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25 pages, 7946 KiB  
Article
Effectiveness of Sorbents in the Equipment of Firefighting Units in Practice
by Miroslav Betuš, Martin Konček, Marian Šofranko, Andrea Rosová, Marek Szücs and Martin Cvoliga
Fire 2024, 7(12), 449; https://doi.org/10.3390/fire7120449 - 29 Nov 2024
Viewed by 505
Abstract
The presented study deals with the effectiveness of sorbents in the equipment of firefighting units in Slovakia. Currently, there are many manufacturers of sorbents on the market and also a number of types of these products. As a result of an emergency on [...] Read more.
The presented study deals with the effectiveness of sorbents in the equipment of firefighting units in Slovakia. Currently, there are many manufacturers of sorbents on the market and also a number of types of these products. As a result of an emergency on the road, especially in the case of traffic accidents, there can be a leakage of dangerous substances. From this point of view, it is necessary to prevent the dangerous substance escaping into the environment as quickly as possible and to choose a suitable sorption material to prevent the leakage. For the stated reasons, the aim of the submitted paper was to research the effectiveness of sorbents used by fire brigades in the Slovak Republic in traffic accidents. Part of the publication is on the specification of sorbents, and as part of the research there is an evaluation of their composition and a description, and according to the method and the successive laboratory tests, the operating fluid that is applied to the selected sorbents. After the test and the resulting values, the initial and absorbed weight of the sorbents were determined. The sorption capacity and absorbency were determined from the resulting values. The time factor and the ability to remove adsorbed sorbents from solid surfaces was evaluated after visualizing the process and the final result. The resulting values were unified and compared with other sorbents, where their suitability for the purposes of firefighting units in practice was determined. Full article
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<p>Vapex (source: elaborated by authors).</p>
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<p>LITE DRY (source: elaborated by authors).</p>
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<p>REOSORB (source: elaborated by authors).</p>
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<p>ECO-DRY (source: elaborated by authors).</p>
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<p>Absodan plus (source: elaborated by authors).</p>
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<p>Spinkleen (source: elaborated by authors).</p>
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<p>Diesel, gasoline, coolant, engine oil, oil + gasoline (source: elaborated by authors).</p>
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<p>Beakers used in research (source: elaborated by authors).</p>
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<p>REOSORB immersed in diesel and after adsorption and dripping (source: elaborated by authors).</p>
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<p>Measuring diesel fuel and determining the initial weight of the sorbent (source: elaborated by authors).</p>
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<p>Sorption process on engine oil (source: elaborated by authors).</p>
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<p>Vapex sorption process with motor gasoline (source: elaborated by authors).</p>
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<p>LITE-DRY immersed in gasoline and after draining (source: elaborated by authors).</p>
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<p>Vapex immersed in engine oil and after draining (source: elaborated by authors).</p>
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<p>REOSORB with coolant and after draining (source: elaborated by authors).</p>
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<p>Absodan, Spilkleen, and ECO-DRY immersed in gasoline and ECO-DRY after dripping (source: elaborated by authors).</p>
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<p>Distribution of sorbents from the point of view of removal (source: elaborated by authors).</p>
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<p>Leaked operating fluids on the road and their backfilling using sorbents (source: elaborated by authors).</p>
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<p>Absorbency of sorbents on operating fluids in % (source: elaborated by authors).</p>
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15 pages, 4301 KiB  
Article
Spatial Distribution of Burned Areas from 1986 to 2023 Using Cloud Computing: A Case Study in Amazonas (Peru)
by Elgar Barboza, Efrain Y. Turpo, Aqil Tariq, Rolando Salas López, Samuel Pizarro, Jhon A. Zabaleta-Santisteban, Angel J. Medina-Medina, Katerin M. Tuesta-Trauco, Manuel Oliva-Cruz and Héctor V. Vásquez
Fire 2024, 7(11), 413; https://doi.org/10.3390/fire7110413 - 13 Nov 2024
Viewed by 954
Abstract
Wildfire represents a significant threat to ecosystems and communities in the Department of Amazonas, Peru, causing losses in biodiversity and land degradation and affecting socioeconomic security. The objective of this study was to analyze the spatial and temporal distribution of burned areas (BAs) [...] Read more.
Wildfire represents a significant threat to ecosystems and communities in the Department of Amazonas, Peru, causing losses in biodiversity and land degradation and affecting socioeconomic security. The objective of this study was to analyze the spatial and temporal distribution of burned areas (BAs) from 1986 to 2023 to identify recurrence patterns and their impact on different types of land use and land cover (LULC). Landsat 5, 7, and 8 satellite images, processed by Google Earth Engine (GEE) using a decision tree approach, were used to map and quantify the affected areas. The results showed that the BAs were mainly concentrated in the provinces of Utcubamba, Luya, and Rodríguez de Mendoza, with a total of 1208.85 km2 burned in 38 years. The most affected land covers were pasture/grassland (38.25%), natural cover (forest, dry forest, and shrubland) (29.55%) and agricultural areas (14.74%). Fires were most frequent between June and November, with the highest peaks in September and August. This study provides crucial evidence for the implementation of sustainable management strategies, fire prevention, and restoration of degraded areas, contributing to the protection and resilience of Amazonian ecosystems against future wildfire threats. Full article
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<p>The Department of Amazonas is located in South America.</p>
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<p>Process of obtaining historical cartography (1986–2023) through cloud computing for the Department of Amazonas.</p>
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<p>Classification of fires in Amazonas on 13 October 2022, (<b>a</b>) SWIR2, NIR, and Red combination, (<b>b</b>) burned area by decision tree classification.</p>
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<p>(<b>a</b>) Mapping of burned areas for Amazonas between 1986 and 2023; (<b>b</b>) cumulative burned areas between 1986 and 2023; (<b>c</b>) annual burned areas between 1986 and 2023; and (<b>d</b>) burned area patterns by month.</p>
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<p>(<b>a</b>) Spatial distribution of fire frequency between 1986 and 2023 in Amazonas, and (<b>b</b>) area burned and proportion of area burned by frequency class.</p>
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<p>(<b>a</b>,<b>b</b>) Spatial distribution of accumulated burned area by LULC type and (<b>c</b>) percentage of accumulated burned area by ecoregion.</p>
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30 pages, 11305 KiB  
Article
A Case Study on the Integration of Remote Sensing for Predicting Complicated Forest Fire Spread
by Pingbo Liu and Gui Zhang
Remote Sens. 2024, 16(21), 3969; https://doi.org/10.3390/rs16213969 - 25 Oct 2024
Viewed by 899
Abstract
Forest fires can occur suddenly and have significant environmental, economic, and social consequences. The timely and accurate evaluation and prediction of their progression, particularly the spread speed in difficult-to-access areas, are essential for emergency management departments to proactively implement prevention strategies and extinguish [...] Read more.
Forest fires can occur suddenly and have significant environmental, economic, and social consequences. The timely and accurate evaluation and prediction of their progression, particularly the spread speed in difficult-to-access areas, are essential for emergency management departments to proactively implement prevention strategies and extinguish fires using scientific methods. This paper provides an analysis of models for predicting forest fire spread in China and globally. Incorporating remote sensing (RS) technology and forest fire science as the theoretical foundation, and utilizing the Wang Zhengfei forest fire spread model (1983), which is noted for its broad adaptability in China as the technical framework, this study constructs a forest fire spread model based on remote sensing interpretation. The model improves the existing model by adding elevation an factor and optimizes the method for acquiring certain parameters. By considering regional landforms (ridge lines, valley lines, and slopes) and vegetation coverage, this paper establishes three-dimensional visual interpretation markers for identifying hotspots; the orientation of the hotspots can be identified to simulate the spread of the fire uphill, downhill, in the direction of the wind, left-level slope, and right-level slope. Then, the data of Sentinel-2 and DEM were used to invert the fuel humidity and slope of pixels in the fire line areas. The statistical inversion data from pixels, which replaced fixed-point values in traditional models, were utilized for predicting forest fire spread speed. In this paper, the model was applied to the case of a forest fire in Mianning County, Sichuan Province, China, and verified using high-time-resolution Himawari-8 data, Gaofen-4 data, and historical data. The results demonstrate that the direction and maximum speed of fire spread for the fire lines in Baifen Mountai, Jiaguer Villageand, Muchanggou, Xujiabaozi, and Zhaizigou are uphill, 16.5 m/min; wind direction, 17.32 m/min; wind direction, 1.59 m/min; and wind direction, 5.67 m/min. The differences are mainly due to the locations of the fire lines, moisture content of combustibles, and maximum slopes being different. Across the entire fire line area, the average rate of increase in the area of open flames within one hour was 3.257 hm2/10 min (square hectares per 10 min), closely matching the average increase rate (3.297 hm2/10 min) monitored by the Himawari-8 satellite in 10 min intervals. In contrast, conventional fixed-point fire spread models predicted an average rate of increase of 3.5637 hm2/10 min, which shows a larger discrepancy compared to the Himawari-8 satellite monitoring results. Moreover, when compared to the fire spot monitoring results from the Gaofen-4 satellite taken 54 min after the initial location of the fire line, the predictions from the RS-enabled fire spread model, which integrates remote sensing interpretations, closely matched the actual observed fire boundaries. Although the predictions from the RS-enabled fire spread model and the traditional model both align with historical data in terms of the overall fire development trends, the RS-enabled model exhibits higher reliability and can provide more accurate information for forest fire emergency departments, enabling effective pre-emptive measures and scientific firefighting strategies. Full article
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<p>Forest fire area in Mianning County, Sichuan, in April 2021.</p>
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<p>Technical route of forest fire spread simulation based on RS interpretation.</p>
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<p>Relationship of temperature and fire spread speed.</p>
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<p>The angle <math display="inline"><semantics> <mrow> <msub> <mrow> <mi mathvariant="sans-serif">α</mi> </mrow> <mrow> <mi mathvariant="normal">N</mi> <mi mathvariant="normal">I</mi> <mi mathvariant="normal">R</mi> </mrow> </msub> </mrow> </semantics></math> formed at the NIR by the reflectance at bands red, NIR, and SWIR1. An additive offset was applied to make spectral values equal at the NIR band (adapted from Shruti Khanna et al. [<a href="#B12-remotesensing-16-03969" class="html-bibr">12</a>]).</p>
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<p>True-color composite image of the Mianning 4.24 forest fire.</p>
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<p>False-color composite image of the Mianning 4.24 forest fire ( numbers 1–6 are the range of fire lines).</p>
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<p>Three-dimensional visualization of the fire scene ( numbers 1–6 are the range of fire lines).</p>
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<p>Normalized vegetation index after error correction.</p>
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<p>The estimated moisture content in combustibles.</p>
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<p>Result of slope extraction from the DEM.</p>
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<p>Prediction of fire line spread distance one hour later.</p>
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<p>Fire area land cover-type map.</p>
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<p>Map of the fire line and Jingkun Expressway locations.</p>
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<p>Dynamic map of the increase in the visible fire area at the Mianning 4.24 forest fire site monitored by the Himawai-8 satellite.</p>
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<p>Himawari-8 remote sensing imagery brightness temperature anomaly monitoring results from 24 April 2021 T03:40 to 24 April 2021 T05:00.</p>
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<p>Himawari-8 remote sensing imagery brightness temperature anomaly monitoring results from 24 April 2021 T03:40 to 24 April 2021 T05:00.</p>
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<p>Comparison of forest fire spread model simulation results and remote sensing monitoring. (<b>a</b>) Forest fire spread simulation results; (<b>b</b>) Himawari-8 remote sensing imagery brightness temperature anomaly monitoring at T03:40; (<b>c</b>) Himawari-8 remote sensing imagery brightness temperature anomaly monitoring at T05:00. (The green line is the Jingkun Expressway; the yellow line is the comparison region).</p>
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<p>Gaofen-4 mid-infrared brightness temperature map.</p>
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<p>Gaofen-4 mid-infrared brightness temperature map (the yellow indicates the boundary of the abnormal brightness temperature).</p>
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<p>Overlaid results of the abnormal brightness temperature boundary and the predicted forest fire spread area (the green line indicates the abnormal brightness temperature boundary; the yellow line indicates the forest fire spread area).</p>
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21 pages, 15871 KiB  
Article
Tracking Forest Disturbance in Northeast China’s Cold-Temperate Forests Using a Temporal Sequence of Landsat Data
by Yueting Wang, Xiang Jia, Xiaoli Zhang, Lingting Lei, Guoqi Chai, Zongqi Yao, Shike Qiu, Jun Du, Jingxu Wang, Zheng Wang and Ran Wang
Remote Sens. 2024, 16(17), 3238; https://doi.org/10.3390/rs16173238 - 1 Sep 2024
Viewed by 1024
Abstract
Cold-temperate forests (CTFs) are not only an important source of wood but also provide significant carbon storage in China. However, under the increasing pressure of human activities and climate change, CTFs are experiencing severe disturbances, such as logging, fires, and pest infestations, leading [...] Read more.
Cold-temperate forests (CTFs) are not only an important source of wood but also provide significant carbon storage in China. However, under the increasing pressure of human activities and climate change, CTFs are experiencing severe disturbances, such as logging, fires, and pest infestations, leading to evident degradation trends. Though these disturbances impact both regional and global carbon budgets and their assessments, the disturbance patterns in CTFs in northern China remain poorly understood. In this paper, the Genhe forest area, which is a typical CTF region located in the Inner Mongolia Autonomous Region, Northeast China (with an area of about 2.001 × 104 km2), was selected as the study area. Based on Landsat historical archived data on the Google Earth Engine (GEE) platform, we used the continuous change detection and classification (CCDC) algorithm and considered seasonal features to detect forest disturbances over nearly 30 years. First, we created six inter-annual time series seasonal vegetation index datasets to map forest coverage using the maximum between-class variance algorithm (OTSU). Second, we used the CCDC algorithm to extract disturbance information. Finally, by using the ECMWF climate reanalysis dataset, MODIS C6, the snow phenology dataset, and forestry department records, we evaluated how disturbances relate to climate and human activities. The results showed that the disturbance map generated using summer (June–August) imagery and the enhanced vegetation index (EVI) had the highest overall accuracy (88%). Forests have been disturbed to the extent of 12.65% (2137.31 km2) over the last 30 years, and the disturbed area generally showed a trend toward reduction, especially after commercial logging activities were banned in 2015. However, there was an unusual increase in the number of disturbed areas in 2002 and 2003 due to large fires. The monitoring of potential widespread forest disturbance due to extreme drought and fire events in the context of climate change should be strengthened in the future, and preventive and salvage measures should be taken in a timely manner. Our results demonstrate that CTF disturbance can be robustly mapped by using the CCDC algorithm based on Landsat time series seasonal imagery in areas with complex meteorological conditions and spatial heterogeneity, which is essential for understanding forest change processes. Full article
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<p>Overview of the study area.</p>
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<p>Forest disturbance analysis workflow.</p>
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<p>Mapping the forest. (<b>a</b>) OTSU value and forest area every year (Summer &amp; EVI); (<b>b</b>) forest cover synthesis map from 1990 to 2021 (Summer &amp; EVI).</p>
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<p>Schematic diagram of typical disturbance types and disturbance processes. (<b>a</b>) Logging in 1999; (<b>b</b>) anthropogenic fire in 2003; (<b>c</b>) wildfires in 2003 and 2010, respectively; (<b>d</b>) logging in 1990 and anthropogenic fire in 2003; (<b>e</b>) EVI curves for the sample points in disturbance areas from (<b>a</b>–<b>d</b>), with red boxes indicating disturbance events.</p>
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<p>Forest disturbance extraction. (<b>a</b>) Forest disturbance zone; (<b>b</b>) disturbance caused by logging after 1990; (<b>c</b>) disturbance caused by man-made fire in 2003; (<b>d</b>) other disturbances caused by multiple factors such as wildfire, etc.; <b>b1</b>–<b>d1</b> show the results of extracting forest disturbance information, <b>b2</b>–<b>d2</b> display the satellite images that correspond to these areas after the disturbance has occurred; (<b>e</b>) forest disturbance zone after fire-induced disturbances have been removed; (<b>f</b>) annual forest disturbance area caused by fires and other factors; the lines in the plot are the univariate linear trendlines.</p>
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<p>Distance of forest disturbance patches from roads and rivers. (<b>a</b>,<b>c</b>) represent the distance of disturbance patches from roads; (<b>b</b>,<b>d</b>) represent the distance of disturbance patches from rivers.</p>
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<p>Number of forest disturbance events. (<b>a</b>) Number of forest disturbance events in Genhe; (<b>b</b>) number of forest disturbance events in each administrative unit.</p>
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<p>The relationship between forest disturbance and its influencing factors. a<sub>i</sub>, b<sub>i</sub>, c<sub>i</sub>, d<sub>i</sub>, and e<sub>i</sub> are models of the area of disturbance and its influencing factors (annual precipitation, annual average temperature, annual snow cover days, the annual number of fires, and annual commercial logging output, respectively) for every year; the pink circles are for the anomalous years (2002 and 2003); the period of (<b>a<sub>1</sub></b>–<b>d<sub>1</sub></b>) is from 1991 to 2020; the period of (<b>a<sub>2</sub></b>–<b>d<sub>2</sub></b>) is from 2011 to 2020; the period of (<b>a<sub>3</sub></b>–<b>c<sub>3</sub></b>) is from 1991 to 2020, the disturbance area of (<b>a<sub>3</sub></b>–<b>c<sub>3</sub></b>) is the disturbance caused by factors other than fire; (<b>d<sub>3</sub></b>) is the model of the disturbance area and burned area for every year from 1991 to 2020; (<b>e<sub>1</sub></b>) annual commercial logging output; the period of (<b>e<sub>2</sub></b>,<b>e<sub>3</sub></b>) is from 1991 to 2015; the disturbance area of (<b>e<sub>3</sub></b>) is the disturbance caused by factors other than fire; the red line in the figure is the univariate linear trendline.</p>
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<p>Time and location of forest disturbance and fires. Note: the blue, pink, and purple areas are the areas where disturbances and fires occurred. It should be noted that the purple areas are areas where disturbances and fires occurred in the same year, and other areas with colors (except white and gray) are all where disturbances were detected but the region of fire did not exist in the auxiliary dataset.</p>
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27 pages, 19132 KiB  
Article
Urban Geomorphology Methods and Applications as a Guideline for Understanding the City Environment
by Alessia Pica, Luca Lämmle, Martina Burnelli, Maurizio Del Monte, Carlo Donadio, Francesco Faccini, Maurizio Lazzari, Andrea Mandarino, Laura Melelli, Archimedes Perez Filho, Filippo Russo, Leonidas Stamatopoulos, Corrado Stanislao and Pierluigi Brandolini
Land 2024, 13(7), 907; https://doi.org/10.3390/land13070907 - 22 Jun 2024
Cited by 5 | Viewed by 1494
Abstract
Cities all over the world have developed on different geological-geomorphological substrates. Different kinds of human activities have operated for millennia as geomorphic agents, generating numerous and various erosion landforms and huge anthropogenic deposits. Considering the increasing demand for land and the expansion of [...] Read more.
Cities all over the world have developed on different geological-geomorphological substrates. Different kinds of human activities have operated for millennia as geomorphic agents, generating numerous and various erosion landforms and huge anthropogenic deposits. Considering the increasing demand for land and the expansion of the built-up areas involving and disturbing any kind of natural system inside and surrounding the actual urban areas, it is not negligible how important the dynamics of the urban environment and its physical evolution are. In this context, this manuscript addresses insights into eight case studies of urban geomorphological analyses of cities in Italy, Greece, and Brazil. The studies are based on surveying and mapping geomorphological processes and landforms in urban areas, supporting both geo-hazard assessment, historical evolution, and paleomorphologies, as well as disseminating knowledge of urban geoheritage and educating about the anthropogenic impact on urban sustainability. We hypothesize that urban geomorphological analysis of several case studies addresses the physical environment of modern cities in a multi-temporal, multidisciplinary, and critical way concerning global changes. Thus, this study aims to illustrate and propose a novel approach to urban geomorphological investigation as a model for the understanding and planning of the physical urban environment on a European and global scale. Full article
(This article belongs to the Section Urban Contexts and Urban-Rural Interactions)
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<p>Location map of the selected case studies. (<b>On the top</b>), a global view of the countries involved; (<b>below left</b>), the 6 Italian cities selected all along the Italian peninsula: Genoa, Perugia, Rome, Pozzuoli, Benevento, and Potenza, and the Greek city—Patras; (<b>below right</b>), the city located in southern Brazil—São João da Barra.</p>
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<p>Schematic drawings of the landform diversity in Rome, focusing on still recognizable natural landforms modified by human activities (<b>a</b>) and anthropogenic landforms of accumulation (<b>b</b>–<b>d</b>), erosion (<b>e</b>), and mixed examples of both (<b>f</b>). In the top right corner, a geomorphological map excerpt and related legend are depicted showing the mapping of the above-mentioned landforms.</p>
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<p>On the left, drainage network modifications and flood prone areas of the morphological amphitheater on which the historic center of Genoa lies. Legend: (1) poorly modified and/or natural riverbed; (2) culverted stream; (3) concrete channel; (4) eaves channel; (5) abandoned channel; (6) exposed buildings; (7) flooding area with returned period &gt; 200 years; and (8) historical flooded area. On the right, the figures show the upper sector of the Lagaccio stream valley affected by relevant man-made morphological modifications: (<b>a</b>) the present-day situation, with the sports facilities on the fills along the stream; (<b>b</b>) the Lagaccio dam lake in the 1960s; and (<b>c</b>) geomorphological section (BH = boreholes).</p>
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<p>(<b>Upper</b>): Geomorphological map of the emerged and submerged coastland of Pozzuoli: 1, La Starza marine terrace rim; 2, retreating shoreline; 3, edge of continental platform: 3a, retreating; 3b, prograding; 4, valley; 5, edge of marine terrace; 6, underwater bar; 7, submerged paleo fan; 8; submerged paleo sea cliff; 9, volcanic rim; 10, underwater cave; 11, sea stack; 12, undersea gas emission; 13 landslide pile; 14, marine terrace; 15, morphostructural depression; 16, gravel; 17, coarse sand; 18, medium sand; 19, fine sand; 20, very fine sand; 21, silt; 22, silt and clay; 23, pyroclastics (Pleistocene-Holocene); 24, submerged tuff (Late Pleistocene-Holocene); 25, reworked pyroclastics, and alluvial and marine deposits (Holocene); 26, submerged archaeological ruins (Roman age). Depth is in meters a.s.l. and the geographic coordinate system is WGS84. (<b>Lower</b>): Geothematic map of the lowering curves of the Phlegraean Fields coastland related to vertical movements between the Greco-Roman period and the present (after [<a href="#B51-land-13-00907" class="html-bibr">51</a>]). Subsidence is in mm/year and the geographic coordinate system is WGS84; DTM Lidar from MATTM—Environmental Remote Sensing Plan (PT-A).</p>
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<p>Patras (urban area), damage recovery on road in coastal zone affected by powerful sea erosion in November 2021.</p>
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<p>Satellite image of 1985 coastline overlapped with the current one, showing the areal gap due to erosion (modified from [<a href="#B69-land-13-00907" class="html-bibr">69</a>]). Below: coastal sector of the municipality of São João da Barra (Rio de Janeiro) consumed by coastal erosion. The yellow dotted line represents the past position of an avenue (N-S view) (Photo: Laboratory of Geomorphology UNICAMP collection, 2023).</p>
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<p>On the left: Geological-stratigraphic structure of the historic center of Potenza (modified from [<a href="#B71-land-13-00907" class="html-bibr">71</a>]). Below left is an old photo from 1857 (with evidence of the earthquake damage), which shows the asymmetric ridge on which Potenza stands and the entire non-urbanized southern side of which the original morphology can be observed. On the right: Geological schematic section and model along the main axis of the Potenza hilltop town (section A-A’, west–east direction), with evidence of the 3 main areas analyzed and the digital model of the top of the clay substrate.</p>
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<p>The slope angle map of Perugia city is on the right of the figure. The map clearly shows the areas with the highest slope angle values (in red), which are all located in the eastern sector of the city or on the eastern facing slope of the fluvial valleys. Additionally, the map indicates areas with a paleomorphological order (black numbered dots) that differs from the current one. All the areas are located close to the downtown area, where the highest and oldest settlement is limited from the ancient Etruscan Wall. On the left side of the image is Grimana square (point 6 in left figure); (<b>a</b>) the initial topographic layout pre-urbanization; (<b>b</b>) the actual topographic layout; (<b>c</b>) volumes of filled material (in red) and eroded areas (in blue).</p>
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<p>(<b>Upper box</b>)—Schematic geomorphological map of the Benevento urban territory. (<b>Lower box</b>)—Simplified maps of the urban expansion of Benevento town from Roman times to the present-day.</p>
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25 pages, 29506 KiB  
Article
All Lives Matter: A Model for Resource Allocation to Fire Departments in Portugal
by Milad K. Eslamzadeh, António Grilo and Pedro Espadinha-Cruz
Fire 2024, 7(6), 206; https://doi.org/10.3390/fire7060206 - 18 Jun 2024
Cited by 1 | Viewed by 977
Abstract
Optimizing Resource Allocation in Fire Departments (RAFD) is crucial for enhancing Fire Protection Services (FPS) and ultimately saving lives. Efficient RAFD ensures that fire departments have the necessary resources to respond effectively to emergencies. This paper presents a method for optimizing RAFD based [...] Read more.
Optimizing Resource Allocation in Fire Departments (RAFD) is crucial for enhancing Fire Protection Services (FPS) and ultimately saving lives. Efficient RAFD ensures that fire departments have the necessary resources to respond effectively to emergencies. This paper presents a method for optimizing RAFD based on performance assessment results, examining its impact on Fire Department (FD) efficiency in Portugal. Evaluating data from 353 FDs, two RAFD optimization methods were assessed: one adhering to Portuguese regulations and constraints, such as budget allocation limitations, and another without such constraints. Integrating a slack-based data envelopment analysis model and mixed-integer linear programming, the study found that incorporating FD efficiency scores in RAFD improved overall efficiency at national, district, and FD levels. While adherence to Portuguese regulations led to balanced resource allocation and a 4% performance improvement at the national level, relaxing constraints yielded an 8% improvement, albeit with potential performance deterioration in some FDs. The detailed budget and efficiency metric analysis provided in this paper offers actionable insights for fire protection services enhancement. This underscores the importance of diverse optimization strategies to enhance FD efficiency, with implications for decision-makers at the Portuguese National Authority for Emergency and Civil Protection and similar organizations globally. Full article
(This article belongs to the Special Issue Combustion and Fire I)
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<p>The PT-RAFD framework-2024, adapted from [<a href="#B9-fire-07-00206" class="html-bibr">9</a>].</p>
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<p>The accessible variables (in green) of the total cost of fire in Portugal.</p>
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<p>(<b>a</b>) The agent-based model implemented in AnyLogic to simulate the travel and response time between PT-FDs and the incidents. (<b>b</b>) Expanded view of an FD (CBV Barcarena) in Lisbon, and utilization of roads by its fire engines.</p>
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<p>The degree of efficiency of PT FDs before and after using PT-RAFD model.</p>
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<p>Number of times efficient FDs appeared as targets for non-efficient FDs in the final dataset, (<b>left</b>): RAFD with using C5; (<b>right</b>): RAFD with relaxing C5.</p>
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<p>Efficiency impact of RAFD with and without C5: (<b>left</b>)—FDs’ efficiency changes post-RAFD implementation; (<b>right</b>)—comparison of RAFD methods on FDs’ efficiency improvement.</p>
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<p>Efficiency changes at the district level with and without using the C5 in PT-RAFD.</p>
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<p>Portuguese districts’ efficiency changes: (<b>left</b>): before RAFD; (<b>middle</b>): after RAFD by using C5; (<b>right</b>): after RAFD by relaxing C5.</p>
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26 pages, 7298 KiB  
Article
Energy Storage Improves Power Plant Flexibility and Economic Performance
by Nenad Sarunac, Javad Khalesi, Mahfuja A. Khuda, Rick Mancini, Pramod Kulkarni and Joel Berger
Energies 2024, 17(11), 2775; https://doi.org/10.3390/en17112775 - 5 Jun 2024
Viewed by 1031
Abstract
Most existing coal-fired power plants were designed for sustained operation at full load to maximize efficiency, reliability, and revenue, as well as to operate air pollution control devices at design conditions. Depending on plant type and design, these plants can adjust output within [...] Read more.
Most existing coal-fired power plants were designed for sustained operation at full load to maximize efficiency, reliability, and revenue, as well as to operate air pollution control devices at design conditions. Depending on plant type and design, these plants can adjust output within a fixed range in response to plant operating or market conditions. The need for flexibility driven by increased penetration of variable and non-dispatchable power generation, such as wind and solar, is shifting the traditional mission profile of thermoelectric power plants in three ways: more frequent shutdowns when market or grid conditions warrant, more aggressive load ramp rates (rate of output change), and a lower minimum sustainable load, which provides a wider operating range and helps avoid costly plant shutdowns. Recent studies have shown that the flexibility of a coal-fired power plant can be improved by energy storage. The objective of this work was to analyze a set of energy storage options and determine their impact on the flexibility and economics of a representative coal-fired power plant. The effect of three energy storage systems integrated with a coal power plant on plant flexibility and economics was investigated. The results obtained in this project show that energy storage systems integrated with a thermal power plant improve plant flexibility and participation in the energy and ancillary services markets, which improves plant financial performance. The study was funded by the U.S. Department Office of Fossil Energy FE-1 under award number DE-FE0031903. Full article
(This article belongs to the Section D: Energy Storage and Application)
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<p>Transient nature of the ESS charging and discharging processes.</p>
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<p>ESS charging and discharging processes during load shift.</p>
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<p>Increase in positive load ramp slope by discharging ESS at the beginning of the load ramp.</p>
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<p>Effect of energy storage charging/discharging on plant load ramp rate.</p>
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<p>EBSILON Professional model of the reference plant with WCC + WCT.</p>
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<p>LP condensate storage system integrated with reference power plant system charging.</p>
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<p>Plant power output as a function of time during charging of the condensate storage tanks.</p>
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<p>Absolute change in the power plant output during LP condensate storage system charging and discharging at minimum and full load.</p>
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<p>Power-to-power roundtrip efficiency <span class="html-italic">η<sub>PP</sub></span> at full load.</p>
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<p>A 2-tank MSS storage system integrated with the reference power plant—system charging.</p>
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<p>Change in power plant output as a function of time during 2-tank MSS storage system charging and discharging at full load.</p>
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<p>Change in plant power output during 2-tank MSS TES system charging and discharging at full load.</p>
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<p>Roundtrip power-to-power and energy-to-energy efficiency vs. feedwater bypass flow.</p>
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<p>Charging and discharging time and flow rate of molten salt vs. feedwater bypass flow.</p>
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<p>Schematic of a FB TES system integrated with the reference plant—system charging.</p>
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<p>HTF temperature at bed exit as a function of the charging time and HTF flow rate.</p>
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<p>Steam extraction and FW bypass flows during FB TES charging and discharging for reference HTF flow of 28 kg/s.</p>
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<p>Change in net power output during the FB TES system charging and discharging for reference HTF flow of 28 kg/s.</p>
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<p>Roundtrip power-to-power efficiency for the design HTF flow of 28 kg/s.</p>
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<p>Levelized earnings for PJM and MISO energy markets for plant capacity factor CF of 50%.</p>
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<p>Annual levelized revenues by category three ESSs described in this paper for the MISO market.</p>
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9 pages, 240 KiB  
Article
Relationship between Simulated Fire Suppression Activities and Acute Cardiac and Respiratory Events in Firefighters
by Roger O. Kollock, William D. Hale, Maddie Fulk, Maddie Seidner, Zora Szabo, Gabriel J. Sanders and Will Peveler
J. Funct. Morphol. Kinesiol. 2024, 9(2), 96; https://doi.org/10.3390/jfmk9020096 - 31 May 2024
Viewed by 1047
Abstract
Cardiac deaths account for the largest share of on-duty firefighter deaths. To help ensure duty fitness and minimize injury risk, many fire departments require the passing of an annual physical ability test, consisting of a battery of simulated fire suppression activities (sFSAs). The [...] Read more.
Cardiac deaths account for the largest share of on-duty firefighter deaths. To help ensure duty fitness and minimize injury risk, many fire departments require the passing of an annual physical ability test, consisting of a battery of simulated fire suppression activities (sFSAs). The purpose of the study was to determine the relationship of sFSA performance to acute cardiac and respiratory events (ACREs) and the effect that estimated VO2max has on sFSA performance. The study was retrospective. As part of an annual physical ability test, five timed sFSAs were performed, summed for a composite time, and categorized into three performance levels (fast, moderate, and slow). Estimated VO2max was determined using the Forestry Step Test. A significant (p = 0.023) linear trend was observed with higher sFSA performance times being associated with a higher proportion of firefighters going on to suffer an ACRE. The estimated VO2max was significantly (p < 0.001) higher in the fast group compared to the slow group. There was not a significant (p = 0.70) difference in estimated VO2max between the moderate and slow groups. Estimated VO2max performance and sFSA performance were significantly correlated, with rs(488) = −0.272 and p < 0.001. Poorer sFSA performance was found to be associated with a higher proportion of ACREs. The results suggest that sFSA performance may be a valid indicator of ACRE injury risk and aerobic capacity. Full article
(This article belongs to the Special Issue Competitive Sports Training and Injury Prevention)
38 pages, 38061 KiB  
Article
Multi-Porous Medium Characterization Reveals Tight Oil Potential in the Shell Limestone Reservoir of the Sichuan Basin
by Guangzhao Zhou, Zanquan Guo, Dongjun Wu, Saihong Xue, Minjie Lin, Wantong Wang, Zihan Zhen and Qingsheng Jin
Processes 2024, 12(6), 1057; https://doi.org/10.3390/pr12061057 - 22 May 2024
Viewed by 876
Abstract
With the continuous deepening of oil and gas exploration and development, unconventional oil and gas resources, represented by tight oil, have become research hotspots. However, few studies have investigated tight oil potential in any systematic way in the shell limestone reservoir of the [...] Read more.
With the continuous deepening of oil and gas exploration and development, unconventional oil and gas resources, represented by tight oil, have become research hotspots. However, few studies have investigated tight oil potential in any systematic way in the shell limestone reservoir of the Sichuan Basin. Herein, we used thin section analysis, X-ray diffraction (XRD), high-pressure mercury intrusion, low-pressure N2 and CO2 adsorption experiments, low-field nuclear magnetic resonance (NMR), focused ion beam–scanning electron microscopy (FIB-SEM), and nano-CT to characterize multi-porous media. The reservoir space controlled by nonfabric, shell, and matrix constitutes all the reservoir space for tight oil. The interconnected porosity was mainly distributed in the range of 1% to 5% (avg. 2.12%). The effective interconnected porosity mainly ranged from 0.5% to 2.0% (avg. 1.59%). The porosity of large fractures was 0.1% to 0.5% (avg. 0.21%). The porosity of isolated pores and bound oil–water pores was 0.2% to 0.8% (avg. 0.44%). The dissolved pores adjacent to fractures, the microfractures controlled by the shell, the microfractures controlled by the matrix, the isolated pores, and the intracrystalline pores constitute five independent pore-throat systems. The development of pores and fractures in shell limestone reservoirs are coupled on the centimeter–millimeter–micron–nanometer scale. Various reservoir-permeability models show continuous distribution characteristics. These findings make an important contribution to the exploration and exploitation of tight oil in shell limestone. Full article
(This article belongs to the Section Energy Systems)
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<p>Geological outline of Da’anzhai Member of the Jurassic in the Sichuan Basin and its stratigraphic information [<a href="#B14-processes-12-01057" class="html-bibr">14</a>].</p>
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<p>The results of pore structure analysis of the X1 and X2 samples. (<b>a</b>). High-pressure mercury intrusion of X1 and X2 samples; (<b>b</b>). CO<sub>2</sub> adsorption of X1 and X2 samples; (<b>c</b>). N<sub>2</sub> adsorption of X1 and X2 samples; (<b>d</b>). Pore size of X1 sample obtained by high-pressure mercury intrusion; (<b>e</b>). Pore structure of X1 sample obtained by CO<sub>2</sub> adsorption; (<b>f</b>). Pore structure of X1 sample obtained by N<sub>2</sub> adsorption; (<b>g</b>). Pore size of X2 sample obtained by high-pressure mercury intrusion; (<b>h</b>). Pore structure of X2 sample obtained by CO<sub>2</sub> adsorption; (<b>i</b>). Pore structure of X1 sample obtained by N<sub>2</sub> adsorption.</p>
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<p>The results of pore structure analysis of the X1 and X2 samples. (<b>a</b>). High-pressure mercury intrusion of X1 and X2 samples; (<b>b</b>). CO<sub>2</sub> adsorption of X1 and X2 samples; (<b>c</b>). N<sub>2</sub> adsorption of X1 and X2 samples; (<b>d</b>). Pore size of X1 sample obtained by high-pressure mercury intrusion; (<b>e</b>). Pore structure of X1 sample obtained by CO<sub>2</sub> adsorption; (<b>f</b>). Pore structure of X1 sample obtained by N<sub>2</sub> adsorption; (<b>g</b>). Pore size of X2 sample obtained by high-pressure mercury intrusion; (<b>h</b>). Pore structure of X2 sample obtained by CO<sub>2</sub> adsorption; (<b>i</b>). Pore structure of X1 sample obtained by N<sub>2</sub> adsorption.</p>
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<p>The results of pore structure analysis of the X1 and X2 samples. (<b>a</b>). High-pressure mercury intrusion of X1 and X2 samples; (<b>b</b>). CO<sub>2</sub> adsorption of X1 and X2 samples; (<b>c</b>). N<sub>2</sub> adsorption of X1 and X2 samples; (<b>d</b>). Pore size of X1 sample obtained by high-pressure mercury intrusion; (<b>e</b>). Pore structure of X1 sample obtained by CO<sub>2</sub> adsorption; (<b>f</b>). Pore structure of X1 sample obtained by N<sub>2</sub> adsorption; (<b>g</b>). Pore size of X2 sample obtained by high-pressure mercury intrusion; (<b>h</b>). Pore structure of X2 sample obtained by CO<sub>2</sub> adsorption; (<b>i</b>). Pore structure of X1 sample obtained by N<sub>2</sub> adsorption.</p>
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<p>The results of pore structure analysis of the X1 and X2 samples. (<b>a</b>). High-pressure mercury intrusion of X1 and X2 samples; (<b>b</b>). CO<sub>2</sub> adsorption of X1 and X2 samples; (<b>c</b>). N<sub>2</sub> adsorption of X1 and X2 samples; (<b>d</b>). Pore size of X1 sample obtained by high-pressure mercury intrusion; (<b>e</b>). Pore structure of X1 sample obtained by CO<sub>2</sub> adsorption; (<b>f</b>). Pore structure of X1 sample obtained by N<sub>2</sub> adsorption; (<b>g</b>). Pore size of X2 sample obtained by high-pressure mercury intrusion; (<b>h</b>). Pore structure of X2 sample obtained by CO<sub>2</sub> adsorption; (<b>i</b>). Pore structure of X1 sample obtained by N<sub>2</sub> adsorption.</p>
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<p>The results of pore structure analysis of the X1 and X2 samples. (<b>a</b>). High-pressure mercury intrusion of X1 and X2 samples; (<b>b</b>). CO<sub>2</sub> adsorption of X1 and X2 samples; (<b>c</b>). N<sub>2</sub> adsorption of X1 and X2 samples; (<b>d</b>). Pore size of X1 sample obtained by high-pressure mercury intrusion; (<b>e</b>). Pore structure of X1 sample obtained by CO<sub>2</sub> adsorption; (<b>f</b>). Pore structure of X1 sample obtained by N<sub>2</sub> adsorption; (<b>g</b>). Pore size of X2 sample obtained by high-pressure mercury intrusion; (<b>h</b>). Pore structure of X2 sample obtained by CO<sub>2</sub> adsorption; (<b>i</b>). Pore structure of X1 sample obtained by N<sub>2</sub> adsorption.</p>
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<p>Micro-scale and nano-scale CT results of X1 and X2 samples. (<b>a</b>). Micro-scale CT scan slice image of X1 sample; (<b>b</b>). Phase segmentation map of X1 sample; (<b>c</b>). Reconstruction of pore network model of X1 sample; (<b>d</b>). Micro-scale CT scan slice image of X2 sample; (<b>e</b>). Phase segmentation map of X2 sample; (<b>f</b>). Reconstruction of pore network model of X2 sample; (<b>g</b>). Nano-scale CT scan slice image of X2 sample; (<b>h</b>). Phase segmentation map of X2 sample; (<b>i</b>). Reconstruction of pore network model of X2 sample.</p>
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<p>The reservoir space controlled by nonfabric in the shell limestone reservoir of the Da’anzhai Member in the Sichuan Basin. (<b>a</b>). X1 well, 2517 m, dissolution fractures, cross-polarized light; (<b>b</b>). X1 well, 2519 m, dissolution pore cavity, cross-polarized light; (<b>c</b>). X1 well, 2522 m, foraminifera, mud crystal, interlayer fracture, cross-polarized light; (<b>d</b>). X1 well, 2518 m, biogenic debris mainly composed of brachiopods, with less foraminifera and gastropoda content and biological erosion within the shell, cross-polarized light; (<b>e</b>). X2 well, 2355 m, flint-filled structural fracture, cross-polarized light; (<b>f</b>). X2 well, 2357 m, interlayer fracture, cross-polarized light; (<b>g</b>). X2 well, 2559 m, structural fracture; (<b>h</b>). X2 well, 2560 m, unfilled tensile crack of mudstone–limestone interbeds developed along the original compression fracture; (<b>i</b>), X2 well, 2565 m, coarse crystalline limestone developed dissolution pore cavity, cross-polarized light.</p>
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<p>The reservoir space controlled by the shell in the shell limestone reservoir of the Da’anzhai Member in the Sichuan Basin. (<b>a</b>). X1 well, 2527 m, oriented arrangement of shells, cross-polarized light; (<b>b</b>). X1 well, 2530 m, shell limestone with developed dissolution fractures between the shells; (<b>c</b>). X2 well, 2566 m, limestone containing biogenic mud crystals, cross-polarized light; (<b>d</b>). X2 well, 2564 m, tabular laumontite crystals filled in intergranular dissolved pores, with intergranular pores developed, SEM; (<b>e</b>). X1 well, 2535 m, interparticle pores between dolomite particles and clay minerals; dolomite particles with good crystalline form; (<b>f</b>). X2 well, 2523.95 m, developed intraparticle pores and interparticle pores in terrestrial minerals; (<b>g</b>). X2 well, angular-shaped intergranular pores in pyrite framboids, 2201.47 m, SEM; (<b>h</b>). X2 well, 2258.85 m, interparticle pores between quartz and calcite; well-developed intraparticle pores within quartz particles, SEM; (<b>i</b>). X1 well, 2548.12 m, intraparticle pores located along cleavage planes of clay particles and interparticle pores between clay and carbonate minerals, SEM.</p>
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<p>The reservoir space controlled by the matrix in the shell limestone reservoir of the Da’anzhai Member in the Sichuan Basin. (<b>a</b>). X2 well, 2566 m, fossiliferous mudstone, intergranular fracture, biogenic debris composed of bivalves, heavily fragmented and recrystallized, with a predominantly muddy matrix, no obvious effect from compaction, cross-polarized light; (<b>b</b>). X2 well, 2569 m, fossiliferous mudstone, biogenic debris composed of large bivalves, affected by wind and waves or water flow, with a gray mud matrix and recrystallization, and small amounts of terrigenous clay, cross-polarized light; (<b>c</b>). X2 well, 2575 m, biogenic debris mainly composed of bivalves, with a small amount of gastropods and foraminifera, matrix is gray mudstone, heavily recrystallized, and contains terrigenous clay, cross-polarized light; (<b>d</b>). X2 well, 2560.6 m, interparticle pores between dolomite particles and clay minerals; dolomite particles with good crystalline form; (<b>e</b>). Well-developed micro-cracks and pores with weak fillings and cements, SEM; (<b>f</b>). Well-developed micro-cracks within matrix minerals with weak filling, SEM; (<b>g</b>). Shell limestone has sutures and is filled with organic matter; (<b>h</b>). Fine-grained biogenic limestone, structural fractures cut the shells vertically, and calcite completely fills the fractures; (<b>i</b>). Fine-grained biogenic limestone. Structural fractures cut through the shells vertically, and calcite completely fills the fractures.</p>
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<p>The T<sub>2</sub> relaxation time of X1 sample.</p>
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<p>Multi-analysis method to identify the multi-porous medium of shell limestone. (<b>a</b>). Double logarithmic pressure recovery curve of typical well test in X1 sample; (<b>b</b>). Typical production curve of the X1 well; (<b>c</b>). The schematic diagram of the seepage characteristics of different pores in the shell limestone of the Da‘anzhai Member.</p>
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<p>Multi-analysis method to identify the multi-porous medium of shell limestone. (<b>a</b>). Double logarithmic pressure recovery curve of typical well test in X1 sample; (<b>b</b>). Typical production curve of the X1 well; (<b>c</b>). The schematic diagram of the seepage characteristics of different pores in the shell limestone of the Da‘anzhai Member.</p>
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<p>SEM of rock samples from the Da’anzhai Member in the central Sichuan Basin. (<b>a</b>). Surface pore rate is 7.6%; (<b>b</b>). Surface pore rate is 8.6%; (<b>c</b>). Surface pore rate is 8.9%; (<b>d</b>). Surface pore rate is 9.9%. The yellow frames in the diagram represent small-scale nanometer pores observed in the SEM.</p>
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<p>Macro-CT scan results of X1 and X2 samples. Light color: high-density area, reflecting the matrix portion; dark color: low-density area, reflecting the pore portion; (<b>a</b>). Macro-CT result of X1 sample; (<b>b</b>). CT slice image of X1 sample; (<b>c</b>). Macro-CT result of X2 sample; (<b>d</b>). CT slice image of X2 sample. The red line represents the x-axis, the blue line represents the y-axis, and the yellow line represents the z-axis.</p>
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<p>Three-dimensional reconstruction and frequency distribution of porosity of X1 and X2 samples. (<b>a</b>). Three-dimensional reconstruction of X1 sample with porosity larger than 5.0%; (<b>b</b>), Three-dimensional reconstruction of X2 sample with porosity larger than 5.0%; (<b>c</b>). Porosity distribution frequency plot of X1 sample obtained by CT; (<b>d</b>). Porosity distribution frequency plot of X2 sample obtained by CT.</p>
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<p>SEM results of X1 and X2 samples. (<b>a</b>). SEM of X1 sample; (<b>b</b>). SEM of X2 sample.</p>
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<p>Nano-scale SEM of X1 and X2 samples. (<b>a</b>). SEM of X1 sample; (<b>b</b>). SEM of X2 sample.</p>
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<p>Nano-scale SEM with development characteristics of fractures of X2 sample. (<b>a</b>). Intergranular microfractures; (<b>b</b>). Calcite grain cleavage fractures.</p>
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<p>Three-dimensional reconstruction of fractures of X1 sample.</p>
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<p>Reservoir-permeability model distribution schematic of shell limestone reservoir in Da’anzhai Member obtained by thin section and CT. (<b>a</b>). Distribution of pore-throat systems in thin sections; (<b>b</b>). Distribution of pore-throat systems in nano-CT. ① Along-fracture dissolution pore type; ② Microfracture type; ③ Isolated pore type; ④ Intergranular pore type.</p>
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<p>SEM of reservoir space in the shell limestone of X1 and X2 samples. (<b>a</b>). X1 well, 2056.3 m, disso-lution holes and dissolution micro-holes; (<b>b</b>). X2 well, 2057 m, shell biofabric pore; (<b>c</b>). X1 well, 2580.9 m, intergranular pores of pyrite; (<b>d</b>). X1 well, 2379.7 m, fragmental grain edge fracture; (<b>e</b>). X1 well, 2672.6 m, inter-shell edge fracture and inter-shell cleavage fracture; (<b>f</b>). X1 well, 2022.2 m, pressure solution fracture line, inter-shell bright calcite.</p>
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<p>Comparison of reservoir-permeability models between shell limestone and tight sandstone. (<b>a</b>). Reservoir-permeability model diagram of tight sandstone; (<b>b</b>). Reservoir-permeability model dia-gram of shell limestone in the Dașanzhai Member.</p>
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18 pages, 1743 KiB  
Review
Analysis of Digital Twins in the Construction Industry: Practical Applications, Purpose, and Parallel with other Industries
by Vanessa Saback, Cosmin Popescu, Thomas Blanksvärd and Björn Täljsten
Buildings 2024, 14(5), 1361; https://doi.org/10.3390/buildings14051361 - 10 May 2024
Viewed by 1781
Abstract
Digital twins (DTs) have become a widely discussed subject, believed to have the potential to solve various problems across different industries, including Engineering & Construction (E&C). However, there is still significant misconception concerning the definition of DTs and their purpose within E&C. This [...] Read more.
Digital twins (DTs) have become a widely discussed subject, believed to have the potential to solve various problems across different industries, including Engineering & Construction (E&C). However, there is still significant misconception concerning the definition of DTs and their purpose within E&C. This study dives deep into identifying DT applications within E&C and the other prominent industries, i.e., Aerospace & Aviation, Manufacturing, Energy & Utilities, Automotive, Healthcare, Smart Cities, Oil & Gas, and Retail. The main challenges to the evolution of DT practical applications are also analyzed. A combination of a literature review, multi-case study analysis, and comparative analysis compose the deployed methodology. Standardization and a maturity level classification are proposed to drive progress of the adoption of DTs. The distinct aspects of the different industries and their assets are evaluated to the conclusion that DTs are better employed for maintenance of structures within E&C. DTs have become a well-worn topic, but the abundance of complex theoretical frameworks is met with simple or inexistent practical applications. Therefore, the novelty of this study lays in its comprehensive analysis of DT applications and real-world implementations—a departure from the often-theoretical discussions surrounding DTs. Full article
(This article belongs to the Special Issue Advances in Digital Construction Management)
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<p>Engineering &amp; Construction industry segments.</p>
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<p>Overview of different industries, the main assets they produce, the respective fabrication time and lifespan of the assets.</p>
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<p>Main purposes of digital twins in other industries.</p>
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<p>Internal challenges: digital transformation in E&amp;C.</p>
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<p>Different levels of digital twins in terms of autonomy, intelligence, learning, and fidelity. Adapted from ARUP [<a href="#B63-buildings-14-01361" class="html-bibr">63</a>].</p>
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16 pages, 5519 KiB  
Review
Current Status of Research on Wildland Fire Impacts on Soil Environment and Soil Organisms and Hotspots Visualization Analysis
by Zhichao Cheng, Song Wu, Dan Wei, Hong Pan, Xiaoyu Fu, Xinming Lu and Libin Yang
Fire 2024, 7(5), 163; https://doi.org/10.3390/fire7050163 - 7 May 2024
Cited by 1 | Viewed by 1370
Abstract
Ecosystems are frequently disturbed by fires that have an important impact on the soil environment and the composition of soil organisms. In order to provide a baseline for the current research and identify trends on the effects of wildland fire on soil environment [...] Read more.
Ecosystems are frequently disturbed by fires that have an important impact on the soil environment and the composition of soil organisms. In order to provide a baseline for the current research and identify trends on the effects of wildland fire on soil environment and biological changes, the available literature was identified from the Web of Science database, covering the period from 1998/1998/1999 (the year of the earliest publication in this field) to 2023. A bibliometric analysis was performed and the data were visually displayed for the number of publications, countries, authors, research institutions, and keywords representing research hotspots. Specifically, the effects of wildland fire on the soil environment, on soil microorganisms and on soil fauna were analyzed. The results show that the annual number of publications describing effects of wildland fire on the soil environment and on soil microorganisms are increasing over time, while those describing effects on soil fauna are fewer and their number remains constant. The largest number of papers originate from the United States, with the United States Department of Agriculture as the research institution with the largest output. The three authors with the largest number of publications are Stefan H. Doerr, Manuel Esteban Lucas-Borja and Jan Jacob Keizer. The research hotspots, as identified by keywords, are highly concentrated on wildfire, fire, organic matter, and biodiversity, amongst others. This study comprehensively analyzes the current situation of the research on the effects of wildland fire on changes in the soil environment and organisms, and provides reference for relevant scientific researchers in this trend and future research hotspots. Full article
(This article belongs to the Special Issue Effects of Fires on Forest Ecosystems)
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<p>Number of annual publications describing effects of wildland fire on the soil environment.</p>
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<p>National co-occurrence mapping of 1770 publications describing effects of wildland fire impacts on the soil environment.</p>
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<p>Author co-occurrence mapping of publications describing effects of wildland fire effects on the soil environment.</p>
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<p>Co-occurrence analysis of high frequency keywords in publications describing effects of the impact of wildland fire on soil environment.</p>
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<p>Number of annual publications describing effects of wildland fire effects on soil microorganisms.</p>
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<p>National co-occurrence mapping of 479 publications describing wildland fire impacts on soil microorganisms.</p>
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<p>Author co-occurrence for publications dealing with wildland fire effects on soil microorganisms.</p>
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<p>High frequency keywords co-occurrence in publications on the impact of wildland fire on soil microorganisms.</p>
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<p>Number of annual publications describing effects of wildland fire effects on the soil fauna.</p>
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<p>National co-occurrence mapping of 139 publications on impact of wildland fire on soil fauna.</p>
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<p>Author co-occurrence mapping for publications on wildland fire effects on soil fauna.</p>
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<p>High frequency keywords co-occurrence related to the impact of wildland fire on soil fauna.</p>
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15 pages, 6621 KiB  
Article
Comparing Machine Learning and Time Series Approaches in Predictive Modeling of Urban Fire Incidents: A Case Study of Austin, Texas
by Yihong Yuan and Andrew Grayson Wylie
ISPRS Int. J. Geo-Inf. 2024, 13(5), 149; https://doi.org/10.3390/ijgi13050149 - 29 Apr 2024
Cited by 2 | Viewed by 1456
Abstract
This study examines urban fire incidents in Austin, Texas using machine learning (Random Forest) and time series (Autoregressive integrated moving average, ARIMA) methods for predictive modeling. Based on a dataset from the City of Austin Fire Department, it addresses the effectiveness of these [...] Read more.
This study examines urban fire incidents in Austin, Texas using machine learning (Random Forest) and time series (Autoregressive integrated moving average, ARIMA) methods for predictive modeling. Based on a dataset from the City of Austin Fire Department, it addresses the effectiveness of these models in predicting fire occurrences and the influence of fire types and urban district characteristics on predictions. The findings indicate that ARIMA models generally excel in predicting most fire types, except for auto fires. Additionally, the results highlight the significant differences in model performance across urban districts, indicating an impact of local features on fire incidence prediction. The research offers insights into temporal patterns of specific fire types, which can provide useful input to urban planning and public safety strategies in rapidly developing cities. In addition, the findings also emphasize the need for tailored predictive models, based on local dynamics and the distinct nature of fire incidents. Full article
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<p>Yearly fire incidents in the ten Austin city council districts.</p>
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<p>Monthly fire occurrence after preprocessing.</p>
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<p>Flowchart of the methodology.</p>
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<p>Predicted values based on a Random Forest model [<a href="#B36-ijgi-13-00149" class="html-bibr">36</a>].</p>
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<p>ARIMA model residuals for all five types of fires.</p>
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<p>Q-Q plots for ARIMA models by fire type.</p>
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<p>Comparing Random Forest and ARIMA.</p>
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<p>Comparing the temporal patterns of small grass fire and auto fire.</p>
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<p>ARIMA model residuals for all districts.</p>
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<p>Q-Q plots for ARIMA models by district.</p>
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<p>Comparing Random Forest and ARIMA by city council district.</p>
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16 pages, 523 KiB  
Article
Evaluation of the Knowledge and Awareness of Firefighters in Turkey in Disaster Risk Management
by Ayşe Ütük and Hayri Baraçlı
Sustainability 2024, 16(9), 3720; https://doi.org/10.3390/su16093720 - 29 Apr 2024
Viewed by 1250
Abstract
Firefighters stand as one of the most effective task forces, striving to minimize losses incurred during disasters. Clarifying the present status of disaster risk management for firefighters can offer insights into the factors influencing response during disasters and how preparedness for such events [...] Read more.
Firefighters stand as one of the most effective task forces, striving to minimize losses incurred during disasters. Clarifying the present status of disaster risk management for firefighters can offer insights into the factors influencing response during disasters and how preparedness for such events can be enhanced. The aim of this study is to assess the current status of fire and rescue services, actively engage in crisis management during disaster risk management, to identify areas for improvement that enhance their involvement in preparatory stages, and to bolster their effectiveness in crisis management. This descriptive, cross-sectional study involved 772 firefighters who had prior experience in disaster response. The findings of this study revealed that firefighters who had undergone first aid training demonstrated the ability to anticipate hazardous situations and behaviors, regularly inspected their equipment, showed awareness of work-related accidents and occupational diseases, and scored statistically higher on the scales. These findings are expected to assist fire departments in establishing a sustainable and comprehensive disaster management cycle. Full article
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<p>Confirmatory factor analysis for the Disaster Risk Management Scale for Firefighters.</p>
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13 pages, 385 KiB  
Article
Knowledge of Infection Prevention and Control and Practice Behaviors among Career and Volunteer Firefighters in Rural Communities
by Edrisa Sanyang, Ashley Adams, Ritchie Taylor, Vernell McDonald, Gretchen Macy and Jacqueline Basham
Merits 2024, 4(2), 146-158; https://doi.org/10.3390/merits4020011 - 10 Apr 2024
Viewed by 1119
Abstract
Due to the emerging threat conditions in the work environment, firefighters are at a high risk of exposure to not only toxic substances but also biological agents in the dayroom and during emergency runs. The aim of this study is to evaluate firefighter [...] Read more.
Due to the emerging threat conditions in the work environment, firefighters are at a high risk of exposure to not only toxic substances but also biological agents in the dayroom and during emergency runs. The aim of this study is to evaluate firefighter (career and volunteer) knowledge and practice behaviors on infection control. This study surveyed 444 firefighters (210 career, 234 volunteer) in rural Northwestern Kentucky. The self-reported survey focused on individual characteristics, knowledge on exposure incident control, precautionary actions, and personal protections. We evaluated the descriptive characteristics of knowledge and practice scores stratified by firefighter groups (career and volunteers). The associations between infection control training received (yes/no) and firefighter knowledge and practice scores were also examined. Firefighters who were trained on infection control prevention had significantly higher knowledge scores (M = 63.7, SD = 13.4 vs. M = 59.7, SD = 15.9; p = 0.012). Volunteer firefighters exhibited better infection control practice behaviors than career firefighters (M = 70.6, SD = 13.0 vs. M = 67.4, SD = 11.1; p = 0.05). Firefighters who followed infection control guidelines (M = 69.5, SD = 11.9 vs. M = 58.1, SD = 9.9; p = 0.012) and expressed need for a comprehensive training on personal protective equipment (PPE) selection (β = 3.41, SE = 1.54, aOR = 30.22, 95% CI: 1.47–620.87; p = 0.028) had significantly higher practice scores compared to those who did not. The study results have policy implications for infection prevention and control (IPC) in rural fire departments, both career and volunteer. A review of infection control policies is needed, especially as it relates to training and practice behaviors during emergency calls and in the dayroom. Results also suggest the need to develop strategies to improve the culture of PPE use and training on the selection of PPEs appropriate to the emergency response type. Full article
(This article belongs to the Special Issue Current Research on Occupational Safety and Health)
26 pages, 8697 KiB  
Article
The Spatial–Temporal Emission of Air Pollutants from Biomass Burning during Haze Episodes in Northern Thailand
by Phakphum Paluang, Watinee Thavorntam and Worradorn Phairuang
Fire 2024, 7(4), 122; https://doi.org/10.3390/fire7040122 - 8 Apr 2024
Cited by 2 | Viewed by 2035
Abstract
Air pollutants from biomass burning, including forest fires and agricultural trash burning, have contributed significantly to the pollution of the Asian atmosphere. Burned area estimates are variable, making it difficult to measure these emissions. Improving emission quantification of these critical air pollution sources [...] Read more.
Air pollutants from biomass burning, including forest fires and agricultural trash burning, have contributed significantly to the pollution of the Asian atmosphere. Burned area estimates are variable, making it difficult to measure these emissions. Improving emission quantification of these critical air pollution sources requires refining methods and collecting thorough data. This study estimates air pollutants from biomass burning, including PMs, NOX, SO2, BC, and OC. Machine learning (ML) with the Random Forest (RF) method was used to assess burned areas in Google Earth Engine. Forest emissions were highest in the upper north and peaked in March and April 2019. Air pollutants from agricultural waste residue were found in the lower north, but harvesting seasons made timing less reliable. Biomass burning was compared to the MODIS aerosol optical depth (AOD) and Sentinel-5P air pollutants, with all comparisons made by the Pollution Control Department (PCD) Thailand air monitoring stations. Agro-industries, mainly sugar factories, produce air pollutants by burning bagasse as biomass fuel. Meanwhile, the emission inventory of agricultural operations in northern Thailand, including that of agro-industry and forest fires, was found to have a good relationship with the monthly average levels of ambient air pollutants. Overall, the information uncovered in this study is vital for air quality control and mitigation in northern Thailand and elsewhere. Full article
(This article belongs to the Special Issue Vegetation Fires and Biomass Burning in Asia)
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<p>Conceptual framework.</p>
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<p>(<b>a</b>) The study area located in northern Thailand. (<b>b</b>) The upper-north boundary. (<b>c</b>) The lower-north boundary.</p>
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<p>(<b>a</b>) Example of map of burned polygons and training data points over the study area. (<b>b</b>) A close view of the black box shown in (<b>a</b>,<b>c</b>). A close view of the black box shown in (<b>a</b>) with the training data point.</p>
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<p>The monthly distribution of burned area during haze episodes in 2019–2021: (<b>a</b>) forests, (<b>b</b>) rice plantations, (<b>c</b>) sugarcane plantations, and (<b>d</b>) corn plantations.</p>
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<p>The Spatial distribution of the burnt area in northern Thailand during haze episodes: (<b>a</b>) 2019, (<b>b</b>) 2020, and (<b>c</b>) 2021.</p>
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<p>Example of map of burned in January 2020 in Chiang Mai. (<b>b</b>) A close view of the red box shown in (<b>a</b>,<b>c</b>). A close view of the red box shown in (<b>a</b>) with Sentinel-2 imagery (B4, B8A, and B11).</p>
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<p>The spatial distribution of the gridded PM<sub>2.5</sub> emissions emitted from forest fire: (<b>a</b>) 2019, (<b>b</b>) 2020, and (<b>c</b>) 2021.</p>
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<p>The spatial distribution of the gridded PM<sub>2.5</sub> emissions emitted from rice waste residues: (<b>a</b>) 2019, (<b>b</b>) 2020, and (<b>c</b>) 2021.</p>
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<p>The spatial distribution of the gridded PM<sub>2.5</sub> emissions emitted from sugarcane waste residues: (<b>a</b>) 2019, (<b>b</b>) 2020, and (<b>c</b>) 2021.</p>
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<p>The spatial distribution of the gridded PM<sub>2.5</sub> emissions emitted from corn waste residues: (<b>a</b>) 2019, (<b>b</b>) 2020, and (<b>c</b>) 2021.</p>
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<p>The amount of sugarcane production and amount of bagasse in 2019–2021 in sugar factories: (<b>a</b>) the amount of sugarcane production and (<b>b</b>) the amount of bagasse.</p>
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<p>The spatial distribution of the gridded PM<sub>2.5</sub> emissions emitted from sugar factories: (grid size of 1 km × 1 km): (<b>a</b>) 2019, (<b>b</b>) 2020, and (<b>c</b>) 2021.</p>
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<p>Monthly average of AOD and monthly air emissions from forest fire and agriculture residues in Chiang Mai Government Center (Chiang Mai-1), including (<b>a</b>) Chiang Mai-1, 2019; (<b>b</b>) Chiang Mai-1, 2020; and (<b>c</b>) Chiang Mai-1, 2021.</p>
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<p>The average AOD and monthly air emissions from forest fire and agriculture residues in Yupparaj Wittayalai School (Chiang Mai-2), which (<b>a</b>). Chiang Mai-2, 2019, (<b>b</b>). Chiang Mai-2, 2020, and (<b>c</b>). Chiang Mai-2, 2021.</p>
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