Nothing Special   »   [go: up one dir, main page]

You seem to have javascript disabled. Please note that many of the page functionalities won't work as expected without javascript enabled.
 
 
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

Article Types

Countries / Regions

remove_circle_outline
remove_circle_outline
remove_circle_outline
remove_circle_outline

Search Results (317)

Search Parameters:
Keywords = large-scale irrigation

Order results
Result details
Results per page
Select all
Export citation of selected articles as:
10 pages, 1898 KiB  
Commentary
Challenging the Chemistry of Climate Change
by Bruce Peachey and Nobuo Maeda
Chemistry 2024, 6(6), 1439-1448; https://doi.org/10.3390/chemistry6060086 (registering DOI) - 16 Nov 2024
Viewed by 156
Abstract
As talk grows about billions or even trillions of dollars being directed toward potential “Net Zero” activities, it is imperative that the chemistry inherent in or driving those actions make scientific sense. The challenge is to close the mass and energy balances to [...] Read more.
As talk grows about billions or even trillions of dollars being directed toward potential “Net Zero” activities, it is imperative that the chemistry inherent in or driving those actions make scientific sense. The challenge is to close the mass and energy balances to the carbon and oxygen cycles in the Earth’s atmosphere and oceans. Several areas of climate science have been identified that chemists can investigate through methods that do not require a supercomputer or a climate model for investigation, most notably the following: (1) The carbon cycle, which still needs to be balanced, as many known streams, such as carbon to landfills, carbon in human-enhanced sewage and land runoff streams, and carbon stored in homes and other material, do not seem to have been accounted for in carbon balances used by the IPCC. (2) Ocean chemistry and balances are required to explain the causes of regional and local-scale salinity, pH, and anoxic conditions vs. global changes. For example, local anoxic conditions are known to be impacted by changes in nutrient discharges to oceans, while large-scale human diversions of fresh water streams for irrigation, power, and industrial cooling must have regional impacts on oceanic salinity and pH. (3) Carbon Capture and Storage (CCS) schemes, if adopted on the large scales being proposed (100s to 1000s of Gt net injection by 2100), should impact the composition of the atmosphere by reducing free oxygen, adding more water from combustion, and displacing saline water from subsurface aquifers. Data indicate that atmospheric oxygen is currently dropping at about twice the rate of CO2 concentrations increasing, which is consistent with combustion chemistry with 1.5 to 2 molecules of oxygen being converted through combustion to 1 molecule of CO2 and 1 to 2 molecules of H2O, with reverse reactions occurring as a result of oxygenic photosynthesis by increased plant growth. The CCS schemes will sabotage these reverse reactions of oxygenic photosynthesis by permanently sequestering the oxygen atoms in each CO2 molecule. Full article
(This article belongs to the Section Physical Chemistry and Chemical Physics)
23 pages, 12566 KiB  
Article
Multispectral Images for Drought Stress Evaluation of Arabica Coffee Genotypes Under Different Irrigation Regimes
by Patrícia Carvalho da Silva, Walter Quadros Ribeiro Junior, Maria Lucrecia Gerosa Ramos, Maurício Ferreira Lopes, Charles Cardoso Santana, Raphael Augusto das Chagas Noqueli Casari, Lemerson de Oliveira Brasileiro, Adriano Delly Veiga, Omar Cruz Rocha, Juaci Vitória Malaquias, Nara Oliveira Silva Souza and Henrique Llacer Roig
Sensors 2024, 24(22), 7271; https://doi.org/10.3390/s24227271 (registering DOI) - 14 Nov 2024
Viewed by 330
Abstract
The advancement of digital agriculture combined with computational tools and Unmanned Aerial Vehicles (UAVs) has opened the way to large-scale data collection for the calculation of vegetation indices (VIs). These vegetation indexes (VIs) are useful for agricultural monitoring, as they highlight the inherent [...] Read more.
The advancement of digital agriculture combined with computational tools and Unmanned Aerial Vehicles (UAVs) has opened the way to large-scale data collection for the calculation of vegetation indices (VIs). These vegetation indexes (VIs) are useful for agricultural monitoring, as they highlight the inherent characteristics of vegetation and optimize the spatial and temporal evaluation of different crops. The experiment tested three coffee genotypes (Catuaí 62, E237 and Iapar 59) under five water regimes: (1) FI 100 (year-round irrigation with 100% replacement of evapotranspiration), (2) FI 50 (year-round irrigation with 50% evapotranspiration replacement), (3) WD 100 (no irrigation from June to September (dry season) and, thereafter, 100% evapotranspiration replacement), (4) WD 50 (no irrigation from June to September (water stress) and, thereafter, 50% evapotranspiration replacement) and (5) rainfed (no irrigation during the year). The irrigated treatments were watered with irrigation and precipitation. Most indices were highest in response to full irrigation (FI 100). The values of the NDVI ranged from 0.87 to 0.58 and the SAVI from 0.65 to 0.38, and the values of these indices were lowest for genotype E237 in the rainfed areas. The indices NDVI, OSAVI, MCARI, NDRE and GDVI were positively correlated very strongly with photosynthesis (A) and strongly with transpiration (E) of the coffee trees. On the other hand, temperature-based indices, such as canopy temperature and the TCARI index correlated negatively with A, E and stomatal conductance (gs). Under full irrigation, the tested genotypes did not differ between the years of evaluation. Overall, the index values of Iapar 59 exceeded those of the other genotypes. The use of VIs to evaluate coffee tree performance under different water managements proved efficient in discriminating the best genotypes and optimal water conditions for each genotype. Given the economic importance of coffee as a crop and its susceptibility to extreme events such as drought, this study provides insights that facilitate the optimization of productivity and resilience of plantations under variable climatic conditions. Full article
(This article belongs to the Section Environmental Sensing)
Show Figures

Figure 1

Figure 1
<p>Location and arrangement of treatments and genotypes in the study area at Embrapa Cerrados in Brasília, DF, in the Cerrado biome.</p>
Full article ">Figure 2
<p>Long-term maximum and minimum average climate data over the past 46 years (1974–2020) in the area.</p>
Full article ">Figure 3
<p>Vegetation indices (<b>A</b>) NDVI, (<b>B</b>) SAVI, (<b>C</b>) NDRE, (<b>D</b>) TCARI, (<b>E</b>) MCARI, (<b>F</b>) GNDVI, (<b>G</b>) MTCI and (<b>H</b>) GDVI, in 2019, for three coffee genotypes (Catuaí 62, E237 and Iapar 59) under five water regimes (FI 100%, FI 50%, WS 100%, WS 50% and Rainfed) during water stress in drought treatments in 2019. Means followed by the same capital letters compare water regimes for each coffee genotype, and lowercase letters compare coffee genotypes within each water regime.</p>
Full article ">Figure 4
<p>Vegetation indices (<b>A</b>) NDVI, (<b>B</b>) SAVI, (<b>C</b>) NDRE, (<b>D</b>) TCARI, (<b>E</b>) MCARI, (<b>F</b>) GNDVI, (<b>G</b>) MTCI and (<b>H</b>) GDVI, in 2020, for three coffee genotypes (Catuaí 62, E237 and Iapar 59) under five water regimes (FI 100%, FI 50%, WS 100%, WS 50% and Rainfed) during water stress in drought treatments in 2019. Means followed by the same capital letters compare water regimes for each coffee genotype, and lowercase letters compare coffee genotypes within each water regime.</p>
Full article ">Figure 5
<p>Vegetation indices NDVI, OSAVI, MCARI, TCARI, NDRE, GNDVI, GDVI and MTCI evaluated for three coffee genotypes (Catuaí 62, E237 and Iapar 59) in response to five water regimes (from left to right, rainfed; WD (water stress) 1, 50%; WD2 50%; FI (full irrigation) in 2019.</p>
Full article ">Figure 6
<p>Vegetation indices NDVI, OSAVI, MCARI, TCARI, NDRE, GNDVI, GDVI and MTCI evaluated for three coffee genotypes (Catuaí 62, E237 and Iapar 59) in response to five water regimes (from left to right, rainfed; WD (water stress) 1, 50%; WD2 50%; FI (full irrigation) in 2020.</p>
Full article ">Figure 7
<p>Correlogram of Pearson’s correlation between vegetation indices and leaf gas exchange in 2019. A: photosynthesis, gs: stomatal conductance, E: transpiration and T: canopy temperature °C. Values close to 1 indicate a strong positive correlation, while values close to −1 represent a strong negative correlation. Values close to 0 suggest an absence of significant linear relationship. In addition, the size of the source observed in the corelogram was used to graphically represent the magnitude of the correlation, allowing a clear visualization of the strength of the associations. Stronger correlations (positive or negative) were highlighted with larger font size and bold, while weaker correlations were presented with smaller and unbold fonts. The statistical significance of the correlations was evaluated at a probability level: * 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 8
<p>Correlogram of Pearson’s correlation between vegetation indices and leaf gas exchange in 2020. A: photosynthesis, gs: stomatal conductance, E: transpiration and T: canopy temperature °C. Values close to 1 indicate a strong positive correlation, while values close to −1 represent a strong negative correlation. Values close to 0 suggest an absence of significant linear relationship. In addition, the size of the source observed in the correlogram was used to graphically represent the magnitude of the correlation, allowing a clear visualization of the strength of the associations. Stronger correlations (positive or negative) were highlighted with larger font size and bold, while weaker correlations were presented with smaller and unbold fonts. The statistical significance of the correlations was evaluated at a probability level: * 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 9
<p>Exploratory analysis of the principal components for vegetation indices and coffee tree physiology and productivity in response to different water regimes and of different genotypes in the growing seasons of 2019 (<b>A</b>,<b>B</b>) and 2020 (<b>C</b>,<b>D</b>). The vectors of the variables projected onto the graphs indicate the magnitude and direction of their contribution to the separation between groups. The length of the vectors reflects the intensity of their influence on the principal components, while their orientation highlights the multivariate differences between the evaluated conditions. The ellipses drawn around the experimental groups represent the intragroup dispersion based on the covariance of the data. The center of each ellipse corresponds to the centroid of the respective group, representing the average position of the observations. The orientation and size of the ellipses indicate the internal variability of each group: more compact ellipses suggest greater homogeneity within the observations. In contrast, larger ellipses indicate greater heterogeneity, possibly associated with the different conditions imposed by the treatments. The distribution of the vectors and the separation of the ellipses demonstrate that the analyzed variables play a significant role in differentiating between the groups of cultivars and irrigation regimes, providing insights into the physiological and spectral responses under each evaluated scenario.</p>
Full article ">
22 pages, 6887 KiB  
Article
Detecting Water Stress in Winter Wheat Based on Multifeature Fusion from UAV Remote Sensing and Stacking Ensemble Learning Method
by He Zhao, Jingjing Wang, Jiali Guo, Xin Hui, Yunling Wang, Dongyu Cai and Haijun Yan
Remote Sens. 2024, 16(21), 4100; https://doi.org/10.3390/rs16214100 - 2 Nov 2024
Viewed by 560
Abstract
The integration of remote sensing technology and machine learning algorithms represents a new research direction for the rapid and large-scale detection of water stress in modern agricultural crops. However, in solving practical agricultural problems, single machine learning algorithms cannot fully explore the potential [...] Read more.
The integration of remote sensing technology and machine learning algorithms represents a new research direction for the rapid and large-scale detection of water stress in modern agricultural crops. However, in solving practical agricultural problems, single machine learning algorithms cannot fully explore the potential information within the data, lacking stability and accuracy. Stacking ensemble learning (SEL) can combine the advantages of multiple single machine learning algorithms to construct more stable predictive models. In this study, threshold values of stomatal conductance (gs) under different soil water stress indices (SWSIs) were proposed to assist managers in irrigation scheduling. In the present study, six irrigation treatments were established for winter wheat to simulate various soil moisture supply conditions. During the critical growth stages, gs was measured and the SWSI was calculated. A spectral camera mounted on an unmanned aerial vehicle (UAV) captured reflectance images in five bands, from which vegetation indices and texture information were extracted. The results indicated that gs at different growth stages of winter wheat was sensitive to soil moisture supply conditions. The correlation between the gs value and SWSI value was high (R2 > 0.79). Therefore, the gs value threshold can reflect the current soil water stress level. Compared with individual machine learning models, the SEL model exhibited higher prediction accuracy, with R2 increasing by 6.67–17.14%. Using a reserved test set, the SEL model demonstrated excellent performance in various evaluation metrics across different growth stages (R2: 0.69–0.87, RMSE: 0.04–0.08 mol m−2 s−1; NRMSE: 12.3–23.6%, MAE: 0.03–0.06 mol m−2 s−1) and exhibited excellent stability and accuracy. This research can play a significant role in achieving large-scale monitoring of crop growth status through UAV, enabling the real-time capture of winter wheat water deficit changes, and providing technical support for precision irrigation. Full article
Show Figures

Figure 1

Figure 1
<p>Location of the study area and the experimental treatments. Note: W0–W5 represent different irrigation levels.</p>
Full article ">Figure 2
<p>The UAV platform and multispectral camera.</p>
Full article ">Figure 3
<p>Image texture type.</p>
Full article ">Figure 4
<p>Stacking ensemble learning model.</p>
Full article ">Figure 5
<p>Stomatal conductance (g<sub>s</sub> mol m<sup>−2</sup> s<sup>−1</sup>) of wheat at the revival, jointing, heading, flowering, and filling stages in 2022 and 2023. Note: Different lowercase letters indicate significant differences in stomatal conductance at a <span class="html-italic">p</span> value of &lt;0.05.</p>
Full article ">Figure 6
<p>Soil water stress index of wheat at the revival, jointing, heading, flowering, and filling stages in 2022 and 2023.</p>
Full article ">Figure 7
<p>Fitting relationship between soil water stress index and g<sub>s</sub> in 2022 and 2023. Note: (<b>a</b>) Revival stage. (<b>b</b>) Jointing stage. (<b>c</b>) Heading stage. (<b>d</b>) Flowering stage. (<b>e</b>) Filling stage.</p>
Full article ">Figure 8
<p>Pearson correlation coefficient between stomatal conductance (g<sub>s</sub>) and vegetation indices (VIs). Note: Revival represents the wheat revival stage; Jointing represents the wheat jointing stage; Heading represents the wheat heading stage; Flowering represents the wheat flowering stage; Filling represents the wheat filling stage; Whole represents the whole growth stage of the wheat.</p>
Full article ">Figure 9
<p>Pearson correlation coefficient of image texture and stomatal conductance (g<sub>s</sub>) at each growth stage in 2022 and 2023. Note: (<b>a</b>) Revival stage. (<b>b</b>) Jointing stage. (<b>c</b>) Heading stage. (<b>d</b>) Flowering stage. (<b>e</b>) Filling stage. (<b>f</b>) Whole wheat growth stage.</p>
Full article ">Figure 10
<p>Estimation of g<sub>s</sub> accuracy based on RF, SVM, XGBoost, and SEL models. Note: (<b>a</b>) Revival stage. (<b>b</b>) Jointing stage. (<b>c</b>) Heading stage. (<b>d</b>) Flowering stage. (<b>e</b>) Filling stage. (<b>f</b>) Whole wheat growth stage.</p>
Full article ">
17 pages, 1796 KiB  
Article
Maize-Straw Biochar Enhances Soil Properties and Grain Yield of Foxtail Millet in a Newly Reclaimed Land
by Xuyan Hou, Wei He, Yi Zhang, Ningning Zhang, Jiakun Yan and Yinglong Chen
Agronomy 2024, 14(11), 2465; https://doi.org/10.3390/agronomy14112465 - 22 Oct 2024
Viewed by 611
Abstract
Large-scale land reclamation has become common in northwestern China; however, low soil fertility and poor soil water-holding capacity limit agricultural production on these reclaimed lands, requiring increased fertilizer and irrigation inputs. Biochar, produced from agricultural waste, has shown potential in improving soil quality [...] Read more.
Large-scale land reclamation has become common in northwestern China; however, low soil fertility and poor soil water-holding capacity limit agricultural production on these reclaimed lands, requiring increased fertilizer and irrigation inputs. Biochar, produced from agricultural waste, has shown potential in improving soil quality and water-holding capacity. In this two-year field study (2021 and 2022), we investigated the effects of biochar produced from maize straw on soil properties and grain yield of foxtail millet grown on newly reclaimed land. Three biochar treatments (3000, 4500, and 6000 kg ha−1) were compared to a control (CK) with no biochar application. Biochar application resulted in increased soil organic matter, total phosphorus, total nitrogen, soil enzyme activity, and soil organic acid content. It also significantly decreased soil pH and bulk density. Compared with the CK, biochar increased available nitrogen from 29.7% to 108% in 2021 and 37.0% to 88.4% in 2022. Similarly, biochar increased available phosphorus from 64.7% to 143% in 2021 and 41.9% to 96.5% in 2022. Grain yields ranged from 3092 to 4753 kg ha−1. Biochar treatments increased grain yield compared to the CK, ranging from 12.2% to 24.6% in 2021 and 27.1% to 53.7% in 2022. Correlation analysis revealed that soil pH was negatively related to soil oxalic acid content, phosphorus content, and sucrase activity. Available nitrogen and phosphorus contents were negatively related to soil bulk density and positively related to catalase activity. Soil water content was negatively correlated with soil bulk density and positively correlated with organic matter. In conclusion, biochar improved the rhizosphere soil pH and the effectiveness of soil fertility in the newly reclaimed soil, resulting in an enhanced grain yield of foxtail millet. Full article
(This article belongs to the Section Agricultural Biosystem and Biological Engineering)
Show Figures

Figure 1

Figure 1
<p>Monthly and long-term averages of precipitation and temperature at the experimental site.</p>
Full article ">Figure 2
<p>Effect of biochar application on soil bulk density (<b>A</b>), pH (<b>B</b>), and soil water content (<b>C</b>). ** indicates significant differences between year (Y), treatment (T), and interaction between year and treatment (Y × T) at <span class="html-italic">p</span> &lt; 0.01. “ns” showed there was no significance. Data are shown as mean ± SD. Different letters indicate significant differences in the same year (<span class="html-italic">p</span> &lt; 0.05).</p>
Full article ">Figure 3
<p>Effect of biochar application on soil organic matter (<b>A</b>), total phosphorus (<b>B</b>), total nitrogen (<b>C</b>), available phosphorus (<b>D</b>) and available nitrogen (<b>E</b>). The legend of the histogram is shown in figure (<b>F</b>). * and ** indicate significant differences between year (Y), treatment (T), and interaction between year and treatment (Y × T) at <span class="html-italic">p</span> &lt; 0.05 and <span class="html-italic">p</span> &lt; 0.01, respectively. “ns” showed there was no significance. Data are shown as mean ± SD. Different letters indicate significant differences in the same year (<span class="html-italic">p</span> &lt; 0.05).</p>
Full article ">Figure 4
<p>Effect of biochar application on soil catalase (<b>A</b>), urease (<b>B</b>), and sucrase (<b>C</b>). * and ** indicate significant differences between year (Y), treatment (T), and interaction between year and treatment (Y × T) at <span class="html-italic">p</span> &lt; 0.05 and <span class="html-italic">p</span> &lt; 0.01, respectively. “ns” showed there was no significance. Data are shown as mean ± SD. Different letters indicate significant differences in the same year (<span class="html-italic">p</span> &lt; 0.05).</p>
Full article ">Figure 5
<p>Effect of biochar application on soil oxalic acid (<b>A</b>), acetic acid (<b>B</b>), and citric acid (<b>C</b>). ** indicates significant differences between year (Y), treatment (T), and interaction between year and treatment (Y × T) at <span class="html-italic">p</span> &lt; 0.01, respectively. “ns” showed there was no significance. Data are shown as mean ± SD. Different letters indicate significant differences in the same year (<span class="html-italic">p</span> &lt; 0.05).</p>
Full article ">Figure 6
<p>A possible mechanism underlying the function of biochar in improving soil quality, plant growth, and grain yield. Biochar improved soil physical properties by decreasing soil bulk density, and due to its sorption, it could increase soil water content (SWC) and minerals in terms of increasing available nitrogen and phosphorus (AN and AP). On the other side, biochar could interact with root by stimulating the secretion of organic acids (oxalic and acetic acid), which might function in improving soil pH. In addition, biochar increased soil organic matter, which could play important roles in improving soil enzymatic activity.</p>
Full article ">
11 pages, 257 KiB  
Communication
Achieving Responsible Reclaimed Water Reuse for Vineyard Irrigation: Lessons from Napa Valley, California and Valle de Guadalupe, Baja California
by Marc Beutel, Leopoldo Mendoza-Espinosa, Clara Medina, Jorge Andrés Morandé, Thomas C. Harmon and Josué Medellín-Azuara
Water 2024, 16(19), 2817; https://doi.org/10.3390/w16192817 - 4 Oct 2024
Viewed by 672
Abstract
Here we report on preliminary efforts to assess the potential to use reclaimed water from municipal wastewater treatment plants for irrigation of vineyards in Napa Valley, California, USA and Valle de Guadalupe, Baja California, Mexico. Vineyards in Napa Valley use a range of [...] Read more.
Here we report on preliminary efforts to assess the potential to use reclaimed water from municipal wastewater treatment plants for irrigation of vineyards in Napa Valley, California, USA and Valle de Guadalupe, Baja California, Mexico. Vineyards in Napa Valley use a range of source waters including 70 L/s of reclaimed water during the summertime irrigation season. Reclaimed water is secondary effluent that undergoes filtration and disinfection and meets stringent total coliform (<240 MPN/100 mL) and turbidity (10 NTU) requirements. Vineyards in Valle de Guadalupe currently use regional groundwater supplies of marginal quality, and there is interest in expanding source waters to include reclaimed water from nearby Ensenada or the more remote Tijuana. Valle de Guadalupe is drier than Napa Valley and has ongoing salinity management challenges, making the region more sensitive to using reclaimed water for irrigation. Several social and economic factors facilitated the implementation of reclaimed water reuse in Napa Valley for vineyard irrigation, including (1) formation of an assessment district by interested growers to help finance pipeline construction, (2) a long-term reclaimed water vineyard irrigation study by agricultural experts that confirmed the reclaimed water was safe, and (3) a well-defined and relatively low unit cost of reclaimed water. In Valle de Guadalupe, the federal government has approved a project to transport 1000 L/s of reclaimed water over 100 km from Tijuana to Valle de Guadalupe. Questions remain including financing of the project, reclaimed water quality, grower interest in using reclaimed water, and community concerns for such a large-scale program. In considering reclaimed water reuse in vineyards, a key issue is implementation of long-term studies showing that reclaimed water is effectively treated and is safe for irrigation, especially from the standpoint of salt content. In addition, the cost of reclaimed water needs to be comparable with traditional water sources. Finally, in addition to assessing economic constraints, social constraints and water user concerns should be comprehensively addressed in the context of a regional integrated water management framework. Full article
(This article belongs to the Special Issue Safe Application of Reclaimed Water in Agriculture)
15 pages, 4826 KiB  
Article
Assessing Evapotranspiration Changes in Response to Cropland Expansion in Tropical Climates
by Leonardo Laipelt, Julia Brusso Rossi, Bruno Comini de Andrade, Morris Scherer-Warren and Anderson Ruhoff
Remote Sens. 2024, 16(18), 3404; https://doi.org/10.3390/rs16183404 - 13 Sep 2024
Viewed by 687
Abstract
The expansion of cropland in tropical regions has significantly accelerated in recent decades, triggering an escalation in water demand and changing the total water loss to the atmosphere (evapotranspiration). Additionally, the increase in areas dedicated to agriculture in tropical climates coincides with an [...] Read more.
The expansion of cropland in tropical regions has significantly accelerated in recent decades, triggering an escalation in water demand and changing the total water loss to the atmosphere (evapotranspiration). Additionally, the increase in areas dedicated to agriculture in tropical climates coincides with an increased frequency of drought events, leading to a series of conflicts among water users. However, detailed studies on the impacts of changes in water use due to agriculture expansion, including irrigation, are still lacking. Furthermore, the higher presence of clouds in tropical environments poses challenges for the availability of high-resolution data for vegetation monitoring via satellite images. This study aims to analyze 37 years of agricultural expansion using the Landsat collection and a satellite-based model (geeSEBAL) to assess changes in evapotranspiration resulting from cropland expansion in tropical climates, focusing on the São Marcos River Basin in Brazil. It also used a methodology for estimating daily evapotranspiration on days without satellite images. The results showed a 34% increase in evapotranspiration from rainfed areas, mainly driven by soybean cultivation. In addition, irrigated areas increased their water use, despite not significantly changing water use at the basin scale. Conversely, natural vegetation areas decreased their evapotranspiration rates by 22%, suggesting possible further implications with advancing changes in land use and land cover. Thus, this study underscores the importance of using satellite-based evapotranspiration estimates to enhance our understanding of water use across different land use types and scales, thereby improving water management strategies on a large scale. Full article
Show Figures

Figure 1

Figure 1
<p>São Marcos River Basin: location in Brazil (<b>a</b>), climate zones according to Köppen–Geiger classification and irrigation pivots (<b>b</b>), and Normalized Difference Vegetation Index (NDVI) values computed using average composition of Landsat 8 for 2021 (<b>c</b>).</p>
Full article ">Figure 2
<p>Daily average of <span class="html-italic">ET</span> illustrated as boxplot for each land cover and use (<b>a</b>) for Landsat scenes between 1986 and 2022. We also illustrated the seasonal monthly average of <span class="html-italic">ET</span> (<b>b</b>), and trends of annual average <span class="html-italic">ET</span> for different land types, with natural vegetation (forest and savanna) demonstrating positive trends over the years, as well as irrigated areas (<b>c</b>).</p>
Full article ">Figure 3
<p>Changes in the <span class="html-italic">ET</span> spatial patterns for the São Marcos River Basin from 1986 to 2022 (<b>a</b>). The contribution of the water usage for each land cover and use between 1986 and 2022 is shown in (<b>b</b>), whereas (<b>c</b>) illustrates changes in land cover and use.</p>
Full article ">Figure 4
<p>Annual composition ET (mm day<sup>−1</sup>) in the São Marcus River Basin between 1986 (<b>a</b>) and 2021 (<b>b</b>). Highlighted plots showed the expressive number of pivot irrigation systems over the basin for specific locations.</p>
Full article ">Figure 5
<p>Monthly <span class="html-italic">ET</span> in the São Marcus River basin was analyzed for each month of one water year (2019 and 2020). During the dry season (May to September), precipitation is limited and radiation availability is high, being a water-limited environment. Consequently, lower <span class="html-italic">ET</span> values are observed during the dry season, while the wet season increases <span class="html-italic">ET</span> rates due to higher precipitation availability.</p>
Full article ">Figure 6
<p>Seasonal differences in daily <span class="html-italic">ET</span> for irrigated and rainfed croplands in the São Marcus River Basin (<b>a</b>), and the difference between both estimations (<b>b</b>). We used a simplified method to fill the gap between Landsat scenes by interpolating <span class="html-italic">EF</span> over time and multiplying with the respective reference <span class="html-italic">ET</span>.</p>
Full article ">
18 pages, 5133 KiB  
Article
Comprehensive Assessment of Climate Change Impacts on River Water Availability for Irrigation, Wheat Crop Area Coverage, and Irrigation Canal Hydraulic Capacity of Large-Scale Irrigation Scheme in Nepal
by Santosh Kaini, Matthew Tom Harrison, Ted Gardner and Ashok K. Sharma
Water 2024, 16(18), 2595; https://doi.org/10.3390/w16182595 - 13 Sep 2024
Viewed by 1509
Abstract
While atmospheric warming intensifies the global water cycle, regionalised effects of climate change on water loss, irrigation supply, and food security are highly variable. Here, we elucidate the impacts of the climate crisis on irrigation water availability and cropping area in Nepal’s largest [...] Read more.
While atmospheric warming intensifies the global water cycle, regionalised effects of climate change on water loss, irrigation supply, and food security are highly variable. Here, we elucidate the impacts of the climate crisis on irrigation water availability and cropping area in Nepal’s largest irrigation scheme, the Sunsari Morang Irrigation Scheme (SMIS), by accounting for the hydraulic capacity of existing canal systems, and potential changes realised under future climates. To capture variability implicit in climate change projections, we invoke multiple Representative Concentration Pathways (RCPs; 4.5 and 8.5) across three time horizons (2016–2045, 2036–2065, and 2071–2100). We reveal that although climate change increases water availability to agriculture from December through March, the designed discharge of 60 m3/s would not be available in February-March for both RCPs under all three time horizons. Weed growth, silt deposition, and poor maintenance have reduced the current canal capacity from the design capacity of 60 m3/s to 53 m3/s up to 10.7 km from the canal intake (representing a 12% reduction in the discharge capacity of the canal). Canal flow is further reduced to 35 m3/s at 13.8 km from canal intake, representing a 27% reduction in flow capacity relative to the original design standards. Based on climate projections, and assuming ceteris paribus irrigation infrastructure, total wheat cropping area could increase by 12–19%, 23–27%, and 12–35% by 2016–2045, 2036–2065, and 2071–2100, respectively, due to increased water availability borne by the changing climate. The case for further investment in irrigation infrastructure via water diversion, or installation of efficient pumps at irrigation canal intakes is compelling. Such investment would catalyse a step-change in the agricultural economy that is urgently needed to sustain the Nepalese economy, and thus evoke beneficial cascading implications for global food security. Full article
(This article belongs to the Special Issue Model-Based Irrigation Management)
Show Figures

Figure 1

Figure 1
<p>(<b>a</b>) Koshi River basin, Sunsari Morang Irrigation Scheme, and administrative boundary of Nepal, (<b>b</b>) Koshi River network and Sunsari Morang Irrigation Intake, (<b>c</b>) Sunsari Morang Irrigation Intake and Irrigation Canal Network. Discharge measurement chainages from 5.2 km to 25.4 km are shown in numbers (1–6) in (<b>c</b>).</p>
Full article ">Figure 2
<p>Overview of the study, including irrigation channels, flow discharge, and climate information modelling.</p>
Full article ">Figure 3
<p>Current meter (manual recorder) used for discharge measurement in the main irrigation canal.</p>
Full article ">Figure 4
<p>Observed and simulated discharge, velocity, and water depth for the (<b>a</b>) calibration and (<b>b</b>) validation periods. Locations of the Chainage 5.2 km, 11.8 km, 13 km, 15 km, 22.5 km, and 25.3 km in the main canal are shown in <a href="#water-16-02595-f001" class="html-fig">Figure 1</a>c.</p>
Full article ">Figure 5
<p>Stage–discharge relationship for the Koshi River at the irrigation canal intake, based on data available from 1996 to 2012. Crest level of the intake structure is 107 m above mean sea level.</p>
Full article ">Figure 6
<p>Headwork intake structure (12 rectangular orifices) of the Sunsari Morang Irrigation Scheme in the Koshi River (<b>a</b>) during the monsoon season, and (<b>b</b>) during the dry season (arrow shows the direction of river flow).</p>
Full article ">Figure 7
<p>Average monthly water available over the crests of the canal intake, which is then available for irrigation during the dry season (data averaged over 1982–2010).</p>
Full article ">Figure 8
<p>Projected average monthly minimum flows into the canal intake along with their standard deviation of the mean for different climate change scenarios (RCPSs) and future time periods, with reference (base) period flow for comparison.</p>
Full article ">
4 pages, 1033 KiB  
Proceeding Paper
Nature-Based Solutions in Cities—A View from a Water Supply Perspective
by Martin Oberascher, Aun Dastgir, Carolina Kinzel and Robert Sitzenfrei
Eng. Proc. 2024, 69(1), 113; https://doi.org/10.3390/engproc2024069113 - 10 Sep 2024
Viewed by 250
Abstract
Nature-Based Solutions (NBSs) are decentralised and planted system elements with multiple benefits, requiring sufficient irrigation during dry weather periods to ensure plant health. In this work, the effects of the large-scale implementation of NBSs in the city centre of Klagenfurt from a water [...] Read more.
Nature-Based Solutions (NBSs) are decentralised and planted system elements with multiple benefits, requiring sufficient irrigation during dry weather periods to ensure plant health. In this work, the effects of the large-scale implementation of NBSs in the city centre of Klagenfurt from a water supply perspective are investigated, combining hydraulic analysis with water resource availability. As the large-scale implementation of NBSs in public squares shows, a coordinated NBS implementation strategy is required to ensure compatibility with the city’s water resources and infrastructure. This also emphasises the importance of alternative water sources for sustainable operations. Full article
Show Figures

Figure 1

Figure 1
<p>(<b>a</b>) Available drinking water for irrigation based on the results of Oberascher, Maussner, Truppe, Eggeling, and Sitzenfrei [<a href="#B5-engproc-69-00113" class="html-bibr">5</a>] and (<b>b</b>) pressure decrease in the water distribution network using only drinking water for irrigation for an implementation degree of 20%.</p>
Full article ">
23 pages, 3342 KiB  
Article
Assessment of Resilience Due to Adoption of Technologies in Frequently Drought-Prone Regions of India
by J. V. N. S. Prasad, N. Loganandhan, P. R. Ramesh, C. A. Rama Rao, B. M. K. Raju, K. V. Rao, A. V. M. Subba Rao, R. Rejani, Sumanta Kundu, Prabhat Kumar Pankaj, C. M. Pradeep, B. V. S. Kiran, Jakku Prasanna, D. V. S. Reddy, V. Venkatasubramanian, Ch. Srinivasarao, V. K. Singh, Rajbir Singh and S. K. Chaudhari
Sustainability 2024, 16(17), 7339; https://doi.org/10.3390/su16177339 - 26 Aug 2024
Viewed by 922
Abstract
Climate change and variability are increasingly affecting agriculture and livelihoods in developing countries, with India being particularly vulnerable. Drought is one of the major climatic constraints impacting large parts of the world. We examined the effects of drought on crop productivity, evaluated the [...] Read more.
Climate change and variability are increasingly affecting agriculture and livelihoods in developing countries, with India being particularly vulnerable. Drought is one of the major climatic constraints impacting large parts of the world. We examined the effects of drought on crop productivity, evaluated the effectiveness of technologies in mitigating these impacts and quantified the resilience gained due to technology adoption. Resilience score and resilience gain are the two indicators used to quantify resilience. The study utilized data gathered from two villages situated in Karnataka, southern India, which have implemented the National Innovations in Climate Resilient Agriculture (NICRA) program, along with data from one control village. Drought has significantly impacted the yields, and the extent of reduction ranged from 23 to 62% compared to the normal year. Adoption of climate-resilient technologies, including improved varieties, water management and livestock practices proved beneficial in increasing yield and income during drought years. The resilience score of various technologies ranged from 71 to 122%, indicating that the technologies had realized an increase in yields in the drought year in comparison to the normal year. The extent of resilience gain ranged from 7 to 68%, indicating that the adoption of technologies contributed to the yield advantage over the farmers’ practice during drought. Water harvesting and critical irrigation have the highest resilience scores and gains, and in situ moisture conservation practices such as trench cum bunding (TCB) have comparable resilience scores and gains. The diversification of enterprises at the farm has a higher resilience score and gain. There is a need to identify climate-resilient technologies that can achieve higher resilience, as the solutions are context-specific. Further, promising technologies need to be scaled by adopting multiple approaches and by creating an enabling environment so as to increase resilience in agricultural systems. Full article
Show Figures

Figure 1

Figure 1
<p>Location of the study area.</p>
Full article ">Figure 2
<p>(<b>a</b>) Effect of adoption of short-duration/drought-escaping varieties of finger millet, groundnut, pigeon pea and maize on yields compared to farmers’ practice during drought and normal rainfall in Tumkur (Karnataka). [FMV_D: finger millet (ML-365)_drought year; FMV_N: finger millet (ML-365)_normal year; NNICRA_D: non-NICRA farmers’ drought year; NNICRA_N: non-NICRA farmers’ normal year; GNV_D: groundnut (ICGV-91114)_drought year; GNV_N: groundnut (ICGV-91114)_normal year; PPV_D: pigeon pea (BRG-2)_drought year; PPV_N: pigeon pea (BRG-2)_normal year; MV_D: maize hybrid drought year; MV_N: maize hybrid normal year]. (<b>b</b>) Effect of adoption of short-duration/drought-escaping varieties of finger millet, groundnut, pigeon pea and maize with supplemental irrigation on yields compared to local varieties without irrigation during drought and normal rainfall in Tumkur. [FMI_D: finger millet (ML-365) with irrigation_drought year; FMI_N: finger millet (ML-365) with irrigation_normal year; FMT_D: finger millet (ML-365) with trench cum bunding_drought year; FMT_N: finger millet (ML-365) with trench cum bunding_normal year; NNICRA_D: non-NICRA farmers_drought year; NNICRA_N: non-NICRA farmers_normal year; GNI_D: groundnut (ICGV-91114) with irrigation_drought year; GNV_N: groundnut (ICGV-91114) with irrigation_normal year; GNT_D: groundnut (ICGV-91114) with trench cum bunding_drought year; GNT_N: groundnut (ICGV-91114) with trench cum bunding_normal year; PPI_D: pigeon pea (BRG-2) with irrigation_drought year; PPI_N: pigeon pea (BRG-2) with irrigation_normal year; PPT_D: pigeon pea (BRG-2) with trench cum bunding_drought year; PPT_N: pigeon pea (BRG-2) with trench cum bunding_normal year; MI_D: maize hybrid with irrigation_drought year; MI_N: maize hybrid with irrigation_normal year; MT_D: maize hybrid with trench cum bunding_drought year; MT_N: maize hybrid with trench cum bunding_normal year].</p>
Full article ">Figure 3
<p>(<b>a</b>) Impact of adoption of short-duration/drought-escaping varieties of finger millet, groundnut, pigeon pea and maize on net returns (INR/ha; USD 1 = INR 80) compared to local varieties during drought and normal rainfall in Tumkur. [FMV_D: finger millet (ML-365)_drought year; FMV_N: finger millet (ML-365)_normal year; NNICRA_D: non-NICRA farmers’_drought year; NNICRA_N: non-NICRA farmers’_normal year; GNV_D: groundnut (ICGV-91114)_drought year; GNV_N: groundnut (ICGV-91114)_normal year; PPV_D: pigeon pea (BRG-2)_drought year; PPV_N: pigeon pea (BRG-2)_normal year; NNICRA_D: MV_D: maize hybrid_drought year; MV_N: maize hybrid_normal year]. (<b>b</b>) Impact of adoption of short-duration/drought-escaping varieties of finger millet, groundnut, pigeon pea and maize with supplemental irrigation on net returns (INR/ha; USD 1 = INR 80) compared to local varieties without irrigation during drought and normal rainfall in Tumkur. [FMI_D: finger millet (ML-365) with irrigation_drought year; FMI_N: finger millet (ML-365) with irrigation_normal year; FMT_D: finger millet (ML-365) with trench cum bunding_drought year; FMT_N: finger millet (ML-365) with trench cum bunding_normal year; NNICRA_D: non-NICRA farmers’_drought year; NNICRA_N: non-NICRA farmers’_normal year; GNI_D: groundnut (ICGV-91114) with irrigation_drought year; GNV_N: groundnut (ICGV-91114) with irrigation_normal year; GNT_D: groundnut (ICGV-91114) with trench cum bunding_drought year; GNT_N: groundnut (ICGV-91114) with trench cum bunding_normal year; PPI_D: pigeon pea (BRG-2) with irrigation_drought year; PPI_N: pigeon pea (BRG-2) with irrigation_normal year; PPT_D: pigeon pea (BRG-2) with trench cum bunding_drought year; PPT_N: pigeon pea (BRG-2) with trench cum bunding_normal year; MI_D: maize hybrid with irrigation_drought year; MI_N: maize hybrid with irrigation_normal year; MT_D: maize hybrid with trench cum bunding_drought year; MT_N: maize hybrid with trench cum bunding_normal year].</p>
Full article ">Figure 4
<p>(<b>a</b>). Impact of feeding of green fodder on milk yield in indigenous cows, crossbred cows and she-buffalo compared to farmers’ practice during drought and normal rainfall in Tumkur. [GFI_D: green fodder (indigenous cow) drought year; GFI_N: green fodder (indigenous cow)_normal year; NNICRA_D: non-NICRA farmers’_drought year; NNICRA_N: non-NICRA farmers_normal year; GFC_D: green fodder (crossbred cow)_drought year; GFC_N: green fodder (crossbred cow)_normal year; GFB_D: green fodder (she-buffalo)_drought year; GFB_N: green fodder (she-buffalo)_normal year]. (<b>b</b>). Impact of feeding green fodder on net returns (INR/ha; USD 1 = INR 80) in indigenous cows, crossbred cows, she-buffalo, goat and sheep compared to farmers’ practice during drought and normal situation in Tumkur. [GFI_D: green fodder (indigenous cow)_drought year; GFI_N: green fodder (indigenous cow)_normal year; NNICRA_D: non-NICRA farmers’_drought year; NNICRA_N: non-NICRA farmers_normal year; GFC_D: green fodder (crossbred cow)_drought year; GFC_N: green fodder (crossbred cow)_normal year; GFB_D: green fodder (she-buffalo)_drought year; GFB_N: green fodder (she-buffalo)_normal year].</p>
Full article ">Figure 5
<p>Resilience in yields due to adoption of short-duration/drought-escaping varieties and crop varieties with irrigation during drought in Tumkur district, India.</p>
Full article ">Figure 6
<p>(<b>a</b>) Resilience in milk yields due to adoption of improved fodder cultivars during drought in Tumkur district, India. (<b>b</b>) Resilience in income due to adoption of improved fodder cultivars during drought in Tumkur district, India.</p>
Full article ">Figure 7
<p>Farming system resilience through multiple interventions during drought in Tumkur district, India.</p>
Full article ">
15 pages, 2028 KiB  
Article
Effect of CO2 Elevation on Tomato Gas Exchange, Root Morphology and Water Use Efficiency under Two N-Fertigation Levels
by Manyi Zhang, Wentong Zhao, Chunshuo Liu, Changtong Xu, Guiyu Wei, Bingjing Cui, Jingxiang Hou, Heng Wan, Yiting Chen, Jiarui Zhang and Zhenhua Wei
Plants 2024, 13(17), 2373; https://doi.org/10.3390/plants13172373 - 26 Aug 2024
Viewed by 539
Abstract
Atmospheric elevated CO2 concentration (e[CO2]) decreases plant nitrogen (N) concentration while increasing water use efficiency (WUE), fertigation increases crop nutrition and WUE in crop; yet the interactive effects of e[CO2] coupled with two N-fertigation levels [...] Read more.
Atmospheric elevated CO2 concentration (e[CO2]) decreases plant nitrogen (N) concentration while increasing water use efficiency (WUE), fertigation increases crop nutrition and WUE in crop; yet the interactive effects of e[CO2] coupled with two N-fertigation levels during deficit irrigation on plant gas exchange, root morphology and WUE remain largely elusive. The objective of this study was to explore the physiological and growth responses of ambient [CO2] (a[CO2], 400 ppm) and e[CO2] (800 ppm) tomato plant exposed to two N-fertigation regimes: (1) full irrigation during N-fertigation (FIN); (2) deficit irrigation during N-fertigation (DIN) under two N fertilizer levels (reduced N (N1, 0.5 g pot−1) and adequate N (N2, 1.0 g pot−1). The results indicated that e[CO2] associated with DIN regime induced the lower N2 plant water use (7.28 L plant−1), maintained leaf water potential (−5.07 MPa) and hydraulic conductivity (0.49 mol m−2 s−1 MPa−1), greater tomato growth in terms of leaf area (7152.75 cm2), specific leaf area (223.61 cm2 g−1), stem and total dry matter (19.54 g and 55.48 g). Specific root length and specific root surface area were increased under N1 fertilization, and root tissue density was promoted in both e[CO2] and DIN environments. Moreover, a smaller and denser leaf stomata (4.96 µm2 and 5.37 mm−2) of N1 plant was obtained at e[CO2] integrated with DIN strategy. Meanwhile, this combination would simultaneously reduce stomatal conductance (0.13 mol m−2 s−1) and transpiration rate (1.91 mmol m−2 s−1), enhance leaf ABA concentration (133.05 ng g−1 FW), contributing to an improvement in WUE from stomatal to whole-plant scale under each N level, especially for applying N1 fertilization (125.95 µmol mol−1, 8.41 µmol mmol−1 and 7.15 g L−1). These findings provide valuable information to optimize water and nitrogen fertilizer management and improve plant water use efficiency, responding to the potential resource-limited and CO2-enriched scenario. Full article
Show Figures

Figure 1

Figure 1
<p>Leaf photosynthetic rate (P<sub>n</sub>) (<b>a</b>), stomatal conductance (g<sub>s</sub>) (<b>b</b>), transpiration rate (T<sub>r</sub>) (<b>c</b>), abscisic acid ([ABA]<sub>leaf</sub>) (<b>d</b>), intrinsic water use efficiency (WUE<sub>i</sub>) (<b>e</b>) and instantaneous water use efficiency (WUE<sub>n</sub>) (<b>f</b>) of tomato plants were affected by [CO<sub>2</sub>] concentration (<span class="html-italic">a</span>[CO<sub>2</sub>] and <span class="html-italic">e</span>[CO<sub>2</sub>]), N-fertigation regime (full irrigation during N-fertigation, FIN; deficit irrigation during N-fertigation, DIN) and N fertilizer level (N1 and N2). Error bars indicate standard error of the mean (n = 4). The results of ANOVA are shown in <a href="#plants-13-02373-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 2
<p>Leaf water potential (Ψ<sub>l</sub>) (<b>a</b>), leaf hydraulic conductivity (K<sub>l</sub>) (<b>b</b>), stomatal aperture (SA) (<b>c</b>) and stomatal density (SD) (<b>d</b>) of tomato plants were affected by [CO<sub>2</sub>] concentration (<span class="html-italic">a</span>[CO<sub>2</sub>] and <span class="html-italic">e</span>[CO<sub>2</sub>]), N-fertigation regime (full irrigation during N-fertigation, FIN; deficit irrigation during N-fertigation, DIN) and N fertilizer level (N1 and N2). Error bars indicate standard error of the mean (n = 4). The results of ANOVA are shown in <a href="#plants-13-02373-t001" class="html-table">Table 1</a>.</p>
Full article ">Figure 3
<p>Leaf area (LA) (<b>a</b>) and specific leaf area (SLA) (<b>b</b>) of tomato plants were affected by [CO<sub>2</sub>] concentration (<span class="html-italic">a</span>[CO<sub>2</sub>] and <span class="html-italic">e</span>[CO<sub>2</sub>]), N-fertigation regime (full irrigation during N-fertigation, FIN; deficit irrigation during N-fertigation, DIN) and N fertilizer level (N1 and N2). Error bars indicate standard error of the mean (n = 4). The results of ANOVA are shown in <a href="#plants-13-02373-t003" class="html-table">Table 3</a>. Different letters after the means indicate significant differences among treatments determined by Tukey’s multiple range test at <span class="html-italic">p</span> &lt; 0.05.</p>
Full article ">Figure 4
<p>Leaf dry matter (LDM) (<b>a</b>), stem dry matter (SDM) (<b>b</b>), root dry matter (RDM) (<b>c</b>), total dry matter (TDM) (<b>d</b>), plant water use (PWU) (<b>e</b>) and plant water use efficiency (WUEp) (<b>f</b>) of tomato plants were affected by [CO<sub>2</sub>] concentration (<span class="html-italic">a</span>[CO<sub>2</sub>] and <span class="html-italic">e</span>[CO<sub>2</sub>]), N-fertigation regime (full irrigation during N-fertigation, FIN; deficit irrigation during N-fertigation, DIN) and N fertilizer level (N1 and N2). Error bars indicate standard error of the mean (n = 4). The results of ANOVA are shown in <a href="#plants-13-02373-t003" class="html-table">Table 3</a>.</p>
Full article ">Figure 5
<p>PCA diagram of tomato plants was affected by [CO<sub>2</sub>] concentration (<span class="html-italic">a</span>[CO<sub>2</sub>] and <span class="html-italic">e</span>[CO<sub>2</sub>]), N-fertigation regime (full irrigation during N-fertigation, FIN; deficit irrigation during N-fertigation, DIN) and N fertilizer level (N1 and N2). Ultramarine vectors were related to P<sub>n</sub>, g<sub>s</sub>, T<sub>r</sub>, [ABA]<sub>leaf</sub>, WUE<sub>i</sub>, WUE<sub>n</sub>, Ψ<sub>l</sub>, K<sub>l</sub>, SA and SD; amaranth vectors were related to LA, SLA, LDM, SDM and RDM; aurantia vectors were related to RL, RD, RSA, RV, SRL, SRSA, RLD and RTD; red vectors were related to TDM, PWU and WUE<sub>p</sub>.</p>
Full article ">
12 pages, 3191 KiB  
Article
A New Approach to Vertical Plant Cultivation Maximises Crop Efficiency
by Mariusz Ptak, Sebastian Wasieńko and Piotr Makuła
Sustainability 2024, 16(16), 7189; https://doi.org/10.3390/su16167189 - 21 Aug 2024
Viewed by 1569
Abstract
This publication presents an innovative tower cultivation device designed to significantly increase vertical farming’s efficiency. The device divides the cultivation system into separate chambers. One division corresponds to the different growth phases of the plants, while another reflects the daily variation in conditions. [...] Read more.
This publication presents an innovative tower cultivation device designed to significantly increase vertical farming’s efficiency. The device divides the cultivation system into separate chambers. One division corresponds to the different growth phases of the plants, while another reflects the daily variation in conditions. Each chamber presents slightly different conditions and cultivation patterns from the others. For the early stages, crops are grown horizontally in trays; once they mature, they are transplanted into mobile cultivation towers. The closed circulation of ventilation and irrigation reduces water consumption by up to 95%. A unique separate day–night division optimises light, temperature, and humidity conditions, mimicking natural growth patterns. This approach not only saves water and energy but also improves cultivation in a three-dimensional space. The presented solution focuses on the often-overlooked aspects of cultivating in vertical farms and makes this method of growing much more cost-effective and feasible to implement on a large scale. Our comparative analysis with other vertical farming solutions is based on publicly available data and provides valuable insights, while acknowledging the potential limitations at play. Full article
Show Figures

Figure 1

Figure 1
<p>The vertical farming approach: advantages and disadvantages compared to traditional soil cultivation.</p>
Full article ">Figure 2
<p>The <b>upper row</b>: (<b>left</b>) an axonometric view of a system for tower plant cultivation; (<b>right</b>) a side view from the perspective of the “day” chamber. The <b>lower row</b>: a view from the “day” and “night” climate module with a focus on the towers and the separation device. 1—“day” climate module A1; 2—“night” climate module A2; 3—separation device; climatic zone divider; 4—suspension system; 5—tower system frame; 6—towers; 7—roller for roller shutters for climatic zone partitions; 8—exposure panel; 9—device sliding system for separating climatic zones; 10—tower cart; 11—pot; 12—mechanism for changing the driving track.</p>
Full article ">Figure 3
<p>Vertical farming with day–night chambers: (<b>a</b>) computer-aided design model, (<b>b</b>) the system during assembly—the towers (in white) are visible, and (<b>c</b>) the prototype module implemented in a grocery shop.</p>
Full article ">Figure 4
<p>Testing different types of plants in a module with variable climatic parameters—the plants are planted in vertical moveable towers.</p>
Full article ">Figure 5
<p>Cultivation process divided into operational zones of robot #1 and #2.</p>
Full article ">
15 pages, 11454 KiB  
Article
Accurate Characterization of Soil Moisture in Wheat Fields with an Improved Drought Index from Unmanned Aerial Vehicle Observations
by Minghan Cheng, Xintong Lu, Zhangxin Liu, Guanshuo Yang, Lili Zhang, Binqian Sun, Zhian Wang, Zhengxian Zhang, Ming Shang and Chengming Sun
Agronomy 2024, 14(8), 1783; https://doi.org/10.3390/agronomy14081783 - 14 Aug 2024
Viewed by 1027
Abstract
Soil moisture content is a crucial indicator for understanding the water requirements of crops. The effective monitoring of soil moisture content can provide support for irrigation decision-making and agricultural water management. Traditional ground-based measurement methods are time-consuming and labor-intensive, and point-scale monitoring cannot [...] Read more.
Soil moisture content is a crucial indicator for understanding the water requirements of crops. The effective monitoring of soil moisture content can provide support for irrigation decision-making and agricultural water management. Traditional ground-based measurement methods are time-consuming and labor-intensive, and point-scale monitoring cannot effectively represent the heterogeneity of soil moisture in the field. Unmanned aerial vehicle (UAV) remote sensing technology offers an efficient and convenient way to monitor soil moisture content in large fields, but airborne multispectral data are prone to spectral saturation effects, which can further affect the accuracy of monitoring soil moisture content. Therefore, we aim to construct effective drought indices for the accurate characterization of soil moisture content in winter wheat fields by utilizing unmanned aerial vehicles (UAVs) equipped with LiDAR, thermal infrared, and multispectral sensors. Initially, we estimated wheat plant height using airborne LiDAR sensors and improved traditional spectral indices in a structured manner based on crop height. Subsequently, we constructed the normalized land surface temperature–structured normalized difference vegetation index (NLST-SNDVI) space by combining the SNDVI with land surface temperature and calculated the improved Temperature–Vegetation Drought Index (iTVDI). The results are summarized as follows: (1) the structured spectral indices exhibit better resistance to spectral saturation, making the NLST-SNDVI space closer to expectations than the NLST-NDVI space, with higher fitting accuracy for wet and dry edges; (2) the iTVDI calculated based on the NLST-SNDVI space can effectively characterize soil moisture content, showing a significant correlation with measured surface soil moisture content; (3) the global Moran’s I calculated based on iTVDI deviations ranges between 0.18 and 0.30, all reaching significant levels, indicating that iTVDI has good spatial applicability. In conclusion, this study proved the effectiveness of the drought index based on a structured vegetation index, and the results can provide support for crop moisture monitoring and irrigation decision-making in the field. Full article
(This article belongs to the Special Issue Unmanned Farms in Smart Agriculture)
Show Figures

Figure 1

Figure 1
<p>Overview of the experimental area and the experimental field. Note: N1: no fertilization, N2: 150 kg/hm<sup>2</sup>, N3: 225 kg/hm<sup>2</sup>, and N4: 300 kg/hm<sup>2</sup>; D1: 1,500,000 plants/hm<sup>2</sup>, D2: 2,250,000 kg/hm<sup>2</sup>, and D3: 3,000,000 kg/hm<sup>2</sup>; V1: Yangmai 13, V2: Yangmai 20, and V3: Yangmai 28.</p>
Full article ">Figure 2
<p>UAV and sensors: (<b>a</b>) DJI M300RTK; (<b>b</b>) DJI M3M.</p>
Full article ">Figure 3
<p>The measured soil moisture content.</p>
Full article ">Figure 4
<p>Flowchart of extracting wheat plant height based on 3D point cloud data.</p>
Full article ">Figure 5
<p>Schematic diagram of spectral saturation effect and structuring of vegetation indices.</p>
Full article ">Figure 6
<p>Schematic diagram of the NLST-SNDVI space.</p>
Full article ">Figure 7
<p>The flowchart of the iTVDI establishment.</p>
Full article ">Figure 8
<p>Map of wheat height in different periods.</p>
Full article ">Figure 9
<p>NLST-NDVI/SNDVI space.</p>
Full article ">Figure 10
<p>The comparison of rSMC with (<b>a</b>) iTVDI and (<b>b</b>) TVDI. Note: * indicates the correlation reached significant level (<span class="html-italic">p</span> &gt; 0.05).</p>
Full article ">Figure 11
<p>The map of iTVDI.</p>
Full article ">Figure 12
<p>The map of iTVDI deviation in different periods.</p>
Full article ">Figure 13
<p>The scatter of NDVI and SNDVI. Note: * indicates the correlation reached significant level (<span class="html-italic">p</span> &gt; 0.05).</p>
Full article ">
47 pages, 26197 KiB  
Review
Review of Subsurface Dam Technology Based on Japan’s Experience in the Ryukyu Arc
by Imaizumi Masayuki
Water 2024, 16(16), 2282; https://doi.org/10.3390/w16162282 - 13 Aug 2024
Viewed by 932
Abstract
Based on the success of an irrigation project that utilized two subsurface dams as water sources on Miyako Island, ten additional subsurface dams have now been completed. The technologies that have made the giant subterranean dam possible are the integrated storage model for [...] Read more.
Based on the success of an irrigation project that utilized two subsurface dams as water sources on Miyako Island, ten additional subsurface dams have now been completed. The technologies that have made the giant subterranean dam possible are the integrated storage model for creating water utilization plans and the Soil Mixed Wall method for constructing cut-off walls. Although it might be tempting to assume that all subsurface dams in the Ryukyu limestone region were built under identical topographical and geological conditions, the reality is quite different. Each dam faced unique geological and construction challenges that engineers skillfully overcame during the building process. The purpose of this paper is to introduce information on the planning and construction technology of agricultural subsurface dams in the Ryukyu Arc, which has not been reported in English so far, and to clarify the characteristics of agricultural subsurface dams in the Ryukyu Arc. There is a strong correlation between the gross reservoir capacity and the active capacity of large-scale subsurface dams. Eleven percent of the construction cost was the cost of design and investigation. The water price is the same as or slightly higher than that of surface dams. Full article
Show Figures

Figure 1

Figure 1
<p>Relationship between geology and subsurface dams from southwestern Japan to the Ryukyu Arc (Geological map is modified from [<a href="#B16-water-16-02282" class="html-bibr">16</a>]. The background submarine topographic map is from the Geospatial Information Authority of Japan [<a href="#B17-water-16-02282" class="html-bibr">17</a>]). The black square indicates the area of <a href="#water-16-02282-f002" class="html-fig">Figure 2</a>.</p>
Full article ">Figure 2
<p>Relationship between geology and subsurface dams around Okinawa Island (modified from [<a href="#B20-water-16-02282" class="html-bibr">20</a>]).</p>
Full article ">Figure 3
<p>Frequency distribution of the permeability of Ryukyu limestone in the Minafuku subsurface dam basin [<a href="#B25-water-16-02282" class="html-bibr">25</a>].</p>
Full article ">Figure 4
<p>Effective porosity of Ryukyu limestone estimated by various methods [<a href="#B25-water-16-02282" class="html-bibr">25</a>].</p>
Full article ">Figure 5
<p>Fluctuations in water level over a five-year period from before the closure of the underground valley with the cut-off wall to the dam’s full water level (EL.31 m) in Sunagawa Dam sub-basin 4 [<a href="#B28-water-16-02282" class="html-bibr">28</a>].</p>
Full article ">Figure 6
<p>Map of Miyako Island and surrounding remote islands (<b>a</b>), Miyako Island 3D topographic map (<b>b</b>), 3D bedrock (Shimajiri Group mudstone) topographic map (<b>c</b>) [<a href="#B34-water-16-02282" class="html-bibr">34</a>], A−A’ geological cross-section (<b>d</b>) [<a href="#B34-water-16-02282" class="html-bibr">34</a>]. Ryukyu limestone is distributed between maps (<b>b</b>,<b>c</b>). The original data of (<b>c</b>,<b>d</b>) are sited from [<a href="#B34-water-16-02282" class="html-bibr">34</a>]. The Minafuku Dam site is located in the midstream part of the Bora basin. For instructions on how to create a 3D map, see the main text.</p>
Full article ">Figure 6 Cont.
<p>Map of Miyako Island and surrounding remote islands (<b>a</b>), Miyako Island 3D topographic map (<b>b</b>), 3D bedrock (Shimajiri Group mudstone) topographic map (<b>c</b>) [<a href="#B34-water-16-02282" class="html-bibr">34</a>], A−A’ geological cross-section (<b>d</b>) [<a href="#B34-water-16-02282" class="html-bibr">34</a>]. Ryukyu limestone is distributed between maps (<b>b</b>,<b>c</b>). The original data of (<b>c</b>,<b>d</b>) are sited from [<a href="#B34-water-16-02282" class="html-bibr">34</a>]. The Minafuku Dam site is located in the midstream part of the Bora basin. For instructions on how to create a 3D map, see the main text.</p>
Full article ">Figure 7
<p>Conceptual diagram of the integrated storage model. Sub-basin division map of the Minafuku basin (<b>a</b>), Conceptual diagram of Minafuku Dam integrated storage model (<b>b</b>) and Tank structure diagram (<b>c</b>) (modified from [<a href="#B5-water-16-02282" class="html-bibr">5</a>]).</p>
Full article ">Figure 8
<p>Conceptual diagram of H-Q curve for integrated storage model. Relationship between limestone volume: V, water storage volume: Q, and groundwater level: H in sub-basin (<b>a</b>), and the relationship between groundwater level and water storage volume for each sub-basin (<b>b</b>). Q is calculated using the formula Q = λ: effective porosity (0.10) × V. The circular numbers (e.g.①) are sub-basin numbers in <a href="#water-16-02282-f007" class="html-fig">Figure 7</a>. ▼ numbers (e.g., 70.0) shows the minimum ground elevations in the sub-basin (②). (<b>b</b>) is modified from [<a href="#B5-water-16-02282" class="html-bibr">5</a>].</p>
Full article ">Figure 9
<p>(<b>a</b>) Conceptual diagram of groundwater flow and (<b>b</b>) composite permeability of the integrated storage model.</p>
Full article ">Figure 10
<p>Permeability distribution map after completion of the Minafuku Dam (<b>a</b>) and grouting specifications (<b>b</b>) (modified from [<a href="#B25-water-16-02282" class="html-bibr">25</a>]). The fault zone shown in the permeability distribution map was consolidated and had low permeability. The black circles in the grout pattern diagram indicate the cement + clay grout holes. They are first injected to fill large gaps. The small gap is then filled with cement at the grout hole, as indicated by the open circle.</p>
Full article ">Figure 11
<p>Construction sequence of a cut-off wall using the MW construction method (<b>a</b>), overall view of construction status (<b>b</b>), tip of the 3-axis auger (<b>c</b>), and state of excavating the completed cut-off wall (<b>d</b>). Cement milk is s discharged from the left and right augers of the 3-axis auger, and air for mixing is sprayed from the center auger.</p>
Full article ">Figure 12
<p>(<b>a</b>) Standard drilling auger φ550 mm × 90 cm pitch and adjustment pile and (<b>b</b>) large-diameter auger for deep drilling φ700 mm × 120 cm pitch (<b>b</b>).</p>
Full article ">Figure 13
<p>Topographical map of southern Okinawa Main Island (<b>a</b>) and distribution map of the Komesu, Makabe, and Ueshiro basins that make up the Komesu Dam watershed (<b>b</b>) [<a href="#B23-water-16-02282" class="html-bibr">23</a>,<a href="#B42-water-16-02282" class="html-bibr">42</a>]. The red line indicates the cut-off wall location of the Komesu dam. Orange lines indicate contour lines at 5 m intervals. The arrow in (<b>b</b>) indicates the flow of groundwater. Further details are provided in the text.</p>
Full article ">Figure 14
<p>3D topography of the Komesu basin (<b>a</b>), 3D topography of the base rock (<b>b</b>). The interval of contour lines in (<b>a</b>) and (b) are 5 m. The yellow arrow indicates the cross-section line of electrical exploration (<a href="#water-16-02282-f015" class="html-fig">Figure 15</a>a).</p>
Full article ">Figure 15
<p>Resistivity cross-section along the coastline and vertical profile of electrical conductivity (EC) (<b>a</b>), 3D saltwater intrusion situation map in 1994 (<b>b</b>) (modified from [<a href="#B53-water-16-02282" class="html-bibr">53</a>]). The cross-section line in (<b>a</b>) is shown in <a href="#water-16-02282-f014" class="html-fig">Figure 14</a>a.</p>
Full article ">Figure 16
<p>Outline of the Komesu subsurface dam (modified from [<a href="#B52-water-16-02282" class="html-bibr">52</a>]).</p>
Full article ">Figure 17
<p>Conception of the reservoir level and saltwater movement in the reservoir area (modified from [<a href="#B52-water-16-02282" class="html-bibr">52</a>,<a href="#B54-water-16-02282" class="html-bibr">54</a>]). (<b>a</b>) Groundwater level is EL.4.0 m or higher; (<b>b</b>) Groundwater level is EL.0.0 m or lower. The boundary between saltwater and freshwater was defined as 5000 μS/cm. Blue arrows indicate groundwater flow. Red arrows indicate saltwater flow.</p>
Full article ">Figure 18
<p>(<b>a</b>) Topographic map; (<b>b</b>) geological map of the Kumejima. The geological map is a simplified map form [<a href="#B29-water-16-02282" class="html-bibr">29</a>]. The squared area indicates the plotted area of <a href="#water-16-02282-f019" class="html-fig">Figure 19</a>.</p>
Full article ">Figure 19
<p>(<b>a</b>) Location of the Kanjin Dam reservoir. (<b>b</b>) 3D topographic map of the area around the Kanjin Dam. (<b>c</b>) 3D topographic map of the Kanjin reservoir before impoundment. (<b>d</b>) 3D topographic map of the top surface of the Shimajiri Group. The background photo of (<b>a</b>) is Google Earth. The 3D topographic area of Kumejima (<b>b</b>) is shown in the box in <a href="#water-16-02282-f018" class="html-fig">Figure 18</a>a. Data for (<b>c</b>) and (<b>d</b>) are from [<a href="#B29-water-16-02282" class="html-bibr">29</a>].</p>
Full article ">Figure 20
<p>Facility conceptual diagram of the Kanjin Dam (Modified from [<a href="#B29-water-16-02282" class="html-bibr">29</a>]). (<b>a</b>) Conceptual cross section from the reservoir to the sea and spillway layout. (<b>b</b>) Geological cross section along cut-off wall line A-A’ (<a href="#water-16-02282-f019" class="html-fig">Figure 19</a>c) and cave location map. When floodwaters exceed the critical high-water level (<b>a</b>), they are diverted from the spillway through an orifice to the doline infiltration basin downstream of the dam, where they infiltrate (arrows indicate floodwater movement). See text for gross reservoir capacity and dead capacity. The cave formations are shown in <a href="#water-16-02282-t003" class="html-table">Table 3</a>. See text for cave closure construction.</p>
Full article ">Figure 21
<p>(<b>a</b>) 3D topography of Ie Island, (<b>b</b>) 3D topography of western Ie Island, (<b>c</b>) 3D bedrock topography, (<b>d</b>) bedrock geological map. The data on the bedrock topography and bedrock geology are from [<a href="#B46-water-16-02282" class="html-bibr">46</a>].</p>
Full article ">Figure 22
<p>Geological cross-section along the Ie dam cut-off wall line A–A’ (modified from [<a href="#B46-water-16-02282" class="html-bibr">46</a>]).</p>
Full article ">Figure 23
<p>Topography of Izena Island (<b>a</b>) and 3D topography and geology around the Senbaru lowland and subsurface dam facility layout (<b>b</b>). The yellow square area in (<b>a</b>) (yellow arrow) indicates the area in (<b>b</b>). The 3D map shows the view of Izena Island from the northwest, where the Senbaru lowland is distributed between two mountains.</p>
Full article ">Figure 24
<p>(<b>a</b>) Conceptual stratigraphic section along A–A’ shown in <a href="#water-16-02282-f025" class="html-fig">Figure 25</a> [<a href="#B40-water-16-02282" class="html-bibr">40</a>], and (<b>b</b>) 3D topographic map of the upper part of the pre-tertiary basement shown "Unconformity Boundary B" in (<b>a</b>), and (<b>c</b>) 3D topographic map of the upper part of the alluvial clay layer shown "Unconformity Boundary C" in (<b>a</b>). A 3D map was created from the original figures in [<a href="#B40-water-16-02282" class="html-bibr">40</a>].</p>
Full article ">Figure 24 Cont.
<p>(<b>a</b>) Conceptual stratigraphic section along A–A’ shown in <a href="#water-16-02282-f025" class="html-fig">Figure 25</a> [<a href="#B40-water-16-02282" class="html-bibr">40</a>], and (<b>b</b>) 3D topographic map of the upper part of the pre-tertiary basement shown "Unconformity Boundary B" in (<b>a</b>), and (<b>c</b>) 3D topographic map of the upper part of the alluvial clay layer shown "Unconformity Boundary C" in (<b>a</b>). A 3D map was created from the original figures in [<a href="#B40-water-16-02282" class="html-bibr">40</a>].</p>
Full article ">Figure 25
<p>(<b>a</b>) Layout of Senbaru dam’s water intake trench, water level distribution during pumping test; (<b>b</b>) layout of water intake trench, relay tank, and water pump (modified from [<a href="#B30-water-16-02282" class="html-bibr">30</a>]). The topographical map in the background of (<b>a</b>) is from the Geospatial Information Authority of Japan tile standard map. The arrows in (<b>b</b>) show the flow of water from the intake trench and the surface reservoir to the pumping station. Opening and closing the gate controls whether groundwater or surface water is used.</p>
Full article ">Figure 26
<p>(<b>a</b>) Structure of Senbaru dam water intake trench, and (<b>b</b>) explanatory diagram of water intake calculation constants (modified from [<a href="#B61-water-16-02282" class="html-bibr">61</a>]).</p>
Full article ">Figure 27
<p>Annual NO<sub>3</sub>-N concentration fluctuations in the Shirakawada and Kajidou water sources, which are tap water sources on Miyako Island, and monthly NO<sub>3</sub>-N concentration fluctuations in the Kajidou water source (Fukusato Dam basin) and Muiga spring water (Nakahara basin) used for the intervention analysis for causal inference (created from data in [<a href="#B68-water-16-02282" class="html-bibr">68</a>]). The locations of the Shirakawada, Kajido and Muiga springs are shown in <a href="#water-16-02282-f006" class="html-fig">Figure 6</a>.</p>
Full article ">Figure 28
<p>Comparison of the accumulation process of infiltration water and the amount of nitrogen leached by infiltration observed in the lysimeter experiment and precipitation events of 30 mm or more. The bar graph shows the daily fluctuation of the total amount of precipitation and irrigation (Modified and added from [<a href="#B75-water-16-02282" class="html-bibr">75</a>]).</p>
Full article ">Figure 29
<p>Intervention Analysis Results. The upper panel displays the observed NO<sub>3</sub>-N concentration data from Kajido (solid line) alongside the estimated data (dotted line), which represents the concentration change without the construction of the subsurface dam. The blue-shaded area indicates the 95% confidence interval for the inferred data. The middle panel provides a pointwise comparison of the observed data and the counterfactual predictions. The lower panel illustrates the cumulative impact of subsurface dam intervention (Imaizumi unpublished data).</p>
Full article ">Figure 30
<p>Relationships between gross reservoir capacity and catchment area (<b>a</b>), gross reservoir capacity and active capacity (<b>b</b>), and gross reservoir capacity and dead capacity (<b>c</b>) of subsurface dams in the Ryukyu Arc.</p>
Full article ">Figure 31
<p>Breakdown of construction costs for the Sunagawa and Fukusato dams.</p>
Full article ">
19 pages, 6138 KiB  
Article
Spectral-Frequency Conversion Derived from Hyperspectral Data Combined with Deep Learning for Estimating Chlorophyll Content in Rice
by Lei Du and Shanjun Luo
Agriculture 2024, 14(7), 1186; https://doi.org/10.3390/agriculture14071186 - 18 Jul 2024
Viewed by 965
Abstract
As a vital pigment for photosynthesis in rice, chlorophyll content is closely correlated with growth status and photosynthetic capacity. The estimation of chlorophyll content allows for the monitoring of rice growth and facilitates precise management in the field, such as the application of [...] Read more.
As a vital pigment for photosynthesis in rice, chlorophyll content is closely correlated with growth status and photosynthetic capacity. The estimation of chlorophyll content allows for the monitoring of rice growth and facilitates precise management in the field, such as the application of fertilizers and irrigation. The advancement of hyperspectral remote sensing technology has made it possible to estimate chlorophyll content non-destructively, quickly, and effectively, offering technical support for managing and monitoring rice growth across wide areas. Although hyperspectral data have a fine spectral resolution, they also cause a large amount of information redundancy and noise. This study focuses on the issues of unstable input variables and the estimation model’s poor applicability to various periods when predicting rice chlorophyll content. By introducing the theory of harmonic analysis and the time-frequency conversion method, a deep neural network (DNN) model framework based on wavelet packet transform-first order differential-harmonic analysis (WPT-FD-HA) was proposed, which avoids the uncertainty in the calculation of spectral parameters. The accuracy of estimating rice chlorophyll content based on WPT-FD and WPT-FD-HA variables was compared at seedling, tillering, jointing, heading, grain filling, milk, and complete periods to evaluate the validity and generalizability of the suggested framework. The results demonstrated that all of the WPT-FD-HA models’ single-period validation accuracy had coefficients of determination (R2) values greater than 0.9 and RMSE values less than 1. The multi-period validation model had a root mean square error (RMSE) of 1.664 and an R2 of 0.971. Even with independent data splitting validation, the multi-period model accuracy can still achieve R2 = 0.95 and RMSE = 1.4. The WPT-FD-HA-based deep learning framework exhibited strong stability. The outcome of this study deserves to be used to monitor rice growth on a broad scale using hyperspectral data. Full article
Show Figures

Figure 1

Figure 1
<p>Design for 42- and 48-plot experiments.</p>
Full article ">Figure 2
<p>Schematic diagram of the deep learning network framework.</p>
Full article ">Figure 3
<p>Dataset partitioning and model validation methods.</p>
Full article ">Figure 4
<p>Changes in rice canopy spectra with SPAD and growth stage: (<b>a</b>) rice canopy reflectance under different chlorophyll contents; (<b>b</b>) changes in rice canopy spectra with growth stage; (<b>c</b>) correlation between rice canopy spectra and chlorophyll content.</p>
Full article ">Figure 5
<p>Correlation analysis of different types of data with chlorophyll content in rice.</p>
Full article ">Figure 6
<p>Correlation of HA characterization parameters with chlorophyll content in rice.</p>
Full article ">Figure 7
<p>Comparison between measured and predicted chlorophyll content based on the DNN model at the seeding, tillering, and jointing stages in the 42-plot experiment (the black line is the fitting line and the red dotted line is the 1:1 line).</p>
Full article ">Figure 8
<p>Comparison between measured and predicted chlorophyll content based on the DNN model at the heading, grain filling, and milk stages in the 42-plot experiment (the black line is the fitting line and the red dotted line is the 1:1 line).</p>
Full article ">Figure 9
<p>Comparison between measured and predicted chlorophyll content based on the DNN model throughout the whole period in the 42-plot experiment (the black line is the fitting line and the red dotted line is the 1:1 line).</p>
Full article ">Figure 10
<p>Comparison between measured and predicted chlorophyll content based on the DNN model throughout the whole period in the 48-plot experiment (the red dotted line is the 1:1 line).</p>
Full article ">
20 pages, 8798 KiB  
Article
Agricultural Drought Model Based on Machine Learning Cubist Algorithm and Its Evaluation
by Sha Sha, Lijuan Wang, Die Hu, Yulong Ren, Xiaoping Wang and Liang Zhang
Hydrology 2024, 11(7), 100; https://doi.org/10.3390/hydrology11070100 - 9 Jul 2024
Viewed by 904
Abstract
Soil moisture is the most direct evaluation index for agricultural drought. It is not only directly affected by meteorological conditions such as precipitation and temperature but is also indirectly influenced by environmental factors such as climate zone, surface vegetation type, soil type, elevation, [...] Read more.
Soil moisture is the most direct evaluation index for agricultural drought. It is not only directly affected by meteorological conditions such as precipitation and temperature but is also indirectly influenced by environmental factors such as climate zone, surface vegetation type, soil type, elevation, and irrigation conditions. These influencing factors have a complex, nonlinear relationship with soil moisture. It is difficult to accurately describe this non-linear relationship using a single indicator constructed from meteorological data, remote sensing data, and other data. It is also difficult to fully consider environmental factors using a single drought index on a large scale. Machine learning (ML) models provide new technology for nonlinear problems such as soil moisture retrieval. Based on the multi-source drought indexes calculated by meteorological, remote sensing, and land surface model data, and environmental factors, and using the Cubist algorithm based on a classification decision tree (CART), a comprehensive agricultural drought monitoring model at 10 cm, 20 cm, and 50 cm depth in Gansu Province is established. The influence of environmental factors and meteorological factors on the accuracy of the comprehensive model is discussed, and the accuracy of the comprehensive model is evaluated. The results show that the comprehensive model has a significant improvement in accuracy compared to the single variable model, which is a decrease of about 26% and 28% in RMSE and MAPE, respectively, compared to the best MCI model. Environmental factors such as season, DEM, and climate zone, especially the DEM, play a crucial role in improving the accuracy of the integrated model. These three environmental factors can comprehensively reduce the average RMSE of the comprehensive model by about 25%. Compared to environmental factors, meteorological factors have a slightly weaker effect on improving the accuracy of comprehensive models, which is a decrease of about 6.5% in RMSE. The fitting accuracy of the comprehensive model in humid and semi-humid areas, as well as semi-arid and semi-humid areas, is significantly higher than that in arid and semi-arid areas. These research results have important guiding significance for improving the accuracy of agricultural drought monitoring in Gansu Province. Full article
Show Figures

Figure 1

Figure 1
<p>Geographical location (<b>a</b>), vegetation type (<b>b</b>), and climate zone diagram of Gansu Province (<b>c</b>).</p>
Full article ">Figure 2
<p>Heat map of the correlation between drought indexes and RSM at a depth of 10 cm. In the figure, * represents <span class="html-italic">p</span> &lt; 0.05, ** represents <span class="html-italic">p</span> &lt; 0.01, *** represents <span class="html-italic">p</span> &lt; 0.001.</p>
Full article ">Figure 3
<p>The box diagram of R2 of CART, Cubist, and RF in training and test data sets by using different numbers of input variables.</p>
Full article ">Figure 4
<p>Cross-validation results of model accuracy under different environmental factors at a depth of 10 cm (In the figure, “NoEnvi” represents no environmental factors, while “S”, “D”, “C”, “I” represent season, DEM, climate zone, and irrigation, respectively).</p>
Full article ">Figure 5
<p>Cross-validation results after adding different variables to the variable sets at 10 cm depth (<b>a</b>), 20 cm depth (<b>b</b>), and 50 cm depth (<b>c</b>).</p>
Full article ">Figure 6
<p>Scatter plots of observation and fitting values for the comprehensive model and MCI model at depths of 10 cm (<b>a</b>), 20 cm (<b>b</b>), and 50 cm (<b>c</b>) on the test dataset (In the figure, (a)~(e) represent humid areas, semi-humid areas, semi-arid areas, semi-arid and semi-humid areas, and arid areas, respectively; 1 and 2 represent the comprehensive model and MCI model, respectively).</p>
Full article ">Figure 7
<p>Time series diagrams of the true and predicted RSM at a depth of 10 cm depth at Gaotai (<b>a</b>), Minle (<b>b</b>), Yuzhong (<b>c</b>), Lintao (<b>d</b>), and Lixian (<b>e</b>) in different climate zones (Gaotai, Minle, Yuzhong, Lintao, and Lixian are located in arid areas, semi-arid and semi-humid areas, semi-arid areas, semi-humid areas, and humid areas, respectively).</p>
Full article ">Figure 8
<p>Spatial distribution diagram of the RSME difference between the model without considering environmental factors and the model considering environmental factors ((<b>a</b>) is only considering season factors, (<b>b</b>) is only considering DEM factors, (<b>c</b>) is only considering climate zone factors, and (<b>d</b>) is considering all three factors simultaneously).</p>
Full article ">Figure 9
<p>Spatial distribution diagram of the RSME difference between the model without considering meteorological factors and the model considering meteorological factors at 10 cm depth ((<b>a</b>) is only considering MCI, (<b>b</b>) is only considering SPI1, (<b>c</b>) is only considering SPI9, (<b>d</b>) is only considering WSA, (<b>e</b>) is considering MCI, SPI1, SPI9, and WSA simultaneously).</p>
Full article ">Figure 10
<p>The drought classification map of the comprehensive agricultural drought index at 10 cm depth in June (<b>a1</b>), July (<b>a2</b>), and August (<b>a3</b>) of 2016, and the percentage of precipitation anomalies in June (<b>b1</b>), July (<b>b2</b>), and August (<b>b3</b>), as well as the actual RSM at 0–30 cm depth on June 16 (<b>c1</b>), July 16 (<b>c2</b>), and August 16 (<b>c3</b>).</p>
Full article ">
Back to TopTop