[go: up one dir, main page]

 
 
Sign in to use this feature.

Years

Between: -

Subjects

remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline

Journals

remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline

Article Types

Countries / Regions

remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline

Search Results (6,772)

Search Parameters:
Keywords = temperature trend

Order results
Result details
Results per page
Select all
Export citation of selected articles as:
15 pages, 4025 KiB  
Article
Time Series Analysis to Estimate the Volume of Drinking Water Consumption in the City of Meoqui, Chihuahua, Mexico
by Martín Alfredo Legarreta-González, César A. Meza-Herrera, Rafael Rodríguez-Martínez, Carlos Servando Chávez-Tiznado and Francisco Gerardo Véliz-Deras
Water 2024, 16(18), 2634; https://doi.org/10.3390/w16182634 (registering DOI) - 17 Sep 2024
Viewed by 112
Abstract
Water is a vital resource for sustaining life and for numerous processes within the transformation industry. It is a finite resource, albeit one that can be renewed, and thus sustainable management is imperative. To achieve this objective, it is necessary to have the [...] Read more.
Water is a vital resource for sustaining life and for numerous processes within the transformation industry. It is a finite resource, albeit one that can be renewed, and thus sustainable management is imperative. To achieve this objective, it is necessary to have the appropriate tools to assist with the planning policies for its management. This paper presents a time series analysis approach to measure and predict the pattern of water consumption by humans throughout subsectors (domestic, commercial, public sector, education, industry, and raw water) and total water consumption in Meoqui, Chihuahua, Mexico with data from 2011 to 2023, applying calibration model techniques to measure uncertainty in the forecasting. The municipality of Meoqui encompasses an area of 342 km2. The climate is semi-arid, with an average annual rainfall of 272 mm and average temperatures of 26.4 °C in summer and 9.7 °C in winter. The municipal seat, which has a population of 23,140, is supplied with water from ten wells, with an average consumption of 20 ± 579 m3 per user. The consumption of the general population indicates the existence of a seasonal autoregressive integrated moving average (SARIMA) (0,1,2)(0,0,2)12 model. (Sen’s Slope = 682.7, p < 0.001). The domestic sector exhibited the highest overall consumption, with a total volume of 17,169,009 m3 (13 ± 93). A SARIMA (2,1,0)(2,0,0)12 model was estimated, with a Sen’s slope of 221.65 and a p-value of less than 0.001. The second-largest consumer of total water was the “raw water” sector, which consumed 5,124,795 (30,146 ± 35,841) m3 and exhibited an SARIMA (0,1,1)(2,0,0)12 model with no statistically significant trend. The resulting models will facilitate the company’s ability to define water resource management strategies in a sustainable manner, in alignment with projected consumption trends. Full article
(This article belongs to the Section Urban Water Management)
Show Figures

Figure 1

Figure 1
<p>Chihuahua State and its municipalities. Meoqui municipality in blue.</p>
Full article ">Figure 2
<p>Satellite view of Meoqui City and location of the wells utilized for the extraction of potable water.</p>
Full article ">Figure 3
<p>ARIMA model plot results with 1-year forecast for the total consumption of potable water in Meoqui, Chihuahua, Mexico.</p>
Full article ">Figure 4
<p>ARIMA model plot results with 1-year forecast for the consumption of potable water from the domestic sector in Meoqui, Chihuahua, Mexico.</p>
Full article ">Figure 5
<p>ARIMA model plot results with 1-year forecast for the consumption of potable water from the commercial sector in Meoqui, Chihuahua, Mexico.</p>
Full article ">Figure 6
<p>Results of the ARIMA model, with a 1-year consumption forecast, for users in the Public sector of Meoqui, Chihuahua, Mexico.</p>
Full article ">Figure 7
<p>Results of the ARIMA model, with a 1-year consumption forecast, for users in the Education sector of Meoqui, Chihuahua, Mexico.</p>
Full article ">Figure 8
<p>Results of the ARIMA model, with a 1-year consumption forecast, for users in the industrial sector of Meoqui, Chihuahua, Mexico.</p>
Full article ">Figure 9
<p>ARIMA model plot results with 1-year forecast for raw water sector consumption in Meoqui, Chihuahua, Mexico.</p>
Full article ">
19 pages, 1502 KiB  
Article
Multi-Spectral Radiation Temperature Measurement: A High-Precision Method Based on Inversion Using an Enhanced Particle Swarm Optimization Algorithm with Multiple Strategies
by Xiaodong Wang and Shuaifeng Han
Sensors 2024, 24(18), 6003; https://doi.org/10.3390/s24186003 (registering DOI) - 17 Sep 2024
Viewed by 171
Abstract
Multi-spectral temperature measurement technology has been found to have extensive applications in engineering practice. Addressing the challenges posed by unknown emissivity in multi-spectral temperature measurement data processing, this paper adds emissivity constraints to the objective function. It proposes a multi-spectral radiation temperature measurement [...] Read more.
Multi-spectral temperature measurement technology has been found to have extensive applications in engineering practice. Addressing the challenges posed by unknown emissivity in multi-spectral temperature measurement data processing, this paper adds emissivity constraints to the objective function. It proposes a multi-spectral radiation temperature measurement data processing model realized through a particle swarm optimization algorithm improved based on multiple strategies. This paper simulates six material models with distinct emissivity trends. The simulation results indicate that the algorithm calculates an average relative temperature error of less than 0.3%, with an average computation time of merely 0.24 s. When applied to the temperature testing of silicon carbide and tungsten, experimental data further confirmed its accuracy: the absolute temperature error for silicon carbide (tungsten) is less than 4 K (7 K), and the average relative error is below 0.4% (0.3%), while two materials maintain an average computation time of 0.33 s. In summary, the improved particle swarm optimization algorithm demonstrates strong performance and high accuracy in multi-spectral radiation thermometry, making it a feasible solution for addressing multi-spectral temperature measurement challenges in practical engineering applications. Additionally, it can be extended to other multi-spectral systems. Full article
Show Figures

Figure 1

Figure 1
<p>Flowchart of the MSPSO algorithm.</p>
Full article ">Figure 2
<p>Calculate the relative error of temperature for six models using the MSPSO algorithm.</p>
Full article ">Figure 3
<p>Calculate the relative error of temperature for six models using the MSPSO algorithm (with 5% random noise).</p>
Full article ">Figure 4
<p>Comparison of emissivity calculated by PSO and MSPSO algorithms with true values (the six subfigures (<b>A</b>–<b>F</b>) represent the emissivity trends of six different materials.).</p>
Full article ">Figure 5
<p>Comparison of computation time, absolute temperature error, and relative temperature error for six models before and after algorithm improvement.</p>
Full article ">Figure 6
<p>The figure shows the convergence of the objective function and the changes in parameters <math display="inline"><semantics> <msub> <mi>c</mi> <mn>1</mn> </msub> </semantics></math> and <math display="inline"><semantics> <msub> <mi>c</mi> <mn>2</mn> </msub> </semantics></math>.</p>
Full article ">Figure 7
<p>The 3D view of the emissivity measuring apparatus.</p>
Full article ">Figure 8
<p>Comparison of measured spectral emissivity values with calculated values from three algorithms for two sample materials. Specifically, (<b>A</b>–<b>C</b>) represent silicon carbide, while (<b>D</b>–<b>F</b>) represent tungsten.</p>
Full article ">
19 pages, 5656 KiB  
Article
Study on the Factors Affecting the Humus Horizon Thickness in the Black Soil Region of Liaoning Province, China
by Ying-Ying Jiang, Jia-Yi Tang and Zhong-Xiu Sun
Agronomy 2024, 14(9), 2106; https://doi.org/10.3390/agronomy14092106 - 15 Sep 2024
Viewed by 384
Abstract
Understanding the spatial variability and driving mechanisms of humus horizon thickness (HHT) degradation is crucial for effective soil degradation prevention in black soil regions. The study compared ordinary kriging interpolation (OK), inverse distance weighted interpolation (IDW), and regression kriging interpolation (RK) using mean [...] Read more.
Understanding the spatial variability and driving mechanisms of humus horizon thickness (HHT) degradation is crucial for effective soil degradation prevention in black soil regions. The study compared ordinary kriging interpolation (OK), inverse distance weighted interpolation (IDW), and regression kriging interpolation (RK) using mean error (ME), mean absolute error (MAE), root mean square error (RMSE), and relative RMSE to select the most accurate model. Environmental variables were then integrated to predict HHT characteristics. Results indicate that: (1) RK was superior to OK and IDW in characterizing HHT with the smallest ME (11.45), RMSE (14.98), MAE (11.45), and RRMSE (0.44). (2) The average annual temperature (0.29), precipitation (0.27), and digital elevation model (DEM) (0.21) were the primary factors influencing the spatial variability of HHT. (3) The HHT exhibited notable variability, with an increasing trend from the southeast towards the central and northern directions, being the thinnest in the southeast. It was thicker in the northeast and southwest regions, thicker but less dense along the southern Bohai coast, thicker yet sporadically distributed in the northwest (especially Chaoyang and Fuxin), and thick with aggregated distribution over a smaller area in the northeastern direction (e.g., Tieling). These findings provide a scientific basis for accurate soil management in Liaoning Province. Full article
(This article belongs to the Section Soil and Plant Nutrition)
Show Figures

Figure 1

Figure 1
<p>Overview of the study area. The red region on the inset map shows the location of Liaoning Province in China.</p>
Full article ">Figure 2
<p>The environmental variables in the study. Notes, (<b>a</b>): average annual temperature; (<b>b</b>): land use type; (<b>c</b>): vegetation type; (<b>d</b>): vegetation type; (<b>e</b>): geomorphology; (<b>f</b>): annual precipitation.</p>
Full article ">Figure 3
<p>Distribution map of sampling points for collected soil data.</p>
Full article ">Figure 4
<p>Random Forest principal schematic [<a href="#B30-agronomy-14-02106" class="html-bibr">30</a>].</p>
Full article ">Figure 5
<p>Histogram of humus horizon thickness data.</p>
Full article ">Figure 6
<p>Interpolation results for humus horizon thickness.</p>
Full article ">Figure 7
<p>RK results of humus horizon thickness.</p>
Full article ">
17 pages, 6295 KiB  
Article
Study on the Effect of Pressure on the Microstructure, Mechanical Properties, and Impact Wear Behavior of Mn-Cr-Ni-Mo Alloyed Steel Fabricated by Squeeze Casting
by Bo Qiu, Longxia Jia, Heng Yang, Zhuoyu Guo, Chuyun Jiang, Shuting Li and Biao Sun
Metals 2024, 14(9), 1054; https://doi.org/10.3390/met14091054 - 15 Sep 2024
Viewed by 360
Abstract
ZG25MnCrNiMo steel samples were prepared by squeeze casting under pressure ranging from 0 to 150 MPa. The effects of pressure on the microstructure, low-temperature toughness, hardness, and impact wear performance of the prepared steels were experimentally investigated. The experimental results indicated that the [...] Read more.
ZG25MnCrNiMo steel samples were prepared by squeeze casting under pressure ranging from 0 to 150 MPa. The effects of pressure on the microstructure, low-temperature toughness, hardness, and impact wear performance of the prepared steels were experimentally investigated. The experimental results indicated that the samples fabricated under pressure exhibited finer grains and a significant ferrite content compared to those produced without pressure. Furthermore, the secondary dendrite arm spacing of the sample produced at 150 MPa decreased by 45.3%, and the ferrite content increased by 39.1% in comparison to the unpressurized sample. The low-temperature impact toughness of the steel at −40 °C initially increased and then decreased as the pressure varied from 0 MPa to 150 MPa. And the toughness achieved an optimal value at a pressure of 30 MPa, which was 65.4% greater than that of gravity casting (0 MPa), while the hardness decreased by only 6.17%. With a further increase in pressure, the impact work decreased linearly while the hardness increased slightly. Impact fracture analysis revealed that the fracture of the steel produced without pressure exhibited a quasi-cleavage morphology. The samples prepared by squeeze casting under 30 MPa still exhibited a large number of fine dimples even at −40 °C, indicative of ductile fracture. In addition, the impact wear performance of the steels displayed a trend of initially decreasing and subsequently increasing across the pressure range of 0–150 MPa. The wear resistance of samples prepared without pressure and at 30 MPa was superior to that at 60 MPa, and the wear resistance deteriorated when the pressure increased to 60 MPa, after which it exhibited an upward trend as the pressure continued to rise. The wear mechanisms of the samples predominantly consisted of impact wear, adhesive wear, and minimal abrasive wear, along with notable occurrences of plastic removal, furrows, and spalling. Full article
Show Figures

Figure 1

Figure 1
<p>Sampling position diagram of the prepared sample.</p>
Full article ">Figure 2
<p>Microstructure of the samples prepared under different pressures: (<b>a</b>) 0 MPa; (<b>b</b>) 30 MPa; (<b>c</b>) 60 MPa; (<b>d</b>) 90 MPa; (<b>e</b>) 120 MPa; (<b>f</b>) 150 MPa.</p>
Full article ">Figure 3
<p>Secondary dendrite arm spacing and ferritic content of the samples prepared under different pressures.</p>
Full article ">Figure 4
<p>SEM images at a higher magnification of the microstructure of the samples prepared under different pressures: (<b>a</b>) 0 MPa; (<b>b</b>) 30 MPa; (<b>c</b>) 60 MPa; (<b>d</b>) 90 MPa; (<b>e</b>) 120 MPa; (<b>f</b>) 150 MPa.</p>
Full article ">Figure 5
<p>XRD analysis of the steel prepared under various pressures.</p>
Full article ">Figure 6
<p>Variation in the density and porosity of the steels prepared at different pressures.</p>
Full article ">Figure 7
<p>(<b>a</b>) Brinell hardness of the samples prepared under different pressures; (<b>b</b>) low-temperature (−40 °C) impact energy of the samples prepared under different pressures.</p>
Full article ">Figure 8
<p>Macro- and micro-impact fracture morphology of the samples prepared under different pressures: (<b>a</b>–<b>a’</b>) 0 MPa; (<b>b</b>–<b>b’</b>) 30 MPa; (<b>c</b>–<b>c’</b>) 60 MPa; (<b>d</b>–<b>d’</b>) 90 MPa; (<b>e</b>–<b>e’</b>) 120 MPa; (<b>f</b>–<b>f’</b>) 150 MPa.</p>
Full article ">Figure 9
<p>EDS analysis results of the impact fracture morphology for the sample prepared under 30 MPa: (<b>a</b>) site 1; (<b>b</b>) site 2.</p>
Full article ">Figure 10
<p>(<b>a</b>) Relationship between wear time and wear loss of the samples prepared under different pressures; (<b>b</b>) wear rate of the samples prepared under different pressures.</p>
Full article ">Figure 11
<p>Morphology of the worn surface of the samples prepared under different pressures: (<b>a</b>) 0 MPa; (<b>b</b>) 30 MPa; (<b>c</b>) 60 MPa; (<b>d</b>) 90 MPa; (<b>e</b>) 120 MPa; (<b>f</b>) 150 MPa.</p>
Full article ">
18 pages, 6210 KiB  
Article
Research on Glacier Changes and Their Influencing Factors in the Yigong Zangbo River Basin of the Tibetan Plateau, China, Based on ICESat-2 Data
by Wei Nie, Qiqi Du, Xuepeng Zhang, Kunxin Wang, Yang Liu, Yongjie Wang, Peng Gou, Qi Luo and Tianyu Zhou
Water 2024, 16(18), 2617; https://doi.org/10.3390/w16182617 - 15 Sep 2024
Viewed by 274
Abstract
The intense changes in glaciers in the southeastern Tibetan Plateau (SETP) have essential impacts on regional water resource management. In order to study the seasonal fluctuations of glaciers in this region and their relationship with climate change, we focus on the Yigong Zangbo [...] Read more.
The intense changes in glaciers in the southeastern Tibetan Plateau (SETP) have essential impacts on regional water resource management. In order to study the seasonal fluctuations of glaciers in this region and their relationship with climate change, we focus on the Yigong Zangbo River Basin in the SETP, extract the annual and seasonal variations of glaciers in the basin during 2018–2023, and analyze their spatio-temporal characteristics through the seasonal-trend decomposition using the LOESS (STL) method. Finally, combining the Extreme Gradient Boosting (XGBoost) model and the Shapley additive explanations (SHAP) model, we assess the comprehensive impact of meteorological factors such as temperature and snowfall on glacier changes. The results indicate that glaciers in the Yigong Zangbo River Basin experienced remarkable mass loss during 2018–2023, with an average annual melting rate of −0.83 ± 0.12 m w.e.∙yr−1. The glacier mass exhibits marked seasonal fluctuations, with increases in January–March (JFM) and April–June (AMJ) and noticeable melting in July–September (JAS) and October–December (OND). The changes over these four periods are 2.12 ± 0.04 m w.e., 0.93 ± 0.15 m w.e., −1.58 ± 0.19 m w.e., and −1.32 ± 0.17 m w.e., respectively. Temperature has been identified as the primary meteorological driver of glacier changes in the study area, surpassing the impact of snowfall. This study uses advanced altimetry data and meteorological data to monitor and analyze glacier changes, which provides valuable data for cryosphere research and also validates a set of replicable research methods, which provides support for future research in related fields. Full article
(This article belongs to the Section Water and Climate Change)
Show Figures

Figure 1

Figure 1
<p>(<b>a</b>) Overview of the study area, (<b>b</b>) distribution of the ICESat-2 points in the study area, and (<b>c</b>) the location of the study area on the Tibetan Plateau.</p>
Full article ">Figure 2
<p>Technical flowchart. “GMC” denotes glacier mass changes, “DEM” the digital elevation model, “RGI” the Randolph Glacier Inventory data, “STL” the seasonal-trend decomposition using LOESS, and “SHAP” the Shapley additive explanations.</p>
Full article ">Figure 3
<p>A schematic diagram of the XGBoost model. The red arrow denotes the selected direction of the tree, the yellow circle denotes the selected node, the green circle denotes the unselected node.</p>
Full article ">Figure 4
<p>Glacier mass change (GMC), seasonal mass difference (<math display="inline"><semantics> <mrow> <mo>∆</mo> <msub> <mrow> <mi mathvariant="normal">M</mi> </mrow> <mrow> <mi mathvariant="normal">S</mi> <mi mathvariant="normal">T</mi> <mi mathvariant="normal">L</mi> </mrow> </msub> </mrow> </semantics></math>), and trend and seasonal components after the STL decomposition.</p>
Full article ">Figure 5
<p>Deseasonalized GMC series X <math display="inline"><semantics> <mrow> <mo>(</mo> <msub> <mrow> <mi mathvariant="normal">X</mi> </mrow> <mrow> <mi mathvariant="normal">i</mi> </mrow> </msub> <mo>=</mo> <msub> <mrow> <mi mathvariant="normal">T</mi> </mrow> <mrow> <mi mathvariant="normal">i</mi> </mrow> </msub> <mo>+</mo> <msub> <mrow> <mi mathvariant="sans-serif">ε</mi> </mrow> <mrow> <mi mathvariant="normal">i</mi> </mrow> </msub> <mo>)</mo> </mrow> </semantics></math>.</p>
Full article ">Figure 6
<p>(<b>a</b>) Average seasonal GMC relative to ALOS DEM (<math display="inline"><semantics> <mrow> <mover accent="true"> <mrow> <mi mathvariant="normal">G</mi> <mi mathvariant="normal">M</mi> <mi mathvariant="normal">C</mi> </mrow> <mo>¯</mo> </mover> </mrow> </semantics></math>) and glacial area with altitude, and (<b>b</b>) average seasonal variation in glacier mass (<math display="inline"><semantics> <mrow> <mover accent="true"> <mrow> <mo>∆</mo> <mi mathvariant="normal">M</mi> </mrow> <mo>¯</mo> </mover> </mrow> </semantics></math>) at different altitudes.</p>
Full article ">Figure 7
<p>Seasonal variation in glacier mass (<math display="inline"><semantics> <mrow> <mover accent="true"> <mrow> <mo>∆</mo> <mi mathvariant="normal">M</mi> </mrow> <mo>¯</mo> </mover> </mrow> </semantics></math>) in (<b>a</b>) JFM, (<b>b</b>) AMJ, (<b>c</b>) JAS, and (<b>d</b>) OND.</p>
Full article ">Figure 8
<p>SHAP values of the meteorological drivers for the GMC.</p>
Full article ">Figure 9
<p>Scatter plots of the SHAP values of (<b>a</b>) temperature and (<b>b</b>) snowfall and their functional relationships with the GMC.</p>
Full article ">Figure 10
<p>(<b>a</b>) Monthly average temperature and accumulated precipitation within the study region (2018–2023); seasonal average (<b>b</b>) temperature and (<b>c</b>) precipitation. “Tem” denotes temperature, “TP” denotes total precipitation, and “SF” denotes snowfall.</p>
Full article ">Figure 11
<p>Seasonal averages of (<b>a</b>–<b>d</b>) temperature and (<b>e</b>–<b>h</b>) snowfall from 2018 to 2023.</p>
Full article ">Figure 12
<p>Variations in the standard deviations of the (<b>a</b>) temperature (<math display="inline"><semantics> <mrow> <msub> <mrow> <mi mathvariant="sans-serif">σ</mi> </mrow> <mrow> <mi mathvariant="normal">T</mi> <mi mathvariant="normal">e</mi> <mi mathvariant="normal">m</mi> </mrow> </msub> </mrow> </semantics></math>), snowfall (<math display="inline"><semantics> <mrow> <msub> <mrow> <mi mathvariant="sans-serif">σ</mi> </mrow> <mrow> <mi mathvariant="normal">S</mi> <mi mathvariant="normal">F</mi> </mrow> </msub> </mrow> </semantics></math>), and (<b>b</b>) seasonal variation in glaciers (<math display="inline"><semantics> <mrow> <msub> <mrow> <mi mathvariant="sans-serif">σ</mi> </mrow> <mrow> <mi mathvariant="sans-serif">Δ</mi> <mi mathvariant="normal">M</mi> </mrow> </msub> </mrow> </semantics></math>) with altitude.</p>
Full article ">
18 pages, 5123 KiB  
Article
Spatiotemporal Changes in the Quantity and Quality of Water in the Xiao Bei Mainstream of the Yellow River and Characteristics of Pollutant Fluxes
by Zhenzhen Yu, Xiaojuan Sun, Li Yan, Yong Li, Huijiao Jin and Shengde Yu
Water 2024, 16(18), 2616; https://doi.org/10.3390/w16182616 - 15 Sep 2024
Viewed by 343
Abstract
The Xiao Bei mainstream, located in the middle reaches of the Yellow River, plays a vital role in regulating the quality of river water. Our study leveraged 73 years of hydrological data (1951–2023) to investigate long-term runoff trends and seasonal variations in the [...] Read more.
The Xiao Bei mainstream, located in the middle reaches of the Yellow River, plays a vital role in regulating the quality of river water. Our study leveraged 73 years of hydrological data (1951–2023) to investigate long-term runoff trends and seasonal variations in the Xiao Bei mainstream and its two key tributaries, the Wei and Fen Rivers. The results indicated a significant decline in runoff over time, with notable interannual fluctuations and an uneven distribution of runoff within the year. The Wei and Fen Rivers contributed 19.75% and 3.59% of the total runoff to the mainstream, respectively. Field monitoring was conducted at 11 locations along the investigated reach of Xiao Bei, assessing eight water quality parameters (temperature, pH, dissolved oxygen (DO), chemical oxygen demand (COD), ammonia nitrogen (NH3-N), total phosphorus (TP), permanganate index (CODMn), and 5-day biochemical oxygen demand (BOD5)). Our long-term results showed that the water quality of the Xiao Bei mainstream during the monitoring period was generally classified as Class III. Water quality parameters at the confluence points of the Wei and Fen Rivers with the Yellow River were higher compared with the mainstream. After these tributaries merged into the mainstream, local sections show increased concentrations, with the water quality parameters exhibiting spatial fluctuations. Considering the mass flux process of transmission of the quantity and quality of water, the annual NH3-N inputs from the Fen and Wei Rivers to the Yellow River accounted for 11.5% and 67.1%, respectively, and TP inputs accounted for 6.8% and 66.18%. These findings underscore the critical pollutant load from tributaries, highlighting the urgent need for effective pollution management strategies targeting these tributaries to improve the overall water quality of the Yellow River. This study sheds light on the spatiotemporal changes in runoff, water quality, and pollutant flux in the Xiao Bei mainstream and its tributaries, providing valuable insights to enhance the protection and management of the Yellow River’s water environment. Full article
Show Figures

Figure 1

Figure 1
<p>Yellow River (<b>left</b>) and map of the study area (<b>right</b>). The mainstream, tributaries, and basin area of the Yellow River are shown on the left. The investigated Xiao Bei mainstream, with the Wei River and Fen River tributaries and the proximal hydrologic and water quality stations are shown on the right.</p>
Full article ">Figure 2
<p>Trends and variations in monthly and annual runoff at Longmen and Tongguan hydrological stations from 1951 to 2023. (<b>a1</b>) Trend of monthly average runoff at Longmen hydrological station. (<b>a2</b>) Differences in runoff from the annual mean at Longmen hydrological station. (<b>b1</b>) Trend of monthly average runoff at Tongguan hydrological station. (<b>b2</b>) Differences in runoff from the annual mean at Tongguan hydrological station.</p>
Full article ">Figure 3
<p>Intra-annual distribution of long-term average runoff for the Xiao Bei mainstream. (<b>a</b>) Graphs of the monthly distribution of density with histograms and rug plots for the Longmen (blue) and Tongguan (orange) stations over 73 years. The smooth curves represent the probability density functions of the runoff data, providing a continuous view of the data’s distribution. The histograms illustrate the frequency of data points within specific intervals, while the rug plots show individual data points along the <span class="html-italic">x</span>-axis. (<b>b</b>) Line plot showing the measured intra-annual average runoff data for Longmen and Tongguan stations.</p>
Full article ">Figure 4
<p>Trends and variations in monthly and annual runoff at Huaxian and Hejin hydrological stations from 1951 to 2023. (<b>a1</b>) Trend of monthly average runoff at Huaxian hydrological station. (<b>a2</b>) Differences in runoff from the annual mean at Huaxian hydrological station. (<b>b1</b>) Trend of monthly average runoff at Hejin hydrological station. (<b>b2</b>) Differences in runoff from the annual mean at Hejin hydrological station.</p>
Full article ">Figure 5
<p>Intra-annual distribution of long-term average runoff from the Wei River (Huaxian hydrological station) and Fen River (Hejin hydrological station). (<b>a</b>) Graphs of the monthly distribution of density with histograms and rug plots for Huaxian (green) and Hejin (purple) stations over 73 years. The smooth curves represent the probability density functions of the runoff data, providing a continuous view of the data’s distribution. The histograms illustrate the frequency of data points within specific intervals, while the rug plots show individual data points along the <span class="html-italic">x</span>-axis. (<b>b</b>) Line plot showing the measured intra-annual average runoff data for Huaxian and Hejin stations.</p>
Full article ">Figure 6
<p>Comparison of average monthly runoff between the tributaries and mainstream of the Yellow River. (<b>a</b>) Contribution of the Fen River to the Yellow River (<b>b</b>) Contribution of the Wei River to the Yellow River.</p>
Full article ">Figure 7
<p>Characterization of the concentrations of factors for monitoring water quality in the Xiao Bei mainstream: Green area display the data distribution and dark area represents the inter quartile range, which spans from the 25th to the 75th percentile of the data.</p>
Full article ">Figure 8
<p>Comparison of water quality factors in the mainstream and tributaries of the Xiao Bei mainstream.</p>
Full article ">Figure 9
<p>Changes in the monitored values of water quality factors over 11 sampling points along the studied reach. (<b>a</b>) Temperature, (<b>b</b>) pH, (<b>c</b>) chemical oxygen demand (COD), (<b>d</b>) ammonia nitrogen (NH<sub>3</sub>-N), (<b>e</b>) total phosphorus (TP), (<b>f</b>) permanganate index (COD<sub>Mn</sub>), (<b>g</b>) 5-day biochemical oxygen demand (BOD<sub>5</sub>).</p>
Full article ">Figure 10
<p>Monthly changes in TP and NH<sub>3</sub>-N fluxes in the Xiao Bei mainstream in 2021.</p>
Full article ">
22 pages, 5560 KiB  
Article
Prediction of the Temperature Field in a Tunnel during Construction Based on Airflow–Surrounding Rock Heat Transfer
by Guofeng Wang, Yongqiao Fang, Kaifu Ren, Fayi Deng, Bo Wang and Heng Zhang
Buildings 2024, 14(9), 2908; https://doi.org/10.3390/buildings14092908 - 14 Sep 2024
Viewed by 231
Abstract
It is important to determine the ventilation required in the construction of deep and long tunnels and the variation law of tunnel temperature fields to reduce the numbers of high-temperature disasters and serious accidents. Based on a tunnel project with a high ground [...] Read more.
It is important to determine the ventilation required in the construction of deep and long tunnels and the variation law of tunnel temperature fields to reduce the numbers of high-temperature disasters and serious accidents. Based on a tunnel project with a high ground temperature, with the help of convection heat transfer theory and the theoretical analysis and calculation method, this paper clarifies the contribution of various heat sources to the air demand during tunnel construction, and reveals the important environmental parameters that determine the ventilation value by changing the construction conditions. The results show that increasing the fresh air temperature greatly increases the required air volume, and the closer the supply air temperature is to 28 °C, the more the air volume needs to be increased. The air temperature away from the palm face is not significantly affected by changes in the supply air temperature. Adjusting the wall temperature greatly accelerates the rate of temperature growth. The supply air temperature rose from 15 to 25 °C, while the tunnel temperature at 800 m only increased by 1.5 °C. Over a 50 m range, the wall temperature rose from 35 to 60 degrees Celsius at a rate of 0.0842 to 0.219 degrees Celsius per meter. The total air volume rises and the surface heat transfer coefficient decreases as the tunnel’s cross-section increases. For every 10 m increase in the tunnel diameter, the temperature at 800 m from the tunnel face drops by about 0.5 °C. Changing the distance between the air duct and the tunnel face has little influence on the temperature distribution law. The general trend is that the farther the air duct outlet is from the tunnel face, the higher the temperature is, and the maximum difference is within the range of 50 m~250 m from the tunnel face. The maximum difference between the air temperatures at 12 m and 27 m is 0.79 °C. The geological structure and geothermal background have the greatest influence on the temperature prediction of high geothermal tunnels. The prediction results are of great significance for guiding tunnel construction, formulating cooling measures, and ensuring construction safety. Full article
Show Figures

Figure 1

Figure 1
<p>High geothermal tunnel construction ventilation heat source diagram.</p>
Full article ">Figure 2
<p>Air demand–supply air temperature curve.</p>
Full article ">Figure 3
<p>Air volume–cooling section length curve.</p>
Full article ">Figure 4
<p>Air volume–wall temperature curve.</p>
Full article ">Figure 5
<p>Distribution law of wind speed on ventilation wall of tunnel.</p>
Full article ">Figure 6
<p>Convective heat transfer of tunnel return air disc.</p>
Full article ">Figure 7
<p>Fitting curve of air thermophysical properties changing with air temperature.</p>
Full article ">Figure 8
<p><span class="html-italic">Nu<sub>c</sub></span> distribution curve of convective heat transfer enhancement zone.</p>
Full article ">Figure 9
<p>Fitting curve and equation of convective heat transfer enhancement.</p>
Full article ">Figure 10
<p>Temperature distribution curve.</p>
Full article ">Figure 11
<p>Mesh generation of 3D model.</p>
Full article ">Figure 12
<p>Comparison curve of calculation results.</p>
Full article ">Figure 13
<p>Temperature distribution law of tunnel with different supply air temperatures. (Note: <span class="html-italic">r</span>—tunnel radius; <span class="html-italic">T</span><sub>a</sub>—wind temperature; <span class="html-italic">T</span><sub>w</sub>—surrounding rock temperature; <span class="html-italic">v</span>—return air velocity; <span class="html-italic">L</span>—distance between air duct and tunnel face.)</p>
Full article ">Figure 14
<p>Distribution law of tunnel air temperature under different wall temperatures.</p>
Full article ">Figure 15
<p>Temperature distribution law of different tunnel section sizes.</p>
Full article ">Figure 16
<p>Distribution law of air temperature at different placement distances of air duct.</p>
Full article ">
17 pages, 6811 KiB  
Article
Effects of Biophysical Factors on Light Use Efficiency at Multiple Time Scales in a Chinese Cork Oak Plantation Ecosystem
by Xiang Gao, Jinsong Zhang, Jinfeng Cai, Ping Meng, Hui Huang and Shoujia Sun
Forests 2024, 15(9), 1620; https://doi.org/10.3390/f15091620 - 14 Sep 2024
Viewed by 202
Abstract
Light use efficiency (LUE) characterizes the efficiency of vegetation in converting photosynthetically active radiation (PAR) into biomass energy through photosynthesis and is a critical parameter for gross primary productivity (GPP) in terrestrial ecosystems. Based on the eddy covariance measurements of a Chinese cork [...] Read more.
Light use efficiency (LUE) characterizes the efficiency of vegetation in converting photosynthetically active radiation (PAR) into biomass energy through photosynthesis and is a critical parameter for gross primary productivity (GPP) in terrestrial ecosystems. Based on the eddy covariance measurements of a Chinese cork oak plantation ecosystem in northern China, the temporal variations in LUE were investigated, and biophysical factors were examined at time scales ranging from hours to years. Our results show that diurnal LUE first increased sharply before 8:30 and then decreased gradually until 12:00, thereafter increasing gradually and reaching the maximum value at sunset during the growing season. The daily and monthly LUE first increased and then decreased within a year and showed a substantial drop around June. The annual LUE ranged from 0.09 to 0.17 g C mol photon−1, and the multiyear mean maximal LUE was 0.30 g C mol photon−1 during 2006–2019. Only GPP (positive) and clearness index (CI) (negative) had consistent effects on LUE at different time scales, and the effects of the remaining biophysical factors on LUE were different as the time scale changed. The effects of air temperature, vapor pressure deficit, precipitation, evaporative fraction, and normalized difference vegetation index on LUE were mainly indirect (via PAR and/or GPP). When CI decreased, an increased ratio of diffuse PAR to PAR produced a more uniform irradiance in the canopy, which ultimately resulted in a higher LUE. Due to climate change in our study area, the annual LUE may decrease in the future but improving management practices may slow or even reverse this trend in the annual LUE in the studied Chinese cork oak plantation. Full article
(This article belongs to the Section Forest Ecophysiology and Biology)
Show Figures

Figure 1

Figure 1
<p>Location of the study site (<b>a</b>) and the observation tower (<b>b</b>).</p>
Full article ">Figure 2
<p>General trends in (<b>a</b>) annual solar radiation (S<sub>r</sub>), (<b>b</b>) annual mean air temperature (T<sub>a</sub>), and (<b>c</b>) annual precipitation (P) in our study area during 1960–2019. The <span class="html-italic">p</span> and s values are the significance levels and slopes of the red lines.</p>
Full article ">Figure 3
<p>Monthly mean diurnal course (PAR &gt; 50 μmol m<sup>–2</sup> s<sup>–1</sup>) of (<b>a</b>) photosynthetically active radiation (PAR), (<b>b</b>) gross primary productivity (GPP), and (<b>c</b>) light use efficiency (LUE) in the Chinese cork oak plantation during the growing seasons of 2018 and 2019.</p>
Full article ">Figure 4
<p>Correlation analysis (<b>a</b>) and path analysis (<b>b</b>) among 30 min biophysical factors and LUE around noon (10:00–14:00) during May–September in 2018 and 2019 in the Chinese cork oak plantation. * Significant at <span class="html-italic">p</span> &lt; 0.05; *** significant at <span class="html-italic">p</span> &lt; 0.001.</p>
Full article ">Figure 5
<p>Seasonal variations in the daily PAR (<b>a</b>), GPP (<b>b</b>), and LUE (<b>c</b>) in the Chinese cork oak plantation in 2018 and 2019.</p>
Full article ">Figure 6
<p>Correlation analysis (<b>a</b>) and path analysis (<b>b</b>) among daily biophysical factors and LUE during May–September in 2018 and 2019 in the Chinese cork oak plantation. * Significant at <span class="html-italic">p</span> &lt; 0.05; ** significant at <span class="html-italic">p</span> &lt; 0.01; *** significant at <span class="html-italic">p</span> &lt; 0.001.</p>
Full article ">Figure 7
<p>Relationship between the CI and (<b>a</b>) GPP; (<b>b</b>) the ratio of diffuse PAR (PAR<sub>f</sub>) to PAR (TD<sub>f</sub>), (<b>c</b>) direct PAR (PAR<sub>r</sub>), and PAR<sub>f</sub> (<b>d</b>); and the effects of PAR<sub>r</sub> (<b>e</b>) and PAR<sub>f</sub> (<b>f</b>) on GPP during May–September in 2018 and 2019 in the Chinese cork oak plantation. Daily GPP (<b>a</b>), TD<sub>f</sub> (<b>b</b>), PAR<sub>r</sub> (<b>c</b>), and PAR<sub>f</sub> (<b>d</b>) were bin-averaged into 0.05 CI increments. Daily GPP was bin-averaged into 2.50 PAR<sub>r</sub> (<b>e</b>) and 2.50 PAR<sub>f</sub> (<b>f</b>).</p>
Full article ">Figure 8
<p>Seasonal variations in monthly PAR (<b>a</b>), T<sub>a</sub> (<b>b</b>), (<b>c</b>) vapor pressure deficit (VPD), P (<b>d</b>), (<b>e</b>) evaporative fraction (EF), CI (<b>f</b>), NDVI (<b>g</b>), GPP (<b>h</b>), and LUE (<b>i</b>) in 2006–2019 in the Chinese cork oak plantation.</p>
Full article ">Figure 9
<p>Correlation analysis among monthly biophysical factors and LUE in 2006–2019 in the Chinese cork oak plantation. * Significant at <span class="html-italic">p</span> &lt; 0.05; ** significant at <span class="html-italic">p</span> &lt; 0.01; *** significant at <span class="html-italic">p</span> &lt; 0.001.</p>
Full article ">Figure 10
<p>Variance inflation factors among monthly influencing factors (<b>a</b>), partial correlation coefficients between monthly biophysical factors and LUE (<b>b</b>), stepwise regression among monthly biophysical factors and LUE (<b>c</b>) in 2006–2019 in the Chinese cork oak plantation. *** significant at <span class="html-italic">p</span> &lt; 0.001.</p>
Full article ">Figure 11
<p>Correlation analysis (<b>a</b>) and path analysis (<b>b</b>) among annual biophysical factors and LUE in 2006–2019 in the Chinese cork oak plantation. * Significant at <span class="html-italic">p</span> &lt; 0.05; ** significant at <span class="html-italic">p</span> &lt; 0.01; *** significant at <span class="html-italic">p</span> &lt; 0.001.</p>
Full article ">
23 pages, 8179 KiB  
Article
Study on Extraordinarily High-Speed Cutting Mechanics and Its Application to Dry Cutting of Aluminum Alloys with Non-Coated Carbide Tools
by Jun Eto, Takehiro Hayasaka, Eiji Shamoto and Liangji Xu
J. Manuf. Mater. Process. 2024, 8(5), 198; https://doi.org/10.3390/jmmp8050198 - 13 Sep 2024
Viewed by 405
Abstract
The friction/adhesion between the tool and chip is generally large in metal cutting, and it causes many problems such as high cutting energy/rough surface finish. To suppress this, cutting fluid and tool coating are used in practice, but they are high in energy/cost [...] Read more.
The friction/adhesion between the tool and chip is generally large in metal cutting, and it causes many problems such as high cutting energy/rough surface finish. To suppress this, cutting fluid and tool coating are used in practice, but they are high in energy/cost and environmentally unfriendly. Therefore, this paper investigates the extraordinarily high-speed cutting (EHS cutting) mechanics of mainly soft and highly heat-conductive materials and proposes their application to solve the friction/adhesion problem in an environmentally friendly manner. In order to clarify the EHS cutting mechanics, a simple analytical model is constructed and experiments are conducted with measurement of the cutting temperature and forces. As a result, the following points are clarified/found: (1) heat softening at the secondary plastic deformation zone rather than the primary plastic deformation zone, (2) friction coefficient drop to 0.170 in EHS cutting, and (3) gradually increasing trend of cutting temperature in EHS cutting. Finally, EHS cutting is applied to dry cutting of aluminum alloys with a non-coated carbide tool and compared to conventional wet cutting with a DLC-coated carbide tool, and it is shown that a coating/coolant can be omitted in this region to achieve environmentally friendly cutting. Full article
Show Figures

Figure 1

Figure 1
<p>Schematic of cutting process and cutting temperature distribution [<a href="#B2-jmmp-08-00198" class="html-bibr">2</a>].</p>
Full article ">Figure 2
<p>Influence of cutting speed on cutting temperature in dry cutting with Al<sub>2</sub>O<sub>3</sub> ceramic tool [<a href="#B19-jmmp-08-00198" class="html-bibr">19</a>].</p>
Full article ">Figure 3
<p>Relation between specific cutting energy <math display="inline"><semantics> <mrow> <mi>k</mi> <mi>s</mi> </mrow> </semantics></math> and specific melt-beginning energy <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>q</mi> </mrow> <mrow> <mi>c</mi> </mrow> </msub> </mrow> </semantics></math>.</p>
Full article ">Figure 4
<p>Tensile property of aluminum alloys against temperature [<a href="#B25-jmmp-08-00198" class="html-bibr">25</a>,<a href="#B26-jmmp-08-00198" class="html-bibr">26</a>].</p>
Full article ">Figure 5
<p>Schematic illustration of calibration system of thermoelectromotive force.</p>
Full article ">Figure 6
<p>Result of TEMF calibration curve between 7050-T7451 alloy and cemented carbide.</p>
Full article ">Figure 7
<p>Photographs of experimental setup for milling-like turning experiments.</p>
Full article ">Figure 8
<p>Schematic of experimental setup.</p>
Full article ">Figure 9
<p>Example of thermoelectromotive force and cutting forces in one spindle revolution at cutting speed <span class="html-italic">V<sub>c</sub></span> = 5184 m/min, feed per revolution <span class="html-italic">f</span> = 0.15 mm/rev, and dry cutting with non-coated carbide tool.</p>
Full article ">Figure 10
<p>Effects of cutting speed <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>V</mi> </mrow> <mrow> <mi>c</mi> </mrow> </msub> </mrow> </semantics></math> on temperatures, cutting forces, average friction coefficient, average shear stress at shear plane, and specific cutting energy at feed per revolution <span class="html-italic">f</span> = 0.15 mm/rev, dry environment, and non-coated tool.</p>
Full article ">Figure 11
<p>Comparison of ultimate tensile strength against temperature and average friction coefficient <math display="inline"><semantics> <mrow> <mi>μ</mi> </mrow> </semantics></math> against cutting temperature in dry environment and with non-coated tool.</p>
Full article ">Figure 12
<p>Effects of feed per revolution <math display="inline"><semantics> <mrow> <mi>f</mi> </mrow> </semantics></math> on cutting temperature and cutting forces at cutting speed <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>V</mi> </mrow> <mrow> <mi>c</mi> </mrow> </msub> </mrow> </semantics></math> = 1465 m/min, dry environment, and non-coated tool.</p>
Full article ">Figure 13
<p>Effects of rake angle <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">α</mi> </mrow> </semantics></math> and cutting speed <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>V</mi> </mrow> <mrow> <mi>c</mi> </mrow> </msub> </mrow> </semantics></math> on cutting temperature, cutting forces, and average friction coefficient at feed per revolution <math display="inline"><semantics> <mrow> <mi>f</mi> <mo>=</mo> <mn>0.15</mn> </mrow> </semantics></math> mm/rev, dry environment, non-coated tool.</p>
Full article ">Figure 14
<p>Photograph of conventional cutting process with external cutting fluid.</p>
Full article ">Figure 15
<p>Comparison of cutting forces, average friction coefficient, and cutting ratio between dry cutting with non-coated tool and wet cutting with DLC-coated tool.</p>
Full article ">Figure 16
<p>Photographs of (<b>a</b>) machined surfaces, (<b>b</b>) chips, and (<b>c</b>) rake faces after cutting at cutting speed <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>V</mi> </mrow> <mrow> <mi>c</mi> </mrow> </msub> <mo>=</mo> </mrow> </semantics></math> 5184 m/min.</p>
Full article ">
20 pages, 4724 KiB  
Article
The Dynamic Prediction Method for Aircraft Cabin Temperatures Based on Flight Test Data
by He Li, Jianjun Zhang, Liangxu Cai, Minwei Li, Yun Fu and Yujun Hao
Aerospace 2024, 11(9), 755; https://doi.org/10.3390/aerospace11090755 - 13 Sep 2024
Viewed by 303
Abstract
For advanced aircraft, the temperature environment inside the cabin is very severe due to the high flight speed and the compact concentration of the electronic equipment in the cabin. Accurately predicting the temperature environment induced inside the cabin during the flight of the [...] Read more.
For advanced aircraft, the temperature environment inside the cabin is very severe due to the high flight speed and the compact concentration of the electronic equipment in the cabin. Accurately predicting the temperature environment induced inside the cabin during the flight of the aircraft can determine the temperature environment requirements of the onboard equipment inside the cabin and provide an accurate input for the thermal design optimization and test verification of the equipment. The temperature environment of the whole aircraft is divided into zones by the cluster analysis method; the heat transfer mechanism of the aircraft cabin is analyzed for the target area; and the influence of internal and external factors on the thermal environment is considered to establish the temperature environment prediction model of the target cabin. The coefficients of the equations in the model are parameterized to extract the long-term stable terms and trend change terms; with the help of the measured data of the flight state, the model coefficients are determined by a stepwise regression method; and the temperature value inside the aircraft cabin is the output by inputting parameters such as flight altitude, flight speed, and external temperature. The model validation results show that the established temperature environment prediction model can accurately predict the change curve of the cabin temperature during the flight of the aircraft, and the model has a good follow-up performance, which reduces the prediction error caused by the temperature hysteresis effect. For an aircraft, the estimated error is 2.8 °C at a confidence level of 95%. Engineering cases show that the application of this method can increase the thermal design requirements of the airborne equipment by 15 °C, increase the low-temperature test conditions by 17 °C, and avoid the problems caused by an insufficient design and over-testing. This method can accurately predict the internal temperature distribution of the cabin during the flight state of the aircraft, help designers determine the thermal design requirements of the airborne equipment, modify the thermal design and temperature test profile, and improve the environmental worth of the equipment. Full article
(This article belongs to the Special Issue Aerospace Human–Machine and Environmental Control Engineering)
Show Figures

Figure 1

Figure 1
<p>Schematic diagram of the structure of the study area (Zone 1).</p>
Full article ">Figure 2
<p>Flight profile A.</p>
Full article ">Figure 3
<p>Prediction results of internal temperature for cabin in flight profile A.</p>
Full article ">Figure 4
<p>Prediction error of internal temperature for cabin in flight profile A.</p>
Full article ">Figure 5
<p>Prediction results of internal temperature for cabin in flight profile B.</p>
Full article ">Figure 6
<p>Prediction error of internal temperature for cabin in flight profile B.</p>
Full article ">Figure 7
<p>Prediction results of internal temperature for cabin in flight profile C.</p>
Full article ">Figure 8
<p>Prediction error of internal temperature for cabin in flight profile C.</p>
Full article ">Figure 9
<p>Prediction results of internal temperature for cabin in flight profile D.</p>
Full article ">Figure 10
<p>Prediction error of internal temperature for cabin in flight profile D.</p>
Full article ">Figure 11
<p>Histogram of prediction model error distribution.</p>
Full article ">Figure 12
<p>The severity of high temperature environmental conditions for a specific aircraft (schematic diagram).</p>
Full article ">Figure 13
<p>The comparison of reliability test profiles.</p>
Full article ">
21 pages, 39126 KiB  
Article
Impacts of Climate Change on the Potential Distribution of Three Cytospora Species in Xinjiang, China
by Quansheng Li, Shanshan Cao, Lei Wang, Ruixia Hou and Wei Sun
Forests 2024, 15(9), 1617; https://doi.org/10.3390/f15091617 - 13 Sep 2024
Viewed by 445
Abstract
Xinjiang is an important forest and fruit production area in China, and Cytospora canker, caused by the genus Cytospora Ehrenb., has caused serious losses to forestry production in Xinjiang. In this study, we constructed ensemble models based on Biomod2 to assess the potential [...] Read more.
Xinjiang is an important forest and fruit production area in China, and Cytospora canker, caused by the genus Cytospora Ehrenb., has caused serious losses to forestry production in Xinjiang. In this study, we constructed ensemble models based on Biomod2 to assess the potential geographical distribution of Cytospora chrysosperma, C. nivea, and C. mali in Xinjiang, China and their changes under different climate change scenarios, using species occurrence data and four types of environmental variables: bioclimatic, topographic, NDVI, and soil. The model performance assessment metrics (AUC and TSS) indicated that the ensemble models are highly reliable. The results showed that NDVI had the most important effect on the distribution of all three species, but there were differences in the response patterns, and bioclimatic factors such as temperature and precipitation also significantly affected the distribution of the three species. C. chrysosperma showed the broadest ecological adaptation and the greatest potential for expansion. C. nivea and C. mali also showed expansion trends, but to a lesser extent. The overlapping geographical distribution areas of the three species increased over time and with an intensification of the climate scenarios, especially under the high-emission SSP585 scenario. The centroids of the geographical distribution for all three species generally shifted towards higher latitude regions in the northeast, reflecting their response to climate warming. C. chrysosperma may become a more prevalent forest health threat in the future, and an increase in the overlapping geographical distribution areas of the three species may lead to an increased risk of multiple infections. These findings provide an important basis for understanding and predicting the distribution and spread of the genus Cytospora in Xinjiang and are important for the development of effective forest disease prevention and control strategies. Full article
(This article belongs to the Section Forest Ecology and Management)
Show Figures

Figure 1

Figure 1
<p>Distribution records of <span class="html-italic">Cytospora chrysosperma</span>, <span class="html-italic">C. nivea</span> and <span class="html-italic">C. mali</span> in Xinjiang, China.</p>
Full article ">Figure 2
<p>Evaluate the predictive performance of each model for the three <span class="html-italic">Cytospora</span> species using the area under the receiver operating characteristic curve (AUC) and true skill statistic (TSS).</p>
Full article ">Figure 3
<p>Response curves of the top 4 most important environmental variables for the three <span class="html-italic">Cytospora</span> species.</p>
Full article ">Figure 4
<p>Current geographical distributions of <span class="html-italic">Cytospora chrysosperma</span>, <span class="html-italic">C. nivea</span>, and <span class="html-italic">C. mali</span> predicted using ensemble models. Potential geographical distributions of (<b>A</b>) <span class="html-italic">C. chrysosperma</span>, (<b>B</b>) <span class="html-italic">C. nivea</span>, and (<b>C</b>) <span class="html-italic">C. mali</span>. (<b>D</b>) Overlapping geographical distribution areas of the three <span class="html-italic">Cytospora</span> species.</p>
Full article ">Figure 5
<p>Potential geographical distribution of <span class="html-italic">Cytospora chrysosperma</span> under different climate scenarios predicted using ensemble model.</p>
Full article ">Figure 6
<p>Potential geographical distribution of <span class="html-italic">Cytospora nivea</span> under different climate scenarios predicted using ensemble model.</p>
Full article ">Figure 7
<p>Potential geographical distribution of <span class="html-italic">Cytospora mali</span> under different climate scenarios predicted using ensemble model.</p>
Full article ">Figure 8
<p>Overlapping geographical distribution areas of <span class="html-italic">Cytospora chrysosperma</span>, <span class="html-italic">C. nivea</span>, and <span class="html-italic">C. mali</span> under different climate scenarios in the future.</p>
Full article ">Figure 9
<p>Centroid shifts of potential suitable area for <span class="html-italic">Cytospora chrysosperma</span>, <span class="html-italic">C. nivea</span>, and <span class="html-italic">C. mali</span> under different climate scenarios. (<b>A</b>) Location of the centroids of potential suitable areas for the three <span class="html-italic">Cytospora</span> species in the study area. (<b>B</b>) Centroid shifts of potential suitable area for <span class="html-italic">C. chrysosperma</span>. (<b>C</b>) Centroid shifts of potential suitable area for <span class="html-italic">C. nivea</span>. (<b>D</b>) Centroid shifts of potential suitable area for <span class="html-italic">C. mali</span>.</p>
Full article ">
15 pages, 11451 KiB  
Article
Impact of Climate Change on Distribution of Suitable Niches for Black Locust (Robinia pseudoacacia L.) Plantation in China
by Shanchao Zhao, Hesong Wang and Yang Liu
Forests 2024, 15(9), 1616; https://doi.org/10.3390/f15091616 - 13 Sep 2024
Viewed by 225
Abstract
Black locust (Robinia pseudoacacia L.), one of the major afforestation species adopted in vegetation restoration, is notable for its rapid root growth and drought resistance. It plays a vital role in improving the natural environment and soil fertility, contributing significantly to soil [...] Read more.
Black locust (Robinia pseudoacacia L.), one of the major afforestation species adopted in vegetation restoration, is notable for its rapid root growth and drought resistance. It plays a vital role in improving the natural environment and soil fertility, contributing significantly to soil and water conservation and biodiversity protection. However, compared with natural forests, due to the low diversity, simple structure and poor stability, planted forests including Robinia pseudoacacia L. are more sensitive to the changing climate, especially in the aspects of growth trend and adaptive range. Studying the ecological characteristics and geographical boundaries of Robinia pseudoacacia L. is therefore important to explore the adaptation of suitable niches to climate change. Here, based on 162 effective distribution records in China and 22 environmental variables, the potential distribution of suitable niches for Robinia pseudoacacia L. plantations in past, present and future climates was simulated by using a Maximum Entropy (MaxEnt) model. The results showed that the accuracy of the MaxEnt model was excellent and the area under the curve (AUC) value reached 0.937. Key environmental factors constraining the distribution and suitable intervals were identified, and the geographical distribution and area changes of Robinia pseudoacacia L. plantations in future climate scenarios were also predicted. The results showed that the current suitable niches for Robinia pseudoacacia L. plantations covered 9.2 × 105 km2, mainly distributed in the Loess Plateau, Huai River Basin, Sichuan Basin, eastern part of the Yunnan–Guizhou Plateau, Shandong Peninsula, and Liaodong Peninsula. The main environmental variables constraining the distribution included the mean temperature of the driest quarter, precipitation of driest the quarter, temperature seasonality and altitude. Among them, the temperature of the driest quarter was the most important factor. Over the past 90 years, the suitable niches in the Sichuan Basin and Yunnan–Guizhou Plateau have not changed significantly, while the suitable niches north of the Qinling Mountains have expanded northward by 2° and the eastern area of Liaoning Province has expanded northward by 1.2°. In future climate scenarios, the potential suitable niches for Robinia pseudoacacia L. are expected to expand significantly in both the periods 2041–2060 and 2061–2080, with a notable increase in highly suitable niches, widely distributed in southern China. A warning was issued for the native vegetation in the above-mentioned areas. This work will be beneficial for developing reasonable afforestation strategies and understanding the adaptability of planted forests to climate change. Full article
(This article belongs to the Section Forest Meteorology and Climate Change)
Show Figures

Figure 1

Figure 1
<p>The distribution records of <span class="html-italic">Robinia pseudoacacia</span> L. and the approximate range of the Loess Plateau and the Yunnan–Guizhou Plateau.</p>
Full article ">Figure 2
<p>Receiver operating characteristic (ROC) curve of the MaxEnt model used in this study.</p>
Full article ">Figure 3
<p>Response curves of <span class="html-italic">Robinia pseudoacacia</span> L. plantations to the main environmental factors.</p>
Full article ">Figure 4
<p>Potential distribution areas of <span class="html-italic">Robinia pseudoacacia</span> L. plantations in the current climate of China.</p>
Full article ">Figure 5
<p>Potential distribution areas of <span class="html-italic">Robinia pseudoacacia</span> L. plantations for the period from 1931 to 1960 in China.</p>
Full article ">Figure 6
<p>Potential distribution areas of <span class="html-italic">Robinia pseudoacacia</span> L. plantations in the period from 1961 to 1990 in China.</p>
Full article ">Figure 7
<p>Potential distribution areas of <span class="html-italic">Robinia pseudoacacia</span> L. plantations in future climate change scenarios (2041–2060).</p>
Full article ">Figure 7 Cont.
<p>Potential distribution areas of <span class="html-italic">Robinia pseudoacacia</span> L. plantations in future climate change scenarios (2041–2060).</p>
Full article ">Figure 8
<p>Potential distribution areas of <span class="html-italic">Robinia pseudoacacia</span> L. plantations in future climate change scenarios (2061–2080).</p>
Full article ">
14 pages, 5812 KiB  
Article
Partially Bio-Based and Biodegradable Poly(Propylene Terephthalate-Co-Adipate) Copolymers: Synthesis, Thermal Properties, and Enzymatic Degradation Behavior
by Ping Song, Mingjun Li, Haonan Wang, Yi Cheng and Zhiyong Wei
Polymers 2024, 16(18), 2588; https://doi.org/10.3390/polym16182588 - 13 Sep 2024
Viewed by 243
Abstract
A series of partially bio-based and biodegradable poly(propylene terephthalate-co-adipate) (PPTA) random copolymers with different components were prepared by the melt polycondensation of petro-based adipic acid and terephthalic acid with bio-based 1,3-propanediol. The microstructure, crystallization behavior, thermal properties, and enzymatic degradation properties were further [...] Read more.
A series of partially bio-based and biodegradable poly(propylene terephthalate-co-adipate) (PPTA) random copolymers with different components were prepared by the melt polycondensation of petro-based adipic acid and terephthalic acid with bio-based 1,3-propanediol. The microstructure, crystallization behavior, thermal properties, and enzymatic degradation properties were further investigated. The thermal decomposition kinetics was deeply analyzed using Friedman’s method, with the thermal degradation activation energy ranging from 297.8 to 302.1 kJ/mol. The crystallinity and wettability of the copolymers decreased with the increase in the content of the third unit, but they were lower than those of the homopolymer. The thermal degradation activation energy E, carbon residue, and reaction level n all showed a decreasing trend. Meanwhile, the initial thermal decomposition temperature (Td) was higher than 350 °C, which can meet the requirements for processing and use. The PPTA copolymer material still showed excellent thermal stability. Adding PA units could regulate the crystallinity, wettability, and degradation rate of PPTA copolymers. The composition of PPTA copolymers in different degradation cycles was characterized by 1H NMR analysis. Further, the copolymers’ surface morphology during the process of enzymatic degradation also was observed by scanning electron microscopy (SEM). The copolymers’ enzymatic degradation accorded with the surface degradation mechanism. The copolymers showed significant degradation behavior within 30 days, and the rate increased with increasing PA content when the PA content exceeded 45.36%. Full article
(This article belongs to the Special Issue Synthesis and Application of Degradable Polymers)
Show Figures

Figure 1

Figure 1
<p>Synthetic routine of PPTA copolymers.</p>
Full article ">Figure 2
<p>(<b>a</b>) <sup>1</sup>H NMR and (<b>b</b>) GPC spectra of PPTA copolymers.</p>
Full article ">Figure 3
<p>(<b>a</b>) Cooling curves and (<b>b</b>) the second heating curves for PPTA copolymers.</p>
Full article ">Figure 4
<p>The relative crystallinity of (<b>a</b>) PPTA-20 and (<b>b</b>) PPTA-40 changes with time at different isothermal crystallization temperatures. Avrami analysis by plotting <span class="html-italic">ln</span>(−<span class="html-italic">ln</span>(l − <span class="html-italic">X</span><sub>t</sub>)) vs. ln<span class="html-italic">t</span> of (<b>c</b>) PPTA-20 and (<b>d</b>) PPTA-40 at various <span class="html-italic">T</span><sub>c</sub> values.</p>
Full article ">Figure 5
<p>(<b>a</b>) Thermogravimetric analysis (TGA), (<b>b</b>) derivative thermogravimetry (DTG), (<b>c</b>) ln(dα/dt) vs. 10<sup>4</sup>/T curves, and (<b>d</b>) <span class="html-italic">ln</span>(1 − α) vs. 10<sup>4</sup>/T curves of PPTA with different compositions.</p>
Full article ">Figure 6
<p>Contact angle photographs of (<b>a</b>) PPT, (<b>b</b>) PPTA-20, (<b>c</b>) PPTA-40, (<b>d</b>) PPTA-60, (<b>e</b>) PPTA-80, and (<b>f</b>) PPA. (<b>g</b>) Diagram of contact angle changing with PA content. (<b>h</b>) Curves of weightlessness of PPTA with different compositions over time.</p>
Full article ">Figure 7
<p>SEM diagrams of PPTA surface under different times of enzyme degradation.</p>
Full article ">
35 pages, 11086 KiB  
Article
Research on the Correlation between Mechanical Seal Face Vibration and Stationary Ring Dynamic Behavior Characteristics
by Yunfeng Song, Hua Li, Wang Xiao, Shuangxi Li and Qingfeng Wang
Lubricants 2024, 12(9), 316; https://doi.org/10.3390/lubricants12090316 - 12 Sep 2024
Viewed by 241
Abstract
To address the lack of reliable measurement methods for identifying wear mechanisms and predicting the state of mechanical seal tribo-parts, this study proposes a method for characterizing tribological behavior based on measuring face vibration acceleration. It aims to uncover the source mechanism of [...] Read more.
To address the lack of reliable measurement methods for identifying wear mechanisms and predicting the state of mechanical seal tribo-parts, this study proposes a method for characterizing tribological behavior based on measuring face vibration acceleration. It aims to uncover the source mechanism of mechanical seal face vibration acceleration influenced by tribology and dynamic behavior. This research delves into the dynamic behavior characteristics and vibration acceleration of the mechanical seal stationary ring. We explored the variation pattern of face vibration acceleration root mean square (RMS) with rotation speed, sealing medium pressure, and face surface roughness. The results indicate that under constant medium pressure, an increase in rotation speed leads to a decrease in acceleration RMS and an increase in face temperature. Similarly, under constant rotation speed, an increase in medium pressure results in nonlinear changes in acceleration RMS, forming an “M” shape, along with an increase in face temperature. Furthermore, under conditions of constant medium pressure and rotation speed, an increase in the surface roughness of the rotating ring face corresponds to an increase in acceleration RMS and face temperature. Upon starting the mechanical seal, both acceleration RMS and temperature initially increase before decreasing, a trend consistent with the Stribeck curve. Full article
(This article belongs to the Special Issue Wear Mechanism Identification and State Prediction of Tribo-Parts)
Show Figures

Figure 1

Figure 1
<p>Mechanical seal structure.</p>
Full article ">Figure 2
<p>Stribeck curve.</p>
Full article ">Figure 3
<p>The face control body in Cartesian coordinates.</p>
Full article ">Figure 4
<p>The Greenwood and Williamson model for contact.</p>
Full article ">Figure 5
<p>Tribological behavior test rig of mechanical seal.</p>
Full article ">Figure 6
<p>Tribological behavior test rig of mechanical seal assembly schematic diagram.</p>
Full article ">Figure 7
<p>Tribological behavior test rig of mechanical seal assembly physical diagram.</p>
Full article ">Figure 8
<p>Installation diagram of thermocouple temperature sensor.</p>
Full article ">Figure 9
<p>Mechanical seal with sensor.</p>
Full article ">Figure 10
<p>Lubrication and cooling system.</p>
Full article ">Figure 11
<p>Rotating ring 1# exterior diagram.</p>
Full article ">Figure 12
<p>Rotating ring 2# exterior diagram.</p>
Full article ">Figure 13
<p>Rotating ring 3# exterior diagram.</p>
Full article ">Figure 14
<p>Rotating ring 4# exterior diagram.</p>
Full article ">Figure 15
<p>Rotating ring 1# surface diagram.</p>
Full article ">Figure 16
<p>Rotating ring 2# surface diagram.</p>
Full article ">Figure 17
<p>Rotating ring 3# surface diagram.</p>
Full article ">Figure 18
<p>Rotating ring 4# surface diagram.</p>
Full article ">Figure 19
<p>Radial acceleration RMS start–stop phase change curve.</p>
Full article ">Figure 20
<p>Tangential acceleration RMS start–stop phase change curve.</p>
Full article ">Figure 21
<p>Axial acceleration RMS start–stop phase change curve.</p>
Full article ">Figure 22
<p>Change curve of face temperature in start–stop stage.</p>
Full article ">Figure 23
<p>Relationship between radial RMS and rotational speed.</p>
Full article ">Figure 24
<p>Relationship between tangential RMS and rotational speed.</p>
Full article ">Figure 25
<p>Relationship between axial RMS and rotational speed.</p>
Full article ">Figure 26
<p>Relationship between temperature and rotational speed.</p>
Full article ">Figure 27
<p>Curve of acceleration RMS changing with medium pressure.</p>
Full article ">Figure 28
<p>Curve of face temperature changing with time.</p>
Full article ">Figure 29
<p>The relationship between the RMS of radial acceleration and surface roughness.</p>
Full article ">Figure 30
<p>The relationship between the RMS of tangential acceleration and surface roughness.</p>
Full article ">Figure 31
<p>The relationship between the RMS of axial acceleration and surface roughness.</p>
Full article ">Figure 32
<p>The relationship between face temperature and surface roughness.</p>
Full article ">
15 pages, 710 KiB  
Article
Trends and Drivers of Flood Occurrence in Germany: A Time Series Analysis of Temperature, Precipitation, and River Discharge
by Mohannad Alobid, Fatih Chellai and István Szűcs
Water 2024, 16(18), 2589; https://doi.org/10.3390/w16182589 - 12 Sep 2024
Viewed by 705
Abstract
Floods in Germany have become increasingly frequent and severe over recent decades, with notable events in 2002, 2013, and 2021. This study examines the trends and drivers of flood occurrences in Germany from 1990 to 2024, focusing on the influence of climate-change-related variables, [...] Read more.
Floods in Germany have become increasingly frequent and severe over recent decades, with notable events in 2002, 2013, and 2021. This study examines the trends and drivers of flood occurrences in Germany from 1990 to 2024, focusing on the influence of climate-change-related variables, such as temperature, precipitation, and river discharge. Using a comprehensive time series analysis, including Auto-Regressive Integrated Moving Average (ARIMA) and Artificial Neural Network (ANN) models and correlation and regression analyses, we identify significant correlations between these climatic variables and flood events. Our findings indicate that rising temperatures (with a mean of 8.46 °C and a maximum of 9 °C) and increased precipitation (averaging 862.26 mm annually)are strongly associated with higher river discharge (mean 214.6 m3/s) and more frequent floods (mean 197.94 events per year). The ANN model outperformed the ARIMA model in flood forecasting, showing lower error metrics (e.g., RMSE of 10.86 vs. 18.83). The analysis underscores the critical impact of climate change on flood risks, highlighting the necessity of adaptive flood-management strategies that incorporate the latest climatic and socio-economic data. This research contributes to the understanding of flood dynamics in Germany and provides valuable insights into future flood risks. Combining flood management with groundwater recharge could effectively lower flood risks and enhance water resources’ mitigation and management. Full article
Show Figures

Figure 1

Figure 1
<p>Time series plot of flood events, rainfall, river discharge, and temperature in Germany from 1990 to 2024.</p>
Full article ">Figure 2
<p>Forecast from NNAR (3,2) of flood events from2025 to 2034.</p>
Full article ">Figure 3
<p>Forecast from ARIMA (0,1,1) of flood events (m<sup>3</sup>/s) from 2025 to 2034.</p>
Full article ">
Back to TopTop