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Keywords = complex ecosystem impact

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23 pages, 11095 KiB  
Article
Bayesian Network Analysis: Assessing and Restoring Ecological Vulnerability in the Shaanxi Section of the Qinling-Daba Mountains Under Global Warming Influences
by Zezhou Hu, Nan Li, Miao Zhang and Miao Miao
Sustainability 2024, 16(22), 10021; https://doi.org/10.3390/su162210021 - 17 Nov 2024
Viewed by 346
Abstract
Human activities, especially industrial production and urbanization, have significantly affected vegetation cover, water resource cycles, climate change, and biodiversity in the Qinling-Daba Mountain region and its surrounding areas. These activities contribute to complex and lasting impacts on ecological vulnerability. The Qinling Mountain region [...] Read more.
Human activities, especially industrial production and urbanization, have significantly affected vegetation cover, water resource cycles, climate change, and biodiversity in the Qinling-Daba Mountain region and its surrounding areas. These activities contribute to complex and lasting impacts on ecological vulnerability. The Qinling Mountain region exhibits a complex interaction with human activities. The current research on the ecological vulnerability of the Qinling Mountain region primarily focuses on spatial distribution and the driving factors. This study innovatively applies the VSD assessment and Bayesian networks to systematically evaluate and simulate the ecological vulnerability of the study area over the past 20 years, which indicates that the integration of the VSD model with the Bayesian network model enables the simulation of dynamic relationships and interactions among various factors within the study areas, providing a more accurate assessment and prediction of ecosystem responses to diverse changes from a dynamic perspective. The key findings are as follows. (1) Areas of potential and slight vulnerability are concentrated in the Qinling-Daba mountainous regions. Over the past 20 years, areas of extreme and high vulnerability have significantly decreased, while areas of potential vulnerability and slight vulnerability have increased. (2) The key factors impacting ecological vulnerability during this period included industrial water use, SO2 emissions, industrial wastewater, and ecological water use. (3) Areas primarily hindering the transition to potential vulnerability are concentrated in well-developed small urban regions within basins. Furthermore, natural factors like altitude and temperature, which cannot be artificially regulated, are the major impediments to future ecological restoration. Therefore, this paper recommends natural restoration strategies based on environmental protection and governance strategies that prioritize green development as complementary measures. The discoveries of the paper provide a novel analytical method for the study of ecological vulnerability in mountainous areas, offering valuable insights for enhancing the accuracy of ecological risk prediction, fostering the integration of interdisciplinary research, and optimizing environmental governance and protection strategies. Full article
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<p>Location of the study area.</p>
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<p>Illustration of the coupling relationship between regional society–ecology and water resources.</p>
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<p>The framework for assessing ecological vulnerability provided by the VSD model.</p>
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<p>Spatial and temporal differentiation of ecological vulnerability. (<b>a</b>–<b>e</b>) depict the spatial distribution of ecological vulnerability in the study area for the years 2000, 2005, 2010, 2015, and 2020, respectively.</p>
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<p>Example of a Bayesian network model in 2020.</p>
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<p>The sensitivity of key driving indicators of ecological vulnerability changes during 2000–2020.</p>
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<p>Probability changes in various driving indicators under different ecological vulnerability scenarios. Note: A, B, C, D, and E represent each of the different ecological vulnerability drivers at different hierarchical range types, with A representing the low state (0–0.2), B representing the lower state (0.2–0.4), C representing the medium state (0.4–0.6), D representing the higher state (0.6–0.8), and E representing the high state (0.8–1).</p>
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<p>Spatial differentiation of sensitive indicators in potential vulnerability scenarios.</p>
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20 pages, 4822 KiB  
Article
Assessment of the Impact of Meteorological Variables on Lake Water Temperature Using the SHapley Additive exPlanations Method
by Teerachai Amnuaylojaroen, Mariusz Ptak and Mariusz Sojka
Water 2024, 16(22), 3296; https://doi.org/10.3390/w16223296 - 17 Nov 2024
Viewed by 286
Abstract
The water temperature of lakes is one of their fundamental characteristics, upon which numerous processes in lake ecosystems depend. Therefore, it is crucial to have detailed knowledge about its changes and the factors driving those changes. In this article, a neural network model [...] Read more.
The water temperature of lakes is one of their fundamental characteristics, upon which numerous processes in lake ecosystems depend. Therefore, it is crucial to have detailed knowledge about its changes and the factors driving those changes. In this article, a neural network model was developed to examine the impact of meteorological variables on lake water temperature by integrating daily meteorological data with data on interday variations. Neural networks were selected for their ability to model complex, non-linear relationships between variables, often found in environmental data. Among various architectures, the Artificial Neural Network (ANN) was chosen due to its superior performance, achieving an R2 of 0.999, MSE of 0.0352, and MAE of 0.1511 in validation tests. These results significantly outperformed other models such as Multi-Layer Perceptrons (MLPs), Recurrent Neural Networks (RNNs), and Long Short-Term Memory (LSTM). Two lakes (Lake Mikołajskie and Sławskie) differing in morphometric parameters and located in different physico-geographical regions of Poland were analyzed. Performance metrics for both lakes show that the model is capable of providing accurate water temperature forecasts, effectively capturing the primary patterns in the data, and generalizing well to new datasets. Key variables in both cases turned out to be air temperature, while the response to wind and cloud cover exhibited diverse characteristics, which is a result of the morphometric features and locations of the measurement sites. Full article
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<p>Location of study objects: Sławskie Lake (<b>A</b>); Mikołajskie Lake (<b>B</b>); blue color-lakes, red color—hydrological station; green color—meteorological station.</p>
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<p>Workflow of this study.</p>
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<p>Learning rate on (<b>a</b>) MSE, (<b>b</b>) MAE, and (<b>c</b>) R<sup>2</sup> of sensitivity analysis.</p>
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<p>Yearly average observed and predicted water temperature from neural network (<b>a</b>); scatter plot of observed and predicted water temperature from neural network model for validation set (<b>b</b>) and test set (<b>c</b>) at Mikołajskie Lake.</p>
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<p>Yearly average observed and predicted water temperature from neural network (<b>a</b>); scatter plot of observed and predicted water temperature from neural network model for validation set (<b>b</b>) and test set (<b>c</b>) at Sławskie Lake.</p>
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<p>Model loss for training and validation data at Mikołajskie (<b>a</b>) and Sławskie (<b>b</b>).</p>
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<p>Feature importance based on SHAP values at Mikołajskie Lake (<b>a</b>), and Sławskie Lake (<b>b</b>). Mean Air Temperature: the average air temperature for the day; Maximum Air Temperature: the highest air temperature recorded during the day; Minimum Air Temperature: the lowest air temperature recorded during the day; Daily Air Temperature Amplitude: the difference between the maximum and minimum air temperatures for the day; Average Wind Speed: the average wind speed recorded over the day; Total Daily Rainfall: the total amount of rainfall recorded for the day; Average Daily Cloud Cover: the average cloud cover observed in octants (scale from 0 to 8); Interday Air Temperature Change: the change in air temperature between consecutive days; Interday Wind Speed Change: the change in average wind speed between consecutive days; Interday Rainfall Change: the change in total daily rainfall between consecutive days; Interday Cloud Cover Change: the change in average cloud cover between consecutive days.</p>
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21 pages, 2447 KiB  
Article
Influence of Organic Matter and Speciation on the Dynamics of Trace Metal Adsorption on Microplastics in Marine Conditions
by Ana Rapljenović, Marko Viskić, Stanislav Frančišković-Bilinski and Vlado Cuculić
Toxics 2024, 12(11), 820; https://doi.org/10.3390/toxics12110820 (registering DOI) - 16 Nov 2024
Viewed by 231
Abstract
Dissolved organic matter (DOM), primarily in the form of humic acid (HA), plays a crucial role in trace metal (TM) speciation and their subsequent adsorption dynamics on microplastics (MP) in aquatic environments. This study evaluates the impact of environmentally relevant concentrations of HA [...] Read more.
Dissolved organic matter (DOM), primarily in the form of humic acid (HA), plays a crucial role in trace metal (TM) speciation and their subsequent adsorption dynamics on microplastics (MP) in aquatic environments. This study evaluates the impact of environmentally relevant concentrations of HA on the adsorption behaviors of essential (Co, Cu, Ni, and Zn) and toxic (Cd and Pb) TMs onto polyethylene (PE) and polypropylene (PP) pellets, as well as PP fibers under marine conditions, during a six-week experiment. The HA concentrations were 0.1, 1, and 5 mg/L, while all metals were in the same amounts (10 µg/L). Results reveal that HA significantly influences the adsorption of Cu, Pb, and Zn on MP, particularly on PP fibers, which exhibited the greatest TM adsorption dynamics. The adsorption patterns correspond to the concentrations of these metals in seawater, with the sequence for pellets being Zn > Cu > Pb > Ni > Co~Cd, and for fibers Cu > Zn > Pb > Co~Ni > Cd. Speciation modeling supported these findings, indicating that Cu, Pb, and Zn predominantly associate with HA in seawater, facilitating their adsorption on MP, whereas Cd, Co, and Ni mainly form free ions and inorganic complexes, resulting in slower adsorption dynamics. Statistical analysis confirmed the influence of HA on the adsorption of Cd, Pb, Cu, and Ni. By investigating the dynamics of TM adsorption on plastics, the influence of DOM on these two contaminants under marine conditions was evaluated. The presented results can help in forming a better understanding of synergistic plastic and trace metal pollution in marine systems that are relevant at the global level, since both contaminants pose a serious threat to aquatic ecosystems. Full article
(This article belongs to the Section Ecotoxicology)
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<p>Flowchart of adsorption experiment, leaching and measurement of TM.</p>
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<p>Adsorption of trace metals on PE pellets in seawater in presence of HA. Adsorbed metal fractions (expressed as ng metal/g fibers) with 95% confidence intervals. Symbols indicate different HA concentrations: black circles represent metal adsorption without HA (0 mg/L HA), blue triangles indicate 0.1 mg/L HA, red squares indicate 1 mg/L HA, and green diamonds represent 5 mg/L HA. The x-axis is scaled unevenly for readability, with a finer scale for the initial 2 days, followed by a broader scale for the period from 2 to 42 days.</p>
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<p>Adsorption of trace metals on PP pellets in seawater in presence of HA. Adsorbed metal fractions (expressed as ng metal/g fibers) with 95% confidence intervals. Symbols indicate different HA concentrations: black circles represent metal adsorption without HA (0 mg/L HA), blue triangles indicate 0.1 mg/L HA, red squares indicate 1 mg/L HA, and green diamonds represent 5 mg/L HA. The x-axis is scaled unevenly for readability, with a finer scale for the initial 2 days, followed by a broader scale for the period from 2 to 42 days.</p>
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<p>Adsorption of metals on PP fibers in seawater in presence of HA. Adsorbed metal fractions (expressed as ng metal/g fibers) with 95% confidence intervals. Symbols indicate different HA concentrations: black circles represent metal adsorption without HA (0 mg/L HA), blue triangles indicate 0.1 mg/L HA, red squares indicate 1 mg/L HA, and green diamonds represent 5 mg/L HA. The x-axis is scaled unevenly for readability, with a finer scale for the initial 2 days, followed by a broader scale for the period from 2 to 42 days.</p>
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13 pages, 2559 KiB  
Article
Precipitation Patterns and Their Role in Modulating Nitrous Oxide Emissions from Arid Desert Soil
by Chunming Xin, Huijun Qin, Yuanshang Guo and Mingzhu He
Land 2024, 13(11), 1920; https://doi.org/10.3390/land13111920 - 15 Nov 2024
Viewed by 248
Abstract
Nitrous oxide (N2O) ranks as the third most significant greenhouse gas, capable of depleting the ozone layer and posing threats to terrestrial ecosystems. Climate change alters precipitation variability, notably in terms of frequency and magnitude. However, the implications of precipitation variability [...] Read more.
Nitrous oxide (N2O) ranks as the third most significant greenhouse gas, capable of depleting the ozone layer and posing threats to terrestrial ecosystems. Climate change alters precipitation variability, notably in terms of frequency and magnitude. However, the implications of precipitation variability on N2O emissions and the underlying mechanisms remain inadequately understood. In this study, employing laboratory incubation methods on three representative sandy soil types (sandy soil, shrub soil, and crust soil), we examined the impacts of diverse precipitation levels (5 mm and 10 mm) and frequencies (7 days and 14 days) on N2O emissions from these soil types. This study aims to clarify the complex connections between soil N2O emission fluxes and soil physicochemical properties in the soil environment. Our findings reveal that the N2O emission flux exhibits heightened responsiveness to 5 mm precipitation events and a 14-day precipitation frequency, and compared to other treatments, the 5 mm precipitation and 14-day precipitation frequency treatment resulted in a 20% increase in cumulative nitrous oxide emissions. Consequently, cumulative N2O emissions were notably elevated under the 5 mm precipitation and 14-day precipitation frequency treatments compared to the other experimental conditions. The N2O emission flux in sandy soil displayed a positive correlation with available phosphorus (AP) and a negative correlation with pH, primarily attributed to the exceedingly low AP content in sandy soil. In shrub soil, the soil N2O emission flux exhibited a significant positive correlation with NH4+-N and a negative correlation with NO3-N. Conversely, no significant correlations were observed between soil N2O emission flux and soil physicochemical properties in crust soil, underscoring the importance of considering plant–soil microbial interactions. Our findings suggest that soil nitrous oxide emissions in arid and semi-arid regions will be particularly responsive to small and frequent rainfall events as precipitation patterns change in the future, primarily due to their soil physicochemical characteristics. Full article
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<p>Variations in mass water content under different experimental conditions. The experimental treatments consisted of a precipitation frequency of 7 days with either 5 mm (F7P5) or 10 mm (F7P10) of precipitation (<b>a</b>), as well as a precipitation frequency of 14 days with either 5 mm (F14P5) or 10 mm (F14P10) of precipitation (<b>b</b>).</p>
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<p>The emission fluxes of N<sub>2</sub>O for each experimental treatment. The experimental treatments comprised F7P5 (<b>a</b>), F7P10 (<b>b</b>), F14P5 (<b>c</b>), and F14P10 (<b>d</b>). The data for each point is represented as the mean value plus or minus the standard error (mean ± SE).</p>
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<p>The total cumulative N<sub>2</sub>O emission across various experimental treatments. Lowercase letters indicate significant differences in N<sub>2</sub>O cumulative emissions between the three soil types, while uppercase letters indicate significant differences between experimental treatments. The identical letter indicates no statistically significant variance, while distinct letters indicate a significant difference.</p>
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<p>The relationships between species N<sub>2</sub>O emission fluxes and soil physicochemical properties in sandy soil (<b>a</b>), shrub soil (<b>b</b>), and crust soil (<b>c</b>).</p>
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<p>The correlation between AP (<b>a</b>) and pH (<b>b</b>) levels and the emission fluxes of soil N<sub>2</sub>O in sandy soil. The red area denotes the 95% confidence interval.</p>
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<p>The correlation between NH<sub>4</sub><sup>+</sup>-N (<b>a</b>) and NO<sub>3</sub><sup>−</sup>-N (<b>b</b>) levels and N<sub>2</sub>O emission fluxes from shrub soil. The red area denotes the 95% confidence interval.</p>
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25 pages, 12861 KiB  
Article
Comparative Phylogeography of Two Specialist Rodents in Forest Fragments in Kenya
by Alois Wambua Mweu, Kenneth Otieno Onditi, Laxman Khanal, Simon Musila, Esther Kioko and Xuelong Jiang
Life 2024, 14(11), 1469; https://doi.org/10.3390/life14111469 - 12 Nov 2024
Viewed by 351
Abstract
The fragmented forests of the Kenya highlands, known for their exceptional species richness and endemism, are among the world’s most important biodiversity hotspots. However, detailed studies on the fauna of these ecosystems—especially specialist species that depend on moist forests, which are particularly threatened [...] Read more.
The fragmented forests of the Kenya highlands, known for their exceptional species richness and endemism, are among the world’s most important biodiversity hotspots. However, detailed studies on the fauna of these ecosystems—especially specialist species that depend on moist forests, which are particularly threatened by habitat fragmentation—are still limited. In this study, we used mitochondrial genes (cytochrome b and the displacement loop) and a nuclear marker (retinol-binding protein 3) to investigate genetic and morphological diversity, phylogenetic associations, historical divergence, population dynamics, and phylogeographic patterns in two rodent species—the soft-furred mouse (Praomys jacksoni) and the African wood mouse (Hylomyscus endorobae)—across Kenya’s forest landscapes. We found a complex genetic structure, with P. jacksoni exhibiting greater genetic diversity than H. endorobae. The Mt. Kenya P. jacksoni populations are significantly genetically different from those in southwestern forests (Mau Forest, Kakamega Forest, and Loita Hills). In contrast, H. endorobae presented no observable biogeographic structuring across its range. The genetic diversity and geographic structuring patterns highlighted selectively strong effects of forest fragmentation and differing species’ ecological and evolutionary responses to these landscape changes. Our findings further underscore the need for expanded sampling across Kenya’s highland forests to better understand species’ changing diversity and distribution patterns in response to the impacts of human-mediated habitat changes. These insights are critical for informing conservation strategies to preserve biodiversity better in this globally important region. Full article
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<p>Distribution maps of <span class="html-italic">Praomys jacksoni</span> and <span class="html-italic">Hylomyscus endorobae</span> across their known distributions<span class="html-italic">;</span> (<b>a</b>) shows the field survey sampling sites in Kenya [red-outlined circles with a red plus sign] and (<b>b</b>) shows the occurrences of these species based on the International Union for Conservation of Nature (IUCN) Red List ranges and geolocated point-occurrence records from the Global Biodiversity Information Facility (GBIF). Grayscale shading in both plots represents elevation with darker shades corresponding to higher elevations. The blue shade in ‘b’ represents the ocean. See the legend for other labeling details.</p>
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<p>Morphological differentiation of the Kenyan <span class="html-italic">Praomys jacksoni</span> and <span class="html-italic">H. endorobae</span> samples from different survey sites.</p>
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<p>Mitochondrial cytochrome b phylogenies for the <span class="html-italic">Praomys</span> and <span class="html-italic">Hylomyscus</span> genera. (<b>a</b>) Genus <span class="html-italic">Praomys</span>, (<b>b</b>) <span class="html-italic">Praomys jacksoni</span> complex, (<b>c</b>) Kenya’s <span class="html-italic">Praomys jacksoni</span>, (<b>d</b>) genus <span class="html-italic">Hylomyscus</span>, (<b>e</b>) <span class="html-italic">Hylomyscus denniae</span> species group, and (<b>f</b>) <span class="html-italic">Hylomyscus endorobae</span>.</p>
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<p>Geographical impacts on genetic structuring within <span class="html-italic">Hylomyscus endorobae</span> and <span class="html-italic">Praomys jacksoni</span> in Kenya. Panel (<b>a</b>) shows the <span class="html-italic">H. endorobae</span> results, and panel (<b>b</b>) shows the <span class="html-italic">P. jacksoni</span> results. The geographical distributions of the samples are overlaid on the elevation layer (darker corresponds to high elevations) in the top figures. The haplotype networks are also shown in corresponding panels, illustrating the genealogical clustering of samples based on localities. The phylogenetic trees in the middle figures are colored based on the sampling locality IDs and match the distribution and haplotype network colors. The correlations between geographic distances (inferred from latitude–longitude sample records) and genetic distances (pairwise nucleotide differences) are shown in the bottom figures.</p>
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<p>Ancestral area reconstructions of <span class="html-italic">Praomys jacksoni</span> (<b>a</b>) and <span class="html-italic">Hylomyscus endorobae</span> (<b>b</b>) based on the dispersal–extinction–cladogenesis model [<a href="#B74-life-14-01469" class="html-bibr">74</a>] implemented in RASP [<a href="#B71-life-14-01469" class="html-bibr">71</a>]. The major sampling sites were used as the biogeographical states and are labeled in the legends with matching color schemes.</p>
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<p>Population dynamics analysis of <span class="html-italic">Hylomyscus endorobae</span> (<b>a</b>) and <span class="html-italic">Praomys jacksoni</span> (<b>b</b>) in Kenya. The main figures (bar plots) show the mismatch distribution analysis, with the <span class="html-italic">y</span>-axis showing the frequency of pairwise nucleotide differences between sequences. The inset plots show the Bayesian skyline plots of population change (<span class="html-italic">y</span>-axis) over evolutionary time (<span class="html-italic">x</span>-axis) to the left and corresponding lineages through time to the right.</p>
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<p>Habitat suitability maps and summary graphs of species distribution modeling projections for habitat suitability scenarios for <span class="html-italic">Praomys jacksoni</span> and <span class="html-italic">Hylomyscus endorobae</span>; (<b>a</b>) shows the range-wide changes to the modeled habitat suitability classes, with (<b>b</b>) showing the corresponding quantitative changes summarized into periods by area change associations. In both (<b>a</b>,<b>b</b>), the panels to the left represent <span class="html-italic">H. endorobae</span>, whereas those to the right represent <span class="html-italic">P. jacksoni</span>. In (<b>a</b>), the x axes represent longitude and the y axes represent latitude.</p>
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<p>Projected land-use changes within the IUCN-recorded species distribution range (<b>a</b>) and within the species’ known distribution range in Kenya (<b>b</b>) for <span class="html-italic">Praomys jacksoni</span> and <span class="html-italic">Hylomyscus endorobae</span>. The range of <span class="html-italic">H. endorobae</span> is entirely nested within the <span class="html-italic">P. jacksoni</span> range (see <a href="#life-14-01469-f001" class="html-fig">Figure 1</a>).</p>
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<p>Projected land-use changes within the IUCN-recorded species distribution range (<b>a</b>) and within the species’ known distribution range in Kenya (<b>b</b>) for <span class="html-italic">Praomys jacksoni</span> and <span class="html-italic">Hylomyscus endorobae</span>. The range of <span class="html-italic">H. endorobae</span> is entirely nested within the <span class="html-italic">P. jacksoni</span> range (see <a href="#life-14-01469-f001" class="html-fig">Figure 1</a>).</p>
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21 pages, 8003 KiB  
Article
The Impact of Seasonal Climate on Dryland Vegetation NPP: The Mediating Role of Phenology
by Xian Liu, Hengkai Li, Yanbing Zhou, Yang Yu and Xiuli Wang
Sustainability 2024, 16(22), 9835; https://doi.org/10.3390/su16229835 - 11 Nov 2024
Viewed by 453
Abstract
Dryland ecosystems are highly sensitive to climate change, making vegetation monitoring crucial for understanding ecological dynamics in these regions. In recent years, climate change, combined with large-scale ecological restoration efforts, has led significant greening in China’s arid areas. However, the mechanisms through which [...] Read more.
Dryland ecosystems are highly sensitive to climate change, making vegetation monitoring crucial for understanding ecological dynamics in these regions. In recent years, climate change, combined with large-scale ecological restoration efforts, has led significant greening in China’s arid areas. However, the mechanisms through which seasonal climate variations regulate vegetation growth are not yet fully understood. This study hypothesizes that seasonal climate change affects net primary productivity (NPP) of vegetation by influencing phenology. We focused on China’s Windbreak and Sand-Fixation Ecological Function Conservation Areas (WSEFCAs) as representative regions of dryland vegetation. The Carnegie–Ames–Stanford Approach (CASA) model was used to estimate vegetation NPP from 2000 to 2020. To extract phenological information, NDVI data were processed using Savitzky–Golay (S–G) filtering and threshold methods to determine the start of season (SOS) and end of season (EOS). The structural equation model (SEM) was constructed to quantitatively assess the contributions of climate change (temperature and precipitation) and phenology to variations in vegetation NPP, identifying the pathways of influence. The results indicate that the average annual NPP in WSEFCAs increased from 55.55 gC/(m2·a) to 75.01 gC/(m2·a), exhibiting uneven spatial distribution. The pathways through which seasonal climate affects vegetation NPP are more complex and uneven. Summer precipitation directly promoted NPP growth (direct effect = 0.243, p < 0.001) while also indirectly enhancing NPP by significantly advancing SOS (0.433, p < 0.001) and delaying EOS (−0.271, p < 0.001), with an indirect effect of 0.133. This finding highlights the critical role of phenology in vegetation growth, particularly in regions with substantial seasonal climate fluctuations. Although the overall ecological environment of WSEFCAs has improved, significant regional disparities remain, especially in northwestern China. This study introduces causal mediation analysis to systematically explore the mechanisms through which seasonal climate change impacts vegetation NPP in WSEFCAs, providing new insights into the broader implications of climate change and offering scientific support for ecological restoration and management strategies in arid regions. Full article
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<p>Study area. (<b>a</b>) Tarim River Basin (Tarim); (<b>b</b>) Altun Desert Steppe (Altun); (<b>c</b>) Heihe River Basin (Heihe); (<b>d</b>) Maowusu Sandland (Maowusu); (<b>e</b>) Hunshandak Sandland (Hunshandak); (<b>f</b>) Horqin Sandland (Horqin). Field observation stations: Aksu (AKA); Linze (LZA); Haibei (HBG); Minle (MQD); Shapotou (SPD); Ordos (ESD); Luancheng (LCA); Yucheng (YCA); Guyuan (GYG); Inner Mongolia (NMG); Naiman (NMD); Shenyang (SYA).</p>
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<p>Technical route. (Analysis of action mechanism: The solid line indicates a significant relationship (<span class="html-italic">p</span> &lt; 0.05), while the dashed line indicates a non-significant relationship. The black line indicates the positive paths, and the red line indicates the negative paths. The asterisks *** and ** indicate significance levels of 0.001 and 0.05).</p>
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<p>Model diagram of the driving mechanism of vegetation NPP change in the WSEFCA.</p>
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<p>Spatial and temporal evolution of vegetation NPP ((<b>A</b>) spatial pattern of vegetation NPP in the study area in 2000, 2005, 2010, 2015 and 2020; (<b>B</b>) changes in vegetation NPP in different years and seasons; and (<b>C</b>) changes in vegetation NPP in different regions (black lines indicate the years with the highest values).</p>
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<p>Spatial and temporal evolution of SOS. (<b>A</b>) Spatial patterns of vegetation SOS in the study area for the years 2000, 2005, 2010, 2015 and 2020. (<b>B</b>) Changes in vegetation SOS in different regions (green boxes represent advancing times, orange represents delaying times).</p>
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<p>Spatial and temporal evolution of EOS. (<b>A</b>) Spatial patterns of vegetation EOS in the study area for the years 2000, 2005, 2010, 2015 and 2020. (<b>B</b>) Changes in vegetation EOS in different regions (green boxes represent advancing times, orange represents delaying times).</p>
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<p>The relationships between climatic factors and NPP, SOS and EOS on seasonal scales. The values on the lines represent standardized throughput coefficients, and the thickness of the arrows indicates the magnitude of the standardized coefficients. A solid line indicates a significant relationship (<span class="html-italic">p</span> &lt; 0.05), while a dashed line indicates a non-significant relationship. Black lines indicate positive paths, and red lines indicate negative paths. The asterisks *** and ** indicate significance levels of 0.001 and 0.05, respectively. R<sup>2</sup> denotes the degree of coexplanation of the variable in question.</p>
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<p>The relationships between climatic factors and NPP, SOS, and EOS on annual scales. The values on the lines represent standardized throughput coefficients, and the thickness of the arrows indicates the magnitude of the standardized coefficients. A solid line indicates a significant relationship (<span class="html-italic">p</span> &lt; 0.05), while a dashed line indicates a non-significant relationship. Black lines indicate positive paths, and red lines indicate negative paths. The asterisks *** indicate a significance level of 0.001. R<sup>2</sup> denotes the degree of coexplanation of the variable in question.</p>
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22 pages, 23996 KiB  
Review
Advances in Global Oyster Reef Restoration: Innovations and Sustainable Ecological Approaches
by Asad Jamil, Ambreen Ahmad, Yong Zhao, Yuxuan Zhao, Chen Yang, Yanping Li, Jianbo Tu, Fuxin Niu, Wenliang Kong and Xianhua Liu
Sustainability 2024, 16(22), 9795; https://doi.org/10.3390/su16229795 - 10 Nov 2024
Viewed by 710
Abstract
Oysters have been recognized as ecological engineers for aquatic ecosystems, as oyster reefs provide critical habitats and foraging locations for other marine species. In the past few decades, anthropogenic activities have negatively impacted oyster reef ecosystems across the globe, resulting in a significant [...] Read more.
Oysters have been recognized as ecological engineers for aquatic ecosystems, as oyster reefs provide critical habitats and foraging locations for other marine species. In the past few decades, anthropogenic activities have negatively impacted oyster reef ecosystems across the globe, resulting in a significant decline in their population. This review critically examines the causes and extent of oyster reef degradation, as well as the effectiveness of restoration initiatives employed to reverse this decline. Furthermore, this review evaluates the effectiveness of restoration strategies employed to rehabilitate oyster reefs. Different approaches, such as genetic improvement, suitable site selection, and oyster seeding to enhance oyster reef restorations, are critically reviewed in this paper. Furthermore, some advanced restoration approaches such as 3D printing, shell recycling, and acoustics technologies are also discussed in this paper, which opens the new doors for researchers in the field of restoration ecology. Challenges and barriers hindering successful restoration are also addressed, including financial constraints, regulatory complexities, and public engagement. The findings and insights presented herein contribute to the growing body of knowledge on oyster reef ecology and serve as a valuable resource for policymakers, scientists, and conservation practitioners seeking effective strategies for restoring these vital coastal ecosystems. Full article
(This article belongs to the Section Sustainable Oceans)
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<p>Schematics of various ecosystem services provided by oyster reefs: water filtration, habitat provision, shoreline protection, and nutrient cycling.</p>
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<p>A geographical map representing a global decline in oyster populations on a global scale. (the map is modified from Beck et al. [<a href="#B15-sustainability-16-09795" class="html-bibr">15</a>]).</p>
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<p>Literature analysis in the field of oyster reef restoration. (<b>A</b>) Publication growth trends; (<b>B</b>) Collaboration among the countries and institutions; (<b>C</b>) Co-occurrence network of keywords analysis; (<b>D</b>) Keywords with strongest citation bursts. The red lines represent the duration of bursts; (<b>E</b>) Countries’ scientific production in the field of oyster reef restoration.</p>
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<p>Factors affecting the oyster populations in marine ecosystems.</p>
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<p>A schematic representation of various approaches/techniques for oyster reef restoration.</p>
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<p>(<b>A</b>) A map of ongoing projects on oyster reef restoration at the global scale (the map is modified from [<a href="#B8-sustainability-16-09795" class="html-bibr">8</a>]; (<b>B</b>–<b>E</b>) Various artificial substrates including bagged oyster shell (<b>B</b>), mixed oyster substrates (<b>C</b>), concrete structures (<b>D</b>) mixed concrete substrates (<b>E</b>) used for the attachment of oysters [<a href="#B48-sustainability-16-09795" class="html-bibr">48</a>].</p>
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17 pages, 5121 KiB  
Article
Study on the Evolutionary Characteristics of Post-Fire Forest Recovery Using Unmanned Aerial Vehicle Imagery and Deep Learning: A Case Study of Jinyun Mountain in Chongqing, China
by Deli Zhu and Peiji Yang
Sustainability 2024, 16(22), 9717; https://doi.org/10.3390/su16229717 - 7 Nov 2024
Viewed by 450
Abstract
Forest fires pose a significant threat to forest ecosystems, with severe impacts on both the environment and human society. Understanding the post-fire recovery processes of forests is crucial for developing strategies for species diversity conservation and ecological restoration and preventing further damage. The [...] Read more.
Forest fires pose a significant threat to forest ecosystems, with severe impacts on both the environment and human society. Understanding the post-fire recovery processes of forests is crucial for developing strategies for species diversity conservation and ecological restoration and preventing further damage. The present study proposes applying the EAswin-Mask2former model based on semantic segmentation in deep learning using visible light band data to better monitor the evolution of burn areas in forests after fires. This model is an improvement of the classical semantic segmentation model Mask2former and can better adapt to the complex environment of burned forest areas. This model employs Swin-Transformer as the backbone for feature extraction, which is particularly advantageous for processing high-resolution images. It also includes the Contextual Transformer (CoT) Block to better capture contextual information capture and incorporates the Efficient Multi-Scale Attention (EMA) Block into the Efficiently Adaptive (EA) Block to enhance the model’s ability to learn key features and long-range dependencies. The experimental results demonstrate that the EAswin-Mask2former model can achieve a mean Intersection-over-Union (mIoU) of 76.35% in segmenting complex forest burn areas across different seasons, representing improvements of 3.26 and 0.58 percentage points, respectively, over the Mask2former models using ResNet and Swin-Transformer backbones, respectively. Moreover, this method surpasses the performance of the DeepLabV3+ and Segformer models by 4.04 and 1.75 percentage points, respectively. Ultimately, the proposed model offers excellent segmentation performance for both forest and burn areas and can effectively track the evolution of burned forests when combined with unmanned aerial vehicle (UAV) remote sensing images. Full article
(This article belongs to the Section Sustainable Forestry)
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<p>Location of the study area. Source from: <a href="https://www.google.com.hk/maps/" target="_blank">https://www.google.com.hk/maps/</a>, accessed on 13 October 2024. Source from: <a href="http://www.bigemap.com/" target="_blank">http://www.bigemap.com/</a>, accessed on 13 October 2024.</p>
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<p>Image data of the same forest area.</p>
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<p>Overall architecture of Mask2former. The Pixel Decoder obtains the outputs of all stages in the feature extraction network and converts them into pixel-level prediction results, obtaining output features with multiple sizes. The largest output feature is used to calculate the mask, while the smaller output features are used as inputs to the Transformer Decoder.</p>
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<p>(<b>a</b>) Swin Transformer Network Architecture; (<b>b</b>) Swin Transformer Block Structure (right). The figure on the right shows two Swin Transformer Blocks connected in series. In network architecture, this structure appears in pairs, at least two of which are grouped together. In this structure, W-MSA represents Multi Head Self-Attention with a window, while SW-MSA represents Multi Head Self-Attention with a sliding window.</p>
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<p>(<b>a</b>) Window Multi-Head Self-Attention, W-MSA and (<b>b</b>) Shifted Window Multi-Head Self-Attention, SW-MSA.</p>
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<p>The approximate calculation process for the adaptive module EA Block. In the figure, the “+” inside a circle indicates that the inputs to that node are added together, and the “*” inside a circle indicates that the inputs are multiplied together.</p>
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<p>Structure of EAswin-Mask2former.</p>
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<p>Some segmentation results of EAswin-Mask2former and other models.</p>
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<p>Comparison of mIou between EAswin-Mask2former and other models. DLV3+, SEG, R-M, and S-M in the table represent DeepLabV3+, Segformer, Resnet50-Mask2former, and Swin-Mask2former, respectively.</p>
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<p>Satellite remote sensing images of the forest area from 2022 to 2024.</p>
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<p>Unmanned aerial vehicle images of Region A at different times and their segmentation effects. The corresponding shooting times from top to bottom are October 2022, March 2023, March 2023, and February 2024.</p>
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<p>Unmanned aerial vehicle images of Region A at different times and their segmentation effects. The corresponding shooting times from top to bottom are October 2022, March 2023, March 2023, and February 2024.</p>
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<p>The trend over time of the burned and damaged area and the proportion of forest area in Region A.</p>
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25 pages, 3441 KiB  
Review
Narrative Review: Advancing Dysbiosis Treatment in Onco-Hematology with Microbiome-Based Therapeutic Approach
by Salomé Biennier, Mathieu Fontaine, Aurore Duquenoy, Carole Schwintner, Joël Doré and Nathalie Corvaia
Microorganisms 2024, 12(11), 2256; https://doi.org/10.3390/microorganisms12112256 - 7 Nov 2024
Viewed by 529
Abstract
This review explores the complex relationship between gut dysbiosis and hematological malignancies, focusing on graft-versus-host disease (GvHD) in allogeneic hematopoietic stem cell transplantation (allo-HSCT) recipients. We discuss how alterations in microbial diversity and composition can influence disease development, progression, and treatment outcomes in [...] Read more.
This review explores the complex relationship between gut dysbiosis and hematological malignancies, focusing on graft-versus-host disease (GvHD) in allogeneic hematopoietic stem cell transplantation (allo-HSCT) recipients. We discuss how alterations in microbial diversity and composition can influence disease development, progression, and treatment outcomes in blood cancers. The mechanisms by which the gut microbiota impacts these conditions are examined, including modulation of immune responses, production of metabolites, and effects on intestinal barrier function. Recent advances in microbiome-based therapies for treating and preventing GvHD are highlighted, with emphasis on full ecosystem standardized donor-derived products. Overall, this review underscores the growing importance of microbiome research in hematology–oncology and its potential to complement existing treatments and improve outcomes for thousands of patients worldwide. Full article
(This article belongs to the Special Issue Intestinal Dysbiosis)
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<p>Illustration of the differences between gut microbiome eubiosis, imbalance, and dysbiosis.</p>
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<p>Patients’ response and outcomes after MaaT013 treatment in the HERACLES study based on Malard et al. [<a href="#B161-microorganisms-12-02256" class="html-bibr">161</a>] (<b>A</b>) Overall survival in HERACLES (<b>B</b>) Overall survival according to response to MaaT013 in HERACLES.</p>
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<p>Pooled versus mono-donor approaches in mouse model based on Reygner et al. [<a href="#B99-microorganisms-12-02256" class="html-bibr">99</a>]. <sup>1</sup> Infectious murine models; <sup>2</sup> <span class="html-italic">C. difficile</span> infectious murine model; <sup>3</sup> Two pathogens tested on murine models (<span class="html-italic">S. enterica</span> serotype Typhimurium and <span class="html-italic">C. difficile</span>) and three pathogens tested on growth inhibition assay (<span class="html-italic">C. difficile</span>, <span class="html-italic">E. faecium</span> vana and <span class="html-italic">K. pneumoniae</span> oxa48).</p>
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17 pages, 1555 KiB  
Review
The Connection Between the Oral Microbiota and the Kynurenine Pathway: Insights into Oral and Certain Systemic Disorders
by Rita Kis-György, Tamás Körtési, Alexandra Anicka and Gábor Nagy-Grócz
Curr. Issues Mol. Biol. 2024, 46(11), 12641-12657; https://doi.org/10.3390/cimb46110750 - 7 Nov 2024
Viewed by 541
Abstract
The oral microbiome, comprising bacteria, fungi, viruses, and protozoa, is essential for maintaining both oral and systemic health. This complex ecosystem includes over 700 bacterial species, such as Streptococcus mutans, which contributes to dental caries through acid production that demineralizes tooth enamel. [...] Read more.
The oral microbiome, comprising bacteria, fungi, viruses, and protozoa, is essential for maintaining both oral and systemic health. This complex ecosystem includes over 700 bacterial species, such as Streptococcus mutans, which contributes to dental caries through acid production that demineralizes tooth enamel. Fungi like Candida and pathogens such as Porphyromonas gingivalis are also significant, as they can lead to periodontal diseases through inflammation and destruction of tooth-supporting structures. Dysbiosis, or microbial imbalance, is a key factor in the development of these oral diseases. Understanding the composition and functions of the oral microbiome is vital for creating targeted therapies for these conditions. Additionally, the kynurenine pathway, which processes the amino acid tryptophan, plays a crucial role in immune regulation, neuroprotection, and inflammation. Oral bacteria can metabolize tryptophan, influencing the production of kynurenine, kynurenic acid, and quinolinic acid, thereby affecting the kynurenine system. The balance of microbial species in the oral cavity can impact tryptophan levels and its metabolites. This narrative review aims to explore the relationship between the oral microbiome, oral diseases, and the kynurenine system in relation to certain systemic diseases. Full article
(This article belongs to the Section Molecular Microbiology)
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<p>Key microbial components of the oral microbiome.</p>
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<p>Main substances of the kynurenine system. This is a schematic summary figure of the KP and potential modulation points influenced by dysbiosis. A detailed description of the KP is available in these publications [<a href="#B32-cimb-46-00750" class="html-bibr">32</a>,<a href="#B33-cimb-46-00750" class="html-bibr">33</a>]. The abbreviations represent the individual components of the kynurenine system. Abbreviations: 3-HA—3-hydroxyanthranilic acid, 3-HK—3-hydroxykynurenine, ANA—anthranilic acid, KYNA—kynurenic acid, L-KYN—L-kynurenine, NAD+—nicotinamide adenine dinucleotide, QUIN—quinolinic acid, Trp—tryptophan, XA—xanthurenic acid. the black arrows indicate the steps of the kynurenine pathway, the red arrows show the potential influences of dysbiosis on the kynurenine pathway.</p>
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<p>Periodontal diseases are strongly associated with the kynurenine pathway [<a href="#B31-cimb-46-00750" class="html-bibr">31</a>,<a href="#B50-cimb-46-00750" class="html-bibr">50</a>,<a href="#B51-cimb-46-00750" class="html-bibr">51</a>]. Abbreviations: IDO—indolamine 2,3-dioxygenase, QUIN—quinolinic acid, Trp—tryptophan.</p>
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<p>A comprehensive overview of the oral microbiome and kynurenine pathway, highlighting their contributions to the pathogenesis of various diseases.</p>
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<p>The bidirectional relationship between oral dysbiosis and the kynurenine system influences several processes that have been shown to play a role in the pathomechanism of various systemic disorders. Abbreviations: 3-HA—3-hydroxyanthranilic acid, 3-HK—3-hydroxykynurenine, ANA—anthranilic acid, KYNA—kynurenic acid, L-KYN—L-kynurenine, NAD+—nicotinamide adenine dinucleotide, QUIN—quinolinic acid, Trp—tryptophan, XA—xanthurenic acid.</p>
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14 pages, 6196 KiB  
Article
Litter and Root Removal Modulates Soil Organic Carbon and Labile Carbon Dynamics in Larch Plantation Ecosystems
by Zhenzhen Hao, Ping Li, Qilang Le, Jiaxin He and Junyong Ma
Forests 2024, 15(11), 1958; https://doi.org/10.3390/f15111958 - 7 Nov 2024
Viewed by 365
Abstract
Plant detritus plays a crucial role in regulating belowground biogeochemical processes in forest ecosystems, particularly influencing labile carbon (C) dynamics and overall soil C storage. However, the specific mechanisms by which litter and roots affect soil organic carbon (SOC) and its components in [...] Read more.
Plant detritus plays a crucial role in regulating belowground biogeochemical processes in forest ecosystems, particularly influencing labile carbon (C) dynamics and overall soil C storage. However, the specific mechanisms by which litter and roots affect soil organic carbon (SOC) and its components in plantations remain insufficiently understood. To investigate this, we conducted a detritus input and removal treatment (DIRT) experiment in a Larix principis-rupprechtii Mayr plantation in the Taiyue Mountains, China, in July 2014. The experiment comprised three treatments: root and litter retention (CK), litter removal (LR), and root and litter removal (RLR). Soil samples were collected from depths of 0–10 cm and 10–20 cm during June, August, and October 2015 to evaluate changes in soil pH, water content (SW), SOC, dissolved organic carbon (DOC), readily oxidizable organic carbon (ROC), and microbial biomass carbon (MBC). The removal of litter and roots significantly increased soil pH (p < 0.05), with pH values being 8.84% and 8.55% higher in the LR and RLR treatments, respectively, compared to CK treatment. SOC levels were significantly reduced by 26.10% and 12.47% in the LR and RLR treatments, respectively (p < 0.05). Similarly, DOC and MBC concentrations decreased following litter and root removal, with DOC content in August being 2.5 times lower than in June. Across all treatments and sampling seasons, SOC content was consistently higher in the 0–10 cm depth, exhibiting increases of 35.15% to 39.44% compared to the 10–20 cm depth (p < 0.001). Significant negative correlations were observed between SOC and the ratios of ROC/SOC, pH, DOC/SOC, and MBC/SOC (R = −0.54 to −0.37; p < 0.05). Path analysis indicated that soil pH had a significant direct negative effect on SOC (p < 0.05), with a standardized path coefficient (β) of −0.36, while ROC had a significant direct positive effect on SOC (β = 0.66, p < 0.05). Additionally, pH indirectly affected SOC by significantly influencing ROC (β = −0.69), thereby impacting SOC indirectly. Random forest analysis also confirmed that the ROC/SOC ratio plays a critical role in SOC regulation. This study reveals the complex interactions between litter and root removal and soil C dynamics in larch plantations, identifying soil pH and ROC as crucial regulator of SOC content. However, the short-term duration and focus on shallow soil depths limit our understanding of long-term impacts and deeper soil C storage. Future research should explore these aspects and consider varying climate conditions to enhance the applicability of our findings. These insights provide a scientific foundation for developing effective forest management strategies and forecasting changes in soil C storage in the context of climate change. Full article
(This article belongs to the Section Forest Ecology and Management)
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<p>(<b>a</b>) Location of the study area in China, (<b>b</b>) elevation map of the study area, and (<b>c</b>) diagram of experimental design for root and litter removal treatments. Three experimental treatments are shown: (CK) Root and Litter Retention: no removal of roots, or litter; (LR) Litter Removal: removal of surface litter, with roots left intact; (RLR) Root and Litter Removal: both roots and litter are removed. Red symbols indicating detritus removal actions.</p>
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<p>Variations in (<b>a</b>) soil pH and (<b>b</b>) soil water content (SW) across different detritus removal treatments, soil depths, and sampling months. Three treatments are shown: CK, litter and root retention; LR, litter removal; RLR, litter and root removal. Values are means ± standard error (SE). Lowercase letters indicate significant differences between treatments within the same sampling month and soil depth, while uppercase letters indicate significant differences between soil depths at the 0.05 significance level according to Tukey’s post hoc test.</p>
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<p>Variations in (<b>a</b>) soil organic carbon (SOC) concentration, (<b>b</b>) readily oxidizable organic carbon (ROC) concentration, (<b>c</b>) dissolved organic carbon (DOC) concentration, and (<b>d</b>) microbial biomass carbon (MBC) concentration across different detritus removal treatments, soil depths, and sampling months. Values are means ± SE. Treatment abbreviations and statistical significance markers follow the same format as described in <a href="#forests-15-01958-f002" class="html-fig">Figure 2</a>.</p>
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<p>(<b>a</b>) Key factors predicting SOC under different detritus removal treatments as identified by random forest models. The <span class="html-italic">y</span>-axis shows the variables contributing to SOC prediction, and the <span class="html-italic">x</span>-axis represents the percentage increase in mean squared error (%IncMSE) indicating the importance of each variable. (<b>b</b>) Pearson’s correlation analysis between influencing factors and SOC. The R<sup>2</sup> value represents the explained variation in SOC. *, ** and *** indicate the significance level at <span class="html-italic">p</span> &lt; 0.05, <span class="html-italic">p</span> &lt; 0.01, <span class="html-italic">p</span> &lt; 0.001, while ‘ns’ denotes a non-significant effect. Abbreviations refer to the above figures and tables.</p>
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<p>(<b>a</b>) Direct and indirect effects of soil pH, soil water content (SW), readily oxidizable organic carbon (ROC), dissolved organic carbon (DOC), and microbial biomass carbon (MBC) on soil organic carbon (SOC) storage, and (<b>b</b>) the standardized total effects of these variables on SOC storage. Red solid lines represent significant positive effects, and blue solid lines represent significant negative effects, while grey dashed lines represent non-significant relationships. The R<sup>2</sup> value indicates the explained variance for each variable. Numbers next to arrows indicate standardized path coefficients, with width of the arrows proportional to the standardized path coefficient. The model’s fit is assessed using AIC, Fisher’s C, and <span class="html-italic">p</span>. * 0.01 &lt; <span class="html-italic">p</span> &lt; 0.05; *** <span class="html-italic">p</span> &lt; 0.001.</p>
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18 pages, 761 KiB  
Article
Modeling Critical Success Factors for Industrial Symbiosis
by Stamatios K. Chrysikopoulos, Panos T. Chountalas, Dimitrios A. Georgakellos and Athanasios G. Lagodimos
Eng 2024, 5(4), 2902-2919; https://doi.org/10.3390/eng5040151 - 7 Nov 2024
Viewed by 382
Abstract
The critical importance of effective industrial symbiosis is emphasized in the rapidly evolving landscape of manufacturing, energy, and environmental sustainability. This study employs the Decision Making Trial and Evaluation Laboratory (DEMATEL) methodology to examine and outline the complex interrelationships among critical success factors [...] Read more.
The critical importance of effective industrial symbiosis is emphasized in the rapidly evolving landscape of manufacturing, energy, and environmental sustainability. This study employs the Decision Making Trial and Evaluation Laboratory (DEMATEL) methodology to examine and outline the complex interrelationships among critical success factors (CSFs) pivotal for the successful implementation of industrial symbiosis. Key findings indicate that leadership and technology are the most significant causal CSFs, driving positive outcomes in waste reduction, environmental impact, and economic growth, identified as primary effect factors. Leadership emerges as the predominant influence, guiding strategic alignment, fostering a collaborative and sustainable organizational culture, and affecting all other CSFs. Technological integration acts both as a direct driver of operational efficiency and as a mediator of leadership’s influence, enabling optimized resource flows and data-driven decision-making. Additional CSFs such as clear communication, enhanced training and education, and policy and regulatory support also serve as essential mediators connecting leadership to key outcomes. This research outlines an actionable pathway for stakeholders, including policymakers, engineers, and corporate executives, to strategically prioritize and utilize these CSFs to promote more resilient and sustainable industrial ecosystems. Full article
(This article belongs to the Special Issue Green Engineering for Sustainable Development 2024)
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<p>Prominence and net effect diagram.</p>
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<p>Marked causal relationships.</p>
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21 pages, 15180 KiB  
Article
Disentangling the Complex Effects of Seasonal Drought, Floor Mass, and Roots on Soil Microbial Biomass in a Subtropical Moist Forest
by Yali Yang, Xianbin Liu, Tao Li, Jinbo Gao, Yuntong Liu and Chao Wang
Forests 2024, 15(11), 1948; https://doi.org/10.3390/f15111948 - 6 Nov 2024
Viewed by 398
Abstract
Severe seasonal droughts driven by global climate change significantly alter the cycling of carbon and nutrients in forest ecosystems, while the investigation into the impacts of floor mass and plant roots on soil microbial biomass within the context of recurrent seasonal droughts is [...] Read more.
Severe seasonal droughts driven by global climate change significantly alter the cycling of carbon and nutrients in forest ecosystems, while the investigation into the impacts of floor mass and plant roots on soil microbial biomass within the context of recurrent seasonal droughts is still rare. To investigate the environmental determinants governing soil microbial biomass with the escalating severity of seasonal droughts, we conducted a study in a montane subtropical moist evergreen broad-leaved forest in southwestern China from June 2019 to May 2023. The study results revealed that soil microbial biomass, as well as soil moisture, floor mass, and plant roots, showed an apparent single-hump modal within one year. In the comparative analysis of the soil microbial biomass fluctuation amplitudes across control and watered plots, a discernible disparity was observed, indicating significant differences in microbial biomass dynamics between the respective experimental conditions. The pooled data revealed a statistically significant influence of seasonal drought, floor mass, plant roots, and their reciprocal interactions on the soil microbial biomass, highlighting these factors as pivotal determinants of microbial community dynamics. This study elucidates the interactive regulatory mechanisms by which seasonal drought, floor mass, and plant roots collectively modulate soil microbial biomass within tropical and subtropical forests, offering insights into the complex ecological processes governing microbial community dynamics. This interactive regulation might influence the trajectory of plant species and soil microbial communities, facilitating their adaptive development and evolutionary responses. Full article
(This article belongs to the Section Forest Soil)
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<p>The location of the study site (<b>left</b>) and the structure of forest ecosystem (<b>right</b>). Note: the green solid circle in the left figure labels the location of the study site; the white frame structure in the right figure is one of our experimental treatments with floor mass and plant root exclusion.</p>
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<p>The conceptual diagram of the relationships among seasonal drought, forest litter, soil, plant roots, and soil microbes in forest ecosystems [<a href="#B1-forests-15-01948" class="html-bibr">1</a>,<a href="#B10-forests-15-01948" class="html-bibr">10</a>,<a href="#B31-forests-15-01948" class="html-bibr">31</a>,<a href="#B32-forests-15-01948" class="html-bibr">32</a>,<a href="#B36-forests-15-01948" class="html-bibr">36</a>,<a href="#B37-forests-15-01948" class="html-bibr">37</a>]. Note: the yellow arrow signifies a unidirectional influence, denoting a single flow of action, whereas the black arrow indicates a bidirectional exchange, depicting a reciprocal and interactive process.</p>
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<p>The monthly dynamics of soil moisture in four experimental subplots of the two field plots (control vs. watered): (<b>a</b>) R+F+ subplot, (<b>b</b>) R+F− subplot, (<b>c</b>) R−F+ subplot, and (<b>d</b>) R−F− subplot. Note: the bar represents ±SE.</p>
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<p>The monthly dynamics of floor mass in two experimental subplots of the two field plots (control vs. watered): (<b>a</b>) R+F+ subplot and (<b>b</b>) R−F+ subplot. Note: the bar represents ±SE.</p>
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<p>The monthly dynamics of plant roots in two experimental subplots of the two field plots (control vs. watered): (<b>a</b>) R+F+ subplot and (<b>b</b>) R+F− subplot. Note: the bar represents ±SE.</p>
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<p>The monthly dynamics of soil MBC in four experimental subplots of the two field plots (control vs. watered): (<b>a</b>) R+F+ subplot, (<b>b</b>) R+F− subplot, (<b>c</b>) R−F+ subplot, and (<b>d</b>) R−F− subplot. Note: the bar represents ±SE.</p>
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<p>The monthly dynamics of soil MBC in four experimental subplots of the two field plots (control vs. watered): (<b>a</b>) R+F+ subplot, (<b>b</b>) R+F− subplot, (<b>c</b>) R−F+ subplot, and (<b>d</b>) R−F− subplot. Note: the bar represents ±SE.</p>
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<p>The monthly dynamics of soil MBN in four experimental subplots of the two field plots (control vs. watered): (<b>a</b>) R+F+ subplot, (<b>b</b>) R+F− subplot, (<b>c</b>) R−F+ subplot, and (<b>d</b>) R−F− subplot. Note: the bar represents ±SE.</p>
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<p>The linear relationships of soil moisture with soil MBC and MBN in four experimental subplots of the two field plots (control vs. watered): soil MBC (<b>a</b>) and soil MBN (<b>b</b>) in the R+F+ subplot; soil MBC (<b>c</b>) and soil MBN (<b>d</b>) in the R+F− subplot; soil MBC (<b>e</b>) and soil MBN (<b>f</b>) in the R−F+ subplot; and soil MBC (<b>g</b>) and soil MBN (<b>h</b>) in the R−F− subplot.</p>
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<p>The linear relationships of soil moisture with soil MBC and MBN in four experimental subplots of the two field plots (control vs. watered): soil MBC (<b>a</b>) and soil MBN (<b>b</b>) in the R+F+ subplot; soil MBC (<b>c</b>) and soil MBN (<b>d</b>) in the R+F− subplot; soil MBC (<b>e</b>) and soil MBN (<b>f</b>) in the R−F+ subplot; and soil MBC (<b>g</b>) and soil MBN (<b>h</b>) in the R−F− subplot.</p>
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<p>The linear relationships of floor mass with soil MBC and MBN in two experimental subplots of the two field plots (control vs. watered): soil MBC (<b>a</b>) and soil MBN (<b>b</b>) in the R+F+ subplot and soil MBC (<b>c</b>) and soil MBN (<b>d</b>) in the R−F+ subplot.</p>
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<p>The linear relationships of plant roots with soil MBC and MBN in two experimental subplots of the two field plots (control vs. watered): soil MBC (<b>a</b>) and soil MBN (<b>b</b>) in the R+F+ subplot and soil MBC (<b>c</b>) and soil MBN (<b>d</b>) in the R+F– subplot.</p>
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<p>The linear relationships of plant roots with soil MBC and MBN in two experimental subplots of the two field plots (control vs. watered): soil MBC (<b>a</b>) and soil MBN (<b>b</b>) in the R+F+ subplot and soil MBC (<b>c</b>) and soil MBN (<b>d</b>) in the R+F– subplot.</p>
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<p>Soil MBC and MBN respectively in correspondence to soil moisture and floor mass (<b>a</b>,<b>b</b>), soil moisture and plant roots (<b>c</b>,<b>d</b>), and floor mass and plant roots (<b>e</b>,<b>f</b>) in the R+F+ subplot of the control plot.</p>
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23 pages, 5513 KiB  
Article
Integrated Chemical and Ecotoxicological Assessment of Metal Contamination in the Andong Watershed: Identifying Key Toxicants and Ecological Risks
by Jiwoong Chung, Su-Hyun Kim, Dae-sik Hwang, Chan-Gyoung Sung, Seong-Dae Moon, Chankook Kim, Mansik Choi and Jong-Hyeon Lee
Water 2024, 16(22), 3176; https://doi.org/10.3390/w16223176 - 6 Nov 2024
Viewed by 474
Abstract
This study employed an integrated field monitoring approach, combining chemical analysis and ecotoxicity testing of multiple environmental matrices—water, sediment, and sediment elutriates—to comprehensively assess the environmental health of the Andong watershed, located near a Zn smelter and mining area. The primary objectives were [...] Read more.
This study employed an integrated field monitoring approach, combining chemical analysis and ecotoxicity testing of multiple environmental matrices—water, sediment, and sediment elutriates—to comprehensively assess the environmental health of the Andong watershed, located near a Zn smelter and mining area. The primary objectives were to evaluate the extent of metal contamination, identify key toxicants contributing to ecological degradation, and trace the sources of these pollutants. Our findings revealed severe metal contamination and significant ecotoxicological effects both in proximity to and downstream from industrial sites. Specifically, Cd, Zn, and Pb were strongly linked to the smelter, while Hg, Ni, Cu, and As were predominantly associated with mining activities in the tributaries. To further assess toxicity of field-collected sediment and their elutriates, a logistic regression analysis was employed to estimate benchmark values for distinguishing between toxic and non-toxic samples, using the sum of toxic units for sediment elutriates and the mean probable effect level (PEL) quotient for sediment toxicity. These models demonstrated greater predictive accuracy than conventional benchmarks for determining toxicity thresholds. Our results highlight that integrating chemical and ecotoxicological monitoring with site-specific concentration–response relationships enhances the precision of ecological risk assessments, facilitating more accurate identification of key toxicants driving mixture toxicity in complex, pollution-impacted aquatic ecosystems. Full article
(This article belongs to the Section Water Quality and Contamination)
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Figure 1

Figure 1
<p>Location map of sampling stations. The left panels show the location of the Nakdong River, situated upstream of Andong Lake. The right panels depict the location of Andong Lake. Panels (<b>A</b>,<b>B</b>) indicate the sampling stations for water bodies: gray circles represent surface water sampling sites in the main stream, and white circles represent surface water sampling sites in tributaries. Panels (<b>C</b>,<b>D</b>) show the sampling stations for surface sediments.</p>
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<p>Variation in the sum of the hazard quotient (HQ) values for eight metals in the surface water as a function of distance from the zinc smelter, along with the contribution of each metal to the total HQ. Andong Lake is located approximately 90 km downstream from the smelter, with the Nakdong River flowing into the lake from upstream.</p>
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<p>Variation in the HQ (hazard quotient) for the individual metals in the surface water according to the distance from the Zn smelter.</p>
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<p>Variation in the mean probable effect level quotient (PELq) for heavy metals in sediments as a function of the distance from the zinc smelter, along with the contribution of each metal to the mean PELq. Andong Lake is located approximately 90 km downstream from the zinc smelter, with the Nakdong River flowing into the lake from upstream.</p>
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<p>Variation in the probable effect level quotient (PELq) of individual metals in sediments as a function of the distance from the Zn smelter.</p>
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<p>The location map showing the sites of the samples with confirmed ecotoxic effects. The left panels (<b>A</b>,<b>C</b>) are the location map of the Nakdong River located upstream of Andong Lake. The right panels (<b>B</b>,<b>D</b>) are the location map of Andong Lake. The upper panels (<b>A</b>,<b>B</b>) show the acute toxic effects of sediments on the amphipod (<span class="html-italic">Hyalella azteca</span>) and the midge (<span class="html-italic">Chironomus riparius</span>). The lower panels (<b>C</b>,<b>D</b>) show the chronic toxic effects of sediment elutriates on the crustacean (<span class="html-italic">Daphnia magna</span>) and fish (<span class="html-italic">Oncorhynchus mykiss</span>). The red semicircles are sediment samples showing toxic effects (toxic effects exceeding 20%). The green semicircles are sediment samples that show no toxic effects (toxic effects less than 20%).</p>
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<p>Variation in the sum of toxic units (<math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">Σ</mi> <mi>T</mi> <mi>U</mi> </mrow> </semantics></math>) for heavy metals in sediment elutriates as a function of the distance from the zinc smelter, along with the contribution of each metal to the total <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">Σ</mi> <mi>T</mi> <mi>U</mi> </mrow> </semantics></math>. Andong Lake is located approximately 90 km downstream from the zinc smelter, with the Nakdong River situated between the smelter and the lake.</p>
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<p>Results of logistic regression analysis for sediment toxicity tests using field-collected samples and the contribution of individual heavy metals to the mean probable effect level quotient (PELq). The upper panels illustrate the comparison between the probability of sediment toxicity and the mean PELq. The lower panels show the contribution of each metal to the mean PELq in sediment samples where toxicity was confirmed for test species <span class="html-italic">Hyalella azteca</span> and <span class="html-italic">Chironomus riparius</span>.</p>
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<p>Results of logistic regression analysis for sediment elutriate toxicity tests using field-collected samples and the contribution of individual heavy metals to the sum of toxic units (<math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">Σ</mi> <mi>T</mi> <mi>U</mi> </mrow> </semantics></math>). The upper panels present the comparison between the probability of sediment elutriate toxicity and the <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">Σ</mi> <mi>T</mi> <mi>U</mi> </mrow> </semantics></math>. The lower panels illustrate the contribution of each metal to the <math display="inline"><semantics> <mrow> <mi>S</mi> <mi>i</mi> <mi>g</mi> <mi>m</mi> <mi>a</mi> <mi>T</mi> <mi>U</mi> </mrow> </semantics></math> in sediment elutriate samples where ecotoxicity was confirmed for test species <span class="html-italic">Daphnia magna</span> and <span class="html-italic">Oncorhynchus mykiss</span>.</p>
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<p>Comparison of water quality variables with the predicted no-effect concentrations (PNECs) for each metal in the surface waters, as derived from the bioavailability models. The PNECs for copper, nickel, and zinc were calculated using the biotic ligand model, while the PNECs for cadmium and lead were determined using hardness-based equations.</p>
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<p>Results of the logistic regression analysis showing the relationship between the probable effect level quotient (PELq) of the individual metals and the probability of acute mortality in <span class="html-italic">Hyalella azteca</span>.</p>
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<p>Results of the logistic regression analysis showing the relationship between the probable effect level quotient (PELq) of the individual metals and the probability of acute mortality in <span class="html-italic">Chironomus riparius</span>.</p>
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<p>Results of the logistic regression analysis showing the relationship between the probable effect level quotient (PELq) of the individual metals and the probability of reproduction inhibition in <span class="html-italic">Daphnia magna</span> and growth inhibition in <span class="html-italic">Oncorhynchus mykiss</span>.</p>
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22 pages, 6361 KiB  
Article
Topography Dominates the Spatial and Temporal Variability of Soil Bulk Density in Typical Arid Zones
by Jia Guo, Yanmin Fan, Yunhao Li, Yanan Bi, Shuaishuai Wang, Yutong Hu, Li Zhang and Wenyue Song
Sustainability 2024, 16(22), 9670; https://doi.org/10.3390/su16229670 - 6 Nov 2024
Viewed by 444
Abstract
Soil bulk density is a crucial indicator for assessing soil matter storage and soil quality. Due to the complexity of sampling soil bulk density, particularly in deeper layers, it is essential to study the spatial distribution patterns of soil bulk density and their [...] Read more.
Soil bulk density is a crucial indicator for assessing soil matter storage and soil quality. Due to the complexity of sampling soil bulk density, particularly in deeper layers, it is essential to study the spatial distribution patterns of soil bulk density and their influencing factors. To address the gap in large-scale studies of vertical (from surface to deeper layers) and horizontal (across a broad area) variations in soil bulk density in arid regions, this study focuses on Changji Prefecture, located in the central northern slope of the Tianshan Mountains and characterized by typical vertical zonation. By integrating classical statistics, geostatistics, and geographic information systems (GISs), this study investigates the spatial distribution patterns and driving factors of soil bulk density. The results indicate that soil bulk density in Changji Prefecture increases with soil depth, with significantly lower values in the surface layer than in deeper layers. Spatially, despite minimal variation in latitude, there is considerable elevation difference within the study area, with the lowest elevations in the central region. Soil bulk density exhibits a spatial distribution pattern of higher values in the northeast (desert areas) and lower values in the southwest (forest areas). The nugget effect in the surface layer (0–20 cm) is substantial at 44.9%, while the deeper layers (20–100 cm) show nugget effects below 25%, suggesting that the influence of both natural and anthropogenic factors on deep soil bulk density is limited and mainly affects the surface layer. Stepwise regression analysis indicates that among topographic factors, slope and elevation are the primary controls of spatial variability in soil bulk density across layers. This research demonstrates that, in arid regions, soil bulk density is influenced primarily by natural factors, with limited impact from human activities. These findings provide valuable data support and theoretical guidance for soil management, agricultural planning, and sustainable ecosystem development in arid regions. Full article
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<p>Maps for the location of the study area and distribution of sampling sites.</p>
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<p>Box maps of soil bulk density in different soil layers.</p>
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<p>Semi-variance maps for soil bulk density in the 0–20 cm (<b>a</b>), 20–40 cm (<b>b</b>), 40–60 cm (<b>c</b>), 60–80 cm (<b>d</b>) and 80–100 cm (<b>e</b>) layers in Changji prefecture. The boxfigure in the picture is the fitting parameter.</p>
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<p>Spatial distribution map of soil bulk density in 0–20 cm (<b>a</b>), 20–40 cm (<b>b</b>), 40–60 cm (<b>c</b>), 60–80 cm (<b>d</b>), and 80–100 cm (<b>e</b>) soil layers.</p>
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<p>Slope grading map (<b>a</b>). Elevation grading chart (<b>b</b>). Slope grade diagram (<b>c</b>). The black dots in the figure are sampling points.</p>
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<p>Relationship between soil bulk density and soil depth (<b>a</b>); the difference in soil bulk density in different soil layers under different slopes (<b>b</b>). Different capital letters indicated significant differences in slope type (<span class="html-italic">p</span> &lt; 0.05). Different lowercase letters indicate significant differences between different soil layers (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>The relationship between soil bulk density and soil depth (<b>a</b>); the difference in soil bulk density in different soil layers of shade slope and sunny slope (<b>b</b>). Different capital letters indicate significant differences in slope type (<span class="html-italic">p</span> &lt; 0.05). Different lowercase letters indicate significant differences between different soil layers (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>The relationship between soil bulk density and soil depth (<b>a</b>); the difference in soil bulk density in different soil layers under different elevation classifications (<b>b</b>). Different capital letters indicate significant differences in elevation type (<span class="html-italic">p</span> &lt; 0.05). Different lowercase letters indicate significant differences between different soil layers (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>Soil bulk density of zonal soil and non-zonal soil in different soil layers. Different capital letters indicate significant differences in soil type (<span class="html-italic">p</span> &lt; 0.05). Different lowercase letters indicate significant differences between different soil layers (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>Soil bulk density of cultivated land and non-cultivated land in different soil layers under zonal soil type (<b>a</b>); soil bulk density in different soil layers of cultivated land and non-cultivated land under non-zonal soil types (<b>b</b>). Different capital letters indicate significant differences in soil type (<span class="html-italic">p</span> &lt; 0.05). Different lowercase letters indicate significant differences between different soil layers (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>Relationship between soil bulk density and soil depth (<b>a</b>); the difference in soil bulk density in different soil layers under different land use types (<b>b</b>). Different capital letters indicate significant differences in different land use types (<span class="html-italic">p</span> &lt; 0.05). Different lowercase letters indicate significant differences between different soil layers (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>Annual average temperature and precipitation in Changji Prefecture (<b>a</b>) Annual average temperature in 2023; (<b>b</b>) Annual average precipitation map for 2023, with black points as sampling points.</p>
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