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Search Results (11,672)

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10 pages, 3980 KiB  
Editorial
Greece 2023: Crazy Summer or New Normal—Lessons Not Learned
by Andreas Matzarakis and Panagiotis Nastos
Atmosphere 2024, 15(10), 1241; https://doi.org/10.3390/atmos15101241 - 17 Oct 2024
Abstract
The year 2023 in Greece started with a mild winter and spring [...] Full article
(This article belongs to the Section Biometeorology and Bioclimatology)
Show Figures

Figure 1

Figure 1
<p>Change in distribution of average mean surface air temperature in Greece, within the period 1951–2020. (World Bank Group; <a href="https://climateknowledgeportal.worldbank.org/country/greece" target="_blank">https://climateknowledgeportal.worldbank.org/country/greece</a>; assessed on 15 July 2024).</p>
Full article ">Figure 2
<p>Temperature change in Greece, relative to the average of 1961–2010 (°C), within the period 1855–2023. Graphics and lead scientist: Ed Hawkins, National Centre for Atmospheric Science, University of Reading., National Centre for Atmospheric Science; UoR. data: Berkeley Earth and ERA5-Land, NOAA, UK Met Office, MeteoSwiss, DWD, SMHI, and UoR and ZAMG.</p>
Full article ">Figure 3
<p>Smoke from the fires in Evros, Viotia, and Parnis mountain in a NASA satellite image captured 22 August 2023. The extent of the burnt areas in 2023 as reported by EFFIS. The yellow dots refer to areas up to 100 ha, orange up to 500 ha, pink up to 1000 ha, red up to 5000 ha, and purple beyond 5000 ha. © EU, 2024—GWIS (small frame).</p>
Full article ">Figure 4
<p>Satellite Precipitation—CMORPH Climate Data Record (CDR) for normal rainfall (mm) in September (<b>upper left graph</b>), total rainfall anomaly (mm) in September 2023 (<b>upper right graph</b>), and percent of normal precipitation (%) in September 2023 (<b>lower graph</b>). Percent normal precipitation is based on Climate Research Unit global weather norms, 1980–2010 (Data: <a href="https://www.ncei.noaa.gov/products/climate-data-records/precipitation-cmorph" target="_blank">https://www.ncei.noaa.gov/products/climate-data-records/precipitation-cmorph</a>, accessed on 25 July 2024).</p>
Full article ">Figure 5
<p>Map of the topography of the baric relation (H500–H1000), the ground isobar, and geopotential height at 500 hPa, on 5. September 2023, 12 UTC. Source: <a href="https://www.wetter3.de/archiv_gfs_dt.html" target="_blank">https://www.wetter3.de/archiv_gfs_dt.html</a>, accessed on 25 July 2024.</p>
Full article ">Figure 6
<p>Widespread flooding over Thessaly region, central Greece, on 5 September 2023. Source: <a href="https://storymaps.arcgis.com/stories/e7dca3fe3d114860872f3108587c23db" target="_blank">https://storymaps.arcgis.com/stories/e7dca3fe3d114860872f3108587c23db</a>, accessed on 25 July 2024.</p>
Full article ">Figure 7
<p>Mean monthly SST (<b>upper graph</b>) and mean monthly SST anomaly (<b>lower graph</b>) in September 2023.</p>
Full article ">Figure 8
<p>Yearly time series for mean Mediterranean SST (<b>upper graph</b>) and Averaged Mediterranean annual SST stripes for the period 1982–2023 (<b>lower graph</b>). All the graphics and analysis are based on daily SST data from GHRSST Level 4 AVHRR_OI Global Blended Sea Surface Temperature Analysis (GDS version 2) from NOAA National Centers for Environmental Information available at PODAAC site (<a href="https://podaac.jpl.nasa.gov/dataset/AVHRR_OI-NCEI-L4-GLOB-v2.1" target="_blank">https://podaac.jpl.nasa.gov/dataset/AVHRR_OI-NCEI-L4-GLOB-v2.1</a>, accessed on 25 July 2024).</p>
Full article ">
15 pages, 3175 KiB  
Article
Dragonfly Functional Diversity in Dinaric Karst Tufa-Depositing Lotic Habitats in a Biodiversity Hotspot
by Marina Vilenica, Vlatka Mičetić Stanković and Mladen Kučinić
Diversity 2024, 16(10), 645; https://doi.org/10.3390/d16100645 - 17 Oct 2024
Abstract
Functional diversity is a key component of biodiversity that reflects various dimensions of ecosystem functioning and the roles organisms play within communities and ecosystems. It is widely used to understand how ecological processes influence biotic assemblages. With an aim to increase our knowledge [...] Read more.
Functional diversity is a key component of biodiversity that reflects various dimensions of ecosystem functioning and the roles organisms play within communities and ecosystems. It is widely used to understand how ecological processes influence biotic assemblages. With an aim to increase our knowledge about dragonfly ecological requirements in tufa-depositing karst habitats, we assessed functional diversity of their assemblages, various life history traits (e.g., stream zonation preference, substrate preference, reproduction type), and relationship between functional diversity and physico-chemical water properties in three types of karst lotic habitats (springs, streams, and tufa barriers) in a biodiversity hotspot in the western Balkan Peninsula. Dragonfly functional diversity was mainly characterized by traits typical for lotic rheophile species with medium dispersal capacity. Among the investigated habitats, tufa barriers, characterized by higher (micro)habitat heterogeneity, higher water velocity, as well as lower conductivity and concentration of nitrates, can be considered as dragonfly functional diversity hotspots. Functional diversity and most of the life history traits were comparable among different substrate types in the studied habitats, indicating higher importance of habitat type in shaping dragonfly functional diversity patterns in karst lotic habitats. Our results should be considered in the management and conservation activities of vulnerable karst freshwater ecosystems and their dragonfly assemblages. Full article
(This article belongs to the Section Freshwater Biodiversity)
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Figure 1

Figure 1
<p>Photo examples of study sites included in the study: springs: (<b>a</b>) Bijela rijeka spring, (<b>b</b>) Crna rijeka spring; streams (and small mountainous rivers): (<b>c</b>) Bijela rijeka middle reaches, (<b>d</b>) Crna rijeka middle reaches, (<b>e</b>) Crna rijeka lower reaches, (<b>f</b>) Plitvica, (<b>g</b>) Korana; tufa barriers: (<b>h</b>) Labudovac, (<b>i</b>) Kozjak–Milanovac, (<b>j</b>) Novakovića Brod.</p>
Full article ">Figure 2
<p>Environmental variables at three Dinaric karst lotic habitat types in the Plitvice Lakes NP, Croatia (shown as mean annual values with standard deviation, SD): (<b>a</b>) nitrate concentration, (<b>b</b>) pH, (<b>c</b>) oxygen saturation, (<b>d</b>) water velocity, (<b>e</b>) conductivity, and (<b>f</b>) alkalinity. Significant differences among the habitat types are indicated by different letters (Kruskal–Wallis H test with multiple comparisons <span class="html-italic">post hoc</span> test, <span class="html-italic">p</span> &lt; 0.05).</p>
Full article ">Figure 3
<p>Environmental variables at three Dinaric karst lotic habitat types in the Plitvice Lakes NP, Croatia (shown as mean annual values with standard deviation, SD): (<b>a</b>) water temperature, (<b>b</b>) oxygen concentration, and (<b>c</b>) ammonia concentration. Non-significant differences among the habitat types are indicated by the letter a (Kruskal–Wallis H test with multiple comparisons <span class="html-italic">post hoc</span> test, <span class="html-italic">p</span> &gt; 0.05).</p>
Full article ">Figure 4
<p>Dragonfly functional diversity (RaoQ index) at three Dinaric karst lotic habitat types in the Plitvice Lakes NP, Croatia (shown as mean with standard deviation, SD). Significant differences among the habitat types are indicated by different letters (Kruskal–Wallis H test with multiple comparisons <span class="html-italic">post hoc</span> test, <span class="html-italic">p</span> &lt; 0.05).</p>
Full article ">Figure 5
<p>Dragonfly functional traits at three Dinaric karst lotic habitat types in the Plitvice Lakes NP, Croatia (shown as mean with standard deviation, SD): (<b>a</b>) body shape, (<b>b</b>) dispersal capacity, (<b>c</b>) stream zonation preference, (<b>d</b>) lateral connectivity preference, (<b>e</b>) current preference, (<b>f</b>) substrate type preference, and (<b>g</b>) reproduction type. Significant differences among the habitat types are indicated by different letters (Kruskal–Wallis H test with multiple comparisons <span class="html-italic">post hoc</span> test, <span class="html-italic">p</span> &lt; 0.05). Legend: DC = dispersal capacity; EUC = eucrenal, HYC = hypocrenal, ERH = epirhithral, MRH = metarhithral, HRH = hyporhithral, EPO = epipotamal, MPO = metapotamal, HPO = hypopotamal, LITT = littoral; EUP = eupotamon, PRP = parapotamon, PLP = plesiopotamon, PAP = palaeopotamon, TMP = temporary water bodies; LIP = limnophil, LRP = limno- to rheophil, RLP = rheo- to limnophil, RPH = rheophil; ARG = argyllal, PEL = pelal, PSA = psammal, AKA = akal, LITH = lithal, PHY = phytal, POM = particulate organic matter; ETS = eggs laid attached to substrate, EIS = eggs laid in substrate, SUB = eggs laid not attached to or in substrate, OWA = eggs laid in open water, IPL = eggs laid inside plant tissue, OPL = eggs laid onto plant material, IRS = eggs laid into submerged soil or onto submerged rock.</p>
Full article ">Figure 6
<p>Redundancy analysis (RDA) ordination biplot showing the relationship between dragonfly functional traits and six significant environmental variables in Dinaric karst lotic habitats in the Plitvice Lakes NP, Croatia. Abbreviations of the functional (life history) traits are in <a href="#diversity-16-00645-f004" class="html-fig">Figure 4</a>.</p>
Full article ">Figure 7
<p>Dragonfly functional diversity (RaoQ index) at four main substrate types in three Dinaric karst lotic habitats in the Plitvice Lakes NP, Croatia (shown as mean with standard deviation, SD) Non-significant differences among the habitat types are indicated by the letter a (Kruskal–Wallis H test with multiple comparisons <span class="html-italic">post hoc</span> test, <span class="html-italic">p</span> &gt; 0.05).</p>
Full article ">Figure 8
<p>Dragonfly functional traits at four main substrate types in three Dinaric karst lotic habitats in the Plitvice Lakes NP, Croatia (shown as mean with standard deviation, SD): (<b>a</b>) body shape, (<b>b</b>) dispersal capacity, (<b>c</b>) stream zonation preference, (<b>d</b>) lateral connectivity preference, (<b>e</b>) current preference, (<b>f</b>) substrate type preference, and (<b>g</b>) reproduction type. Significant differences among the habitat types are indicated by different letters (Kruskal–Wallis H test with multiple comparisons post hoc test, <span class="html-italic">p</span> &lt; 0.05). Abbreviations of the functional (life history) traits are in <a href="#diversity-16-00645-f005" class="html-fig">Figure 5</a>.</p>
Full article ">
26 pages, 8947 KiB  
Article
Angle of Attack Characteristics of Full-Active and Semi-Active Flapping Foil Propulsors
by Lei Mei, Wenhui Yan, Junwei Zhou, Yongqi Tang and Weichao Shi
Water 2024, 16(20), 2957; https://doi.org/10.3390/w16202957 - 17 Oct 2024
Abstract
As a propulsor with a good application prospect, the flapping foil has been a hot research topic in the past decade. Although the research results of flapping foils have been very abundant, the performance-influencing mechanism of flapping foils is still not perfect, and [...] Read more.
As a propulsor with a good application prospect, the flapping foil has been a hot research topic in the past decade. Although the research results of flapping foils have been very abundant, the performance-influencing mechanism of flapping foils is still not perfect, and the research considering three-dimensional (3D) effects for engineering applications is still very limited. Based on the above considerations, a systematic and parametric analysis of a small aspect ratio flapping foil is conducted to correlate the influencing factors including angle of attack (AoA) characteristics and wake vortex on the propulsive efficiency. Three-dimensional numerical analyses of full-active and semi-active flapping foils are carried out in this paper, in which the former focuses on different heave amplitudes and pitch amplitudes, and the latter concentrates on different spring stiffnesses. The analysis covers the full range of advance coefficient, which starts around 0 and ends at a thrust drop of 0. Firstly, the influence of the maximum AoA (αmax) on the efficiency and thrust coefficient of these two kinds of flapping foils is analyzed. The results show that for the small aspect ratio flapping foil in this paper, regardless of the full-active or semi-active form, the peak efficiency as high as 75% for both generally appears around αmax = 0.2 rad, while the peak thrust coefficient of 0.5 occurs near αmax = 0.3 rad. Then, by analyzing the wake flow field, it is found that the lower efficiency of larger αmax working points is mainly due to the larger vortex dissipation loss, while the lower efficiency of smaller αmax working points is mainly due to the larger friction loss of the foil surface. Furthermore, the plumpness of different AoA curves is compared and analyzed. It was found that, unlike the results of full-active flapping foils, the shape of the AoA curve of semi-active flapping foils with different spring stiffnesses is similar, and the relationship with efficiency is not strictly corresponding. This study is expected to provide guidance on both academics and industries in relevant fields. Full article
(This article belongs to the Special Issue CFD in Fluid Machinery Design and Optimization)
Show Figures

Figure 1

Figure 1
<p>Three-dimensional geometric shape of the flapping foil.</p>
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<p>Sketch of the flapping foil propulsion motion.</p>
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<p>Schematic illustration of a semi-active flapping foil with forced heave motion and attached torsion spring (The blue part is the torsion spring, and the red part is the rigid connection with the actuator).</p>
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<p>Schematic diagram of the computational domain and gradual mesh refinement.</p>
Full article ">Figure 5
<p>Comparisons of the propulsive efficiency <span class="html-italic">η</span> and the thrust coefficient <span class="html-italic">c<sub>T</sub></span> with previous experimental results for <span class="html-italic">α<sub>max</sub></span> = 20°.</p>
Full article ">Figure 6
<p>Comparison of vorticity patterns visualized in the foil wake (<math display="inline"><semantics> <mrow> <msub> <mrow> <mi>S</mi> <mi>t</mi> </mrow> <mrow> <mi>D</mi> </mrow> </msub> <mo>=</mo> <mn>0.08</mn> <mo>,</mo> <mtext> </mtext> <msub> <mrow> <mi>A</mi> </mrow> <mrow> <mi>D</mi> </mrow> </msub> <mo>=</mo> <mn>1.4</mn> </mrow> </semantics></math>). (Experimental results are from Figure 3c in Schnipper [<a href="#B29-water-16-02957" class="html-bibr">29</a>]).</p>
Full article ">Figure 7
<p>Experimental site and related equipment.</p>
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<p>Comparisons of the propulsive efficiency <span class="html-italic">η</span> with experimental results for <span class="html-italic">α<sub>max</sub></span> = 20°.</p>
Full article ">Figure 9
<p>Comparison of hydrodynamic force between simulation and experimental results. (<b>a</b>) <span class="html-italic">J</span> = 2.45, (<b>b</b>) <span class="html-italic">J</span> = 5.24.</p>
Full article ">Figure 10
<p>Propulsive efficiency <span class="html-italic">η</span> and thrust coefficient <span class="html-italic">K<sub>T</sub></span> of a full-active flapping foil as function of <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>α</mi> </mrow> <mrow> <mi>m</mi> <mi>a</mi> <mi>x</mi> </mrow> </msub> </mrow> </semantics></math>, for different pitching angles. (<b>a</b>) <math display="inline"><semantics> <mrow> <mi>η</mi> <mo>−</mo> <msub> <mrow> <mi>α</mi> </mrow> <mrow> <mi>m</mi> <mi>a</mi> <mi>x</mi> </mrow> </msub> </mrow> </semantics></math>, (<b>b</b>) <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>K</mi> </mrow> <mrow> <mi>T</mi> </mrow> </msub> <mo>−</mo> <msub> <mrow> <mi>α</mi> </mrow> <mrow> <mi>m</mi> <mi>a</mi> <mi>x</mi> </mrow> </msub> </mrow> </semantics></math>.</p>
Full article ">Figure 11
<p>Propulsive efficiency <span class="html-italic">η</span> and thrust coefficient <span class="html-italic">K<sub>T</sub></span> of a full-active flapping foil as function of advance coefficient <span class="html-italic">J</span>, for different pitching angles. (<b>a</b>) <math display="inline"><semantics> <mrow> <mi>η</mi> <mo>−</mo> <mi>J</mi> </mrow> </semantics></math>, (<b>b</b>) <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>K</mi> </mrow> <mrow> <mi>T</mi> </mrow> </msub> <mo>−</mo> <mi>J</mi> </mrow> </semantics></math>.</p>
Full article ">Figure 12
<p>Propulsive efficiency <span class="html-italic">η</span> of a full-active flapping foil as function of <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>α</mi> </mrow> <mrow> <mi>m</mi> <mi>a</mi> <mi>x</mi> </mrow> </msub> </mrow> </semantics></math>, for a series of heaving amplitudes. (<b>a</b>) <span class="html-italic">θ</span><sub>0</sub> = 0.3 rad, (<b>b</b>) <span class="html-italic">θ</span><sub>0</sub> = 0.5 rad.</p>
Full article ">Figure 13
<p>Thrust coefficient <span class="html-italic">K<sub>T</sub></span> of a full-active flapping foil as function of <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>α</mi> </mrow> <mrow> <mi>m</mi> <mi>a</mi> <mi>x</mi> </mrow> </msub> </mrow> </semantics></math>, for a series of heaving amplitudes. (<b>a</b>) <span class="html-italic">θ</span><sub>0</sub> = 0.3 rad, (<b>b</b>) <span class="html-italic">θ</span><sub>0</sub> = 0.5 rad.</p>
Full article ">Figure 14
<p>Propulsive efficiency <span class="html-italic">η</span> of a semi-active flapping foil as function of <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>α</mi> </mrow> <mrow> <mi>m</mi> <mi>a</mi> <mi>x</mi> </mrow> </msub> <mtext> </mtext> </mrow> </semantics></math>and advance coefficient <span class="html-italic">J</span> for a series of spring stiffness ratios. (<b>a</b>) <span class="html-italic">θ</span><sub>0</sub> = 0.3 rad, (<b>b</b>) <span class="html-italic">θ</span><sub>0</sub> = 0.5 rad.</p>
Full article ">Figure 15
<p>Thrust coefficient <span class="html-italic">K<sub>T</sub></span> of a semi-active flapping foil as function of <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>α</mi> </mrow> <mrow> <mi>m</mi> <mi>a</mi> <mi>x</mi> </mrow> </msub> </mrow> </semantics></math><span class="html-italic">,</span> for a series of heaving amplitudes. (<b>a</b>) <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>K</mi> </mrow> <mrow> <mi>T</mi> </mrow> </msub> <mo>−</mo> <mi>J</mi> </mrow> </semantics></math>, (<b>b</b>) <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>K</mi> </mrow> <mrow> <mi>T</mi> </mrow> </msub> <mo>−</mo> <msub> <mrow> <mi>α</mi> </mrow> <mrow> <mi>m</mi> <mi>a</mi> <mi>x</mi> </mrow> </msub> </mrow> </semantics></math>.</p>
Full article ">Figure 16
<p>Vortex structure and distribution of an active flapping foil under six working conditions (<math display="inline"><semantics> <mrow> <msub> <mrow> <mi>y</mi> </mrow> <mrow> <mn>0</mn> </mrow> </msub> <mo>/</mo> <mi>c</mi> <mo>=</mo> <mn>2.5</mn> <mo>,</mo> <mtext> </mtext> <msub> <mrow> <mi>θ</mi> </mrow> <mrow> <mn>0</mn> </mrow> </msub> <mo>=</mo> <mn>0.5</mn> <mtext> </mtext> <mi mathvariant="normal">r</mi> <mi mathvariant="normal">a</mi> <mi mathvariant="normal">d</mi> </mrow> </semantics></math>).</p>
Full article ">Figure 17
<p>Velocity distributions and tip vortex structure of flow field at different pitching angles.</p>
Full article ">Figure 18
<p>Sketch of forces on a flapping foil.</p>
Full article ">Figure 19
<p>Velocity cloud diagrams and tip vortex structures of flow fields at different heave amplitudes.</p>
Full article ">Figure 20
<p>Flow field vortex structure of a semi-active flapping foil with different spring stiffnesses.</p>
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<p>Comparison of AoA time-history curves at different pitch amplitudes.</p>
Full article ">Figure 22
<p>AoA duration curves of a semi-active flapping foil with different spring stiffnesses. (<b>a</b>) <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>α</mi> </mrow> <mrow> <mi>m</mi> <mi>a</mi> <mi>x</mi> </mrow> </msub> <mo>=</mo> <mn>0.18</mn> <mtext> </mtext> <mi mathvariant="normal">r</mi> <mi mathvariant="normal">a</mi> <mi mathvariant="normal">d</mi> </mrow> </semantics></math>, (<b>b</b>) <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>α</mi> </mrow> <mrow> <mi>m</mi> <mi>a</mi> <mi>x</mi> </mrow> </msub> <mo>=</mo> <mn>0.5</mn> <mtext> </mtext> <mi mathvariant="normal">r</mi> <mi mathvariant="normal">a</mi> <mi mathvariant="normal">d</mi> </mrow> </semantics></math>.</p>
Full article ">Figure 23
<p>Pitch motion and AoA time-history curves of a semi-active flapping foil (<math display="inline"><semantics> <mrow> <msup> <mi>K</mi> <mo>′</mo> </msup> <mo>=</mo> <mn>0.8</mn> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>α</mi> </mrow> <mrow> <mi>m</mi> <mi>a</mi> <mi>x</mi> </mrow> </msub> <mo>=</mo> <mn>0.18</mn> <mo>,</mo> <mtext> </mtext> <mn>0.5</mn> <mtext> </mtext> <mi mathvariant="normal">r</mi> <mi mathvariant="normal">a</mi> <mi mathvariant="normal">d</mi> </mrow> </semantics></math>).</p>
Full article ">
18 pages, 4036 KiB  
Article
Theoretical Research and Numerical Analysis of a New Assembled Shuttle-Shaped Self-Centering Mild Steel Energy Dissipation Brace
by Yao Chen, Zhonghua Liu and Jianchao Zhao
Buildings 2024, 14(10), 3285; https://doi.org/10.3390/buildings14103285 - 17 Oct 2024
Abstract
To solve the problem of large residual deformation and high repair cost of traditional frame structures after an earthquake, a new type of assembled shuttle-shaped self-centering mild steel energy dissipation brace (ASSSEDB) with stable stiffness, material saving, and easy replacement was proposed. The [...] Read more.
To solve the problem of large residual deformation and high repair cost of traditional frame structures after an earthquake, a new type of assembled shuttle-shaped self-centering mild steel energy dissipation brace (ASSSEDB) with stable stiffness, material saving, and easy replacement was proposed. The plastic deformation of mild steel is used to dissipate energy, and the disc spring system provides a reset function. Based on the working mechanism of energy dissipation brace, a restoring force model for the ASSSEDB was established, and then the numerical analysis was carried out by ANSYS to verify the accuracy of the proposed model. The results confirm that the ASSSEDB has stable energy dissipation ability and a resetting function, with a full hysteresis curve. The finite element analysis results align well with the developed restoring force model, and the maximum deviations of initial stiffness and ultimate capacity are, respectively, 1.4% and 2.3%, which indicates that the established restoring force model can provide a theoretical basis for design of the ASSSEDB. Furthermore, the time history analysis was carried out to assess the seismic performance of a six-story steel frame structure using the proposed ASSSEDB. The results show that compared with the steel frame structure with BRBs, the proposed ASSSEDB can decrease the residual deformation of structures by up to 93.41%. The self-centering ratio of the ASSSEDB is crucial in controlling residual deformation of structures, and it is recommended to be greater than 1.0. Full article
(This article belongs to the Section Building Structures)
Show Figures

Figure 1

Figure 1
<p>Structural details of the ASSSEDB. 1. guide rod; 2. pre-tightening nut; 3. disc spring; 4. shuttle-shaped tube; 5. mild steel energy dissipation element; 6. energy dissipation fixing piece; 7. cavity body; 8. ear plate; 9. middle enclosed cavity; 10. fixed baffle; 11. end cavity.</p>
Full article ">Figure 2
<p>Bilinear model of the mild steel energy dissipation element system.</p>
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<p>Restoring force model of disc spring system.</p>
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<p>Restoring force model of the ASSSEDB.</p>
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<p>Loading setup of experiment in Amadeo et al. [<a href="#B36-buildings-14-03285" class="html-bibr">36</a>].</p>
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<p>Comparison of Amadeo et al.’s [<a href="#B36-buildings-14-03285" class="html-bibr">36</a>] experimental results and numerical analysis results.</p>
Full article ">Figure 7
<p>Finite element model of ASSSEDB.</p>
Full article ">Figure 8
<p>Comparison of finite element model results with restoring force model results.</p>
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<p>Plan and elevation of braced steel frame structure. (<b>a</b>) Structural plan (unit: mm); (<b>b</b>) Structural elevation (unit: mm).</p>
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<p>Plan and elevation of braced steel frame structure. (<b>a</b>) Structural plan (unit: mm); (<b>b</b>) Structural elevation (unit: mm).</p>
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<p>Numerical model of braced steel frame structure.</p>
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<p>Story drift of structures. (<b>a</b>) 70 gal; (<b>b</b>) 200 gal; (<b>c</b>) 400 gal; (<b>d</b>) BRB; (<b>e</b>) FAR.</p>
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<p>Residual deformation of structures. (<b>a</b>) 70 gal; (<b>b</b>) 200 gal; (<b>c</b>) 400 gal; (<b>d</b>) BRB.</p>
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<p>Initial stiffness of ASSSEDB. (<b>a</b>) Maximum displacement; (<b>b</b>) Story drift; (<b>c</b>) Residual deformation.</p>
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<p>Self-centering ratio of ASSSEDB. (<b>a</b>) Maximum displacement; (<b>b</b>) Story drift; (<b>c</b>) Residual deformation.</p>
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11 pages, 505 KiB  
Article
Robustness Assessment of Oncology Dose-Finding Trials Using the Modified Fragility Index
by Amy X. Shi, Heng Zhou, Lei Nie, Lifeng Lin, Hongjian Li and Haitao Chu
Cancers 2024, 16(20), 3504; https://doi.org/10.3390/cancers16203504 - 17 Oct 2024
Viewed by 158
Abstract
Objectives: The sample sizes of phase I trials are typically small; some designs may lead to inaccurate estimation of the maximum tolerated dose (MTD). The objective of this study was to propose a metric assessing whether the MTD decision is sensitive to enrolling [...] Read more.
Objectives: The sample sizes of phase I trials are typically small; some designs may lead to inaccurate estimation of the maximum tolerated dose (MTD). The objective of this study was to propose a metric assessing whether the MTD decision is sensitive to enrolling a few additional subjects in a phase I dose-finding trial. Methods: Numerous model-based and model-assisted designs have been proposed to improve the efficiency and accuracy of finding the MTD. The Fragility Index (FI) is a widely used metric quantifying the statistical robustness of randomized controlled trials by estimating the number of events needed to change a statistically significant result to non-significant (or vice versa). We propose a modified Fragility Index (mFI), defined as the minimum number of additional participants required to potentially change the estimated MTD, to supplement existing designs identifying fragile phase I trial results. Findings: Three oncology trials were used to illustrate how to evaluate the fragility of phase I trials using mFI. The results showed that two of the trials were not sensitive to additional subjects’ participation while the third trial was quite fragile to one or two additional subjects. Conclusions: The mFI can be a useful metric assessing the fragility of phase I trials and facilitating robust identification of MTD. Full article
(This article belongs to the Special Issue Application of Biostatistics in Cancer Research)
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<p>Flowchart of Calculating the modified Fragility Index in a Dose-Finding Trial.</p>
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22 pages, 2438 KiB  
Article
Applying a Comprehensive Model for Single-Ring Infiltration: Assessment of Temporal Changes in Saturated Hydraulic Conductivity and Physical Soil Properties
by Mirko Castellini, Simone Di Prima, Luisa Giglio, Rita Leogrande, Vincenzo Alagna, Dario Autovino, Michele Rinaldi and Massimo Iovino
Water 2024, 16(20), 2950; https://doi.org/10.3390/w16202950 - 16 Oct 2024
Viewed by 304
Abstract
Modeling agricultural systems, from the point of view of saving and optimizing water, is a challenging task, because it may require multiple soil physical and hydraulic measurements to investigate the entire crop cycle. The Beerkan method was proposed as a quick and easy [...] Read more.
Modeling agricultural systems, from the point of view of saving and optimizing water, is a challenging task, because it may require multiple soil physical and hydraulic measurements to investigate the entire crop cycle. The Beerkan method was proposed as a quick and easy approach to estimate the saturated soil hydraulic conductivity, Ks. In this study, a new complete three-dimensional model for Beerkan experiments recently proposed was used. It consists of thirteen different calculation approaches that differ in estimating the macroscopic capillary length, initial (θi) and saturated (θs) soil water contents, use transient or steady-state infiltration data, and different fitting methods to transient data. A steady-state version of the simplified method based on a Beerkan infiltration run (SSBI) was used as the benchmark. Measurements were carried out on five sampling dates during a single growing season (from November to June) in a long-term experiment in which two soil management systems were compared, i.e., minimum tillage (MT) and no tillage (NT). The objectives of this work were (i) to test the proposed new model and calculation approaches under real field conditions, (ii) investigate the impact of MT and NT on soil properties, and (iii) obtain information on the seasonal variability of Ks and other main soil physical properties (θi, soil bulk density, ρb, and water retention curve) under MT and NT. The results showed that the model always overestimated Ks compared to SSBI. Indeed, the estimated Ks differed by a factor of 11 when the most data demanding (A1) approach was considered by a factor of 4–8, depending on the transient or steady-state phase use, when A3 was considered and by a practically negligible factor of 1.0–1.9 with A4. A relatively higher seasonal variability was detected for θi at the MT than NT system. Under both MT and NT, ρb did not change between November and April but increased significantly until the end of the season. The selected calculation approaches provided substantially coherent information on Ks seasonal evolution. Regardless of the approach, the results showed a temporal stability of Ks at least from early April to June under NT; conversely, the MT system was, overall, more affected by temporal changes with a relative stability at the beginning and middle of the season. These findings suggest that a common sampling time for determining Ks could be set at early spring. Soil management affected the soil properties, because the NT system was significantly wetter and more compact than MT on four out of five dates. However, only NT showed a significantly increasing correlation between Ks and the modal pore diameter, suggesting the presence of a relatively smaller and better interconnected pore network in the no-tilled soil. This study confirms the need to test infiltration models under real field conditions to evaluate their pros and cons. The Beerkan method was effective for intensive soil sampling and accurate field investigations on the temporal variability of Ks. Full article
(This article belongs to the Special Issue Soil Dynamics and Water Resource Management)
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<p>Timeline of the field measurements (i.e., Beerkan infiltration tests and soil sampling) carried out under minimum tillage (MT) and no tillage (NT) plots in the 5 sampling dates (i.e., from 1 to 5). Numbers marked with lowercase or uppercase green letters represent the number of days elapsed between the beginning and the end of a single sampling date (d) and the time between two successive sampling dates (D). The daily rainfall was reported as a black continuous line.</p>
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<p>Box plots of soil water content at the time of sampling (θ<span class="html-italic"><sub>i</sub></span>) and soil bulk density (ρ<sub>b</sub>) carried out for each sampling date (1 to 5) under minimum tillage (MT) and no tillage (NT). The thick red–green line within each box represents the mean value (the fine black line, the median); for improved interpretation, mean values are also reported by numbers. Circles represent outliers. For a given soil management, inferences of the THSD-test between dates (i.e., x vs. y) are summarized on the right (* <span class="html-italic">p</span> &lt; 0.05; ** <span class="html-italic">p</span> &lt; 0.01; n.s. not significant). For a given sampling date, inferences of the two tailed <span class="html-italic">t</span>-test between MT and NT were reported under the NT boxes (* <span class="html-italic">p</span> &lt; 0.05; n.s. not significant).</p>
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<p>Mean values of the measured soil water retention data (Obs) for each sampling time (1 to 5) for minimum tillage (MT) and no tillage (NT) systems. The Brooks and Corey (BC) fitting curve (lines) are also reported (sample size, <span class="html-italic">N,</span> was between 5 and 12).</p>
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<p>Cumulative infiltration carried out under minimum tillage and no tillage plots (MT and NT) during the five sampling dates. Note that mean curves were represented with black-red dashed lines.</p>
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<p>Success percentage of saturated hydraulic conductivity estimation obtained with the five calculation approaches (A1 to A5). The acronyms CI, CL, and DL refer to fitting methods used to analyze the transient-state data (i.e., cumulative infiltration, cumulative linearization, and differential linearization, respectively), while SS refers to steady-state data. A1 to A4 refer to the Stewart and Abou Najm [<a href="#B35-water-16-02950" class="html-bibr">35</a>] model, while A5 refers to the SSBI method (Bagarello et al. [<a href="#B51-water-16-02950" class="html-bibr">51</a>]). Note that, for each soil management, the sample size N = 34 refers to the sum of the five sampling dates.</p>
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<p>Empirical cumulative frequency distribution of the saturated hydraulic conductivity (<span class="html-italic">K<sub>s</sub></span>) obtained from different calculation criteria and considering the minimum dataset (N = 44).</p>
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<p>Comparison between estimated <span class="html-italic">K<sub>s</sub></span> values obtained with A5 criterion (<span class="html-italic">K<sub>s</sub></span>–A5) against the calculation criteria A1, A3, and A4 and different fitting methods CI, CL, and DL (<span class="html-italic">K<sub>s</sub></span>–A<sub>n</sub>) using the minimum dataset (N = 44).</p>
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<p>Box plots of saturated hydraulic conductivity (<span class="html-italic">K<sub>s</sub></span>) at different sampling dates for minimum tillage (MT) and no tillage (NT) management systems conducted using the A1, A3<sub>SS</sub>, and A5 (SSBI) approaches. For a given soil management, inferences of the THSD test between dates (i.e., x vs. y) are summarized on the right (* <span class="html-italic">p</span> &lt; 0.05; ** <span class="html-italic">p</span> &lt; 0.01; n.s. not significant). For a given sampling date, inferences of the two tailed <span class="html-italic">t</span>-test between MT and NT were reported near NT boxes (* <span class="html-italic">p</span> &lt; 0.05; n.s. not significant). For the general interpretation on box plots, please refer to the captions in <a href="#water-16-02950-f002" class="html-fig">Figure 2</a>. Note that the discrepancies regarding the statistical significances among the three calculation criteria are shown with red character.</p>
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<p>Ratio of saturated hydraulic conductivity obtained with approaches A1 and A5 (SSBI) against the relative error of the fitting of the functional relationships to the experimental data (<b>a</b>), and examples of fitting accuracy for the minimum (Er<sub>FIT</sub> = 1.8%; experiment MT1-SD3) (<b>b</b>), intermediate (Er<sub>FIT</sub> = 15.8%; NT1-SD3) (<b>c</b>), and maximum (Er<sub>FIT</sub> = 31.7%; NT5-SD5) (<b>d</b>) values, as labeled in subpanel (<b>a</b>) (black-edged points). The black continuous regression line corresponds to the whole set of data.</p>
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<p>Normalized pore volume distributions and corresponding modal diameters (continuous and dotted lines, respectively) for the first (1) and last (5) sampling dates under no tillage, NT, and minimum tillage, MT (<b>a</b>), and a correlation between the saturated hydraulic conductivity (<span class="html-italic">K<sub>s</sub></span>) and modal pores diameter (<span class="html-italic">d<sub>mode</sub></span>) for all sampling dates (<b>b</b>). Note that the <span class="html-italic">K<sub>s</sub></span> values refer to the medians obtained with Approach 5 (SSBI).</p>
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13 pages, 225 KiB  
Article
The Effect of Course Delivery Mode on Student Performance and Student Satisfaction: A Case Study
by Johannes Reichgelt and Tim C. Smith
Trends High. Educ. 2024, 3(4), 872-884; https://doi.org/10.3390/higheredu3040050 - 16 Oct 2024
Viewed by 274
Abstract
There is an ongoing debate in the halls of traditional universities about the effectiveness of course delivery modes other than face-to-face instruction. This paper reports on a natural experiment that we were able to conduct in Spring 2022 as we offered the same [...] Read more.
There is an ongoing debate in the halls of traditional universities about the effectiveness of course delivery modes other than face-to-face instruction. This paper reports on a natural experiment that we were able to conduct in Spring 2022 as we offered the same course to similar student populations in three different delivery modes (face-to-face, synchronously online via Teams, and asynchronously online). While about a quarter of the students who responded to a survey about their preferred delivery mode who were not enrolled in a face-to-face class indicated that they preferred a face-to-face class, the experiment did not find any differences between the three groups in terms of their assessment of teaching or in their performance both in the course overall or in the individual assignments in the course. While the experiment may suffer some shortcomings, the results indicate that a well-designed online course, delivered synchronously or asynchronously, may encourage student learning more effectively than a face-to-face course. Full article
16 pages, 6843 KiB  
Article
Seasonal–Diurnal Distribution of Lightning over Bulgaria and the Black Sea and Its Relationship with Sea Surface Temperature
by Savka Petrova, Rumjana Mitzeva, Vassiliki Kotroni and Elisaveta Peneva
Atmosphere 2024, 15(10), 1233; https://doi.org/10.3390/atmos15101233 (registering DOI) - 15 Oct 2024
Viewed by 181
Abstract
A seasonal–diurnal analysis of land-sea contrast in lightning activity over Bulgaria and the Black Sea over 10 years is presented here. The maximum number of flashes over both surface types is registered during the summer (with a peak over Bulgaria in June and [...] Read more.
A seasonal–diurnal analysis of land-sea contrast in lightning activity over Bulgaria and the Black Sea over 10 years is presented here. The maximum number of flashes over both surface types is registered during the summer (with a peak over Bulgaria in June and over the Black Sea in July) and a minimum number in winter (December/February, respectively). During spring, the maximum flash density is observed over Bulgaria (in May), while in autumn, it is over the Black Sea (in September). The results show that only in autumn lightning activity dominates over the Black Sea compared to over land (Bulgaria), while in winter, spring, and summer is vice versa. For this reason, an additional investigation was conducted to determine whether there is a relationship between lightning activity and the sea surface temperature (SST) of the Black Sea in autumn. The analysis reveals that the influence of SST on the formation of thunderstorms over the Black Sea varies depending on the diurnal time interval, with the effect being more significant at night. At nighttime intervals, there is a clear trend of increasing mean flash frequency per case with rising SST (linear correlation coefficients range from R = 0.92 to 0.98), while during the daytime, this trend is not as evident. This indicates that, during the day, other favorable atmospheric processes have a greater influence on the formation of thunderstorms than sea-surface temperature, while in the autumn night hours, the higher SST values probably play a more significant role in thunderstorms formation, in combination with the corresponding orographic conditions. Full article
(This article belongs to the Special Issue Atmospheric Electricity (2nd Edition))
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<p>Elevation [m] in the studied area. Positive numbers represent the elevation above the sea level, negative numbers—below the sea level. The data are taken from the GEBCO 1-min global grid (<a href="http://www.gebco.net" target="_blank">www.gebco.net</a>, accessed on 1 May 2022).</p>
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<p>Spatial distribution of the number of recorded flashes within 0.25° × 0.25° grid boxes over Bulgaria and the Black Sea during winter (<b>a</b>), spring (<b>b</b>), summer (<b>c</b>), and autumn (<b>d</b>) from March 2005 to February 2015. The color scale represents the number of flashes; note that the scale is different in each season.</p>
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<p>Flash density (flashes/km<sup>2</sup>) over the Black Sea (blue columns) and Bulgaria (white columns) during winter (DJF), spring (MAM), summer (JJA), and autumn (SON) from March 2005 to February 2015.</p>
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<p>Flash density (flashes/km<sup>2</sup>) for months in winter (<b>a</b>), spring (<b>b</b>), summer (<b>c</b>), and autumn (<b>d</b>) over the Black Sea (blue columns) and Bulgaria (white columns), March 2005–February 2015.</p>
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<p>Diurnal variation of flash density (flashes/km<sup>2</sup>) at 3-h time intervals during winter (<b>a</b>), spring (<b>b</b>), summer (<b>c</b>), and autumn (<b>d</b>) over the Black Sea (blue columns) and Bulgaria (white columns) from March 2005 to February 2015. Local time is UTC + 2 h or UTC + 3 h.</p>
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<p>Diurnal spatial distribution of the number of flashes at 3-h time intervals in boxes of 0.25 × 0.25 degrees for each season: (<b>a</b>)—winter (DFJ), (<b>b</b>)—spring (MAM), (<b>c</b>)—summer (JJA), (<b>d</b>)—autumn (SON) of the 10 years (Marth 2005–February 2015). The color scale represents the number of flashes; note that the scale is different in each season. Local time is UTC + 2 h or UTC + 3 h.</p>
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<p>Spatial distribution of number of recorded flashes in boxes of 0.25° × 0.25° over Bulgaria and the Black Sea for September (2005–2014).</p>
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<p>Mean values of sea surface temperature (SST) for September (2005–2014).</p>
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<p>Box and Whisker plot of the sea surface temperature (SST) for the cases with and without flashes for all four investigated time-intervals from September months. (median-blue line; 25th–75th percentile, blue box; 10th–90th percentile). LT = UTC + 3 h.</p>
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<p>Box and Whisker plot of the flash frequency (number of lightning per case) as a function of sea surface temperature (SST) during nighttime intervals ((1800–2100) UTC; (0000–0300) UTC) and daytime intervals ((0600–0900) UTC; (1200–1500) UTC). (trend line of: mean—red line, median—yellow line; 25th–75th percentile, blue box; 10th–90th percentile, whisker; the value in blue box is number of cloud cases). LT = UTC + 3 h. The analysis includes the September months of the period 2005–2014.</p>
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<p>Spatial–diurnal distribution of flashes at 3-h time intervals: nighttime (1800–2100) UTC, (0000–0300) UTC and daytime (0600–0900) UTC, (1200–1500) UTC for the September months (2005–2014). LT = UTC + 3 h.</p>
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22 pages, 1409 KiB  
Review
Studies on Heavy Precipitation in Portugal: A Systematic Review
by José Cruz, Margarida Belo-Pereira, André Fonseca and João A. Santos
Climate 2024, 12(10), 163; https://doi.org/10.3390/cli12100163 (registering DOI) - 15 Oct 2024
Viewed by 355
Abstract
This systematic review, based on an adaptation of the Preferred Reporting Items for Systematic Reviews and Meta-Analyses (PRISMA) statement from 2020, focuses on studies of the atmospheric mechanisms underlying extreme precipitation events in mainland Portugal, as well as observed trends and projections. The [...] Read more.
This systematic review, based on an adaptation of the Preferred Reporting Items for Systematic Reviews and Meta-Analyses (PRISMA) statement from 2020, focuses on studies of the atmospheric mechanisms underlying extreme precipitation events in mainland Portugal, as well as observed trends and projections. The 54 selected articles cover the period from 2000 to 2024, in which the most used keywords are “portugal” and “extreme precipitation”. Of the 54, 23 analyse trends and climate projections of precipitation events, confirming a decrease in total annual precipitation, especially in autumn and spring, accompanied by an increase in the frequency and intensity of extreme precipitation events in autumn, spring and winter. Several articles (twelve) analyse the relationship between synoptic-scale circulation and heavy precipitation, using an atmospheric circulation types approach. Others (two) establish the link with teleconnection patterns, namely the North Atlantic Oscillation (NAO), and still others (three) explore the role of atmospheric rivers. Additionally, five articles focus on evaluating databases and Numerical Weather Prediction (NWP) models, and nine articles focus on precipitation-related extreme weather events, such as tornadoes, hail and lightning activity. Despite significant advances in the study of extreme precipitation events in Portugal, there is still a lack of studies on hourly or sub-hourly scales, which is critical to understanding mesoscale, short-lived events. Several studies show NWP models still have limitations in simulating extreme precipitation events, especially in complex orography areas. Therefore, a better understanding of such events is fundamental to promoting continuous improvements in operational weather forecasting and contributing to more reliable forecasts of such events in the future. Full article
(This article belongs to the Section Weather, Events and Impacts)
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<p>Map of the NUT II administrative divisions of mainland Portugal, and the main rivers.</p>
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<p>Scheme of the methodology applied in the current systematic literature review.</p>
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<p>PRISMA flow diagram of the systematic literature review search adapted from [<a href="#B29-climate-12-00163" class="html-bibr">29</a>].</p>
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<p>Temporal distribution of articles included in the systematic review by publication year.</p>
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<p>Constructed Author’s Keywords (DE) co-occurrence network, used at least twice, using VOSviewer.</p>
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21 pages, 8586 KiB  
Article
Solute Transport in a Multi-Channel Karst System with Immobile Zones: An Example of Downtown Salado Spring Complex, Salado, Texas
by Toluwaleke Ajayi, Joe C. Yelderman and Stephen M. Powers
Water 2024, 16(20), 2928; https://doi.org/10.3390/w16202928 (registering DOI) - 15 Oct 2024
Viewed by 281
Abstract
To investigate the influence of flow rate increment on the solute transport parameter of immobile zones in a karst system, a dye tracer test was conducted in the Downtown Salado Spring Complex (DSSC) comprising three springs: Big Boiling, Anderson, and Doc Benedict springs. [...] Read more.
To investigate the influence of flow rate increment on the solute transport parameter of immobile zones in a karst system, a dye tracer test was conducted in the Downtown Salado Spring Complex (DSSC) comprising three springs: Big Boiling, Anderson, and Doc Benedict springs. The Multiflow two-region nonequilibrium model (2RNE) was used to simulate the breakthrough curve (BTC) of the springs, and changes in the solute transport parameters in response to flow rate increment were observed. The simulation result showed that the 2RNE model was capable of reproducing the BTC of all the DSSC springs, with an R-squared value greater than 0.9 in all flow rate increment scenarios. The research demonstrates that a positive correlation will exist between the flow rate and solute transport parameter of the immobile zones if the tracer transport to the spring is truly influenced by immobile zones. In contrast, a negative correlation will exist between the flow rate and mass transfer coefficient if the immobile zone has less influence. Overall, the research provides insights into contaminant movement in karst by documenting how tracers are retained in the immobile fluid zone. Full article
(This article belongs to the Section Hydrogeology)
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<p>Illustration of flow within karst conduit. The tracer in the mobile fluid zone is transported by advection (mobile fluid velocity, <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>V</mi> </mrow> <mrow> <mi>m</mi> </mrow> </msub> </mrow> </semantics></math>) and dispersion (<math display="inline"><semantics> <mrow> <msub> <mrow> <mi>D</mi> </mrow> <mrow> <mi>m</mi> </mrow> </msub> </mrow> </semantics></math>). The partition coefficient <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">ψ</mi> </mrow> </semantics></math> accounts for the proportion of mobile zones while the mass transfer coefficient ω accounts for the mass exchange between the mobile and immobile fluid zones.</p>
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<p>A stratigraphic section that cuts across the Northern Segment of the Edward BFZ aquifer [<a href="#B47-water-16-02928" class="html-bibr">47</a>]. The red box represents the location of the study area, which shows that the Edwards limestone crops out at the surface and is considered the aquifer unit.</p>
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<p>Geologic map of the Northern Segment of the Edward BFZ aquifer, modified after Wong and Yelderman [<a href="#B47-water-16-02928" class="html-bibr">47</a>]. The DSSC study area is shown in the red box.</p>
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<p>Satellite imagery of the springs in the Downtown Salado Spring Complex (DSSC). The DSSC springs are Big Boiling Spring, Anderson Spring, and Doc Benedict Spring. The springs are all indicated by red circles, while the blue triangle shows the location of the cave well in the area.</p>
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<p>A schematic representation of the multiflow modeling approach incorporated into the MFIT model program [<a href="#B36-water-16-02928" class="html-bibr">36</a>]. The transport of the tracers from injection to the detection point is assumed to occur via a flow network that consists of N-independent one-dimensional channels. Each of the channels represents fractures and conduits through which solute is transported into karst springs and the model assumes that there is no mass exchange between each of the channels. In other words, the channels are independent of each other. Using solute transport analytical equations from the 2RNE incorporated into the MFIT program, the model can define the solute transport parameters for each channel.</p>
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<p>(<b>a</b>) Breakthrough curves of Anderson Spring, (<b>b</b>) breakthrough curve of Doc Benedict Spring, and (<b>c</b>) breakthrough curve of Big Boiling Spring. The blue and green line plot represents the observed rhodamine concentration and the percentage of dye recovery, respectively.</p>
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<p>Model output for a flow rate of 72 m<sup>3</sup>/h for Doc Benedict Spring.</p>
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<p>2RNE Modeling output for flow rate variation for Doc Benedict Spring: (<b>a</b>) model output for a flow rate of 77 m<sup>3</sup>/h, (<b>b</b>) model output for a flow rate of 82 m<sup>3</sup>/h, (<b>c</b>) model output for a flow rate of 87 m<sup>3</sup>/h, and (<b>d</b>) model output for a flow rate of 92 m<sup>3</sup>/h.</p>
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<p>Correlation plot for Doc Benedict Spring (<b>a</b>) correlation between Q and <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">ψ</mi> </mrow> </semantics></math>, (<b>b</b>) correlation between Q and <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">ω</mi> </mrow> </semantics></math>, and (<b>c</b>) correlation between Q and D.</p>
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<p>2RNE Modeling output for flow rate variation for Anderson Spring: (<b>a</b>) model output at a flow rate of 136 m<sup>3</sup>/h, (<b>b</b>) model output at a flow rate of 141 m<sup>3</sup>/h, (<b>c</b>) model output at a flow rate of 146 m<sup>3</sup>/h, and (<b>d</b>) model output at a flow rate of 151 m<sup>3</sup>/h.</p>
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<p>Correlation plot for Anderson Spring: (<b>a</b>) correlation between Q and D, (<b>b</b>) correlation between Q and <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">ω</mi> </mrow> </semantics></math>, and (<b>c</b>) correlation between Q and <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">ψ</mi> </mrow> </semantics></math>.</p>
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<p>2RNE Modeling output for flow rate variation for Big Boiling Spring: (<b>a</b>) model output at a flow rate of 1069 m<sup>3</sup>/h, (<b>b</b>) model output at a flow rate of 1074 m<sup>3</sup>/h, (<b>c</b>) model output at a flow rate of 1079 m<sup>3</sup>/h, and (<b>d</b>) model output at a flow rate of 1084 m<sup>3</sup>/h.</p>
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<p>Correlation plot for Big Boiling Spring (<b>a</b>) correlation between Q and D, (<b>b</b>) correlation between Q and <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">ω</mi> </mrow> </semantics></math>, and (<b>c</b>) correlation between Q and <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">ψ</mi> </mrow> </semantics></math>.</p>
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16 pages, 5433 KiB  
Article
The Effect of Hive Type on Colony Homeostasis and Performance in the Honey Bee (Apis mellifera)
by Rola Kutby, Barbara Baer-Imhoof, Samuel Robinson, Lucy Porter and Boris Baer
Insects 2024, 15(10), 800; https://doi.org/10.3390/insects15100800 - 14 Oct 2024
Viewed by 263
Abstract
The colonies of honey bees are mostly sessile organisms. Consequently, the type of nest boxes that beekeepers provide to their bees should impact a colony’s ability to maintain homeostasis, which is a key determinant of performance and fitness. Here, we used European honey [...] Read more.
The colonies of honey bees are mostly sessile organisms. Consequently, the type of nest boxes that beekeepers provide to their bees should impact a colony’s ability to maintain homeostasis, which is a key determinant of performance and fitness. Here, we used European honey bees (Apis mellifera) and provided them with two hive setups widely used and known as Langstroth and Warré. We compared colony performance in a Mediterranean climate for five months from late spring to early autumn, which covered the most active time of bees and included periods of heat and drought. We found that irrespective of hive type or season, honey bees kept hive temperature and humidity within a remarkably narrow range. Nevertheless, the hive type impacted the daily fluctuations in temperature and humidity. In Warré hives, where bees have more autonomy to build and maintain their combs, we found that bees were able to reduce daily fluctuations in temperature and humidity and kept both measures closer to the overall average. This increase in colony homeostasis found in Warré hives negatively correlated with other hive performance indicators, such as immunocompetence. We conclude that different hive types affect key areas, such as the central part of the colony with frames of developing brood or the queen, which are the most susceptible individuals. This implies that climatic changes resulting in extreme weather events are expected to impact colony performance and fitness, especially in non-managed honey bees that are limited by available nesting sites. For managed bees, adaptations to existing hive setups could be provided to help bees minimize the effects of abiotic stress. Full article
(This article belongs to the Section Insect Societies and Sociality)
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<p>The solid red lines provide mean hive temperatures during the experiment in °C ± 95% CI, measured in the brood area of either Langstroth (<b>left panels</b>) or Warré (<b>right panels</b>) hives. The corresponding outside temperatures are provided as dotted red lines. Temperatures recorded at 9:00 a.m. are shown in the upper and those collected at 3:00 p.m. in the lower panels. The blue bar provides the corresponding medians ± 95% CI calculated for each hive type and time of the day.</p>
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<p>Mean hive temperatures in °C (±95% CI) at 9:00 a.m. and 3:00 p.m. for honey bee colonies kept in Langstroth (white bars) and Warré (grey bars) hives. The horizontal red bar shows the overall median ± 95% CI. Mean temperatures differed between hive types as well as the time of the day as indicated by a significant hive type × time of the day interaction term (ANOVA, hive type × time of day interaction, F<sub>1, 1521</sub> = 22.79, <span class="html-italic">p</span> &lt; 0.001). The three asterisks (***) indicate levels of significance between groups where <span class="html-italic">p</span> values are &lt; 0.001.</p>
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<p>The solid blue lines show relative humidity (RH) (mean ± 95% CI) of honey bee colonies kept in Langstroth (<b>left panels</b>) and Warré (<b>right panels</b>) hives in the mornings (<b>upper panels</b>) and afternoons (<b>lower panels</b>). Corresponding outside RH is provided by the dotted blue lines. The horizontal red bars show the overall median ± 95% CI for each hive type and time of the day.</p>
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<p>Mean relative humidity (RH) in % ± 95% CI in honey bee hives at 9:00 a.m. and 3:00 p.m. in Langstroth (white bars) and Warré (grey bars) hives. The horizontal red bar shows the overall median ± 95% CI. Mean relative humidity was lower in Warré hives, but the difference was larger in the afternoons compared to the mornings (ANOVA, hive type × time of day interaction, F<sub>1, 1521</sub> = 12.36, <span class="html-italic">p</span> &lt; 0.001. The three asterisks (***) indicate levels of significance between groups where <span class="html-italic">p</span> values are &lt; 0.001.</p>
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<p>Blue solid lines show mean ± 95% CI absolute humidity (AH) in Langstroth (<b>left panels</b>) and Warre (<b>right panels</b>) hives; the corresponding outside AH is provided by the dotted blue line. Upper panels show morning data at 9:00 a.m. and lower panels at 3:00 p.m. The horizontal red bar represent the corresponding median ± 95% CI calculated for each hive type and time of the day separately.</p>
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<p>Mean absolute humidity (AH) ± 95% confidence interval in the brood area of Langstroth (white bars) and Warré hives (grey bars) in the morning (<b>left side</b>) and afternoon (<b>right side</b>). The horizontal red bar represent the overall median ± 95% CI. Mean absolute humidity was lower in Warre hives, but the difference was larger in the afternoons compared to the mornings (ANOVA, Hive type × Time of the day interaction, F<sub>1, 1521</sub> = 50.02, <span class="html-italic">p</span> &lt; 0.001). The three asterisks (***) indicate levels of significance between groups where <span class="html-italic">p</span> values are &lt; 0.001.</p>
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<p>The white bars represent data collected from Langstroth hives, and the gray bars represent data from Warré hives. (<b>a</b>) Mean ± 95% CI encapsulation response of bees was higher at the start than at the end of the experiment (ANOVA, F<sub>1, 156</sub> = 41.74, <span class="html-italic">p</span> &lt; 0.001) and higher in bees collected from Langstroth-compared to Warré hives. The latter was significant for the bees we collected at the end of the experiment (ANOVA, F<sub>2, 12</sub> = 39.28, <span class="html-italic">p</span> &lt; 0.05). (<b>b</b>) All colonies gained weight during the experiment irrespectively of hive type (ANOVA, F<sub>2, 12</sub> = 39.28, <span class="html-italic">p</span> &lt; 0.001. (<b>c</b>) The mean area of wax comb in Langstroth and Warré hives was significantly higher at the end (Day 130) of the experiment compared to the start (ANOVA, F<sub>1, 6</sub> = 129.62, <span class="html-italic">p</span> &lt; 0.001). The increase in wax comb area differed between the two hive types (ANOVA, F<sub>1, 6</sub> = 53.94, <span class="html-italic">p</span> &lt; 0.001. (<b>d</b>) Langstroth hives stored more honey at the end of the experiment compared to Warré hives but the difference was not statistically significant. A single asterisk (*) indicates statical differences where <span class="html-italic">p</span> &lt; 0.05 while three asterixis (***) are used to indicate <span class="html-italic">p</span> values &lt; 0.001.</p>
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26 pages, 3516 KiB  
Article
Early Cervical Cancer Diagnosis with SWIN-Transformer and Convolutional Neural Networks
by Foziya Ahmed Mohammed, Kula Kekeba Tune, Juhar Ahmed Mohammed, Tizazu Alemu Wassu and Seid Muhie
Diagnostics 2024, 14(20), 2286; https://doi.org/10.3390/diagnostics14202286 - 14 Oct 2024
Viewed by 251
Abstract
Introduction: Early diagnosis of cervical cancer at the precancerous stage is critical for effective treatment and improved patient outcomes. Objective: This study aims to explore the use of SWIN Transformer and Convolutional Neural Network (CNN) hybrid models combined with transfer learning to classify [...] Read more.
Introduction: Early diagnosis of cervical cancer at the precancerous stage is critical for effective treatment and improved patient outcomes. Objective: This study aims to explore the use of SWIN Transformer and Convolutional Neural Network (CNN) hybrid models combined with transfer learning to classify precancerous colposcopy images. Methods: Out of 913 images from 200 cases obtained from the Colposcopy Image Bank of the International Agency for Research on Cancer, 898 met quality standards and were classified as normal, precancerous, or cancerous based on colposcopy and histopathological findings. The cases corresponding to the 360 precancerous images, along with an equal number of normal cases, were divided into a 70/30 train–test split. The SWIN Transformer and CNN hybrid model combines the advantages of local feature extraction by CNNs with the global context modeling by SWIN Transformers, resulting in superior classification performance and a more automated process. The hybrid model approach involves enhancing image quality through preprocessing, extracting local features with CNNs, capturing the global context with the SWIN Transformer, integrating these features for classification, and refining the training process by tuning hyperparameters. Results: The trained model achieved the following classification performances on fivefold cross-validation data: a 94% Area Under the Curve (AUC), an 88% F1 score, and 87% accuracy. On two completely independent test sets, which were never seen by the model during training, the model achieved an 80% AUC, a 75% F1 score, and 75% accuracy on the first test set (precancerous vs. normal) and an 82% AUC, a 78% F1 score, and 75% accuracy on the second test set (cancer vs. normal). Conclusions: These high-performance metrics demonstrate the models’ effectiveness in distinguishing precancerous from normal colposcopy images, even with modest datasets, limited data augmentation, and the smaller effect size of precancerous images compared to malignant lesions. The findings suggest that these techniques can significantly aid in the early detection of cervical cancer at the precancerous stage. Full article
(This article belongs to the Special Issue Machine Learning in Obstetrics and Gynecology Diagnosis)
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<p>(<b>a</b>) Colposcopy images from each of the normal, precancerous, and cancer groups. (<b>b</b>) Provisional diagnosis vs. cancer status: The provisional diagnosis during colposcopy, which relies on the clinician’s initial visual and clinical assessment, is important for categorizing cervical lesions as normal, precancerous, or cancerous. An analysis of the provided dataset highlights specific provisional diagnoses associated with each final cancer status. For cases ultimately confirmed as normal, the most frequent provisional diagnosis was “Type 1 Transition Zone (TZ); normal.” In precancerous cases, “Types 1, 2, and 3 TZ; HSIL” and “Type 1 TZ; LSIL” were commonly noted. For cancer cases, “Type 3 TZ; suspicion of invasive squamous cell carcinoma” was the predominant provisional diagnosis.</p>
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<p>Histopathology vs. cancer diagnosis: A histopathological analysis was used to determine the final diagnosis of cervical lesions identified during colposcopy. In normal cases, histopathology was often not performed, suggesting that the colposcopy assessment alone was sufficient. When histopathology was performed, findings such as CIN1 or the absence of dysplasia supported the normal diagnosis. Precancerous cases were characterized by moderate to severe dysplasia (CIN2, CIN3), low-grade squamous intraepithelial lesions (LSILs), and high-grade squamous intraepithelial lesions (HSILs), indicating varying degrees of abnormality with potential progression to cancer. Cancer cases were confirmed by histopathological evidence of invasive adenocarcinoma, squamous cell carcinoma, or adenocarcinoma in situ. These findings highlight the role of histopathology in accurately diagnosing and categorizing cervical lesions, guiding appropriate patient management and treatment strategies.</p>
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<p>An architectural flowchart illustrating the integrated process where the SWIN Transformer architecture and CNN are combined into a hybrid model for the binary classification of colposcopy images. This diagram highlights the seamless interaction between the two components, demonstrating how they work together to enhance the accuracy of image classification. The CNN and SWIN Transformer processes are parallel, and both outputs are integrated before classification. This flowchart includes specific steps within the SWIN Transformer architecture (swin_base_patch4_window7_224), such as patch partitioning, embedding, window-based self-attention, and merging, before integrating with the CNN outputs. After integration, the process flows through classification, post-processing, and final output generation. Detailed steps and the Python code are available at <a href="https://github.com/Foziyaam/SWIN-Transformer-and-CNN-for-Cervical-Cancer" target="_blank">https://github.com/Foziyaam/SWIN-Transformer-and-CNN-for-Cervical-Cancer</a>.</p>
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<p>Summary statistics—overall case diagnosis distribution: This summary statistics provides an overview of the distribution of colposcopy cases by diagnosis, Swede score distribution, and HPV status distribution, encapsulating the key aspects of the clinical findings. The distribution of overall case diagnoses indicates a predominance of non-cancer cases, with a significant portion of precancerous and some cancer cases.</p>
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<p>Distribution of cancer diagnoses by HPV status and transformation zone. These are 196 cases, since one of the cases does not have HPV test results.</p>
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<p>Correlation between Swede scores and cancer diagnosis. (<b>a</b>) Normal cases have the lowest-to-no Swede scores and precancerous moderate, while cancer cases have very high Swede scores. (<b>b</b>) Swede scores were significantly correlated with cancer diagnosis (r = 0.3 and <span class="html-italic">p</span> = 2e−05) and negatively correlated with normal diagnosis (r = 0.2 and <span class="html-italic">p</span> = 9e−04) while there was no significant correlation with the precancerous diagnosis.</p>
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<p>(<b>a</b>) Training loss across epochs; fivefold cross-validation metrics (red curve is the smoothing of the actual curve—the black line): (<b>b</b>) validation ROC curve for the validation set; (<b>c</b>) confusion matrix for the validation set. Validation sensitivity, 0.86; specificity, 0.90; positive predictive value (precision), 0.92; negative predictive value, 0.81; accuracy, 0.87; F1 score, 0.88; and AUC, 0.94.</p>
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<p>Performance of the trained model on the first test data (precancerous vs. normal): (<b>a</b>) ROC curve for test set 1 (precancerous versus normal); (<b>b</b>) confusion matrix for the performance of the model on test set 1 (precancerous vs. normal group). The values of the model’s performance metrics include sensitivity, 0.75; specificity, 0.75; positive predictive value, 0.76; negative predictive value, 0.74; accuracy, 0.75; F1 score, 0.75; and AUC, 0.80. The performance was tested using the same hyperparameters that were used for training: batch size = 32, epochs = 30, learning rate = 5e−05, weight decay = 5e−02, and gamma = 0.8.</p>
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<p>Performance of the second test set (images from cancer and normal cases): (<b>a</b>) ROC curve for test set 2 (cancer versus normal); (<b>b</b>) confusion matrix for the performance of the model on test set 2 (cancer vs. normal). Values of the important metrics include sensitivity, 0.72; specificity, 0.80; positive predictive value, 0.85; negative predictive value, 0.65; accuracy, 0.75; F1, 0.78; and AUC, 0.82. The same hyperparameters were used for this evaluation as well.</p>
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16 pages, 720 KiB  
Article
Effect of Time-Restricted Eating on Circulating Levels of IGF1 and Its Binding Proteins in Obesity: An Exploratory Analysis of a Randomized Controlled Trial
by Rand Talal Akasheh, Aparna Ankireddy, Kelsey Gabel, Mark Ezpeleta, Shuhao Lin, Chandra Mohan Tamatam, Sekhar P. Reddy, Bonnie Spring, Ting-Yuan David Cheng, Luigi Fontana, Seema Ahsan Khan, Krista A. Varady, Sofia Cienfuegos and Faiza Kalam
Nutrients 2024, 16(20), 3476; https://doi.org/10.3390/nu16203476 - 14 Oct 2024
Viewed by 470
Abstract
Obesity is associated with alterations in circulating IGF1, IGF1-binding proteins (IGFBPs), insulin, inflammatory markers, and hormones implicated in cardiovascular disease, diabetes, cancer, and aging. However, the effects of 4 and 6 h time-restricted eating (TRE) on circulating IGF1 and IGFBPs is uncertain. Objective: [...] Read more.
Obesity is associated with alterations in circulating IGF1, IGF1-binding proteins (IGFBPs), insulin, inflammatory markers, and hormones implicated in cardiovascular disease, diabetes, cancer, and aging. However, the effects of 4 and 6 h time-restricted eating (TRE) on circulating IGF1 and IGFBPs is uncertain. Objective: This study aimed to investigate the effects of TRE on plasma IGF1, IGFBP1, IGFBP2, and IGFBP3, and whether these effects were mediated by weight loss or body composition changes. Insulin sensitivity, glucose control, adipokines, and inflammatory markers were also examined. Design: An exploratory analysis of an 8-week randomized controlled trial implementing a daily TRE intervention was carried out. Participants/Setting: This study was conducted at the University of Illinois at Chicago in 2019. Participants with obesity were randomized to 4 or 6 h TRE (n = 35) or a control (n = 14) group. Plasma biomarkers were measured by ELISA at baseline and week 8. In a sub-analysis, participants were stratified into higher- (>3.5%) and lower- (≤3.5%) weight-loss groups. Intervention: Participants fasted daily from 7 p.m. to 3 p.m. in the 4 h TRE group (20 h) and from 7 p.m. to 1 p.m. in the 6 h TRE group (18 h), followed by ad libitum eating for the remainder of the day. Controls received no dietary recommendations. Main outcome measures: IGF1, IGFBPs, hsCRP, and adipokines were the main outcome measures of this analysis. Statistical Analysis: Repeated measures ANOVA and mediation analysis were conducted. Results: Body weight significantly decreased with TRE (−3.6 ± 0.3%), contrasting with controls (+0.2 ± 0.5%, p < 0.001). Significant effects of TRE over time were observed on plasma IGFBP2, insulin, HOMA-IR, and 8-isoprostane levels, without affecting other biomarkers. In the sub-analysis, IGFBP2 increased while leptin and 8-isoprostane decreased significantly only in the “higher weight loss” subgroup. Changes in insulin and HOMA-IR were related to TRE adherence. Conclusions: Eight-week daily 4 to 6 h TRE did not affect IGF1, IGFBP1, or IGFBP3 levels but improved insulin, HOMA-IR, and 8-isoprostane. IGFBP2 increased and leptin decreased when weight loss exceeded 3.5% of baseline. Full article
(This article belongs to the Special Issue Intermittent Fasting: A Heart-Healthy Dietary Strategy?)
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<p>Percentage of weight loss relative to baseline, stratified according to final weight loss percentage (lower vs. higher) over 8 weeks of time-restricted eating intervention. Data are expressed as mean ± SEM for percentage of weight loss (WL%) relative to baseline body weight. Participants were stratified into lower WL% (≤3.5%, n = 29) and higher WL% (&gt;3.5%, n = 20). * <span class="html-italic">p</span> &lt; 0.05 and *** <span class="html-italic">p</span> &lt; 0.001 for mean weight loss percentage in a specific week vs. group-matched baseline.</p>
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<p>Weight loss as a mediator of the effects of TRE on IGFBP2, 8-isoprostane, insulin, and HOMA-IR. Mediation models presenting (<b>A</b>) weight loss as a mediator of the increase in serum IGFBP2 and the decrease in serum 8-isoprostane levels induced by TRE; (<b>B</b>) weight loss as a mediator of the decrease in serum insulin and HOMA-IR induced by TRE, and the reversed model where the reduction in serum insulin or HOMA-IR mediate the effect of TRE on weight loss; and (<b>C</b>) fat mass loss as mediator of the decrease in serum leptin and the increase in high-molecular-weight adiponectin induced by TRE. The indirect effects of all these models were not significant, suggesting no mediation. IGFBP2: insulin-like growth factor 2; HOMA-IR: homeostatic model assessment of insulin resistance.</p>
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16 pages, 5848 KiB  
Article
Composition and Biogeochemical Effects of Carbohydrates in Aerosols in Coastal Environment
by Hung-Yu Chen and Ting-Wen Liu
J. Mar. Sci. Eng. 2024, 12(10), 1834; https://doi.org/10.3390/jmse12101834 - 14 Oct 2024
Viewed by 478
Abstract
We adopted a simple and rapid measurement method to analyze the concentrations of monosaccharides (MCHO) and polysaccharides (PCHO) in carbohydrates, a subset of organic carbon found in size-fractionated atmospheric particles. Seasonal and source-related factors influenced carbohydrate concentrations, with total water-soluble carbohydrates (TCHO) accounting [...] Read more.
We adopted a simple and rapid measurement method to analyze the concentrations of monosaccharides (MCHO) and polysaccharides (PCHO) in carbohydrates, a subset of organic carbon found in size-fractionated atmospheric particles. Seasonal and source-related factors influenced carbohydrate concentrations, with total water-soluble carbohydrates (TCHO) accounting for approximately 23% of the water-soluble organic carbon (WSOC) in spring when biological activity was high. We observed that the mode of aerosol transport significantly influenced the particle size distribution of carbohydrates, with MCHO exhibiting relatively high concentrations in fine particles (<1 μm) and PCHO showing higher concentrations in coarse particles (>1 μm). Moreover, our results revealed that MCHO and PCHO contributed 51% and 49%, respectively, to the TCHO concentration. This contribution varied by approximately ±19% depending on the season, suggesting the importance of both MCHO and PCHO. Additionally, through the combined use of principal component analysis (PCA) and positive matrix factorization (PMF), we determined that biomass burning accounts for 30% of the aerosol. Notably, biomass burning accounts for approximately 52% of the WSOC flux, with MCHO accounting for approximately 78% of the carbon from this source, indicating the substantial influence of biomass burning on aerosol composition. The average concentration of TCHO/WSOC in the atmosphere was approximately 18%, similar to the marine environment, reflecting the relationship between the biogeochemical cycles of the two environments. Finally, the fluxes of MCHO and PCHO were 1.10 and 5.28 mg C m−2 yr−1, respectively. We also found that the contribution of atmospheric deposition to marine primary productivity in winter was 15 times greater than that in summer, indicating that atmospheric deposition had a significant impact on marine ecosystems during nutrient-poor seasons. Additionally, we discovered that WSOC accounts for approximately 62% of the dissolved organic carbon (DOC) in the Min River, suggesting that atmospheric deposition could be a major source of organic carbon in the region. Full article
(This article belongs to the Section Chemical Oceanography)
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<p>Sampling location.</p>
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<p>Reaction formula for the phenol–sulfuric acid method [<a href="#B21-jmse-12-01834" class="html-bibr">21</a>].</p>
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<p>Air mass backward trajectories for the four seasons in Matsu.</p>
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<p>Relationship between carbohydrate concentration, temperature, and precipitation.</p>
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<p>The percentage of each substance in aerosol particles.</p>
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<p>Seasonal carbohydrate concentrations.</p>
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<p>Particle size distribution of carbohydrates.</p>
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<p>Proportion of TCHO in WSOC.</p>
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<p>Global distribution of carbohydrates. Note: <sup>a</sup> [<a href="#B8-jmse-12-01834" class="html-bibr">8</a>]; <sup>b</sup> [<a href="#B43-jmse-12-01834" class="html-bibr">43</a>]; <sup>c</sup> [<a href="#B1-jmse-12-01834" class="html-bibr">1</a>]; <sup>d</sup> [<a href="#B13-jmse-12-01834" class="html-bibr">13</a>]; <sup>e</sup> [<a href="#B45-jmse-12-01834" class="html-bibr">45</a>]; <sup>f</sup> [<a href="#B46-jmse-12-01834" class="html-bibr">46</a>]; <sup>g</sup> [<a href="#B44-jmse-12-01834" class="html-bibr">44</a>]; <sup>h</sup> [<a href="#B9-jmse-12-01834" class="html-bibr">9</a>]; <sup>i</sup> this study; <sup>j</sup> [<a href="#B11-jmse-12-01834" class="html-bibr">11</a>]; <sup>k</sup> [<a href="#B36-jmse-12-01834" class="html-bibr">36</a>].</p>
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<p>PMF for each species.</p>
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<p>Sources contributing to WSOC.</p>
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18 pages, 2241 KiB  
Article
Effects of Straw Input on the Yield and Water-Use Efficiency of Spring Maize in Film-Mulched Farmland
by Yisheng Lou, Xu Zhang, Shiyu Zhang, Na Li, Yidong Zhao, Wei Bai, Zhanxiang Sun and Zhe Zhang
Agriculture 2024, 14(10), 1803; https://doi.org/10.3390/agriculture14101803 - 13 Oct 2024
Viewed by 442
Abstract
To provide a theoretical basis for the sustainable application of autumn mulching technology, we examined the effects of straw input on spring maize yield and water-use efficiency in film-mulched farmland. Based on the positioning tests of different mulching methods conducted in 2013, non-mulching [...] Read more.
To provide a theoretical basis for the sustainable application of autumn mulching technology, we examined the effects of straw input on spring maize yield and water-use efficiency in film-mulched farmland. Based on the positioning tests of different mulching methods conducted in 2013, non-mulching (NM), spring mulching (SM), autumn mulching (AM), and autumn mulching combined with the return of straw (AMS) were selected in western Liaoning from 2018 to 2021. Spring maize yield, yield component factors, soil water content, and water-use efficiency under the four treatments were assessed. In each year, the AMS treatment significantly increased the maize yield, which was 48.22%, 9.33%, 30.66%, and 9.92%, and 11.78%, 7.71%, 12.86%, and 4.77% higher than that obtained after the SM and AM treatments, respectively. However, the harvest index was not significantly improved by AMS. AMS treatment significantly improved the precipitation utilization rate in all assessed years. Moreover, the crop water consumption was significantly increased by AMS treatment. Compared with the NM treatment, water-use efficiencies for economic and biological yield were also significantly improved. Thus, autumn mulching combined with straw-returning technology is an effective technical measure for improve spring maize yield and water-use efficiency in semi-arid areas of western Liaoning. Full article
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<p>Rainfall and average temperature during the maize-growing period.</p>
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<p>Effects of continuous film mulching combined with straw returning on spring maize yield in different years. A different letter within a column for treatments is significantly different at the <span class="html-italic">p</span> &lt; 0.05. NM, no mulching; SM, spring mulching; AM, autumn mulching; AMS, autumn straw mulching.</p>
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<p>Effects of straw returning and different mulching techniques on biological yield and harvest index of maize. A different letter within a column for treatments is significantly different at the <span class="html-italic">p</span> &lt; 0.05. NM, no mulching; SM, spring mulching; AM, autumn mulching; AMS, autumn straw mulching.</p>
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<p>Correlation analysis of spring maize yield components. In the legend, X1 represents cob length, X2 represents cob thickness, X3 represents grain row number per cob, X4 represents number of grains per row, and X5 represents 100-grain weight. ** means significant difference in treatment at <span class="html-italic">p</span> &lt; 0.01, same as below.</p>
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<p>Dynamic changes of soil moisture content in 0~100 cm stratified layers of spring maize during different growth periods under continuous film mulching combined with straw returning.</p>
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<p>Effects of continuous film mulching combined with straw returning on precipitation-use efficiency during the growth period. A different letter within a column for treatments is significantly different at the <span class="html-italic">p</span> &lt; 0.05. NM, no mulching; SM, spring mulching; AM, autumn mulching; AMS, autumn straw mulching.</p>
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<p>Relationship between yield and water-use efficiency.</p>
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