“…Hence, it is necessary to conduct further research in the study area to explore the impact of vegetation restoration under fragile lithologies to make the results of this study more universally applicable. Second, the connection between the bedrock and vegetation can be clarified from nutrients (Beig et al, 2022; Ibrahimi et al, 2022; Khan et al, 2021). The availability of many mineral nutrients that are critically important for plant growth may be controlled by chemical and physical processes at the soil–bedrock interface (Dai et al, 2018).…”
Section: Discussionmentioning
confidence: 99%
“…Hence, it is necessary to conduct further research in the study area to explore the impact of vegetation restoration under fragile lithologies to make the results of this study more universally applicable. Second, the connection between the bedrock and vegetation can be clarified from nutrients (Beig et al, 2022;Ibrahimi et al, 2022;Khan et al, 2021).…”
Section: Implications Limitations and Future Research Of This Studymentioning
confidence: 99%
“…For example, irrigation with treated wastewater may affect soil quality (Ibrahimi et al, 2022), and tillage practices may alter soil texture, organic matter, and porosity (Amami et al, 2021). In addition, different fertilization methods also affect soil organic matter (Khalid et al, 2022; Khan et al, 2021; Zafar et al, 2021). However, the mechanisms affecting the changes in soil properties are sometimes inconsistent owing to differences in environmental factors (Hu et al, 2018).…”
Ecological restoration projects have significantly increased global vegetation cover and reduced soil erosion. However, it is very challenging to clarify the complex soil erosion mechanisms of limestone and dolomite in the southwest karst region and to identify the key factors affecting erosion. The study site has a subtropical monsoon climate with precipitation concentrated during the rainy season from May to September. In this study, four plantation restoration measures with a recovery time of approximately 16 years were selected, which included arbor forest, orchard, grassland, and cropland (control). Soil physical–chemical properties and soil erodibility K values were used to evaluate the soil erosion characteristics. The results showed that both limestone and dolomite exhibited lower soil bulk density as well as higher capillary porosity, and soil water‐stable aggregates after revegetation. The limestone and dolomite K values were reduced by 12%–15% and 15%–17%, respectively. However, the K value of limestone was 17.9% higher than that of dolomite, indicating that dolomite exhibited a higher stability. Through redundancy analysis and structural equation modeling, revegetation was found to reduce soil erosion by influencing the soil particle composition. The silt was the key factor influencing soil erosion, accounting for 84.4% and 78.2% of the variation in the limestone and dolomite K values, respectively. These findings suggest that vegetation restoration enhances soil erosion resistance; however, the effectiveness of restoration is controlled by the lithology in the southwest karst region. These findings provide a reference for soil and water management and vegetation restoration.
“…Hence, it is necessary to conduct further research in the study area to explore the impact of vegetation restoration under fragile lithologies to make the results of this study more universally applicable. Second, the connection between the bedrock and vegetation can be clarified from nutrients (Beig et al, 2022; Ibrahimi et al, 2022; Khan et al, 2021). The availability of many mineral nutrients that are critically important for plant growth may be controlled by chemical and physical processes at the soil–bedrock interface (Dai et al, 2018).…”
Section: Discussionmentioning
confidence: 99%
“…Hence, it is necessary to conduct further research in the study area to explore the impact of vegetation restoration under fragile lithologies to make the results of this study more universally applicable. Second, the connection between the bedrock and vegetation can be clarified from nutrients (Beig et al, 2022;Ibrahimi et al, 2022;Khan et al, 2021).…”
Section: Implications Limitations and Future Research Of This Studymentioning
confidence: 99%
“…For example, irrigation with treated wastewater may affect soil quality (Ibrahimi et al, 2022), and tillage practices may alter soil texture, organic matter, and porosity (Amami et al, 2021). In addition, different fertilization methods also affect soil organic matter (Khalid et al, 2022; Khan et al, 2021; Zafar et al, 2021). However, the mechanisms affecting the changes in soil properties are sometimes inconsistent owing to differences in environmental factors (Hu et al, 2018).…”
Ecological restoration projects have significantly increased global vegetation cover and reduced soil erosion. However, it is very challenging to clarify the complex soil erosion mechanisms of limestone and dolomite in the southwest karst region and to identify the key factors affecting erosion. The study site has a subtropical monsoon climate with precipitation concentrated during the rainy season from May to September. In this study, four plantation restoration measures with a recovery time of approximately 16 years were selected, which included arbor forest, orchard, grassland, and cropland (control). Soil physical–chemical properties and soil erodibility K values were used to evaluate the soil erosion characteristics. The results showed that both limestone and dolomite exhibited lower soil bulk density as well as higher capillary porosity, and soil water‐stable aggregates after revegetation. The limestone and dolomite K values were reduced by 12%–15% and 15%–17%, respectively. However, the K value of limestone was 17.9% higher than that of dolomite, indicating that dolomite exhibited a higher stability. Through redundancy analysis and structural equation modeling, revegetation was found to reduce soil erosion by influencing the soil particle composition. The silt was the key factor influencing soil erosion, accounting for 84.4% and 78.2% of the variation in the limestone and dolomite K values, respectively. These findings suggest that vegetation restoration enhances soil erosion resistance; however, the effectiveness of restoration is controlled by the lithology in the southwest karst region. These findings provide a reference for soil and water management and vegetation restoration.
“…Rice plants fertilized with exogenous urea–chitosan nanohybrid (i.e., 500 mg/L) + 60% classical urea, significantly enhanced the growth and yield-related traits ( Elshayb et al., 2022 ). In Sorghum bicolor (L.) Moench, application of the calcium nitrate-gelatin (CNG) coated urea showed maximum dry matter accumulation, high average plant chlorophyll content and apparent nitrogen recovery (ANR) of 71.14% in shoot and 4.5% in roots, respectively ( Khan et al., 2021 ). In Solanum tuberosum L., application of the nano-tri combination (N+Mo+B) increased chlorophyll content, the yield of the dry vegetative part, starch content, total protein and ascorbic acid ( Al-juthery and Al-Maamouri, 2020 ).…”
Drought is a leading threat that impinges on plant growth and productivity. Nanotechnology is considered an adequate tool for resolving various environmental issues by offering avant-garde and pragmatic solutions. Using nutrients in the nano-scale including CaP-U NPs is a novel fertilization strategy for crops. The present study was conducted to develop and utilize environment-friendly urea nanoparticles (NPs) based nano-fertilizers as a crop nutrient. The high solubility of urea molecules was controlled by integrating them with a matrix of calcium phosphate nanoparticles (CaP NPs). CaP NPs contain high phosphorous and outstanding biocompatibility. Scanning electron microscopy (FE-SEM), transmission electron microscopy (TEM) and X-ray diffraction analysis (XRD) were used to characterize the fabricated NPs. FE-SEM determined no areas of phase separation in urea and calcium phosphate, indicating the successful formation of an encapsulated nanocomposite between the two nano matrices. TEM examination confirmed a fiber-like structure of CaP-U NPs with 15 to 50 nm diameter and 100 to 200 nm length. The synthesized CaP-U NPs and bulk urea (0.0, 0.1% and 0.5%) were applied by foliar sprays at an interval of 15 days on pre-sowed VL-379 variety of finger millet (Eleusine coracana (L.) Gaertn.), under irrigated and drought conditions. The application of the CaP-U NPs significantly enhanced different plant growth attributes such as shoot length (29.4 & 41%), root length (46.4 & 51%), shoot fresh (33.6 & 55.8%) and dry weight (63 & 59.1%), and root fresh (57 & 61%) and dry weight (78 & 80.7%), improved pigment system (chlorophyll) and activated plant defense enzymes such as proline (35.4%), superoxide dismutase (47.7%), guaiacol peroxidase (30.2%), ascorbate peroxidase (70%) under both irrigated and drought conditions. Superimposition of five treatment combinations on drought suggested that CaP-U NPs at 0.5 followed by 0.1% provided the highest growth indices and defense-related enzymes, which were significantly different. Overall, our findings suggested that synthesized CaP-U NPs treatment of finger millet seeds improved plant growth and enzymatic regulation, particularly more in drought conditions providing insight into the strategy for not only finger millet but probably for other commercial cereals crops which suffer from fluctuating environmental conditions.
“…Calcium oxide is one such compound that is abundant in nature and it shows basic properties upon dissolution in water. 64 Thus, a composite made of calcium oxide will modulate the release of a substrate embedded within and improvise acid-base properties to control the release without polluting the environment. Hence, there is a requirement to explore the structural features of different salts and composites of urea or thiourea-derived compounds.…”
The structural characterisation of self-assemblies and photoluminescence of the perchlorate salts of the 1-(naphthalen-1-yl)-3-(pyridin-4-ylmethyl)urea (naphurea) and 1-(naphthalen-1-yl)-3-(pyridin-4-ylmethyl)thiourea (naphthiourea) and their comparision with the parent urea or thiourea derivatives are presented....
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