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23 pages, 4058 KiB  
Article
Improving Flood Streamflow Estimation of Ungauged Small Reservoir Basins Using Remote Sensing and Hydrological Modeling
by Fangrong Zhou, Nan Wu, Yuning Luo, Yuhao Wang, Yi Ma, Yifan Wang and Ke Zhang
Remote Sens. 2024, 16(23), 4399; https://doi.org/10.3390/rs16234399 - 24 Nov 2024
Viewed by 566
Abstract
Small- and medium-sized reservoirs significantly alter natural flood processes, making it essential to understand their impact on runoff for effective water resource management. However, the lack of measured data for most small reservoirs poses challenges for accurately simulating their behavior. This study proposes [...] Read more.
Small- and medium-sized reservoirs significantly alter natural flood processes, making it essential to understand their impact on runoff for effective water resource management. However, the lack of measured data for most small reservoirs poses challenges for accurately simulating their behavior. This study proposes a novel method that utilizes readily available satellite observation data, integrating hydraulic, hydrological, and mathematical formulas to derive outflow coefficients. Based on the Grid-XinAnJiang (GXAJ) model, the enhanced GXAJ-R model accounts for the storage and release effects of ungauged reservoirs and is applied to the Tunxi watershed. Results show that the original GXAJ model achieved a stable performance with an average NSE of 0.88 during calibration, while the NSE values of the GXAJ and GXAJ-R models during validation ranged from 0.78 to 0.97 and 0.85 to 0.99, respectively, with an average improvement of 0.03 in the GXAJ-R model. This enhanced model significantly improves peak flow simulation accuracy, reduces relative flood peak error by approximately 10%, and replicates the flood flow process with higher fidelity. Additionally, the area–volume model derived from classified small-scale data demonstrates high accuracy and reliability, with correlation coefficients above 0.8, making it applicable to other ungauged reservoirs. The OTSU-NDWI method, which improves the NDWI, effectively enhances the accuracy of water body extraction from remote sensing, achieving overall accuracy and kappa coefficient values exceeding 0.8 and 0.6, respectively. This study highlights the potential of integrating satellite data with hydrological models to enhance the understanding of reservoir behavior in data-scarce regions. It also suggests the possibility of broader applications in similarly ungauged basins, providing valuable tools for flood management and risk assessment. Full article
(This article belongs to the Special Issue Remote Sensing for Terrestrial Hydrologic Variables)
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<p>Geographical location and reservoir distribution map of Tunxi basin; the upper right corner shows the Xinanjiang Reservoir catchment area, located in the north of the Tunxi River Basin, as an example of water extraction.</p>
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<p>Flowchart of this study.</p>
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<p>Schematic diagram of flow over a practical weir without gate control, 1-1 and 2-2 are sections used to calculate the energy equation.</p>
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<p>GXAJ-R model framework diagram.</p>
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<p>Schematic of grid–reservoir classification, where (<b>a</b>–<b>c</b>) represent Case a to Case c respectively.</p>
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<p>Water body extraction results for the Dongfanghong Reservoir catchment area in 2017.</p>
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<p>Comparison of water body extraction accuracy for the Dongfanghong Reservoir area between NDWI and OTSU-NDWI methods from 2014 to 2017, (<b>a</b>) is the box plot of OA and KC, and (<b>b</b>) is the relationship between the reservoir water area extracted by remote sensing and the measured value.</p>
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<p>Simulated hourly streamflow at the Tunxi basin outlet for the GXAJ and GXAJ-R models.</p>
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<p>Model performance indicators. (<b>a</b>) NSE, (<b>b</b>) RTE, (<b>c</b>) RRE, (<b>d</b>) RPE.</p>
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13 pages, 6176 KiB  
Article
Study of Flooding Behavior and Discharge from Karot Dam in the Event of a Possible Breach by Using the Hydrodynamic Model
by Lilian Thomas Momburi, Changwen Li, Frank N. M. Masami, Minglei Ren and Isaac Otoo
Water 2024, 16(20), 2922; https://doi.org/10.3390/w16202922 - 14 Oct 2024
Viewed by 760
Abstract
This study utilizes the MIKE 11 hydrodynamic model developed by the Danish Hydraulic Institute to simulate flood behavior downstream of Karot Dam under multi-year in-flow conditions. The key parameters analyzed include breach characteristics, flood duration, water depth, flow velocity, discharge rate, and downstream [...] Read more.
This study utilizes the MIKE 11 hydrodynamic model developed by the Danish Hydraulic Institute to simulate flood behavior downstream of Karot Dam under multi-year in-flow conditions. The key parameters analyzed include breach characteristics, flood duration, water depth, flow velocity, discharge rate, and downstream distance. After dam failure, the peak discharge reaches 33,171 m3/s, exceeding the 10,000-year recurrence peak flow of 32,300 m3/s, with a breach duration of 2 h. The estimated peak discharge after simulation using empirical equations and comparative analyses showed maximum flood discharges of 28,187 m3/s, 28,922 m3/s, and 29,769 m3/s, with breach widths of 181 m, 256 m, and 331 m, respectively. The peak discharge predicted to reach the outlet with travel time ranging from 4 h 25 min to 4 h 40 min. Under multi-year average inflow conditions, Mangla Dam faces no risk of failure, with a maximum outflow of 12,097 m3/s and a spillway capacity of 30,147 m3/s. The model accurately predicted discharge values, with a strong correlation coefficient of R2 = 0.9653, indicating strong agreement between the actual water level data and predicted discharge. These insights are essential for developing effective emergency response strategies to mitigate the risks associated with dam failure. Full article
(This article belongs to the Special Issue Advances in Hydraulic and Water Resources Research (2nd Edition))
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<p>Location of the Jhelum River, showing Karot Dam and Mangla Dam.</p>
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<p>Centered 6-point Abbott scheme and channel section used in the Mike 11 hydrodynamic model for computational purposes.</p>
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<p>River network channel with location of cross-sections.</p>
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<p>Schematic diagram of the Karot Dam breach process, under the condition of multi-year average inflow.</p>
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<p>Peak discharge processes under different dam-break durations.</p>
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<p>Peak discharge processes under varying dam-break duration.</p>
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<p>Peak discharge along the downstream section after the dam break.</p>
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<p>Water level process of different typical sections at downstream of the dam.</p>
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<p>Downstream maximum flood water surface profile after the Karot Dam break.</p>
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<p>One-way maximum velocity at downstream of Karot Dam.</p>
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<p>Flow discharge process of a one-way typical downstream section following the dam break.</p>
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<p>Comparison of measured and calculated discharge for the model at downstream of the dam.</p>
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16 pages, 2819 KiB  
Article
Turkey’s Hydropower Potential in the Near Future and the Possible Impacts of Climate Change—A Case Study of the Euphrates–Tigris Basin
by Goksel Ezgi Guzey and Bihrat Onoz
Climate 2024, 12(10), 156; https://doi.org/10.3390/cli12100156 - 3 Oct 2024
Viewed by 861
Abstract
Hydropower is becoming an important renewable energy source in Turkey, but the ever-changing atmospheric and climatic conditions of Turkey make it very difficult to be projected efficiently. Thus, an efficient estimation technique is crucial for it to be adopted as a reliable energy [...] Read more.
Hydropower is becoming an important renewable energy source in Turkey, but the ever-changing atmospheric and climatic conditions of Turkey make it very difficult to be projected efficiently. Thus, an efficient estimation technique is crucial for it to be adopted as a reliable energy source in the future. This study evaluates Turkey’s hydropower potential in the Euphrates–Tigris Basin under changing climatic conditions. We adapted an empirical equation to model reservoir outflows, considering the site-specific characteristics of 14 major dams. Initial results from employing a model with a constant empirical coefficient, α, yielded moderate predictive accuracy, with R2 values ranging from 0.289 to 0.612. A polynomial regression identified optimal α values tailored to each dam’s surface area, significantly improving model performance. The adjusted α reduced predictive bias and increased R2 values, enhancing forecast reliability. Seasonal analysis revealed distinct hydropower trends: Ataturk Dam showed a notable decrease of 5.5% in hydropower generation up to 2050, while Birecik and Keban Dams exhibited increases of 2.5% and 2.2%, respectively. By putting these discoveries into practice, water resource management may become more robust and sustainable, which is essential for meeting Turkey’s rising energy needs and preparing for future climatic challenges. This study contributes valuable insights for optimizing reservoir operations, ensuring long-term hydropower sustainability, and enhancing the resilience of water resource management systems globally. Full article
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<p>From top to bottom: major dams in the ETRB with the location of the 14 dams studied. The ETR basin studies with the corresponding streamflow stations present.</p>
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<p>Example of data obtained for the Ataturk dam (from 2015) showing flow and hydropower generated.</p>
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<p>The distribution of alpha (α) values generated by varying the standard deviation (σ) of the random variable ε. Different σ values were used to assess the sensitivity of α to variations in ε. While only these three ranges are shown for clarity, a broader range from 0.01 to 1 with a 0.02 interval was generated. The normal (Gaussian) distribution was used for ε, providing a realistic simulation of uncertainties.</p>
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<p>Normalized 1:1 scatter plots for the predictive performance of the initial equation for all dams (α = 0.5). The scatter plots display the relationship between the normalized observed and normalized predicted values for the reservoir outflow across multiple dams. Each plot corresponds to a different dam, with the dam name and the coefficient of determination (R<sup>2</sup>) value indicated. The diagonal red line represents the perfect 1:1 relationship between observed and predicted values. Normalization is done to ensure consistency in comparing the magnitude of values across different dams and to reveal systematic biases.</p>
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<p>Performance metrics (PBIAS, NSE, and R<sup>2</sup>) for different dams located along a river system or basin.</p>
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<p>This graph illustrates the process of determining the optimal value of the parameter alpha (α) for the Keban Dam, based on minimizing different error metrics. The vertical axis represents the error values, while the horizontal axis shows the range of alpha values considered. The blue line corresponds to the PBIAS (Percent Bias) error, the red line represents the NSE (Nash–Sutcliffe Efficiency) error, and the green line depicts the R<sup>2</sup> error. The vertical dashed line highlights the chosen optimal alpha value of 0.851, which appears to minimize the overall errors across the different metrics for the Keban Dam.</p>
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<p>Streamflow releases estimated from the HBV model with the adjusted parameters. The HBV model corresponds to RCP 8.5 projections, with NSE = 0.752.</p>
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<p>Seasonal trends observed for the releases at each dam.</p>
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<p>Hydropower generation time series for the dams.</p>
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<p>Yearly rate of change for hydropower generation.</p>
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27 pages, 13088 KiB  
Article
Effects of Surface Layer Physics Schemes on the Simulated Intensity and Structure of Typhoon Rai (2021)
by Thi-Huyen Hoang, Ching-Yuang Huang and Thi-Chinh Nguyen
Atmosphere 2024, 15(9), 1140; https://doi.org/10.3390/atmos15091140 - 20 Sep 2024
Viewed by 713
Abstract
The influences of surface layer (SL) physics schemes on the simulated intensity and structure of Typhoon Rai (2021) are investigated using the WRF model. Numerical experiments using different SL physics schemes—revised MM5 scheme (MM5), Eta similarity scheme (CTL), and Mellor–Yamada–Nakanishi–Niino scheme (MYNN)—are conducted. [...] Read more.
The influences of surface layer (SL) physics schemes on the simulated intensity and structure of Typhoon Rai (2021) are investigated using the WRF model. Numerical experiments using different SL physics schemes—revised MM5 scheme (MM5), Eta similarity scheme (CTL), and Mellor–Yamada–Nakanishi–Niino scheme (MYNN)—are conducted. The results show that the intensity forecast of Typhoon Rai is largely influenced by SL physics schemes, while its track forecast is not significantly affected. All three experiments can successfully capture the movement of Rai, while CTL provides better intensity simulation compared to the other two experiments. The higher ratio of enthalpy exchange coefficient to drag coefficient (CK/CD) in CTL than MM5 and MYNN leads to significantly increased surface enthalpy fluxes, which are crucial for the typhoon intensification of the former. To explore the influence of SL physics on the structural evolution of the typhoon, the azimuthal-mean angular momentum (AM) budget is utilized. The results indicate that asymmetric eddy terms may also largely contribute to the AM tendencies, which are relatively more comparable in the weaker TC for MM5, compared to the stronger TC with the dominant symmetric mean terms for CTL. Furthermore, the extended Sawyer–Eliassen (SE) equation is solved to quantify the transverse circulations of the typhoon induced by different forcing sources for CTL and MM5. The SE solution indicates that the transverse circulation above and within the boundary layer is predominantly induced by diabatic heating and turbulent friction, respectively, for both CTL and MM5, while all other physical forcing terms are relatively insignificant for the induced transverse circulation for CTL, except for the large contribution from the eddy forcing in the upper-tropospheric outflow for MM5. With the stronger connective heating in the eyewall and boundary-layer radial inflow, the linear SE analysis agrees much better with the nonlinear simulation for CTL than MM5. Full article
(This article belongs to the Section Meteorology)
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<p>The WRF model domains for Rai at the initial time. The outermost box (d01) denotes the outermost domain, while the red and blue boxes (d02 and d03, respectively) denote the two inner moving domains. The dashed black line (JMA) with cycles at intervals of 24 h indicates the best track from JMA from 0000 UTC 14 December to 0000 UTC 18 December 2021.</p>
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<p>(<b>a</b>) Tracks of Typhoon Rai, including the best track data from JTWC (dashed black line) and JMA (solid black line), as well as simulated tracks for CTL (red line), MM5 (blue line), and MYNN (green line), during the period from 0000 UTC 14 December to 0000 UTC 18 December 2021. Circle symbols in (<b>a</b>) indicate the time every 24 h. (<b>b</b>) as in (<b>a</b>), but for the 10-m maximum wind speed (V<sub>max</sub>, m s<sup>−1</sup>).</p>
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<p>12-h accumulated precipitation (mm) during 48–60 h from (<b>a</b>) multi-satellite precipitation product GSMaP, (<b>b</b>) CTL, (<b>c</b>) MM5, and (<b>d</b>) MYNN. (<b>e</b>), (<b>f</b>), (<b>g</b>), and (<b>h</b>) as in (<b>a</b>), (<b>b</b>), (<b>c</b>), and (<b>d</b>), respectively, but during 60–72 h. (<b>i</b>), (<b>j</b>), (<b>k</b>), and (<b>l</b>) as in (<b>a</b>), (<b>b</b>), (<b>c</b>), and (<b>d</b>), respectively, but during 72–84 h.</p>
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<p>Simulated ratio of enthalpy exchange coefficient to drag coefficient (C<sub>K</sub>/C<sub>D</sub>) as a function of 10-m wind speed for CTL (red line), MM5 (blue line), and MYNN (green line) at 54 h.</p>
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<p>Time evolutions of (<b>a</b>) friction velocity (m s<sup>−1</sup>), (<b>b</b>) surface sensible heat flux (W m<sup>−2</sup>), and (<b>c</b>) surface latent heat flux (W m<sup>−2</sup>) for CTL (red line), MM5 (blue line), and MYNN (green line), averaged within the area of 300 × 300 km around the typhoon center from 24 h to 72 h.</p>
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<p>Horizontal distribution of 10-m wind speed (shaded color, m s<sup>−1</sup>) for (<b>a</b>) CTL, (<b>b</b>) MM5, and (<b>c</b>) MYNN at 54 h. (<b>d</b>), (<b>e</b>), and (<b>f</b>) as in (<b>a</b>), (<b>b</b>), and (<b>c</b>), respectively, but for friction velocity (m s<sup>−1</sup>). (<b>g</b>), (<b>h</b>), and (<b>i</b>) as in (<b>a</b>), (<b>b</b>), and (<b>c</b>), respectively, but for surface sensible heat flux (W m<sup>−2</sup>). (<b>j</b>), (<b>k</b>), and (<b>l</b>) as in (<b>a</b>), (<b>b</b>), and (<b>c</b>), respectively, but for surface latent heat flux (W m<sup>−2</sup>). The black vectors in (<b>a</b>–<b>c</b>) denote the 10-m horizontal wind speed.</p>
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<p>Azimuthal-mean tangential velocity (m s<sup>−1</sup>) in the radius–height cross-section at 54 h for (<b>a</b>) CTL and (<b>b</b>) MM5. (<b>c</b>) and (<b>d</b>) as in (<b>a</b>) and (<b>b</b>), respectively, but for the radial velocity (m s<sup>−1</sup>). The black line in (<b>a</b>,<b>b</b>) represents the height of the maximum tangential wind speed (h<sub>vt</sub>). The black line in (<b>c</b>,<b>d</b>) represents the inflow layer depth (h<sub>vr</sub>).</p>
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<p>Time–radius Hovmöller diagrams of azimuthal-mean tangential wind (m s<sup>−1</sup>) at 2-km height for (<b>a</b>) CTL and (<b>b</b>) MM5 from 24 h to 72 h. (<b>c</b>) and (<b>d</b>) as in (<b>a</b>) and (<b>b</b>), respectively, but for radial wind (m s<sup>−1</sup>) at 0.25-km height. The black line in (<b>a</b>,<b>b</b>) represents the radius of maximum tangential wind speed (RMW) at 2 km height. The green line in (<b>c</b>,<b>d</b>) represents the maximum inflow at 0.25-km height.</p>
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<p>Azimuthal-mean potential temperature (K) in the radius–height cross-section for (<b>a</b>) CTL and (<b>b</b>) MM5 at 54 h. The thick black line represents the RMW.</p>
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<p>Time–height Hovmöller diagrams of azimuthal-mean potential temperature (K) inside RMW for (<b>a</b>) CTL and (<b>b</b>) MM5. (<b>c</b>) and (<b>d</b>) as in (<b>a</b>) and (<b>b</b>), respectively, but for warm core (K) averaged inside a radius of 1.5 degrees from the typhoon center.</p>
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<p>Azimuthal-mean flow (shaded color) in the radius–height cross-section of radial velocity (m s<sup>−1</sup>) for (<b>a</b>) CTL and (<b>b</b>) MM5 at 54 h. (<b>c</b>) and (<b>d</b>) as in (<b>a</b>) and (<b>b</b>), respectively, but for tangential velocity (m s<sup>−1</sup>). (<b>e</b>) and (<b>f</b>) as in (<b>a</b>) and (<b>b</b>), respectively, but for vertical velocity (m s<sup>−1</sup>). (<b>g</b>) and (<b>h</b>) as in (<b>a</b>) and (<b>b</b>), respectively, but for latent heating rate (K h<sup>−1</sup>). The green line represents the RMW. The reference vector in the lower right corner represents the radial and vertical wind components.</p>
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<p>Radius–height cross-sections of azimuthal-mean angular momentum (AAM) (shaded color, 10<sup>6</sup> m<sup>2</sup> s<sup>−1</sup>) for (<b>a</b>) CTL and (<b>b</b>) MM5 at 54 h. The green line represents the RMW. The reference vector in the lower right corner represents the radial and vertical wind components.</p>
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<p>Radius–height cross-section of azimuthal-mean AM budget terms (shaded color, m<sup>2</sup> s<sup>−2</sup>), including (<b>a</b>) radial advection of mean AM, (<b>b</b>) radial advection of eddy AM, (<b>c</b>) vertical advection of mean AM, (<b>d</b>) vertical advection of eddy AM, (<b>e</b>) mean Coriolis force term, and (<b>f</b>) sum of all AM budget terms for CTL at 54 h. The green line represents the RMW. The reference vector in the lower right corner represents the radial and vertical wind components.</p>
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<p>As in <a href="#atmosphere-15-01140-f013" class="html-fig">Figure 13</a>, but for MM5 including (<b>a</b>) radial advection of mean AM, (<b>b</b>) radial advection of eddy AM, (<b>c</b>) vertical advection of mean AM, (<b>d</b>) vertical advection of eddy AM, (<b>e</b>) mean Coriolis force term, and (<b>f</b>) sum of all AM budget terms for CTL at 54 h. The green line represents the RMW. The reference vector in the lower right corner represents the radial and vertical wind components.</p>
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<p>Azimuthal-mean radial velocity (shaded colors, m s<sup>−1</sup>) at 54 h from the Sawyer–Eliassen (SE) solution with total forcing sources for (<b>a</b>) CTL and (<b>b</b>) MM5. (<b>c</b>) and (<b>d</b>) as in (<b>a</b>) and (<b>b</b>), respectively, but with symmetric diabatic heating only. (<b>e</b>) and (<b>f</b>) as in (<b>a</b>) and (<b>b</b>), respectively, but with asymmetric eddy momentum and heating only. (<b>g</b>) and (<b>h</b>) as in (<b>a</b>) and (<b>b</b>), respectively, but with turbulent momentum diffusion only. (<b>i</b>) and (<b>j</b>) as in (<b>a</b>) and (<b>b</b>), respectively, but with residual terms only. The wind vectors (m s<sup>−1</sup>) induced by the total forcing sources overlapped in each panel indicate the radial and vertical wind components (m s<sup>−1</sup>) with their reference vectors given at the lower right corner.</p>
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<p>Azimuthal-mean vertical velocity (shaded colors, m s<sup>−1</sup>) at 54 h from the Sawyer–Eliassen (SE) solution with total forcing sources for (<b>a</b>) CTL and (<b>b</b>) MM5. (<b>c</b>) and (<b>d</b>) as in (<b>a</b>) and (<b>b</b>), respectively, but with symmetric diabatic heating only. (<b>e</b>) and (<b>f</b>) as in (<b>a</b>) and (<b>b</b>), respectively, but with asymmetric eddy momentum and heating only. (<b>g</b>) and (<b>h</b>) as in (<b>a</b>) and (<b>b</b>), respectively, but with residual terms only. The wind vectors (m s<sup>−1</sup>) induced by the total forcing sources overlapped in each panel indicate the radial and vertical wind components (m s<sup>−1</sup>) with their reference vectors given at the lower right corner.</p>
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11 pages, 1810 KiB  
Article
Experimental Investigation of a Water–Air Heat Recovery System
by Robert Ștefan Vizitiu, Ștefănica Eliza Vizitiu, Andrei Burlacu, Chérifa Abid, Marius Costel Balan and Nicoleta Elena Kaba
Sustainability 2024, 16(17), 7686; https://doi.org/10.3390/su16177686 - 4 Sep 2024
Viewed by 637
Abstract
The implementation of energy-saving measures has a substantial and beneficial impact on the preservation of energy resources as well as the reduction of carbon dioxide emissions. This study focuses on the design and experimental analysis of a water-to-air heat recovery system aimed at [...] Read more.
The implementation of energy-saving measures has a substantial and beneficial impact on the preservation of energy resources as well as the reduction of carbon dioxide emissions. This study focuses on the design and experimental analysis of a water-to-air heat recovery system aimed at capturing waste heat from wastewater and transferring it to a fresh cold air stream using heat pipe technology. The research problem addressed in this study is the efficient recovery of low-grade thermal energy from wastewater, which is often underutilized. The prototype heat recovery unit was designed, manufactured, and tested in the laboratory to assess its performance across various operating conditions. The experimental setup included a system where the primary agent, hot water, was heated to 60 °C and circulated through the evaporator section of the heat recovery unit, while the secondary agent, fresh air, was forced through the condenser section. The system’s performance was evaluated under different air velocities, ranging from 3.5 m/s to 4.5 m/s, corresponding to airflow rates of 207.1 m3/h and 268.6 m3/h, respectively. The study employed analytical methods alongside empirical testing to determine the effectiveness of the heat recovery system, with the global heat transfer coefficient calculated for different scenarios. The efficiency of the system varied between 25% and 51.6%, depending on the temperature and speed of the fresh air stream. The most significant temperature difference observed between the inflow and outflow of the fresh air stream was 16.8 °C, resulting in a thermal output of 1553 W. Additionally, the average (mean) overall heat transfer coefficient of the unit was calculated to be 49 W/m2 K, which aligns with values reported in the literature for similar systems. The results demonstrate the potential of the designed system for practical applications in energy conservation and carbon emission reduction. Full article
(This article belongs to the Section Energy Sustainability)
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<p>The 3D design of the HPHE.</p>
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<p>The laboratory experimental stand: 1—Evaporator, 2—Condenser, 3—Electric heater, 4—Fan speed control switch, 5—LT BTM-420SD electronic thermometer, 6—Fan.</p>
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<p>Temperature difference of air between outlet and inlet.</p>
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<p>The efficiency of the heat recovery system.</p>
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<p>Temperature variation of the air in the most efficient scenario.</p>
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15 pages, 1223 KiB  
Article
Revolutionizing Bladder Health: Artificial-Intelligence-Powered Automatic Measurement of Bladder Volume Using Two-Dimensional Ultrasound
by Evan Avraham Alpert, Daniel David Gold, Deganit Kobliner-Friedman, Michael Wagner and Ziv Dadon
Diagnostics 2024, 14(16), 1829; https://doi.org/10.3390/diagnostics14161829 - 22 Aug 2024
Viewed by 863
Abstract
Introduction: Measuring elevated post-void residual volume is important for diagnosing urinary outflow tract obstruction and cauda equina syndrome. Catheter placement is exact but painful, invasive, and may cause infection, whereas an ultrasound is accurate, painless, and safe. Aim: The purpose of this single-center [...] Read more.
Introduction: Measuring elevated post-void residual volume is important for diagnosing urinary outflow tract obstruction and cauda equina syndrome. Catheter placement is exact but painful, invasive, and may cause infection, whereas an ultrasound is accurate, painless, and safe. Aim: The purpose of this single-center study is to evaluate the accuracy of a module for artificial-intelligence (AI)-based fully automated bladder volume (BV) prospective measurement using two-dimensional ultrasound images, as compared with manual measurement by expert sonographers. Methods: Pairs of transverse and longitudinal bladder images were obtained from patients evaluated in an urgent care clinic. The scans were prospectively analyzed by the automated module using the prolate ellipsoid method. The same examinations were manually measured by a blinded expert sonographer. The two methods were compared using the Pearson correlation, kappa coefficients, and the Bland–Altman method. Results: A total of 111 pairs of transverse and longitudinal views were included. A very strong correlation was found between the manual BV measurements and the AI-based module with r = 0.97 [95% CI: 0.96–0.98]. The specificity and sensitivity for the diagnosis of an elevated post-void residual volume using a threshold ≥200 mL were 1.00 and 0.82, respectively. An almost-perfect agreement between manual and automated methods was obtained (kappa = 0.85). Perfect reproducibility was found for both inter- and intra-observer agreements. Conclusion: This AI-based module provides an accurate automated measurement of the BV based on ultrasound images. This novel method demonstrates a very strong correlation with the gold standard, making it a potentially valuable decision-support tool for non-experts in acute settings. Full article
(This article belongs to the Special Issue The Role of AI in Ultrasound)
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<p>The automated bladder volume and dimension measurements of transverse (<b>left</b> panel) and longitudinal (<b>right</b> panel) clips, as calculated using the AI-based tool LVivo Bladder, with the prolate ellipsoid method using the three dimensions of the bladder. The red lines represent the individual diameters. The mint-colored shape the automated trace of the outline of the bladder wall.</p>
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<p><b>A</b> comparison of the bladder volume measurements using the AI-based tool vs. the gold standard: (<b>A</b>) The Pearson correlation and (<b>B</b>) agreement assessment using the Bland–Altman plot. (<b>A</b>) The correlation scatter plot with a regression line and a Pearson correlation coefficient of 0.972 (<span class="html-italic">p</span> &lt; 0.001). (<b>B</b>) The bladder volume assessment agreement revealed a mean bias of 17.10 (the red line), with the limits of agreement ranging from 86.87 to −52.67 (the yellow lines).</p>
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<p>A comparison of the D1 diameter measurements using the AI-based tool vs. the gold standard: (<b>A</b>) The Pearson correlation and (<b>B</b>) agreement assessment using the Bland–Altman plot. (<b>A</b>) A correlation scatter plot with a regression line and a Pearson correlation coefficient of 0.992 (<span class="html-italic">p</span> &lt; 0.001). (<b>B</b>) The D1 assessment agreement revealed a mean bias of 2.39 (the red line), with the limits of agreement ranging from 7.95 to −3.17 (the yellow lines).</p>
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<p>A comparison of the D2 diameter measurements using the AI-based tool vs. the gold standard: (<b>A</b>) The Pearson correlation and (<b>B</b>) agreement assessment using the Bland–Altman plot. (<b>A</b>) A correlation scatter plot with a regression line and a Pearson correlation coefficient of 0.945 (<span class="html-italic">p</span> &lt; 0.001). (<b>B</b>) The D2 assessment agreement revealed a mean bias of 1.87 (the red line), with the limits of agreement ranging from 11.55 to −7.81 (the yellow lines).</p>
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<p><b>A</b> comparison of the D3 diameter measurements using the AI-based tool vs. the gold standard: (<b>A</b>) The Pearson correlation and (<b>B</b>) agreement assessment using the Bland–Altman plot. (<b>A</b>) A correlation scatter plot with a regression line and a Pearson correlation coefficient of 0.896 (<span class="html-italic">p</span> &lt; 0.001). (<b>B</b>) The D3 assessment agreement revealed a mean bias of 1.61 (the red line), with the limits of agreement ranging from 15.83 to −12.62 (the yellow lines).</p>
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19 pages, 5168 KiB  
Article
A Consolidated Linearised Progressive Flooding Simulation Method for Onboard Decision Support
by Luca Braidotti, Jasna Prpić-Oršić, Serena Bertagna and Vittorio Bucci
J. Mar. Sci. Eng. 2024, 12(8), 1367; https://doi.org/10.3390/jmse12081367 - 11 Aug 2024
Viewed by 614
Abstract
In pursuing quick and precise progressive flooding simulations for decision-making support, the linearised method has emerged and undergone refinement in recent years, becoming a reliable tool, especially for onboard decision support. This study consolidates and enhances the modelling approach based on a system [...] Read more.
In pursuing quick and precise progressive flooding simulations for decision-making support, the linearised method has emerged and undergone refinement in recent years, becoming a reliable tool, especially for onboard decision support. This study consolidates and enhances the modelling approach based on a system of differential-algebraic equations capable of accommodating compartments filled with floodwater. The system can be linearised to permit analytical solutions, facilitating the utilization of larger time increments compared to conventional solvers for differential equations. Performance enhancements are achieved through the implementation of an adaptive time-step mechanism during the integration process. Furthermore, here, a correction coefficient for opening areas is introduced to enable the accurate modelling of free outflow scenarios, thereby mitigating issues associated with the assumption of deeply submerged openings used in governing equations. Experimental validation is conducted to compare the method’s efficacy against recent model-scale tests, specifically emphasising the improvements stemming from the correction for free outflow. Full article
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<p>Ship-fixed and auxiliary Earth-fixed reference systems [<a href="#B31-jmse-12-01367" class="html-bibr">31</a>].</p>
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<p>Flowchart of the main loop of the simulation process.</p>
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<p>Illustration of a simple three-room geometry [<a href="#B31-jmse-12-01367" class="html-bibr">31</a>].</p>
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<p>Sketch of different submersion statuses of a large opening: (<b>a</b>) deeply submerged; (<b>b</b>) free outflow with deeply submerged part; (<b>c</b>) deeply submerged one side only; (<b>d</b>) free outflow.</p>
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<p>Experimental setup utilized [<a href="#B35-jmse-12-01367" class="html-bibr">35</a>]. All measurements are in mm. Floodwater levels in C1 and C2 were measured using level sensors 27 and 23, respectively.</p>
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<p>Mesh of the box-model used to simulate progressive flooding.</p>
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<p>Simulated and experimental water levels in compartment C1.</p>
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<p>Simulated and experimental water levels in compartment C2.</p>
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<p>Experimental setup utilized [<a href="#B38-jmse-12-01367" class="html-bibr">38</a>]. All measurements are in mm. Floodwater levels in C1 and C2 were measured using level sensors 27 and 23, respectively.</p>
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<p>Mesh of the shop model rooms used for simulating progressive flooding.</p>
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<p>Comparison of the experimental and simulated heel, trim, and levels recorded by sensors for the ship model.</p>
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16 pages, 4297 KiB  
Article
Development of an Explicit Water Level Pool Routing Method in Reservoirs
by Alfonso Arrieta-Pastrana, Oscar E. Coronado-Hernández and Vicente S. Fuertes-Miquel
Water 2024, 16(14), 2042; https://doi.org/10.3390/w16142042 - 19 Jul 2024
Viewed by 909
Abstract
Local regulations control the additional runoff produced by urbanization processes. Sustainable urban drainage systems can mitigate the issues associated with increased runoff by employing infiltration basins, detention ponds, wet ponds, and constructed wetlands. Traditionally, the Water Level Pool Routing Method, which relies on [...] Read more.
Local regulations control the additional runoff produced by urbanization processes. Sustainable urban drainage systems can mitigate the issues associated with increased runoff by employing infiltration basins, detention ponds, wet ponds, and constructed wetlands. Traditionally, the Water Level Pool Routing Method, which relies on an implicit calculation scheme, has been used to calculate outflow hydrographs in reservoirs. In this research, an explicit scheme for the Water Level Pool Routing Method has been developed. The proposed model is applied to a case study where the reservoir has a surface area of 9.12 hectares. The influence of weir width and the discharge coefficient is also analyzed. Additionally, the variation in time step does not significantly affect the response of the proposed model, demonstrating its adequacy as a novel method. The proposed model is compared to the traditional method, yielding similar results in an analyzed ornamental reservoir (low percentage reduction in peak flow). However, a case study with experimental data reveals that the proposed model provides better accuracy than the traditional method. In addition, the proposed model is more efficient as it reduces computational time compared to the implicit scheme (conventional method). Finally, the proposed model is simplified for small watersheds by applying the rational method for computing an inflow hydrograph. Full article
(This article belongs to the Section Hydrology)
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<p>Components of a system: (<b>a</b>) relationship between <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>Q</mi> </mrow> <mrow> <mi>I</mi> <mo>,</mo> <mi>t</mi> </mrow> </msub> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>Q</mi> </mrow> <mrow> <mi>O</mi> <mo>,</mo> <mi>t</mi> </mrow> </msub> </mrow> </semantics></math> at time <math display="inline"><semantics> <mrow> <mi>t</mi> </mrow> </semantics></math>; (<b>b</b>) relationship between <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>Q</mi> </mrow> <mrow> <mi>I</mi> <mo>,</mo> <mi>t</mi> <mo>+</mo> <mo>∆</mo> <mi>t</mi> </mrow> </msub> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>Q</mi> </mrow> <mrow> <mi>O</mi> <mo>,</mo> <mi>t</mi> <mo>+</mo> <mo>∆</mo> <mi>t</mi> </mrow> </msub> </mrow> </semantics></math> at time <math display="inline"><semantics> <mrow> <mi>t</mi> <mo>+</mo> <mo>∆</mo> <mi>t</mi> </mrow> </semantics></math>; (<b>c</b>) water flow hydrograph; and (<b>d</b>) rectangular weir.</p>
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<p>Characteristics of a triangular hydrograph.</p>
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<p>Methodology.</p>
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<p>Location of the case study: (<b>a</b>) general location of the city of Cartagena, Colombia; (<b>b</b>) location of the neighborhood Barcelona de Indias; and (<b>c</b>) aerial photographs for delineation of the watershed.</p>
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<p>Inflow hydrograph.</p>
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<p>Outflow hydrograph and water level inside the reservoir.</p>
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<p>Sensitivity analysis for the water level pool routing: (<b>a</b>) weir width; and (<b>b</b>) discharge coefficient.</p>
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<p>Analysis of time step using the proposed model.</p>
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<p>Assessing the storage–outflow relation: (<b>a</b>) water-surface-elevation–storage relation; (<b>b</b>) weir discharge rating curve; and (<b>c</b>) storage–outflow function.</p>
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<p>Comparison of the outflow hydrograph considering the explicit (proposed model) and implicit methods for water level pool routing.</p>
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<p>Dispersion graph of the outflow hydrograph (EWLPM—proposed model—versus IWLPM).</p>
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<p>Representation of the triangular unit inflow hydrograph and outflow hydrographs as a function of the parameter <math display="inline"><semantics> <mrow> <mi>K</mi> </mrow> </semantics></math>.</p>
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<p>Comparison of outflow hydrographs: experimental measurements versus calculated results from EWLPM (explicit method) and IWLPM (implicit or traditional method).</p>
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15 pages, 2307 KiB  
Article
Explicit Scheme for a Hydrological Channel Routing: Mathematical Model and Practical Application
by Alfonso Arrieta-Pastrana, Oscar E. Coronado-Hernández and Jairo R. Coronado-Hernández
Water 2024, 16(11), 1480; https://doi.org/10.3390/w16111480 - 23 May 2024
Cited by 1 | Viewed by 978
Abstract
The computation of hydrographs in large watersheds necessitates utilizing channel routing, which calculates the movement of hydrographs along channel branches. Routing methods rely on an implicit scheme to facilitate numerical resolution, which requires more computational time than the explicit scheme. This study presents [...] Read more.
The computation of hydrographs in large watersheds necessitates utilizing channel routing, which calculates the movement of hydrographs along channel branches. Routing methods rely on an implicit scheme to facilitate numerical resolution, which requires more computational time than the explicit scheme. This study presents an explicit scheme channel routing model that offers a versatile approach to open channel flow analysis. The model is based on mass conservation principles and Manning equations, and it can accommodate varying bed slopes, making it highly adaptable to diverse hydraulic scenarios. In addition, the proposed model considers backwater effects, which enhances its applicability in practical scenarios. The model was tested in a practical application on a rectangular channel with a width of 7 m, and the results showed that it can accurately predict outflow hydrographs and handle different flow conditions. Comparative analyses with existing models revealed that the proposed model’s performance in generating water flow oscillations was competitive. Moreover, sensitivity analyses were performed, which showed that the model is highly responsive to parameter variations, such as Manning’s coefficient, bed slope, and channel width. The comparison of peak flows and peak times between the proposed model and existing methods further emphasized the model’s reliability and efficiency in simulating channel routing processes. This research introduces a valuable addition to the field of hydrology by proposing a practical and effective channel routing model that integrates essential hydraulic principles and parameters. The results of the proposed model (lumped routing) are comparable with the solution provided by the Muskingum–Cunge method (distributed routing). It is of utmost importance to note that the proposed model applies to channel branches with bed slopes below 6°. Full article
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<p>Flow hydrograph representation.</p>
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<p>Free surface scheme.</p>
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<p>Diagram of a trapezoidal cross section.</p>
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<p>Inflow hydrograph.</p>
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<p>Results of the open channel routing.</p>
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<p>Sensitivity analysis for the channel routing: (<b>a</b>) Manning’s coefficient; (<b>b</b>) bed slope; (<b>c</b>) width of the channel.</p>
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<p>Variation of time step in the proposed model.</p>
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<p>Comparison between the proposed model and the other channel routing methods.</p>
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<p>Comparison between the proposed model versus Muskingum–Cunge method considering different bed slopes.</p>
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16 pages, 8403 KiB  
Article
The Impact of Beaver Dams on the Dynamic of Groundwater Levels at Łąki Soleckie
by Sławomir Bajkowski, Ryszard Oleszczuk, Janusz Urbański, Jan Jadczyszyn and Marta Kiraga
Sustainability 2024, 16(10), 4135; https://doi.org/10.3390/su16104135 - 15 May 2024
Viewed by 837
Abstract
Areas excluded from agricultural production are susceptible to the presence of beaver families. The most significant changes occur during the initial period, when agricultural utilization is abandoned and beavers establish their presence on the land. During this period, some parcels remain uncultivated, while [...] Read more.
Areas excluded from agricultural production are susceptible to the presence of beaver families. The most significant changes occur during the initial period, when agricultural utilization is abandoned and beavers establish their presence on the land. During this period, some parcels remain uncultivated, while agricultural activities persist in neighboring areas. This situation is accompanied by the destruction of beaver dams, especially during periods of abundant water resources, and notably during intensive fieldwork. The article presents field studies aimed at determining the extent to which constructed and operational beaver dams contribute to changes in groundwater levels in drained peatland areas. In order to protect and sustainably use peat soils, it is necessary to maintain their high moisture content by ensuring a high groundwater level elevation. This can be achieved through the use of existing damming structures in the area (levees, weirs). Beaver dams can also serve a similar function, blocking the outflow of water from peat lands by raising the water level and consequently retaining it naturally. The specific objective was to develop principles for verifying factors influencing the effects of beaver dam construction on groundwater levels in fields within their range of influence. The water table levels within the study area during rainless periods were influenced by water levels in ditches, dependent on beaver activity in the nearby river. Beaver activities, manifested through dam construction, were influenced by periodic water resources in the river, defined by the cumulative monthly precipitation. Factors affecting groundwater levels in rainless periods on the plots also included the distance from the river cross-section and the permeability of soils expressed by the filtration coefficient of the active layer. Beaver dams had the greatest impact on stabilizing the water table in the soil profile closest to the river. Full article
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<p>Map of the development of the research facility area: (<b>a</b>)—year 2001.06, (<b>b</b>)—year 2011.05, (<b>c</b>)—year 2020.08, (<b>d</b>)—year 2022.07, (<b>e</b>)—PLH140055 Łąki Soleckie, (<b>f</b>)—research quarter.</p>
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<p>Elevation of water levels in ditches and wells in cross section: (<b>a</b>)—P1, (<b>b</b>)—P2, (<b>c</b>)—P3, (<b>d</b>)—P4. P<sub>d</sub>—daily precipitation (mm), P<sub>p</sub>—periodic precipitation (mm).</p>
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<p>Groundwater level S<sub>1–4</sub> relation to the surface water in ditches R-29 and R-27 for measurements: (<b>a</b>)—M<sub>1–4</sub> = 720 data, (<b>b</b>)—without precipitation for existing dams N<sub>1–4</sub> = 324 data, (<b>c</b>)—without periodic precipitation W<sub>1–4</sub> = 164 data, (<b>d</b>)—5 days or more without precipitation Z<sub>1–4</sub> = 72 data.</p>
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<p>Ranges of the groundwater levels S for cross sections: M… Z—maximum and minimum elevations in sections; sM… sZ—average elevations in sections; P—cross section.</p>
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<p>Statistics of the linear simple and multiple regression function according to Equation (1): R<sup>2</sup>—determination coefficient; sY—standard error of the estimate.</p>
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<p>Calculated according to Equation (10), groundwater levels S (m.a.s.l.) relation to the surface water in ditches R-29 and R-27: (<b>a</b>)—Z<sub>1–4</sub> = 72 data; (<b>b</b>)—M<sub>1–4</sub> = 720 data.</p>
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<p>Ranges of the groundwater levels for procedure stages: E1–4—stages of data analysis; E5—model verification stage according to Equation (10). Max—maximum; Min—minimum; Mean—average value.</p>
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<p>Measured (Si) and calculated (Y_Si) groundwater level in wells in cross section: (<b>a</b>)—P1, (<b>b</b>)—P2, (<b>c</b>)—P3, (<b>d</b>)—P4. P1_S1, P2_S2, P3_S3, P4_S4—measured groundwater level in cross sections; Y_S1, Y_S2, Y_S3, Y_S4—calculated groundwater levels in cross sections according to Equation (10).</p>
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24 pages, 9497 KiB  
Article
Net Transport Patterns of Surficial Marine Sediments in the North Aegean Sea, Greece
by Ioannis Vakalas and Irene Zananiri
J. Mar. Sci. Eng. 2024, 12(3), 512; https://doi.org/10.3390/jmse12030512 - 20 Mar 2024
Cited by 1 | Viewed by 1018
Abstract
The spatial distribution of sediments on the seafloor reflects the various dynamic processes involved in the marine realm. To analyze sediment transport patterns in the North Aegean Sea, 323 surficial samples were obtained and studied. The granulometry data revealed a diverse range of [...] Read more.
The spatial distribution of sediments on the seafloor reflects the various dynamic processes involved in the marine realm. To analyze sediment transport patterns in the North Aegean Sea, 323 surficial samples were obtained and studied. The granulometry data revealed a diverse range of grain sizes of surficial sediments, ranging from purely sandy to clay. The predominant size classes were silt and muddy sand, followed by sandy silt and mud. However, there were very few samples that fell within the clay classes. The sorting coefficient ranged from 0.21 to 5.48, while skewness ranged from −1.09 to 1.29. The sediment transport patterns were analyzed based on the grain-size parameters (mean, sorting, and skewness). The results showed the variability of flow parameters involved in sediment distribution. River influx and longshore drift near the shoreline are the most significant factors affecting sediment transport. At the open sea, sediment distribution is mainly controlled by general water circulation patterns, especially by the outflow of low-salinity waters from the Black Sea through the Dardanelles and the Marmara Sea. The heterogeneity of sediment textural parameters across the study area suggests that seafloor sediments are further reworked in areas where water masses are highly energetic. It can be concluded that open sea water circulation controls sediment distribution patterns at the open shelf, while close to the coast, river discharge plays a key role. Full article
(This article belongs to the Special Issue Recent Advances in Geological Oceanography II)
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<p>Reference map where the red rectangle marks the study area. The bathymetry hillshade is from the EMODNET database [<a href="#B18-jmse-12-00512" class="html-bibr">18</a>].</p>
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<p>Sampling stations across the study area. Bathymetric contour lines are also shown. The bathymetry hillshade is from the EMODNET database [<a href="#B18-jmse-12-00512" class="html-bibr">18</a>].</p>
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<p>Ternary diagrams representing sample classification [<a href="#B11-jmse-12-00512" class="html-bibr">11</a>].</p>
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<p>Spatial distribution of gravel–sand, silt, and clay ((<b>a</b>–<b>c</b>) respectively).</p>
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<p>Statistical parameters (mean, sorting, skewness) spatial distribution ((<b>a</b>–<b>c</b>) respectively).</p>
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<p>Statistical parameters correlations. The coloring of the various groups of Y-Axis is consistent with the classification presented in <a href="#jmse-12-00512-f005" class="html-fig">Figure 5</a>.</p>
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<p>(<b>a</b>) Histogram of the average vector length of the 100 randomly distributed datasets. (<b>b</b>) Estimation of vector length L90 for a significance level of 0.1. (<b>c</b>) Estimation of vector length L95 for a significance level of 0.05 and (<b>d</b>) Estimation of vector length L99 for a significance level of 0.01. The red part of the plots corresponds to the critical area for the significance tests.</p>
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<p>Net sediment transport pattern across the study area.</p>
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<p>(<b>a</b>) Generalized water circulation pattern where the flow circulation vectors of the various research are also shown [<a href="#B39-jmse-12-00512" class="html-bibr">39</a>,<a href="#B46-jmse-12-00512" class="html-bibr">46</a>,<a href="#B47-jmse-12-00512" class="html-bibr">47</a>]. (<b>b</b>) Vertical salinity distribution across section AB for winter (modified from [<a href="#B38-jmse-12-00512" class="html-bibr">38</a>]). (<b>c</b>) Vertical salinity distribution across section AB for summer (modified from [<a href="#B38-jmse-12-00512" class="html-bibr">38</a>]).</p>
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<p>(<b>a</b>) Surface salinity during winter. (<b>b</b>) Surface salinity during summer (modified from [<a href="#B38-jmse-12-00512" class="html-bibr">38</a>]).</p>
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18 pages, 6327 KiB  
Article
Evaluating the Effectiveness of Rainwater Storage Tanks Based on Different Enabling Rules
by Yongwei Gong, Ge Meng, Kun Tian and Zhuolun Li
Water 2024, 16(5), 787; https://doi.org/10.3390/w16050787 - 6 Mar 2024
Viewed by 1181
Abstract
A proposed method for analyzing the effectiveness of rainwater storage tanks (RWSTs) based on various enabling rule scenarios has been proposed to address the issue of incomplete strategies and measures for controlling excessive rainwater runoff. Three enabling rules for RWSTs have been proposed, [...] Read more.
A proposed method for analyzing the effectiveness of rainwater storage tanks (RWSTs) based on various enabling rule scenarios has been proposed to address the issue of incomplete strategies and measures for controlling excessive rainwater runoff. Three enabling rules for RWSTs have been proposed, as follows: enabling rule I, which involves activation upon rainfall; enabling rule II, which requires the rainfall intensity to reach a predetermined threshold; and enabling rule III, which necessitates the cumulative rainfall to reach a set threshold. In order to assess the effectiveness of these enabling rules when reducing the total volume of rainwater outflow (TVRO), peak flow rate (PFR), and peak flow velocity (PFV), a comparative analysis was conducted to determine which enabling rule yielded the most optimal control effect. The findings indicate that the enabling rule I is responsible for determining the optimal unit catchment’s rainfall capture volume (UCRCV), which is measured at 300 m3·ha−1. Additionally, the control effect of the TVRO of the RWSTs remains largely unaffected by the peak proportion coefficient. Enabling rule II establishes the optimal activation threshold at a rainfall intensity of 1 mm·min−1; under this enabling rule, RWSTs demonstrate the most effective control over PFR and PFV. Enabling rule III enables the determination of the optimal activation threshold, which is set at a cumulative rainfall of 20 mm; under this enabling rule, the implementation of the RWST technique yields the most effective control over the TVRO. Consequently, the optimal rainwater runoff reduction plan for the study area has been successfully determined, providing valuable guidance for the implementation of scientific and reasonable optimal runoff management. Full article
(This article belongs to the Special Issue Urban Flooding Control and Sponge City Construction)
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<p>Location of the study area.</p>
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<p>Multi model coupling: (<b>a</b>) surface runoff model, (<b>b</b>) network convergence model, (<b>c</b>) ground surface flowing model of 2D, and (<b>d</b>) river confluence model.</p>
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<p>Location of RWSTs.</p>
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<p>Rainfall pattern in the study area.</p>
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<p>Calibration and validation results of InfoWorks ICM: (<b>a</b>) calibration result (6 August 2016), (<b>b</b>) calibration result (26 July 2017), (<b>c</b>) verification result (6 August 2017), and (<b>d</b>) verification result (18 August 2017).</p>
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<p>Control effect of TVRO from RWSTs under different enabling rule scenarios. (<b>a</b>,<b>c</b>,<b>e</b>) TVRO at different return periods with enabling rules I, II and III, respectively (<span class="html-italic">P</span> = 1, 3, 5, 10, 20, 50a, <span class="html-italic">r</span> = 0.3). (<b>b</b>,<b>d</b>,<b>f</b>) TVRO at different rain peak coefficients with enabling rules I, II and III, respectively (<span class="html-italic">P</span> = 20a, <span class="html-italic">r</span> = 0.3, 0.5, 0.7).</p>
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<p>PFR control effect of RWSTs under different enabling rule scenarios. (<b>a</b>,<b>c</b>,<b>e</b>) PFR at different return periods with enabling rules Ⅰ, Ⅱ and III, respectively (<span class="html-italic">P</span> = 1, 3, 5, 10, 20, 50a, <span class="html-italic">r</span> = 0.3). (<b>b</b>,<b>d</b>,<b>f</b>) PFR at different rain peak coefficients with enabling rules Ⅰ, Ⅱ and III, respectively (<span class="html-italic">P</span> = 20a, <span class="html-italic">r</span> = 0.3, 0.5, 0.7).</p>
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<p>PFR control effect of RWSTs under different enabling rule scenarios. (<b>a</b>,<b>c</b>,<b>e</b>) PFR at different return periods with enabling rules Ⅰ, Ⅱ and III, respectively (<span class="html-italic">P</span> = 1, 3, 5, 10, 20, 50a, <span class="html-italic">r</span> = 0.3). (<b>b</b>,<b>d</b>,<b>f</b>) PFR at different rain peak coefficients with enabling rules Ⅰ, Ⅱ and III, respectively (<span class="html-italic">P</span> = 20a, <span class="html-italic">r</span> = 0.3, 0.5, 0.7).</p>
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<p>Effect of RWST flow control in different enabling rule scenarios. (<b>a</b>,<b>c</b>,<b>e</b>) PFV at different return periods with enabling rules Ⅰ, Ⅱ and III, respectively (<span class="html-italic">P</span> = 1, 3, 5, 10, 20, 50a, <span class="html-italic">r</span> = 0.3). (<b>b</b>,<b>d</b>,<b>f</b>) PFV at different rain peak coefficient with enabling rules Ⅰ, Ⅱ and III, respectively (<span class="html-italic">P</span> = 20a, <span class="html-italic">r</span> = 0.3, 0.5, 0.7).</p>
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<p>Effect of RWST flow control in different enabling rule scenarios. (<b>a</b>,<b>c</b>,<b>e</b>) PFV at different return periods with enabling rules Ⅰ, Ⅱ and III, respectively (<span class="html-italic">P</span> = 1, 3, 5, 10, 20, 50a, <span class="html-italic">r</span> = 0.3). (<b>b</b>,<b>d</b>,<b>f</b>) PFV at different rain peak coefficient with enabling rules Ⅰ, Ⅱ and III, respectively (<span class="html-italic">P</span> = 20a, <span class="html-italic">r</span> = 0.3, 0.5, 0.7).</p>
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<p>Comparison of TVRO under different enabling rules of RWSTs (<span class="html-italic">P</span> = 1, 3, 5, 10, 20, 50a, <span class="html-italic">r</span> = 0.3). (<b>a</b>) Effect of TVRO control and (<b>b</b>) reduction rate of total external emissions.</p>
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<p>Comparison of PFR under different enabling rules of RWSTs (<span class="html-italic">P</span> = 1, 3, 5, 10, 20, 50a, <span class="html-italic">r</span> = 0.3). (<b>a</b>) PFR control effect and (<b>b</b>)PFR reduction rate.</p>
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<p>Comparison of PFV under different enabling rules of RWSTs (<span class="html-italic">P</span> = 1, 3, 5, 10, 20, 50a, <span class="html-italic">r</span> = 0.3). (<b>a</b>) PFV control effect and (<b>b</b>) PFV reduction rate.</p>
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<p>Performance of enabling rules of different RWSTs: (<b>a</b>,<b>b</b>) represent the control effects of TVRO, PFR, and PFV on 1 August 2016 and 14 August 2016, respectively.</p>
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25 pages, 14641 KiB  
Article
Inequality Evolution of Economic Gains and Environmental Losses in Chinese Interprovincial Trade during 2007–2017
by Yuan Qian, Huan Zheng, Xin Cao, Ting Li, Lin Zhao and Sulian Wang
Sustainability 2024, 16(5), 2033; https://doi.org/10.3390/su16052033 - 29 Feb 2024
Viewed by 817
Abstract
A reduction in SO2 emissions is important for sustainable development. However, China uses territorial emissions to determine its SO2 emission mitigation targets, ignoring the emissions that are incorporated into interregional trade. In addition to the transfer of pollution, value added can [...] Read more.
A reduction in SO2 emissions is important for sustainable development. However, China uses territorial emissions to determine its SO2 emission mitigation targets, ignoring the emissions that are incorporated into interregional trade. In addition to the transfer of pollution, value added can also be exchanged with trade, resulting in environmental inequality among regions. In this study, we estimate the embodied SO2 emissions (ESE) under production-, consumption-, and income-based accounting principles and quantify the embodied value added (EVA) within the interprovincial trade during 2007–2017 using the multi-regional input–output (MRIO) model. The inequalities between the ESE and EVA are further investigated using the Gini coefficients method and the regional environmental index method. The results indicate that ~34.7–43.4% of SO2 emissions and ~24.6–30.8% of value added were triggered by interprovincial trade. Furthermore, developed provinces mainly outsourced their emissions to less developed provinces, particularly to those nearby. Concerning the value added, it was mainly outsourced from less developed provinces to developed provinces during 2007–2010, with no clear patterns observed during 2012–2017. The study’s findings indicate that the high inequality of SO2 emissions and value added also occurred between developed and less developed provinces. Particularly, the Gini coefficients of value inflow–SO2 outflow (VISO) were larger than those of value outflow–SO2 inflow (VOSI), which indicated that, besides the direct emissions, consumption-based emissions should be considered when allocating the environmental responsibility among provinces. These findings are valuable for shaping pathways towards achieving regional economic coordination and sustainable development. Full article
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<p>Research framework of this study.</p>
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<p>PBE for 30 Chinese provinces during 2007–2017 (Unit: 10,000 tons). (Abbreviations of 30 mainland provinces refer to Qian et al. [<a href="#B16-sustainability-16-02033" class="html-bibr">16</a>]).</p>
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<p>CBE for 30 Chinese provinces during 2007–2017 (Unit: 10,000 tons).</p>
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<p>IBE for 30 Chinese provinces during 2007–2017 (Unit: 10,000 tons).</p>
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<p>SO<sub>2</sub> emissions under three perspectives in 2017 (Unit: 10,000 tons).</p>
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<p>Inflows and outflows of ESE in China (Unit: Mt).</p>
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<p>Inflows and outflows of EVA in China (Unit: Million RMB).</p>
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<p>Net flows of ESE and EVA through interprovincial trade in 2017 (the sizes of bubbles indicate the regional GDP per capita at 2012 constant price).</p>
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<p>Transfers of ESE among eight regions in China (Unit: kt) (Note: the numbers beside the rainbows outside the belts indicate the outflows of ESE).</p>
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<p>Transfers of EVA among eight regions in China (Unit: Million RMB) (Note: the numbers beside the rainbows outside the belts indicate the outflows of EVA).</p>
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<p>Lorenz curves and Gini coefficients of VOSI and VISO in 2007–2017.</p>
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<p>The REI index matrix among 30 Chinese provinces in 2017.</p>
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<p>SO<sub>2</sub> emissions under three perspectives in 2007 (Unit: 10,000 tons).</p>
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<p>SO<sub>2</sub> emissions under three perspectives in 2010 (Unit: 10,000 tons).</p>
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<p>SO<sub>2</sub> emissions under three perspectives in 2012 (Unit: 10,000 tons).</p>
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<p>SO<sub>2</sub> emissions under three perspectives in 2015 (Unit: 10,000 tons).</p>
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<p>Net flows of ESE and EVA in 2007 (the sizes of bubbles indicate the regional GDP per capita at 2012 constant price).</p>
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<p>Net flows of ESE and EVA in 2010 (the sizes of bubbles indicate the regional GDP per capita at 2012 constant price).</p>
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<p>Net flows of ESE and EVA in 2012 (the sizes of bubbles indicate the regional GDP per capita at 2012 constant price).</p>
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<p>Net flows of ESE and EVA in 2015 (the sizes of bubbles indicate the regional GDP per capita at 2012 constant price).</p>
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<p>The REI index matrix among 30 Chinese provinces in 2007.</p>
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<p>The REI index matrix among 30 Chinese provinces in 2010.</p>
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<p>The REI index matrix among 30 Chinese provinces in 2012.</p>
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<p>The REI index matrix among 30 Chinese provinces in 2015.</p>
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22 pages, 7815 KiB  
Article
Quantitative Groundwater Modelling under Data Scarcity: The Example of the Wadi El Bey Coastal Aquifer (Tunisia)
by Hatem Baccouche, Manon Lincker, Hanene Akrout, Thuraya Mellah, Yves Armando and Gerhard Schäfer
Water 2024, 16(4), 522; https://doi.org/10.3390/w16040522 - 6 Feb 2024
Viewed by 1644
Abstract
The Grombalia aquifer constitutes a complex aquifer system formed by shallow, unconfined, semi-deep, and deep aquifers at different exploitation levels. In this study, we focused on the upper aquifer, the Wadi El Bey coastal aquifer. To assess natural aquifer recharge, we used a [...] Read more.
The Grombalia aquifer constitutes a complex aquifer system formed by shallow, unconfined, semi-deep, and deep aquifers at different exploitation levels. In this study, we focused on the upper aquifer, the Wadi El Bey coastal aquifer. To assess natural aquifer recharge, we used a novel physiography-based method that uses soil texture-dependent potential infiltration coefficients and monthly rainfall data. The developed transient flow model was then applied to compute the temporal variation in the groundwater level in 34 observation wells from 1973 to 2020, taking into account the time series of spatially variable groundwater recharge, artificial groundwater recharge from 5 surface infiltration basins, pumping rates on 740 wells, and internal prescribed head cells to mimic water exchange between the wadis and aquifer. The quantified deviations in the computed hydraulic heads from measured water levels are acceptable because the database used to construct a scientifically sound and reliable groundwater model was limited. Further work is required to collect field data to quantitatively assess the local inflow and outflow rates between surface water and groundwater. The simulation of 12 climate scenarios highlighted a bi-structured north—south behaviour in the hydraulic heads: an increase in the north and a depletion in the south. A further increase in the pumping rate would, thus, be severe for the southern part of the Wadi El Bey aquifer. Full article
(This article belongs to the Topic Advances in Hydrogeological Research)
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<p>Location of the study site (<b>a</b>) and schematic view of the hydrogeological N—S cross section of the Grombalia unconfined aquifer [<a href="#B21-water-16-00522" class="html-bibr">21</a>] (<b>b</b>), 3D view of the numerical model with location of wadis (yellow dots) (<b>c</b>), location of observation wells, wadi points, and artificial recharge basins implemented in the groundwater flow model (<b>d</b>), and boundary conditions of the numerical model (plan view): prescribed water heads (blue circles) (<b>e</b>), and 740 pumping wells (yellow dots) (<b>f</b>).</p>
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<p>Hydraulic head variation evaluated for the 36 wadi points: (<b>a</b>) Group 1, (<b>b</b>) Group 2, (<b>c</b>) Group 3, and (<b>d</b>) Group 4. Notably, in the legend, the wadi points are abbreviated as WP.</p>
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<p>Spatial distribution of both drainable porosity (<b>a</b>) and isotropic hydraulic conductivity (<b>b</b>).</p>
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<p>Groundwater recharge adopted in the transient flow model: (<b>a</b>) location of the selected seven zones and time-dependent (monthly variable) groundwater recharge for zones (<b>b</b>) RN Perm 4, (<b>c</b>) Perm 25 North, (<b>d</b>) Perm 25 South, (<b>e</b>) RN Perm 35, (<b>f</b>) RN Perm 40, (<b>g</b>) RN Perm 80 North, and (<b>h</b>) RN Perm 80 South. Note: <span class="html-italic">t</span> = 0 d and <span class="html-italic">t</span> = 17,503 d correspond to 1 January 1973 and 31 December 2020, respectively.</p>
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<p>Hydraulic head distribution computed at steady-state flow conditions for 1972 (<b>a</b>) and compared to manually interpolated isolines obtained from field observations (dark lines) and isolines computed with MODFLOW (red lines [<a href="#B27-water-16-00522" class="html-bibr">27</a>]) (<b>b</b>).</p>
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<p>Locations of the 70 chosen virtual observation points (<b>a</b>) and cross-plot of our computed hydraulic heads against the “observed” hydraulic heads obtained in the previous numerical studies of Hammami [<a href="#B27-water-16-00522" class="html-bibr">27</a>] and Gaaloul et al. [<a href="#B14-water-16-00522" class="html-bibr">14</a>] (<b>b</b>). The blue line shown in <a href="#water-16-00522-f006" class="html-fig">Figure 6</a>b represents the 1:1 line.</p>
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<p>Pumping rate applied for each of the 740 wells from 1973 to 2020 (<b>a</b>) and infiltration rate implemented in the model for each of the five artificial recharge basins active between 1990 and 2015 (<b>b</b>).</p>
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<p>Transient flow model: starting values of the hydraulic head on 1 January 1973 (<b>a</b>), and computed hydraulic heads on 31 December 1983 (<b>b</b>), 31 December 1993 (<b>c</b>), 31 December 2003 (<b>d</b>), 31 December 2013 (<b>e</b>), and 31 December 2020 (<b>f</b>). The 25 m contour line is highlighted as a reference for the mean groundwater level.</p>
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<p>Effect of wadis on the transient water balance: (<b>a</b>) cumulative water volume computed (in+/out−) across the fixed head boundaries of the domain and across fixed head nodes located on all 36 Wadi points and those of Oued El Bey-El Melah (Wadi Points 1, 4, 6, 8, 10, 15, 19, 23, 28, 31, 32, and 33; <a href="#water-16-00522-f001" class="html-fig">Figure 1</a>d); (<b>b</b>) inflow and outflow rates computed over the fixed head nodes along Oued El Bey-El Melah. The cumulative inflow water volume across the fixed head boundaries of the total domain (<a href="#water-16-00522-f009" class="html-fig">Figure 9</a>a) corresponds entirely to the water volume coming from the 36 Wadi points. Note: <span class="html-italic">t</span> = 0 d and <span class="html-italic">t</span> = 17,503 d correspond to 1 January 1973 and 31 December 2020, respectively.</p>
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<p>Cross-plot of the computed hydraulic heads against observed water heads at (<b>a</b>) starting values of hydraulic head on 1 January 1973 and computed hydraulic heads for 31 December 1983 (<b>b</b>); 31 December 1993 (<b>c</b>); 31 December 2003 (<b>d</b>); 31 December 2013 (<b>e</b>); and 31 December 2020 (<b>f</b>). The blue lines represent the 1:1 lines; the scatterplot is qualified by the mean error (<math display="inline"><semantics> <mrow> <mover accent="true"> <mrow> <mi>E</mi> </mrow> <mo>¯</mo> </mover> </mrow> </semantics></math>), root mean square error (RMS), and standard deviation (σ), with all the error metrics expressed in metres.</p>
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<p>Hydraulic heads computed from 1973 to 2020 compared to those measured at the four selected observation wells, placed along a north—south longitudinal section in the study site, starting in the north: (<b>a</b>) 2379, (<b>b</b>) 12,406, (<b>c</b>) 8588, and (<b>d</b>) 11,419. The locations of the four observation wells are shown in <a href="#water-16-00522-f001" class="html-fig">Figure 1</a>d. Note: <span class="html-italic">t</span> = 0 d and <span class="html-italic">t</span> = 17,503 d correspond to 1 January 1973 and 31 December 2020, respectively.</p>
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<p>Monthly zonal groundwater recharge (<span class="html-italic">GR</span>) expressed in meter per day for eight distinct zones (see <a href="#water-16-00522-f004" class="html-fig">Figure 4</a>a) used in climate scenario 1 based on RCP 4.5 (<b>a</b>–<b>h</b>) and RCP 8.5 (<b>i</b>–<b>p</b>). Notably, the groundwater recharges in zones ‘RN35’ and ‘RN80’ have been divided into two subzones: one located in the north and one in the south.</p>
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<p>Map of the hydraulic heads computed with climate scenario 1 based on RCP 4.5 at different time stages: starting values on 1 January 2021 (<b>a</b>); 31 December 2040 (<b>b</b>); 31 December 2060 (<b>c</b>); 31 December 2098 (<b>d</b>). The 25 m contour line is highlighted as a reference for the mean groundwater level.</p>
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<p>Results of the time-dependent hydraulic head calculations (from January 2021 to December 2098) under climate scenario 1 for RCP 4.5 (<b>a</b>) and RCP 8.5 (<b>b</b>) at the four selected observation wells.</p>
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<p>Histogram of the hydraulic head differences calculated for RCPs 4.5 (<b>a</b>) and 8.5 (<b>b</b>) from a long-term perspective with regard to baseline hydraulic heads in 2021.</p>
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16 pages, 4408 KiB  
Article
Simulation Test of The Aerodynamic Environment of A Missile-Borne Pulsed Laser Forward Detection System at High Flight Speed
by Peng Liu, Jian Li, Tuan Hua and He Zhang
Photonics 2023, 10(12), 1363; https://doi.org/10.3390/photonics10121363 - 10 Dec 2023
Viewed by 1382
Abstract
When a missile-borne pulsed laser forward detection system flies at supersonic speed, the laser beam will be distorted by the uneven outflow field, resulting in a significant reduction in ranging accuracy. In this paper, the impact of high flight speed on a pulsed [...] Read more.
When a missile-borne pulsed laser forward detection system flies at supersonic speed, the laser beam will be distorted by the uneven outflow field, resulting in a significant reduction in ranging accuracy. In this paper, the impact of high flight speed on a pulsed laser detection system is studied. First, a new ray tracing method with adaptive step size adjustment is proposed, which greatly improves the computational efficiency. Second, the aerodynamic environment of a munition flying at high speed is simulated by an intermittent transonic and supersonic wind tunnel to obtain the schlieren data of the flow field at various Mach numbers. The schlieren data present a shock wave structure similar to that of the simulation. In addition, the variation patterns of the pulsed laser echo waveform of the model under different aerodynamic conditions are studied to evaluate the detectability and operational stability of the laser detection system under static conditions. The test results match the simulation results well, and the two offer relatively consistent shock wave structures, which verifies the correctness and effectiveness of the flow field simulation model. The test echo waveforms are in good agreement with the simulated echo waveforms; the relative errors between the peak values of test and simulated echo waveforms at various Mach numbers do not exceed 20%, and the correlation coefficients between the test and simulated echo waveforms all exceed 0.7, indicating high correlations between the two. Full article
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<p>Relative error of ray tracing along the z-axis.</p>
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<p>Geometric model of the missile body.</p>
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<p>Wind tunnel performance indexes.</p>
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<p>Schematic diagram of the test layout.</p>
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<p>Schlieren diagrams of the flow field at the model front and rear.</p>
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<p>Comparison of schlieren diagrams of the flow field.</p>
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<p>Comparison of test echo waveforms at different Mach numbers.</p>
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<p>Test and simulated echo waveforms at different Mach numbers.</p>
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