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26 pages, 7916 KiB  
Article
Machine Learning-Based Framework to Predict the Combined Effects of Climate Change and Floating Photovoltaic Systems Installation on Water Quality of Open-Water Lakes
by Nagavinothini Ravichandran and Balamurugan Paneerselvam
Sustainability 2025, 17(4), 1696; https://doi.org/10.3390/su17041696 - 18 Feb 2025
Abstract
Floating photovoltaic (FPV) systems represent a promising advancement in renewable energy technology; however, a comprehensive understanding of their environmental impacts is essential. The effects of FPV installation on lake water temperature remain unclear, potentially hindering the development of the technology due to associated [...] Read more.
Floating photovoltaic (FPV) systems represent a promising advancement in renewable energy technology; however, a comprehensive understanding of their environmental impacts is essential. The effects of FPV installation on lake water temperature remain unclear, potentially hindering the development of the technology due to associated negative implications for aquatic ecosystems. Furthermore, the rise in water temperature associated with climate change poses additional threats to open-water bodies. In this context, the current study endeavors to develop a machine learning (ML)-based framework to assess the combined impact of climate change and the installation of FPV systems on the water quality of open-water lakes. This framework involves the creation of three predictive models and a forecasting model utilizing various ML algorithms, concentrating on temperature and water quality predictions. The framework was applied to a case study assessing the impact of installing three distinct FPV systems on the water quality of Oostvoornse Lake in the Netherlands, employing water quality data available in the literature. The findings indicate a temporal increase in both air and water temperatures at the site, underscoring the ramifications of climate change. Additionally, the results suggest that FPV installations can influence lake thermal dynamics, leading to variations in water temperature and dissolved oxygen concentration, which presents both opportunities and challenges in addressing the impacts of climate change. The proposed framework will be an effective tool for evaluating the effects of FPV systems on water quality throughout their operational lifespan while addressing significant climate change issues. Full article
(This article belongs to the Special Issue Impacts of Climate Change on the Water–Food–Energy Nexus)
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<p>Machine learning-based framework for prediction of water quality affected by FPV systems and climate change.</p>
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<p>Steps involved in data procurement and preprocessing.</p>
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<p>Prediction and forecasting models used in the present study.</p>
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<p>Combined impact analysis from the developed ML models.</p>
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<p>Location of Oostvoornse Lake and the FPV pilot project.</p>
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<p>Schematic top view of the FPV systems at Oostvoornse Lake: (<b>a</b>) FPV 1, (<b>b</b>) FPV 2, and (<b>c</b>) FPV 3.</p>
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<p>Actual and predicted values of response variables from the best model: (<b>a</b>) FPV system water temperature model, (<b>b</b>) dissolved oxygen model, (<b>c</b>) air–water temperature model, and (<b>d</b>) temperature forecasting model.</p>
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<p>Forecasted air temperature for the lifespan of FPV systems.</p>
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<p>Comparison of monthly mean air temperature of reference period with the 10-year mean air temperature at different time periods: (<b>a</b>) 2023–2032, (<b>b</b>) 2033–2042, and (<b>c</b>) 2043–2052.</p>
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<p>Comparison of monthly mean air temperature of reference period with the 10-year mean air temperature at different time periods: (<b>a</b>) 2023–2032, (<b>b</b>) 2033–2042, and (<b>c</b>) 2043–2052.</p>
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<p>Comparison of predicted air and water temperature for the different time periods: (<b>a</b>) maximum temperature and (<b>b</b>) minimum temperature.</p>
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<p>Comparison of predicted air and water temperature for the different time periods: (<b>a</b>) maximum temperature and (<b>b</b>) minimum temperature.</p>
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<p>Comparison of water temperature in open-water and FPV-covered regions for different FPV systems: (<b>a</b>) maximum temperature and (<b>b</b>) minimum temperature.</p>
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<p>Comparison of DO concentration in open-water and FPV-covered locations under different time periods during (<b>a</b>) summer and (<b>b</b>) winter seasons.</p>
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13 pages, 1829 KiB  
Article
Identifying AMF-Rich Tir Wheat Rhizospheres to Foster Microbial Inoculants Useful in Sustainable Agriculture: Evidence from the Van Lake Basin
by Solmaz Najafi, Mehmet Ülker, Younes Rezaee Danesh, Semra Demir, Erol Oral, Fevzi Altuner, Siyami Karaca, Meriç Balci, Burak Özdemir, Bulut Sargin, Aynur Dilsiz, Çağlar Sagun, Ezelhan Selem, Sana Jamal Salih, Mina Najafi, Beatrice Farda and Marika Pellegrini
Sustainability 2025, 17(4), 1676; https://doi.org/10.3390/su17041676 - 18 Feb 2025
Viewed by 1
Abstract
Arbuscular mycorrhizal fungi (AMF) play a pivotal role in sustainable agriculture by enhancing nutrient efficiency and reducing the dependence on synthetic fertilizers. Developing these sustainable, effective products requires knowledge of the target plant and its associated microbial communities in the production landscape of [...] Read more.
Arbuscular mycorrhizal fungi (AMF) play a pivotal role in sustainable agriculture by enhancing nutrient efficiency and reducing the dependence on synthetic fertilizers. Developing these sustainable, effective products requires knowledge of the target plant and its associated microbial communities in the production landscape of interest. This study focused on AMF populations associated with Tir wheat in six main locations of Türkiye’s Van Lake Basin. The Erçek-Özalp-Saray region exhibited the highest organic matter values. Higher available phosphorous contents were found for Erciş-Patnos and Muradiye. The Erciş-Patnos region exhibited the highest AMF density (120 spores/10 g soil) and frequency (75%), while the lowest AMF density (45 spores/10 g soil) was recorded in Muradiye. Sand contents correlated positively with spore number and mycorrhizal frequency and negatively with silt and clay. Based on these results, Erciş-Patnos was elected as the best location for the isolation of AMF spores suitable for the development of microbial-based tools for Tir wheat cultivation. These results are very important in the current context of climate change, which mandates the use of low-impact environmental strategies. Further research should explore the interactions of AMFs with other microorganisms to optimize their ecological benefits. However, the results of this study provide a valuable basis for future investigations of AMF-based products for use in sustainable Tir wheat cultivation. Full article
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<p>Results of soil physicochemical parameters (i.e., electrical conductivity, organic matter, available phosphorous, calcium carbonate contents, and USDA (United States Department of Agriculture) soil texture classification) organized based on the six sampling locations: Bitlis-Ahlat, Erciş-Patnos, Erçek-Özalp-Saray, Muradiye, Muş, and Van-Gevaş. For organic matter and phosphorous, results followed by different case letters are significantly different according to the Conover–Iman test (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>AMF parameters (spore number, mycorrhizal frequency, and mycorrhizal density) determined in soil samples collected from different locations. Means followed by the same case letter (a–c) are not significantly different according to the Conover–Iman test (α = 0.05).</p>
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<p>Correlations among physicochemical and AMF soil parameters.</p>
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<p>Linear regression plots showing relationships between soil texture components (sand, silt, and clay) and AMF parameters. Significant differences were recorded for all correlations investigated (<span class="html-italic">p</span> &lt; 0.05). Coefficients of determination (R<sup>2</sup>) and <span class="html-italic">p</span>-values: SN vs. sand (R<sup>2</sup> = 0.074, <span class="html-italic">p</span> = 0.003), SN vs. silt (R<sup>2</sup> = 0.089, <span class="html-italic">p</span> = 0.001), SN vs. clay (R<sup>2</sup> = 0.036, <span class="html-italic">p</span> = 0.043), F% vs. sand (R<sup>2</sup> = 0.105, <span class="html-italic">p</span> = 0.0004), F% vs. silt (R<sup>2</sup> = 0.124, <span class="html-italic">p</span> = 0.0001) (spore number—SN, mycorrhizal frequency—F%).</p>
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20 pages, 4133 KiB  
Article
The Influence of Juniper on the Soil Properties of Pine Stands in the Taiga Zone of the European North
by Maria Vladimirovna Medvedeva and Boris Vladimirovich Raevsky
Forests 2025, 16(2), 365; https://doi.org/10.3390/f16020365 - 17 Feb 2025
Viewed by 200
Abstract
This study was performed on the territory of Northern Europe in the Middle taiga subzone of Karelia. The work was conducted at two test sites (Site I, Site II) located in a pine forest in the coastal area of Lake Segozero. In these [...] Read more.
This study was performed on the territory of Northern Europe in the Middle taiga subzone of Karelia. The work was conducted at two test sites (Site I, Site II) located in a pine forest in the coastal area of Lake Segozero. In these territories, areas under juniper (UCB) and under lingonberry-blueberry plant microgroups (CB) were isolated. This article presents the results of the effect of juniper on the properties of the upper soil horizon, forest litter (O), and mineral podzolic horizon (E (UCB)). The forest floor (O), and the mineral podzolic horizon (E) of soils located under the lingonberry-blueberry plant microgroup (CB) were selected as controls. The volume weight; acidity; content of total C, total N, total K, and total P had differences in different horizons (O, E) of the soils at the studied sites (Site I, Site II; CB, UCB). The results showed a tendency for C and N reserves to increase in the upper soil horizon under juniper. K and P reserves in this soil horizon tended to decrease. An increase in catalase activity was found in soils under juniper (Site I, II—UCB), which indicates a change in redox conditions. An increase in the rate of cellulose decomposition was noted in UCB sites compared with CB, which is consistent with the results of other studies. Mathematical and statistical analysis confirmed the formation of vegetative microgroups (CB and UCB) in cranberry pine (Site I, Site II) and also allowed us to identify conjugate pairs of chemical parameters (nitrogen reserves, C, catalase activity, and cellulose-destroying ability of soils) that differ in these sites. Full article
(This article belongs to the Special Issue Carbon, Nitrogen, and Phosphorus Storage and Cycling in Forest Soil)
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<p>The location of the studied sites in the Middle taiga subzone of Karelia (Site I and Site II).</p>
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<p>The layout of the plants (<span class="html-italic">Juniperus communis</span>) in the area (Site I, Site II) (<b>A</b>) and the place of soil selection for analysis (<b>B</b>).</p>
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<p>Stock of organic carbon and elements of the mineral nutrition of plants in soils under juniper in northern Karelia at various sites: Site I and Site II. The vertical line represents the mean ± standard error of the measurements.</p>
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<p>Stock of organic carbon and elements of the mineral nutrition of plants in soils under juniper in northern Karelia at various sites: Site I and Site II. The vertical line represents the mean ± standard error of the measurements.</p>
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<p>The activity of catalase (mL O<sub>2</sub>/g soil/5 min) and relative changes (RCh) of activity the catalase in soil under juniper in northern Karelia at Site I and Site II: cowberry-bilberry microgroup of plants (CB), juniper- cowberry-bilberry microgroup of plants (UCB). The vertical line represents the mean ± standard error of the measurements.</p>
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<p>Cellulolytic activity (% of cellulose decomposition) of O and E horizons of soils under various plant microgroups (cowberry-bilberry microgroup of plants (CB), juniper-cowberry-bilberry microgroup of plants (UCB) in northern Karelia at Site I and Site II. The data above the bars represent the mean ± standard error of the measurements.</p>
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<p>Principal component analysis of the ten properties of soils (pH, total C (TC), total N (TN), total K (TK), total P (TP), H, katalase (Kat)); soil depth interval (SDI) formed in two sites (Site I, Site II) under cowberry-bilberry microgroup of plants (CB) and juniper-cowberry-bilberry microgroup of plants (UCB). Red symbols correspond to the CB, blue—UCB, respectively, Site I and Site II.</p>
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<p>Dendrogram analysis of some parameters (pH, total C (TC), total N (TN), total K (TK), total P (TP), hydrolytic acidity (H), katalase (Kat), stock of O layer (StO), soil depth interval (SDI), KME (coefficient of moisture expansion) of soils under juniper in northern Karelia at Site I and Site II: cowberry-bilberry microgroup of plants (CB) and juniper-cowberry-bilberry microgroup of plants (UCB) at various sites.</p>
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21 pages, 24193 KiB  
Article
How Hydrological Extremes Affect the Chlorophyll-a Concentration in Inland Water in Jiujiang City, China: Evidence from Satellite Remote Sensing
by Wei Jiang, Xiaohui Ding, Fanping Kong, Gan Luo, Tengfei Long, Zhiguo Pang, Shiai Cui, Jie Liu and Elhadi Adam
ISPRS Int. J. Geo-Inf. 2025, 14(2), 85; https://doi.org/10.3390/ijgi14020085 - 15 Feb 2025
Viewed by 218
Abstract
From 2020 to 2022, hydrological extremes such as severe floods and droughts occurred successively in Jiujiang city, Poyang Lake Basin, posing a threat to regional water quality safety. The chlorophyll-a (Chl-a) concentration is a key indicator of river eutrophication. Until now, there has [...] Read more.
From 2020 to 2022, hydrological extremes such as severe floods and droughts occurred successively in Jiujiang city, Poyang Lake Basin, posing a threat to regional water quality safety. The chlorophyll-a (Chl-a) concentration is a key indicator of river eutrophication. Until now, there has been a lack of empirical research exploring the Chl-a trend in inland water in Jiujiang in the context of hydrological extremes. In this study, Sentinel-2 satellite remote sensing data sourced from the Google Earth Engine (GEE) cloud platform, along with hourly water quality data collected from monitoring stations in Jiujiang city, Jiangxi Province, China, are utilized to develop a quantitative inversion model for the Chl-a concentration. The Chl-a concentrations for various inland water types were estimated for each quarter from 2020 to 2022, and the spatiotemporal distribution was analyzed. The main findings are as follows: (1) the quantitative inversion model for the Chl-a concentration was validated via in situ measurements, with a coefficient of determination of 0.563; (2) the spatial estimates of the Chl-a concentration revealed a slight increasing trend, increasing by 0.1193 μg/L from 2020 to 2022, closely aligning with the monitoring-station data; (3) an extreme drought in 2022 led to less water in inland water bodies, and consequently, the Chl-a concentration displayed a significant upward trend, especially in Poyang Lake, where the mean Chl-a concentration increased by approximately 1 μg/L from Q1 to Q2 in 2022. These findings revealed the seasonal changes in the Chl-a concentrations in inland waters in the context of extreme hydrological events, thus providing valuable information for the sustainable management of water quality in Jiujiang city. Full article
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<p>Map of the study area showing the distribution of water quality monitoring stations.</p>
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<p>Overall flowchart of this study.</p>
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<p>The values of the correlation coefficients between bands/band combinations and the measured Chl-a concentration.</p>
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<p>Scatter plot fitting results for the Chl-a concentration.</p>
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<p>Spatial distribution maps of the Chl-a concentration. (<b>a</b>), (<b>b</b>), and (<b>c</b>) are the four quarters (Q1, Q2, Q3, and Q4) of the Chl-a concentration inversion results in 2020, 2021 and 2022, respectively.</p>
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<p>Spatial distribution maps of the Chl-a concentration. (<b>a</b>), (<b>b</b>), and (<b>c</b>) are the four quarters (Q1, Q2, Q3, and Q4) of the Chl-a concentration inversion results in 2020, 2021 and 2022, respectively.</p>
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<p>Spatial distribution of the Chl-a concentration in Poyang Lake in the four quarters (Q1, Q2, Q3, and Q4) of 2020, 2021, and 2022.</p>
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<p>The measured mean Chl-a concentrations and error intervals at the monitoring stations in Poyang Lake.</p>
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<p>(<b>A</b>) Quarterly changes from 2020 to 2023, and (<b>B</b>) four quarterly average changes in the Chl-a concentration in each lake.</p>
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<p>The spatial distribution of the Chl-a concentration in Saicheng Lake in four quarters (Q1, Q2, Q3, and Q4) from 2020 to 2022.</p>
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<p>The quarterly spatial distribution of the Chl-a concentration in Zhelin Reservoir (four quarters: Q1, Q2, Q3, and Q4) from 2020 to 2022.</p>
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<p>The spatial distribution changes of the Chl-a concentration in aquaculture ponds over four different quarters (Q1, Q2, Q3, and Q4) of 2020, 2021, and 2022.</p>
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<p>Abnormally high Chl-a concentrations upstream of the Xiu River in Q4 of 2020 (<b>a</b>) and Q1 of 2021 (<b>b</b>).</p>
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28 pages, 12804 KiB  
Article
Comparing the Effects of Erosion and Accretion Along the Coast of Pontchartrain Lake and New Orleans in the United States of America
by Silvia V. González Rodríguez, Vicente Negro Valdecantos, José María del Campo and Vanessa Torrodero Numpaque
Sustainability 2025, 17(4), 1578; https://doi.org/10.3390/su17041578 - 14 Feb 2025
Viewed by 312
Abstract
This research examines the transformation of the Lake Pontchartrain coastal landscape, including the New Orleans shoreline. The paper addresses the critical need to understand long-term environmental change through a comprehensive geospatial analysis of historical cartographic representations. The study employs a methodology involving three [...] Read more.
This research examines the transformation of the Lake Pontchartrain coastal landscape, including the New Orleans shoreline. The paper addresses the critical need to understand long-term environmental change through a comprehensive geospatial analysis of historical cartographic representations. The study employs a methodology involving three key steps: (1) georeferencing maps using QGis v. 3.4.8., (2) vectorization using AutoCAD v. 2013, and (3) comparative spatial analysis to quantify coastal morphological changes. The quantitative results reveal significant coastal dynamics, with Lake Pontchartrain experiencing a total erosion balance of −36.42 km2, although the New Orleans coastal zone has experienced land reclamation. This loss can be attributed to the synergistic interaction of natural (e.g., subsidence, sea level rise, hurricanes) and anthropogenic (e.g., urban development, infrastructure, ecological fragmentation) processes that have accelerated coastal erosion in the study area. The research provides a critical historical analysis of the evolution of coastal landscapes in response to anthropogenic influences. However, the methodology is constrained when it comes to addressing the socioeconomic impacts. Nevertheless, the study considered the profound environmental and societal consequences of historical governmental and social decisions, thereby underscoring the intricate interplay between natural processes and human intervention in coastal ecosystems. These findings contribute to a more profound comprehension of the processes of coastal landscape transformation, underscoring the dynamic and fragile nature of coastal environments. Full article
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<p>Georeferenced location (plane coordinates) of the Pontchartrain Lake in Louisiana, USA. USA is located in North America at the bottom right (geographic coordinates). Use coordinate system WGS84, Datum NAD83.</p>
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<p>Design elevations of the flood protection system across the New Orleans region. Source: [<a href="#B19-sustainability-17-01578" class="html-bibr">19</a>].</p>
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<p>South Lake Pontchartrain Causeway Toll Plaza, Metairie. Source: Historic American Engineering Survey photo via Library of Congress website at <a href="https://www.loc.gov/resource/hhh.la0640.photos/?sp=2&amp;st=image" target="_blank">https://www.loc.gov/resource/hhh.la0640.photos/?sp=2&amp;st=image</a> (accessed on 17 August 2024).</p>
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<p>North Lake Pontchartrain Causeway Terminus, Mandeville. Source: <a href="https://www.youtube.com/watch?v=Lm0ZyeCEoOM" target="_blank">https://www.youtube.com/watch?v=Lm0ZyeCEoOM</a> (accessed on 17 August 2024).</p>
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<p>Sketch H showing the progress of the survey in Section No. 8 1846–1852. Source: United States Coast Survey. Wikimedia Commons. Available online: <a href="https://w.wiki/BFVC" target="_blank">https://w.wiki/BFVC</a>. (accessed on 11 October 2023)</p>
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<p>2023 aerial photographs. (<b>A</b>) 10 aerial image captures (framed) that correspond to the study area analyzed in this work sites (framed) that correspond with the important places analyzed in this paper. (<b>B</b>) Enlarged representation (part of Irish Bayou) to allow visual verification of the cartographic reliability of the analyzed coast. Source: own elaboration, taken from Google Earth.</p>
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<p>Coastline superimposition of the vectorized cartographic plans of 1853 and 2023. Source: own elaboration.</p>
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<p>This detail from a map of New Orleans and the surrounding area, dated 1925, is courtesy of the Library of Congress for [<a href="#B39-sustainability-17-01578" class="html-bibr">39</a>]. It shows the Lakefront project accretion area. Source: <a href="https://www.raremaps.com/gallery/detail/73429/map-of-the-city-of-new-orleans-and-vicinity-july-1925-guillot-adam" target="_blank">https://www.raremaps.com/gallery/detail/73429/map-of-the-city-of-new-orleans-and-vicinity-july-1925-guillot-adam</a>, (accessed on 14 August 2024).</p>
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<p>Accretion map for the Lakefront project. Green line corresponds to the 2023 coastline, and Roman numerals indicate the name of the study zone. Source: Own elaboration.</p>
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<p>Current location of Fort St. John and distance to the mouth of the canal in Lake Pontchartrain. Source: Google Maps 2023.</p>
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<p>Erosion and accretion in zones VIII–XII. Source: Own elaboration on aerial image of Google Maps 2023.</p>
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<p>Accretion in the XIV Mandeville zone. Source: Own elaboration of aerial image from Google Maps 2023.</p>
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<p>Erosion in zone XV St. Tammany Refuge. Source: Own elaboration of aerial image from Google Maps 2023.</p>
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<p>Accretion in the zone XVI Big Branch Marsh National Wildlife Refuge. Source: Own elaboration on aerial image of Google Maps 2023.</p>
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<p>Erosion and accretion in the XVII Irish Bayou zone. Source: Own elaboration of aerial image from Google Maps 2023.</p>
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<p>Massive land loss projected over the next 50 years according to CPRA, 2017. Source: [<a href="#B51-sustainability-17-01578" class="html-bibr">51</a>].</p>
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<p>The coastal morphology of Lake Pontchartrain and New Orleans. Source: [<a href="#B49-sustainability-17-01578" class="html-bibr">49</a>].</p>
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<p>Coastal land surface changes in terms of erosion and accretion. Source: [<a href="#B30-sustainability-17-01578" class="html-bibr">30</a>].</p>
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<p>Persistent land loss and land gain on the Lake Pontchartrain shoreline, as defined by the Coastal Wetlands Planning, Protection, and Restoration Act Program (n.d.), 1932–2010. Source: [<a href="#B30-sustainability-17-01578" class="html-bibr">30</a>].</p>
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27 pages, 8424 KiB  
Article
Research on the Algorithm of Lake Surface Height Inversion in Qinghai Lake Based on Sentinel-3A Altimeter
by Chuntao Chen, Xiaoqing Li, Jianhua Zhu, Hailong Peng, Youhua Xue, Wanlin Zhai, Mingsen Lin, Yufei Zhang, Jiajia Liu and Yili Zhao
Remote Sens. 2025, 17(4), 647; https://doi.org/10.3390/rs17040647 - 14 Feb 2025
Viewed by 244
Abstract
Lakes are a crucial component of inland water bodies, and changes in their water levels serve as key indicators of global climate change. Traditional methods of lake water level monitoring rely heavily on hydrological stations, but there are problems such as regional representativeness, [...] Read more.
Lakes are a crucial component of inland water bodies, and changes in their water levels serve as key indicators of global climate change. Traditional methods of lake water level monitoring rely heavily on hydrological stations, but there are problems such as regional representativeness, data stability, and high maintenance costs. The satellite altimeter is an essential tool in lake research, with the Synthetic Aperture Radar (SAR) altimeter offering a high spatial resolution. This enables precise and quantitative observations of lake water levels on a large scale. In this study, we used Sentinel-3A SAR Radar Altimeter (SRAL) data to establish a more reasonable lake height inversion algorithm for satellite-derived lake heights. Subsequently, using this technology, a systematic analysis study was conducted with Qinghai Lake as the case study area. By employing regional filtering, threshold filtering, and altimeter range filtering techniques, we obtained effective satellite altimeter height measurements of the lake surface height. To enhance the accuracy of the data, we combined these measurements with GPS buoy-based geoid data from Qinghai Lake, normalizing lake surface height data from different periods and locations to a fixed reference point. A dataset based on SAR altimeter data was then constructed to track lake surface height changes in Qinghai Lake. Using data from the Sentinel-3A altimeter’s 067 pass over Qinghai Lake, which has spanned 96 cycles since its launch in 2016, we analyzed over seven years of lake surface height variations. The results show that the lake surface height exhibits distinct seasonal patterns, peaking in September and October and reaching its lowest levels in April and May. From 2016 to 2023, Qinghai Lake showed a general upward trend, with an increase of 2.41 m in lake surface height, corresponding to a rate of 30.0 cm per year. Specifically, from 2016 to 2020, the lake surface height rose at a rate of 47.2 cm per year, while from 2020 to 2022, the height remained relatively stable. Full article
(This article belongs to the Special Issue Remote Sensing in Monitoring Coastal and Inland Waters)
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<p>Schematic of the Qinghai Lake experimental site in 2019 (the green circle with * indicate tide gauge installation points; and the red triangle denote GPS reference station locations).</p>
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<p>Establishment of GPS reference station.</p>
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<p>Diagram of the installation of the tide gauge on the centering rod in an erect position (the red circle is level bubble, which indicates the centralization of the centering rod).</p>
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<p>Deployment strategy for the GPS buoy.</p>
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<p>Water level data measured by the pressure tide gauge installed in the air.</p>
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<p>Tide gauge measurement of water level changes in Qinghai Lake on 15 July 2019.</p>
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<p>Schematic diagram of the method for measuring lake surface height with a pressure-type tide gauge.</p>
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<p>Results of the first comparative test between the tide gauge and GPS buoy.</p>
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<p>Results of the second comparative test between the tide gauge and GPS buoy.</p>
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<p>Variation in lake water level during geoid measurement on 15 July 2019.</p>
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<p>Variation in lake water level during geoid measurement in July 2019.</p>
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<p>Distribution of Qinghai Lake water surface height derived from Sentinel-3A 067 pass with latitude.</p>
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<p>Variations in lake surface height of Qinghai Lake derived from Sentinel-3A 067 pass after regional screening.</p>
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<p>Variations in lake surface height of Qinghai Lake derived from Sentinel-3A after regional and threshold filtering.</p>
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<p>Time series of lake surface height derived from Sentinel-3A SRAL after regional and threshold filtering.</p>
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<p>Single-pass standard deviation (StD) statistics of lake surface heights derived from Sentinel-3A SRAL after regional and threshold filtering.</p>
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<p>Comparative plot of the time series of lake surface heights and the standard deviation (StD) of lake surface height in the same pass.</p>
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<p>Time series of lake surface height derived from the improved and effective satellite altimeter extraction method for Qinghai Lake.</p>
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<p>The normalized average lake surface height of Qinghai Lake obtained after normalization. (<b>a</b>) The rising trend of Qinghai Lake water level; (<b>b</b>) The distribution of residuals.</p>
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<p>Distribution of annual average lake surface height changes of Qinghai Lake.</p>
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16 pages, 3161 KiB  
Article
Eutrophication Conditions in Two High Mountain Lakes: The Influence of Climate Conditions and Environmental Pollution
by Fátima Goretti García-Miranda, Claudia Muro, Yolanda Alvarado, José Luis Expósito-Castillo and Héctor Víctor Cabadas-Báez
Hydrology 2025, 12(2), 32; https://doi.org/10.3390/hydrology12020032 - 13 Feb 2025
Viewed by 289
Abstract
The lakes known as El Sol and La Luna are high mountain water deposits located in Mexico within an inactive volcanic system. These lakes are of ecological importance because they are unique in Mexico. However, currently, the lakes have experienced changes in their [...] Read more.
The lakes known as El Sol and La Luna are high mountain water deposits located in Mexico within an inactive volcanic system. These lakes are of ecological importance because they are unique in Mexico. However, currently, the lakes have experienced changes in their shape and an increase in algae blooms, coupled with the degradation of the basin, which has alerted government entities to the need to address the lakes’ problems. To address the environmental status of El Sol and La Luna, a trophic study was conducted during the period of 2021–2023, including an analysis of the influence of climatic variables, lake water quality, and eutrophication conditions. The trophic state was established based on the eutrophication index. The Pearson correlations defined the eutrophication interrelation between the distinct factors influencing the lakes’ status. El Sol registered higher eutrophication conditions than La Luna. El Sol was identified as seasonal eutrophic and La Luna as transitioning from oligotrophic to mesotrophic, showing high levels of chlorophyll, total phosphorus, and total nitrogen and low water transparency. The principal factors altering the eutrophic conditions were water pollution and climatic variables (precipitation and ambient temperature). Eutrophication was the prime factor impacting perimeter loss at El Sol, whereas at La Luna, it was due to a decline in precipitation. Full article
(This article belongs to the Topic Advances in Hydrological Remote Sensing)
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<p>(<b>a</b>) Flora and Fauna Protection Area of the Nevado de Toluca (black line), volcano, and the core site of Lakes El Sol and La Luna (red line). (<b>b</b>) The volcano’s location within Mexico. (<b>c</b>) Lakes El Sol and La Luna in the volcano (blue area).</p>
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<p>Sampling sites for water from Lakes El Sol and La Luna (delimited by red dash lines, corresponding to the current lakes’ perimeters).</p>
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<p>Climatic parameters in the crater area of Lakes El Sol and La Luna (2009–2023).</p>
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<p>(<b>a</b>) Hydrological basin shape (red circles) and lake perimeters based on data from the previous decade of 2011–2020. (<b>b</b>) Hydrological basin shape (red circles) and lake perimeters based on data from 2021 to 2023. The yellow line in Lake El Sol and the green line in Lake La Luna indicate the change in their size and hydrology at different times, showing the loss of the water column. (<b>c</b>) Lake perimeter data (km) between 2009 and 2023.</p>
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<p>Historical changes in the quality parameters of lake water. Past decades and the 2021–2023 period. (<b>a</b>) pH, (<b>b</b>) water temperature, (<b>c</b>) total nitrogen, (<b>d</b>) total phosphorus, (<b>e</b>) chlorophyll-a, and (<b>f</b>) Secchi disk.</p>
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<p>(<b>a</b>) Distribution of impacted sites in Lakes El Sol and La Luna by Chl-a. (<b>b</b>) Image of Lake El Sol water showing high levels of algae proliferation.</p>
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27 pages, 10948 KiB  
Article
The Role of Atmospheric Circulation Patterns in Water Storage of the World’s Largest High-Altitude Landslide-Dammed Lake
by Xuefeng Deng, Yizhen Li, Jingjing Zhang, Lingxin Kong, Jilili Abuduwaili, Majid Gulayozov, Anvar Kodirov and Long Ma
Atmosphere 2025, 16(2), 209; https://doi.org/10.3390/atmos16020209 - 12 Feb 2025
Viewed by 276
Abstract
This study reconstructed the annual lake surface area (LSA) and absolute lake water storage (LWS) changes of Lake Sarez, the world’s largest high-altitude landslide-dammed lake, from 1992 to 2023 using multi-source remote sensing data. All available Landsat images were used to extract the [...] Read more.
This study reconstructed the annual lake surface area (LSA) and absolute lake water storage (LWS) changes of Lake Sarez, the world’s largest high-altitude landslide-dammed lake, from 1992 to 2023 using multi-source remote sensing data. All available Landsat images were used to extract the LSA using an improved multi-index threshold method, which incorporates a slope mask and threshold adjustment to enhance the boundary delineation accuracy (Kappa coefficient = 0.94). By combining the LSA with high-resolution DEM and the GLOBathy bathymetry dataset, the absolute LWS was reconstructed, fluctuating between 12.3 × 109 and 12.8 × 109 m3. A water balance analysis revealed that inflow runoff (IRO) was the primary driver of LWS changes, contributing 54.57%. The cross-wavelet transform and wavelet coherence analyses showed that the precipitation (PRE) and snow water equivalent (SWE) were key climatic factors that directly influenced the variability of IRO, impacting the interannual water availability in the lake, with PRE having a more sustained impact. Temperature indirectly regulated IRO by affecting SWE and potential evapotranspiration. Furthermore, IRO exhibited different resonance periods and time lags with various atmospheric circulation factors, with the Pacific Decadal Oscillation and North Atlantic Oscillation having the most significant influence on its interannual variations. These findings provide crucial insights into the hydrological behavior of Lake Sarez under climate change and offer a novel approach for studying water storage dynamics in high-altitude landslide-dammed lakes, thereby supporting regional water resource management and ecological conservation. Full article
(This article belongs to the Section Meteorology)
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<p>Geographical location of Lake Sarez on the Pamir Plateau (<b>a</b>) and overview of the lake-river system (<b>b</b>).</p>
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<p>Number of Landsat image observations in the Lake Sarez region: (<b>a</b>) annual observation counts from 1992 to 2023; and (<b>b</b>) total monthly observation counts from 1992 to 2023.</p>
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<p>Flowchart showing the study methodology framework and procedures.</p>
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<p>Conceptual diagram illustrating the multi-index threshold method.</p>
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<p>Time series of the extracted LSA and observed annual maximum lake level in Lake Sarez.</p>
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<p>Estimation model of absolute LWS changes based on bathymetry data and AW3D-5m DEM.</p>
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<p>(<b>a</b>) Elevation–storage curve of Lake Sarez and (<b>b</b>) area–storage curve of Lake Sarez.</p>
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<p>Time series of LSA and absolute LWS changes in Lake Sarez from 1992 to 2023.</p>
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<p>Time series plot of variations in IRO and absolute LWS.</p>
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<p>Interannual variations in IRO and basin climate factors in Lake Sarez from 1992 to 2023.</p>
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<p>XWT (<b>a</b>–<b>d</b>) and WTC (<b>e</b>–<b>h</b>) analysis of IRO and basin climate factors in Lake Sarez (The thin arc line in the figure is the wavelet effect cone curve, the black thick line is the boundary of the 95% confidence threshold, the arrow indicates the relative phase difference, → indicates in-phase variation, ← indicates anti-phase variation).</p>
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<p>XWT (<b>a</b>–<b>d</b>) and WTC (<b>e</b>–<b>h</b>) between IRO and atmospheric circulation factors in Lake Sarez (The thin arc line in the figure is the wavelet effect cone curve, the black thick line is the boundary of the 95% confidence threshold, the arrow indicates the relative phase difference, → indicates in-phase variation, ← indicates anti-phase variation).</p>
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25 pages, 12059 KiB  
Article
Albufera Lagoon Ecological State Study Through the Temporal Analysis Tools Developed with PerúSAT-1 Satellite
by Bárbara Alvado, Luis Saldarriaga, Xavier Sòria-Perpinyà, Juan Miguel Soria, Jorge Vicent, Antonio Ruíz-Verdú, Clara García-Martínez, Eduardo Vicente and Jesus Delegido
Sensors 2025, 25(4), 1103; https://doi.org/10.3390/s25041103 - 12 Feb 2025
Viewed by 378
Abstract
The Albufera of Valencia (Spain) is a representative case of pressure on water quality, which caused the hypertrophic state of the lake to completely change the ecosystem that once featured crystal clear waters. PerúSAT-1 is the first Peruvian remote sensing satellite developed for [...] Read more.
The Albufera of Valencia (Spain) is a representative case of pressure on water quality, which caused the hypertrophic state of the lake to completely change the ecosystem that once featured crystal clear waters. PerúSAT-1 is the first Peruvian remote sensing satellite developed for natural disaster monitoring. Its high spatial resolution makes it an ideal sensor for capturing highly detailed products, which are useful for a variety of applications. The ability to change its acquisition geometry allows for an increase in revisit time. The main objective of this study is to assess the potential of PerúSAT-1′s multispectral images to develop multi-parameter algorithms to evaluate the ecological state of the Albufera lagoon. During five field campaigns, samples were taken, and measurements of ecological indicators (chlorophyll-a, Secchi disk depth, total suspended matter, and its organic-inorganic fraction) were made. All possible combinations of two bands were obtained and subsequently correlated with the biophysical variables by fitting a linear regression between the field data and the band combinations. The equations for estimating all the water variables result in the following R2 values: 0.76 for chlorophyll-a (NRMSE: 16%), 0.75 for Secchi disk depth (NRMSE: 15%), 0.84 for total suspended matter (NRMSE: 11%), 0.76 for the inorganic fraction (NRMSE: 15%), and 0.87 for the organic fraction (NRMSE: 9%). Finally, the equations were applied to the Albufera lagoon images to obtain thematic maps for all variables. Full article
(This article belongs to the Special Issue Application of Satellite Remote Sensing in Geospatial Monitoring)
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<p>Study area location <span class="html-italic">L’Albufera de València</span>. Green dots are the sampling points.</p>
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<p>PerúSAT-1 images over the Albufera lagoon. Image TOA (<b>a</b>), without atmospheric correction, and image BOA (<b>b</b>), with atmospheric correction.</p>
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<p>Validation of atmospheric correction data.</p>
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<p>Boxplot of the values range for the water quality parameters. The box bounds the interquartile range (IQR: 25–75 percentile), the horizontal line inside the box indicates the median, and the error bars indicate the 90th above and 10th below percentiles. Dots indicate the outliers.</p>
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<p>Chl-<span class="html-italic">a</span> in situ as a function of ND (B4 − B1)/(B4 + B1).</p>
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<p>SDD in situ as a function of ND (B4 − B1)/(B4 + B1).</p>
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<p>TSM in situ as a function of SR (B1/B4).</p>
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<p>PIM in situ as a function of ND (B3/B1).</p>
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<p>POM in situ as a function of SR (B3/B4).</p>
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<p>Estimation maps of Chl-<span class="html-italic">a</span> (μg/L). From left to right and up to down: winter, spring, summer, and autumn.</p>
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<p>Estimation maps of SDD (m). From left to right and up to down: winter, spring, summer, and autumn.</p>
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<p>Estimation maps of TSM (mg/L). From left to right and up to down: winter, spring, summer, and autumn.</p>
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<p>Estimation maps of PIM (mg/L). From left to right and up to down: winter, spring, summer, and autumn.</p>
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<p>Estimation maps of POM (mg/L). From left to right and up to down: winter, spring, summer, and autumn.</p>
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<p>10 m pixel (<b>left</b>) of S2 image vs. 2.8 m pixel (<b>right</b>) of PerúSAT-1 image.</p>
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<p>Subset of “Obera ditch” area for PerúSAT-1 product (<b>top</b>) and S2 product (<b>bottom</b>).</p>
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<p>Estimation maps of Chl-<span class="html-italic">a</span>. Acquisition data: 20 April 2023. Left: S2 image; right: PerúSAT-1 image.</p>
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<p>Estimation maps of SDD. Acquisition data: 20 April 2023. Left: S2 image; right: PerúSAT-1 image.</p>
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<p>Estimation maps of TSM. Acquisition data: 20 April 2023. Left: S2 image; right: PerúSAT-1 image.</p>
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<p>Estimation maps of PIM. Acquisition data: 20 April 2023. Left: S2 image; right: PerúSAT-1 image.</p>
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<p>Estimation maps of POM. Acquisition data: 20 April 2023. Left: S2 image; right: PerúSAT-1 image.</p>
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<p>Subset of “Obera ditch” area for PerúSAT-1 Chl-<span class="html-italic">a</span> product (<b>top</b>) and S2 Chl-<span class="html-italic">a</span> product (<b>bottom</b>).</p>
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22 pages, 5447 KiB  
Article
Indicators of Climate-Driven Change in Long-Term Zooplankton Composition: Insights from Lake Maggiore (Italy)
by Rossana Caroni, Roberta Piscia and Marina Manca
Water 2025, 17(4), 511; https://doi.org/10.3390/w17040511 - 11 Feb 2025
Viewed by 500
Abstract
Freshwater zooplankton are a key component of lake food webs and a responsive indicator of changes occurring in an ecosystem’s structure and functioning. A new challenge under climate change is to disentangle the effects of lake warming from changes in lake trophic conditions, [...] Read more.
Freshwater zooplankton are a key component of lake food webs and a responsive indicator of changes occurring in an ecosystem’s structure and functioning. A new challenge under climate change is to disentangle the effects of lake warming from changes in lake trophic conditions, and ultimately to relate them to changes in zooplankton and ecosystem functioning. In this study, we examined the zooplankton community of the large deep subalpine Lake Maggiore (Italy) over a period of four decades, spanning changes in both lake trophic conditions and climate warming. Using monthly data from the upper 50 m of water depth, we analyzed long-term trends and investigated the application of zooplankton biomass-based indices in order to provide a better understanding of the changes in the lake ecosystem over time. Examining annual and seasonal patterns of different zooplankton taxa and groups, we observed over time a decreased contribution of Daphnia sp. during the summer and a concurrent increase in microzooplankton, suggesting a change in phytoplankton control in the lake during the recent period. Our study demonstrates that zooplankton communities integrate environmental changes, and underlines the importance of long-term monitoring and the inclusion of seasonality and the entire size range of zooplankton as key components to allow the interpretation of lake ecosystem functioning in response to trophic and climatic changes. Full article
(This article belongs to the Section Biodiversity and Functionality of Aquatic Ecosystems)
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<p>Chlorophyll-<span class="html-italic">a</span> concentration (mg/m<sup>3</sup>) in the upper 20 m depth of Lake Maggiore during the investigated time period (1981–2019). (<b>Top graph</b>): time series of monthly data. A blue smoothed LOWESS trend line has been fit to the data. (<b>Bottom graph</b>): Theil–Sen trend; significance is reported (* = 0.05, ** = 0.01, *** = 0.001).</p>
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<p>Time series of total zooplankton (<b>top graph</b>) and <span class="html-italic">Daphnia</span> (<b>bottom graph</b>) biomass (mg dry weight/m<sup>3</sup>) during the investigated time period (1981–2019). Open circles and lines refer to monthly data, blue lines to LOWESS smoothed values.</p>
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<p>Time series 1981–2019 of rotifers (<b>top graph</b>) and nauplii (<b>bottom graph</b>) biomass (mg dry weight/m<sup>3</sup>). The open circle lines refer to monthly data, blue lines to LOWESS smoothed values. A gap in 1993–1994 is because samples were not collected for the small zooplankton fraction.</p>
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<p>Theil–Sen trend analysis for the studied period (1981–2019) of microzooplankton biomass (mg dry weight/m<sup>3</sup>) in Lake Maggiore. Red solid lines indicate Theil–Sen trends, and dotted red lines the 95% confidence. The slope of annual change and the statistical significance (* = 0.05, ** = 0.01, *** = 0.001) are reported.</p>
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<p>Time series of the ratio of total zooplankton biomass to chlorophyll-<span class="html-italic">a</span> concentration in Lake Maggiore. The line with open circles refers to monthly data, and the blue line to LOWESS smoothed values.</p>
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<p>Seasonal (Theil–Sen) trends for <span class="html-italic">Daphnia</span> biomass (<b>upper graph</b>) microzooplankton (nauplii and monogonont rotifers) (<b>lower graph</b>) biomass in Lake Maggiore. Red solid lines indicate Theil–Sen trends, and dotted red lines the 95% confidence intervals. For each season, ratios of annual change and statistical significance (* = 0.05, ** = 0.01, *** = 0.001) are reported. Time period: 1981–2019.</p>
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<p>Seasonal (Theil–Sen) trends for the ratio of total zooplankton biomass to [Chl-<span class="html-italic">a</span>] in Lake Maggiore. Red solid lines indicate Theil–Sen trends, and dotted red lines the 95% confidence intervals. For each season, ratios of annual change and statistical significance (* = 0.05, ** = 0.01, *** = 0.001) are reported. Time period: 1981–2019.</p>
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<p>Summer values (mean of June–July–August) of the ratio of total zooplankton biomass to [Chl-<span class="html-italic">a</span>] (<b>top graph</b>), ratio of <span class="html-italic">Daphnia</span> biomass to [Chl-<span class="html-italic">a</span>] (<b>second graph</b>) and ratio of microzooplankton biomass to [Chl-<span class="html-italic">a</span>] (<b>bottom graph</b>). Blue line represents LOWESS smoothed estimate.</p>
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<p>Ridge plot by month of <span class="html-italic">Daphnia</span> (in blue) and microzooplankton (MIC in green) biomass (mg dry weight/m<sup>3</sup>) in Lake Maggiore during the studied period (1981–2019).</p>
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16 pages, 2375 KiB  
Article
Response of Community Characteristics and Assembly Mechanisms of cbbL-Carrier Carbon-Fixing Microorganisms to Precipitation Changes in Alpine Lakeshore Wetland
by Ni Zhang, Siyu Wang, Shijia Zhou, Desheng Qi, Jing Ma and Kelong Chen
Agriculture 2025, 15(4), 379; https://doi.org/10.3390/agriculture15040379 - 11 Feb 2025
Viewed by 296
Abstract
Precipitation change strongly influences soil microbial communities, and precipitation patterns have become a key factor affecting carbon and nitrogen cycling processes in wetland ecosystems. The cbbL gene is a key gene in the fixation of carbon dioxide during the Calvin cycle. However, the [...] Read more.
Precipitation change strongly influences soil microbial communities, and precipitation patterns have become a key factor affecting carbon and nitrogen cycling processes in wetland ecosystems. The cbbL gene is a key gene in the fixation of carbon dioxide during the Calvin cycle. However, the response of cbbL-carrier carbon-fixing microorganisms in the lakeshore wetland to precipitation change remains unclear. To this end, we established 25% and 50% increased and decreased precipitation treatments, along with a natural control, and used high-throughput sequencing to investigate the response of the cbbL-carrier carbon-fixing microbial community in a lakeshore wetland of Qinghai Lake in response to precipitation change. The results showed that a 25% reduced precipitation treatment significantly increased the relative abundance of Chlorophyta and Bradyrhizobium. pH was found to be the most important factor influencing the carbon-fixing microbial community, with a significant positive correlation with Ferrithrix. A 25% increased precipitation treatment significantly increased the relative abundance of aerobic chemoheterotrophy and chemoheterotrophy, while a 25% reduced precipitation treatment significantly increased the relative abundance of nitrogen fixation. The increased precipitation and 50% reduced precipitation treatments shift the community assembly process of cbbL-carrier carbon-fixing microorganisms from randomness to determinism. Co-occurrence network analysis showed that the network complexity and connectivity between species of cbbL-carrier carbon-fixing microorganisms initially decreased and then increased with increasing precipitation. In summary, precipitation change tended to reduce the carbon sequestration potential of the lakeshore wetland, while a 25% reduced precipitation treatment favored the nitrogen fixation process in these wetlands. Full article
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<p>Physicochemical properties of soil in lakeshore wetlands under precipitation changes. Letters ‘abc’ indicate significance; identical letters denote no significant difference (<span class="html-italic">p</span> &gt; 0.05), while different letters indicate significant differences (<span class="html-italic">p</span> &lt; 0.05). Tem: soil temperature; Hum: soil humidity; TN: total nitrogen; TC: total carbon; pH: soil pH.</p>
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<p>Diversity characteristics of cbbL-carrier carbon-fixing microbial communities in lakeshore wetland under precipitation changes. (<b>a</b>) Alpha diversity indices; (<b>b</b>) PCA (Principal Component Analysis); (<b>c</b>) grouping validity verification. * indicates <span class="html-italic">p</span> &lt; 0.05.</p>
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<p>Composition of cbbL-carrier carbon-fixing microbial communities in lakeshore wetland under precipitation changes. (<b>a</b>) Dominant phyla; (<b>b</b>) dominant genera; (<b>c</b>) differential phyla; (<b>d</b>) differential genera; (<b>e</b>) ASV distribution across groups. Letters ‘ab’ indicate significance; identical letters denote no significant difference (<span class="html-italic">p</span> &gt; 0.05), while different letters indicate significant differences (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>cbbL-carrier microbial functional groups under precipitation change in lakeshore wetland. (<b>a</b>) Top 10 major functional groups; (<b>b</b>) differential functional groups between treatments; (<b>c</b>) microbial taxa corresponding to differential functional groups. Letters ‘ab’ indicate significance; identical letters denote no significant difference (<span class="html-italic">p</span> &gt; 0.05), while different letters indicate significant differences (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>Correlation analysis between cbbL-carrier carbon-fixing microorganisms and environmental factors in lakeshore wetland. (<b>a</b>) Redundancy analysis of dominant genera and physicochemical factors; (<b>b</b>) correlation heatmap of dominant genera and physicochemical factors; (<b>c</b>) hierarchical partitioning analysis of factors influencing microbial community structure; (<b>d</b>) hierarchical partitioning analysis of factors influencing diversity of denitrifying microbial communities. * indicates <span class="html-italic">p</span> &lt; 0.05. Tem: soil temperature; Hum: soil humidity; TN: total nitrogen; TC: total carbon; pH: soil pH.</p>
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<p>Community assembly of cbbL-carrier carbon-fixing microorganisms in lakeshore wetland. (<b>a</b>) Distribution of βNTI index; (<b>b</b>) distribution of carbon-fixing microbial community assembly processes.</p>
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<p>The network patterns of the cbbL-carrier carbon-fixing microorganisms under precipitation changes in the lakeshore wetland. The size of the nodes represents their degree; the node colors indicate different modules; the edge colors represent positive or negative correlations, with red indicating positive correlations and green indicating negative correlations.</p>
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21 pages, 4875 KiB  
Article
Late 20th Century Hypereutrophication of Northern Alberta’s Utikuma Lake
by Carling R. Walsh, Fabian Grey, R. Timothy Patterson, Maxim Ralchenko, Calder W. Patterson, Eduard G. Reinhardt, Dennis Grey, Henry Grey and Dwayne Thunder
Environments 2025, 12(2), 63; https://doi.org/10.3390/environments12020063 - 11 Feb 2025
Viewed by 325
Abstract
Eutrophication in Canadian lakes degrades water quality, disrupts ecosystems, and poses health risks due to potential development of harmful algal blooms. It also economically impacts the general public, industries like recreational and commercial fishing, and tourism. Analysis of a 140-year core record from [...] Read more.
Eutrophication in Canadian lakes degrades water quality, disrupts ecosystems, and poses health risks due to potential development of harmful algal blooms. It also economically impacts the general public, industries like recreational and commercial fishing, and tourism. Analysis of a 140-year core record from Utikuma Lake, northern Alberta, revealed the processes behind the lake’s current hypereutrophic conditions. End-member modeling analysis (EMMA) of the sediment grain size data identified catchment runoff linked to specific sedimentological processes. ITRAX X-ray fluorescence (XRF) elements/ratios were analyzed to assess changes in precipitation, weathering, and catchment runoff and to document changes in lake productivity over time. Five end members (EMs) were identified and linked to five distinct erosional and sedimentary processes, including moderate and severe precipitation events, warm and cool spring freshet, and anthropogenic catchment disturbances. Cluster analysis of EMMA and XRF data identified five distinct depositional periods from the late 19th century to the present, distinguished by characteristic rates of productivity, rainfall, weathering, and runoff linked to natural and anthropogenic drivers. The most significant transition in the record occurred in 1996, marked by an abrupt increase in both biological productivity and catchment runoff, leading to the hypereutrophic conditions that persist to the present. This limnological shift was primarily triggered by a sudden discharge from a decommissioned sewage treatment lagoon into the lake. Spectral and wavelet analysis confirmed the influence of the Arctic Oscillation, El Niño Southern Oscillation, North Atlantic Oscillation, and Pacific Decadal Oscillation on runoff processes in Utikuma Lake’s catchment. Full article
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<p>Map showing Utikuma Lake, its location within Canada (star, upper right inset), as well as the location of the community of Atikameg (Whitefish Lake First Nation #459) on the western shore. The coring site is indicated by a red star, at which four closely spaced gravity cores were collected. Location and core details are presented in <a href="#environments-12-00063-t001" class="html-table">Table 1</a>. Bathymetric contours are given in meters.</p>
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<p>Photographs showing (<b>A</b>) collection of a UWITEC gravity core from Utikuma Lake as the bottom of the core is capped upon recovery, (<b>B</b>) a UWITEC core barrel filled with a core mounted on a custom-built portable extruder that can be deployed in the field and which can produce 1 mm resolution subsamples, and (<b>C</b>) a 1 mm resolution subsample being transferred from the extruder into a sample bag for subsequent analysis.</p>
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<p><sup>210</sup>Pb age model (black) and standard deviation (grey) for Utikuma Lake, with an average sedimentation rate of 1.5 mm/yr.</p>
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<p>Utikuma Lake Core BU1 grain size frequency distributions for the 200 subsamples (gray plots), as well as the distribution of five robust end members (EMs) derived from the model that best explains the sediment grain size distributions.</p>
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<p>Down core EMMA and normalized ITRAX elemental profiles for Utikuma Lake in core BU1, plotted against depth and estimated age. The CONISS cluster dendrogram (right) indicates five zones, the boundaries of which are marked by horizontal red lines.</p>
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<p>Spectral and wavelet time series analysis results of the normalized ITRAX elemental profiles for Utikuma Lake Core BU1. Red noise (AR1) and confidence levels are indicated on the spectrogram (<b>left</b>). Periodicities are indicated when the spectral power is statistically significant at 90%. Likewise, time-frequency areas of high spectral power, shown in red, which are statistically significant at 90% are indicated with black contouring on the CWT scalogram (<b>right</b>). CONISS boundaries (white dashed lines) overlay the wavelet scalograms.</p>
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<p>Spectral and wavelet analysis results for the five identified end members (EMs) identified in Utikuma Lake Core BU1. Oscillations above the 90% confidence level are labeled in the spectral time series results (<b>left</b>) and encircled in a solid black line in the wavelet time series analyses (<b>right</b>). CONISS boundaries (white dashed lines) overlay the wavelet scalograms.</p>
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<p>Cross wavelet transforms (XWTs) of EM02 and EM03 with annual snowfall total in Campsie, AB, and each of the PDO, ENSO, AO, and NAO. Oscillations above the 90% confidence level are encircled in a solid black line.</p>
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<p>Cross wavelet transforms (XWTs) of EM01 and EM04 with annual rainfall total in Campsie, AB, and each of the PDO and ENSO. Oscillations above the 90% confidence level are encircled in a solid black line.</p>
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<p>Continuous wavelet transform (CWT) of the Pacific Decadal Oscillation. Oscillations above the 90% confidence level are encircled in a solid black line.</p>
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15 pages, 1883 KiB  
Article
Evaluation Index System for Thermokarst Lake Susceptibility: An Effective Tool for Disaster Warning on the Qinghai–Tibet Plateau, China
by Lan Li, Yilu Zhao, Xuan Li, Wankui Ni and Fujun Niu
Sustainability 2025, 17(4), 1464; https://doi.org/10.3390/su17041464 - 11 Feb 2025
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Abstract
In the context of global warming, landscapes with ice-rich permafrost, such as the Qinghai–Tibet Plateau (QTP), are highly vulnerable. The expansion of thermokarst lakes erodes the surrounding land, leading to collapses of various scales and posing a threat to nearby infrastructure and the [...] Read more.
In the context of global warming, landscapes with ice-rich permafrost, such as the Qinghai–Tibet Plateau (QTP), are highly vulnerable. The expansion of thermokarst lakes erodes the surrounding land, leading to collapses of various scales and posing a threat to nearby infrastructure and the environment. Assessing the susceptibility of thermokarst lakes in remote, data-scarce areas remains a challenging task. In this study, Landsat imagery and human–computer interaction were employed to improve the accuracy of thermokarst lake classification. The study also identified the key factors influencing the occurrence of thermokarst lakes, including the lake density, soil moisture (SM), slope, vegetation, snow cover, ground temperature, precipitation, and permafrost stability (PS). The results indicate that the most susceptible areas cover 19.02% of the QTP’s permafrost region, primarily located in southwestern Qinghai, northeastern Tibet, and the Hoh Xil region. This study provides a framework for mapping the spatial distribution of thermokarst lakes and contributes to understanding the impact of climate change on the QTP. Full article
(This article belongs to the Special Issue Geological Environment Monitoring and Early Warning Systems)
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<p>Assessment units and LD.</p>
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<p>Zoning Map of the Susceptibility of thermokarst Lake in Permafrost Regions.</p>
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29 pages, 5698 KiB  
Article
Reconstructing Historical Land Use and Anthropogenic Inputs in Lake Victoria Basin: Insights from PAH and n-Alkane Trends
by Camille Joy Enalbes, Dennis M. Njagi, Chen Luo, Daniel Olago and Joyanto Routh
Toxics 2025, 13(2), 130; https://doi.org/10.3390/toxics13020130 - 10 Feb 2025
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Abstract
Over the past century, human activities have profoundly transformed global ecosystems. Lake Victoria in East Africa exemplifies these challenges, showcasing the interplay of anthropogenic pressures driven by land use changes, urbanization, agriculture, and industrialization. Our comprehensive study investigates polycyclic aromatic hydrocarbons (PAHs) and [...] Read more.
Over the past century, human activities have profoundly transformed global ecosystems. Lake Victoria in East Africa exemplifies these challenges, showcasing the interplay of anthropogenic pressures driven by land use changes, urbanization, agriculture, and industrialization. Our comprehensive study investigates polycyclic aromatic hydrocarbons (PAHs) and n-alkanes in the lake and its catchment to trace their sources and historical deposition. Sediment cores were collected from six sites within the catchment, representing diverse landforms and human activities, ensuring a comprehensive understanding of the basin. The results indicate significant spatial and temporal variations in both PAH and n-alkane profiles, reflecting diverse land use changes and development trajectories in the basin. Urban sites often exhibited higher concentrations of PAHs and short-chain n-alkanes, indicative of anthropogenic sources such as fossil fuel combustion, the input of petroleum hydrocarbons, and industrial emissions. In contrast, rural areas showed low PAH levels and a dominance of long-chain n-alkanes from terrestrial plant waxes. The n-alkane ratios, including the Carbon Preference Index and the Terrigenous–Aquatic Ratio, suggested shifts in organic matter sources over time, corresponding with land use changes and increased human activities. A mid-20th century shift toward increased anthropogenic contributions was observed across sites, coinciding with post-independence development. The mid-lake sediment core integrated inputs from multiple sub-catchments, providing a comprehensive record of basin-scale changes. These findings highlight three distinct periods of organic matter input: pre-1960s, dominated by natural and biogenic sources; 1960s–1990s, marked by increasing anthropogenic influence; and post-1990s, characterized by complex mixtures of pyrogenic, petrogenic, and biogenic sources. This study underscores the cumulative environmental and aquatic ecosystem effects of urbanization (rural vs. urban sites), industrialization, and land use changes over the past century. The combined analyses of PAHs and n-alkanes provide a comprehensive understanding of historical and ongoing environmental impacts, emphasizing the need for integrated management strategies that address pollutant inputs to preserve Lake Victoria’s ecological integrity. Full article
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<p>Study sites in the Lake Victoria Basin in Kenya.</p>
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<p>Mean PAH concentrations (ng/g dry weight) in sediment cores from sites in Lake Victoria and its catchment.</p>
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<p>Summary of LMW/HMW PAH ratio vs. depth and age in sediment cores from Lake Victoria and its catchment.</p>
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<p>Summary of FLA/(FLA + Pyr) ratio vs. depth and age in sediment cores from sites in Lake Victoria and its catchment.</p>
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<p>Summary of IP/(IP + BghiP) ratio vs. depth and age in sediment cores from sites in Lake Victoria and its catchment.</p>
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<p>Total concentration of n-alkanes (mg/kg dry weight) in sediment cores from sites in Lake Victoria and its catchment.</p>
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<p>Summary of n-alkane LMW/HMW ratio vs. depth and age in sediment cores from Lake Victoria and its catchment.</p>
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<p>Summary of TAR vs. depth and age in sediment cores from Lake Victoria and its catchment.</p>
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<p>Summary of CPI ratio vs. depth and age in sediment cores from Lake Victoria and its catchment.</p>
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<p>Principal component analysis showing the multivariate variation amongst different organic carbon sources (TOC, black carbon, PAH, and n-alkanes) in the Lake Victoria catchment.</p>
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<p>Correlation matrix of TOC, BC, PAH, and n-alkanes in the Lake Victoria catchment. Green denotes positive values, whereas red denotes negative values.</p>
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<p>PAH ring profiles and mean carcinogenic PAH (cPAH) from sites in Lake Victoria catchment.</p>
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<p>Comparison of PAH concentrations and changes in land use and land cover (LULC) in the Nyando–Yala and Nzoia–Sio basins from 1985 to 2014 (adapted from [<a href="#B11-toxics-13-00130" class="html-bibr">11</a>]). The PAH concentrations on the left are from the bottom of the core, and those on the right are from the top, showing the change in the most abundant PAH levels.</p>
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21 pages, 5458 KiB  
Article
Cumulative Ecological Impact of Cascade Hydropower Development on Fish Community Structure in the Main Stream of the Xijiang River, China
by Yuansheng Zhu, Jiayang He, Fangyuan Xiong, Zhiqiang Wu, Jiajun Zhang, Yusen Li, Yong Lin, Anyou He, Dapeng Wang and Yaoquan Han
Animals 2025, 15(4), 495; https://doi.org/10.3390/ani15040495 - 10 Feb 2025
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Abstract
In recent decades, dams worldwide are increasingly constructed in a row along a single river or basin, thus forming reservoir cascades, and in turn producing cumulative ecological effects along these areas. The use of multimetric indices (MMI) based on fish assemblages to assess [...] Read more.
In recent decades, dams worldwide are increasingly constructed in a row along a single river or basin, thus forming reservoir cascades, and in turn producing cumulative ecological effects along these areas. The use of multimetric indices (MMI) based on fish assemblages to assess the ecological health status of rivers and lakes has also been extensively developed. However, to date, there are no studies that employ MMI for the identification of the cumulative effects of reservoir cascades. The aim of this study was to develop a new Fish-based Index of Biotic Integrity (F-IBI) that can effectively identify the cumulative effects of reservoir cascades on fish assemblages in two important habitats (the free-flowing reach between reservoirs and the transition zone in the reservoir). Fish assemblages from 12 sites were sampled along the cascade reservoirs in the Xijiang River, China. First, through screening for redundancy, precision, and responsiveness of the candidate metrics, a new F-IBI based on ecological trait information of fish species composition was developed to estimate the ecological status of all sites. F-IBI scores exhibited an obviously downward trend from upstream to downstream in a reservoir cascade, and the transition zones in the reservoir displayed significantly lower F-IBI scores than the free-flowing reaches between reservoirs. Secondly, using Random Forest models, it was shown that the F-IBI can effectively identify the cumulative effects of the reservoir cascades on fish assemblages. Furthermore, we also demonstrated metric-specific responses to different stressors, particularly the multiple reservoir cascades, which showed the following: (1) The F-IBI index system developed based on the Random Forest model can effectively identify the superimposed effects of cascade power stations on fish integrity changes, with the cumulative time effect and the GDP index of river segments playing a key role; (2) To effectively protect the fish resources in the main stream of the Xijiang River, where priority should be given to the habitat of the natural flowing river sections between the reservoirs. At the same time, environmental regulatory policies should be formulated accordingly based on the human development status of each river section. Full article
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<p>Distribution map of 12 sampling points in the mainstream of the Xijiang River. Note: 11 constructed hydropower stations, arranged downstream as follows: Tianshengqiao First Grade (<b>I</b>), Tianshengqiao Second Grade (<b>II</b>), Pingban (<b>III</b>), Longtan (<b>IV</b>), Yantan (<b>V</b>), Dahua (<b>VI</b>), Bailongtan (<b>VII</b>), Letan (<b>VIII</b>), Qiaogong (<b>IX</b>), Datengxia (<b>X</b>), and Changzhou (<b>XI</b>).</p>
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<p>(<b>a</b>) Hopkins clustering trend analysis of historical fish species in each reach in the mainstream of the Xijiang River; (<b>b</b>) Hierarchical clustering analysis based on the composition of historical fish species in the mainstream of the Xijiang River, the different color boxes show different cluster groups.</p>
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<p>(<b>a</b>) Spearman correlations for 25 biological traits; (<b>b</b>) Discriminative power screening based on boxplot; (<b>c</b>) The concentrated change trend of the historical and current monitoring values of the 11 indicators; (<b>d</b>) The sensitivity analysis of the historical reference values and the current monitoring values of 11 indicators. Note: EF, endemic fishes; SF, surface fishes; MF, midwater fishes; DF, demersal fishes; EFM, epistatic fish of mouth; NFM, normotopia fish of mouth; HFM, hypooral fish of mouth; OF, omnivorous fishes; HF, herbivorous fishes; PF, planktivorous fishes; FZ, fishes as zoobenthivores; MIF, migratory fishes; HYF, hydrostatic fishes; EUF, eurytopicity fishes; CUF, current-loving cold water fishes; TAF, tabular fishes; CYF, cylindrical fishes; LAF, lateral fishes; FUF, fusiform fishes; SIF, sinking-egg fishes; FLF, floating egg fish; DRF, drifting-egg fish; SPF, special ways of spawning fish. H, the historical reference values; T, the current monitoring values.</p>
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<p>(<b>a</b>) F-IBI scores and F-IBI scoring grades for each sampling site; (<b>b</b>) Comparison of each sensitive index in two different habitats; (<b>c</b>) Comparison of each F-IBI scores in two different habitats. Note: NFM, normotopia fish of mouth; PF, planktivorous fishes; HYF, hydrostatic fishes; CUF, current-loving cold water fishes; LAF, lateral fishes; SIF, sinking-egg fishes; FLF, floating egg fish; SPF, special ways of spawning fish; NRAD, the natural reach between two adjacent dams; TR, transitional region in reservoir.</p>
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<p>(<b>a</b>) Relative contribution of environmental variables based on two different methods (%IncMSE and IncNodePurity); (<b>b</b>) Relationships between F-IBI scores and four important environment variables. Note: WA, water Area; VR, average annual runoff; TEM, mean air temperature; PRE, mean annual precipitation; NRAD, natural free-flowing reach between two adjacent dams, LUR, proportion of land use, HT, habitat type, GDP, gross domestic product; DWN, density of water network; CTP, cumulative effect time of power station; ALT, altitude. The shaded area represents the 95% confidence interval.</p>
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<p>The Random Forest model for predicting F-IBI scores of eight sensitive indicators in 12 reaches of the Xijiang River main stream and the relative contribution ability of environmental variables in predicting F-IBI scores of single sensitive indicators based on IncMSE and IncNodePurity. Note: WA, water area; VR, average annual runoff; TEM, mean air temperature; PRE, mean annual precipitation; NRAD, natural free-flowing reach between two adjacent dams; LUR, proportion of land use; HT, habitat type; GDP, gross domestic product; DWN, density of water network, CTP, cumulative effect time of power station; ALT, altitude. NFM, normotopia fish of mouth; PF, planktivorous fishes; HYF, hydrostatic fishes; CUF, current-loving cold water fishes; LAF, lateral fishes; SIF, sinking-egg fishes; FLF, floating egg fish; SPF, special ways of spawning fish.</p>
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