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Search Results (444)

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19 pages, 8454 KiB  
Article
Analysis of Vegetation Changes and Driving Factors on the Qinghai-Tibet Plateau from 2000 to 2022
by Xiaoqi Ren, Peng Hou, Yutiao Ma, Rongfei Ma, Jiahao Wang and Le Xie
Forests 2024, 15(12), 2188; https://doi.org/10.3390/f15122188 - 12 Dec 2024
Viewed by 231
Abstract
This study assesses the impact of climate change and human activities on vegetation dynamics (kNDVI) on the Qinghai-Tibet Plateau (QTP) between 2000 and 2022, considering both lag and cumulative effects. Given the QTP’s high sensitivity to climate change and human activities, it is [...] Read more.
This study assesses the impact of climate change and human activities on vegetation dynamics (kNDVI) on the Qinghai-Tibet Plateau (QTP) between 2000 and 2022, considering both lag and cumulative effects. Given the QTP’s high sensitivity to climate change and human activities, it is imperative to understand their effects on vegetation for the sustainable development of regional and national terrestrial ecosystems. Using MOD13Q1 NDVI and climate and human activity data, we applied methods such as Sen-MK, lag and cumulative effect analysis, improved residual analysis, and geographical detector analysis. The outcomes were as follows. (1) The vegetation kNDVI on the QTP showed an overall fluctuating growth trend between 2000 and 2022; improved regions were more significant than degraded regions, with improved regions primarily distributed in humid and semi-humid areas with favorable climate conditions, and degraded regions primarily in arid and semi-arid areas; this implies that climate conditions have a significant impact on vegetation changes on the QTP. (2) The analysis of lag and cumulative effects revealed that temperature and precipitation have a substantial cumulative effect on vegetation kNDVI on the QTP. The vegetation kNDVI showed a lag effect of 0 months and a cumulative effect of 1 month for temperature, and a lag effect of 0 months and a cumulative effect of 2 months for precipitation, respectively. (3) Improved residual analysis based on lag and cumulative effects revealed that human activities positively contributed 66% to the changes in vegetation kNDVI on the QTP, suggesting a notable positive impact of human activities. Geographical detector analysis indicated that, among different human activity factors affecting vegetation kNDVI changes, the explanatory power in 2005 and 2015 ranked as X3 (livestock density) > X1 (population density) > X2 (per capita GDP) > X4 (artificial afforestation density) > X5 (land use type), and in 2020, as X3 > X4 > X1 > X5 > X2. The explanatory power of afforestation density and land use type has relatively increased, indicating that recent efforts in ecological protection and restoration on the QTP, including developing artificial forest areas and afforestation programs, have considerably contributed to vegetation greening. Full article
(This article belongs to the Special Issue Application of Remote Sensing in Vegetation Dynamic and Ecology)
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<p>Overview map of the study area.</p>
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<p>Temporal trends in kNDVI.</p>
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<p>Spatial variation trends of kNDVI.</p>
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<p>Spatial variation trends of kNDVI for different vegetation types.</p>
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<p>Relationship between temperature, precipitation, and kNDVI temporal changes.</p>
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<p>Lagged and accumulative effects of temperature and precipitation on vegetation kNDVI.</p>
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<p>Proportions of lagged and accumulative effects of temperature and precipitation on vegetation kNDVI.</p>
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<p>Temperature lagged and cumulative impacts across various vegetation types.</p>
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<p>Precipitation lagged and cumulative impacts across various vegetation types.</p>
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<p>Distribution of driving factors results.</p>
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<p>Contributions of climate change and human activities to vegetation dynamics.</p>
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<p>Single factor detection results.</p>
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<p>(<b>a</b>–<b>d</b>) Pearson correlation coefficient between (<b>a</b>) kNDVI and temperature, (<b>b</b>) kNDVI and precipitation, (<b>c</b>) NDVI and temperature, and (<b>d</b>) NDVI and precipitation.</p>
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<p>Spatial variation trends of NDVI.</p>
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14 pages, 8299 KiB  
Article
Hydrochemical Characteristics and Genesis of Sand–Gravel Brine Deposits in the Mahai Basin of the Northern Qinghai–Tibetan Plateau
by Hongkui Bai, Tong Pan, Guang Han, Qishun Fan, Qing Miao and Haiyi Bu
Water 2024, 16(24), 3562; https://doi.org/10.3390/w16243562 - 11 Dec 2024
Viewed by 330
Abstract
The sand–gravel brine deposit in the Mahai Basin is a newly discovered large-scale potassium–bearing brine deposit. The potassium–bearing brine is primarily found at depths exceeding 150 m within the porous alluvial and fluvial sand–gravel reservoir of the Middle to Lower Pleistocene. This deposit [...] Read more.
The sand–gravel brine deposit in the Mahai Basin is a newly discovered large-scale potassium–bearing brine deposit. The potassium–bearing brine is primarily found at depths exceeding 150 m within the porous alluvial and fluvial sand–gravel reservoir of the Middle to Lower Pleistocene. This deposit is characterized by a relatively shallow water table, moderate–to–strong aquifer productivity, high salinity, and a KCl content that meets the conditions for exploitation, with the advantage of reduced salt crystallization during well mining, making it a potential reserve base for potash development. A geochemical analysis of the sand–gravel brine revealed consistent trends for the major ions K+, Na+, Mg2+, Cl, and SO42− along the east–west axis of the alluvial fan, while Ca2+ showed an opposite trend compared to Mg2+. Along the exploration lines from north to south, the concentrations of the main ions gradually increase. The brine is enriched in Na+ and Cl ions, while SO42− and HCO3 are depleted. In the K+-Na+-Mg2+/Cl-H2O (25 °C) quaternary phase diagram, the brine falls within the halite stability field, with the hydrochemical type classified as chloride type. The brine coefficient characteristics indicate a multi-source origin involving residual evaporation, salt rock leaching, and metamorphic sedimentary brine. Comparison studies of the ionic composition and isotopic signatures (δD, δ18O, δ37Cl, and δ7Li) of deep sand–gravel brines in the study area with interstitial and confined brines in the southern depression suggest similar geochemical characteristics between them. The genetic analysis of the deposit proposes that during the basin tectonic evolution, the potassium-rich interstitial and confined brines originally located in the southern depression of the Mahai Basin were displaced under compressional forces and migrated northward as the depositional center shifted, eventually backfilling into the loose alluvial and fluvial sand and gravel reservoirs at the front of the Saishiteng Mountains, forming the deep sand–gravel brine deposits in the foreland. Full article
(This article belongs to the Section Hydrogeology)
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<p>Geological and hydrologic settings and sampling locations in MHB: (<b>a</b>) the location of Qaidam Basin; (<b>b</b>) distribution map of MHB and sampling sites; (<b>c</b>) precipitation of Q<sub>1</sub><sup>p</sup> to Q<sub>4</sub><sup>h</sup> salt minerals in MHB; and (<b>d</b>) stratigraphic and lithological distribution of MHB and its surrounding area.</p>
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<p>Geological–hydrogeological vertical profile map of the study area.</p>
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<p>Vertical variation curve of major ion content in deep sand–gravel brine of the Mahai Basin.</p>
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<p>K<sup>+</sup>, Na<sup>+</sup>, and Mg<sup>2+</sup>/Cl<sup>−</sup>-H<sub>2</sub>O system (25 °C stability phase diagram).</p>
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<p>Evolution schematic diagram of salt lakes in the Mahai Basin: (<b>a</b>) deep lake, shallow lake, and lacustrine environments in the Mahai area before the Neogene; (<b>b</b>) the Saishiteng Mountain Front Fault, Lenghu Fault, and other thrust faults in the Mahai Basin gradually formed; (<b>c</b>) from the end of the Pliocene to the end of the Middle Pleistocene, with the uplift of the Lenghu Anticline, the Mahai Basin became separated and enclosed from the ancient Qaidam Lake; (<b>d</b>) controlled by tectonic movements and landforms, the sedimentary center, i.e., the lake, shrank and migrated eastward, forming the Mahai Salt Lake in a depression close to the recharge source.</p>
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<p>Hydrogen and oxygen isotopes of brines and surrounding water in the Mahai Basin. Data source: Yuqia River water and snowmelt water from [<a href="#B29-water-16-03562" class="html-bibr">29</a>]; lake water from [<a href="#B4-water-16-03562" class="html-bibr">4</a>]; inter-brine (intercrystalline brine) from [<a href="#B12-water-16-03562" class="html-bibr">12</a>,<a href="#B30-water-16-03562" class="html-bibr">30</a>]; confined brines (dark blue triangle) from [<a href="#B15-water-16-03562" class="html-bibr">15</a>]; confined brines (light blue triangle) from [<a href="#B12-water-16-03562" class="html-bibr">12</a>]; sand–gravel brines (red triangle) from [<a href="#B11-water-16-03562" class="html-bibr">11</a>]; sand–gravel brines (green triangle) from [<a href="#B7-water-16-03562" class="html-bibr">7</a>]; oilfield waters from [<a href="#B9-water-16-03562" class="html-bibr">9</a>]; and inter-brine (intercrystalline; hollow blue triangle) from [<a href="#B17-water-16-03562" class="html-bibr">17</a>]. WQB: the western Qaidam Basin (including Dalangtan Basin, Heibei Basin, Chahansilatu Basin, Kunteyi Basin, and Mahai basin); MH: Mahai Basin; LH: Lenghu; KTY: Kunteyi Basin. GMWL: global meteoric water line (GMWL, δD = 8 × δ<sup>18</sup>O + 10) [<a href="#B4-water-16-03562" class="html-bibr">4</a>,<a href="#B30-water-16-03562" class="html-bibr">30</a>]; LEL: the evaporation line of Qaidam Basin (LEL, δD = 5 × δ<sup>18</sup>O − 25) [<a href="#B7-water-16-03562" class="html-bibr">7</a>]; LMWL: local meteoric water line (LMWL, δD = 7.6 × δ<sup>18</sup>O + 2.6) [<a href="#B31-water-16-03562" class="html-bibr">31</a>].</p>
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20 pages, 28685 KiB  
Article
Dynamic Response of Vegetation Net Primary Productivity to Climate and Human Impacts in Mining-Dominated Basin in Inner Mongolia, China
by Ye Yang, Guilan Li, Yidi Wang, Lijie Wu, Kaifang Ding, Shilu Xing, Yilong Zhang and Luxing Zhang
Atmosphere 2024, 15(12), 1457; https://doi.org/10.3390/atmos15121457 - 5 Dec 2024
Viewed by 406
Abstract
The net primary productivity (NPP) of vegetation is the key indicator for assessing ecosystem productivity and carbon cycling. The Ulan Mulun River Basin (UMRB) in Northwest China is a typical coal mining area, including open-pit mining (OPM) and underground coal mining (UGM). There [...] Read more.
The net primary productivity (NPP) of vegetation is the key indicator for assessing ecosystem productivity and carbon cycling. The Ulan Mulun River Basin (UMRB) in Northwest China is a typical coal mining area, including open-pit mining (OPM) and underground coal mining (UGM). There are limited studies utilizing long-term, high-resolution data to investigate the spatiotemporal and driving mechanisms of NPP in different types of mining and non-coal mining (NCM) areas. In this study, NPP was estimated using high-resolution Landsat data (30 m) and an improved CASA model for the period 1987–2022. The spatiotemporal variations in NPP across the basin were systematically investigated using Theil–Sen–MK trend analysis, partial derivatives, and multivariate regression residual to explore and quantify the impacts of climate variability (CV) and human activities (HAs) on the different coal mining and NCM areas. The research results show that the overall fluctuating upward trend of vegetation cover in the country is 64.84% during the period from 1987 to 2022. However, there is a decreasing trend of NPP in the coal mining areas. Precipitation was the major factor influencing the change in NPP (21.835 gC/m2/a), while HAs had a lesser effect (4.667 gC/m2/a). In addition, UGM and NCM were more positively affected by HAs than OPM, while OPM was more positively affected by CV than UGM and NCM. These findings can guide scientific ecological restoration strategies, assess carbon balance impacts, and optimize land management and planning in mining areas to achieve a balance between resource development and environmental protection. Full article
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<p>Research map includes (<b>a</b>) location of UMRB within China, (<b>b</b>) elevations and administrative divisions, (<b>c</b>) location within Inner Mongolia, (<b>d</b>) and distribution of coal mines.</p>
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<p>A diagram of the technical pathway.</p>
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<p>Comparison of estimated NPP to MOD17A3HGF NPP: (<b>a</b>) comparison in 2005, (<b>b</b>) comparison in 2011, (<b>c</b>) comparison in 2016, (<b>d</b>) and comparison in 2022.</p>
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<p>Temporal changes in annual average NPP.</p>
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<p>The spatial distribution of NPP trends in the UMRB, 1987–2022. S<sub>npp</sub> stands for the Sen slope of NPP, and |Z| is an indicator of the statistical test.</p>
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<p>Spatial distribution characteristics of annual NPP in UMRB from 1987 to 2022.</p>
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<p>Interannual variations in mean temperature (<b>a</b>), cumulative precipitation (<b>b</b>), and radiation (<b>c</b>) in UMRB from 1987 to 2022.</p>
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<p>Relative contributions of CV and HAs to NPP.</p>
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<p>Contributions of CV and HAs to NPP changes in different areas of UMRB from 1987 to 2022.</p>
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<p>Contributions of temperature (<b>a</b>), precipitation (<b>b</b>), and solar radiation (<b>c</b>) to NPP changes in UMRB. Area proportions of positive and negative effects for each influencing factor (<b>d</b>).</p>
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<p>Contributions of CV (<b>a</b>) and HAs (<b>b</b>) to NPP changes in UMRB.</p>
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<p>Dominant factor zoning of NPP changes in UMRB from 1987 to 2022.</p>
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24 pages, 4915 KiB  
Article
Spatio-Temporal Heterogeneity of Ecological Quality in a Typical Dryland of Northern China Driven by Climate Change and Human Activities
by Shuai Li, Junliang Gao, Pu Guo, Ge Zhang, Yu Ren, Qi Lu, Qinwen Bai and Jiahua Lu
Plants 2024, 13(23), 3341; https://doi.org/10.3390/plants13233341 - 28 Nov 2024
Viewed by 388
Abstract
With the intensification of climate change and anthropogenic impacts, the ecological environment in drylands faces serious challenges, underscoring the necessity for regionally adapted ecological quality evaluation. This study evaluates the suitability of the original Remote Sensing Ecological Index (oRSEI), modified RSEI (mRSEI), and [...] Read more.
With the intensification of climate change and anthropogenic impacts, the ecological environment in drylands faces serious challenges, underscoring the necessity for regionally adapted ecological quality evaluation. This study evaluates the suitability of the original Remote Sensing Ecological Index (oRSEI), modified RSEI (mRSEI), and adapted RSEI (aRSEI) in a typical dryland region of northern China. Spatio-temporal changes in ecological quality from 2000 to 2022 were analyzed using Theil–Sen median trend analysis, the Mann–Kendall test, and the Hurst exponent. Multiple regression residual analysis quantified the relative contributions of climate change and human activities to ecological quality changes. Results showed that (1) the aRSEI was the most suitable index for the study area; (2) observed changes exhibited significant spatial heterogeneity, with improvements generally in the inner areas of the Yellow River and declines in the outer areas; and (3) changes in ecological quality were primarily driven by climate change and human activities, with human activities dominating from 2000 to 2011 and the influence of climate change increasing from 2012 to 2022. This study compares the efficacy of RSEIs in evaluating dryland ecological quality, identifies spatio-temporal change patterns, and elucidates driving mechanisms, offering scientific evidence and policy recommendations for targeted conservation and restoration measures to address future changes in dryland regions. Full article
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<p>Spatial distribution of and differences in three indices in 2022. (<b>a</b>–<b>c</b>): Spatial distribution of the oRSEI, aRSEI, and mRSEI, respectively. (<b>d</b>) Spatial differences between the oRSEI and aRSEI. (<b>e</b>) Spatial differences between the oRSEI and mRSEI. Note: SL: significantly low; OL: obviously low; LL: slightly low; NC: no change; LH: slightly high; OH: obviously high; SH: significantly high.</p>
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<p>Violin plots of oRSEI, aRSEI, and mRSEI from 2000 to 2022.</p>
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<p>The distribution (<b>a</b>) and classification (<b>b</b>) of ecological quality in the study area in 2022.</p>
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<p>Changes in (<b>a</b>) and area transition matrix of (<b>b</b>) ecological quality levels from 2000 to 2022.</p>
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<p>Time series trend of ecological quality, Mann–Kendall significance test, and Mann–Kendall mutation test in the significant-change area. (<b>a</b>) Theil–Sen median trend analysis from 2000 to 2022. (<b>b</b>) Theil–Sen median trend analysis and Mann–Kendall significant test from 2000 to 2022. (<b>c</b>) Mann–Kendall mutation test in the significant-improvement areas. (<b>d</b>) Mann–Kendall mutation test in the significant-decline areas. Note: UF: forward trend statistical value; UB: backward trend statistical value.</p>
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<p>Hurst exponent (<b>a</b>) and future trends (<b>b</b>) in the study area. Note: CD: continuous decline, ITD: improvement to decline, ST: stable, DTI: decline to improvement, CI: continuous improvement, UN: uncertain.</p>
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<p>Spatial distribution of climate change and human activity contributions to ecological quality change in significant-change areas. (<b>a</b>) Climate change contribution in the significant-improvement areas. (<b>b</b>) Human activity contribution in the significant-improvement areas. (<b>c</b>) Climate change contribution in the significant-decline areas. (<b>d</b>) Human activity contribution in the significant-decline areas.</p>
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<p>Spatial pattern of and changes in climate factors. (<b>a</b>) Spatial pattern of annual precipitation. (<b>b</b>) Spatial pattern of annual mean temperature. (<b>c</b>,<b>d</b>) Changes in annual precipitation, annual mean temperature, and potential evapotranspiration.</p>
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<p>Overview of the study area. (<b>a</b>) Location of the study area. (<b>b</b>) ArcGIS online map (World Imagery). (<b>c</b>) Land use map in 2020 (GlobeLand30).</p>
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<p>Technical workflow.</p>
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15 pages, 5509 KiB  
Article
Multimodal Video Analysis for Crowd Anomaly Detection Using Open Access Tourism Cameras
by Alejandro Dionis-Ros, Joan Vila-Francés, Rafael Magdalena-Benedito, Fernando Mateo and Antonio J. Serrano-López
Appl. Sci. 2024, 14(23), 11075; https://doi.org/10.3390/app142311075 - 28 Nov 2024
Viewed by 391
Abstract
In this article, we propose the detection of crowd anomalies through the extraction of information in the form of time series in video format using a multimodal approach. Through pattern recognition algorithms and segmentation, informative measures of the number of people and image [...] Read more.
In this article, we propose the detection of crowd anomalies through the extraction of information in the form of time series in video format using a multimodal approach. Through pattern recognition algorithms and segmentation, informative measures of the number of people and image occupancy are extracted at regular intervals, which are then analyzed to obtain trends and anomalous behaviors. Specifically, through temporal decomposition and residual analysis, intervals or specific situations of unusual behaviors are identified, which can be used in decision-making and the improvement of actions in sectors related to human movement such as tourism or security. This methodology introduces a novel, privacy-focused approach by analyzing anonymized metrics rather than tracking or recognizing individuals, setting a new standard for ethical crowd monitoring. Applied to the webcam of Turisme Comunitat Valenciana in the town of Morella (Comunitat Valenciana, Spain), this approach has shown excellent results, correctly detecting specific anomalous situations and unusual overall increases during the previous weekend and during the October 2023 festivities. These results have been obtained while preserving the confidentiality of individuals at all times by using measures that maximize anonymity, without trajectory recording or person recognition. Full article
(This article belongs to the Special Issue Advanced Image Analysis and Processing Technologies and Applications)
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<p>Original and background frames shown before and after applying CLAHE processing and grayscale transformation.</p>
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<p>SSIM comparison results. (<b>a</b>) Displays detections provided by Yolo. (<b>b</b>) Shows various cutouts from the background frame corresponding to examples of a false positive, a false negative, and a true positive, respectively. (<b>c</b>) Presents cutouts from the original frame representing examples of a false positive, a false negative, and a true positive, respectively.</p>
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<p>Weekly distribution of median detection series. <span class="html-italic">X</span>-axis in intervals of 15 min.</p>
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<p>Weekly distribution of IQR detection series. <span class="html-italic">X</span>-axis in intervals of 15 min.</p>
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<p>Augmented detection series.</p>
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<p>Weekly distribution of the median of the heatmap series. <span class="html-italic">X</span>-axis in intervals of 15 min.</p>
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<p>Weekly distribution of the standard deviation of the heatmap series. <span class="html-italic">X</span>-axis in intervals of 15 min.</p>
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<p>Augmented heatmap saturation percentage series.</p>
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<p>Diagram of the employed methodology.</p>
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<p>STL decomposition of the detection series.</p>
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<p>STL decomposition of the heatmap saturation percentage series.</p>
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<p>Trend threshold in detection series.</p>
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<p>Trend threshold in heatmap saturation percenteage series.</p>
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<p>Plot of detection residual with point anomalies.</p>
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<p>Justification of anomalies in detection series. (<b>a</b>) 11 October 2023 10:15:00 (Anomaly). (<b>b</b>) 4 October 2023 10:15:00 (Previous week). (<b>c</b>) 20 September 2023 10:15:00 (3 weeks earlier).</p>
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<p>Plot of heatmap saturation percentage residual with point anomalies.</p>
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<p>Justification of anomalies in heatmap series. (<b>a</b>) 1 October 2023 10:45:00 (Previous day) [0.001601]. (<b>b</b>) 2 October 2023 10:45:00 (Anomaly) [0.012045]. (<b>c</b>) 3 October 2023 10:45:00 (Next day) [0.008394].</p>
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19 pages, 11101 KiB  
Article
An ML-Based Ensemble Approach for the Precision Classification of Mangroves, Trend Analysis, and Priority Reforestation Areas in Asir, Saudi Arabia
by Asma A. Al-Huqail, Zubairul Islam and Hanan F. Al-Harbi
Sustainability 2024, 16(23), 10355; https://doi.org/10.3390/su162310355 - 26 Nov 2024
Viewed by 625
Abstract
In the recent past, mangrove ecosystems have undergone significant transformation, necessitating precise classification, the assessment of ecological changes, and the identification of suitable sites for urgent replantation. Therefore, this study aims to address three key objectives: first, to map the current extent of [...] Read more.
In the recent past, mangrove ecosystems have undergone significant transformation, necessitating precise classification, the assessment of ecological changes, and the identification of suitable sites for urgent replantation. Therefore, this study aims to address three key objectives: first, to map the current extent of mangroves; second, to assess the ecological changes within these ecosystems; and third, to identify suitable areas for replantation, ensuring their sustainability across coastal Asir. The mangrove classification was conducted using an ensemble of machine learning models, utilizing the key spectral indices from Landsat 8 data for 2023. To analyze the ecological trends and to assess the changes over time, Landsat 5–8 data from 1991 to 2023 were used. Finally, a generalized additive model (GAM) identified the areas suitable for reforestation. The EC identified the mangrove area as 14.69 sq. km, with a 95.6% F1 score, 91.3% OA, and a KC of 0.83. The trends in the NDVI and LST increased (p = 0.029, 0.049), whereas the NDWI showed no significant change (p = 0.186). The GAM model demonstrated a strong fit (with an adjusted R2 of 0.89) and high predictive accuracy (R2 = 0.91) for mangrove priority reforestation suitability, confirmed by a 10-fold cross-validation and minimal bias in the residual diagnostics. The suitability varied across groups, with Group (e) showing the highest suitability at 77%. Moran’s I analysis revealed significant spatial clustering. This study provides actionable insights for mangrove reforestation, supporting the for sustainable development through targeted efforts that enhance ecological resilience in coastal regions. Full article
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<p>Geographical extent of the Asir mangrove ecosystems, showing the distribution of the reference samples (green for mangroves, red for non-mangroves) across the study area. The study area is divided into five areas (<b>a</b>–<b>e</b>), spanning from north to south. The mangrove distribution follows the pattern of thriving in protected areas such as lagoons, tidal flats, and wadis. The division aids in understanding the spatial variations in mangrove coverage, as detailed in <a href="#sustainability-16-10355-t001" class="html-table">Table 1</a>.</p>
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<p>Methodological framework for mangrove classification using Landsat 8 OLI data and ML classifiers. The process begins with atmospheric correction followed by the computation of the spectral indices. An annual mosaic (the median composite) is created and masked using spectral index and elevation data from ASTER GDEM. The normalized band values are input into the ML algorithms. The training and test samples are used for the model training and testing. The final output consists of mangrove/non-mangrove classifications, with an accuracy assessment performed to evaluate the model performance based on the reference data.</p>
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<p>Mangroves along the Asir coast in groups (<b>a</b>–<b>e</b>), classified via an ensemble model that is based on majority voting from RF, SVM, and XGB predictions (green). The red outline indicates the GMW dataset for comparison. The classified data highlight the detection of smaller, scattered mangrove patches that were not captured by the GMW dataset, highlighting the enhanced accuracy of the ensemble approach.</p>
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<p>Radar plot comparing the internal performance metrics.</p>
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<p>Radar plot comparing the independent performance metrics.</p>
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<p>NDVI trends with <span class="html-italic">p</span>-values &lt; 1 (which shows all trends) based on Kendall’s tau-b correlation (1991–2023) for the Asir mangroves. The subfigures represent trends for groups (<b>a</b>–<b>e</b>).</p>
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<p>LST trends with <span class="html-italic">p</span>-values &lt; 1 (which shows all trends) based on Kendall’s tau-b correlation (1991–2023) for the Asir mangroves. The subfigures represent trends for groups (<b>a</b>–<b>e</b>).</p>
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<p>NDWI trends with <span class="html-italic">p</span>-values &lt; 1 (which shows all trends) based on Kendall’s tau-b correlation (1991–2023) for the Asir mangroves. The subfigures represent trends for groups (<b>a</b>–<b>e</b>).</p>
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<p>Predicted suitability for mangrove plantations along the Asir coast via a generalized additive model (GAM). The subfigures represent trends for groups (<b>a</b>–<b>e</b>).</p>
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<p>Response curves of the predictors for predicting mangrove reforestation suitability via generalized additive model (GAM) analysis.</p>
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<p>Subfigures (<b>a</b>–<b>c</b>) represent mangroves narrow patches not classified due to Landsat 8 spatial resolution limitations.</p>
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20 pages, 21022 KiB  
Article
Decoupling the Impacts of Climate Change and Human Activities on Terrestrial Vegetation Carbon Sink
by Shuheng Dong, Wanxia Ren, Xiaobin Dong, Fan Lei, Xue-Chao Wang, Linglin Xie and Xiafei Zhou
Remote Sens. 2024, 16(23), 4417; https://doi.org/10.3390/rs16234417 - 26 Nov 2024
Viewed by 408
Abstract
Net ecosystem productivity (NEP) plays a vital role in quantifying the carbon exchange between the atmosphere and terrestrial ecosystems. Understanding the effects of dominant driving forces and their respective contribution rates on NEP can aid in the effective management of terrestrial carbon sinks, [...] Read more.
Net ecosystem productivity (NEP) plays a vital role in quantifying the carbon exchange between the atmosphere and terrestrial ecosystems. Understanding the effects of dominant driving forces and their respective contribution rates on NEP can aid in the effective management of terrestrial carbon sinks, especially in rapidly urbanizing coastal areas where climate change (CC) and human activities (HA) occur frequently. Combining MODIS NPP products and meteorological data from 2000 to 2020, this paper established a Modis NPP-Soil heterotrophic respiration (Rh) model to estimate the magnitude of NEP in China’s coastal zone (CCZ). Hotspot analysis, variation trend, partial correlation, and residual analysis were applied to explore the spatiotemporal patterns of NEP and the contributions of CC and HA to the dynamics of NEP. We also explored the changes in NEP in different land use types. It was found that there is a clear north–south difference in the spatial pattern of NEP in CCZ, with Zhejiang Province serving as the main watershed for this difference. In addition, NEP in most regions showed an improvement trend, especially in the Beijing–Tianjin–Hebei region and Shandong Province, but the pixel values of NEP here were generally not as high as that in most southern provinces. According to the types of driving forces, the improvement of NEP in these regions primarily results from the synergistic effects of CC and HA. NEP changes in provinces south of Zhejiang are mainly dominated by single-factor-driven degradation. The area where HA contributes to the increase in NEP is much larger than that of CC. From the perspective of land use types, forests and farmland are the dominant contributors to the magnitude of NEP in CCZ. Full article
(This article belongs to the Special Issue Mapping Essential Elements of Agricultural Land Using Remote Sensing)
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<p>Location, topography, and main land use types of CCZ.</p>
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<p>Spatiotemporal dynamics of NEP in CCZ.</p>
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<p>Average NEP changes in the main provincial-level administrative regions from 2000 to 2020.</p>
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<p>Hotspot cluster map of average NEP in CCZ.</p>
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<p>Spatial distribution of NEP trend types and area proportion in different provinces.</p>
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<p>Partial correlation types of NEP and meteorological factors: (<b>a</b>) NEP-Temperature; (<b>b</b>) NET-Precipitation.</p>
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<p>Partial correlation coefficients of NEP and meteorological factors: (<b>a</b>) NEP-Temperature; (<b>b</b>) NET-Precipitation.</p>
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<p>Spatial distribution of NEP driver types and their area proportion.</p>
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<p>Contribution rate distribution of CC and HA: (<b>a</b>) Climate change; (<b>b</b>) Human activities.</p>
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<p>Relative contribution ratio of CC and HA.</p>
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<p>Area proportion of NEP trend types.</p>
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<p>Area proportion of NEP diver types.</p>
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19 pages, 6527 KiB  
Article
The Shear Behavior of the Curved Interface in Polyurethane-Concrete Composite Structures
by Bin Li, Xiangyang Wang, Yin Wang, Yanting Ji, Jing Wang, Xueming Du and Niannian Wang
Appl. Sci. 2024, 14(23), 10915; https://doi.org/10.3390/app142310915 - 25 Nov 2024
Viewed by 425
Abstract
Polyurethane grouting trenchless technology has been widely applied to the rehabilitation of concealed defects in engineering structures. The interfacial properties between polyurethane and engineering structures are key factors determining the stability of the composite structure. In practical applications, the interface shapes of different [...] Read more.
Polyurethane grouting trenchless technology has been widely applied to the rehabilitation of concealed defects in engineering structures. The interfacial properties between polyurethane and engineering structures are key factors determining the stability of the composite structure. In practical applications, the interface shapes of different engineering structures vary significantly, and the influence of the interface shape on interfacial properties should not be overlooked. This study focuses on engineering structures with curved interfaces, such as pile foundations, pipelines, and tunnels. Direct shear tests were conducted on polyurethane and concrete composite specimens with curved interfaces. A comparative analysis of the shear behavior between curved and planar composite specimens was performed, and the influence of arc diameter and polyurethane density on the shear behavior of curved and planar composite specimens was investigated. Additionally, SEM (Scanning Electron Microscopy) was used to conduct a microscopic examination of the interfaces with different polyurethane densities after failure, and the microscopic shear mechanisms between polyurethane and concrete materials were explored. The results revealed that the shear behavior of curved specimens was significantly higher than that of planar specimens. The shear strengths of curved specimens with diameters of 400 mm, 500 mm, and 700 mm were approximately 1.50, 1.39, and 1.10 times those of planar specimens, respectively. With increasing polyurethane density, the variation trend of shear strength in curved specimens was similar to that of planar specimens. However, significant differences were observed in the shear modulus, peak displacement, and shear residual strength between curved and planar specimens as the polyurethane density varied. Different diameter curved interface specimens exhibited a similar trend of shear strength variation with polyurethane density, gradually decreasing as the curvature diameter increased, and ultimately approaching that of planar specimens. Full article
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<p>Mold made by 3D printing.</p>
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<p>Curved concrete specimen.</p>
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<p>Manufacturing process of polyurethane–concrete composite specimens.</p>
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<p>Direct shear test equipment of the polyurethane–concrete composite specimens.</p>
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<p>Interface forms of polyurethane–concrete composite specimens.</p>
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<p>Shear stress-displacement curves of curved and planar composite specimens: (<b>a</b>) curved specimen R250, (<b>b</b>) planar specimens, (<b>c</b>) theoretical curve of curved specimen R250, and (<b>d</b>) theoretical curve of the planar specimen.</p>
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<p>Shear strength of curved and planar specimens with different polyurethane densities.</p>
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<p>Shear modulus of curved and planar composite specimens with different polyurethane densities.</p>
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<p>Peak shear displacements of curved and planar composite specimens with different polyurethane densities.</p>
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<p>Shear residual strength of curved and planar composite specimens with different polyurethane densities.</p>
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<p>Shear stress-displacement curves of curved and planar composite specimens with different arc diameters: (<b>a</b>) curved specimen R200, (<b>b</b>) curved specimen R250, (<b>c</b>) curved specimen R350, and (<b>d</b>) planar specimens.</p>
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<p>Shear stress-displacement curves of curved and planar composite specimens with different arc diameters: (<b>a</b>) density = 0.33 g/cm<sup>3</sup>, (<b>b</b>) density = 0.42 g/cm<sup>3</sup>, (<b>c</b>) density = 0.51 g/cm<sup>3</sup>, (<b>d</b>) density = 0.58 g/cm<sup>3</sup>, and (<b>e</b>) density = 0.66 g/cm<sup>3</sup>.</p>
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<p>Variation in shear strength with polyurethane density for planar and curved composite specimens with different arc diameters.</p>
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<p>Variation in shear strength with arc diameter for planar and curved composite specimens with different polyurethane densities.</p>
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<p>Multiple relationships of shear strength between curved s and planar specimens.</p>
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<p>(<b>a</b>) Variation in shear modulus with polyurethane density for planar and curved composite specimens with different arc diameters, and (<b>b</b>) variation in shear modulus with arc diameter for planar and curved composite specimens with different polyurethane densities.</p>
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<p>Variation in peak displacement with polyurethane density for planar and curved composite specimens with different arc diameters.</p>
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<p>Variation in peak shear displacement with arc diameter for curved composite specimens with different polyurethane densities.</p>
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<p>Shear residual strength of curved composite specimens: (<b>a</b>) variation in residual strength with polyurethane densities for specimens with different arc diameters, and (<b>b</b>) variation in residual strength with arc diameter for specimens with different polyurethane densities.</p>
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<p>SEM scan images of the interfacial microstructures of curved and planar specimens: (<b>a</b>) curved specimen, and (<b>b</b>) planar specimen.</p>
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<p>SEM scan images of the microstructures of interface regions in polyurethane-concrete composite specimens with different densities: (<b>a</b>) density = 0.30 g/cm<sup>3</sup>, (<b>b</b>) density = 0.55 g/cm<sup>3</sup>, and (<b>c</b>) density = 0.80 g/cm<sup>3</sup>.</p>
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28 pages, 5287 KiB  
Article
Bayesian Identification of High-Performance Aircraft Aerodynamic Behaviour
by Muhammad Fawad Mazhar, Syed Manzar Abbas, Muhammad Wasim and Zeashan Hameed Khan
Aerospace 2024, 11(12), 960; https://doi.org/10.3390/aerospace11120960 - 21 Nov 2024
Viewed by 351
Abstract
In this paper, nonlinear system identification using Bayesian network has been implemented to discover open-loop lateral-directional aerodynamic model parameters of an agile aircraft using a grey box modelling structure. Our novel technique has been demonstrated on simulated flight data from an F-16 nonlinear [...] Read more.
In this paper, nonlinear system identification using Bayesian network has been implemented to discover open-loop lateral-directional aerodynamic model parameters of an agile aircraft using a grey box modelling structure. Our novel technique has been demonstrated on simulated flight data from an F-16 nonlinear simulation of its Flight Dynamic Model (FDM). A mathematical model has been obtained using time series analysis of a Box–Jenkins (BJ) model structure, and parameter refinement has been performed using Bayesian mechanics. The aircraft nonlinear Flight Dynamic Model is adequately excited with doublet inputs, as per the dictates of its natural frequency, in accordance with non-parametric modelling (Finite Impulse Response) estimates. Time histories of optimized doublet inputs in the form of aileron and rudder deflections, and outputs in the form of roll and yaw rates are recorded. Dataset is pre-processed by implementing de-trending, smoothing, and filtering techniques. Blend of System Identification time-domain grey box modelling structures to include Output Error (OE) and Box–Jenkins (BJ) Models are stage-wise implemented in multiple flight conditions under varied stochastic models. Furthermore, a reduced order parsimonious model is obtained using Akaike information Criteria (AIC). Parameter error minimization activity is conducted using the Levenberg–Marquardt (L-M) Algorithm, and parameter refinement is performed using the Bayesian Algorithm due to its natural connection with grey box modelling. Comparative analysis of different nonlinear estimators is performed to obtain best estimates for the lateral–directional aerodynamic model of supersonic aircraft. Model Quality Assessment is conducted through statistical techniques namely: Residual Analysis, Best Fit Percentage, Fit Percentage Error, Mean Squared Error, and Model order. Results have shown promising one-step model predictions with an accuracy of 96.25%. Being a sequel to our previous research work for postulating longitudinal aerodynamic model of supersonic aircraft, this work completes the overall aerodynamic model, further leading towards insight to its flight control laws and subsequent simulator design. Full article
(This article belongs to the Section Aeronautics)
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Graphical abstract
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<p>Research Framework.</p>
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<p>Top Level Simulink Model of Aircraft Flight Dynamic Model (MATLAB-2021b).</p>
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<p>F-16 6-DOF Dynamics [<a href="#B39-aerospace-11-00960" class="html-bibr">39</a>].</p>
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<p>Optimal Input Design Flowchart.</p>
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<p>Bayesian Implementation Flowchart.</p>
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<p>F-16 Kinematics Variables [<a href="#B39-aerospace-11-00960" class="html-bibr">39</a>].</p>
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<p>Non-Parametric (FIR) Model of Aircraft.</p>
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<p>Bode Plot Aircraft Lateral Dynamics.</p>
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<p>Simulated Time-Skewed 2-1-1 Doublet Inputs—Aileron (δa) and Rudder (δr).</p>
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<p>Roll and Yaw Rate Time histories in repose to 2-1-1 Doublet Inputs.</p>
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<p>Roll and Pitch Angle time histories to 2-1-1 Doublet Inputs.</p>
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<p>Aircraft Parameter Refinement Flow chart.</p>
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<p>(<b>a</b>) Initial OE Model; (<b>b</b>) Reduced Order OE Model; (<b>c</b>) Initial BJ Model; (<b>d</b>) Optimized BJ Model; (<b>e</b>) Residual Correlation; (<b>f</b>) pdf of Model Parameters; (<b>g</b>) Posterior Sensitivity Analysis (K-L Divergence)—Straight and Level Flight.</p>
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<p>(<b>a</b>) Initial OE Model; (<b>b</b>) Reduced Order OE Model; (<b>c</b>) Initial BJ Model; (<b>d</b>) Optimized BJ Model; (<b>e</b>) Residual Correlation; (<b>f</b>) pdf of Model Parameters; (<b>g</b>) Posterior Sensitivity Analysis (K-L Divergence)—Straight and Level Flight.</p>
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<p>(<b>a</b>) Initial OE Model; (<b>b</b>) Reduced Order OE Model; (<b>c</b>) Initial BJ Model; (<b>d</b>) Optimized BJ Model; (<b>e</b>) Residual Correlation; (<b>f</b>) pdf of Model Parameters; (<b>g</b>) Posterior Sensitivity Analysis (K-L Divergence)—Coordinated Turn Flight.</p>
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21 pages, 18849 KiB  
Article
What Drives Vegetation Evolution in the Middle Reaches of the Yellow River Basin, Climate Change or Human Activities?
by Mengmeng Gao, Nan Yang and Qiong Liu
Sustainability 2024, 16(22), 10122; https://doi.org/10.3390/su162210122 - 20 Nov 2024
Viewed by 454
Abstract
The middle reaches of the Yellow River Basin (MYRB) are known for their significant soil erosion and fragile ecological environment, where vegetation growth is important. However, the vegetation’s reaction to climate change (CC) and human activity (HA), and the potential driving mechanisms underlying [...] Read more.
The middle reaches of the Yellow River Basin (MYRB) are known for their significant soil erosion and fragile ecological environment, where vegetation growth is important. However, the vegetation’s reaction to climate change (CC) and human activity (HA), and the potential driving mechanisms underlying such changes in the MYRB, have not yet been clarified. Thus, based on remote sensing data, combined with trend analysis and the Hurst method and supplemented by the structural equation model (SEM) and residual analysis method, we aimed to conduct an analysis of the spatio-temporal evolution of the normalized difference vegetation index (NDVI) in the MYRB from 2000 to 2020. Additionally, we explored how climate and human factors together affect the NDVI and quantified the proportion of their respective contributions to NDVI change. The NDVI exhibited a fluctuating upward trend in the MYRB. Moreover, approximately 97.7% of the area showed an improving trend, with nearly 50% of the area continuing to maintain an improving trend. Precipitation and temperature had positive effects on the NDVI, while vapor pressure deficit (VPD) and land use intensity (LUI) had negative effects. HA played a pivotal role in the vegetation improvement area with a contribution rate of 67.53%. The study revealed NDVI variations and emphasized the influence of HA on the NDVI in the MYRB. The findings are vital in comprehending the response mechanism of ecosystems and guiding reasonable environmental protection policies, which is beneficial for the sustainable development of the region. Full article
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<p>(<b>a</b>) Geographical location and topography; (<b>b</b>) land use in 2020; (<b>c</b>) subwatersheds of the middle reaches of the Yellow River Basin (MYRB).</p>
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<p>The annual average NDVI from 2000 to 2020 in the MYRB.</p>
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<p>Violin plots of the annual average NDVI distribution in the different subwatersheds.</p>
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<p>Inter-annual NDVI trends in (<b>a</b>) MYRB and its subwatersheds, (<b>b</b>) HL, (<b>c</b>) LS, (<b>d</b>) SH from 2000 to 2020.</p>
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<p>Inter-annual NDVI trends in (<b>a</b>) MYRB and its subwatersheds, (<b>b</b>) HL, (<b>c</b>) LS, (<b>d</b>) SH from 2000 to 2020.</p>
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<p>(<b>a</b>) Spatial distributions of slope of NDVI and (<b>b</b>) significant change in the MYRB.</p>
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<p>Area (<b>a</b>) and proportions (<b>b</b>) of different NDVI variation trends in different subwatersheds from 2000 to 2020.</p>
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<p>The (<b>a</b>) value and (<b>b</b>) classification of Hurst exponent of the NDVI in the MYRB.</p>
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<p>Trend sustainability in the MYRB.</p>
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<p>(<b>a</b>) Distribution map of land use conversion in the consistent significant improvement areas and (<b>b</b>) consistent significant degradation areas from 2000 to 2020. GL, grassland; CL, cropland; FL, forest land; IL, impervious land; and CL-GL, stands for cropland converted to grassland.</p>
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<p>Structural equation modeling results for the NDVI dynamics driven by influencing factors. The solid blue single-arrow lines represent significant positive pathways (<span class="html-italic">p</span> &lt; 0.05); The solid red single-arrow lines represent significant negative pathways (<span class="html-italic">p</span> &lt; 0.05); Dashed arrows represent nonsignificant pathways (<span class="html-italic">p</span> &gt; 0.05). Numbers placed next to the arrows represent the standardized path coefficients. PRE, precipitation; TEM, temperature; RAD, solar radiation; VPD, vapor pressure deficit; LUI, land use intensity; and PD, population density.</p>
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<p>Trends of predicted (<b>a</b>) NDVI and (<b>b</b>) residual NDVI variations in the MRYB from 2000 to 2020.</p>
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<p>(<b>a</b>) Positive and (<b>b</b>) negative contributions of CC and (<b>c</b>) positive and (<b>d</b>) negative contributions of HA to NDVI in the MYRB from 2000 to 2020.</p>
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<p>Sankey diagram of land use transfer. CL, cropland; FL, forest; SL, shrubland; GL, grassland; WL, water land; S/I, snow/ice; BL, bareland; IL, impervious land; and WL, wetland.</p>
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<p>Change trend in (<b>a</b>) LUI and (<b>b</b>) NDVI; correlation of scatter plot between LUI and NDVI in terms of (<b>c</b>) temporal trends and (<b>d</b>) spatial distribution.</p>
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<p>Change trend in (<b>a</b>) LUI and (<b>b</b>) NDVI; correlation of scatter plot between LUI and NDVI in terms of (<b>c</b>) temporal trends and (<b>d</b>) spatial distribution.</p>
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<p>Change trend of LUI and NDVI in population density grade.</p>
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<p>Change trend of (<b>a</b>) precipitation and (<b>b</b>) VPD in vegetation degradation areas.</p>
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19 pages, 7052 KiB  
Article
Insights into the Acute Stress of Glutaraldehyde Disinfectant on Short-Term Wet Anaerobic Digestion System of Pig Manure: Dose Response, Performance Variation, and Microbial Community Structure
by Yongming Wu, Fangfei Li, Liuxing Wu, Shifu He, Peiyu Liang, Lei Zhang, Zhijian Wu, Tao Zhang, Yajun Liu, Xiangmin Liu, Xueping Huang, Lin Zhu, Maolin Wang and Mi Deng
Water 2024, 16(22), 3279; https://doi.org/10.3390/w16223279 - 15 Nov 2024
Viewed by 630
Abstract
The outbreak of epidemics such as African swine fever has intensified the use of disinfectants in pig farms, resulting in an increasing residual concentration of disinfectants in environmental media; however, the high-frequency excessive use of disinfectants that damage pig farm manure anaerobic fermentation [...] Read more.
The outbreak of epidemics such as African swine fever has intensified the use of disinfectants in pig farms, resulting in an increasing residual concentration of disinfectants in environmental media; however, the high-frequency excessive use of disinfectants that damage pig farm manure anaerobic fermentation systems and their mechanisms has not attracted enough attention. Especially, the complex effects of residual disinfectants on anaerobic fermentation systems for pig manure remain poorly understood, thus impeding the application of disinfectants in practical anaerobic fermentation systems. Herein, we explored the effects of glutaraldehyde disinfectant on methane production, effluent physicochemical indices, and microbial communities in a fully automated methanogenic potential test system (AMPTSII). The results show that adding glutaraldehyde led to remarkable alterations in methane production, chemical oxygen demand (COD), volatile solids (VS), and polysaccharide and phosphorus concentrations. During the anaerobic process, the production of methane displayed a notable decrease of 5.0–98% in all glutaraldehyde treatments, and the trend was especially apparent for treatments containing high levels of glutaraldehyde. Comparisons of the effluent quality showed that in the presence of 0.002–0.04% glutaraldehyde, the COD and total phosphorus (TP) increased by 12–310% and 15–27%, respectively. Moreover, the addition of 0.01–0.08% glutaraldehyde decreased the ammonium (NH4+-N) concentration and VS degradation rate by 7.7–15% and 4.9–26.2%. Furthermore, microbiological analysis showed that the glutaraldehyde treatments had adverse effects on the microbial community. Notably, certain functional bacteria were restrained, as highlighted by the decreases in relative abundance and microbial diversity by 1.3–17% and 0.06–21%, respectively. This study provides a theoretical basis for the rational use of disinfectants in anaerobic fermentation systems. Full article
(This article belongs to the Special Issue The Control of Legacy and Emerging Pollutants in Soil and Water)
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<p>Fully automated methane potential test system (AMPTS II): (<b>a</b>) Anaerobic fermentation unit, (<b>b</b>) CO<sub>2</sub> adsorption unit, (<b>c</b>) Computing and data processing.</p>
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<p>Effects of glutaraldehyde on effluent properties during the anaerobic fermentation process: (<b>a</b>) Chemical oxygen demand (COD), (<b>b</b>) Total phosphorus (TP), (<b>c</b>) Ammonia nitrogen (NH<sub>4</sub><sup>+</sup>-N), (<b>d</b>) Total nitrogen (TN), (<b>e</b>) Polysaccharide (NH<sub>4</sub><sup>+</sup>-N), (<b>f</b>) pH value, (<b>g</b>) Volatile suspended solids (VS), (<b>h</b>) Total suspended solids (TS). *, <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.</p>
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<p>(<b>a</b>,<b>b</b>) Effects of glutaraldehyde on methane production in anaerobic fermentation systems. *, <span class="html-italic">p</span> &lt; 0.05; ***, <span class="html-italic">p</span> &lt; 0.001.</p>
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<p>Effect of glutaraldehyde on microbial Alpha diversity index and dysbiosis index in anaerobic fermentation systems: (<b>a</b>) Chao Indices, (<b>b</b>) Ace Indices, (<b>c</b>) Shannon Indices, (<b>d</b>) Simpson Indices, (<b>e</b>) MDI index of pre-reaction, (<b>f</b>) MDI index of post-reaction. *, <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.</p>
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<p>Effects of glutaraldehyde on the microbial community structure of anaerobic sludge: (<b>a</b>) Phylum level, (<b>b</b>) genus level, (<b>c</b>) PCoA analysis, (<b>d</b>) Chloroflexi Pre-reaction changes, (<b>e</b>) <span class="html-italic">Syntrophomonas</span> Pre-reaction changes, and (<b>f</b>) <span class="html-italic">Bacteroides</span> Post-reaction changes. *, <span class="html-italic">p</span> &lt; 0.05.</p>
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<p>Correlations among main microbial species and key physicochemical indices: (<b>a</b>) redundancy analysis (RDA) and (<b>b</b>) Correlation of environmental factors. *, <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.</p>
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<p>Functional and community analysis of related genes: (<b>A</b>,<b>B</b>) Gene functions of microflora at different stages, (<b>C</b>) Venn diagram for pre-reaction genus levels, (<b>D</b>) Venn diagram for post-reaction genus levels.</p>
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17 pages, 5157 KiB  
Article
Analysis of Downstream Sediment Transport Trends Based on In Situ Data and Numerical Simulation
by Yuxi Wu, Xiwen Li, Enjin Zhao, Yang Wang, Shiyou Zhang, Zhiming Xu, Qinjun Wang, Dongxu Jiang and Zhuang Xing
J. Mar. Sci. Eng. 2024, 12(11), 1982; https://doi.org/10.3390/jmse12111982 - 2 Nov 2024
Viewed by 954
Abstract
This study conducted an in-depth analysis of the sediment dynamics in the lower reaches of the Changhua River and its estuary on Hainan Island. Through field collection of topographic data and sediment sampling, combined with advanced computational techniques, the study explored the transport [...] Read more.
This study conducted an in-depth analysis of the sediment dynamics in the lower reaches of the Changhua River and its estuary on Hainan Island. Through field collection of topographic data and sediment sampling, combined with advanced computational techniques, the study explored the transport pathways and depositional patterns of sediments. The grain size trend analysis (GSTA) method was utilized, in conjunction with the Flemming triangle diagram method, to classify the dynamic environment of the sediments. Furthermore, hydrodynamic modeling results were integrated to further analyze the transport trends of the sediments. The study revealed that the sediment types in the research area are complex, primarily consisting of gravelly sand and sandy gravel, indicating a generally coarse sedimentary environment in the region. The sediments in the lower reaches of the Changhua River generally transport towards the south and southwest (in the direction of Beili Bay). The net sediment transport directions inferred from the GSTA model are largely consistent with the Eulerian residual flow patterns, especially in the offshore area, where discrepancies are observed in the nearshore zone. The nearshore transport is influenced by the combined effects of alongshore currents, residual flows, and river inputs, while the offshore transport exhibits a shift from the northwest to southwest directions, reflecting the regional circulation patterns. Full article
(This article belongs to the Special Issue Advance in Sedimentology and Coastal and Marine Geology—2nd Edition)
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<p>Land use patterns in Hainan province with a focus on the Changhua River Basin, the black star refers to the source of the Changhua River (Origin: International Research Center of Big Data for Sustainable Development Goals. DOI: 10.12237/casearth.63eb24d7819aec795e09af68. [<a href="#B36-jmse-12-01982" class="html-bibr">36</a>]).</p>
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<p>Geographical extent of the study area in the lower reaches of the Changhua River and its estuary, highlighting the key sampling locations and topographical features that influence sediment transport dynamics: (<b>a</b>) Orange Box Denotes the Study Area with 3 Major Estuaries (A, B, C), and Changhua Port Located at Estuary C. (<b>b</b>) Red Box Encompasses Villages and 40 Sampling Points Within the Study Area.</p>
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<p>(<b>a</b>) Annual Discharge in the Lower Reaches of the Changhua River: The maximum value of 587 m<sup>3</sup>/s occurred in August 2018. (<b>b</b>) Annual Sediment Concentration in the Lower Reaches of the Changhua River: The maximum value of 0.772 kg/m<sup>3</sup> was recorded in July 2014. (<b>c</b>) Annual Sediment Transport Rate in the Lower Reaches of the Changhua River: The maximum value of 373 kg/s was reached in August 2018.</p>
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<p>The Flemming Triangle Diagram under Different Numbers of Sample Points: (<b>a</b>) The blue hexagons represent the distribution of the original sampling points, serving as the control group. (<b>b</b>) The red dots indicate the distribution of 80% of the sampling points. (<b>c</b>) The green triangles show the distribution of 60% of the sampling points.</p>
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<p>The study and simulation area consisted of a mesh file (mesh triangulation and boundary conditions) and applied in the model: The grid resolution varies from 0.2 km in the offshore region to 50 m in the main research area near the river channel.</p>
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<p>(<b>a</b>) Spatial distributions of the mean diameter of the surface sediment. (<b>b</b>) Spatial distributions of the sorting coefficient. (<b>c</b>) Spatial distributions of the skewness. (<b>d</b>) Spatial distributions of the sediment types in the study area.</p>
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<p>(<b>a</b>) Distribution characteristics of sediment classification in the study area. (<b>b</b>) Sediment classification according to Flemming triangle diagram: Dividing the study area into four sedimentary regions: Northern Offshore Depositional Zone (red dots), Central Offshore Depositional Zone (green triangles), Southern Offshore Depositional Zone (purple rhombuses), and Downstream River Channel Depositional Zone (blue hexagons).</p>
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<p>Trends in sediment transport in the Changhua river estuary and downstream areas: The base map is a bathymetric map of the seabed, and the red arrows represent the direction of sediment transport.</p>
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<p>(<b>a</b>) Eulerian residual current fields during summer (flood season) (<b>b</b>) Eulerian residual current fields during spring (dry season).</p>
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20 pages, 8411 KiB  
Article
Long-Term Mechanical Deterioration Trends and Mechanisms of SBS-Modified Asphalt Mixtures
by Jinquan Wang and Maijian Liu
Coatings 2024, 14(11), 1363; https://doi.org/10.3390/coatings14111363 - 26 Oct 2024
Viewed by 815
Abstract
Understanding the long-term performance deterioration trends and mechanisms of asphalt pavement is crucial for effective maintenance strategies. This study characterizes and correlates the multi-scale performance deterioration of a 14-year asphalt pavement. Air void measurements, indirect tensile (IDT) fatigue testing, Fourier transform infrared spectroscopy [...] Read more.
Understanding the long-term performance deterioration trends and mechanisms of asphalt pavement is crucial for effective maintenance strategies. This study characterizes and correlates the multi-scale performance deterioration of a 14-year asphalt pavement. Air void measurements, indirect tensile (IDT) fatigue testing, Fourier transform infrared spectroscopy (FTIR), and dynamic shear rheometer (DSR) testing were conducted on pavement cores and recovered binder. Multiple regression analysis was then performed on various performance indicators. Laboratory results indicate that the chemical composition and viscoelastic properties of SBS-modified binders evolve rapidly in the first few years, followed by a relatively stable aging rate. After 14 years, the mechanical and rheological properties of lower-layer mixtures deteriorate to a similar degree as the surface layer. Correlation analysis revealed that the residual strength of the mixture is more influenced by air voids, while reductions in fatigue life are primarily driven by binder aging. These findings highlight the necessity of applying preventive maintenance within the first 3–5 years to rejuvenate the surface asphalt and rehabilitate both the surface and underlying layers after long-term service. Full article
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<p>Flowchart of this study.</p>
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<p>Annual climate data.</p>
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<p>Annual traffic volume and ESAL.</p>
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<p>Core samples of different service years.</p>
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<p>Gradation of pavement cores: (<b>a</b>) SMA 13 for upper layer, (<b>b</b>) SMA16 for lower layer.</p>
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<p>Flowchart of sample preparation and performance test.</p>
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<p>Load–displacement curve of IDT tests.</p>
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<p>Air void content at different service years.</p>
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<p>Local Fourier transform infrared spectra of recovered asphalt of different service years.</p>
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<p>Aging reaction of base asphalt and SBS polymer.</p>
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<p>Infrared index at different service years: (<b>a</b>) upper-layer asphalt, (<b>b</b>) lower-layer asphalt.</p>
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<p>Binder’s rheological property at different service years: (<b>a</b>) <span class="html-italic">G*</span> at 25 °C, (<b>b</b>) <span class="html-italic">G*</span> at 65 °C, (<b>c</b>) <span class="html-italic">δ</span> at 25 °C, (<b>d</b>) <span class="html-italic">δ</span> at 65 °C, (<b>e</b>) <span class="html-italic">G*</span> × sin<span class="html-italic">δ</span>, (<b>f</b>) <span class="html-italic">G*</span>/sin<span class="html-italic">δ</span>.</p>
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<p>IDT test results at different service years: (<b>a</b>) IDT strength, (<b>b</b>) displacement, (<b>c</b>) fracture energy.</p>
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<p>Fatigue life at different service years and stress levels: (<b>a</b>) 0.45 MPa, (<b>b</b>) 0.65 MPa, (<b>c</b>) 0.9 MPa.</p>
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<p>Binder chemical and rheological correlation results: (<b>a</b>) <span class="html-italic">CI</span> and rheological indicators, (<b>b</b>) <span class="html-italic">BI</span> and rheological indicators.</p>
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39 pages, 26365 KiB  
Article
A Case Study on the Possibility of Extending the Service Life of the Demining Machine Belt
by Miroslav Blatnický, Ján Dižo, Marek Brůna and Marek Matejka
Materials 2024, 17(21), 5206; https://doi.org/10.3390/ma17215206 - 25 Oct 2024
Viewed by 494
Abstract
The operational practice of the design of the Bozena 5 demining machine has shown that its belts are the critical component that fundamentally affects the functionality of the entire machine. This article is a practical continuation and extension of the previous research results [...] Read more.
The operational practice of the design of the Bozena 5 demining machine has shown that its belts are the critical component that fundamentally affects the functionality of the entire machine. This article is a practical continuation and extension of the previous research results from the point of view of materials (research of the uniaxial fatigue life in bending and torsion), calculation (creation of the necessary mathematical, analytical and numerical models for the research) and construction (i.e., patented design of the belt tensioning of this machine). All these actions are aimed at a single objective—to achieve a condition that guarantees a sufficient service life without malfunctions, since repairing these machines in the field is often impossible. Therefore, this study examined the fatigue life of welded joints (uniaxial bending and torsion) of S960 QL and S500MC steels welded by MAG technology. Subsequently, the data were compared with previous results (electron and laser welds) and the influence of each type of weld on the fatigue life relative to the base material was discussed. It was found that conventional MAG technology had a more significant negative impact on the fatigue life of the base material than non-conventional technologies. This trend was particularly true for the bending stress. At the same time, the bending stress was identified by the FEM analysis as the dominant load on the belt. The maximum stress in the belt link under the considered boundary conditions was approximately 240 MPa (in bending). This stress corresponded to the continuous fatigue life (more than 107 cycles) for both base materials tested (S960QL, S500MC). In the whole studied spectrum of controlled deformation amplitudes (Manson–Coffin), the life of MAG welds was lower in comparison with the base material and with welds made by unconventional technologies. All the activities carried out so far (research on microstructure, hardness, strength, residual stresses, tribological properties and fatigue life) have shown that the original belt design (S500MC) using MAG technology has significant deficiencies in the state of optimal life. It is expected that the proposed material change (use of S960QL instead of S500MC) and work with advanced technologies will bring this state significantly closer. Full article
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<p>(<b>a</b>) Demining machine Božena 5; (<b>b</b>) Detail of the rotating cylinder with chains and flails.</p>
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<p>(<b>a</b>) Belt link article with damage; (<b>b</b>) The detail of its typical damage in service.</p>
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<p>Perspective of the spatial arrangement of the belt member.</p>
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<p>Defining the movement possibilities of individual loading mechanisms of test specimens for (<b>a</b>) torsion; (<b>b</b>) bending.</p>
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<p>Testing device for measuring the fatigue life of materials.</p>
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<p>CAD model of (<b>a</b>) eccentric; (<b>b</b>) body creating an eccentric pair.</p>
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<p>Calculation scheme of the resulting deflection of the eccentric pair.</p>
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<p>Calculation scheme of the mechanism causing bending of the test samples.</p>
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<p>Calculation scheme of the mechanism causing torsion of the test samples.</p>
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<p>(<b>a</b>) Determined angles of rotation; (<b>b</b>) Determined angles of twist of test samples for individual eccentric pairs.</p>
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<p>The optimal shape of the fatigue test specimen for the test condition of the experimental workplace.</p>
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<p>Defining groups of finite elements in the FEM model of the test specimen.</p>
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<p>Plastic bilinear material model.</p>
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<p>Entered boundary conditions of numerical simulation (B point—a point for a definition of boundary conditions).</p>
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<p>(<b>a</b>) Considered action of the driving force F<sub>p</sub> on the front wheel. (<b>b</b>) The component of the gravity force in the incline of the machine.</p>
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<p>CAD model of the structural design of belt tensioning using two guide rods.</p>
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<p>CAD model of the Božena 5 chassis with mounting of the proposed design solution for tensioning the belt.</p>
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<p>Strength ratios in contact between the belt and the rosette.</p>
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<p>Prepared FEM model of the test specimen for numerical calculation of stresses achieved during the test process.</p>
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<p>Results for the distribution of the reduced stress of the sample under bending stress.</p>
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<p>Results for the reduced stress distribution of the torsionally stressed sample.</p>
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<p>Calibration curves of values of shear and normal stresses of the material of the S500MC test sample and its arc welds for all levels of bending and twisting loads.</p>
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<p>Calibration curves of values of shear and normal stresses of the material of the test sample S960QL and its welds (laser, electron, arc) for all levels of bending and twisting loads.</p>
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<p>Fatigue curves (Manson–Coffin) of the tested material S960QL and its welds (electron, laser, MAG) and the tested material S500MC and its weld (MAG) from cyclic torsion loading.</p>
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<p>Fatigue curves (Manson–Coffin) of the tested material S960QL and its welds (electron, laser, MAG) and the tested material S500MC and its weld (MAG) from cyclic bending loading.</p>
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<p>Comparison of measured data with recommended FAT curves for normal stress in the weld.</p>
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<p>Comparison of measured data with the recommended FAT curve for tangential stress in the weld.</p>
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<p>Equivalent von Mises stress in the belt–rosette structure at the maximum tension force F<sub>vn</sub> = 60,000 N allowed by the tensioning system.</p>
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<p>Values of the reduced tension of the proposed design of the tensioning mechanism of the belt when combining the maximum possible force effects.</p>
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<p>Displacement values of the proposed design of the belt tensioning mechanism when combining the maximum possible force effects.</p>
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<p>Outline and side view of the tensioning mechanism (1—wheel hub, 2—front bracket, 3—rear bracket, 4—hydraulic cylinder bracket, 5—pin 1, 6—pin 2, 7—guide rod, 8—hydraulic cylinder 70/30/150, 9—retaining ring 30, 10—retaining ring 75, 11—slip sleeve, 12—bearing 50 × 75 × 8, 13—crown nut M36, 14—cotter pin).</p>
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18 pages, 27309 KiB  
Article
Impact of Natural and Human Factors on Dryland Vegetation in Eurasia from 2003 to 2022
by Jinyue Liu, Jie Zhao, Junhao He, Pengyi Zhang, Fan Yi, Chao Yue, Liang Wang, Dawei Mei, Si Teng, Luyao Duan, Nuoxi Sun and Zhenhong Hu
Plants 2024, 13(21), 2985; https://doi.org/10.3390/plants13212985 - 25 Oct 2024
Viewed by 565
Abstract
Eurasian dryland ecosystems consist mainly of cropland and grassland, and their changes are driven by both natural factors and human activities. This study utilized the normalized difference vegetation index (NDVI), gross primary productivity (GPP) and solar-induced chlorophyll fluorescence (SIF) to analyze the changing [...] Read more.
Eurasian dryland ecosystems consist mainly of cropland and grassland, and their changes are driven by both natural factors and human activities. This study utilized the normalized difference vegetation index (NDVI), gross primary productivity (GPP) and solar-induced chlorophyll fluorescence (SIF) to analyze the changing characteristics of vegetation activity in Eurasia over the past two decades. Additionally, we integrated the mean annual temperature (MAT), the mean annual precipitation (MAP), the soil moisture (SM), the vapor pressure deficit (VPD) and the terrestrial water storage (TWS) to analyze natural factors’ influence on the vegetation activity from 2003 to 2022. Through partial correlation and residual analysis, we quantitatively described the contributions of both natural and human factors to changes in vegetation activity. The results indicated an overall increasing trend in vegetation activity in Eurasia; the growth rates of vegetation greenness, productivity and photosynthetic capacity were 1.00 × 10−3 yr−1 (p < 0.01), 1.30 g C m−2 yr−2 (p < 0.01) and 1.00 × 10−3 Wm−2μm−1sr−1yr−1 (p < 0.01), respectively. Furthermore, we found that soil moisture was the most important natural factor influencing vegetation activity. Human activities were identified as the main driving factors of vegetation activity in the Eurasian drylands. The relative contributions of human-induced changes to NDVI, GPP and SIF were 52.45%, 55.81% and 74.18%, respectively. These findings can deepen our understanding of the impacts of current natural change and intensified human activities on dryland vegetation coverage change in Eurasia. Full article
(This article belongs to the Special Issue Forest Disturbance and Management)
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<p>The spatial distribution map of aridity levels (<b>a</b>) and vegetation types (<b>b</b>) in the Eurasian drylands. WCE, EEU, the MED, WSB, ESB, WCA, ECA, TIB, EAS, ARP and SAS represent West and Central Europe, E. Europe, Mediterranean, W. Siberia, E. Siberia, W. C. Asia, E. C. Asia, Tibet Plateau, E. Asia, Arabian Peninsula and S. Asia, respectively.</p>
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<p>Interannual variation of normalized difference vegetation index (NDVI, (<b>a</b>)), gross primary productivity (GPP, (<b>b</b>)) and solar-induced chlorophyll fluorescence (SIF, (<b>c</b>)) in Eurasian drylands during 2003–2022. Shading denotes 95% prediction intervals. All regressions were significant (<span class="html-italic">p</span> &lt; 0.05, the Student’s <span class="html-italic">t</span>-test).</p>
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<p>Spatial distribution of the temporal trends in normalized difference vegetation index (NDVI, (<b>a</b>)), gross primary productivity (GPP, (<b>b</b>)) and solar-induced chlorophyll fluorescence (SIF, (<b>c</b>)) during 2003–2022.</p>
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<p>Temporal trends in the mean annual temperature (MAT, (<b>a</b>)), mean annual precipitation (MAP, (<b>b</b>)), soil moisture (SM, (<b>c</b>)), vapor pressure deficit (VPD, (<b>d</b>)) and terrestrial water storage (TWS, (<b>e</b>)) in Eurasian drylands during 2003–2022, respectively. Solid (dashed) lines indicate significant (insignificant) regressions (<span class="html-italic">p</span> &lt; 0.05, the Student’s <span class="html-italic">t</span>-test).</p>
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<p>Spatial distribution of the linear trends in mean annual temperature (MAT, (<b>a</b>)), mean annual precipitation (MAP, (<b>b</b>)), soil moisture (SM, (<b>c</b>)), vapor pressure deficit (VPD, (<b>d</b>)) and terrestrial water storage (TWS, (<b>e</b>)) from 2003 to 2022.</p>
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<p>Spatial patterns of partial correlation coefficient between NDVI, GPP, SIF and natural factors. (<b>a</b>,<b>d</b>,<b>g</b>,<b>j</b>,<b>m</b>) show the partial correlation coefficient between normalized difference vegetation index (NDVI) and mean annual temperature (MAT), mean annual precipitation (MAP), soil moisture (SM), vapor pressure deficit (VPD) and terrestrial water storage (TWS), respectively. (<b>b</b>,<b>e</b>,<b>h</b>,<b>k</b>,<b>n</b>) show the partial correlation coefficient between gross primary productivity (GPP) and MAT, MAP, SM, VPD and TWS, respectively. (<b>c</b>,<b>f</b>,<b>i</b>,<b>l</b>,<b>o</b>) show the partial correlation coefficient between solar-induced chlorophyll fluorescence (SIF) and MAT, MAP, SM, VPD and TWS, respectively.</p>
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<p>Partial correlation coefficient between NDVI, GPP, SIF and natural factors. Red, blue and green bars represent the normalized difference vegetation index (NDVI), the gross primary productivity (GPP) and the solar-induced chlorophyll fluorescence (SIF), respectively. MAT (<b>a</b>), MAP (<b>b</b>), SM (<b>c</b>), VPD (<b>d</b>) and TWS (<b>e</b>) represent the mean annual temperature, the mean annual precipitation, the soil moisture, the vapor pressure deficit and the terrestrial water storage, respectively. WCE, EEU, the MED, WSB, ESB, WCA, ECA, TIB, EAS, ARP and SAS represent West and Central Europe, E. Europe, Mediterranean, W. Siberia, E. Siberia, W. C. Asia, E. C. Asia, Tibet Plateau, E. Asia, Arabian Peninsula and S. Asia, respectively. The symbol “*” indicates that the partial correlation coefficient has passed the significance test with <span class="html-italic">p</span> &lt; 0.05.</p>
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<p>Spatial distributions of the relative contributions of natural and human factors to the changes in the normalized difference vegetation index (NDVI, (<b>a</b>,<b>b</b>)), gross primary productivity (GPP, (<b>c</b>,<b>d</b>)) and solar-induced chlorophyll fluorescence (SIF, (<b>e</b>,<b>f</b>)). Left and right columns represent natural and human factors, respectively.</p>
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<p>Relative contributions of natural and human factors to the changes in the normalized difference vegetation index (NDVI), gross primary productivity (GPP) and solar-induced chlorophyll fluorescence (SIF) in WCE (West and Central Europe), EEU (E. Europe), the MED (Mediterranean), WSB (W. Siberia), ESB (E. Siberia), WCA (W. C. Asia), ECA (E. C. Asia), TIB (Tibet Plateau), EAS (E. Asia), ARP (Arabian Peninsula) and SAS (S. Asia). Red, blue and green bars represent NDVI, GPP and SIF, respectively.</p>
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<p>Spatial distribution of normalized difference vegetation index (NDVI, (<b>a</b>)), gross primary productivity (GPP, (<b>b</b>)) and solar-induced chlorophyll fluorescence (SIF, (<b>c</b>)) change drivers. “Improvement” represents an increasing trend in vegetation index over the past 20 years, while “degradation” indicates a declining trend in vegetation index over the same period.</p>
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