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Search Results (385)

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Keywords = anthropogenic CO2 emissions

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18 pages, 4008 KiB  
Article
Source and Ecological Risk Assessment of Potentially Toxic Metals in Urban Riverine Sediments Using Multivariate Analytical and Statistical Tools
by Xiaojun Zheng, Abdul Rehman, Shan Zhong, Shah Faisal, Muhammad Mahroz Hussain, Syeda Urooj Fatima and Daolin Du
Land 2025, 14(1), 32; https://doi.org/10.3390/land14010032 - 27 Dec 2024
Viewed by 389
Abstract
Multivariate and statistical tool advancements help to assess potential pollution threats, their geochemical distribution, and the competition between natural and anthropogenic influences, particularly on sediment contamination with potentially toxic metals (PTMs). For this, riverine sediments from 25 locations along urban banksides of the [...] Read more.
Multivariate and statistical tool advancements help to assess potential pollution threats, their geochemical distribution, and the competition between natural and anthropogenic influences, particularly on sediment contamination with potentially toxic metals (PTMs). For this, riverine sediments from 25 locations along urban banksides of the River Ravi, Pakistan, were collected and analyzed to explore the distribution, pollution, ecological, and toxicity risk indices of PTMs like Al, As, Cd, Co, Cr, Cu, Fe, Hg, Mn, Ni, Pb, Sb, Sn, Sr, V, and Zn using Inductively Coupled Plasma–Optical Emission Spectrometry (ICP-OES) technique. Additionally, techniques such as X-ray Diffraction (XRD) and Scanning Electron Microscopy–Energy Dispersive X-ray Spectroscopy (SEM-EDS) were employed to investigate the mineralogical and morphological aspects. The results indicated that mean concentrations (mg kg−1) of Cd (2.37), Cr (128), Hg (16.6), Pb (26.6), and Sb (2.44) were significantly higher than reference values given for upper continental crust (UCC) and world soil average (WSA), posing potential threats. Furthermore, the geochemical pollution indices showed that sediments were moderately polluted with Cd (Igeo = 2.37, EF = 12.1, and CF = 7.89) and extremely polluted with Hg (Igeo = 4.54, EF = 63.2, and CF = 41.41). Ecological and toxicity risks were calculated to be extremely high, using respective models, predominantly due to Hg (Eri = 1656 and ITRI = 91.6). SEM-EDS illustrated the small extent of anthropogenic particles having predominant concentrations of Zn, Fe, Pb, and Sr. Multivariate statistical analyses revealed significant associations between the concentrations of PTMs and the sampling locations, highlighting the anthropogenic contributions linked to local land-use characteristics. The present study concludes that River Ravi sediments exhibit moderate levels of Cd and extreme pollution by Hg, both of which contribute highly to extreme ecological and toxicity risks, influenced by both natural and anthropogenic contributions. Full article
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<p>Location of the sampling sites across the River Ravi. Details of the sampling area, geographical coordinates, and land-use type attributed to each location are provided in <a href="#app1-land-14-00032" class="html-app">Table S1</a>.</p>
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<p>The box plot shows the mean, median, and range of the geo-accumulation index (<span class="html-italic">I</span><sub>geo</sub>) for various PTMs.</p>
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<p>The box plots show the mean, median, and range of values for (<b>a</b>) enrichment factors (EFs) and (<b>b</b>) contamination factors (CFs) of various PTMs.</p>
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<p>Bar graph illustrations reveal the alarming values of the Nemerow pollution index (NPI), especially for chromium (Cr), antimony (Sb), cadmium (Cd) and mercury (Hg) in the sediments of River Ravi, Punjab, Pakistan.</p>
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<p>The box plots show the mean, median, and range of values for (<b>a</b>) the Ecological Risk Index (Eri) and (<b>b</b>) the Integrated Toxicity Risk Index (ITRI) of PTMs.</p>
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<p>X-ray diffraction analysis (XRD) spectra for representative sediment samples (SS4, SS12, SS18, SS22) showing corresponding peaks for a range of minerals, including Q = Quartz, K = Kaolinite, F = Feldspar, and C = Calcite.</p>
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<p>Scanning electron microscopy (SEM) images show the anthropogenic influence in the riverine sediments, by showing distinguished particles. EDS spectra indicated the quantitative proportion of various PTMs from corresponding particles.</p>
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<p>Results of multivariate statistical analysis illustrating the (<b>a</b>) corrplot of Pearson’s correlation coefficient (PCC) at <span class="html-italic">p</span> &lt; 0.05; (<b>b</b>) cluster analysis (CA) dendrogram; and (<b>c</b>) principal component analysis (PCA) using the rotation method (varimax with Kaiser normalization).</p>
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19 pages, 5204 KiB  
Article
Assessment of Heavy Metal Content and Identification of Their Sources in Bottom Sediments and Various Macrophyte Species of the Narew River (Poland)
by Mirosław Skorbiłowicz and Marcin Sidoruk
Minerals 2025, 15(1), 8; https://doi.org/10.3390/min15010008 - 25 Dec 2024
Viewed by 274
Abstract
The condition of the aquatic environment, particularly in protected areas of high ecological value such as the Narew River, requires detailed monitoring to identify and minimise the impact of anthropogenic factors on the ecosystem. This study focused on the content of heavy metals [...] Read more.
The condition of the aquatic environment, particularly in protected areas of high ecological value such as the Narew River, requires detailed monitoring to identify and minimise the impact of anthropogenic factors on the ecosystem. This study focused on the content of heavy metals in bottom sediments and macrophytes of the Narew River, emphasising the influence of human activities and natural factors on this ecologically valuable ecosystem. Pb, Cr, Zn, Cd, Fe, and Mn concentrations were analysed in sediment samples, and ten macrophyte species were collected at 11 sampling points along the river. A geochemical index (Igeo) and multivariate statistical analyses were employed to identify sources of contamination. The digested samples (sediments and plants) were analysed for Pb, Cr, Cu, Zn, Ni, Cd, Fe, and Mn using flame atomic absorption spectrometry (AAS) on an ICE 3500 Thermo Scientific spectrometer, with a measurement error below 5%, validated against certified reference materials. The study results indicated that most metals, including Ni, Cr, Co, Fe, and Mn, predominantly originate from natural geological processes. In contrast, Zn, Cd, Cu, and Pb were identified as being enriched due to anthropogenic activities. An analysis of macrophytes revealed varied patterns of metal accumulation, which correspond to the bioavailability of metals and their environmental concentrations. Comprehensive statistical analyses provided insights into the predominant sources of metal contamination, closely associated with industrial emissions, agricultural runoff, and transportation activities. The integration of sediment and macrophyte monitoring allowed for a thorough evaluation of the Narew River ecosystem, facilitating the identification of key pollution sources. These findings highlight the critical need for measures to mitigate anthropogenic contributions of heavy metals—particularly from industrial, agricultural, and transportation sectors—to safeguard the Narew River’s unique ecological and natural heritage. Full article
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<p>Locations of measurement points along the Narew River in Poland.</p>
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<p>Factor scores in points—bottom sediments.</p>
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<p>Factor scores in points—macrophytes.</p>
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<p>Hierarchical dendrograms for heavy metals in sediments obtained by Ward’s hierarchical clustering method.</p>
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<p>Hierarchical dendrograms for heavy metals in macrophytes were obtained by Ward’s hierarchical clustering method.</p>
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14 pages, 2492 KiB  
Article
Long-Term Variation Characteristics and Health Risks of Atmospheric Hg in the Largest City in Northwestern China
by Yuqi Pang, Hongmei Xu, Mengyun Yang, Bin Zhang, Liyan Liu, Sulin Chen, Jing Xue, Hui Zhang and Zhenxing Shen
Toxics 2024, 12(12), 935; https://doi.org/10.3390/toxics12120935 - 23 Dec 2024
Viewed by 304
Abstract
In this study, gaseous element mercury (GEM) and gaseous oxidized mercury (GOM) in the atmosphere were continuously observed at a minute resolution from 1 April 2019 to 31 December 2020 in urban Xi’an, the largest central city in Northwestern China. The concentrations of [...] Read more.
In this study, gaseous element mercury (GEM) and gaseous oxidized mercury (GOM) in the atmosphere were continuously observed at a minute resolution from 1 April 2019 to 31 December 2020 in urban Xi’an, the largest central city in Northwestern China. The concentrations of GEM and GOM drastically fluctuated within the ranges of 0.022–297 ng/m3 and 0.092–381 pg/m3, showing average values of 5.78 ± 7.36 ng/m3 and 14.2 ± 20.8 pg/m3, respectively. GEM and GOM showed a decreasing trend of 0.121 ng/m3 and 0.472 pg/m3 per month, respectively, which we believe was mainly caused by anthropogenic sources, especially by a reduction in coal-fired emissions, rather than meteorological factors. The significant positive correlation between GEM and PM2.5, SO2, NO2, and CO, as well as Cr, As, and Pb in PM2.5 also proves that. GEM showed a higher concentration at nighttime than daytime, while an M-shaped diurnal trend was observed for GOM. The hazard quotient of GEM for both males and females decreased at a rate of 0.003 per month, and children aged 2–5 were more sensitive to non-carcinogenic health risks. The changing trends, controlling factors, and human health risks of Hg in the atmosphere are necessary and crucial to study for improving our understanding of the impacts of Hg in Northwestern China. Full article
(This article belongs to the Special Issue Atmospheric Emissions Characteristics and Its Impact on Human Health)
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Graphical abstract
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<p>The location of the sampling site and Hg sampling system.</p>
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<p>The average monthly variation in GEM and GOM concentrations and Sen’s regression curves.</p>
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<p>Diurnal variation of GEM and GOM concentrations in 2019 and 2020.</p>
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<p>Seasonal variations in GEM and GOM concentrations from November 2019 to November 2020. The dotted gray lines represent the mean values, the solid gray lines within each box represent the median values, the boundaries of the boxes represent 25th and 75th percentiles, the whiskers indicate 10th and 90th percentiles, and the small dots represent outliers.</p>
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<p>Correlation between GEM, GOM, and other air pollutants (Cr, As, and Pb refer to their concentrations in PM<sub>2.5</sub>) and meteorological factors; ** indicates significant correlation at the 0.01 level (double tailed); * indicates significant correlation at the 0.05 level (double tailed).</p>
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<p>The hazard quotient (HQ) and Sen’s regression curves of GEM for different genders in Xi’an during the study period.</p>
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<p>Comparison of HQ of GEM at different age groups and different genders in April 2019 and December 2020 in Xi’an.</p>
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19 pages, 22817 KiB  
Article
Urban Single Precipitation Events: A Key for Characterizing Sources of Air Contaminants and the Dynamics of Atmospheric Chemistry Exchanges
by Maciej Górka, Aldona Pilarz, Magdalena Modelska, Anetta Drzeniecka-Osiadacz, Anna Potysz and David Widory
Water 2024, 16(24), 3701; https://doi.org/10.3390/w16243701 - 22 Dec 2024
Viewed by 453
Abstract
The chemistry of atmospheric precipitation serves as an important proxy for discriminating the source(s) of air contaminants in urban environments as well as to discuss the dynamic of atmospheric chemistry exchanges. This approach can be undertaken at time scales varying from single events [...] Read more.
The chemistry of atmospheric precipitation serves as an important proxy for discriminating the source(s) of air contaminants in urban environments as well as to discuss the dynamic of atmospheric chemistry exchanges. This approach can be undertaken at time scales varying from single events to seasonal and yearly time frames. Here, we characterized the chemical composition of two single rain episodes (18 July 2018 and 21 February 2019) collected in Wrocław (SW Poland). Our results demonstrated inner variations and seasonality (within the rain event as well as between summer and winter), both in ion concentrations as well as in their potential relations with local air contaminants and scavenging processes. Coupling statistical analysis of chemical parameters with meteorological/synoptic conditions and HYSPLIT back trajectories allowed us to identify three main factors (i.e., principal components; PC) controlling the chemical composition of precipitation, and that these fluctuated during each event: (i) PC1 (40%) was interpreted as reflecting the long-range transport and/or anthropogenic influences of emission sources that included biomass burning, fossil fuel combustion, industrial processes, and inputs of crustal origin; (ii) PC2 (20%) represents the dissolution of atmospheric CO2 and HF into ionic forms; and (iii) PC3 (20%) originates from agricultural activities and/or biomass burning. Time variations during the rain events showed that each factor was more important at the start of the event. The study of both SO42− and Ca2+ concentrations showed that while sea spray inputs fluctuated during both rain events, their overall impact was relatively low. Finally, below-cloud particle scavenging processes were only observed for PM10 at the start of the winter rain episode, which was probably explained by the corresponding low rain intensity and an overlap from local aerosol emissions. Our study demonstrates the importance of multi-time scale approaches to explain the chemical variability in rainwater and both its relation to emission sources and the atmosphere operating processes. Full article
(This article belongs to the Section Urban Water Management)
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<p>Study sites in Wrocław (SW Poland): University of Wrocław (UWr), where precipitation was collected; IMWM and CIEP air quality monitoring stations.</p>
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<p>Time variations in the meteorological parameters and chemical composition for precipitation samples collected on 18 July 2018: (<b>A</b>) precipitation at IMWM station, wind velocity and air temperature at UWr station, wind rose (24 h); (<b>B</b>) SO<sub>2</sub>, NO<sub>x</sub>, PM<sub>10</sub>, PM<sub>2.5</sub>, O<sub>3</sub> concentrations at CIEP station; (<b>C</b>) anion concentrations in precipitation; (<b>D</b>) pH, EC, and cation concentrations in precipitation.</p>
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<p>Time variations in the meteorological parameters and chemical composition for precipitation samples collected during on 21 February 2019: (<b>A</b>) precipitation at IMWM and UWr stations, wind velocity and air temperature at UWr station, wind rose (24 h); (<b>B</b>) SO<sub>2</sub>, NO<sub>x</sub>, PM<sub>10</sub>, PM<sub>2.5</sub>, O<sub>3</sub> concentrations at CIEP station; (<b>C</b>) anion concentrations in precipitation; (<b>D</b>) pH, EC, and cation concentrations in precipitation.</p>
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<p>The 48 h NOAA HYSPLIT back trajectories showing air mass movement to Wrocław for the (<b>A</b>) summer (18 July 2018) and (<b>C</b>) winter (21 February 2019) precipitation episodes at 12:00 UTC. KNMI synoptic charts (<a href="https://www.knmi.nl" target="_blank">https://www.knmi.nl</a>, accessed on 29 March 2023) corresponding to the two SOM-based weather patterns at 12:00 UTC on (<b>B</b>) 18 July 2018 and (<b>D</b>) 21 February 2021. Prominent synoptic features: L—low-pressure system; H—high-pressure system; blue—cold front; red—warm front; magenta—occluded front.</p>
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<p>Time variations in the calculated concentrations of nSS and SS sulfates and nSS and SS calcium ions in rainwater for the (<b>A</b>,<b>B</b>) summer (18 July 2018) and (<b>C</b>,<b>D</b>) winter (21 February 2019) rain episodes. Equations used for calculations are detailed in the text.</p>
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<p>Time variations in the rainwater sample scores on each principal component analysis (PCA) principal component for (<b>A</b>) summer (18 July 2018) and (<b>B</b>) winter (21 February 2019) precipitation episodes. Results of the PCA for each precipitation event are also presented. Highlighted red values identify significant loadings.</p>
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26 pages, 13005 KiB  
Article
Analysis of Time–Frequency Characteristics and Influencing Factors of Air Quality Based on Functional Data in Fujian
by Huirou Shen, Yanglan Xiao, Linyi You, Yijing Zheng, Houzhan Xie, Yihan Xu, Zhongzhu Chen, Aidi Wu, Yuning Huang and Tiange You
Atmosphere 2024, 15(12), 1510; https://doi.org/10.3390/atmos15121510 - 17 Dec 2024
Viewed by 398
Abstract
Increased air pollution is driven by anthropogenic pollution emissions and climate change, which pose great challenges to environmental governance. Strengthening the monitoring of regional air quality levels and analyzing the causes of regional pollution is conducive to the management and sustainable development of [...] Read more.
Increased air pollution is driven by anthropogenic pollution emissions and climate change, which pose great challenges to environmental governance. Strengthening the monitoring of regional air quality levels and analyzing the causes of regional pollution is conducive to the management and sustainable development of the regional atmosphere. Functional data obtained on a wavelet basis were used in the fitting of air quality data of Fujian Province, and wavelet decomposition was performed to obtain low-frequency and high-frequency information. While the Fourier basis cannot adaptively adjust the time–frequency window, resulting in the loss of location information of special frequencies, the wavelet basis solves this problem. Functional analysis of variance was utilized for analyzing spatial differences in air pollution characteristics. Furthermore, the study established a multivariate functional linear regression model to explore the impact of meteorological factors and ozone precursor factors. The results indicated that the overall air quality was gradually improving in Fujian Province, but the concentration of ozone was progressively increasing. Air pollution in coastal areas was higher than that in inland areas. The p-values of the functional analysis of variance for energy values and crest values were less than 0.05. Moreover, the energy entropy and kurtosis values were greater than 0.05. There were significant differences of AQI in the fluctuation amplitude and variation characteristics of different cities. The total squared multiple correlation of regression model was above 50% on average. Ozone is currently the most serious pollution factor, mainly affected by wind speed, temperature, NO2, and CO. In summer, it was principally influenced by VOCs. The findings of this study could act as a reference in exploring the time–frequency characteristics of air quality data and support of air pollution control. Full article
(This article belongs to the Section Air Quality)
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<p>Location of the study area (FZ: Fuzhou, LY: Longyan, ND: Ningde, NP: Nanping, PT: Putian, QZ: Quanzhou, SM: Sanming, XM: Xiamen, ZZ: Zhangzhou).</p>
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<p>Flowchart of research methods in the study.</p>
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<p>Overall trend chart of AQI and six pollutants when the decomposition level is 11 (unit: μg/m<sup>3</sup>, except for CO: mg/m<sup>3</sup>).</p>
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<p>LDF and MSE values at different decomposition levels of AQI.</p>
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<p>The AQI and six types of air pollutant curves fitted (unit: μg/m<sup>3</sup>, except for CO: mg/m<sup>3</sup>).</p>
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<p>AQI wavelet variance and cumulative contribution rate.</p>
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<p>Detail components of AQI.</p>
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<p>Detail components of SO<sub>2</sub> (unit: μg/m<sup>3</sup>).</p>
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<p>Detail components of PM<sub>10</sub> (unit: μg/m<sup>3</sup>).</p>
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<p>Detail components of PM<sub>2.5</sub> (unit: μg/m<sup>3</sup>).</p>
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<p>Detail components of O<sub>3</sub> (unit: μg/m<sup>3</sup>).</p>
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<p>Detail components of NO<sub>2</sub> (unit: μg/m<sup>3</sup>).</p>
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<p>Detail components of CO (unit: mg/m<sup>3</sup>).</p>
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<p>AQI energy value box diagram (Group1: FZ, Group 2: LY, Group 3: ND, Group 4: NP, Group 5: PT, Group 6: QZ, Group 7: SM, Group 8: XM, Group 9: ZZ).</p>
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<p>AQI energy entropy box diagram (Group1: FZ, Group 2: LY, Group 3: ND, Group 4: NP, Group 5: PT, Group 6: QZ, Group 7: SM, Group 8: XM, Group 9: ZZ).</p>
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<p>AQI kurtosis box diagram (Group1: FZ, Group 2: LY, Group 3: ND, Group 4: NP, Group 5: PT, Group 6: QZ, Group 7: SM, Group 8: XM, Group 9: ZZ).</p>
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<p>AQI crest value box diagram (Group1: FZ, Group 2: LY, Group 3: ND, Group 4: NP, Group 5: PT, Group 6: QZ, Group 7: SM, Group 8: XM, Group 9: ZZ).</p>
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<p>The left figure shows the total squared multiple correlation, and the right figure shows the squared multiple correlation of ozone precursors CO and NO<sub>2</sub> with O<sub>3</sub> concentration.</p>
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<p>Dynamic changes in the degree of influence of NO<sub>2</sub> concentration, CO concentration, maximum temperature, wind speed, relative humidity, and visibility on O<sub>3</sub> based on the multivariate functional linear model.</p>
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12 pages, 305 KiB  
Article
Analysis of Toxic Element Levels and Health Risks in Different Soybean Species (Glycine max, Vigna radiata, Vigna angularis, Vigna mungo)
by Juan R. Jáudenes-Marrero, Greta Giannantonio, Soraya Paz-Montelongo, Arturo Hardisson, Javier Darias-Rosales, Dailos González-Weller, Ángel J. Gutiérrez, Carmen Rubio and Samuel Alejandro-Vega
Nutrients 2024, 16(24), 4290; https://doi.org/10.3390/nu16244290 - 12 Dec 2024
Viewed by 606
Abstract
Background: Soybeans are a widely consumed legume, essential in Western diets and especially prominent in vegan and vegetarian nutrition. However, environmental contamination from anthropogenic sources, such as industrial emissions, wastewater, and pesticide use, has led to the accumulation of non-essential and toxic elements [...] Read more.
Background: Soybeans are a widely consumed legume, essential in Western diets and especially prominent in vegan and vegetarian nutrition. However, environmental contamination from anthropogenic sources, such as industrial emissions, wastewater, and pesticide use, has led to the accumulation of non-essential and toxic elements in legumes, potentially impacting human health. Method: This study quantified the levels of 11 potential toxic elements (Al, B, Ba, Cd, Co, Cr, Li, Ni, Pb, Sr, V) in 90 samples of four soybean species (Glycine max, Vigna radiata, Vigna angularis, Vigna mungo) using inductively coupled plasma optical emission spectrometry (ICP-OES). Results: Results showed that boron had the highest mean content (9.52 mg/kg ww), followed by aluminum (6.73 mg/kg ww). Among the toxic metals, cadmium was most concentrated in green soybeans (0.03 mg/kg ww), and black soybeans had the highest level of lead (0.07 mg/kg ww). Based on an average soybean consumption of 50 g/day, no immediate health risk was detected. However, lithium and nickel were present in substantial amounts, with lithium contributing 31.43–48.57% and nickel 6.81–39.56% of their respective provisional daily intake limits, especially from red soybeans (V. angularis). Conclusions: This study highlights the importance of monitoring toxic elements in soybeans and calls for stricter environmental management practices to minimize contamination, ensuring the safety of soy products as their global consumption rises. Full article
(This article belongs to the Special Issue New Advances in Dietary Assessment)
14 pages, 3622 KiB  
Article
Comparative Study of the NOx, CO Emissions, and Stabilization Characteristics of H2-Enriched Liquefied Petroleum Gas in a Swirl Burner
by Abay Mukhamediyarovich Dostiyarov, Dias Raybekovich Umyshev, Zhanar Abdeshevna Aidymbayeva, Ayaulym Konusbekovna Yamanbekova, Zhansaya Serikkyzy Duisenbek, Madina Bakytzhanovna Kumargazina, Nurlan Rezhepbayevich Kartjanov and Ainur Serikbayevna Begimbetova
Energies 2024, 17(23), 6132; https://doi.org/10.3390/en17236132 - 5 Dec 2024
Viewed by 486
Abstract
The global shift toward renewable fuels and the reduction in anthropogenic environmental impact have become increasingly critical. However, the current challenges in fully transitioning to environmentally friendly fuels necessitate the use of transitional fuel mixtures. While many alternatives have been explored, the combination [...] Read more.
The global shift toward renewable fuels and the reduction in anthropogenic environmental impact have become increasingly critical. However, the current challenges in fully transitioning to environmentally friendly fuels necessitate the use of transitional fuel mixtures. While many alternatives have been explored, the combination of hydrogen and LPG appears to be the most practical under the conditions specific to Kazakhstan. This study presents experimental findings on a novel burner system that utilizes the airflow swirl and hydrogen enrichment of LPG. It evaluates the effects of hydrogen addition, fuel supply methods, and swirl intensity—achieved by adjusting the outlet vanes—on flame stabilization as well as NOx and CO emissions. The results show that the minimum NOx concentration achieved was 12.08 ppm, while the minimum CO concentration was 101 ppm. Flame stabilization studies indicate that supplying the fuel at the center of the burner, rather than at the base, improves stabilization by 23%. Additionally, increasing the proportion of hydrogen positively affects stabilization. However, the analysis also reveals that, as the hydrogen content in the fuel rises, NOx concentrations increase. These findings highlight the importance of balancing the hydrogen enrichment, airflow swirl, and fuel supply methods to achieve optimal combustion performance. While hydrogen-enriched LPG offers enhanced flame stabilization, the associated rise in NOx emissions presents a challenge that requires careful management to maintain both efficiency and environmental compliance. Full article
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<p>Experimental research methodology.</p>
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<p>Experimental burner device and equipment.</p>
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<p>Dependence of flame stabilization on the vane angle and fraction of hydrogen.</p>
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<p>Lean blow-off dependence from vane angle at a constant hydrogen fraction value.</p>
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<p>Dependence of NOx emissions on vane angle and fraction of hydrogen.</p>
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<p>Dependence of NOx emissions on the vane angle.</p>
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<p>Dependence of CO emissions on the vane angle and fraction of hydrogen.</p>
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<p>Dependence of CO emissions on the vane angle.</p>
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<p>Flame shape dependence on the vane angle.</p>
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6 pages, 798 KiB  
Proceeding Paper
Eco-Friendly Composites—Environmental Assessment of Mine Tailings-Based Geopolymers
by Kinga Korniejenko, Beata Figiela, Michał Łach and Barbara Kozub
Mater. Proc. 2023, 15(1), 94; https://doi.org/10.3390/materproc2023015094 - 4 Dec 2024
Viewed by 678
Abstract
Resource efficiency is one of the basic principles of a circular economy (CE). It can be achieved by finding replacements for natural raw materials using anthropogenic raw materials, including by-products from industrial processes and waste materials. In the case of the Polish economy, [...] Read more.
Resource efficiency is one of the basic principles of a circular economy (CE). It can be achieved by finding replacements for natural raw materials using anthropogenic raw materials, including by-products from industrial processes and waste materials. In the case of the Polish economy, one possible source is the mining tailings from hard coal exploration and also the waste material from post-mining heaps. The main objective of this work is to present the results of an environmental analysis of geopolymers based on mine tailings. Two geopolymer materials were compared using life cycle assessment (LCA) methodology principles. One of them was based on metakaolin, and the second on industrial waste, mainly from coal shale, as a waste product of hard coal mining. The results show that replacing the original material with alternatives such as metakaolin from mine tailings, reduces the environmental impact, including CO2 emissions. The main findings can be helpful in the implementation of CE, especially the development of sustainable materials, which is one of the crucial elements of introducing closed loops into practice. Full article
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<p>Results of the search in the Scopus database: (<b>a</b>) published documents by year; (<b>b</b>) published documents by type [<a href="#B12-materproc-15-00094" class="html-bibr">12</a>].</p>
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<p>Total energy consumption: (<b>a</b>) metakaolin-based geopolymer; (<b>b</b>) mine tailing-based geopolymer.</p>
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<p>GHG emissions: (<b>a</b>) metakaolin-based geopolymer; (<b>b</b>) mine tailing-based geopolymer.</p>
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19 pages, 1444 KiB  
Review
Possible Impacts of Elevated CO2 and Temperature on Growth and Development of Grain Legumes
by Rajanna G. Adireddy, Saseendran S. Anapalli, Krishna N. Reddy, Partson Mubvumba and Justin George
Environments 2024, 11(12), 273; https://doi.org/10.3390/environments11120273 - 2 Dec 2024
Viewed by 853
Abstract
Carbon dioxide (CO2) is the most abundant greenhouse gas (GHG) in the atmosphere and the substrate for the photosynthetic fixation of carbohydrates in plants. Increasing GHGs from anthropogenic emissions is warming the Earth’s atmospheric system at an alarming rate and changing [...] Read more.
Carbon dioxide (CO2) is the most abundant greenhouse gas (GHG) in the atmosphere and the substrate for the photosynthetic fixation of carbohydrates in plants. Increasing GHGs from anthropogenic emissions is warming the Earth’s atmospheric system at an alarming rate and changing its climate, which can affect photosynthesis and other biochemical reactions in crop plants favorably or unfavorably, depending on plant species. For the substrate role in plant carbon reduction reactions, CO2 concentration ([CO2]) in air potentially enhances photosynthesis. However, N uptake and availability for protein synthesis can be a potential limiting factor in enhanced biomass synthesis under enriched [CO2] conditions across species. Legumes are C3 plants and symbiotic N fixers and are expected to benefit from enhanced [CO2] in the air. However, the concurrent increase in air temperatures with enhanced [CO2] demands more detailed investigations on the effects of [CO2] enhancement on grain legume growth and yield. In this article, we critically reviewed and presented the online literature on growth, phenology, photosynthetic rate, stomatal conductance, productivity, soil health, and insect behavior under elevated [CO2] and temperature conditions. The review revealed that specific leaf weight, pod weight, and nodule number and weight increased significantly under elevated [CO2] of up to 750 ppm. Under elevated [CO2], two mechanisms that were affected were the photosynthesis rate (increased) and stomatal conductivity (decreased), which helped enhance water use efficiency in the C3 legume plants to achieve higher yields. Exposure of legumes to elevated levels of [CO2] when water stressed resulted in an increase of 58% in [CO2] uptake, 73% in transpiration efficiency, and 41% in rubisco carboxylation and decreased stomatal conductance by 15–30%. The elevated [CO2] enhanced the yields of soybean by 10–101%, peanut by 28–39%, mung bean by 20–28%, chickpea by 26–31%, and pigeon pea by 31–38% over ambient [CO2]. However, seed nutritional qualities like protein, Zn, and Ca were significantly decreased. Increased soil temperatures stimulate microbial activity, spiking organic matter decomposition rates and nutrient release into the soil system. Elevated temperatures impact insect behavior through higher plant feeding rates, posing an enhanced risk of invasive pest attacks in legumes. However, further investigations on the potential interaction effects of elevated [CO2] and temperatures and extreme climate events on growth, seed yields and nutritional qualities, soil health, and insect behavior are required to develop climate-resilient management practices through the development of novel genotypes, irrigation technologies, and fertilizer management for sustainable legume production systems. Full article
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<p>Response of legumes to elevated [CO<sub>2</sub>] and temperature measured from open-top chambers, free-air [CO<sub>2</sub>] enrichment experiments (FACE), and controlled indoor and outdoor growth chambers.</p>
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<p>Response of elevated [CO<sub>2</sub>] and temperature in legume crops. [<a href="#B1-environments-11-00273" class="html-bibr">1</a>,<a href="#B6-environments-11-00273" class="html-bibr">6</a>,<a href="#B98-environments-11-00273" class="html-bibr">98</a>].</p>
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15 pages, 2639 KiB  
Article
Effects of Prescribed Burns on Soil Respiration in Semi-Arid Grasslands
by Juan Carlos De la Cruz Domínguez, Teresa Alfaro Reyna, Carlos Alberto Aguirre Gutierrez, Víctor Manuel Rodríguez Moreno and Josué Delgado Balbuena
Fire 2024, 7(12), 450; https://doi.org/10.3390/fire7120450 - 30 Nov 2024
Viewed by 536
Abstract
Carbon fluxes are valuable indicators of soil and ecosystem health, particularly in the context of climate change, where reducing carbon emissions from anthropogenic activities, such as forest fires, is a global priority. This study aimed to evaluate the impact of prescribed burns on [...] Read more.
Carbon fluxes are valuable indicators of soil and ecosystem health, particularly in the context of climate change, where reducing carbon emissions from anthropogenic activities, such as forest fires, is a global priority. This study aimed to evaluate the impact of prescribed burns on soil respiration in semi-arid grasslands. Two treatments were applied: a prescribed burn on a 12.29 ha paddock of an introduced grass (Eragostis curvula) with 11.6 t ha−1 of available fuel, and a simulation of three fire intensities, over 28 circular plots (80 cm in diameter) of natural grasslands (Bouteloua gracilis). Fire intensities were simulated by burning with butane gas inside an iron barrel, which represented three amounts of fuel biomass and an unburned treatment. Soil respiration was measured with a soil respiration chamber over two months, with readings collected in the morning and afternoon. Moreover, CO2 emissions by combustion and productivity after fire treatment were quantified. The prescribed burns significantly reduced soil respiration: all fire intensities resulted in a decrease in soil respiration when compared with the unburned area. Changes in albedo increased the soil temperature; however, there was no relationship between changes in temperature and soil respiration; in contrast, precipitation highly stimulated it. These findings suggest that fire, under certain conditions, may not lead to more CO2 being emitted into the atmosphere by stimulating soil respiration, whereas aboveground biomass was reduced by 60%. However, considering the effects of fire in the long-term on changes in nutrient deposition, aboveground and belowground biomass, and soil properties is crucial to effectively quantify its impact on the global carbon cycle. Full article
(This article belongs to the Special Issue Fire in Savanna Landscapes, Volume II)
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<p>Location map of the study area and experimental plot design.</p>
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<p>Availability of initial biomass, residual biomass, and emitted carbon after prescribed burn application.</p>
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<p>Time series of shortwave (285–3000 nm) and longwave radiation (4500–42,000 nm) at the study site one day before the burn (arrow indicates the day of the burn) and days after it. The upper panel shows downwelling radiation, while the lower panel presents upwelling radiation. Day of year (DOY).</p>
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<p>Soil respiration rates, soil temperature, and precipitation before and after burn prescription. Day of year (DOY).</p>
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<p>Diurnal carbon fluxes recorded with the eddy covariance system. The arrow indicates the occurrence of precipitation on day 130. Day of year (DOY).</p>
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<p>Temporal variation of soil respiration in the three intensity treatments and the control, during the period from 21 June to 17 August 2021.</p>
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57 pages, 8823 KiB  
Review
Comprehensive Comparative Review of the Cement Experimental Testing Under CO2 Conditions
by Khizar Abid, Andrés Felipe Baena Velásquez and Catalin Teodoriu
Energies 2024, 17(23), 5968; https://doi.org/10.3390/en17235968 - 27 Nov 2024
Viewed by 1026
Abstract
Global warming is presently one of the most pressing issues the planet faces, with the emission of greenhouse gasses being a primary concern. Among these gasses, CO2 is the most detrimental because, among all the greenhouse gasses resulting from anthropogenic sources, CO [...] Read more.
Global warming is presently one of the most pressing issues the planet faces, with the emission of greenhouse gasses being a primary concern. Among these gasses, CO2 is the most detrimental because, among all the greenhouse gasses resulting from anthropogenic sources, CO2 currently contributes the largest share to global warming. Therefore, to reduce the adverse effects of climate change, many countries have signed the Paris Agreement, according to which net zero emissions of CO2 will be achieved by 2050. In this respect, Carbon Capture and Sequestration (CCS) is a critical technology that will play a vital role in achieving the net zero goal. It allows CO2 from emission sources to be injected into suitable subsurface geological formations, aiming to confine CO2 underground for hundreds of years. Therefore, the confinement of CO2 is crucial, and the success of CCS projects depends on it. One of the main components on which the confinement of the CO2 relies is the integrity of the cement. As it acts as the barrier that restricts the movement of the sequestrated CO2 to the surface. However, in a CO2-rich environment, cement reacts with CO2, leading to the deterioration of its physical, chemical, transfer, morphological, and mechanical properties. This degradation can create flow paths that enable the leakage of sequestered CO2 to the surface, posing risks to humans, animals, and the environment. To address this issue, numerous studies have investigated the use of various additives in cement to reduce carbonation, thus enhancing the cement’s resistance to supercritical (sc) CO2 and maintaining its integrity. This paper provides a comprehensive review of current research on cement carbonation tests conducted by different authors. It includes detailed descriptions of the additives used, testing setups, curing conditions, methodologies employed, and experimental outcomes. This study will help to provide a better understanding of the carbonation process of the cement sample exposed to a CO2-rich environment, along with the pros and cons of the additives used in the cement. A significant challenge identified in this research is the lack of a standardized procedure for conducting carbonation tests, as each study reviewed employed a unique methodology, making direct comparisons difficult. Nonetheless, the paper provides an overview of the most commonly used temperatures, pressures, curing durations, and carbonation periods in the studies reviewed. Full article
(This article belongs to the Section B3: Carbon Emission and Utilization)
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<p>CO<sub>2</sub> being processed and injected in the suitable geological formation [<a href="#B12-energies-17-05968" class="html-bibr">12</a>].</p>
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<p>Phase diagram of CO<sub>2</sub> [<a href="#B20-energies-17-05968" class="html-bibr">20</a>].</p>
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<p>Carbonation zones in the cement [<a href="#B17-energies-17-05968" class="html-bibr">17</a>,<a href="#B33-energies-17-05968" class="html-bibr">33</a>].</p>
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<p>Carbonation setup used by the studies carried out by Duguid and Scherer [<a href="#B34-energies-17-05968" class="html-bibr">34</a>]. Upper section represents the sandstone reservoir condition, while lower part corresponds to the limestone reservoir condition.</p>
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<p>Static reactor used for the testing of dynamic and static carbonation tests by Laudet, et al. [<a href="#B37-energies-17-05968" class="html-bibr">37</a>].</p>
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<p>Static testing cell used by Santra and Sweatman [<a href="#B38-energies-17-05968" class="html-bibr">38</a>] for their studies.</p>
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<p>Well-bore test cell used by Syed et al. [<a href="#B39-energies-17-05968" class="html-bibr">39</a>]. (<b>a</b>) Central mechanism of the testing chamber in which annulus is shown where the cement was poured in (<b>b</b>) Complete assembly of the wellbore cell.</p>
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<p>Setup to which the wellbore test cell was connected by Syed, et al. [<a href="#B39-energies-17-05968" class="html-bibr">39</a>].</p>
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<p>Cement sandstone plug composite and the testing setup of core flooding used by Connell, et al. [<a href="#B40-energies-17-05968" class="html-bibr">40</a>].</p>
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<p>Static carbonation vessel used in studies conducted by Yang, et al. [<a href="#B42-energies-17-05968" class="html-bibr">42</a>].</p>
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<p>Autoclave used for the studies of Costa et al. [<a href="#B43-energies-17-05968" class="html-bibr">43</a>,<a href="#B44-energies-17-05968" class="html-bibr">44</a>].</p>
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<p>Testing schematic used for the carbonation testing by Costa et al. [<a href="#B46-energies-17-05968" class="html-bibr">46</a>].</p>
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<p>HPHT carbonation vessel used by Xu et al. [<a href="#B47-energies-17-05968" class="html-bibr">47</a>].</p>
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<p>HPHT vessel used for the studies carried out by Mahmoud and Elkatatny [<a href="#B49-energies-17-05968" class="html-bibr">49</a>].</p>
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<p>Carbonation setup used for the studies of olive waste cement composite conducted by [<a href="#B51-energies-17-05968" class="html-bibr">51</a>].</p>
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<p>High-pressure vessel used for the studies by Ledesma, et al. [<a href="#B53-energies-17-05968" class="html-bibr">53</a>].</p>
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<p>Schematic and picture of the static reactor used by the studies carried out by Abid, et al. [<a href="#B54-energies-17-05968" class="html-bibr">54</a>] and Tiong, et al. [<a href="#B55-energies-17-05968" class="html-bibr">55</a>].</p>
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<p>Pressure vessel used by Batista, et al. [<a href="#B56-energies-17-05968" class="html-bibr">56</a>] for their carbonation tests.</p>
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<p>HPHT static reactor used for the carbonation testing for the studies carried out by Ponzi, et al. [<a href="#B57-energies-17-05968" class="html-bibr">57</a>]. (<b>A</b>) Cross-sectional veiw (<b>B</b>) Full setup of the carbonation vessel.</p>
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<p>Carbonation testing setup utilized by Jani and Imqam [<a href="#B58-energies-17-05968" class="html-bibr">58</a>].</p>
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<p>Methodology used for the testing of different formulations of cement by Costa, et al. [<a href="#B61-energies-17-05968" class="html-bibr">61</a>].</p>
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<p>HPHT testing cattle used for the pore characterization studies carried out by Gu, et al. [<a href="#B62-energies-17-05968" class="html-bibr">62</a>]. The schematic picture has been modified.</p>
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<p>Static reactor with two different compartments used for the studies of Moraes and Costa [<a href="#B63-energies-17-05968" class="html-bibr">63</a>].</p>
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<p>HPHT corrosion kettle used by Peng, et al. [<a href="#B66-energies-17-05968" class="html-bibr">66</a>] for their studies.</p>
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<p>HPHT static testing vessel used for the studies of Wu, et al. [<a href="#B70-energies-17-05968" class="html-bibr">70</a>]. The picture has been modified.</p>
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<p>Reactor used for the carbonation test studies carried out by Kravanja and Knez [<a href="#B73-energies-17-05968" class="html-bibr">73</a>].</p>
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<p>Carbonation testing setup used by the studies carried out by Barría, et al. [<a href="#B79-energies-17-05968" class="html-bibr">79</a>]. This schematic image has been modified.</p>
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<p>Histogram of initial curing.</p>
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<p>Histogram of carbonation period.</p>
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19 pages, 6256 KiB  
Article
Major and Trace Airborne Elements and Ecological Risk Assessment: Georgia Moss Survey 2019–2023
by Omari Chaligava, Inga Zinicovscaia, Alexandra Peshkova, Nikita Yushin, Marina Frontasyeva, Konstantin Vergel, Makhabbat Nurkassimova and Liliana Cepoi
Plants 2024, 13(23), 3298; https://doi.org/10.3390/plants13233298 - 23 Nov 2024
Viewed by 768
Abstract
The study, carried out as part of the International Cooperative Program on Effects of Air Pollution on Natural Vegetation and Crops, involved collecting 95 moss samples across the territory of Georgia during the period from 2019 to 2023. Primarily samples of Hypnum cupressiforme [...] Read more.
The study, carried out as part of the International Cooperative Program on Effects of Air Pollution on Natural Vegetation and Crops, involved collecting 95 moss samples across the territory of Georgia during the period from 2019 to 2023. Primarily samples of Hypnum cupressiforme were selected, with supplementary samples of Abietinella abietina, Pleurozium schreberi, and Hylocomium splendens in cases of the former’s absence. The content of 14 elements (Al, Ba, Cd, Co, Cr, Cu, Fe, Mn, Ni, Pb, S, Sr, V, and Zn) was detected using Inductively Coupled Plasma Atomic Emission Spectroscopy (ICP-AES), while the Hg content was determined using a Direct Mercury Analyzer. To identify any relationships between chemical elements and to depict their sources, multivariate statistics was applied. Principal component analysis identified three main components: PC1 (geogenic, 43.4%), PC2 (anthropogenic, 13.3%), and PC3 (local anomalies, 8.5%). The results were compared with the first moss survey conducted in Georgia in the period from 2014 to 2017, offering insights into temporal trends of air quality. Utilizing GIS, a spatial map illustrating pollution levels across Georgia, based on the Pollution Load Index, was generated. The Potential Environmental Risk Index emphasized significant risks associated with mercury and cadmium at several locations. The study highlights the utility of moss biomonitoring in assessing air pollution and identifying hotspots of contamination. The findings from this study could be beneficial for future biomonitoring research in areas with varying physical and geographical conditions. Full article
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<p>Correlation matrix between the elements of the entire initial data set. X stands for not significant.</p>
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<p>(<b>a</b>) Biplot of PC1 and PC2 denote the first two principal components explaining 56.7% of the variance in the data. (<b>b</b>) Biplot of PC2 and PC3 represent the second and third principal components explaining 21.8% of the variance in the data. Each point, distinguished by a unique combination of color and symbol, represents a sample of one of the four species. Arrows emanate from the origin, representing the variables.</p>
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<p>(<b>a</b>) Biplot of PC1 and PC2 denote the first two principal components explaining 56.7% of the variance in the data. (<b>b</b>) Biplot of PC2 and PC3 represent the second and third principal components explaining 21.8% of the variance in the data. Each point, distinguished by a unique combination of color and symbol, represents a sample of one of the four species. Arrows emanate from the origin, representing the variables.</p>
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<p>PMF analysis factor fingerprint showing the percentage contribution of three identified factors (Factor 1, Factor 2, Factor 3) across various elements measured in the moss samples.</p>
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<p>Comparison of Contamination Factors (CF) between current (95 Samples) and previous (120 Samples) moss surveys in Georgia.</p>
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<p>Spatial distribution of the Pollution Load Index (PLI) across all sampling locations. The PLI is represented by colored dots on the map, with different colors indicating varying levels of pollution. Each dot corresponds to a specific sampling site, numbered for reference purposes.</p>
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<p>Boxplots of the Potential Ecological Risk Index (PERI) for selected elements accumulated by the mosses.</p>
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<p>Map of sampling locations with color-coded markers to indicate moss species collected. Red dots indicate <span class="html-italic">Abietinella abietina</span>, green—<span class="html-italic">Hylocomium splendens</span>, yellow—<span class="html-italic">Hypnum cupressiforme</span>, and blue—<span class="html-italic">Pleurozium schreberi</span>.</p>
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22 pages, 16197 KiB  
Article
Accounting for Climate and Inherent Soil Quality in United Nations (UN) Land Degradation Analysis: A Case Study of the State of Arizona (USA)
by Elena A. Mikhailova, Hamdi A. Zurqani, Lili Lin, Zhenbang Hao, Christopher J. Post, Mark A. Schlautman, Gregory C. Post and George B. Shepherd
Climate 2024, 12(12), 194; https://doi.org/10.3390/cli12120194 - 21 Nov 2024
Viewed by 1062
Abstract
Climate change and land degradation (LD) are some of the most critical challenges for humanity. Land degradation (LD) is the focus of the United Nations (UN) Convention to Combat Desertification (UNCCD) and the UN Sustainable Development Goal (SDG 15: Life on Land). Land [...] Read more.
Climate change and land degradation (LD) are some of the most critical challenges for humanity. Land degradation (LD) is the focus of the United Nations (UN) Convention to Combat Desertification (UNCCD) and the UN Sustainable Development Goal (SDG 15: Life on Land). Land degradation is composed of inherent and anthropogenic LD, which are both impacted by inherent soil quality (SQ) and climate. Conventional LD analysis does not take into account inherent SQ because it is not the result of land use/land cover change (LULC), which can be tracked using remote sensing platforms. Furthermore, traditional LD analysis does not link anthropogenic LD to climate change through greenhouse gas (GHG) emissions. This study uses one of the indicators for LD for SDG 15 (15.3.1: Proportion of land that is degraded over the total land area) to demonstrate how to account for inherent SQ in anthropogenic LD with corresponding GHG emissions over time using the state of Arizona (AZ) as a case study. The inherent SQ of AZ is skewed towards low-SQ soils (Entisols: 29.3%, Aridisols: 49.4%), which, when combined with climate, define the inherent LD status. Currently, 8.6% of land in AZ has experienced anthropogenic LD primarily because of developments (urbanization) (42.8%) and agriculture (32.2%). All six soil orders have experienced varying degrees of anthropogenic LD. All land developments in AZ can be linked to damages from LD, with 4862.6 km2 developed, resulting in midpoint losses of 8.7 × 1010 kg of total soil carbon (TSC) and a midpoint social cost of carbon dioxide emissions (SC-CO2) of $14.7B (where B = billion = 109, USD). Arizona was not land degradation neutral (LDN) based on an increase (+9.6%) in the anthropogenic LD overall and an increase in developments (+29.5%) between 2001 and 2021. Considering ongoing climate change impacts in AZ, this increase in urbanization represents reverse climate change adaptation (RCCA) because of the increased population. The state of AZ has 82.0% of the total state area for nature-based solutions (NBS). However, this area is dominated by soils with inherently low SQ (e.g., Entisols, Aridisols, etc.), which complicates efforts for climate change adaptation. Full article
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<p>Anthropogenic land degradation (LD) can be defined as the total of the individual amounts of barren, developed, and agricultural land covers, which are directly linked to inherent soil quality (SQ) and impacted by climate (adapted from Mikhailova et al. 2024 [<a href="#B7-climate-12-00194" class="html-bibr">7</a>]).</p>
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<p>Arizona (AZ) (USA) soil map (31°20′ N to 37° N; 109°03′ W to 114°49′ W) acquired from the SSURGO soils spatial database [<a href="#B12-climate-12-00194" class="html-bibr">12</a>]. The inherent soil quality (soil suitability) of AZ is dominated by slightly weathered Entisols (29.3%) and moderately weathered Aridisols (49.4%).</p>
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<p>Flowchart of geospatial analysis used in this study. Analysis was completed using ArcGIS Pro 2.6 software. Land cover change analysis used the raster calculator to compute differences between satellite remote sensing datasets from 2001 and 2021 (Multi-Resolution Land Characteristics Consortium (MRLC) [<a href="#B25-climate-12-00194" class="html-bibr">25</a>]). The resulting change raster was converted to vector format using the raster to polygon tool and then unioned with the vector soil spatial data (SSURGO) [<a href="#B12-climate-12-00194" class="html-bibr">12</a>] using the union tool. The land cover change/soils dataset was combined with the vector administrative units using the intersect tool, which were subsequently tabulated for soil and land cover change areas.</p>
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<p>Land cover map of the state of Arizona (AZ) (USA) for 2021 (31°20′ N to 37° N; 109°03′ W to 114°49′ W) (based on data from MRLC [<a href="#B25-climate-12-00194" class="html-bibr">25</a>]).</p>
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<p>Anthropogenically degraded land proportion (%) by county for the state of Arizona (AZ) (USA) in 2021. The amount of anthropogenically degraded land was calculated as the total of degraded land from agriculture (cultivated crops and hay/pasture), from development (developed, high intensity; developed, medium intensity; developed, low intensity; developed, open space), and barren land. This figure shows the status of anthropogenic land degradation in 2021, but it is unlikely to include historical anthropogenic land degradation along with the bulk of the inherent land degradation.</p>
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<p>Proportion of land (%) that could potentially be used for nature-based solutions (NBS) by county in the state of Arizona (AZ) (USA) in 2021. Potential land available for NBS is defined by barren land, shrub/scrub, and herbaceous land cover classes to provide potential land areas without impacting other land uses. Almost 85% of the NBS total area is composed of soils with low soil quality (SQ) (Entisols and Aridisols) that are likely not suitable for NBS despite their wide occurrence in AZ. Land availability for NBS in AZ is further limited by private land ownership.</p>
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<p>Damages from land degradation from recent land developments between 2001 and 2021 in Arizona (AZ) (USA): (<b>a</b>) soil organic carbon (SOC) loss (kg of C), (<b>b</b>) soil inorganic carbon (SIC) loss (kg of C), (<b>c</b>) total soil carbon (TSC) loss (kg of C), and (<b>d</b>) related emissions from TSC loss with midpoint “realized” social costs of soil carbon (C) (SC-CO<sub>2</sub>) based on an Environmental Protection Agency (EPA)-calculated SC-CO<sub>2</sub> of <span>$</span>46 per metric ton of CO<sub>2</sub> [<a href="#B23-climate-12-00194" class="html-bibr">23</a>]. Note: M = million = 10<sup>6</sup>, B = billion = 10<sup>9</sup>, <span>$</span> = United States dollar (USD).</p>
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<p>Damages from land degradation from the loss of potential land for soil carbon (C) sequestration from (<b>a</b>) past land developments that occurred before and up through 2021, and (<b>b</b>) recent developments between 2001 and 2021 for Arizona (AZ) (USA).</p>
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<p>Total land degradation (LD), as newly proposed, is the total of the individual amounts of inherent (“natural”) LD and anthropogenic LD (barren, developed, and agricultural land covers), which are directly linked to inherent soil quality (SQ) and impacted by climate and climate change (adapted from Mikhailova et al. 2024 [<a href="#B7-climate-12-00194" class="html-bibr">7</a>]). Anthropogenic LD generates costs associated with damages.</p>
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34 pages, 41034 KiB  
Article
The Dynamics of Air Pollution in the Southwestern Part of the Caspian Sea Basin (Based on the Analysis of Sentinel-5 Satellite Data Utilizing the Google Earth Engine Cloud-Computing Platform)
by Vladimir Tabunshchik, Aleksandra Nikiforova, Nastasia Lineva, Polina Drygval, Roman Gorbunov, Tatiana Gorbunova, Ibragim Kerimov, Cam Nhung Pham, Nikolai Bratanov and Mariia Kiseleva
Atmosphere 2024, 15(11), 1371; https://doi.org/10.3390/atmos15111371 - 14 Nov 2024
Viewed by 620
Abstract
The Caspian region represents a complex and unique system of terrestrial, coastal, and aquatic environments, marked by an exceptional landscape and biological diversity. This diversity, however, is increasingly threatened by substantial anthropogenic pressures. One notable impact of this human influence is the rising [...] Read more.
The Caspian region represents a complex and unique system of terrestrial, coastal, and aquatic environments, marked by an exceptional landscape and biological diversity. This diversity, however, is increasingly threatened by substantial anthropogenic pressures. One notable impact of this human influence is the rising concentration of pollutants atypical for the atmosphere. Advances in science and technology now make it possible to detect certain atmospheric pollutants using remote Earth observation techniques, specifically through data from the Sentinel-5 satellite, which provides continuous insights into atmospheric contamination. This article investigates the dynamics of atmospheric pollution in the southwestern part of the Caspian Sea basin using Sentinel-5P satellite data and the cloud-computing capabilities of the Google Earth Engine (GEE) platform. The study encompasses an analysis of concentrations of seven key pollutants: nitrogen dioxide (NO2), formaldehyde (HCHO), carbon monoxide (CO), ozone (O3), sulfur dioxide (SO2), methane (CH4), and the Aerosol Index (AI). Spatial and temporal variations in pollution fields were examined for the Caspian region and the basins of the seven rivers (key areas) flowing into the Caspian Sea: Sunzha, Sulak, Ulluchay, Karachay, Atachay, Haraz, and Gorgan. The research methodology is based on the use of data from the Sentinel-5 satellite, SRTM DEM data on absolute elevations, surface temperature data, and population density data. Data processing is performed using the Google Earth Engine cloud-computing platform and the ArcGIS software suite. The main aim of this study is to evaluate the spatiotemporal variability of pollutant concentration fields in these regions from 2018 to 2023 and to identify the primary factors influencing pollution distribution. The study’s findings reveal that the Heraz and Gorgan River basins have the highest concentrations of nitrogen dioxide and Aerosol Index levels, marking these basins as the most vulnerable to atmospheric pollution among those assessed. Additionally, the Gorgan basin exhibited elevated carbon monoxide levels, while the highest ozone concentrations were detected in the Sunzha basin. Our temporal analysis demonstrated a substantial influence of the COVID-19 pandemic on pollutant dispersion patterns. Our correlation analysis identified absolute elevation as a key factor affecting pollutant distribution, particularly for carbon monoxide, ozone, and aerosol indices. Population density showed the strongest correlation with nitrogen dioxide distribution. Other pollutants exhibited more complex distribution patterns, influenced by diverse mechanisms associated with local emission sources and atmospheric dynamics. Full article
(This article belongs to the Special Issue Study of Air Pollution Based on Remote Sensing (2nd Edition))
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<p>Geographic location of the study area.</p>
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<p>Overall methodology for air pollution assessment and the evaluation of its relationship with geographical factors.</p>
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<p>Distribution of Aerosol Index: (<b>a</b>) 2018, (<b>b</b>) 2019, (<b>c</b>) 2020, (<b>d</b>) 2021, (<b>e</b>) 2022, and (<b>f</b>) 2023.</p>
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<p>Distribution of Aerosol Index: (<b>a</b>) 2018, (<b>b</b>) 2019, (<b>c</b>) 2020, (<b>d</b>) 2021, (<b>e</b>) 2022, and (<b>f</b>) 2023.</p>
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<p>Distribution of nitrogen dioxide concentrations: (<b>a</b>) 2018, (<b>b</b>) 2019, (<b>c</b>) 2020, (<b>d</b>) 2021, (<b>e</b>) 2022, and (<b>f</b>) 2023.</p>
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<p>Distribution of ozone concentrations: (<b>a</b>) 2018, (<b>b</b>) 2019, (<b>c</b>) 2020, (<b>d</b>) 2021, (<b>e</b>) 2022, and (<b>f</b>) 2023.</p>
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<p>Distribution of ozone concentrations: (<b>a</b>) 2018, (<b>b</b>) 2019, (<b>c</b>) 2020, (<b>d</b>) 2021, (<b>e</b>) 2022, and (<b>f</b>) 2023.</p>
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<p>Distribution of carbon monoxide concentrations: (<b>a</b>) 2018, (<b>b</b>) 2019, (<b>c</b>) 2020, (<b>d</b>) 2021, (<b>e</b>) 2022, and (<b>f</b>) 2023.</p>
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<p>Distribution of carbon monoxide concentrations: (<b>a</b>) 2018, (<b>b</b>) 2019, (<b>c</b>) 2020, (<b>d</b>) 2021, (<b>e</b>) 2022, and (<b>f</b>) 2023.</p>
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<p>Distribution of formaldehyde concentrations: (<b>a</b>) 2018, (<b>b</b>) 2019, (<b>c</b>) 2020, (<b>d</b>) 2021, (<b>e</b>) 2022, and (<b>f</b>) 2023.</p>
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<p>Distribution of sulfur dioxide concentrations: (<b>a</b>) 2018, (<b>b</b>) 2019, (<b>c</b>) 2020, (<b>d</b>) 2021, (<b>e</b>) 2022, and (<b>f</b>) 2023.</p>
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<p>Distribution of methane concentrations: (<b>a</b>) 2018, (<b>b</b>) 2019, (<b>c</b>) 2020, (<b>d</b>) 2021, (<b>e</b>) 2022, and (<b>f</b>) 2023.</p>
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<p>Distribution of methane concentrations: (<b>a</b>) 2018, (<b>b</b>) 2019, (<b>c</b>) 2020, (<b>d</b>) 2021, (<b>e</b>) 2022, and (<b>f</b>) 2023.</p>
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<p>Intra-annual dynamics of average Aerosol Index concentrations in the river basins of Sunzha, Sulak, Ulluchay, Karachay, Atachay, Haraz, and Gorgan.</p>
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<p>Intra-annual dynamics of average carbon monoxide concentrations in the river basins of Sunzha, Sulak, Ulluchay, Karachay, Atachay, Haraz, and Gorgan.</p>
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<p>Intra-annual dynamics of average formaldehyde concentrations in the river basins of Sunzha, Sulak, Ulluchay, Karachay, Atachay, Haraz, and Gorgan.</p>
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<p>Intra-annual dynamics of average carbon ozone concentrations in the river basins of Sunzha, Sulak, Ulluchay, Karachay, Atachay, Haraz, and Gorgan.</p>
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<p>Intra-annual dynamics of average nitrogen dioxide concentrations in the river basins of Sunzha, Sulak, Ulluchay, Karachay, Atachay, Haraz, and Gorgan.</p>
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<p>Intra-annual dynamics of average sulfur dioxide concentrations in the river basins of Sunzha, Sulak, Ulluchay, Karachay, Atachay, Haraz, and Gorgan.</p>
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<p>Correlation diagrams between pollution indicators and geographic factors in the Caspian region: (<b>a</b>) 2019, (<b>b</b>) 2020, (<b>c</b>) 2021, and (<b>d</b>) 2022.</p>
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<p>Correlation diagrams between pollution indicators and geographic factors in the Sunzha River basin: (<b>a</b>) 2019, (<b>b</b>) 2020, (<b>c</b>) 2021, and (<b>d</b>) 2022.</p>
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<p>Correlation diagrams between pollution indicators and geographic factors in the Sulak River basin: (<b>a</b>) 2019, (<b>b</b>) 2020, (<b>c</b>) 2021, and (<b>d</b>) 2022.</p>
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<p>Correlation diagrams between pollution indicators and geographic factors in the Ulluchay River basin: (<b>a</b>) 2019, (<b>b</b>) 2020, (<b>c</b>) 2021, and (<b>d</b>) 2022.</p>
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<p>Correlation diagrams between pollution indicators and geographic factors in the Karachay River basin: (<b>a</b>) 2019, (<b>b</b>) 2020, (<b>c</b>) 2021, and (<b>d</b>) 2022.</p>
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<p>Correlation diagrams between pollution indicators and geographic factors in the Atachay River basin: (<b>a</b>) 2019, (<b>b</b>) 2020, (<b>c</b>) 2021, and (<b>d</b>) 2022.</p>
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<p>Correlation diagrams between pollution indicators and geographic factors in the Haraz River basin: (<b>a</b>) 2019, (<b>b</b>) 2020, (<b>c</b>) 2021, and (<b>d</b>) 2022.</p>
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<p>Correlation diagrams between pollution indicators and geographic factors in the Gorgan River basin: (<b>a</b>) 2019, (<b>b</b>) 2020, (<b>c</b>) 2021, and (<b>d</b>) 2022.</p>
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<p>Average Aerosol Index values from 2018 to 2023 in the basins of small and medium rivers of the Caspian Sea.</p>
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<p>Average nitrogen dioxide concentrations from 2018 to 2023 in the basins of small- and medium-sized rivers of the Caspian Sea.</p>
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<p>Average tropospheric ozone concentrations from 2018 to 2023 in the basins of small- and medium-sized rivers of the Caspian Sea.</p>
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<p>Average carbon monoxide concentrations in the basins of small- and medium-sized rivers in the Caspian Sea from 2018 to 2023.</p>
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<p>Average formaldehyde concentrations from 2018 to 2023 in the basins of small- and medium-sized rivers in the Caspian Sea region.</p>
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<p>Average sulfur dioxide concentrations in the basins of small- and medium-sized rivers in the Caspian Sea from 2018 to 2023.</p>
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19 pages, 534 KiB  
Review
A Comprehensive Review of CO2 Mineral Sequestration Methods Using Coal Fly Ash for Carbon Capture, Utilisation, and Storage (CCUS) Technology
by Alicja Uliasz-Bocheńczyk
Energies 2024, 17(22), 5605; https://doi.org/10.3390/en17225605 - 9 Nov 2024
Viewed by 783
Abstract
CO2 emissions from fossil fuel combustion are the main source of anthropogenic greenhouse gases (GHGs). A method of reducing CO2 emissions is CCUS (carbon capture, utilisation, and storage) technology. One part of CCUS technology involves mineral sequestration as its final stage, [...] Read more.
CO2 emissions from fossil fuel combustion are the main source of anthropogenic greenhouse gases (GHGs). A method of reducing CO2 emissions is CCUS (carbon capture, utilisation, and storage) technology. One part of CCUS technology involves mineral sequestration as its final stage, utilisation, which can be carried out using natural raw materials or waste. This is a particularly interesting option for power and CHP plants that use coal as their primary fuel. Combustion processes produce fly ash as a waste by-product, which has a high potential for CO2 sequestration. Calcium fly ash from lignite combustion and fly ash from fluidised bed boilers have particularly high potential due to their high CaO content. Fly ash can be used in the mineral sequestration of CO2 via direct and indirect carbonation. Both methods use CO2 and flue gases. Studies conducted so far have analysed the influence of factors such as temperature, pressure, and the liquid-to-solid (L/S) ratio on the carbonation process, which have shown different effects depending on the ash used and the form of the process. Due to the large differences found in the properties of fly ash, related primarily to the type of fuel and boiler used, the process of mineral CO2 sequestration requires much research into its feasibility on an industrial scale. However, the method is promising for industrial applications due to the possibility of reducing CO2 emissions and, at the same time, recovering waste. Full article
(This article belongs to the Section B3: Carbon Emission and Utilization)
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<p>Proposal to develop CO<sub>2</sub> mineral sequestration research using fly ash.</p>
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