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Search Results (8,356)

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19 pages, 2227 KiB  
Article
Applications of the Separation of Variables Method and Duhamel’s Principle to Instantaneously Released Point-Source Solute Model in Water Environmental Flow
by Ran Gao, Juncai Gao and Linlin Chu
Sustainability 2024, 16(16), 6912; https://doi.org/10.3390/su16166912 (registering DOI) - 12 Aug 2024
Abstract
The transport–diffusion problem of point-source solutes in water environmental flows is an important issue in environmental fluid mechanics, with significant theoretical and practical implications for sustainable development and the ecological management and environmental protection of water. This study presents a model for instantaneously [...] Read more.
The transport–diffusion problem of point-source solutes in water environmental flows is an important issue in environmental fluid mechanics, with significant theoretical and practical implications for sustainable development and the ecological management and environmental protection of water. This study presents a model for instantaneously released multi-point-source solutes, utilizing the separation of variables method and Duhamel’s principle to solve classical mathematical physics equations. The zeroth-order and first-order concentration moment equations, which are crucial for predicting the cross-sectional average concentration of instantaneously released point-source solutes, are systematically addressed. The accuracy of the analytical results is confirmed by comparing them with the relevant literature. Furthermore, a general discussion is provided based on the study’s findings (including an ideal physical model of Couette flow), and an analytical solution (a recursive relationship) for higher-order concentration moments is deduced. Finally, this study quantitatively discusses downstream environmental ecological effects by examining the movement of released point-source solute centroids in the river, illustrating that the time needed for the released point-source solute to have an environmental–ecological impact downstream of the river is dependent on the initial release location. Under the specified engineering parameters, for the release location at the bottom boundary point of the channel (z0 = 0 m), the midpoint (z0 = 5 m), and the water-surface point (z0 = 10 m), the time for additional displacement of released solute centroid to reach the asymptotic value in three cases is 4.0 h, 1.0 h, and 4.5 h; the asymptotic values are approximately −0.087 km, 0.012 km, and 0.055 km, respectively. These results not only correspond with the conclusions of previous research but also provide a more extensive range of numerical results. This study establishes the groundwork for theoretical research on more complex water environmental flow models and provides a theoretical basis for engineering computations aimed at contributing to the environmental management of rivers and lakes. Full article
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<p>Model of single-point-source solute instantaneous release. The inverted triangle at the top, represents Horizontal plane, namely Reference point for height measurement; and diagonal lines at the bottom, represents the boundary of the channel.</p>
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<p>Model of multi-point-source solute instantaneous release.</p>
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<p>∆<span class="html-italic">x</span>-<span class="html-italic">t</span> curve of movement of point-source solute centroid (<span class="html-italic">z</span><sub>0</sub> = 0 m).</p>
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<p>∆<span class="html-italic">x</span>-<span class="html-italic">t</span> curve of movement of point-source solute centroid (<span class="html-italic">z</span><sub>0</sub> = 5 m).</p>
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<p>Total displacement <span class="html-italic">x</span> of the solute centroid over time <span class="html-italic">t</span> (<span class="html-italic">z</span><sub>0</sub> = 0 m).</p>
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<p>Total displacement <span class="html-italic">x</span> of the solute centroid over time <span class="html-italic">t</span> (<span class="html-italic">z</span><sub>0</sub> = 5 m).</p>
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22 pages, 9472 KiB  
Article
Cascaded-Filter-Based Reverberation Suppression Method of Short-Pulse Continuous Wave for Active Sonar
by Yonglin Cui, Shuhan Liao, Juncheng Gao, Haidong Zhu, Nengtong Zhao and An Luo
Remote Sens. 2024, 16(16), 2949; https://doi.org/10.3390/rs16162949 (registering DOI) - 12 Aug 2024
Abstract
Reverberation is the main background interference in active sonar and seriously interferes with the extraction of the target echo. Active sonar systems can use short-pulse continuous wave (CW) signals to reduce the reverberation intensity. However, as the pulse width of the CW signals [...] Read more.
Reverberation is the main background interference in active sonar and seriously interferes with the extraction of the target echo. Active sonar systems can use short-pulse continuous wave (CW) signals to reduce the reverberation intensity. However, as the pulse width of the CW signals decreases, the reverberation envelope exhibits a high-frequency oscillating phenomenon. Active sonar often uses the cell average constant false alarm ratio (CA-CFAR) method to process the reverberation, which steadily decays with transmission distance. However, the high-frequency oscillation of the reverberation envelope deteriorates the performance of CA-CFAR, which causes a higher false alarm rate. To tackle this problem, the formation mechanism of the high-frequency oscillation characteristics of the reverberation envelope of the short-pulse-width CW signals is modeled and analyzed, and on this basis, an α filter is designed to suppress the high-frequency oscillation of the reverberation envelope before applying CA-CFAR. The simulation and lake trial results indicate that this method can effectively suppress high-frequency oscillations of the reverberation envelope, as well as exhibit robustness and resistance to reverberation interference. Full article
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<p>Different reverberation backgrounds. (<b>a</b>) Steadily-decay reverberation background. (<b>b</b>) Non-steadily-decay reverberation background.</p>
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<p>The performance comparison of SO-CFAR, GO-CFAR and CA-CFAR.</p>
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<p>Flow diagram of CA-CFAR.</p>
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<p>The oscillations of the reverberation envelope of CW signals with different pulse widths.</p>
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<p>The spectrum of the reverberation envelope of 0.5 s CW.</p>
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<p>The detection performance comparison of CA-CFAR under different reverberation envelope oscillations. (<b>a</b>) Low-frequency oscillation. (<b>b</b>) High-frequency oscillation.</p>
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<p>The cell scattering model.</p>
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<p>The form of backscattered waves and the output of match filter.</p>
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<p>The flowchart of <span class="html-italic">α</span> filter.</p>
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<p>The amplitude frequency characteristic of the <span class="html-italic">α</span> filter.</p>
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<p>The logic of the cascaded reverberation suppression method.</p>
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<p>The simulated reverberation signal and its spectrum. (<b>a</b>) The reverberation signal containing the target echo. (<b>b</b>) The spectrum of the reverberation envelope.</p>
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<p>Processing results of different methods. (<b>a</b>) CA-CFAR. (<b>b</b>) SO-CFAR. (<b>c</b>) GO-CFAR. (<b>d</b>) <span class="html-italic">α</span>-CA-CFAR.</p>
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<p>Probability of target detection vs. SRR with CA-CFAR, SO-CFAR, GO-CFAR and <span class="html-italic">α</span>-CA-CFAR.</p>
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<p>False alarm rate vs. RNR with CA-CFAR, SO-CFAR, GO-CFAR and <span class="html-italic">α</span>-CA-CFAR.</p>
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<p>Schematic diagram of the distribution of the lake trial.</p>
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<p>Detection results of different methods for 0.05 s CW. (<b>a</b>) CA-CFAR. (<b>b</b>) SO-CFAR. (<b>c</b>) GO-CFAR. (<b>d</b>) <span class="html-italic">α</span>-CA-CFAR.</p>
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<p>The spectrum of the reverberation envelope at the bearing of 53°.</p>
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<p>Waveform comparison between target echo and reverberation interference.</p>
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<p>Detection results of different methods for 0.1 s CW. (<b>a</b>) CA-CFAR. (<b>b</b>) SO-CFAR. (<b>c</b>) GO-CFAR. (<b>d</b>) <span class="html-italic">α</span>-CA-CFAR.</p>
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<p>The spectrum of the reverberation envelope at the bearing of 70° when transmitting a 0.1 s CW signal.</p>
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<p>Detection results of different methods for 0.2 s CW. (<b>a</b>) CA-CFAR. (<b>b</b>) SO-CFAR. (<b>c</b>) GO-CFAR. (<b>d</b>) <span class="html-italic">α</span>-CA-CFAR.</p>
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<p>The spectrum of the reverberation envelope at the bearing of 150°.</p>
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<p>Detection results of different methods for 0.5 s CW. (<b>a</b>) CA-CFAR. (<b>b</b>) SO-CFAR. (<b>c</b>) GO-CFAR. (<b>d</b>) <span class="html-italic">α</span>-CA-CFAR.</p>
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<p>The spectrum of the reverberation envelope at the bearing of 70° when transmitting a 0.5 s CW signal.</p>
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<p>Simulated target signal and its frequency spectrum emitted by the transponder ship. (<b>a</b>) Simulated target signal. (<b>b</b>) The frequency spectrum of the simulated target signal.</p>
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<p>The reverberation envelope and its spectrum of the transmission of a 10 s, 495 Hz CW signal. (<b>a</b>) The reverberation envelope of the transmission of a 10 s, 495 Hz CW signal. (<b>b</b>) The frequency spectrum of the reverberation envelope of the transmission of a 10 s, 495 Hz CW signal.</p>
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19 pages, 3622 KiB  
Article
Predictive Functional Profiling Reveals Putative Metabolic Capacities of Bacterial Communities in Drinking Water Resources and Distribution Supply in Mega Manila, Philippines
by Arizaldo E. Castro and Marie Christine M. Obusan
Water 2024, 16(16), 2267; https://doi.org/10.3390/w16162267 (registering DOI) - 12 Aug 2024
Abstract
Assessing bacterial communities across water resources is crucial for understanding ecological dynamics and improving water quality management. This study examines the functional profiles of bacterial communities in drinking water resources in Mega Manila, Philippines, including Laguna Lake tributaries, pre-treatment plant sites, groundwater sources, [...] Read more.
Assessing bacterial communities across water resources is crucial for understanding ecological dynamics and improving water quality management. This study examines the functional profiles of bacterial communities in drinking water resources in Mega Manila, Philippines, including Laguna Lake tributaries, pre-treatment plant sites, groundwater sources, and post-treatment plant sites. Using eDNA sequencing, flux balance analysis, and taxonomy-to-phenotype mapping, we identified metabolic pathways involved in nutrient metabolism, pollutant degradation, antibio- tic synthesis, and nutrient cycling. Despite site variations, there are shared metabolic pathways, suggesting the influence of common ecological factors. Site-specific differences in pathways like ascorbate, aldarate, and phenylalanine metabolism indicate localized environmental adaptations. Antibiotic synthesis pathways, such as streptomycin and polyketide sugar unit biosynthesis, were detected across sites. Bacterial communities in raw and pre-treatment water showed potential for pollutant degradation such as for endocrine-disrupting chemicals. High levels of ammonia-oxidizing and sulfate-reducing bacteria in pre- and post-treatment water suggest active nitrogen removal and pH neutralization, indicating a need to reassess existing water treatment approaches. This study underscores the adaptability of bacterial communities to environmental factors, as well as the importance of considering their functional profiles in assessing drinking water quality resources in urban areas. Full article
(This article belongs to the Section Biodiversity and Functionality of Aquatic Ecosystems)
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<p>Seventeen (17) water sampling sites across Mega Manila, Philippines used in the current study: Laguna Lake Tributary sites (<span class="html-italic">n</span> = 5), deep well sites (<span class="html-italic">n</span> = 2), before treatment plant sites (<span class="html-italic">n</span> = 7), and after treatment plant sites (<span class="html-italic">n</span> = 3). Sampling site map was generated using ArcGIS Pro 3.3.</p>
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<p>Bacterial community taxonomic profiles across all sampling sites.</p>
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<p>Predicted functional profiles of Laguna Lake tributaries and before treatment plant sites with shotgun sequence data.</p>
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<p>(<b>a</b>) Benzoate degradation (BioCyc ID: PWY−283); (<b>b</b>) Dioxin degradation (BioCyc ID: P661−PWY); (<b>c</b>) Styrene degradation (BioCyc ID: PWY−6941); (<b>d</b>) Ammonia oxidation (BioCyc ID: PWY−7082); (<b>e</b>) Sulfate reduction (BioCyc ID: DISSULFRED−PWY). Degradation pathways are adapted from the MetaCyc metabolic pathway database [<a href="https://metacyc.org/" target="_blank">https://metacyc.org/</a>] (accessed on 1 July 2024).</p>
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<p>(<b>a</b>) Benzoate degradation (BioCyc ID: PWY−283); (<b>b</b>) Dioxin degradation (BioCyc ID: P661−PWY); (<b>c</b>) Styrene degradation (BioCyc ID: PWY−6941); (<b>d</b>) Ammonia oxidation (BioCyc ID: PWY−7082); (<b>e</b>) Sulfate reduction (BioCyc ID: DISSULFRED−PWY). Degradation pathways are adapted from the MetaCyc metabolic pathway database [<a href="https://metacyc.org/" target="_blank">https://metacyc.org/</a>] (accessed on 1 July 2024).</p>
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<p>Predicted functional profiles of Pasig River, before treatment plant sites, deep wells, and after treatment plant sites.</p>
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26 pages, 14290 KiB  
Article
Exploratory Analysis Using Deep Learning for Water-Body Segmentation of Peru’s High-Mountain Remote Sensing Images
by William Isaac Perez-Torres, Diego Armando Uman-Flores, Andres Benjamin Quispe-Quispe, Facundo Palomino-Quispe, Emili Bezerra, Quefren Leher, Thuanne Paixão and Ana Beatriz Alvarez
Sensors 2024, 24(16), 5177; https://doi.org/10.3390/s24165177 (registering DOI) - 10 Aug 2024
Viewed by 388
Abstract
High-mountain water bodies represent critical components of their ecosystems, serving as vital freshwater reservoirs, environmental regulators, and sentinels of climate change. To understand the environmental dynamics of these regions, comprehensive analyses of lakes across spatial and temporal scales are necessary. While remote sensing [...] Read more.
High-mountain water bodies represent critical components of their ecosystems, serving as vital freshwater reservoirs, environmental regulators, and sentinels of climate change. To understand the environmental dynamics of these regions, comprehensive analyses of lakes across spatial and temporal scales are necessary. While remote sensing offers a powerful tool for lake monitoring, applications in high-mountain terrain present unique challenges. The Ancash and Cuzco regions of the Peruvian Andes exemplify these challenges. These regions harbor numerous high-mountain lakes, which are crucial for fresh water supply and environmental regulation. This paper presents an exploratory examination of remote sensing techniques for lake monitoring in the Ancash and Cuzco regions of the Peruvian Andes. The study compares three deep learning models for lake segmentation: the well-established DeepWaterMapV2 and WatNet models and the adapted WaterSegDiff model, which is based on a combination of diffusion and transformation mechanisms specifically conditioned for lake segmentation. In addition, the Normalized Difference Water Index (NDWI) with Otsu thresholding is used for comparison purposes. To capture lakes across these regions, a new dataset was created with Landsat-8 multispectral imagery (bands 2–7) from 2013 to 2023. Quantitative and qualitative analyses were performed using metrics such as Mean Intersection over Union (MIoU), Pixel Accuracy (PA), and F1 Score. The results achieved indicate equivalent performance of DeepWaterMapV2 and WatNet encoder–decoder architectures, achieving adequate lake segmentation despite the challenging geographical and atmospheric conditions inherent in high-mountain environments. In the qualitative analysis, the behavior of the WaterSegDiff model was considered promising for the proposed application. Considering that WatNet is less computationally complex, with 3.4 million parameters, this architecture becomes the most pertinent to implement. Additionally, a detailed temporal analysis of Lake Singrenacocha in the Vilcanota Mountains was conducted, pointing out the more significant behavior of the WatNet model. Full article
(This article belongs to the Special Issue Application of Satellite Remote Sensing in Geospatial Monitoring)
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<p>Location of the study area.</p>
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<p>Landsat-8 scenes selected for study.</p>
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<p>Combining process from B2 to B7 into a single 6-channel image.</p>
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<p>From left to right: <math display="inline"><semantics> <mrow> <mo>(</mo> <mi>θ</mi> <mo>,</mo> <mi>ρ</mi> <mo>)</mo> </mrow> </semantics></math> parameter space, deskwed image, cropped image, and division of the image into 256 × 256 pixel patches.</p>
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<p>Mask creation process.</p>
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<p>WatNet model architecture.</p>
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<p>DeepWaterMapV2 model architecture based on 3 primary blocks.</p>
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<p>General architecture of WaterSegDiff based on a conditioning model and a diffusion model that integrate their information through two conditioning mechanisms, <math display="inline"><semantics> <mi mathvariant="script">U</mi> </semantics></math>-SA and SS-Former.</p>
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<p>SS-Former internal architecture consisting of two symmetrical cross-attention modules.</p>
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<p>Qualitative analysis of 5 selected samples that represent large lakes with compact structures. Showing the RGB image, ground truth, NDWI, WatNet, DeepWaterMapV2, and WaterSegDiff results. (<b>a</b>) Large and irregular lake, (<b>b</b>) two lakes with compact structure, (<b>c</b>) scene with river crossing, (<b>d</b>) large lake in mountainous region, (<b>e</b>) lake surrounded by dense vegetation.</p>
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<p>Qualitative analysis of 5 selected samples that represent small and dispersed lakes. Showing the RGB image, ground truth, NDWI, WatNet, DeepWaterMapV2, and WaterSegDiff results. (<b>a</b>,<b>b</b>) Snowy scene with shadows with presence of clear and turbid lakes, (<b>c</b>) completely snowy scene, (<b>d</b>,<b>e</b>) partially snowy area with scattered lakes.</p>
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<p>The edges extracted from Lake Singrenacocha based on NDWI, WatNet, DeepWaterMapV2, and WaterSegDiff. Highlights in yellow, green, blue, and red for the years 2014, 2016, 2018, and 2020, respectively.</p>
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<p>Graphical representation of the segmentation performance of Lake Singrenacocha during the years 2014, 2016, 2018, and 2020.</p>
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25 pages, 9251 KiB  
Article
Genesis of Analcite in Black Shales and Its Indication for Hydrocarbon Enrichment—A Case Study of the Permian Pingdiquan Formation in the Junggar Basin, Xinjiang, China
by Yang Bai, Xin Jiao, Yiqun Liu, Xu Li, Xu Zhang and Zhexuan Li
Minerals 2024, 14(8), 810; https://doi.org/10.3390/min14080810 (registering DOI) - 10 Aug 2024
Viewed by 283
Abstract
This study investigates the genesis of analcite in black shale from continental lakes and its implications for hydrocarbon enrichment, with a case study of the Permian Pingdiquan Formation in the Junggar Basin, Xinjiang, China. As an alkaline mineral, analcite is extensively developed in [...] Read more.
This study investigates the genesis of analcite in black shale from continental lakes and its implications for hydrocarbon enrichment, with a case study of the Permian Pingdiquan Formation in the Junggar Basin, Xinjiang, China. As an alkaline mineral, analcite is extensively developed in China’s lacustrine black shale hydrocarbon source rocks and is linked to hydrocarbon distribution. However, the mechanisms of its formation and its impact on hydrocarbon generation and accumulation remain insufficiently understood. This paper employs a multi-analytical approach, including petrological observations, geochemical analysis, and X-ray diffraction, to characterize analcite and its association with hydrocarbon source rocks. The study identifies a hydrothermal sedimentary origin for analcite, suggesting that it forms under conditions of alkaline lake water and volcanic activity, which are conducive to organic matter enrichment. The analcite content in the studied samples exhibits a significant variation, with higher contents associated with hydrocarbon accumulation zones, suggesting its role in hydrocarbon generation and accumulation. This paper reports that analcite-bearing rocks display characteristics of high-quality reservoirs, enhancing the permeability and porosity of the rock, which is essential for hydrocarbon storage and migration. In conclusion, this paper underscores the importance of analcite as a key mineral indicator for hydrocarbon potential in black shale formations and provides valuable insights for further geological and hydrocarbon exploration in similar settings. Full article
(This article belongs to the Special Issue Petrological and Geochemical Characteristics of Reservoirs)
22 pages, 12424 KiB  
Article
Monitoring and Analysis of Eco-Environmental Quality in Daihai Lake Basin from 1985 to 2022 Based on the Remote Sensing Ecological Index
by Bowen Ye, Biao Sun, Xiaohong Shi, Yunliang Zhao, Yuying Guo, Jiaqi Pang, Weize Yao, Yaxin Hu and Yunxi Zhao
Sustainability 2024, 16(16), 6854; https://doi.org/10.3390/su16166854 (registering DOI) - 9 Aug 2024
Viewed by 490
Abstract
Exploring eco-environmental quality dynamics in the Daihai Lake Basin has significant implications for the conservation of ecological environments in the semi-arid and arid regions of northern China. Based on the Google Earth Engine (GEE) platform, the remote sensing ecological index (RSEI) was constructed [...] Read more.
Exploring eco-environmental quality dynamics in the Daihai Lake Basin has significant implications for the conservation of ecological environments in the semi-arid and arid regions of northern China. Based on the Google Earth Engine (GEE) platform, the remote sensing ecological index (RSEI) was constructed by coupling Landsat SR remote sensing data from 1985 to 2022. The spatial significance of the RSEI was analyzed using linear regression equations and an F-test. The spatial correlation, distribution characteristics, and driving factors behind the RSEI were explored using Moran’s index and a geodetector. The results indicated that (1) the RSEI was appropriate for evaluating eco-environmental quality in the Daihai Lake Basin. (2) From 1985 to 2022, the eco-environmental quality of the Daihai Lake Basin exhibited a positive trend but remained subpar. (3) A positive spatial autocorrelation was demonstrated for eco-environmental quality with increasing spatial aggregation. (4) Significant eco-environmental quality degradation (slope < 0) occurred primarily in Sanyiquan Town in the northeastern region of the basin and in Tiancheng Township in the southeastern region. Conversely, a notable improvement (slope > 0) was predominantly observed in Yongxing and Liusumu in southwestern Daihai. (5) The improvement in the ecological environment of the Daihai Lake Basin was primarily attributed to an increase in NDVI and WET and a decrease in NDBSI and LST. The interaction between NDVI and LST had the greatest explanatory power for the ecological environment. Among the external driving factors, DEM (elevation) was the dominant factor in the RSEI and had the strongest explanatory power. The interaction between DEM and LST was the most significant, and the driving factors were enhanced. This study provided a theoretical basis for the sustainable development of the Daihai Lake Basin, which is crucial for the local ecological environment and economic development. Full article
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<p>Location of the study area.</p>
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<p>Flowchart.</p>
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<p>Correlation between RSEI and each index.</p>
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<p>Change curves of NDVI, WET, NDBSI, LST, and RSEI in the Daihai Lake Basin from 1985 to 2022 and mutation point test of RSEI change. (<b>a</b>) NDVI, (<b>b</b>) WET, (<b>c</b>) NDBSI, (<b>d</b>) LST, (<b>e</b>) RSEI, and (<b>f</b>) mutation point test.</p>
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<p>Spatial distribution of the RSEI index in the Daihai Lake Basin during change node years.</p>
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<p>Area and proportion of RSEI grades in the year of the change node in the Daihai Lake Basin. (<b>a</b>) Area of RSEI grades, (<b>b</b>) proportion of RSEI grades.</p>
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<p>Analysis of the dynamic change trend in the Daihai Lake Basin from 1985 to 2022. (<b>a</b>) slope, (<b>b</b>) F test.</p>
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<p>LISA clustering diagram of the RSEI index in the Daihai Lake Basin.</p>
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<p>Detection results of driving factors of the RSEI in the Daihai Lake Basin.</p>
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<p>Interactive detection results of factors influencing the RSEI in the Daihai Lake Basin from 1990 to 2015: (<b>a</b>) 1990, (<b>b</b>) 1995, (<b>c</b>) 2000, (<b>d</b>) 2005, (<b>e</b>) 2010, and (<b>f</b>) 2015.</p>
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<p>Correlation diagram of RSEI and CHEQ in the Daihai Lake Basin.</p>
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18 pages, 6145 KiB  
Article
Black Carbon in the Air of the Baikal Region, (Russia): Sources and Spatiotemporal Variations
by Tamara V. Khodzher, Elena P. Yausheva, Maxim Yu. Shikhovtsev, Galina S. Zhamsueva, Alexander S. Zayakhanov and Liudmila P. Golobokova
Appl. Sci. 2024, 14(16), 6996; https://doi.org/10.3390/app14166996 - 9 Aug 2024
Viewed by 217
Abstract
In recent years, the role of the atmosphere in the formation of the chemical composition of water in Lake Baikal and its tributaries has been increasing. In this regard, the study of equivalent black carbon (eBC) in the air above the lake and [...] Read more.
In recent years, the role of the atmosphere in the formation of the chemical composition of water in Lake Baikal and its tributaries has been increasing. In this regard, the study of equivalent black carbon (eBC) in the air above the lake and its coast has an important practical application. This paper presents the results of the mass concentration of eBC and submicron aerosol in the air above the water area of Lake Baikal, which were obtained during expeditions onboard research vessels in the summer of 2019 and 2023. We analyzed the data from the coastal monitoring station Listvyanka. To measure eBC, an MDA-02 aethalometer was used in the water area of the lake, and a BAC-10 aethalometer at the Listvyanka station. The background level of the eBC concentration in the air at different areas of the lake ranged between 0.15 and 0.3 µg m−3. The results of the two expeditions revealed the influence of the coastal settlements and the air mass transport along the valleys of the lake’s large tributaries on the five- to twentyfold growth of the eBC concentration in the near-water atmosphere. In the diurnal dynamics of eBC near settlements, we recorded high values in the evening and at night. In background areas, the diurnal dynamics were poorly manifested. In the summer of 2019, there were smoke plumes in the water area of Lake Baikal from distant wildfires and a local fire site on the east coast of the lake. The eBC concentration increased to 5–6 µg m−3, which was 10 to 40 times higher than the background. The long-range transport of plumes from coal-fired thermal power plants in large cities of the region made the major contribution to the eBC concentration at «Listvyanka» in winter, which data on aerosol, gas impurities, and meteorological parameters confirmed. Full article
(This article belongs to the Special Issue Air Pollution and Its Impact on the Atmospheric Environment)
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<p>Routes of comprehensive scientific expeditions in the water area of Lake Baikal, 2019 and 2023 (<b>a</b>); RV “Akademik V.A. Koptyug” and location of measuring equipment on the upper deck, 2019 (<b>b</b>).</p>
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<p>Location and equipment of the atmospheric monitoring station “Listvyanka”: (1) layout of the Listvyanka reference station with the largest air pollution sources at Lake Baikal; (2) station location on the hilltop; (3) the main module of the reference station; (4) MTP-5 temperature profiler; (5) Sokol-M1 meteorological complex; (6) RA-915AM spectrometer; gas analyzer; (7) Hg; gas analyzer; (8) K-100 (CO); (9) R-310A gas analyzer (NO<sub>2</sub> and NO); (10) CV-320 gas analyzer (SO<sub>2</sub>); (11) BAC-10 aethalometer analyzer eBC; (12) DUSTTRAK 8533 dust analyzer (PM<sub>10</sub>, PM<sub>2,5</sub>, and PM<sub>1.0</sub>).</p>
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<p>Spatiotemporal variability of the eBC mass concentration in the coastal zone of Lake Baikal during the 2019.</p>
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<p>Satellite image of the territory near Lake Baikal: (<b>a</b>) with wildfire sites in the north (28–29 July 2019); (<b>b</b>,<b>c</b>) backward trajectories calculated using the HYSPLIT models for 29 July 2019 (GMT) (<a href="http://fires-dv.kosmosnimki.ru" target="_blank">http://fires-dv.kosmosnimki.ru</a>, accessed on 1 June 2024).</p>
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<p>Satellite image of the central basin of Lake Baikal: (<b>a</b>) with smoke plume from a wildfire near Sosnovka Bay (red circle); (<b>b</b>) backward trajectories calculated using the HYSPLIT model for 26 July 2019 (GMT).</p>
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<p>Spatiotemporal variability of the eBC mass concentration in the coastal water area of Lake Baikal during the expedition in the summer of 2023.</p>
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<p>Diurnal variation of the eBC mass concentration under background conditions (<b>a</b>) and near populated areas. (<b>b</b>) RMSD areas are highlighted in color.</p>
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<p>Dynamics of mean monthly temperature and humidity at the Listvyanka station in 2023–2024.</p>
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<p>Mean hourly concentrations of eBC and SO<sub>2</sub> at the Listvyanka station, January 2024.</p>
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<p>Mean hourly concentrations of BC, nitrogen oxide, and sulfur dioxide (<b>a</b>) and meteorological parameters at the Listvyanka station (<b>b</b>), September 2023.</p>
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23 pages, 19594 KiB  
Article
The Identification of Historic Plant Landscape Characteristics and Conservation Strategies for Longevity Hill Based on the WSL Monoplotting Tool
by Jingyu Wu, Yao Xiao, Linjie Zhu and Sihua Cheng
Land 2024, 13(8), 1255; https://doi.org/10.3390/land13081255 - 9 Aug 2024
Viewed by 239
Abstract
The surrounding environment of architectural heritage sites is integral to cultural heritage protection; plant landscapes play crucial roles in them. Controlling plant spaces and appearances is essential for preserving plant landscapes. A World Cultural Heritage Site, the Summer Palace has undergone multiple changes [...] Read more.
The surrounding environment of architectural heritage sites is integral to cultural heritage protection; plant landscapes play crucial roles in them. Controlling plant spaces and appearances is essential for preserving plant landscapes. A World Cultural Heritage Site, the Summer Palace has undergone multiple changes since the 1860s; restoring and protecting plant landscapes has been an ongoing research focus. However, data accuracy limitations have hindered analyses of the overall spatial characteristics of historical gardens. Here, the historical dynamics and unique landscape features of plants on the front hill of Longevity Hill (FLH) are explored, and conservation and renewal strategies are proposed. Geographic information system (GIS) and WSL Monoplotting Tool are used to identify historical plant spaces. Plant space types are classified, and their landscape characteristics are analyzed. On the basis of historical events, the historical plant spaces on the FLH can be divided into two major categories and six subcategories. The vegetation retention area (south side) was less affected, and the plant landscape along Kunming Lake was the most well-preserved. However, the vegetation-damaged area (north side) was impacted more in the western part than in the eastern part, with notable changes in spatial landscape characteristics, particularly regarding forest function, morphology, and structure. Strategies are proposed for reducing human intervention and adjusting retention areas; furthermore, historical images and spatial grading in damaged areas can be used to suggest landscape adjustment and restoration strategies. This study introduces a method for analyzing the historical characteristics of plant landscapes over time that can be used to protect cultural heritage sites worldwide. Full article
(This article belongs to the Special Issue Urban Landscape Transformation vs. Heritage)
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<p>(<b>a</b>) Location of the Summer Palace; (<b>b</b>) map of the Summer Palace (courtesy of Big Map) with specific study areas indicated by the red line.</p>
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<p>Analysis of the basic architecture and structure of Longevity Hill.</p>
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<p>Locations of historical photographs (identified through field research).</p>
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<p>Schematic diagram of the WSL Monoplotting Tool.</p>
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<p>Geo-aligning and adding vectorization to photos via MPT 2.0 software.</p>
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<p>Mapping of vectorized information: (<b>a</b>) areas of altered botanical landscapes in the 1900 photographs and (<b>b</b>) areas of altered botanical landscapes in the plane mapped 1900. Red line: identification of the spatial extent of plant damage in MPT2.0 for the 1890 photograph; yellow area: the extent of the red line in the photograph that corresponds to the extent of the red line in the plane after geo-calibration.</p>
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<p>(<b>a</b>) Spatial division of the FLH planted landscapes and (<b>b</b>) the FLH partition event correspondence chart. Different colors represent the impacts of different events, as detailed in <a href="#land-13-01255-t002" class="html-table">Table 2</a>.</p>
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<p>Spatial delineation process of historical plants on the FLH.</p>
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<p>Spatial classification of plants in the FLH.</p>
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<p>Spatial classification of plants in the vegetation retention area.</p>
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<p>Spatial classification of plants in the vegetation damage area.</p>
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<p>Type I-1 planted spatial landscape conservation strategies.</p>
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<p>Type I-2 planted spatial landscape conservation strategies.</p>
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<p>Type II-2 and 4 planted spatial landscape conservation strategies.</p>
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<p>Type II-1 and 3 planted spatial landscape conservation strategies.</p>
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13 pages, 1796 KiB  
Article
Using Muscle Element Fingerprint Analysis (EFA) to Trace and Determine the Source of Hypophthalmichthys nobilis in the Yangtze River Basin
by Chao Song, Chengyao Yang, Feng Zhao, Jilin Xie, Hong Tao, Xiaorong Huang and Ping Zhuang
Fishes 2024, 9(8), 316; https://doi.org/10.3390/fishes9080316 - 9 Aug 2024
Viewed by 233
Abstract
Hypophthalmichthys nobilis are widely distributed in the Yangtze River basin and its related lakes. They are an important economic fish species and are a famous cultured species known as the “Four Famous Domestic Fishes” in China. Currently, with the fishing ban in the [...] Read more.
Hypophthalmichthys nobilis are widely distributed in the Yangtze River basin and its related lakes. They are an important economic fish species and are a famous cultured species known as the “Four Famous Domestic Fishes” in China. Currently, with the fishing ban in the Yangtze River basin, fishing for H. nobilis in the natural water bodies of the Yangtze River basin has been completely prohibited. In order to identify the sources of H. nobilis appearing in the market, further control and accountability is necessary to trace the sources of H. nobilis in the Yangtze River basin and its related water bodies. Therefore, this study identified and traced different sources of H. nobilis through muscle element fingerprint analysis (EFA). The results show that H. nobilis from different stations have characteristic element compositions. The characteristic element of H. nobilis from Wuhan (WH) is Pb, which is significantly higher than that in other stations; the characteristic element from Anqing (AQ) is Hg, which is significantly higher than that in other stations; and the characteristic element from Taihu (TH) is Al, which is significantly higher than that in other water areas. Multivariate analysis selected different spatial distribution patterns in four discriminative element ratios (Pb/Ca, Cr/Ca, Na/Ca, and Al/Ca) in the muscle of H. nobilis in the Yangtze River basin and its related lakes. This study suggests that the screened discriminative elements can be used to visually distinguish different sources of H. nobilis and to quickly trace and verify the origin of newly emerging samples. Therefore, the use of selected discriminative element fingerprint features to trace the origin of new samples has been proven to be feasible. By further discriminating and verifying the muscle element fingerprints of new samples, the discrimination rate is high. Therefore, a multivariate analysis of muscle element fingerprints can be used for tracing the origins of samples of unknown origin in market supervision. Full article
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<p><span class="html-italic">H. nobilis</span> sampling stations.</p>
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<p>Scatter diagram of PC1 and PC2 (<b>a</b>), and PC1 and PC3 (<b>b</b>), and PC2 and PC3 (<b>c</b>) of 19 element ratios in the muscles of <span class="html-italic">H. nobilis</span> from three stations in the Yangtze River basin.</p>
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<p>Element to Ca ratios of <span class="html-italic">H. nobilis</span> muscle from three stations in the Yangtze River basin (WH, AQ, and TH) and the positive control of AQ (PC-AQ). Different colors of red, blue, yellow and green represent different groups of WH, AQ, TH and PC-AQ, respectively. The horizontal line in the box is the median, and that at the ends of the vertical line segment on the upper and lower sides of the box shows the maximum and minimum, respectively. The empty box (□) represents the average value, and the solid diamond (♦) represents the extreme value. Different letters (a, b) denote significant differences between groups of samples.</p>
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<p>Scatter plot of scores based on the first two canonical discriminant functions for four groups of WH, AQ, TH, and PC-AQ.</p>
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19 pages, 7874 KiB  
Article
Mapping the Fraction of Vegetation Coverage of Potamogeton crispus L. in a Shallow Lake of Northern China Based on UAV and Satellite Data
by Junjie Chen, Quanzhou Yu, Fenghua Zhao, Huaizhen Zhang, Tianquan Liang, Hao Li, Zhentan Yu, Hongli Zhang, Ruyun Liu, Anran Xu and Shaoqiang Wang
Remote Sens. 2024, 16(16), 2917; https://doi.org/10.3390/rs16162917 - 9 Aug 2024
Viewed by 351
Abstract
Under the background of global change, the lake water environment is facing a huge threat from eutrophication. The rapid increase in curly-leaf pondweed (Potamogeton crispus L.) in recent years has seriously threatened the ecological balance and the water diversion safety of the [...] Read more.
Under the background of global change, the lake water environment is facing a huge threat from eutrophication. The rapid increase in curly-leaf pondweed (Potamogeton crispus L.) in recent years has seriously threatened the ecological balance and the water diversion safety of the eastern route of China’s South-to-North Water Diversion Project. The monitoring and control of curly-leaf pondweed is imperative in shallow lakes of northern China. Unmanned Aerial Vehicles (UAVs) have great potential for monitoring aquatic vegetation. However, merely using satellite remote sensing to detect submerged vegetation is not sufficient, and the monitoring of UAVs on aquatic vegetation is rarely systematically evaluated. In this study, taking Nansi Lake as a case, we employed Red–Green–Blue (RGB) UAV and satellite datasets to evaluate the monitoring of RGB Vegetation Indices (VIs) in pondweed and mapped the dynamic patterns of the pondweed Fractional Vegetation Coverage (FVC) in Nansi Lake. The pondweed FVC values were extracted using the RGB VIs and the machine learning method. The extraction of the UAV RGB images was evaluated by correlations, accuracy assessments and separability. The correlation between VIs and FVC was used to invert the pondweed FVC in Nansi Lake. The RGB VIs were also calculated using Gaofen-2 (GF-2) and were compared with UAV and Sentinel-2 data. Our results showed the following: (1) The RGB UAV could effectively monitor the FVC of pondweed, especially when using Support Vector Machine that (SVM) has a high ability to recognize pondweed in UAV RGB images. Two RGB VIs, RCC and RGRI, appeared best suited for monitoring aquatic plants. The correlations between four RGB VIs based on GF-2, i.e., GCC, BRI, VDVI, and RGBVI and FVCSVM calculated by the UAV (p < 0.01) were better than those obtained with other RGB VIs. Thus, the RGB VIs of GF-2 were not as effective as those of the UAV in pondweed monitoring. (2) The binomial estimation model constructed by the Normalized Difference Water Index (NDWI) of Sentinel-2 showed a high accuracy (R2 = 0.7505, RMSE = 0.169) for pondweed FVC and can be used for mapping the FVC of pondweed in Nansi Lake. (3) Combined with the Sentinel-2 time-series data, we mapped the dynamic patterns of pondweed FVC in Nansi Lake. It was determined that the flooding of pondweed in Nansi Lake has been alleviated in recent years, but the rapid increase in pondweed in part of Nansi Lake remains a challenging management issue. This study provides practical tools and methodology for the innovative remote sensing monitoring of submerged vegetation. Full article
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<p>Location of the study area with the distribution of the sample sites. (<b>a</b>) Location of the study area; (<b>b</b>) detailed location of the study area; (<b>c</b>) sample points in the study area; (<b>d</b>) sample points in Dushan Lake; (<b>e</b>) sample points in Weishan Lake.</p>
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<p>A flowchart of this study.</p>
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<p>Illustration of RGB VI separability determination.</p>
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<p>FVC box plots extracted by different methods, including SVM, the Dimidiate Pixel Model and dynamic thresholding.</p>
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<p>The correlation coefficients between the different FVC values extracted by SVM, the Dimidiate Pixel Model and dynamic thresholding.</p>
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<p>(<b>a</b>) Correlation between remote sensing VIs, FVC<sub>NDVI</sub>, FVCsvm and the mean RGB VIs, (<b>b</b>) correlation between remote sensing VIs, FVC<sub>NDVI</sub>, FVCsvm and FVC values by UAV. “*” and “**” represent significant differences, with <span class="html-italic">p</span> &lt; 0.05 and <span class="html-italic">p</span> &lt; 0.01, respectively.</p>
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<p>Correlation analysis between RGB VIs by GF-2 and the means of RGB VIs by the UAV (<b>a</b>), FVC by the UAV (<b>b</b>) and remote sensing VIs by Sentinel-2 (<b>c</b>). “*” and “**” represent significant differences, with <span class="html-italic">p</span> &lt; 0.05 and <span class="html-italic">p</span> &lt; 0.01, respectively.</p>
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<p>Accuracy assessment results for RGB VIs. (<b>a</b>) Overall accuracy, (<b>b</b>) F1 score.</p>
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<p>Statistical results of separability in the acquired images for RGB VIs.</p>
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<p>Comparison between estimated and measured pondweed FVC.</p>
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<p>Mapping pondweed FVC in Nansi Lake based on the NDWI binomial estimation model (14 May 2023).</p>
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<p>Seasonal change in pondweed FVC in Nansi Lake, 2023.</p>
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<p>Inter-annual changes in pondweed FVC in Nansi Lake, 2018–2023.</p>
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<p>Different growth periods of pondweed imaged by the RGB UAV.</p>
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21 pages, 9141 KiB  
Article
Heavy Metal Groundwater Transport Mitigation from an Ore Enrichment Plant Tailing at Kazakhstan’s Balkhash Lake
by Dauren Muratkhanov, Vladimir Mirlas, Yaakov Anker, Oxana Miroshnichenko, Vladimir Smolyar, Timur Rakhimov, Yevgeniy Sotnikov and Valentina Rakhimova
Sustainability 2024, 16(16), 6816; https://doi.org/10.3390/su16166816 - 8 Aug 2024
Viewed by 415
Abstract
Sustainable potable groundwater supply is crucial for human development and the preservation of natural habitats. The largest endorheic inland lake in Kazakhstan, Balkhash Lake, is the main water resource for the arid southeastern part of the country. Several ore enrichment plants that are [...] Read more.
Sustainable potable groundwater supply is crucial for human development and the preservation of natural habitats. The largest endorheic inland lake in Kazakhstan, Balkhash Lake, is the main water resource for the arid southeastern part of the country. Several ore enrichment plants that are located along its shore have heavy metal pollution potential. The study area is located around a plant that has an evident anthropogenic impact on the Balkhash Lake aquatic ecological system, with ten known heavy metal toxic hotspots endangering fragile habitats, including some indigenous human communities. This study assessed the risk of heavy metal contamination from tailing dump operations, storage ponds, and related facilities and suggested management practices for preventing this risk. The coastal zone risk assessment analysis used an innovative integrated groundwater numerical flow and transport model that predicted the spread of groundwater contamination from tailing dump operations under several mitigation strategies. Heavy metal pollution prevention models included a no-action scenario, a filtration barrier construction scenario, and two scenarios involving the drilling of drainage wells between the pollution sources and the lake. The scenario assessment indicates that drilling ten drainage wells down to the bedrock between the existing drainage channel and the lake is the optimal engineering solution for confining pollution. Under these conditions, pollution from tailings will not reach Lake Balkhash during the forecast period. The methods and tools used in this study to enable mining activity without environmental implications for the region can be applied to sites with similar anthropogenic influences worldwide. Full article
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<p>The study site location map and the Balkhash Industrial Area aerial photo display industrial objects included in the model’s schematization where the orange line is an interface with water bodies, the purple line is the tailing storage interface, black lines are barriers, and green lines are drains. The figure was prepared by Corel Draw with a base experimental site image taken from Google Earth.</p>
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<p>Hydrogeological cross-section along lines A–B (<a href="#sustainability-16-06816-f001" class="html-fig">Figure 1</a>). 1—upper-middle Quaternary lacustrine aquifer; 2—Pliocene aquitard of Pavlodar formations; 3—Miocene aquitard of Argyn formations; 4—Meso-Cenozoic water-bearing formations; 5—Carboniferous aquifer; 6—Paleozoic zone of fractured intrusive rocks; 7—tectonic faults; 8—groundwater level; 9—upper Quaternary technogenic aquifer, bulk soil; 10—sands with gravel inclusions; 11—crushed stones; 12—loams; 13—clays; 14—granites; 15—syenite porphyries; 16—dacite porphyries; 17—fractured rock; 18—well. Numbers: on top—well number, bottom—well depth, m; on the left in the numerator—mineralization, g/L; in the denominator—temperature, °C; on the right: in the numerator—well flow rate, L/s; in the denominator—drawdown, m. Shading corresponds to the chemical composition of groundwater in the sampled interval with the predominance of chloride and sulfate anions.</p>
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<p>The conceptual working process applied for the Balkhash Lake contamination risk assessment (<b>a</b>) and model application steps (<b>b</b>).</p>
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<p>Model calibration results.</p>
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<p>(<b>a</b>) Path lines of particles released from the source of pollution by the area tracked with MODPATH and (<b>b</b>) heavy metal spatial distribution in groundwater for ten years after contaminant release without a change in hydrogeological conditions (legend in <a href="#sustainability-16-06816-t001" class="html-table">Table 1</a>).</p>
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<p>Spatial distribution of heavy metals in groundwater from 14 drainage wells drilled between the drainage channel and Lake Balkhash (<b>a</b>) and for the scenario of drilling ten drainage wells between the drainage channel and Lake Balkhash (<b>b</b>).</p>
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<p>Spatial distribution of heavy metals in groundwater for the scenario of boundary construction between the drainage channel and Lake Balkhash.</p>
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<p>Spatial distribution of heavy metals in groundwater for the scenario of drainage wells drilled between the tailings pond drainage channel and the lake.</p>
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<p>Results of heavy metal concentration in groundwater monitoring wells over time.</p>
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<p>Sampling points on a map of heavy metal halo distribution in groundwater at the time of sampling in 2020.</p>
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<p>Calibration graph of the observed and calculated heavy metal concentrations at the sampling points.</p>
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<p>Relative sensitivity coefficients concerning different input parameters for a ±50% change in each parameter.</p>
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19 pages, 2056 KiB  
Article
Evaluation of Ecosystem Protection and Restoration Effects Based on the Mountain-River-Forest-Field-Lake-Grass Community Concept: A Case Study of the Hunjiang River Basin in Jilin Province, China
by Yu Wang and Yu Li
Water 2024, 16(16), 2239; https://doi.org/10.3390/w16162239 - 8 Aug 2024
Viewed by 480
Abstract
The protection and restoration projects of the mountain-river-forest-field-lake-grass (MRFFLG) system are the mainstream focus of China’s current ecological environment protection. A reasonable method for calculating ecosystem service values (ESVs) is a prerequisite for determining the ecological service functions of a watershed. However, how [...] Read more.
The protection and restoration projects of the mountain-river-forest-field-lake-grass (MRFFLG) system are the mainstream focus of China’s current ecological environment protection. A reasonable method for calculating ecosystem service values (ESVs) is a prerequisite for determining the ecological service functions of a watershed. However, how to effectively implement and evaluate the systematic nature of the ecological protection and restoration of the MRFFLG system remains one of the pressing issues. This paper takes the protection and restoration project of the MRFFLG system in the Hunjiang River Basin (HRB) of Jilin Province, China, as an empirical case. Firstly, it constructs an ESVs system to quantify the comprehensive ecological protection and restoration effects of the MRFFLG system. The results show that the forest ecosystem in the HRB has the highest ecological value. Furthermore, by introducing the interval planning method, an uncertain optimization model is constructed with the objective function of maximizing the ecosystem service value of the HRB, and constraints such as restoration costs, unit restoration price, and restoration area. The results show that the total ESVs has increased, with a maximum increase of 348,413.79 × 104 CNY. Finally, the introduction of the fuzzy method reduced the total interval of ESVs by 49.89%, effectively shortening the assessment interval. This study applies the interval-fuzzy method to the protection and restoration projects of the MRFFLG system, effectively measuring the comprehensive management effects of the MRFFLG system in the HRB. This paper provides a theoretical basis for the development of subsequent MRFFLG projects and offers theoretical references for promoting the ecological environment assessment of the comprehensive MRFFLG system. Full article
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<p>Geographical location of study area.</p>
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<p>Research roadmap for ES value accounting.</p>
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<p>The percentage of ESVs for the three ecosystems.</p>
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<p>Optimization of ecosystem restoration area in Hunjiang River (ha).</p>
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<p>Total ESVs of the HRB based on the interval programming and interval-fuzzy programming models.</p>
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19 pages, 1692 KiB  
Review
Sources, Transport, and Accumulation of Synthetic Microfiber Wastes in Aquatic and Terrestrial Environments
by Kundan Samal, Satya Ranjan Samal, Saurabh Mishra and Jagdeep Kumar Nayak
Water 2024, 16(16), 2238; https://doi.org/10.3390/w16162238 - 8 Aug 2024
Viewed by 735
Abstract
The global proliferation of synthetic microfiber waste has emerged as a pressing environmental concern due to its widespread distribution in both aquatic and terrestrial ecosystems. Primary sources of synthetic microfibers include laundering of synthetic textiles, manufacturing, and plastic breakdown, with transport via wastewater, [...] Read more.
The global proliferation of synthetic microfiber waste has emerged as a pressing environmental concern due to its widespread distribution in both aquatic and terrestrial ecosystems. Primary sources of synthetic microfibers include laundering of synthetic textiles, manufacturing, and plastic breakdown, with transport via wastewater, runoff, atmospheric deposition, and animal ingestion. This review highlights the sources of microfiber formation and accumulation, ranging from freshwater lakes and rivers to deep-sea sediments. The presence of microfibers in agricultural soils, urban dust, and even remote locations indicates atmospheric transportation and diverse accumulation patterns. Additionally, this review discusses the transportation of microfibers through various pathways and elaborates on various treatment technologies for microfiber removal and reduction. The potential human health impacts and mitigation solutions are also highlighted. Overall, this review aims to provide comprehensive knowledge of the sources, transport mechanisms, and accumulation patterns of synthetic microfibers, emphasizing their multifaceted environmental impact and the need for further research to develop effective solutions. Full article
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<p>An indicative scheme of microfibers’ sources.</p>
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<p>Timeframe for degradation of various plastic products (<a href="https://scdhec.gov" target="_blank">https://scdhec.gov</a> (accessed on 22 July 2024)).</p>
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<p>Schematic of the sources, generation, transportation, and accumulation of microplastics [<a href="#B55-water-16-02238" class="html-bibr">55</a>].</p>
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<p>Health impacts of microfibers in humans.</p>
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22 pages, 3742 KiB  
Article
LAQUA: a LAndsat water QUality retrieval tool for east African lakes
by Aidan Byrne, Davide Lomeo, Winnie Owoko, Christopher Mulanda Aura, Kobingi Nyakeya, Cyprian Odoli, James Mugo, Conland Barongo, Julius Kiplagat, Naftaly Mwirigi, Sean Avery, Michael A. Chadwick, Ken Norris, Emma J. Tebbs and on behalf of the NSF-IRES Lake Victoria Research Consortium
Remote Sens. 2024, 16(16), 2903; https://doi.org/10.3390/rs16162903 - 8 Aug 2024
Viewed by 549
Abstract
East African lakes support the food and water security of millions of people. Yet, a lack of continuous long-term water quality data for these waterbodies impedes their sustainable management. While satellite-based water quality retrieval methods have been developed for lakes globally, African lakes [...] Read more.
East African lakes support the food and water security of millions of people. Yet, a lack of continuous long-term water quality data for these waterbodies impedes their sustainable management. While satellite-based water quality retrieval methods have been developed for lakes globally, African lakes are typically underrepresented in training data, limiting the applicability of existing methods to the region. Hence, this study aimed to (1) assess the accuracy of existing and newly developed water quality band algorithms for East African lakes and (2) make satellite-derived water quality information easily accessible through a Google Earth Engine application (app), named LAndsat water QUality retrieval tool for east African lakes (LAQUA). We collated a dataset of existing and newly collected in situ surface water quality samples from seven lakes to develop and test Landsat water quality retrieval models. Twenty-one published algorithms were evaluated and compared with newly developed linear and quadratic regression models, to determine the most suitable Landsat band algorithms for chlorophyll-a, total suspended solids (TSS), and Secchi disk depth (SDD) for East African lakes. The three-band algorithm, parameterised using data for East African lakes, proved the most suitable for chlorophyll-a retrieval (R2 = 0.717, p < 0.001, RMSE = 22.917 μg/L), a novel index developed in this study, the Modified Suspended Matter Index (MSMI), was the most accurate for TSS retrieval (R2 = 0.822, p < 0.001, RMSE = 9.006 mg/L), and an existing global model was the most accurate for SDD estimation (R2 = 0.933, p < 0.001, RMSE = 0.073 m). The LAQUA app we developed provides easy access to the best performing retrieval models, facilitating the use of water quality information for management and evidence-informed policy making for East African lakes. Full article
(This article belongs to the Special Issue Remote Sensing Band Ratios for the Assessment of Water Quality)
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<p>Overview of the methodology used for data collection, model assessment, and application development. Detailed app development steps are provided in <a href="#sec2dot6-remotesensing-16-02903" class="html-sec">Section 2.6</a>. TOA means top-of-atmosphere.</p>
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<p>(<b>A</b>) The seven study lakes with <span class="html-italic">in situ</span> water quality data used for model development: 1 is Ziway, Ethiopia; 2 is Chamo, Ethiopia; 3 is Turkana, Kenya/Ethiopia; 4 is Baringo, Kenya; 5 is Bogoria, Kenya; 6 is Oloidien, Kenya; 7 is Victoria, Kenya/Uganda/Tanzania. (<b>B</b>) The data collection transects for Lake Baringo, Kenya, in September 2023. Diamonds indicate data collected on 18 September and triangles indicate data collected on 19 September. (<b>C</b>) The region in which <span class="html-italic">in situ</span> data were collected for Lake Victoria in this study. (<b>D</b>) The data collection transects in Winam Gulf, in the Kenyan region of Lake Victoria, on 13 September 2023. Diamonds indicate individual sampling points along each transect.</p>
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<p>Flow diagram of the Google Earth Engine app development steps, image preprocessing methods, and model application.</p>
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<p>(<b>A</b>) Models for the best predictive band algorithms for chlorophyll-<span class="html-italic">a</span> and total suspended solids (TSS). There is no plot for Secchi disk depth (SDD) as the best performing model utilises the existing Song <span class="html-italic">et al.</span> (2022) equation. Grey bars indicate 95% confidence intervals. Data points from each study lake are distinguished by colour and marker shape and are summarized in the lake key. (<b>B</b>) Predicted vs. observed values for the best performing models for chlorophyll-<span class="html-italic">a</span>, TSS, and SDD. The black lines represent the linear relationship, and the grey bars are the 95% confidence intervals. Dashed lines indicate a perfect match with a slope of 1 and intercept of 0.</p>
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<p>The best performing retrieval models applied to a Landsat 9 image from September 2023 for (<b>A</b>) Lake Baringo—a turbid freshwater lake in Kenya, and (<b>B</b>) Lake Bogoria—a highly productive alkaline–saline lake approximately 20 km south of Baringo.</p>
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12 pages, 1759 KiB  
Article
Zooplankton Assemblages of an Argentinean Saline Lake during Three Contrasting Hydroperiods and a Comparison with Hatching Experiments
by Santiago Andrés Echaniz, Alicia María Vignatti and Gabriela Cecilia Cabrera
Limnol. Rev. 2024, 24(3), 301-312; https://doi.org/10.3390/limnolrev24030018 - 8 Aug 2024
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Abstract
Many saline lakes are temporary, with large variations in salinity, and their biota is adapted to withstand unfavorable periods. Utracan Lake, in a protected area in central Argentina, was studied on three occasions under different environmental conditions. In 2007, depth and salinity were [...] Read more.
Many saline lakes are temporary, with large variations in salinity, and their biota is adapted to withstand unfavorable periods. Utracan Lake, in a protected area in central Argentina, was studied on three occasions under different environmental conditions. In 2007, depth and salinity were 2 m and 33 g/L, and six species were recorded in the zooplankton. In 2009–2010, its maximum depth was 0.3 m, its salinity exceeded 230 g/L, and only Artemia persimilis was recorded. Field studies to compare the active zooplankton of a third period were combined with laboratory tests to ascertain the composition of the egg bank (flotation with sucrose) and zooplankton succession (hatching from sediments). In 2017–2018 (third period), the depth and salinity were 1.75 ± 0.17 m and 47.19 ± 11.40 g/L, respectively. Five species were recorded, and A. persimilis was found coexisting with cladocerans, copepods, and rotifers. Brachionus plicatilis, Hexarthra fennica, Boeckella poopoensis, A. persimilis, and a single specimen of Moina eugeniae were recorded in hatching experiments; however, the latter species was not recorded again. No cladoceran ephippia were recorded in the flotation tests. Salt accumulation on the sediments during the Utracan drought (2010–2016) would have deteriorated the ephippia. The register of M. eugeniae in 2017–2018 could be largely because of recolonization by waterfowl. The conservation of Utracan Lake is therefore advisable, and the same goes for other nearby saline lakes, which can act as sources of propagules that cross terrestrial areas through transport by wind or zoochory. Full article
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Figure 1
<p>Geographic location of Utracan Lake.</p>
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<p>Average annual rainfall between 1921 and 2023 in the region where Utracan Lake is located, determined in General Acha City. Solid line: annual average. Dashed line: time trend.</p>
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<p>Variation in dissolved oxygen concentration and pH (<b>A</b>) and salinity (<b>B</b>) throughout the hatching bioassays from the sediment of Utracan Lake.</p>
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<p>Species that hatched from the egg bank of the sediment of Utracan Lake and the periods during which they were recorded in the hatching bioassays.</p>
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<p>Variation in the average density of the three typical species of the mesosaline periods registered throughout the hatching bioassays from the sediment of Utracan Lake. <span class="html-italic">Boeckella poopoensis</span> includes copepodites and adults.</p>
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