the Z-score (at 2.33). Green indicates compatible points and red indicates incompatible points.</p>
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<p>Compatibility checks where the <span class="html-italic">x</span>-axis shows the dam pillar labels and the <span class="html-italic">y</span>-axis shows the displacement in mm. (<b>a</b>) Compatibility checks between free-adjusted networks using the F-statistic. (<b>b</b>) Compatibility checks between free-adjusted networks using the t-statistic. Green indicates compatible points and red indicates incompatible points.</p>
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<p>(<b>a</b>) Histogram comparing between epoch 50 least square-adjusted dam points and predicted Kalman filter points. (<b>b</b>) Kalman filter-derived average velocity and heading for each dam pillar across eight years of epochs.</p>
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21 pages, 11353 KiB  
Article
Exploring the Ground-Penetrating Radar Technique’s Effectiveness in Diagnosing Hydropower Dam Crest Conditions: Insights from Gura Apelor and Herculane Dams, Romania
by Alexandra Georgiana Gerea and Andrei Emilian Mihai
Appl. Sci. 2024, 14(16), 7212; https://doi.org/10.3390/app14167212 - 16 Aug 2024
Viewed by 381
Abstract
When it comes to hydropower dam safety, continuous and comprehensive monitoring is increasingly important. Especially for aging dams, this can pose a difficult challenge that benefits from a multimethod analysis. Here, we present the use and suitability of a geophysical method, Ground Penetrating [...] Read more.
When it comes to hydropower dam safety, continuous and comprehensive monitoring is increasingly important. Especially for aging dams, this can pose a difficult challenge that benefits from a multimethod analysis. Here, we present the use and suitability of a geophysical method, Ground Penetrating Radar (GPR), for the non-invasive assessment of two distinct types of hydropower dams in Romania: Herculane (a concrete arch dam) and Gura Apelor (an embankment dam with a rockfill and clay core). Unlike traditional monitoring methods for dam safety in Romania, which might provide an incomplete overview, GPR offers a broader, non-destructive approach to evaluating some elements of dam integrity. Here, we present the results of surveys carried out with a 200 MHz antenna on the crests of both dams. The aim was to conduct a rapid assessment of the crest condition and identify the potential damage to the crest that may elude standard monitoring techniques. The surveys provide an imaging indicative of the structural integrity, although this is more challenging in the embankment dam, and additionally we provide significant information regarding the deformations in the upper layers. This complements data from routine topo-geodetical surveys, offering a potential explanation for the vertical displacements observed therein. We highlight several areas of potential deformation as well as degradation in subsurface structures such as rebars. The results underscore the value of GPR in supplementing established dam monitoring methods, highlighting its effectiveness in different contexts and dam types, as well as its potential in shaping future standards for dam safety management in Romania. Full article
(This article belongs to the Special Issue Advances in Geosciences: Techniques, Applications, and Challenges)
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<p>Location of the two dams. Left—the Herculane (concrete) dam in the Caraș-Severin county. Right—the Gura Apelor (embankment) dam in Hunedoara county.</p>
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<p>The vertical section of the dam. 1—clay core, 2—inverted filters, 3—rock, 4 and 5—filling prisms. The height of the dam is 168 m and the width of the crest is 12 m. Image reproduced after Popovici, 2022 [<a href="#B23-applsci-14-07212" class="html-bibr">23</a>].</p>
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<p>Damage visible at the surface of the dam, on the crest: left—the Herculane dam crest surface; right—the Gura Apelor dam.</p>
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<p>The elements of the Herculane dam visible from the downstream side: dam’s crest, the hydropower plant, the entrance to the gallery, gangways, and spillways.</p>
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<p>Representation of the basic operation principles of the GPR data collection and functionality.</p>
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<p>Left—the profiles (marked with red) on the Gura Apelor dam (GA1–GA4). Right—the profiles (marked with red) on the Herculane dam (H1 and H2). Not at scale.</p>
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<p>Processed data from profiles GA2 (up) and GA4 (down) on the Gura Apelor dam. Area of interest marked with rectangles and horizons marked with arrows.</p>
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<p>Close up on the area of interest marked as a subsidence. Processed data from profiles GA2 (up) and GA4 (down) on the Gura Apelor dam.</p>
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<p>Data from the profiles GA2 and GA4 from the Gura Apelor dam, highlighted with different colors, are the three horizons from the surface.</p>
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<p>The topo-geodetic network at the Gura Apelor dam, reproduction after Avram et. al., 2017 [<a href="#B44-applsci-14-07212" class="html-bibr">44</a>].</p>
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<p>Leveling data measured at the benchmarks from the dam’s crest, as described by Avram et al., 2017 [<a href="#B44-applsci-14-07212" class="html-bibr">44</a>] using data from <a href="#applsci-14-07212-t0A3" class="html-table">Table A3</a>. The orientation of the graph matches the orientation of the GPR profiles.</p>
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<p>Processed data from the set 1 (S1). Up—profile H1; down—H1 profile with migration applied.</p>
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<p>Processed data from the second data set, S2. Up—profile H1; down—profile H1 with migration applied.</p>
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28 pages, 3081 KiB  
Article
Credibility and the Social Function of Property: A Saga of Mega-Dams, Eviction, and Privatization, as Told by Displaced Communities in Malaysia
by Peter Ho, Bin Md Saman Nor-Hisham and Heng Zhao
Land 2024, 13(8), 1207; https://doi.org/10.3390/land13081207 - 5 Aug 2024
Viewed by 454
Abstract
Globally, the forced displacement of socially vulnerable communities causes significant contestation, irrespective of whether that occurs for mega-projects or smaller infrastructural, agricultural, urban renewal, or property developments. Despite multilateral guidelines for “socially inclusive” development, it is difficult to avoid the marginalization of evicted, [...] Read more.
Globally, the forced displacement of socially vulnerable communities causes significant contestation, irrespective of whether that occurs for mega-projects or smaller infrastructural, agricultural, urban renewal, or property developments. Despite multilateral guidelines for “socially inclusive” development, it is difficult to avoid the marginalization of evicted, local communities. Grounded on the credibility thesis, this article provides a new, theoretical basis for understanding the “social function of property” and how this may be used as a criterion to assess whether development-induced and resettlement projects should be given the go-ahead. Methodologically, this article employs the FAT (Formal, Actual, and Targeted) Institutional Framework to unpack the social function of property. To this end, it analyzes the acquisition and privatization of the common property of Indigenous Peoples to construct the Malaysian Bakun Hydroelectric Project, purportedly Asia’s second-largest dam. The FAT analysis ascertains the following three conditions on which basis projects should be halted: (1) the property of the evicted communities fulfills a critical role in providing social welfare; (2) the said function is disregarded by the expropriating agency; (3) the power divides between the expropriator and expropriated prevent meaningful participation by the latter. This study demonstrates that the social function of property can be effectively measured and validates the FAT Framework as a viable tool to analyze development-induced projects (and policies), with particular reference to expropriation, privatization, and formalization. Full article
(This article belongs to the Special Issue Feature Papers for 'Land Socio-Economic and Political Issues' Section)
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<p>Longhouse communities of Orang Ulu affected by the Bakun Dam. Source: Illustrated by authors. Note light blue.</p>
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<p>Aerial view of the Bakun Dam (<b>a</b>). View of Bakun Dam (<b>b</b>). Source [<a href="#B76-land-13-01207" class="html-bibr">76</a>].</p>
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<p>FAT Framework. Source [<a href="#B16-land-13-01207" class="html-bibr">16</a>].</p>
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<p>Percentage of population by employment at the RSSA in 1996. Source [<a href="#B64-land-13-01207" class="html-bibr">64</a>], pp. 3–12.</p>
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<p>Naha Jalei Village established by Orang Ulu refusing to relocate (<b>left</b>)—Villagers from Naha Jalei returning from hunting (<b>right</b>). Source: Photos by Nor-Hisham.</p>
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<p>View on authorities’ compliance with land acquisition procedures. Source: This survey.</p>
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<p>Views on land acquisition procedures. Source: This survey.</p>
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<p>The slash and burn for shifting cultivation at the RSSA (<b>a</b>). The stream at the RSSA claimed by authorities as suitable for fishery (<b>b</b>). Source: Photograph by Nor-Hisham.</p>
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<p>Is the power of the Customary Council of Elders reduced at the RSSA? Source: This survey.</p>
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<p>Illegally reclaimed land planted with corn (<b>a</b>) along main road leading to the RSSA community center; (<b>b</b>) main road to Uma Belor longhouse, RSSA. Source: Photos by Nor-Hisham.</p>
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<p>Temporal FAT analysis of Bakun Dam. Source: Illustrated by authors.</p>
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18 pages, 2773 KiB  
Article
Seepage–Deformation Coupling Analysis of a Core Wall Rockfill Dam Subject to Rapid Fluctuations in the Reservoir Water Level
by Xueqin Zheng, Bin Yan, Wei Wang, Kenan Du and Yixiang Fang
Water 2024, 16(11), 1621; https://doi.org/10.3390/w16111621 - 5 Jun 2024
Viewed by 659
Abstract
Core wall rockfill dams are susceptible to cracking at the dam’s crest, as well as collapse and settlement of the rockfill during storage and operation periods, particularly due to rapid fluctuations in the water level in pumped storage power stations. Most studies on [...] Read more.
Core wall rockfill dams are susceptible to cracking at the dam’s crest, as well as collapse and settlement of the rockfill during storage and operation periods, particularly due to rapid fluctuations in the water level in pumped storage power stations. Most studies on the impact of fluctuations in the reservoir’s water level on dam deformation have considered fluctuations of less than 5 m/d, while pumped storage power stations experience much larger fluctuations. Additionally, the seepage and stress fields within the dam’s rock and soil interact and influence each other. Few studies have used the coupling theory of seepage and stress to analyze seepage and deformation in core wall rockfill dams. To address these issues, a finite element model using seepage–stress coupling theory was utilized to investigate the variations in the phreatic line, earth pressure, and deformation of a core wall rockfill dam due to rapid fluctuations in the reservoir’s water level. Additionally, the results of the finite element simulation were compared with and analyzed alongside safety monitoring data. The results indicated that, upon a sudden decrease in the reservoir’s water level, there was a lag in the decline of the phreatic line in Rockfill I, which created a large hydraulic gradient, resulting in a reverse seepage field on the dam’s slope surface and generating a drag force directed upstream. Consequently, a significant concentration of stress occurred on one-third of the upstream slope surface of the dam and the seepage curtain, and the increase in horizontal displacement was substantially greater than the increase in settlement from one-third of the rockfill’s height to the dam’s foundation. The deformation was more sensitive to the lowest water level of the reservoir rather than to the fastest rate of decline. Sudden rises in the reservoir’s water level result in decreased horizontal displacements and settlement of the dam. Amid rapid fluctuations of the reservoir’s water level, changes in the vertical earth pressure were more pronounced at the bottom of the core wall than in its midsection. Compared with the core wall, variations in the vertical earth pressure in the upstream and downstream filter layers were minor at similar elevations. A peak horizontal displacement of 6.5 mm was noted at one-third the height of Rockfill I, with the greatest increase in settlement of 3.5 mm at the dam’s crest. To ensure a project’s safety, it is crucial to control the elevation of the lowest point during a sudden drop in the reservoir’s level and to carefully monitor for cracks or voids within approximately one-third of the dam’s height in Rockfill I and at the dam crest. This study’s results provide a scientific basis for assessing core wall rockfill dams’ health and securing long-term safety at pumped storage power facilities. Full article
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<p>A typical section of the dam.</p>
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<p>Layout of measurement points on a typical section of the dam.</p>
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<p>Hydrograph of the reservoir’s water level, exhibiting temporal variations.</p>
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<p>Cloud maps of pore water pressure at different typical moments (unit: kPa).</p>
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<p>Monitoring data of the seepage pressure.</p>
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<p>Cloud maps of vertical soil pressure at different typical moments (unit: kPa).</p>
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<p>Comparison between the simulated and monitored values of vertical soil pressure.</p>
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<p>Chart illustrating the time variation of increments in horizontal displacement.</p>
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<p>Chart illustrating the time variation of increments in settlement.</p>
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<p>Cloud maps of horizontal displacement at different typical moments (unit: mm).</p>
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<p>Cloud maps of settlement at different typical moments (unit: mm).</p>
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<p>Vector diagram of the dam’s deformation.</p>
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26 pages, 28099 KiB  
Article
Modelling and Validation of the Derna Dam Break Event
by Alessandro Annunziato, Marzia Santini, Chiara Proietti, Ludovica de Girolamo, Valerio Lorini, Andrea Gerhardinger and Michele Tucci
GeoHazards 2024, 5(2), 504-529; https://doi.org/10.3390/geohazards5020026 - 1 Jun 2024
Viewed by 746
Abstract
The catastrophic failure of two dams in Libya on 10 and 11 September 2023 resulted in the devastating flooding of the city of Derna, which is located downstream of the dams, causing more than 6000 fatalities and displacing thousands of residents. The failure [...] Read more.
The catastrophic failure of two dams in Libya on 10 and 11 September 2023 resulted in the devastating flooding of the city of Derna, which is located downstream of the dams, causing more than 6000 fatalities and displacing thousands of residents. The failure was attributed to heavy rainfall from Storm Daniel, leading to the dams reaching full capacity and subsequently overflowing and failing. This paper presents an analysis of the dam break, including the modelling of flow discharge and the resulting flooding of Derna. For validation purposes, this study compares the modelled quantities with post-event satellite imagery from UNOSAT and Copernicus, local reports, and data collected from social media using AI detection. The findings provide valuable insights into the dynamics of the dam break and its initial parameters, as well as an assessment of the accuracy of the results. The analysis is performed using a rapid estimation technique developed by JRC to provide the international emergency community with a swift overview of the impact and damage assessment of potential or actual dam break events. The use of all available data shows a satisfactory comparison with the calculated quantities. The rapid modelling of dam break events and combined analysis of multiple data types are proven suitable for promptly assessing the expected dynamic of the event, as well as reconstructing the unknown initial conditions before the break. Incorporating sensitivity analyses provides an estimate of the uncertainties associated with the deduced values of the unknown parameters and their relative importance in the analysis. Full article
(This article belongs to the Topic Geotechnics for Hazard Mitigation)
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<p>Satellite image showing Storm Daniel evolving in the Mediterranean Sea and affecting the northern areas of Libya (<sup>©</sup>EUMETSAT2023).</p>
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<p>Situation map for the Libya floods (JRC and ECHO) [<a href="#B4-geohazards-05-00026" class="html-bibr">4</a>].</p>
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<p>City of Derna before (left, 19 June 2023) and after (right, 13 September) the flood (<sup>©</sup>Google Earth).</p>
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<p>Geographic location of the dams with indication of approximate distance between the two (basemap from Open Street Map (OSM)).</p>
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<p>Dam geometry.</p>
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<p>Drawing from image of Derna Dam overfill discharge pipe (image acquired from Erges) [<a href="#B17-geohazards-05-00026" class="html-bibr">17</a>].</p>
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<p>Drawing from image of the original form of the dam before the collapse (image acquired from DredgeWire) [<a href="#B24-geohazards-05-00026" class="html-bibr">24</a>].</p>
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<p>Drawing from image of the destroyed dam (image acquired from Eduvast) [<a href="#B25-geohazards-05-00026" class="html-bibr">25</a>].</p>
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<p>Calculated water propagation in the first 50 min following the Derna dam break, considering a reservoir water level of 225 m, a break size of 260 m, a Manning roughness coefficient set at 0.015 s/m<sup>1/3</sup>, and an empty downstream river (basemap from OSM).</p>
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<p>Effect of lake water height on peak flow (blue line) and arrival time (orange line) in Derna (22.62784/32.74522).</p>
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<p>Flood water level at the entrance of Derna (22.62784/32.74522) with different lake water heights.</p>
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<p>Effect of initial lake water height on the flood extent in Derna. The red line represents the flood extent assessed by Copernicus EMSR696 [<a href="#B21-geohazards-05-00026" class="html-bibr">21</a>], and the blue line corresponds to UNOSAT FL20230912 as of 13 September 2023 [<a href="#B22-geohazards-05-00026" class="html-bibr">22</a>] (basemap from OSM).</p>
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<p>Effect of Manning roughness coefficient on the peak flow (blue line) and the arrival time (orange line) at the entrance of Derna (22.62784/32.74522).</p>
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<p>Flood wave height at the entrance of Derna (22.62784/32.74522) with different Manning roughness coefficients.</p>
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<p>Effect of Manning roughness coefficient (s/m<sup>1/3</sup>) on flooding in Derna. The red line represents the flood extent assessed by Copernicus EMSR696 [<a href="#B21-geohazards-05-00026" class="html-bibr">21</a>], and the blue line corresponds to UNOSAT FL20230912 as of 13 September 2023 [<a href="#B22-geohazards-05-00026" class="html-bibr">22</a>] (basemap from OSM).</p>
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<p>Effect of break width on the peak flow (blue line) and the arrival time (orange line) at the entrance of Derna (22.62784/32.74522).</p>
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<p>Measured and predicted break formation times, Froelich [<a href="#B29-geohazards-05-00026" class="html-bibr">29</a>].</p>
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<p>Arrival time as a function of initial water level in the river.</p>
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<p>Effect of the presence of the river downstream of the dam when imposing 0.0625, 1.25, or 2.5 m<sup>2</sup>/s as flux in each cell of the lake reservoir.</p>
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<p>Effect of river flow on Derna inundation. The red line represents the flood extent assessed by Copernicus EMSR696 [<a href="#B21-geohazards-05-00026" class="html-bibr">21</a>], and the blue line corresponds to UNOSAT FL20230912 as of 13 September 2023 [<a href="#B22-geohazards-05-00026" class="html-bibr">22</a>] (basemap from OSM).</p>
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<p>Calculated flood travel time (basemap from OSM).</p>
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<p>Flood arrival times in Derna (JRC and basemap from Copernicus).</p>
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<p>Maximum flow depth for the nominal case in the Al-Maghar neighbourhood. The computed data are compared with the flood extents identified by UNOSAT (blue line) [<a href="#B22-geohazards-05-00026" class="html-bibr">22</a>] and Copernicus EMS (red line) [<a href="#B21-geohazards-05-00026" class="html-bibr">21</a>] (basemap from OSM).</p>
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<p>Top figure: SRTM contour [<a href="#B7-geohazards-05-00026" class="html-bibr">7</a>] with flow depth greater than 0 in yellow; the blue arrows indicate elevated areas. Bottom figure: SRTM contour [<a href="#B7-geohazards-05-00026" class="html-bibr">7</a>] with the detailed maximum flow depth (basemap from OSM).</p>
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<p>Comparison of the flood depth from modelling and from visual interpretation of images at selected locations (JRC and basemap from Copernicus).</p>
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<p>Comparison between interpreted and modelled flood depths at selected locations. Red bars: visual interpretation from social media; blue bars: model results with an assumed water height in the reservoir of 230 m; green bars: model results with an assumed water height in the reservoir of 225 m.</p>
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24 pages, 8788 KiB  
Article
Deformation Characteristics and Activation Dynamics of the Xiaomojiu Landslide in the Upper Jinsha River Basin Revealed by Multi-Track InSAR Analysis
by Xu Ma, Junhuan Peng, Yuhan Su, Mengyao Shi, Yueze Zheng, Xu Li and Xinwei Jiang
Remote Sens. 2024, 16(11), 1940; https://doi.org/10.3390/rs16111940 - 28 May 2024
Viewed by 575
Abstract
The upper Jinsha River, located in a high-mountain gorge with complex geological features, is highly prone to large-scale landslides, which could result in the formation of dammed lakes. Analyzing the movement characteristics of the typical Xiaomojiu landslide in this area contributes to a [...] Read more.
The upper Jinsha River, located in a high-mountain gorge with complex geological features, is highly prone to large-scale landslides, which could result in the formation of dammed lakes. Analyzing the movement characteristics of the typical Xiaomojiu landslide in this area contributes to a better understanding of the dynamics of landslides in the region, which is of great significance for landslide risk prediction and analysis. True displacement data on the surface of landslides are crucial for understanding the morphological changes in landslides, providing fundamental parameters for dynamic analysis and risk assessment. This study proposes a method for calculating the actual deformation of landslide bodies based on multi-track Interferometric Synthetic Aperture Radar (InSAR) deformation data. It iteratively solves for the optimal true deformation vector of the landslide on a per-pixel basis under a least-squares constraint based on the assumption of consistent displacement direction among adjacent points on the landslide surface. Using multi-track Sentinel data from 2017 to 2023, the line of sight (LOS) accumulative de-formation of the Xiaomojiu landslide was obtained, with a maximum LOS deformation of −126 mm/year. The true surface displacement of the Xiaomojiu landslide after activation was calculated using LOS deformation. The development of two rotational sub-slipping zones on the landslide body is inferred based on the distribution of actual displacements along the central profile line. Analysis of temporal changes in water body area data revealed that the Xiaomojiu landslide was activated after a barrier lake event and continuously moved due to the influence of higher water levels’ in the river channel. In conclusion, the proposed method can be applied to calculate the true surface displacement of landslides with complex mechanisms for analyzing the movement status of landslide bodies. Furthermore, the spatiotemporal analysis of the Xiaomojiu landslide characteristics can support analyzing the mechanisms of similar landslides in the Jinsha River Basin. Full article
(This article belongs to the Special Issue Application of Remote Sensing Approaches in Geohazard Risk)
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<p>(<b>a</b>) Optical image of the Xiaomojiu landslide, (<b>b</b>) geological map of the study area at 1:2,500,000 scale, (<b>c</b>) map showing the location of the Xiaomojiu landslide, (<b>d</b>) schematic image showing the remaining debris blocking the river channel after the breach of the Baige landslide barrier lake.</p>
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<p>Flowchart for the SAR data processing and true deformation inversion.</p>
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<p>This study used the spatial and temporal baselines of the Sentinel-1 data from Ascending orbit Path 99 (<b>a</b>), Descending orbit Path 33 (<b>b</b>), and Descending orbit Path 106 (<b>c</b>). Blue dots represent ascending track data, and red dots represent descending track data.</p>
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<p>(<b>a</b>) NEU-directional projection delineates the satellite LOS motion vector. (<b>b</b>) NEU-directional projection of the authentic ground deformation vector.</p>
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<p>C-index distribution for the Xiaomojiu landslide on three orbits: (<b>a</b>) orbit A99, (<b>b</b>) orbit D33, and (<b>c</b>) orbit D106. The black arrow represents the direction of the river flow. Positive values indicate proximity to the satellite, while negative values indicate distance from the satellite. When |C| = 1, the LOS direction is parallel to the direction of the steepest slope, and when C = 0, the LOS direction is perpendicular to the direction of the steepest slope.</p>
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<p>Different combinations of ground displacement directions correspond to projection coefficient C-index values, (<b>a</b>,<b>d</b>)ascending path 99; (<b>b</b>,<b>e</b>) descending path 33; (<b>c</b>,<b>f</b>) descending path 106.</p>
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<p>LOS Annual Average Displacement Velocity and Velocity Profile Maps. (<b>a</b>,<b>b</b>,<b>d</b>) Depict the velocity maps for ascending path 99, descending path 33, and descending path 106, respectively. In (<b>e</b>), AA’, BB’, and CC’ represent three profiles along the downslope direction, while DD’ and EE’ denote two cross profiles. (<b>c</b>,<b>f</b>–<b>i</b>) Correspond to the velocity distribution maps of the three orbits for profiles AA’, BB’, CC’, DD’, and EE’, respectively.</p>
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<p>(<b>a</b>) P1 to P4 cumulative ascending orbit path 99 temporal cumulative strain map, (<b>c</b>) P1 to P4 cumulative descending orbit path 33 temporal cumulative deformation map, (<b>d</b>) distribution map of four points P1 to P4, (<b>e</b>) P1 to P4 cumulative ascending orbit path 106 temporal cumulative strain map. (<b>b</b>) This sub-figure is a magnified view of (<b>a</b>), where solid black lines represent the dates of the two failures of the Baige landslide, and black dashed lines represent the dates of the debris flow events from the barrier lake outburst. In all sub-figures, the light red EVENT represents the barrier lake events formed by the two failures of the Baige landslide. PRECIP represents the monthly total precipitation in the region from 2017 to 2022 [<a href="#B49-remotesensing-16-01940" class="html-bibr">49</a>].</p>
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<p>Different methods yield 3D deformation maps of the Xiaomojiu landslide. The first row displays the NEU direction deformation maps computed using the SPFM method: (<b>a</b>–<b>c</b>). The second row showcases the NEU direction deformation maps computed using the SPF-LSM method: (<b>d</b>–<b>f</b>). The third row exhibits the NEU direction deformation maps obtained from the APFM method: (<b>g</b>–<b>i</b>). Finally, the fourth row presents the NEU direction deformation maps calculated using the AOCM method: (<b>j</b>–<b>l</b>).</p>
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<p>(<b>a</b>) Accumulated true deformation along profile BB’ (from October 2018 to May 2021), (<b>b</b>) angle between the true deformation direction along profile BB’ and the horizontal plane, (<b>c</b>) deviation between the corresponding inclination angle along profile BB’ and the negative slope angle, (<b>d</b>) the distribution of displacement vectors along profile BB’ is illustrated, with vertical dashed lines employed to delineate variations in angles. The dashed line (slip surface*) indicates the inferred sliding surface derived from prior research and computational outcomes.</p>
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<p>K-means clustering results of landslide blocks and typical multi-track average temporal results; trends of average cumulative deformation for landslide blocks across three orbits, (<b>a</b>) Block C12, (<b>c</b>) Block C2, (<b>d</b>) Block C9, (<b>e</b>) Block C8, (<b>f</b>) Block C5. The temporal data’s light-colored upper and lower bounds represent the standard deviation range. (<b>b</b>) Spatial distribution map of clustering results.</p>
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<p>Box plots of the actual deformation characteristics within sub-blocks obtained from K-means clustering, (<b>a</b>) comparative distribution of angle <math display="inline"><semantics> <mi>α</mi> </semantics></math> in different sub-block regions, (<b>b</b>) comparative distribution of angle <math display="inline"><semantics> <mi>β</mi> </semantics></math> in different sub-block regions, (<b>c</b>) comparative distribution of angle <math display="inline"><semantics> <mrow> <msub> <mi>D</mi> <mrow> <mi>t</mi> <mi>r</mi> <mi>u</mi> <mi>e</mi> </mrow> </msub> </mrow> </semantics></math> in different sub-block regions, (<b>d</b>) comparative distribution of standard deviation <math display="inline"><semantics> <mrow> <msub> <mi>D</mi> <mrow> <mi>t</mi> <mi>r</mi> <mi>u</mi> <mi>e</mi> </mrow> </msub> </mrow> </semantics></math> in different sub-block regions, (<b>e</b>) comparative distribution of the number of ground points in different sub-block regions.</p>
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<p>(<b>a</b>) Overlay image of D33 orbit VV and VH backscatter images (in dB), with the light purple area representing the river buffer zone generated based on elevation. (<b>b</b>) Partial VV+VH image before the first occurrence of the Baige landslide damming lake on 28 September 2018. (<b>c</b>) Partial VV+VH image two hours after the first occurrence of the Baige landslide damming lake on 10 October 2018. (<b>d</b>) Distribution map of pixel values within the river buffer zone, where the first peak represents water bodies, and the second peak represents land. (<b>e</b>) The time series plot of the total pixel count within the river buffer zone was calculated using the threshold segmentation method.</p>
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<p>Shows optical remote sensing images from the GF-2 satellite on 28 February 2018 (<b>a</b>), 1 February 2019 (<b>c</b>), 16 November 2020 (<b>d</b>), 21 April 2022 (<b>e</b>), 4 July 2022 (<b>f</b>), 14 November 2022 (<b>g</b>), 27 January 2023 (<b>h</b>), and 21 April 2023 (<b>i</b>). Another optical remote sensing image was taken from a GF-7 satellite on 1 November 2018 (<b>b</b>).</p>
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28 pages, 21043 KiB  
Article
Study on the Characteristics and Evolution Laws of Seepage Damage in Red Mud Tailings Dams
by Shiqi Chang, Xiaoqiang Dong, Xiaofeng Liu, Xin Xu, Haoru Zhang and Yinhao Huang
Water 2024, 16(11), 1487; https://doi.org/10.3390/w16111487 - 23 May 2024
Viewed by 547
Abstract
Seepage damage is a significant factor leading to red mud tailings dam failures. Laboratory tests on seepage damage were conducted to investigate the damage characteristics and distribution laws of red mud tailings dams, including soil pressure, infiltration line, pore water pressure, dam displacement, [...] Read more.
Seepage damage is a significant factor leading to red mud tailings dam failures. Laboratory tests on seepage damage were conducted to investigate the damage characteristics and distribution laws of red mud tailings dams, including soil pressure, infiltration line, pore water pressure, dam displacement, and crack evolution. The findings revealed the seepage damage mechanisms of red mud slopes, offering insights for the safe operation and seepage damage prevention of red mud tailings dams. The results showed that the higher the water level is in the red mud tailings dam, the higher position the infiltration line is when it reaches the slope face. At the highest infiltration line point of the slope surface, the increase of pore water pressure is the highest and the change of horizontal soil pressure is the highest. Consequently, increased pore water pressure leads to decreased effective stress and shear strength, increasing the susceptibility to damage. Cracks resulting from seepage damage predominantly form below the infiltration line; the higher the infiltration lines is on the slope surface, the higher the position of the main crack formations is. The displacement of the dam body primarily occurs due to the continuous expansion of major cracks; the higher the infiltration lines are on the slope surface, the larger the displacement of the dam body is. Full article
(This article belongs to the Special Issue Research Advances in Hydraulic Structure and Geotechnical Engineering)
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<p>Laboratory test tank.</p>
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<p>The water level control system.</p>
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<p>Spirit level, pin, and steel ruler.</p>
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<p>Layout of benchmarks.</p>
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<p>Red mud tamping and data monitoring.</p>
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<p>Location of sensor burial for working condition T1. (<b>a</b>) Layout location of soil pressure sensors. (<b>b</b>) Location of soil moisture sensor arrangement. (<b>c</b>) Pore water pressure sensor burial location.</p>
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<p>Location of sensor burial for working condition T1. (<b>a</b>) Layout location of soil pressure sensors. (<b>b</b>) Location of soil moisture sensor arrangement. (<b>c</b>) Pore water pressure sensor burial location.</p>
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<p>Location of sensor burial for working condition T2. (<b>a</b>) Layout location of soil pressure sensors. (<b>b</b>) Location of soil moisture sensor arrangement. (<b>c</b>) Pore water pressure sensor burial location.</p>
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<p>Location of sensor burial for working condition T2. (<b>a</b>) Layout location of soil pressure sensors. (<b>b</b>) Location of soil moisture sensor arrangement. (<b>c</b>) Pore water pressure sensor burial location.</p>
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<p>Distribution of moisture content in conditions T1 and T2.</p>
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<p>Evolution law of infiltration line under working conditions T1 and T2.</p>
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<p>Distribution of vertical soil pressure near the slope in condition T1.</p>
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<p>Distribution of horizontal soil pressure near the slope in condition T1.</p>
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<p>Transmission of horizontal thrust in condition T1.</p>
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<p>Distribution of vertical soil pressure near the slope in condition T2.</p>
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<p>Horizontal soil pressure distribution under condition T2.</p>
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<p>Trend of pore water pressure change in working conditions T1 and T2.</p>
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<p>Location of pin embedding. (<b>a</b>) Horizontal arrangement of pins. (<b>b</b>) Vertical arrangement of pins.</p>
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<p>The displacement measurement of the red mud dam body.</p>
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<p>Displacement of red mud dam body with seepage failure in condition T1. (<b>a</b>) The infiltration line reaches the slope surface. (<b>b</b>) Tiny cracks appear on the slope surface. (<b>c</b>) Red mud dam damage.</p>
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<p>Displacement of red mud dam body under condition T1.</p>
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<p>Displacement of red mud dam body with seepage failure in condition T2. (<b>a</b>) The infiltration line reaches the slope surface. (<b>b</b>) Cracks appear at the top of the slope. (<b>c</b>) Red mud dam damage.</p>
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<p>Displacement of red mud dam body under condition T2. (<b>a</b>) First column of dam displacements. (<b>b</b>) Second column of dam displacements. (<b>c</b>) Third column of dam displacements.</p>
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<p>The occurrence of micro cracks on the slope in condition T1.</p>
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<p>Development and extension of microcracks in condition T1.</p>
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<p>Longitudinal crack propagation in condition T1. (<b>a</b>) Longitudinal crack propagation in condition T1. (<b>b</b>) Crack depth during the longitudinal crack propagation stage of condition T1.</p>
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<p>Final morphology of longitudinal cracks in condition T1. (<b>a</b>) Final morphology of longitudinal cracks in condition T1. (<b>b</b>) The depth and width of the final stage of longitudinal cracks in condition T1.</p>
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<p>The occurrence of micro cracks on the slope in condition T2. (<b>a</b>) At the top of the slope. (<b>b</b>) In the middle of the slope.</p>
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<p>Development and propagation of microcracks in condition T2. (<b>a</b>) The appearance of micro cracks at the top of the slope. (<b>b</b>) The development of cracks at the top of the slope. (<b>c</b>,<b>d</b>) Expansion of cracks at the top of the slope. (<b>e</b>) The final stage of slope top cracks.</p>
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<p>Development and propagation of microcracks in condition T2. (<b>a</b>) The appearance of micro cracks at the top of the slope. (<b>b</b>) The development of cracks at the top of the slope. (<b>c</b>,<b>d</b>) Expansion of cracks at the top of the slope. (<b>e</b>) The final stage of slope top cracks.</p>
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<p>Longitudinal crack propagation in condition T2. (<b>a</b>) Expansion of longitudinal cracks in condition T2. (<b>b</b>) Crack depth during the longitudinal crack propagation stage of condition T2.</p>
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<p>Final morphology of longitudinal cracks in condition T2. (<b>a</b>) Final morphology of longitudinal cracks in condition T2. (<b>b</b>) The depth and width of the final stage of longitudinal cracks in condition T2.</p>
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18 pages, 14030 KiB  
Article
Deformation Risk Assessment of the Lar Dam: Monitoring Its Stability Condition
by Mehrnoosh Ghadimi and Mohammadali Kiani
Sustainability 2024, 16(11), 4335; https://doi.org/10.3390/su16114335 - 21 May 2024
Viewed by 646
Abstract
Dam stability is one of the most essential geotechnical engineering challenges. Studying the structural behavior of dams during their useful life is an essential component of their safety. Terrestrial surveying network approaches are typically expensive and time-consuming. Over the last decade, the interferometric [...] Read more.
Dam stability is one of the most essential geotechnical engineering challenges. Studying the structural behavior of dams during their useful life is an essential component of their safety. Terrestrial surveying network approaches are typically expensive and time-consuming. Over the last decade, the interferometric synthetic aperture radar (InSAR) method has been widely used to monitor millimeter displacements in dam crests. This research investigates the structural monitoring of the Lar Dam in Iran, using InSAR and the terrestrial surveying network technique to identify the possible failure risk of the dam. Sentinel-1A images taken from 5 February 2015 to 30 September 2019 and TerraSAR-X (09.05.2018 to 16.08.2018) images were analyzed to investigate the dam’s behavior. The InSAR results were compared with those of the terrestrial surveying network for the period of 1992 to 2019. The Sentinel-1 results implied that the dam on the left side moved over 8 mm/yr. However, the pillars to the left abutment indicated an uplift, which is consistent with the TerraSAR-X results. Also, the TerraSAR-X data indicated an 8 mm displacement over a three-month period. The terrestrial surveying showed that the largest uplift was 19.68 mm at the TB4 point on the left side and upstream of the body, while this amount was 10 mm in the interferometry analysis for the period of 2015–2020. The subsidence rate increased from the middle part toward the left abutment. The geological observations made during the ninth stage of the terrestrial surveying network indicate that there was horizontal and vertical movement over time, from 1992 to 2019. However, the results of the InSAR processing in the crown were similar to those of the terrestrial surveying network. Although different comparisons were used for the measurements, the difference in the displacement rates was reasonable, but all three methods showed the same trend in terms of uplift and displacement. Full article
(This article belongs to the Section Hazards and Sustainability)
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<p>The Lar Dam location. (<b>a</b>) The red rectangle depicts the Sentinel-1A frame; (<b>b</b>) the yellow rectangle represents the TSX frame, while the blue rectangle represents the Lar Dam location; and (<b>c</b>) the Lar geological map [<a href="#B25-sustainability-16-04335" class="html-bibr">25</a>].</p>
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<p>Geological section of the dam foundation: (<b>a</b>) lava flow at crack location; (<b>b</b>) erosion caused circular-shaped holes on the berm along the right bank [<a href="#B28-sustainability-16-04335" class="html-bibr">28</a>].</p>
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<p>A longitudinal crack formed on the berm at a height of 2462 m, with water leakage into the crack.</p>
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<p>The water escape locations near the opening pumping tunnel in the Haraz Valley (<b>a</b>) and (<b>b</b>) the Galugah Valley.</p>
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<p>The blue circles on the riprap layer of Lar Dam represent deformations.</p>
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<p>Vertical movement of the riprap layer in the Lar Dam.</p>
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<p>(<b>a</b>) Locations of the geodetic points in the Google Earth image. (<b>b</b>) Locations of the geodetic points and horizontal displacements collected in 1992, 2013, and 2019 [<a href="#B1-sustainability-16-04335" class="html-bibr">1</a>].</p>
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<p>Mean LOS velocity obtained from TerraSAR-X during the period of May 2018 to August 2018, in the ascending (<b>a</b>) and descending orbits (<b>b</b>), respectively. (<b>c</b>) The mean linear velocity with TerraSAR-X during the period of May 2018 to August 2018 in the ascending orbit.</p>
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<p>Mean LOS velocity for Sentinel-1 (2015–2019) processed using GMTSAR. Positive is toward the satellite.</p>
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<p>(<b>a</b>) The vertical deformation of pillar points on the Lar Dam in the period of 1992–2013. (<b>b</b>) The vertical deformation of pillar points on the Lar Dam in the period of 2013–2019.</p>
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<p>Comparison of vertical displacements in TerraSAR-X and Sentinel-1 images.</p>
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<p>Comparison of vertical displacements in TerraSAR-X and Sentinel-1 images.</p>
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<p>Linear regression between terrestrial surveying network and Sentinel-1.</p>
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