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17 pages, 35858 KiB  
Article
Performance Analysis of Pile Group Installation in Saturated Clay
by Wenlin Xiong, Zihang Li, Dan Hu and Fen Li
Appl. Sci. 2024, 14(18), 8321; https://doi.org/10.3390/app14188321 (registering DOI) - 15 Sep 2024
Abstract
In offshore pile engineering, the installation of jacked piles generates compaction effects within soil, thus further affecting previously installed adjacent piles. This study proposes a three-dimensional numerical model for pile group installation, soil consolidation, and loading analysis. Subsequently, the effect of pile spacing [...] Read more.
In offshore pile engineering, the installation of jacked piles generates compaction effects within soil, thus further affecting previously installed adjacent piles. This study proposes a three-dimensional numerical model for pile group installation, soil consolidation, and loading analysis. Subsequently, the effect of pile spacing and pile length-to-diameter ratio on the deformation, internal forces, and vertical bearing capacity of adjacent piles are investigated. The results indicate that with an increase in pile center distance, the peak lateral displacement of the adjacent piles decreases, whereas the peak vertical displacement increases. As the pile length-to-diameter ratio increases, the peak vertical and lateral displacements of the adjacent piles are enhanced. In addition, the peak axial force of the adjacent piles initially decreases and then increases with the penetration depth of the subsequent pile, whereas the peak bending moment initially increases and then decreases. The vertical bearing capacity of the subsequent pile is significantly superior to that of the adjacent piles. Therefore, the effects of pile installation on adjacent piles should be included in pile engineering. The impact of the subsequent pile installation on the bearing capacity of adjacent piles can be significantly reduced by increasing the pile center distance and pile length-to-diameter ratio. The findings provide useful guidance for pile group engineering. Full article
(This article belongs to the Section Marine Science and Engineering)
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Figure 1

Figure 1
<p>(<b>a</b>) Geometry mesh and (<b>b</b>) model boundary conditions.</p>
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<p>Soil response caused by single pile installation: (<b>a</b>) radial displacement, (<b>b</b>) excess pore pressure, (<b>c</b>) volumetric stress, and (<b>d</b>) variation in volumetric stress with depth.</p>
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<p>Comparison of calculated (<b>a</b>) radial soil displacement [<a href="#B3-applsci-14-08321" class="html-bibr">3</a>,<a href="#B36-applsci-14-08321" class="html-bibr">36</a>] and (<b>b</b>) excess pore pressure with test results along the radial distance [<a href="#B3-applsci-14-08321" class="html-bibr">3</a>,<a href="#B12-applsci-14-08321" class="html-bibr">12</a>,<a href="#B37-applsci-14-08321" class="html-bibr">37</a>,<a href="#B38-applsci-14-08321" class="html-bibr">38</a>].</p>
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<p>Dissipation of excess pore pressure in the soil consolidation stage [<a href="#B33-applsci-14-08321" class="html-bibr">33</a>].</p>
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<p>Load–displacement curve of the pile after 8.65 days of consolidation [<a href="#B33-applsci-14-08321" class="html-bibr">33</a>].</p>
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<p>Schematic diagram of the two-pile group installation.</p>
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<p>Schematic diagram of the separate auxiliary tube method.</p>
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<p>Lateral displacement of adjacent pile with subsequent pile penetration depth.</p>
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<p>The effect of <span class="html-italic">S</span> and <span class="html-italic">L</span>/<span class="html-italic">D</span><sub>e</sub> on the lateral displacement of the adjacent pile.</p>
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<p>The influence of <span class="html-italic">S</span> and <span class="html-italic">L</span>/<span class="html-italic">D</span><sub>e</sub> on the vertical displacement of the adjacent pile.</p>
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<p>Influence of <span class="html-italic">S</span> and <span class="html-italic">L</span>/<span class="html-italic">D</span><sub>e</sub> on the peak displacement of the adjacent pile.</p>
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<p>Internal forces of adjacent pile with different penetration depths of subsequent pile.</p>
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<p>Variation in peak axial force and peak bending moment with <span class="html-italic">S</span>.</p>
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<p>Variation in peak axial force and peak bending moment with <span class="html-italic">L</span>/<span class="html-italic">D</span><sub>e</sub>.</p>
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<p>Pore pressure distribution of soil at different times: (<b>a</b>) after pile installation, (<b>b</b>) after 5 days, (<b>c</b>) after 10 days, (<b>d</b>) after 20 days, (<b>e</b>) after 50 days, and (<b>f</b>) after 100 days.</p>
Full article ">Figure 15 Cont.
<p>Pore pressure distribution of soil at different times: (<b>a</b>) after pile installation, (<b>b</b>) after 5 days, (<b>c</b>) after 10 days, (<b>d</b>) after 20 days, (<b>e</b>) after 50 days, and (<b>f</b>) after 100 days.</p>
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<p>Variation in radial effective stress in soil at different depths.</p>
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<p>Load–displacement curves of piles.</p>
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<p>Changes in vertical bearing capacity of the adjacent and subsequent pile with time.</p>
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<p>Effects of <span class="html-italic">S</span> and <span class="html-italic">L</span>/<span class="html-italic">D</span><sub>e</sub> on vertical bearing capacity of adjacent pile.</p>
Full article ">
15 pages, 19478 KiB  
Article
Source Apportionment and Human Health Risks of Potentially Toxic Elements in the Surface Water of Coal Mining Areas
by Yuting Yan, Yunhui Zhang, Zhan Xie, Xiangchuan Wu, Chunlin Tu, Qingsong Chen and Lanchu Tao
Toxics 2024, 12(9), 673; https://doi.org/10.3390/toxics12090673 (registering DOI) - 15 Sep 2024
Abstract
Contamination with potentially toxic elements (PTEs) frequently occurs in surface water in coal mining areas. This study analyzed 34 surface water samples collected from the Yunnan–Guizhou Plateau for their hydrochemical characteristics, spatial distribution, source apportionment, and human health risks. Our statistical analysis showed [...] Read more.
Contamination with potentially toxic elements (PTEs) frequently occurs in surface water in coal mining areas. This study analyzed 34 surface water samples collected from the Yunnan–Guizhou Plateau for their hydrochemical characteristics, spatial distribution, source apportionment, and human health risks. Our statistical analysis showed that the average concentrations of PTEs in the surface water ranked as follows: Fe > Al > Zn > Mn > Ba > B> Ni > Li > Cd > Mo > Cu > Co > Hg > Se > As > Pb > Sb. The spatial analysis revealed that samples with high concentrations of Fe, Al, and Mn were predominantly distributed in the main stream, Xichong River, and Yangchang River. Positive matrix factorization (PMF) identified four sources of PTEs in the surface water. Hg, As, and Se originated from wastewater discharged by coal preparation plants and coal mines. Mo, Li, and B originated from the dissolution of clay minerals in coal seams. Elevated concentrations of Cu, Fe, Al, Mn, Co, and Ni were attributed to the dissolution of kaolinite, illite, chalcopyrite, pyrite, and minerals associated with Co and Ni in coal seams. Cd, Zn, and Pb were derived from coal melting and traffic release. The deterministic health risks assessment showed that 94.12% of the surface water samples presented non-carcinogenic risks below the health limit of 1. Meanwhile, 73.56% of the surface water samples with elevated As posed level III carcinogenic risk to the local populations. Special attention to drinking water safety for children is warranted due to their lower metabolic capacity for detoxifying PTEs. This study provides insight for PTE management in sustainable water environments. Full article
(This article belongs to the Section Metals and Radioactive Substances)
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Figure 1
<p>(<b>a</b>) Location of the Yunnan–Guizhou Plateau in China, (<b>b</b>) location of the study area in the Yunnan–Guizhou Plateau, and (<b>c</b>) location of surface water, groundwater, and mine water sampling sites in the study area (sample size = 34).</p>
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<p>Box plots with the standard of potentially toxic elements for drinking surface water (sample size = 34).</p>
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<p>Spatial distribution map of concentrations of potentially toxic elements: (<b>a</b>) Fe, (<b>b</b>) Mn, (<b>c</b>) Cu, (<b>d</b>) Zn, (<b>e</b>) Al, (<b>f</b>) Hg, (<b>g</b>) As, (<b>h</b>) Se, (<b>i</b>) Cd, (<b>j</b>) Pb, (<b>k</b>) Li, (<b>l</b>) B, (<b>m</b>) Ba, (<b>n</b>) Sb, (<b>o</b>) Ni, (<b>p</b>) Co, and (<b>q</b>) Mo (sample size = 34).</p>
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<p>Source contributions of PTEs based on the PMF model: (<b>a</b>) relative contributions of PTEs to PMF factors and (<b>b</b>) average contributions of PMF factors (sample size = 34).</p>
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<p>Non-carcinogenic health risks of surface water to children, men, and women: (<b>a</b>) Fe, (<b>b</b>) Mn, (<b>c</b>) Cu, (<b>d</b>) Zn, (<b>e</b>) Al, (<b>f</b>) As, (<b>g</b>) Se, (<b>h</b>) Cd, (<b>i</b>) Li, (<b>j</b>) B, (<b>k</b>) Ba, (<b>l</b>) Sb, (<b>m</b>) Ni, (<b>n</b>) Co, and (<b>o</b>) Mo (sample size = 34).</p>
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<p>Sensitive non-carcinogenic PTE ranking for HI.</p>
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<p>Non-carcinogenic and carcinogenic health risks of PTEs in surface water to children, men, and women: (<b>a</b>) hazard index (HI) and (<b>b</b>) cancer risk (CR) (sample size = 34).</p>
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<p>Spatial distribution map of hazard index (HI) and cancer risk (CR) of PTEs in surface water. HI to (<b>a</b>) children, (<b>b</b>) men, and (<b>c</b>) women and CR to (<b>d</b>) children, (<b>e</b>) men, and (<b>f</b>) women (sample size = 34).</p>
Full article ">
17 pages, 6340 KiB  
Article
Shale Oil Generation Conditions and Exploration Prospects of the Cretaceous Nenjiang Formation in the Changling Depression, Songliao Basin, China
by Wenjun Zhang, Wenyu Zhang, Shumin Lin, Xing Ke, Min Zhang and Taohua He
Minerals 2024, 14(9), 942; https://doi.org/10.3390/min14090942 (registering DOI) - 15 Sep 2024
Abstract
Low-maturity shale oil predominates in shale oil resources. China’s onshore shale oil, particularly the Cretaceous Nenjiang Formation in the Songliao Basin, holds significant potential for low-maturity shale oil, presenting promising exploration and development prospects. This study delves into the hydrocarbon generation conditions, reservoir [...] Read more.
Low-maturity shale oil predominates in shale oil resources. China’s onshore shale oil, particularly the Cretaceous Nenjiang Formation in the Songliao Basin, holds significant potential for low-maturity shale oil, presenting promising exploration and development prospects. This study delves into the hydrocarbon generation conditions, reservoir characteristics, and oil-bearing property analysis of the mud shale from the Nen-1 and Nen-2 sub-formations of the Nenjiang Formation to pinpoint favorable intervals for shale oil exploration. Through the integration of lithology, pressure, and fracture distribution data in the study area, favorable zones were delineated. The Nen-1 sub-formation is widely distributed in the Changling Depression, with mud shale thickness ranging from 30 to 100 m and a total organic content exceeding 2.0%. Type I kerogen predominated as the source rock, while some samples contained type II kerogen. Organic microcomponents primarily comprised algal bodies, with vitrinite reflectance (Ro) ranging from 0.5% to 0.8%. Compared to Nen-1 shale, Nen-2 shale exhibited less total organic content, kerogen type, and thermal evolution degree, albeit both are conducive to low-maturity shale oil generation. The Nen-1 and Nen-2 sub-formations predominantly consist of clay, quartz, feldspar, calcite, and pyrite minerals, with minor dolomite, siderite, and anhydrite. Hydrocarbons primarily reside in microfractures and micropores, including interlayer micropores, organic matter micropores, intra-cuticle micropores, and intercrystalline microporosity, with interlayer and intra-cuticle micropores being dominant. The free oil content (S1) in Nen-1 shale ranged from 0.01 mg/g to 5.04 mg/g (average: 1.13 mg/g), while in Nen-2 shale, it ranged from 0.01 mg/g to 3.28 mg/g (average: 0.75 mg/g). The Nen-1 and Nen-2 sub-formations are identified as potential intervals for shale oil exploration. Considering total organic content, oil saturation, vitrinite reflectance, and shale formation thickness in the study area, the favorable zone for low-maturity shale oil generation is primarily situated in the Heidimiao Sub-Depression and its vicinity. The Nen-2 shale-oil-enriched zone is concentrated in the northwest part of the Heidimiao Sub-Depression, while the Nen-1 shale-oil-enriched zone lies in the northeast part. Full article
(This article belongs to the Topic Petroleum Geology and Geochemistry of Sedimentary Basins)
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Figure 1

Figure 1
<p>Structural unit and stratigraphic section of the Changling Sag in the Songliao Basin. The two pentagonal stars are the main layers of this study.</p>
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<p>The TOC distribution frequency diagram of the Nen-1 and Nen-2 in the Changling Sag.</p>
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<p>The division diagram of organic matter types in the Nen-1 and Nen-2 in the Changling Sag.</p>
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<p>The relationship between <span class="html-italic">R<sub>o</sub></span>, <span class="html-italic">T</span><sub>max</sub>, and buried depth of the Nen-1 and Nen-2 in the Changling Sag.</p>
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<p>Comprehensive evaluation map of hydrocarbon generation potential and hydrocarbon generation tendency of the Nen-1 and Nen-2 in the Changling Sag, Songliao Basin.</p>
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<p>Mineral composition content diagram of shale in the Nen-1 and Nen-2 in the Changling Depression (taking Yaonan 5 well as an example).</p>
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<p>Micropore diameter distribution map of the Nenjiang Formation in the Changling Sag.</p>
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<p>Distribution of the pore throat radius of the Nen 1 shale in the Yaonan 5 well of the Changling Sag, Songliao Basin.</p>
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<p>The crossplot of source rocks (S<sub>1</sub> + S<sub>2</sub>), S<sub>1</sub> and TOC in the Nen-1 and Nen-2 in the Changling Depression.</p>
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<p>The variation trend of S<sub>1</sub> (<b>a</b>) and OSI (<b>b</b>) with depth in the Nen-1 and Nen-2 in the Changling Sag.</p>
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<p>The favorable enrichment area of shale oil in the Nen-2 in the Changling Sag, Songliao Basin.</p>
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<p>The favorable enrichment area of shale oil in the Nen-1 in the Changling Sag, Songliao Basin.</p>
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17 pages, 1399 KiB  
Article
Wood- and Manure-Derived Biochars Reduce Antibiotic Residues and Shift Antibiotic Resistance Genes and Microbial Communities in Manure Applied Forage–Soil Systems
by Gyucheol Choi, Jeff A. Brady, Olabiyi Obayomi, Emily Green, Caroly Leija, Kristin Sefcik, Daisy Gonzalez, Cosette B. Taggart, James P. Muir and Eunsung Kan
Agronomy 2024, 14(9), 2100; https://doi.org/10.3390/agronomy14092100 (registering DOI) - 15 Sep 2024
Viewed by 147
Abstract
The increasing use of antibiotics in livestock poses environmental risks, leading to contamination of agricultural soils and propagation of microbial antibiotic-resistant genes (ARGs). This study examined the impacts of wood- and manure-derived biochar (BC) on antibiotic residues, ARGs, and microbial communities in sandy [...] Read more.
The increasing use of antibiotics in livestock poses environmental risks, leading to contamination of agricultural soils and propagation of microbial antibiotic-resistant genes (ARGs). This study examined the impacts of wood- and manure-derived biochar (BC) on antibiotic residues, ARGs, and microbial communities in sandy loam and clay loam soils amended with manure in Cynodon dactylon pastures. We hypothesized that BC amendments would influence the degradation of antibiotics and the structure of microbial communities based on their physicochemical properties and soil types. Our results demonstrated that wood BC reduced the concentrations of tetracycline and sulfonamides, particularly in sandy loam soil, due to its larger surface area and hydrophobic properties. In contrast, manure BC provided additional nutrients and supported atmospheric nitrogen-fixing microbial groups, especially in clay loam soil, while exhibiting variable efficiency in reducing antibiotic residues due to its lower surface area and higher ash content. These findings underscore the differential impacts of each BC type, emphasizing the need for tailored BC applications based on soil type to effectively mitigate antibiotic contamination and promote sustainable agricultural practices. In conclusion, wood BC was more effective in enhancing soil health by reducing antibiotic residues and improving microbial diversity, particularly in sandy loam soils, while manure BC was beneficial for nutrient cycling in clay loam soils. Full article
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Figure 1
<p>Residual tetracycline (<b>A</b>) and SMZ/SMX (<b>B</b>) concentration in each soil after 90 days. Different letters above bars indicate significant differences between conditions (<span class="html-italic">p</span> &lt; 0.05, Duncan’s test). Sandy loam, SL; clay loam, CL; no biochar, NB (white); wood biochar, WB (gray); manure biochar, MB (black).</p>
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<p>Taxonomic distribution of prokaryotic (<b>A</b>) and fungal (<b>B</b>) sequences at the phylum level for each condition. Sequences with a relative abundance of &lt;1% in all samples were classified as “Others”. SL = sandy loam soil; CL = clay loam soil; MB = manure biochar; WB = wood biochar; NB = no biochar applied.</p>
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<p>NMDS plot for prokaryotic community structure (<b>A</b>) and fungal community structure (<b>B</b>) based on phylum-level distribution. Samples are labeled with the corresponding condition. SL = sandy loam soil; CL = clay loam soil; MB = manure biochar; WB = wood biochar; NB = no biochar applied.</p>
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<p>Relative abundance of <span class="html-italic">tetA</span> and <span class="html-italic">folP</span> based on the PICRUSt prediction model. Different letters above bars indicate significant differences between conditions (<span class="html-italic">p</span> &lt; 0.05, Duncan’s test). SL = sandy loam soil; CL = clay loam soil; MB = manure biochar; WB = wood biochar; NB = no biochar applied.</p>
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16 pages, 11780 KiB  
Article
Hydraulic and Hydrogeochemical Characterization of Carbonate Aquifers in Arid Regions: A Case from the Western Desert, Egypt
by Mahmoud M. Khalil, Mostafa Mahmoud, Dimitrios E. Alexakis, Dimitra E. Gamvroula, Emad Youssef, Esam El-Sayed, Mohamed H. Farag, Mohamed Ahmed, Peiyue Li, Ahmed Ali and Esam Ismail
Water 2024, 16(18), 2610; https://doi.org/10.3390/w16182610 (registering DOI) - 14 Sep 2024
Viewed by 244
Abstract
Using geochemical and pumping test data from 80 groundwater wells, the chemical, hydrologic, and hydraulic properties of the fractured Eocene carbonate aquifer located west of the Al-Minya district, the Western Desert, Egypt, have been characterized and determined to guarantee sustainable management of groundwater [...] Read more.
Using geochemical and pumping test data from 80 groundwater wells, the chemical, hydrologic, and hydraulic properties of the fractured Eocene carbonate aquifer located west of the Al-Minya district, the Western Desert, Egypt, have been characterized and determined to guarantee sustainable management of groundwater resources under large-scale desert reclamation projects. The hydrochemical data show that groundwater from the fractured Eocene carbonate aquifer has a high concentration of Na+ and Cl and varies in salinity from 2176 to 2912 mg/L (brackish water). Water–rock interaction and ion exchange processes are the most dominant processes controlling groundwater composition. The carbonate aquifer exists under confined to semi-confined conditions, and the depth to groundwater increases eastward. From the potentiometric head data, deep-seated faults are the suggested pathways for gas-rich water ascending from the deep Nubian aquifer system into the overlying shallow carbonate aquifer. This mechanism enhances the dissolution and karstification of carbonate rocks, especially in the vicinity of faulted sites, and is supported by the significant loss of mud circulation during well drilling operations. The average estimated hydraulic parameters, based on the analysis of step-drawdown, long-duration pumping and recovery tests, indicate that the Eocene carbonate aquifer has a wide range of transmissivity (T) that is between 336.39 and 389,309.28 m2/d (average: 18,405.21 m2/d), hydraulic conductivity (K) between 1.31 and 1420.84 m/d (average: 70.29 m/d), and specific capacity (Sc) between 44.4 and 17,376.24 m2/d (average: 45.24 m2/d). On the other hand, the performance characteristics of drilled wells show that well efficiency ranges between 0.47 and 97.08%, and well losses range between 2.92 and 99.53%. In addition to variations in carbonate aquifer thickness and clay/shale content, the existence of strong karstification features, i.e., fissures, fractures or caverns, and solution cavities, in the Eocene carbonate aquifer are responsible for variability in the K and T values. The observed high well losses might be related to turbulent flow within and adjacent to the wells drilled in conductive fracture zones. The current approach can be further used to enhance local aquifer models and improve strategies for identifying the most productive zones in similar aquifer systems. Full article
22 pages, 19530 KiB  
Article
Cascading Landslide: Kinematic and Finite Element Method Analysis through Remote Sensing Techniques
by Claudia Zito, Massimo Mangifesta, Mirko Francioni, Luigi Guerriero, Diego Di Martire, Domenico Calcaterra and Nicola Sciarra
Remote Sens. 2024, 16(18), 3423; https://doi.org/10.3390/rs16183423 (registering DOI) - 14 Sep 2024
Viewed by 217
Abstract
Cascading landslides are specific multi-hazard events in which a primary movement triggers successive landslide processes. Areas with dynamic and quickly changing environments are more prone to this type of phenomena. Both the kind and the evolution velocity of a landslide depends on the [...] Read more.
Cascading landslides are specific multi-hazard events in which a primary movement triggers successive landslide processes. Areas with dynamic and quickly changing environments are more prone to this type of phenomena. Both the kind and the evolution velocity of a landslide depends on the materials involved. Indeed, rockfalls are generated when rocks fall from a very steep slope, while debris flow and/or mudslides are generated by fine materials like silt and clay after strong water imbibition. These events can amplify the damage caused by the initial trigger and propagate instability along a slope, often resulting in significant environmental and societal impacts. The Morino-Rendinara cascading landslide, situated in the Ernici Mountains along the border of the Abruzzo and Lazio regions (Italy), serves as a notable example of the complexities and devastating consequences associated with such events. In March 2021, a substantial debris flow event obstructed the Liri River, marking the latest step in a series of landslide events. Conventional techniques such as geomorphological observations and geological surveys may not provide exhaustive information to explain the landslide phenomena in progress. For this reason, UAV image acquisition, InSAR interferometry, and pixel offset analysis can be used to improve the knowledge of the mechanism and kinematics of landslide events. In this work, the interferometric data ranged from 3 January 2020 to 24 March 2023, while the pixel offset data covered the period from 2016 to 2022. The choice of such an extensive data window provided comprehensive insight into the investigated events, including the possibility of identifying other unrecorded events and aiding in the development of more effective mitigation strategies. Furthermore, to supplement the analysis, a specific finite element method for slope stability analysis was used to reconstruct the deep geometry of the system, emphasizing the effect of groundwater-level flow on slope stability. All of the findings indicate that major landslide activities were concentrated during the heavy rainfall season, with movements ranging from several centimeters per year. These results were consistent with numerical analyses, which showed that the potential slip surface became significantly more unstable when the water table was elevated. Full article
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Figure 1
<p>Aerial and field images of the Morino-Rendinara landslide that are representative of the impact of the landslide on the environment. (<b>a</b>) Overview of phenomenon taken from Google Earth [<a href="#B16-remotesensing-16-03423" class="html-bibr">16</a>] satellite images of 13 June 2022, from the upper sector near Morino Hamlet to the lower sector, Liri River, and deep-seated rotational slide; (<b>b</b>) Details of rockfall/avalanches sector; (<b>c</b>) Debris flow source area; (<b>d</b>) Debris flow transit zone; (<b>e</b>) Lowest debris flow transit zone; (<b>f</b>) Liri River dam; and (<b>g</b>) Effect on Liri River dam.</p>
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<p>Geographical location of Morino-Rendinara. Green lines indicate the regional boundaries; red lines indicate the municipality of Morino, Castronovo, and San Vincenzo Valle Roveto composing the involved municipality; the light blue square indicates the landslide and the study area.</p>
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<p>Geological map extract from the CARG (Geological CARtography Map n.220 Sora) Project [<a href="#B22-remotesensing-16-03423" class="html-bibr">22</a>], with indications of the geological formations and tectonic processes present in the area.</p>
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<p>Maps of the survey and debritic cover layer reconstruction using cross-sections to empathize the heterogeneity of deposits covering the substrate. (a) The section develops on maximum slope line. (b) The section develops on perpendicular direction.</p>
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<p>Conceptual flow chart of the work phases.</p>
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<p>Spatiotemporal baseline map of SBAS-InSAR interferometric data of ascending track (<b>a</b>) and descending track (<b>b</b>).</p>
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<p>The inventory map was drawn using the results of the study. The image identifies three main mechanisms: a rockfall in the upper part, a deep-seated rotational slide in the central part, and a debris flow in the lower part.</p>
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<p>Details of the landslide inventory map. The various fillings show the different landslide types identified in the study area: the rockfall in the upper part, the deep-seated rotational slide in the central part, and the debris flow in the lower part of the slope.</p>
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<p>PS velocity along the ascending (<b>a</b>) and descending (<b>b</b>) geometries from 2020 to 2023. Red dots indicate major velocity trends and instability, green and blue dots indicate minor velocity and stable sectors.</p>
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<p>Selected time series in ascending geometry (<b>a</b>) and descending geometry (<b>b</b>). The analyzed time series illustrates a very unstable sector represented by reflectors P106_60-61 and 102_57 in ascending geometry and P_70_141-141-136 in descending geometry. Additionally, some stable sectors are represented, such as P_83_135-143, P_85_68, and P_86_69.</p>
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<p>Time series vs. rainfall analyses. (<b>a</b>) Monthly cumulative rainfall for analysis period vs. one ascending and descending representative time series; (<b>b</b>) Daily cumulative rainfall for analysis period vs. one ascending and descending representative time series; (<b>c</b>) Cumulative rainfall for analysis period vs. one ascending and descending representative time series.</p>
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<p>Shear strain index results of the 2D numerical modelling with different pore pressure conditions. (<b>a</b>) Analysis without pore pressure; (<b>b</b>) Analysis with water table 0.5 m from ground level; (<b>c</b>) Analysis with water table 2.0 m from ground level; (<b>d</b>) Analysis with water table 6.0 m from ground level.</p>
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23 pages, 11116 KiB  
Article
Experimental and Numerical Characterization of the In-Plane Shear Behavior of a Load-Bearing Hollow Clay Brick Masonry System with High Thermal Performance
by Michele Serpilli, Alessandro Cameli and Francesca Stazi
Buildings 2024, 14(9), 2903; https://doi.org/10.3390/buildings14092903 (registering DOI) - 14 Sep 2024
Viewed by 151
Abstract
Modern masonry systems are generally built with hollow clay bricks with high thermal insulating properties, fulfilling the latest sustainability and environmental criteria for constructions. Despite the growing use of sustainable masonries in seismic-prone countries, there is a notable lack of experimental and numerical [...] Read more.
Modern masonry systems are generally built with hollow clay bricks with high thermal insulating properties, fulfilling the latest sustainability and environmental criteria for constructions. Despite the growing use of sustainable masonries in seismic-prone countries, there is a notable lack of experimental and numerical data on their structural behavior under lateral in-plane loads. The present study investigates the in-plane shear behavior of load-bearing masonry walls with thin bed joints and thermal insulating hollow clay blocks. Shear-compression tests were performed on three specimens to obtain information about their shear strength, displacement capacity and failure modes. The experimental characterization was supplemented by three shear tests on triplets, along with flexural and compression tests on the mortar for the thin joints. Furthermore, two Finite Element (FE) models were built to simulate the shear-compression tests, considering different constitutive laws and brick-to-brick contact types. The numerical simulations were able to describe both the shear failure modes and the shear strength values. The results showed that the experimental shear strength was 53% higher than the one obtained through Eurocode 6. The maximum shear load was found to be up to 75% greater compared to similar masonry specimens from the literature. These findings contribute to a better understanding of the potential structural applications of sustainable hollow clay block masonry in earthquake-prone areas. Full article
(This article belongs to the Special Issue The Latest Research on Building Materials and Structures)
20 pages, 1236 KiB  
Article
Photo-Fenton Treatment under UV and Vis Light Reduces Pollution and Toxicity in Water from Madín Dam, Mexico
by Deysi Amado-Piña, Rubi Romero, Emmanuel Salazar Carmona, Armando Ramírez-Serrano, Leobardo Manuel Gómez-Oliván, Gustavo Elizalde-Velázquez and Reyna Natividad
Catalysts 2024, 14(9), 620; https://doi.org/10.3390/catal14090620 (registering DOI) - 14 Sep 2024
Viewed by 171
Abstract
Water from Madín Dam in Mexico has been shown to contain a wide variety of pollutants such as drugs, pesticides, personal care products and compounds that are released into the environment as waste from production processes. In this work, the effect of the [...] Read more.
Water from Madín Dam in Mexico has been shown to contain a wide variety of pollutants such as drugs, pesticides, personal care products and compounds that are released into the environment as waste from production processes. In this work, the effect of the main process variables on the percentage of total organic carbon (TOC) removal in water samples from the Madín reservoir was studied by applying a photo-Fenton treatment catalyzed with iron-pillared clays. The catalyst was characterized by XRD, N2 physisorption, DRS and XPS. The sampling and characterization of the water from the Madín reservoir was carried out according to Mexican standards. The system for treatment tests was 0.1 L of reaction volume and a controlled temperature of 23–25 °C, and the reaction system was kept under constant stirring. After 4 h of treatment time under UV light, the TOC removal was 90%, and it was 60% under Vis light. The main ROS involved in the photo-Fenton process driven by UVC light were hydroxyl radicals, while hydroperoxyl radicals predominate in the Vis-light-driven process. Evidence of superoxide anion participation was not found. The toxicity of untreated and treated water was assessed on Danio rerio specimens, and it was observed to be reduced after the photo-Fenton treatment. Full article
(This article belongs to the Section Photocatalysis)
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<p>Diffractograms of Fe-PILC and bentonite clay.</p>
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<p>Total organic carbon removal efficiency in water samples from Madín reservoir through different treatment processes. Reaction volume: 0.1 L, T: 25 C, pH<sub>o</sub>: 6.02, treatment time: 60 min, UV light: 254 nm, 166 W/m<sup>2</sup>, Vis light: (3 lamps, 100 W/m<sup>2</sup> each).</p>
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<p>Effect of initial oxygen presence (photo-Fenton-N<sub>2</sub>) and addition of radical scavengers (isopropanol, IPA; benzoquinone, BQ) to the photo-Fenton system under (<b>a</b>) UVC light (254 nm, 166 W/m<sup>2</sup>) and (<b>b</b>) Vis light (3 lamps, 100 W/m<sup>2</sup> each). Reaction conditions: volume: 0.1 L, T: 25 °C, pH<sub>o</sub>: 6.02, catalyst loading (W<sub>cat</sub>): 0.500 g/L, reaction time: 60 min for processes in (<b>a</b>) and 240 min for processes in (<b>b</b>).</p>
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<p>Location of the water sampling stations inside the Madín Dam: New Madín (1), Old Madín (2), entrance of the Tlalnepantla River (3), entrance of the San Juan River (4), dam curtain (5).</p>
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17 pages, 11981 KiB  
Article
The Enamelled Tiles of Olite’s Castle (Spain): Characterization, Provenance, and Manufacture Technology
by Iván Ruiz-Ardanaz, Esther Lasheras and Adrián Durán
Crystals 2024, 14(9), 813; https://doi.org/10.3390/cryst14090813 (registering DOI) - 14 Sep 2024
Viewed by 188
Abstract
The objective of this study was to determine the authorship, provenance, and technology of the mudejar enamelled tiles from the Olite Castle (northern Spain, 14th century). According to previous knowledge, Olite’s enamelled tiles had been manufactured in Manises (Valencia, Spain). The analysis of [...] Read more.
The objective of this study was to determine the authorship, provenance, and technology of the mudejar enamelled tiles from the Olite Castle (northern Spain, 14th century). According to previous knowledge, Olite’s enamelled tiles had been manufactured in Manises (Valencia, Spain). The analysis of ceramic pastes revealed the existence of two different chemical compositions, suggesting the use of two different clay sources, probably one from the Tudela area, and another from the Tafalla–Olite area. Those probably made in the Tudela area stood out with a higher diopside (CaMgSi2O6) content. Those probably made in the Tafalla–Olite area stood out for their calcium-bearing minerals, such as calcite (CaCO3) or gehlenite (Ca2Al(AlSi)O7). On this basis, production in Manises has been ruled out. However, it is highly probable that the artisans of Manises would have led the production from Tudela. The study of the firing temperatures and composition of the enamels indicated that the production methods and materials used in Tafalla–Olite (800–850 °C) and Tudela (higher than 900 °C) were different, reflecting the influence of local and Manises artisans, respectively. In Olite tiles, enamel was applied following recipes from the 14th and 15th centuries. Full article
(This article belongs to the Collection Topic Collection: Mineralogical Crystallography)
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<p>(<b>a</b>) A reconstruction drawing of the Tudela Castle in the 14th century by Iñaki Dieguez Uribeondo. (<b>b</b>) An image of the New Palace of Olite Castle today by Jorab (licenced under CC BY 3.0.) [<a href="#B4-crystals-14-00813" class="html-bibr">4</a>,<a href="#B5-crystals-14-00813" class="html-bibr">5</a>].</p>
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<p>(<b>a</b>) The location of Olite and the rest of the places mentioned in the text in northeastern Spain at the beginning of the 15th century. (<b>b</b>) A map of Olite’s castle with its differentiated areas [<a href="#B6-crystals-14-00813" class="html-bibr">6</a>].</p>
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<p>A digital reconstruction of the enamelled wall tiles, paving tiles, bricks, and roof tiles found in Olite’s castle. Only two brown enamel thin tiles have been discovered, although they probably also existed in the form of thick tiles, roof tiles, and bricks.</p>
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<p>Analysed samples from Olite’s castle: OM-1 to -3, polychrome thin tile; OT-1 to -3, monochrome green enamelled thin tile; OT-4, monochrome green enamelled thin tile; OT-5, monochrome blue enamelled thick tile; OT-6, white enamelled brick; and OT-7, blue enamelled brick.</p>
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<p>X-ray diffraction patterns of the pastes from Olite’s castle. Abbreviations: I–illite; A–anorthite; N–analcime; G–gehlenite; Q–quartz; C–calcite; D–diopside; H–haematite.</p>
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<p>X-ray diffraction patterns of the enamels from Olite’s castle. Abbreviations: Y–gypsum; Q–quartz; Cs–Cassiterite; C–calcite; D–diopside.</p>
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<p>Visual schematic representation of quartz, diopside, and cassiterite structures. Modified from Webmineral.com [<a href="#B23-crystals-14-00813" class="html-bibr">23</a>].</p>
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<p>Optical microscope images of cross-sections of samples OM-1, OM-2, OT-1, OT-4, OT-5, OT-6, and OT-7.</p>
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<p>FE-SEM/EDS images of samples OM-1 (<b>a</b>) and OT-1 (<b>b</b>). Note that in <a href="#crystals-14-00813-f009" class="html-fig">Figure 9</a>a, the enamelled surface is rotated 13° counterclockwise and <a href="#crystals-14-00813-f009" class="html-fig">Figure 9</a>b is rotated 116° clockwise. Abbreviations: SE—secondary electron image.</p>
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14 pages, 3830 KiB  
Article
Calcined Clays as Concrete Additive in Structural Concrete: Workability, Mechanical Properties, Durability, and Sustainability Performance
by Bastian Strybny, Tobias Schack, Julian Link and Michael Haist
Materials 2024, 17(18), 4517; https://doi.org/10.3390/ma17184517 (registering DOI) - 14 Sep 2024
Viewed by 274
Abstract
Calcined clays (CCs) as supplementary cementitious materials (SCMs) can be a promising option to reduce clinker content and CO2 emissions in eco-friendly concretes. Although CCs as components of composite cements in combination with Ordinary Portland Cement (OPC) and limestone powder (LSP) have [...] Read more.
Calcined clays (CCs) as supplementary cementitious materials (SCMs) can be a promising option to reduce clinker content and CO2 emissions in eco-friendly concretes. Although CCs as components of composite cements in combination with Ordinary Portland Cement (OPC) and limestone powder (LSP) have attracted industry interest, their use as concrete additives is limited. This study investigates the effects of the addition of CCs on the fresh and hardened properties of industry-standard ready-mixed concretes. Four concrete mix designs, each with three superplasticizer dosages, were tested, resulting in 12 variations. The CCs used, which are typical of 2:1 bentonite clays with low metakaolin content, reflect the clays available in Germany. The results showed that CCs significantly influenced the workability, which could be controlled with a high superplasticizer dosage. Increased CC contents reduced bleeding tendencies, which was beneficial for certain structural applications. Early age strength decreased with CCs, but the 28-day strength exceeded that of pure OPC concretes up to 30 wt% CCs. Resistance to CO2-induced carbonation decreased with higher levels of CCs but was comparable up to 15 wt%. Freeze–thaw damage decreased, and chloride migration resistance improved due to a denser microstructure. The global warming potential (GWP) of the concretes tested is in line with that reported in the literature for concretes made from highly blended cements, suggesting that CCs can improve the sustainability of concrete production. Full article
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<p>(<b>a</b>) Changes of the concrete spread flow diameter in dependence of the CC content for concretes without superplasticizer but with different water–binder ratios; (<b>b</b>) for concretes with various superplasticizer dosages and constant water–binder ratios w/b = 0.5.</p>
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<p>(<b>a</b>) Changes of the concrete spread flow diameter in dependence of the hydration time for different CC contents with superplasticizer dosages of 1.00 wt% per binder; (<b>b</b>) for a selected mix with a CC content of 15 wt% with various superplasticizer dosages.</p>
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<p>Changes in the maximum bleeding water are dependent on the CC content for concretes with different superplasticizer dosages.</p>
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<p>(<b>a</b>) Compressive strength of all concrete compositions investigated as a function of age; (<b>b</b>) compressive strength as a function of CC content (numbers and arrows indicate the factor by which the strength increased between 7 d and 28 d).</p>
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<p>Changes of the carbonation depth in dependence on the CC content after 7 d and 28 d concrete age according to [<a href="#B45-materials-17-04517" class="html-bibr">45</a>].</p>
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<p>Chloride migration coefficient D<sub>Cl</sub> determined with the RCM test [<a href="#B46-materials-17-04517" class="html-bibr">46</a>].</p>
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<p>(<b>a</b>) Internal damage—relative dynamic modulus of elasticity; (<b>b</b>) and outer damage—concrete spalling—of all concretes investigated with the CIF-test according to [<a href="#B47-materials-17-04517" class="html-bibr">47</a>].</p>
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<p>(<b>a</b>) Binder intensity b<sub>i</sub>; (<b>b</b>) CO<sub>2,e</sub> intensity for the results from this study compared to the literature data [<a href="#B8-materials-17-04517" class="html-bibr">8</a>,<a href="#B50-materials-17-04517" class="html-bibr">50</a>,<a href="#B51-materials-17-04517" class="html-bibr">51</a>].</p>
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14 pages, 2618 KiB  
Review
A Critical Review of the Crucial Role of the Yellow River’s Sediment in the Interfacial Migration and Fate of Pollutants and Prospects for the Application of Environmental Sediment Restoration
by Xiaojuan Sun, Zhenzhen Yu, Qiting Zuo, Quantao Cui, Ziyu Song, Lin Gong, Shoushu Liu and Wei Zhang
Toxics 2024, 12(9), 669; https://doi.org/10.3390/toxics12090669 (registering DOI) - 14 Sep 2024
Viewed by 161
Abstract
Considering the increasing sediment content and increasing sediment flux of the Yellow River over the years, it is of significance to investigate the potential interfacial force mechanism between pollutants and Yellow River sediment. This article has reviewed the current research on the Yellow [...] Read more.
Considering the increasing sediment content and increasing sediment flux of the Yellow River over the years, it is of significance to investigate the potential interfacial force mechanism between pollutants and Yellow River sediment. This article has reviewed the current research on the Yellow River sediments’ mineral structures while investigating the potential interaction force between sediment and pollutants in the water environment. This article has conducted a comprehensive analysis of the influence of sediment on the migration of pollutants in the water environment. What is more, the authors have provided an outlook on the future applications of sediment in ecological environmental systems. Yellow River sediment mainly included minerals and some clay phases, while its irregular surface provided sites for the interface adsorption of pollutants. The interface force between the sediment and pollutants is mainly attributed to promoting bacterial growth on the surface of sediments, physisorption, and chemisorption forces. The sediments carry and transport pollutants during the long-distance water flow migration process. The sediment should be effectively utilized and better integrated into ecological or environmental restoration systems. This article provides a reference for studying the behavior of Yellow River sediment and the direction of future efficient utilization. Full article
(This article belongs to the Section Toxicity Reduction and Environmental Remediation)
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<p>(<b>a</b>) The main geological conditions along the Yellow River and the dominant mineral composition in the collected sediment samples; (<b>b</b>) SEM image of the collected suspended sediments downstream of the Yellow River [<a href="#B14-toxics-12-00669" class="html-bibr">14</a>,<a href="#B22-toxics-12-00669" class="html-bibr">22</a>]; and (<b>c</b>) XRD patterns of the collected suspended sediments downstream of the Yellow River [<a href="#B14-toxics-12-00669" class="html-bibr">14</a>,<a href="#B22-toxics-12-00669" class="html-bibr">22</a>].</p>
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<p>The potential interface interactions between the sediment and pollutants: (<b>A</b>) sediment acting in the nitrification/denitrification process. (<b>B</b>) contributions of different components of sediment to the adsorption of TC. Herein, (a) presenting adsorption capacity of different components of SS to TC; (b) K<sub>d</sub> values and (c) presenting the contributions of different mineral fractions to the overall adsorption coefficients; adsorption energies (d) SiO<sub>2</sub>, (e) Al<sub>2</sub>O<sub>3</sub>, and (f) Fe<sub>2</sub>O<sub>3</sub> for TC adsorption. (<b>C</b>) sediment interfacial reaction with heavy metal ions; (<b>D</b>) potential interfacial reaction between sediment (collected from the Lanzhou section) and CTC.</p>
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<p>The potential influence of SS on transport pathways and dispersion of pollutants: (<b>a</b>) SS with oil pollutants; (<b>b</b>) SS with trace metals; (<b>c</b>) SS with P; (<b>d</b>) SS with heavy metals.</p>
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<p>Potential application of sediment in the environmental restoration process: (<b>a</b>) sediment application in eco-concrete materials; (<b>b</b>) a mechanism diagram of sediment acting in the environmental remediation process.</p>
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14 pages, 3409 KiB  
Article
The Synergistic Effect of Calcained Coal-Series Kaolinite and Limestone on the Hydration of Portland Cement
by Jin Tang, Yue Yu, Yuanqing Bu, Bing Ma, Hao Zhou, Rong Zhou, Jiaqing Wang and Houhu Zhang
Materials 2024, 17(18), 4512; https://doi.org/10.3390/ma17184512 - 13 Sep 2024
Viewed by 274
Abstract
Limestone calcined clay cement (LC3) presents a promising alternative material due to its reduced CO2 emissions and superior mechanical properties compared to traditional Portland cement (PC). This study investigates the synergistic effect of calcined coal-series kaolinite (CCK) and limestone (LS) [...] Read more.
Limestone calcined clay cement (LC3) presents a promising alternative material due to its reduced CO2 emissions and superior mechanical properties compared to traditional Portland cement (PC). This study investigates the synergistic effect of calcined coal-series kaolinite (CCK) and limestone (LS) on the hydration behavior of cement, specifically focusing on varying mass ratios. The combination of CCK and LS promotes the formation of strätlingite and carboaluminates, which enhances early-age strength development. Additionally, the inclusion of CCK facilitates the formation of carboaluminates during later stages of hydration. After 56 days of hydration, the content of carboaluminates is over 10%wt. This stimulation of secondary hydration products significantly refines the evolution of pore structure, with the harmful large pores gradually transformed into harmless medium pores and gel pores, leading to marked improvements in compressive strength from 7 to 28 days. Replacing 45% PC with CCK and LS at mass ratio of 7 to 2, the compressive strength of blends reaches 47.2 MPa at 28 days. Overall, the synergistic interaction between CCK and LS presents unique opportunities to minimize the CO2 footprint of the cement industry without compromising early and long-term performance. Full article
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<p>XRD patterns of (<b>a</b>) clinker, (<b>b</b>) limestone, (<b>c</b>) gypsum, and (<b>d</b>) coal-series kaolinite before and after 750 °C 2 h calcination.</p>
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<p>Particle size distribution curve of raw materials.</p>
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<p>Effect of CCK and LS on the compressive strength of cement.</p>
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<p>The isothermal calorimetry curves of per gram of blends (<b>a</b>) rate of hydration and (<b>b</b>) cumulative heat of hydration.</p>
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<p>XRD patterns of blends after (<b>a</b>) 1 d, (<b>b</b>) 3 d, (<b>c</b>) 7 d, (<b>d</b>) 28 d, and (<b>e</b>) 56 d of hydration. The main peak of ettringite (E), monosulfoaluminate (Ms), hemicarboaluminate (HC), monocarboaluminate (MC), ferrite (F), portlandite (CH), strätlingite (S), and quartz (Q) were observed.</p>
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<p>The formation of (<b>a</b>) HC and (<b>b</b>) MC during cement hydration, calculated by XRD refinement measurement.</p>
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<p>The (<b>a</b>) formation of ettringite and (<b>b</b>) DoH of clinker during cement hydration, calculated by XRD refinement measurement.</p>
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<p>The thermogravimetric and different thermogravimetric resulted after hydrated (<b>a</b>) 3 d and (<b>b</b>) 28 d.</p>
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<p>The (<b>a</b>) portlandite content and (<b>b</b>) bound water content after 1, 3, 7, and 28 d of hydration.</p>
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<p>Pore size distribution of blends after (<b>a</b>) 7 d and (<b>b</b>) 28 d of hydration; porosity distribution of blends after (<b>c</b>) 7 d and (<b>d</b>) 28 d of hydration.</p>
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28 pages, 10672 KiB  
Article
Interdisciplinary Analysis and the Role of Experiments in Raw Materials and Technology Identification for Prehistoric Pottery in the Bistrița River Basin (Romania)
by Ana Drob, Neculai Bolohan, Viorica Vasilache, Bogdan-Gabriel Rățoi and Mihai Brebu
Heritage 2024, 7(9), 5120-5147; https://doi.org/10.3390/heritage7090242 - 13 Sep 2024
Viewed by 372
Abstract
The paper presents an interdisciplinary study based on an experimental model for investigating clay sources to identify prehistoric human behavior regarding resources. The study focuses on the Middle Bronze Age (1955/1773–1739/1614 cal. BC) settlement of Siliştea-Pe Cetățuie in eastern Romania, where archaeological [...] Read more.
The paper presents an interdisciplinary study based on an experimental model for investigating clay sources to identify prehistoric human behavior regarding resources. The study focuses on the Middle Bronze Age (1955/1773–1739/1614 cal. BC) settlement of Siliştea-Pe Cetățuie in eastern Romania, where archaeological materials from the Costișa and Monteoru cultures were discovered. Standard criteria for macroscopic analysis and analytical techniques, such as optical microscopy (OM), Scanning Electron Microscopy with Energy Dispersive X-ray Spectroscopy (SEM-EDX), Micro-Fourier Transform Infrared Spectroscopy (µ-FTIR), and thermal analysis (DTA and TG), were used to investigate the ceramic material from multiple points of view. The results showed that there were no significant differences between the ceramics of the two communities. Putting together the data obtained from macroscopic and physico-chemical analyses helped in partially reconstructing ancient human behaviors related to the production and use of ceramic vessels. Full article
(This article belongs to the Special Issue Recent Progress in Cultural Heritage Diagnostics)
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<p>Map showing the clay samples used in the experiment’s source areas: (<b>a</b>)—Sources S1 and S2 (clay deposit); (<b>b</b>)—Sources S3 and S4 (slope of the settlement).</p>
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<p>(<b>I</b>) The clay samples collected: (<b>a</b>) crushed; (<b>b</b>) sieved. (<b>II</b>) The test samples obtained after firing: (<b>a</b>)—450 °C; (<b>b</b>)—700 °C; (<b>c</b>)—900 °C.</p>
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<p>OM images of the Costișa ceramic fragments from Siliștea-<span class="html-italic">Pe Cetățuie</span> (50× magnification).</p>
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<p>OM images of the Monteoru ceramic fragments from Siliștea-<span class="html-italic">Pe Cetățuie</span> (50× magnification).</p>
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<p>Mineralogical section of fragment C9: Q—quartz; Mu—muscovite; Fp—plagioclase feldspar; L—limestone lithoclast; M—amorphic matrix ((<b>a</b>)—parallel nicoli; (<b>b</b>)—cross nicoli).</p>
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<p>Mineralogical section of fragment C23: Q—quartz; Qp—polycrystalline quartz; Mu—muscovite; Fp—plagioclase feldspar; Lc—sandstone lithoclast; M—amorphic matrix ((<b>a</b>)—parallel nicoli; (<b>b</b>)—cross nicoli).</p>
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<p>Mineralogical section of fragment M2: Q—quartz; Mu—muscovite ((<b>a</b>)—parallel nicoli; (<b>b</b>)—cross nicoli).</p>
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<p>Mineralogical section of fragment M15: Q—quartz; Mu—muscovite; Ah—hematite aggregates; Cc—ceramoclaste; Fp—plagioclase feldspar; Pp—primary pores ((<b>a</b>)—parallel nicoli; (<b>b</b>)—cross nicoli).</p>
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<p>SEM micrographs of the Costișa pottery clay matrix (C1–C24) from Siliștea-<span class="html-italic">Pe Cetățuie</span> (200× magnification).</p>
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<p>SEM micrographs of the Monteoru pottery clay matrix (M1–M24) from Siliștea-<span class="html-italic">Pe Cetățuie</span> (200× magnification).</p>
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<p>FTIR spectra for the Costișa pottery clay matrix from Siliștea-<span class="html-italic">Pe Cetățuie</span>.</p>
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<p>FTIR spectra for the Monteoru pottery clay matrix from Siliștea-<span class="html-italic">Pe Cetățuie</span>.</p>
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<p>OM images of the clay samples used in the experimental study: (<b>a</b>) unfired clay; (<b>b</b>) 450 °C; (<b>c</b>) 700 °C; (<b>d</b>) 900 °C (50× magnifications).</p>
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<p>Mineralogical section of sample S2: Q—quartz; Lc—limestone lithoclaste; Mu—muscovite; Fp—plagioclase feldspars; C—calcite; O—oolite; B—foraminifera <span class="html-italic">Ammonia beccarii</span>, <span class="html-italic">Porosononion subranosus</span>, and <span class="html-italic">Bulimina</span> sp. and calcareous algae ((<b>a</b>): parallel nicoli; (<b>b</b>): crossed nicoli).</p>
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<p>Mineralogical sections of sample S4: Q—quartz; Qm—monocrystalline quartz; Qp—polycrystalline quartz; Lt—possible volcanic lithoclast; Mu—muscovite; Fp—plagioclase feldspars; C—calcite; B—plant fragment ((<b>a</b>): parallel nicoli; (<b>b</b>): crossed nicoli).</p>
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<p>FTIR spectra for the clay sources: (<b>a</b>)—450 °C; (<b>b</b>)—700 °C; (<b>c</b>)—900 °C (Blue—S1; Red—S2; Green—S3; Orange—S4).</p>
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<p>DTA (<b>a</b>) and TG/DTG (<b>b</b>) curves for samples C3, M17, and source S2.</p>
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<p>DTA (<b>a</b>) and TG/DTG (<b>b</b>) curves for samples C24, M21, and source S4.</p>
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6 pages, 16630 KiB  
Brief Report
First Record of Romanechite in the Apulian Karst (Southern Italy) Resulting from the Interaction of Limestones and Clay Minerals
by Annamaria Fornelli, Francesca Micheletti, Pasquale Acquafredda and Annarosa Mangone
Minerals 2024, 14(9), 935; https://doi.org/10.3390/min14090935 - 13 Sep 2024
Viewed by 173
Abstract
A new occurrence of the Mn-Ba ore mineral, romanechite, has been discovered in a small paleo-doline of the Apulian karst on Mesozoic carbonate rock successions, characterized by reddish incrustations and nodules made essentially by Fe-bearing calcite. The conditions under which Mn-Ba ore minerals [...] Read more.
A new occurrence of the Mn-Ba ore mineral, romanechite, has been discovered in a small paleo-doline of the Apulian karst on Mesozoic carbonate rock successions, characterized by reddish incrustations and nodules made essentially by Fe-bearing calcite. The conditions under which Mn-Ba ore minerals form represent an intriguing area of research, as these minerals can act as scavengers for heavy elements, impacting soils, surface sediments, and even associated aquatic systems. The genesis of romanechite is linked to the progressive interaction of silicate aqueous solutions enriched in Al, Si, and Fe with the limestone substrate. The findings provide new insights into the genetic processes responsible for the formation of reddish Mn incrustations, supporting their polygenetic origin because of the chemical alteration of limestone and allochthonous siliciclastic muds. Full article
(This article belongs to the Section Clays and Engineered Mineral Materials)
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<p>(<b>a</b>) Location of the Murge area in the Italian territory. (<b>b</b>) The paleo-doline sampling site. (<b>c</b>) Typical field appearance of the studied karst products. (<b>d</b>) Detail of the red incrustations on limestone bedrock. (<b>e</b>) Detail of one of the studied samples (polished cutting surface: romanechite is dark in color).</p>
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<p>Representative baseline-subtracted Raman spectra acquired with a 633 nm laser—50X LWD objective, 0.3 mW. The presence of romanechite, according to [<a href="#B1-minerals-14-00935" class="html-bibr">1</a>], is highlighted by the Raman bands at 148, 202, 287, 378, 509, 586, and 628 cm<sup>−1</sup>.</p>
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<p>SEM-BSE images of luminescent and massive romanechite (Rom 2) grown on acicular, felt-like crystals (Rom 1) within pores occupied by kaolinite (Kln). Cal = calcite.</p>
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<p>SEM-BSE images and relative elemental maps of acicular romanechite (Rom 1) and globular romanechite (Rom 2) showing more luminescent rings alongside less luminescent and porous rings. Kln = kaolinite; Cal = calcite.</p>
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13 pages, 3527 KiB  
Article
The Influence of Vibration Frequency and Vibration Duration on the Mechanical Properties of Zhanjiang Formation Structural Clay
by Yanhua Xie, Bin Tang, Yansong Shi, Shuaiyu Liu, Jiankun Hu and Binghui Zhang
Appl. Sci. 2024, 14(18), 8262; https://doi.org/10.3390/app14188262 - 13 Sep 2024
Viewed by 204
Abstract
Vibration frequency and vibration duration are disturbance factors for the structural properties of clay. This study investigates how the vibration frequency and vibration duration from construction disturbances affect the mechanical properties of Zhanjiang Formation structural clay. An electric, frequency-adjustable vibration table applied varying [...] Read more.
Vibration frequency and vibration duration are disturbance factors for the structural properties of clay. This study investigates how the vibration frequency and vibration duration from construction disturbances affect the mechanical properties of Zhanjiang Formation structural clay. An electric, frequency-adjustable vibration table applied varying frequencies and durations of vibration to undisturbed soil, creating structural clay samples with different disturbance degrees. Unconfined compressive strength tests and one-dimensional consolidation compression tests were conducted on these samples to obtain disturbance degrees RDq and RDS, defined by strength loss values and compression deformation characteristics, respectively. Orthogonal experiments and grey correlation analysis were used to explore the effects of vibration frequency and vibration duration on the mechanical properties of Zhanjiang Formation structural clay. The results indicated that disturbance degrees RDq and RDS increased linearly with increase in vibration frequency and vibration duration. Range analysis was conducted using two-factor three-level orthogonal experiment of disturbance degrees, and a grey relational analysis model was established to determine the primary and secondary effects of vibration duration and vibration frequency on the mechanical properties of Zhanjiang Formation structural clay. The results demonstrated that the findings from orthogonal experiments and grey relational analysis were consistent, showing that vibration duration had a more significant impact than vibration frequency on the mechanical properties of structural clay. The conclusion suggests that vibration disturbance manifests as a “fatigue damage effect”. Continuous vibration disturbance progressively weakens the cementation bonds between soil particles due to “accumulated” energy, leading to gradual fracture and destruction. With constant vibration frequency, longer durations, or with constant duration, higher frequencies intensify the “fatigue damage effect” of vibration disturbance. Furthermore, during vibration disturbance, Zhanjiang Formation structural clay shows a more pronounced “fatigue damage effect” from vibration duration than from vibration frequency, with cementation bonds between soil particles weakening more effectively due to “accumulated” energy. The research findings enhance the understanding of how vibration frequency and vibration duration from disturbance sources impact the mechanical properties of Zhanjiang Formation structural clay, offer theoretical guidance for using construction vibration machinery, and provide a reference for preventing and controlling soil disturbance. Full article
(This article belongs to the Section Civil Engineering)
Show Figures

Figure 1

Figure 1
<p>Relationship between vibration frequency/duration and unconfined compressive strength.</p>
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<p>Compression curves of samples under different conditions: (<b>a</b>) 20 Hz; (<b>b</b>) 35 Hz; (<b>c</b>) 50 Hz; (<b>d</b>) <math display="inline"><semantics> <mrow> <mo>ln</mo> <mo stretchy="false">(</mo> <mn>1</mn> <mo>+</mo> <mi>e</mi> <mo stretchy="false">)</mo> <mo>−</mo> <mo>lg</mo> <mi>p</mi> </mrow> </semantics></math> curve.</p>
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<p>Variation in disturbance degree <math display="inline"><semantics> <mrow> <msub> <mi mathvariant="italic">RD</mi> <mi>q</mi> </msub> </mrow> </semantics></math> with vibration duration and vibration frequency: (<b>a</b>) Vibration duration; (<b>b</b>) Vibration frequency.</p>
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<p>Variation in disturbance degree <math display="inline"><semantics> <mrow> <msub> <mi mathvariant="italic">RD</mi> <mi>s</mi> </msub> </mrow> </semantics></math> with vibration duration and vibration frequency: (<b>a</b>) Vibration duration; (<b>b</b>) Vibrating frequency.</p>
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<p>Changes in microstructure before and after disturbance: (<b>a</b>) Undisturbed sample; (<b>b</b>) Disturbed sample (<math display="inline"><semantics> <mrow> <msub> <mi mathvariant="italic">RD</mi> <mi>q</mi> </msub> </mrow> </semantics></math> = 0.42 and <math display="inline"><semantics> <mrow> <msub> <mi mathvariant="italic">RD</mi> <mi>s</mi> </msub> </mrow> </semantics></math> = 33.3%).</p>
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