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24 pages, 9635 KiB  
Article
A Novel Adaptive Sand Cat Swarm Optimization Algorithm for Feature Selection and Global Optimization
by Ruru Liu, Rencheng Fang, Tao Zeng, Hongmei Fei, Quan Qi, Pengxiang Zuo, Liping Xu and Wei Liu
Biomimetics 2024, 9(11), 701; https://doi.org/10.3390/biomimetics9110701 (registering DOI) - 15 Nov 2024
Abstract
Feature selection (FS) constitutes a critical stage within the realms of machine learning and data mining, with the objective of eliminating irrelevant features while guaranteeing model accuracy. Nevertheless, in datasets featuring a multitude of features, choosing the optimal feature poses a significant challenge. [...] Read more.
Feature selection (FS) constitutes a critical stage within the realms of machine learning and data mining, with the objective of eliminating irrelevant features while guaranteeing model accuracy. Nevertheless, in datasets featuring a multitude of features, choosing the optimal feature poses a significant challenge. This study presents an enhanced Sand Cat Swarm Optimization algorithm (MSCSO) to improve the feature selection process, augmenting the algorithm’s global search capacity and convergence rate via multiple innovative strategies. Specifically, this study devised logistic chaotic mapping and lens imaging reverse learning approaches for population initialization to enhance population diversity; balanced global exploration and local development capabilities through nonlinear parameter processing; and introduced a Weibull flight strategy and triangular parade strategy to optimize individual position updates. Additionally, the Gaussian–Cauchy mutation strategy was employed to improve the algorithm’s ability to overcome local optima. The experimental results demonstrate that MSCSO performs well on 65.2% of the test functions in the CEC2005 benchmark test; on the 15 datasets of UCI, MSCSO achieved the best average fitness in 93.3% of the datasets and achieved the fewest feature selections in 86.7% of the datasets while attaining the best average accuracy across 100% of the datasets, significantly outperforming other comparative algorithms. Full article
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<p>Flow chart of MSCSO optimization algorithm.</p>
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<p>Comparison of convergence curves of MSCSO and other optimization algorithms for global optimization.</p>
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<p>Comparison of convergence curves of MSCSO and other optimization algorithms for global optimization.</p>
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<p>Average fitness across 15 datasets.</p>
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<p>Average number of features across 15 datasets.</p>
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<p>Average accuracy across 15 datasets.</p>
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<p>Comparison of convergence curves of MSCSO feature selection with other optimization algorithms.</p>
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14 pages, 13165 KiB  
Article
Detection and Monitoring of Mining-Induced Seismicity Based on Machine Learning and Template Matching: A Case Study from Dongchuan Copper Mine, China
by Tao Wu, Zhikun Liu and Shaopeng Yan
Sensors 2024, 24(22), 7312; https://doi.org/10.3390/s24227312 (registering DOI) - 15 Nov 2024
Abstract
The detection and monitoring of mining-induced seismicity are essential for understanding the mechanisms behind earthquakes and mitigating seismic hazards. However, traditional underground seismic monitoring networks for mining-induced seismicity are challenging to install and operate, which has limited their widespread application. In recent years, [...] Read more.
The detection and monitoring of mining-induced seismicity are essential for understanding the mechanisms behind earthquakes and mitigating seismic hazards. However, traditional underground seismic monitoring networks for mining-induced seismicity are challenging to install and operate, which has limited their widespread application. In recent years, an alternative approach has emerged: utilizing dense seismic arrays at the surface to monitor mining-induced seismicity. This paper proposes a rapid and efficient data processing scheme for the detection and monitoring of mining-induced seismicity based on the surface dense array. The proposed workflow includes machine learning-based phase picking and P-wave first-motion-polarity picking, followed by rapid phase association, precise earthquake location, and template matching for detecting small earthquakes to enhance the completeness of the earthquake catalog. Additionally, it also provides focal mechanism solutions for larger mining-induced events. We applied this workflow to the continuous waveform data from 90 seismic stations over a period of 27 days around the Dongchuan Copper Mine, Yunnan Province, China. Our results yielded 1536 high-quality earthquake locations and two focal mechanism solutions for larger events. By analyzing the spatiotemporal distribution of these events, we are able to investigate the mechanisms of the induced seismic clusters near the Shijiangjun and Lanniping deposits. Our findings highlight the excellent monitoring capability and application potential of the workflow based on machine learning and template matching compared with conventional techniques. Full article
(This article belongs to the Special Issue Sensors and Sensing Technologies for Seismic Detection and Monitoring)
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<p>Workflow diagram showing the detection and monitoring of mining-induced earthquakes.</p>
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<p>(<b>a</b>) Location of Dongchuan Copper Mine in China. (<b>b</b>) Distribution of deposits in Dongchuan Copper Mine and seismic stations used in this study. Blue dots indicate the epicenter of the regional network catalog from 2009 to 2021. Abbreviations: SKS, Sikeshu; YKS, Yikeshu; YM, Yinmin; LX, Luoxue; SJJ, Shijiangjun; LNP, Lanniping; BXL, Baixila.</p>
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<p>An example of machine learning-based phase picking. (<b>a</b>) A segment of 30 s waveforms starting from 02:36:30. (<b>b</b>) Probabilities of P-wave phase (blue) and S-wave phase (red). The picking probabilities threshold is set to 0.3 in this study. The event near 20:36:33 can be detected due to its high probability; however, the event within the red rectangle at 02:36:50 cannot be detected.</p>
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<p>(<b>a</b>) The 1D velocity model used for phase association. (<b>b</b>) Travel time–hypocentral distance curves of 856 associated earthquakes.</p>
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<p>Earthquake catalog comparison between (<b>a</b>) phase association, (<b>b</b>) absolute location, (<b>c</b>) relative location, and (<b>d</b>) template matching. Yellow dots indicate the Cu deposits. Red dots indicate the epicenter of seismic events. Open triangles indicate the short-period stations. Green triangles indicate the broadband stations. Black solid triangle indicates the reginal station.</p>
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<p>Magnitude–time plot of seismicity during the entire study period.</p>
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<p>Comparison of magnitude completeness between regional network catalog and dense array catalog obtained in this study.</p>
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<p>High-precision earthquake catalog (same as <a href="#sensors-24-07312-f005" class="html-fig">Figure 5</a>d) around the Dongchuan Copper Mines using a dense seismic array, machine learning, and template matching. (<b>a</b>) Map view. (<b>b</b>) West–east cross-section. (<b>c</b>) North–south cross-section. (<b>d</b>) Enlarged view of SJJ cluster. (<b>e</b>) Enlarged view of LNP cluster. Beach balls indicate the focal mechanism. Yellow dots indicate the Cu deposits. Red dots indicate the epicenter of seismic events. Open triangles indicate the seismic stations.</p>
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<p>(<b>a</b>) The 3D view of the SJJ (red) and LNP (orange) clusters. (<b>b</b>) The projections of the SJJ and LNP clusters on each plane in 3D space.</p>
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<p>Cumulative number of seismicity and seismicity rate per day for (<b>a</b>) SJJ cluster and (<b>b</b>) LNP cluster, respectively.</p>
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22 pages, 10503 KiB  
Article
Dynamics of Changes in the Surface Area of Water Bodies in Subsidence Basins in Mining Areas
by Martyna A. Rzetala, Robert Machowski, Maksymilian Solarski and Mariusz Rzetala
Water 2024, 16(22), 3280; https://doi.org/10.3390/w16223280 - 15 Nov 2024
Viewed by 120
Abstract
The Silesian Upland in southern Poland is known as a place where subsidence processes induced by mining activities occur in an area of nearly 1500 square kilometres, with many water bodies that formed in subsidence basins. This study concerned the dynamics of changes [...] Read more.
The Silesian Upland in southern Poland is known as a place where subsidence processes induced by mining activities occur in an area of nearly 1500 square kilometres, with many water bodies that formed in subsidence basins. This study concerned the dynamics of changes in the occurrence, boundaries and area of water bodies in subsidence basins (using orthoimagery from 1996 to 2023), as well as the assessment of the factors underlying the morphogenetic and hydrogenetic transformations of these basins. Within the subsidence basins covered by the study, water bodies occupied a total area that changed from 9.22 hectares in 1996 to 48.43 hectares in 2003, with a maximum of 52.30 hectares in 2009. The obtained figures testify to the extremely dynamic changes taking place in subsidence basins, which are unprecedented within such short time intervals in the case of other morphogenetic types of lakes and anthropogenic water bodies (for instance, from 1996 to 2003, the basin of the Brantka water body in Bytom underwent a more than two-fold change in its area, with RA values in the range of 54.4% to 131.9). A reflection of the dynamics of short-term changes in the water bodies in question in the period from 1996 to 2023 is the increase in the water area of the three studied water bodies, which was projected by linear regression to range from 0.09 hectares/year to 0.56 hectares/year. The area change trends, as determined by polynomial regression, suggest a slight decrease in the water table within the last few years, as well as within the next few years, for each of the studied basins. Full article
(This article belongs to the Section Hydrology)
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<p>Locations of studied water bodies in subsidence basins on the Silesian Upland: (<b>A</b>)—Poland; (<b>B</b>)—Silesian Upland; ➀—the Brandka water body in Bytom; ➁—the water body in the Szotkówka River valley in Połomia; ➂—the Bory water body in Sosnowiec.</p>
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<p>Conceptual models of water-body functioning in subsidence basins on the Silesian Upland: (<b>A</b>) The Brandka water body in Bytom; (<b>B</b>) the water body in the Szotkówka River valley in Połomia; (<b>C</b>) the Bory water body in Sosnowiec. 1—fluvial silts, sands and gravels (Holocene); 2—glaciofluvial sands and gravels (Pleistocene); 3—glacial sands, gravels and boulders (Pleistocene); 4—silty loam (Pleistocene); 5—silty loam on stratified sands and gravels (Pleistocene); 6—loess (Pleistocene); 7—clays, sandy clays, sands and sandstones (Neogene); 8—light-grey marly dolomites, Diplopora dolomites, ore-bearing dolomites, and banded and wavy-bedded limestones (Middle Triassic); 9—sandstones, coal, shales (Upper Carboniferous); 10—claystones, mudstones and coal (Upper Carboniferous); 11—sandstones, mudstones, conglomerates, claystones and coal (Upper Carboniferous); 12—anthropogenic forms (e.g., embankments and allochthonous sediments filling basins as a result of human activity); 13—water bodies; 14—land surface before the occurrence of continuous and discontinuous deformation processes; 15—groundwater table of the first aquifer; 16—groundwater present in lower aquifers (including those affected by mining drainage); 17—crack lines induced by mining activities; 18—former and modern mine workings; 19—trees and shrubs; 20—herbaceous vegetation; 21—rush vegetation (sedentation); 22—transportation routes; 23—various forms of evaporation; 24—precipitation; 25—surface runoff; 26—inflows (surface and underground, including debris supply); 27—outflows (surface and underground).</p>
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<p>Changes in the area of the Brandka water body from 1996 to 2023 (source: [<a href="#B87-water-16-03280" class="html-bibr">87</a>]; simplified and supplemented): 1—water bodies in subsidence basins; 2—the extent of water bodies in subsidence basins in 2023.</p>
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<p>Changes in the area of the water body in the subsidence basin in the Szotkówka River valley in Połomia from 1996 to 2023 (source: [<a href="#B87-water-16-03280" class="html-bibr">87</a>]; simplified and supplemented): 1—water bodies in subsidence basins; 2—the extent of water bodies in subsidence basins in 2023.</p>
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<p>Destroyed power-line pole within the water body in the Szotkówka River valley in Połomia in 2013 (photo: R. Machowski).</p>
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<p>Changes in the area of the Bory water body in Sosnowiec from 1996 to 2023 (source: [<a href="#B87-water-16-03280" class="html-bibr">87</a>]; simplified and supplemented): 1—water bodies in subsidence basins; 2—the extent of water bodies in subsidence basins in 2023.</p>
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<p>Flooded base of a high-voltage power-line mast and haul road within the Bory water body in Sosnowiec in 2013 (photo: R. Machowski).</p>
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<p>Trends in changes in the area of water bodies in subsidence basins on the Silesian Upland in 1996–2023 determined by linear and polynomial regression. (<b>A</b>) The Brandka water body in Bytom; (<b>B</b>) the water body in the Szotkówka River valley in Połomia; (<b>C</b>) the Bory water body in Sosnowiec.</p>
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17 pages, 6592 KiB  
Article
Determining the Boundaries of Overlying Strata Collapse Above Mined-Out Panels of Zhomart Mine Using Seismic Data
by Sara Istekova, Alexander Makarov, Dina Tolybaeva, Arman Sirazhev and Kuanysh Togizov
Geosciences 2024, 14(11), 310; https://doi.org/10.3390/geosciences14110310 - 15 Nov 2024
Viewed by 125
Abstract
The present article is devoted to the issue of studying the patterns of displacement of superincumbent rock over panels of a mine obtained using advanced seismic technologies, allowing for the study of the boundaries of caving zones in the depths of rock mass. [...] Read more.
The present article is devoted to the issue of studying the patterns of displacement of superincumbent rock over panels of a mine obtained using advanced seismic technologies, allowing for the study of the boundaries of caving zones in the depths of rock mass. A seismic exploration has been performed in local areas of Zhomart mine responsible for the development of Zhaman-Aybat cuprous sandstone deposits in Central Kazakhstan at the stage of repeated mining with pulling of previously non-mined ore pillars and superincumbent rock caving. A 2D field seismic exploration has been accomplished, totaling to 8000-line m of seismic lines using seismic shot point. The survey depth varied from 455 m to 625 m. The state-of-the-art technologies of kinematic and dynamic analysis of wavefield have been widely used during data processing and interpretation targeted at identifying anomalies associated with the structural heterogeneity of the pays and rock mass, engaging modern algorithms and mathematical apparatuses of specialized geodata processing systems. The above effort resulted in new data regarding the location and morphology of the reflectors, characterizing geological heterogeneity of the section, zones of smooth rock displacement, and displacement of strata with significant disturbance of the rocks overlying mined-out productive pay. The potential of the application of modern 2D seismic exploration to studying an underworked zone with altered physical and mechanical properties located over an ore deposit has been assessed. The novelty and practical significance of the research lies in the determination of the boundaries of zones of displacement and superincumbent rock caving over the panels obtained using state-of-the-art technologies of seismic exploration. The deliverables may be used to improve the process of recognizing specific types of technogenic heterogeneities in the rock mass, impacting the efficiency and safety of subsurface ore mining, both for localization and mining monitoring. Full article
(This article belongs to the Section Geophysics)
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<p>Geological section of the Zhaman-Aybat deposit.</p>
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<p>The state of mining operations at Zhomart mine. The areas of re-mining are highlighted in yellow.</p>
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<p>Ground surface subsidence along profile line 1.</p>
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<p>Timewise subsidence above the panels 39 ÷ 43. Start time: 1—re-mining of ore pillars with collapse of overlying strata; 2—escalation of the geomechanical status of the mine; 3—forecast of rock caving and mining activity stoppage.</p>
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<p>Benioff Graph for seismic energy (E) relief from the rock mass. Stars—human-made earthquakes and their energy class (<span class="html-italic">K</span> = <span class="html-italic">lgE</span>). Start time: 2—escalation of the geomechanical status of the mine; 3—forecast of collapse and mining activity stoppage.</p>
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<p>Time cross-section—line 02 (vertical scale—two-way travel time, ms).</p>
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<p>Picking of horizons and main faults along line 02 (<b>left</b>) and line 03 (<b>right</b>). The legend is the same as for <a href="#geosciences-14-00310-f006" class="html-fig">Figure 6</a>.</p>
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<p>VSP P-wave average velocity from wells 216, 219, and 225 (velocity versus depth).</p>
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<p>Isochrone map (<b>a</b>) and structural map (<b>b</b>) of horizon RII (base of Taskuduk Formation sediments).</p>
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<p>Geoseismic section: lines 02 (<b>left</b>) and 03 (<b>right</b>).</p>
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<p>Seismic attribute interpretation of line 2 (time domain). Deep sections: (<b>a</b>) coherence; (<b>b</b>) spectral decomposition.</p>
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<p>Part of seismic line 02 showing zones of hanging of the overlying rock mass in the area of panels 41-40-30-1 (the highlighted yellow dash-dotted line); maximum deflection is monitored in the area of panels 50–51.</p>
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<p>Part of line 02. Interpretation results. Distinguished hanging zone of the superincumbent rock over the mined-out space.</p>
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<p>Profile fragment 02. Interpretation results. Step between panels 41 and 40.</p>
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19 pages, 12300 KiB  
Article
Initial Desorption Characteristics of Gas in Tectonic Coal Under Vibration and Its Impact on Coal and Gas Outbursts
by Maoliang Shen, Zhonggang Huo, Longyong Shu, Can Zhao, Huijie Zhang and Weihua Wang
Processes 2024, 12(11), 2548; https://doi.org/10.3390/pr12112548 - 14 Nov 2024
Viewed by 236
Abstract
The rapid desorption of gas in coal is an important cause of gas over-limit and outbursts. In order to explain the causes of coal and gas outbursts induced by vibration, this paper studies the gas desorption experiments of tectonic coal with different particle [...] Read more.
The rapid desorption of gas in coal is an important cause of gas over-limit and outbursts. In order to explain the causes of coal and gas outbursts induced by vibration, this paper studies the gas desorption experiments of tectonic coal with different particle sizes and different adsorption equilibrium pressures under 0~50 Hz vibration. High-pressure mercury intrusion experiments were used to measure the changes in pore volume and specific surface area of tectonic coal before and after vibration, revealing the control of pore structure changes on the initial desorption capacity of gas. Additionally, from the perspective of energy transformation during coal and gas outbursts, the effect of vibration on the process of coal and gas outbursts in tectonic coal was analyzed. The results showed that tectonic coal has strong initial desorption capacity, desorbing 29.58% to 54.51% of the ultimate desorption volume within 10 min. Vibration with frequencies of 0~50 Hz increased both the gas desorption ratios and desorption volume as the frequency increased. The initial desorption rate also increased with the vibration frequency, and vibration can enhance the initial desorption capacity of tectonic coal and delay the attenuation of desorption rate. Vibration affected the changes in the initial gas desorption rate and desorption rate attenuation coefficient by increasing the pore volume and specific surface area, with the changes in macropores and mesopores primarily affecting the initial desorption rate and 0~10 min desorption ratios, while the changes in micropores and minipores mainly influenced the attenuation rate of the desorption rate. Vibration increased the free gas expansion energy of tectonic coal as the frequency increased. During the incubation and triggering processes of coal and gas outbursts, vibration has been observed to accelerate the fragmentation and destabilisation of the coal body, while simultaneously increasing the gas expansion energy to a point where it reaches the threshold energy necessary for coal transportation, thus inducing and triggering the coal and gas protrusion. The study results elucidate, from an energy perspective, the underlying mechanisms that facilitate the occurrence of coal and gas outbursts, providing theoretical guidance for coal and gas outburst prevention and mine safety production. Full article
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<p>Mesoscopic characteristics of the coal sample.</p>
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<p>Schematic diagram and physical diagram of experimental equipment.</p>
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<p>Gas desorption volume and desorption ratios characteristics of vibrated coal samples with different particle sizes.</p>
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<p>Fitting results and fitting formula of the desorption rate for vibrated tectonic coal with different particle sizes over 0~10 min.</p>
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<p>Variation trends in V<sub>0</sub> and k in vibrated tectonic coal with different particle sizes. (<b>a</b>) Variation trends in the initial desorption rates in vibrated tectonic coal with different particle sizes; (<b>b</b>) variation trends in desorption rate attenuation coefficient in vibrated tectonic coal with different particle sizes.</p>
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<p>Characteristics of gas desorption volume and desorption rate in vibrated tectonic coal under varying adsorption equilibrium pressures.</p>
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<p>Fitting results and fitting formula of desorption rate in vibrated tectonic coal within 0~10 min under different equilibrium pressures.</p>
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<p>Variation trends in initial desorption rate <span class="html-italic">V</span><sub>0</sub> and desorption rate attenuation coefficient k in vibrated tectonic coal under different adsorption equilibrium pressures. (<b>a</b>) Variation trends in the initial desorption rates in vibrated tectonic coal under different adsorption equilibrium pressures; (<b>b</b>) variation trends in desorption rate attenuation coefficient in vibrated tectonic coal under different adsorption equilibrium pressures.</p>
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<p>Pore volume and specific surface area of different pore sizes in vibrated tectonic coal.</p>
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<p>Results of correlation analysis between pore structure characteristic parameters and gas initial desorption capacity characteristic parameters.</p>
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<p>The variation trend of gas expansion energy in vibrated tectonic coal.</p>
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<p>The process of coal and gas outburst induced and stimulated by vibration.</p>
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17 pages, 7989 KiB  
Article
Numerical Investigation of Network-Based Shock Wave Propagation of Designated Methane Explosion Source in Subsurface Mine Ventilation System Using 1D FDM Code
by Sisi Que, Jiaqin Zeng and Liang Wang
Sustainability 2024, 16(22), 9935; https://doi.org/10.3390/su16229935 - 14 Nov 2024
Viewed by 212
Abstract
In coal mining operations, methane explosions constitute a severe safety risk, endangering miners’ lives and causing substantial economic losses, which, in turn, weaken the production efficiency and economic benefits of the mining industry and hinder the sustainable development of the industry. To address [...] Read more.
In coal mining operations, methane explosions constitute a severe safety risk, endangering miners’ lives and causing substantial economic losses, which, in turn, weaken the production efficiency and economic benefits of the mining industry and hinder the sustainable development of the industry. To address this challenge, this article explores the application of decoupling network-based methods in methane explosion simulation, aiming to optimize underground mine ventilation system design through scientific means and enhance safety protection for miners. We used the one-dimensional finite difference method (FDM) software Flowmaster to simulate the propagation process of shock waves from a gas explosion source in complex underground tunnel networks, covering a wide range of scenarios from laboratory-scale parallel network samples to full-scale experimental mine settings. During the simulation, we traced the pressure loss in the propagation of the shock wave in detail, taking into account the effects of pipeline friction, shock losses caused by bends and obstacles, T-joint branching connections, and cross-sectional changes. The results of these two case studies were presented, leading to the following insights: (1) geometric variations within airway networks exert a relatively minor influence on overpressure; (2) the positioning of the vent positively contributes to attenuation effects; (3) rarefaction waves propagate over greater distances than compression waves; and (4) oscillatory phenomena were detected in the conduits connecting to the surface. This research introduces a computationally efficient method for predicting methane explosions in complex underground ventilation networks, offering reasonable engineering accuracy. These research results provide valuable references for the safe design of underground mine ventilation systems, which can help to create a safer and more efficient mining environment and effectively protect the lives of miners. Full article
(This article belongs to the Section Environmental Sustainability and Applications)
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<p>(<b>a</b>) Top view of the Parallel Sample Network schematic. (<b>b</b>) Geometric model for Flowmaster of the Sample Parallel Network from the top view.</p>
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<p>Overpressure history in the case of 8% volumetric concentration methane explosion in the airway with dimensions of both width and height of 0.08 m and 4.25 m in length.</p>
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<p>Surface of pressure, time, and pipe length plots for (<b>a</b>) C17, (<b>b</b>) C2, (<b>c</b>) C5, (<b>d</b>) C8, (<b>e</b>) C9, (<b>f</b>) C4, (<b>g</b>) C13, and (<b>h</b>) C14.</p>
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<p>Surface of pressure, time, and pipe length plots for (<b>a</b>) C17, (<b>b</b>) C2, (<b>c</b>) C5, (<b>d</b>) C8, (<b>e</b>) C9, (<b>f</b>) C4, (<b>g</b>) C13, and (<b>h</b>) C14.</p>
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<p>Pressure distribution in pipe components at 0.065 s (in bar).</p>
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<p>Illustration depicting underground airways at the main experimental mine, Missouri S&amp;T, Rolla, MO.</p>
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<p>Geometric model experimental mine used in Flowmaster.</p>
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<p>Surface of temporal dimensions, pressure, and length plots of (<b>a</b>) C59 (region 1), (<b>b</b>) C9 (region 2), (<b>c</b>) C24 (region 3), (<b>d</b>) C11 (region 4), (<b>e</b>) C31 (region 5), (<b>f</b>) C29 (region 6), (<b>g</b>) C43 (region 7), (<b>h</b>) C50 (region 8), (<b>i</b>) C53 (shaft 1), and (<b>j</b>) C2 (portal 2).</p>
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<p>Surface of temporal dimensions, pressure, and length plots of (<b>a</b>) C59 (region 1), (<b>b</b>) C9 (region 2), (<b>c</b>) C24 (region 3), (<b>d</b>) C11 (region 4), (<b>e</b>) C31 (region 5), (<b>f</b>) C29 (region 6), (<b>g</b>) C43 (region 7), (<b>h</b>) C50 (region 8), (<b>i</b>) C53 (shaft 1), and (<b>j</b>) C2 (portal 2).</p>
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<p>The distribution of pressure in the airway network at (<b>a</b>) 0.039 s for regions 7 and 8, (<b>b</b>) 0.195 s for regions 7 and 8, (<b>c</b>) 0.039 s for regions 1 to 6, and (<b>d</b>) 0.195 s for regions 1 to 6 of the experimental mine (in bar).</p>
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11 pages, 353 KiB  
Article
Damage Effect and Injury Range of Shock Waves in Mine Methane Explosion
by Zhenzhen Jia, Qing Ye, Wei Xiong and Jialin Liu
Methane 2024, 3(4), 584-594; https://doi.org/10.3390/methane3040033 - 14 Nov 2024
Viewed by 183
Abstract
During the process of mining underground coal, the coal emits a large amount of methane into the mining space, which may lead to methane accumulation and exceed explosion safety limits When the methane encounters a fire source, a methane explosion may occur. The [...] Read more.
During the process of mining underground coal, the coal emits a large amount of methane into the mining space, which may lead to methane accumulation and exceed explosion safety limits When the methane encounters a fire source, a methane explosion may occur. The forceful impact caused by a methane explosion in an underground roadway can cause serious damage to the roadway structures and even lead to the collapse of the ventilation system. At the same time, the explosion impact may result in the death of workers and cause physical injury to the surviving workers. Therefore, it is necessary to study the damage effect and injury range of methane explosions. On the basis of the damage criteria and damage characteristics of methane explosions, according to the overpressure distribution of shock waves in the propagation process of a methane explosion, the explosion hazard range is divided into four ranges (from inside to outside): death range, serious injury range, minor injury range, and safety range. Four injury degrees of shock wave overpressure to personal body (slight, medium, serious injury, death), and seven damage degrees of overpressure to structures are also analyzed. The thresholds of their damage (destruction) are determined. On this basis, an experimental system and numerical simulation are constructed to measure damage characteristics, the overpressure value, and the range distance of a methane explosion with different initial explosion intensities. According to the experimental and numerical results, the attenuation formula of a methane explosion shock wave in the propagation process is derived. The research results show that the overpressure and impulse of shock waves are selected as the damage criteria for comprehensive evaluation, and the overpressure criterion is suitable of determining the injury (failure) range over long distances. The four injury ranges are in line with the actual situation and are reasonable. The injury degree also conforms to the medical results, which can be used to guide the injury degree of mine methane explosions. The injury range caused by methane explosions with different initial explosion intensities is reasonable and is basically consistent with the on-site situation. The derived attenuation formula and calculated safety distance are in good agreement with the experimental and numerical results. The research results can provide guidance and help in the escape, rescue, and protection of coal mine underground person. Full article
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<p>Diagram of experimental system for methane explosion. <b><span class="html-italic">Note</span></b>: 1. Methane explosion experiment pipe; 2. Vacuum instrumentation; 3. Methane explosion ignition device; 4. Pumping system; 5. Methane distribution system; 6. Methane explosion pressure measurement system; 7. Flame propagation velocity measurement system; 8. Dynamic value-acquisition and analysis system; 9. Explosion chamber.</p>
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16 pages, 2277 KiB  
Review
Drug Discovery in the Age of Artificial Intelligence: Transformative Target-Based Approaches
by Akshata Yashwant Patne, Sai Madhav Dhulipala, William Lawless, Satya Prakash, Shyam S. Mohapatra and Subhra Mohapatra
Int. J. Mol. Sci. 2024, 25(22), 12233; https://doi.org/10.3390/ijms252212233 - 14 Nov 2024
Viewed by 248
Abstract
The complexities inherent in drug development are multi-faceted and often hamper accuracy, speed and efficiency, thereby limiting success. This review explores how recent developments in machine learning (ML) are significantly impacting target-based drug discovery, particularly in small-molecule approaches. The Simplified Molecular Input Line [...] Read more.
The complexities inherent in drug development are multi-faceted and often hamper accuracy, speed and efficiency, thereby limiting success. This review explores how recent developments in machine learning (ML) are significantly impacting target-based drug discovery, particularly in small-molecule approaches. The Simplified Molecular Input Line Entry System (SMILES), which translates a chemical compound’s three-dimensional structure into a string of symbols, is now widely used in drug design, mining, and repurposing. Utilizing ML and natural language processing techniques, SMILES has revolutionized lead identification, high-throughput screening and virtual screening. ML models enhance the accuracy of predicting binding affinity and selectivity, reducing the need for extensive experimental screening. Additionally, deep learning, with its strengths in analyzing spatial and sequential data through convolutional neural networks (CNNs) and recurrent neural networks (RNNs), shows promise for virtual screening, target identification, and de novo drug design. Fragment-based approaches also benefit from ML algorithms and techniques like generative adversarial networks (GANs), which predict fragment properties and binding affinities, aiding in hit selection and design optimization. Structure-based drug design, which relies on high-resolution protein structures, leverages ML models for accurate predictions of binding interactions. While challenges such as interpretability and data quality remain, ML’s transformative impact accelerates target-based drug discovery, increasing efficiency and innovation. Its potential to deliver new and improved treatments for various diseases is significant. Full article
(This article belongs to the Special Issue Techniques and Strategies in Drug Design and Discovery, 2nd Edition)
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<p>Example of algorithms and classifiers in ML models [<a href="#B4-ijms-25-12233" class="html-bibr">4</a>,<a href="#B5-ijms-25-12233" class="html-bibr">5</a>].</p>
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<p>Example of algorithms and classifiers in ML models for small molecule-based approach drug discovery [<a href="#B9-ijms-25-12233" class="html-bibr">9</a>].</p>
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<p>Example of algorithms and classifiers in ML models for a fragment-based approach to drug discovery [<a href="#B24-ijms-25-12233" class="html-bibr">24</a>].</p>
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<p>Example of Algorithms and Classifiers in ML Models for Structure-Based Approach Drug Discovery [<a href="#B46-ijms-25-12233" class="html-bibr">46</a>].</p>
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25 pages, 2385 KiB  
Article
Toward the Construction of a Sustainable Society: Assessing the Temporal Variations in and Two-Dimensional Decoupling of Carbon Dioxide Emissions in Anhui Province, China
by Kerong Zhang, Liangyu Jiang and Wuyi Liu
Sustainability 2024, 16(22), 9923; https://doi.org/10.3390/su16229923 - 14 Nov 2024
Viewed by 300
Abstract
This study comprehensively assessed carbon dioxide emissions over a span of two decades, from 2000 to 2020, with the decomposition and decoupling analyses considering multiple influence factors across both short-term and long-term dimensions. The results revealed great fluctuations in the decoupling analysis index [...] Read more.
This study comprehensively assessed carbon dioxide emissions over a span of two decades, from 2000 to 2020, with the decomposition and decoupling analyses considering multiple influence factors across both short-term and long-term dimensions. The results revealed great fluctuations in the decoupling analysis index (DAI) for subjected sectors such as natural resource processing, electricity, gas, water, textiles, machinery, and electronics manufacturing. Of note, significantly changed sectoral DAIs were observed in urban traffic and transportation, logistics warehousing, and the postal industry within Anhui Province. In contrast, the DAIs of other sectors and social services exhibited a weak decoupling state in Anhui Province. The industrial sectors responsible for mining and textiles and the energy structure encompassing electricity, gas, and water emerged as the primary contributors to carbon dioxide emissions. Additionally, the efficiency of the socio-economic development (EDE) was identified as the principal driver of carbon dioxide emissions during the observed period, while the energy consumption intensity (ECI) served as the putative crucial inhibiting factor. The two-dimensional decoupling of carbon dioxide emissions attributable to the EDE demonstrated a gradual transition from industrial sectors to buildings and tertiary industries from 2000 to 2020. In the future, the interaction between urban carbon dioxide emissions and the socio-economic landscape should be optimized to foster integrated social sustainable development in Anhui Province. Full article
(This article belongs to the Section Social Ecology and Sustainability)
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<p>Map of research area (Anhui Province, AH in abbreviation).</p>
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<p>Trends of decoupling index changes for five national economic sectors in Anhui Province from 2000 to 2019.</p>
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<p>Trends of decoupling index changes for five industrial sectors in Anhui Province from 2000 to 2020.</p>
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<p>Trends of DAIs of five national economic sectors in each period.</p>
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<p>Trends of DAIs of the five industrial sectors in each period.</p>
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<p>Decomposition trends of the LMDI of the five national economic sectors in each period.</p>
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<p>LMDI decomposition trends of the five industrial sectors in each period.</p>
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22 pages, 3196 KiB  
Article
Simulation Study of Gas Seepage in Goaf Based on Fracture–Seepage Coupling Field
by Hongsheng Wang, Huaming An and Xin Zhang
Fire 2024, 7(11), 414; https://doi.org/10.3390/fire7110414 - 13 Nov 2024
Viewed by 339
Abstract
In order to solve the problem of gas overrun in the fully mechanized caving face and the upper corner of high gas and extra-thick coal seam, the fracture and caving process of the roof in the goaf is analyzed and studied by using [...] Read more.
In order to solve the problem of gas overrun in the fully mechanized caving face and the upper corner of high gas and extra-thick coal seam, the fracture and caving process of the roof in the goaf is analyzed and studied by using the relevant theories of fracture mechanics and seepage mechanics. The mathematical model of fracture and caving of the immediate roof and main roof in the goaf is established. Combined with ANSYS Fluent 6.3.26, the seepage process of gas in coal and rock accumulation in the goaf under different ventilation modes is simulated. The distribution law of gas concentration in the goaf is obtained, and the application scope of different ventilation modes is determined. In addition, the influence of the tail roadway application and the wind speed size on the gas concentration in the goaf and the upper corner of the fully mechanized caving face is also explored. The results show that, affected by wind speed and rock porosity, along the strike of the goaf, about 30 m near the working face, the gas concentration is low and growth is slow. In the range of 30~160 m, the gas concentration increases rapidly and reaches a higher value. After 160 m, the gas concentration tends to be stable. Along with the tendency of the working face, the gas concentration in the goaf increases gradually from the inlet side to the return side, and the gas concentration increases noticeably near the return air roadway. Along the vertical direction of the goaf, the gas concentration gradually increases, and the concentration of the fracture zone basically reaches 100%. Different ventilation modes have different application scopes. The U-type ventilation mode is suitable for the scenario of less desorption gas in the coal seam, while U + I and U + L-type ventilation modes are suitable for the scenario of more desorption gas in coal seam or higher mining intensity. The application of the tail roadway can reduce the gas concentration in the upper corner to a certain extent, but it has limited influence on the overall gas concentration distribution in the goaf. In addition, when the wind speed of the working face should be controlled at 2.0~3.5 m/s, it is more conducive to the discharge of gas, the method of reducing the gas concentration in the upper corner by increasing the wind speed of the working face is more suitable for the case where the absolute gas emission of the fully mechanized caving face is low, and the effect is limited when the absolute gas emission is high. The above conclusions provide a reference for solving the problem of gas overrun in the goaf and the upper corner of a fully mechanized caving face. Full article
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<p>Division of the three horizontal and vertical zones in goaf.</p>
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<p>Geometric model of working face.</p>
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<p>Geometric model of goaf before initial weighting under U-type ventilation mode.</p>
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<p>Velocity cloud map of roof before initial weighting.</p>
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<p>Velocity vector map of roof before initial weighting.</p>
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<p>Gas concentration distribution map of roof before initial weighting.</p>
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<p>Geometric model of goaf after initial weighting under U-type ventilation mode.</p>
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<p>Distribution cloud map of air leakage velocity in goaf under U-type ventilation mode.</p>
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<p>Gas concentration cloud map when v = 1.5 m/s under U-type ventilation mode: (<b>a</b>) Gas concentration cloud map in goaf from floor z = 3 m; (<b>b</b>) Gas concentration cloud map in goaf from floor z = 10 m; (<b>c</b>) Gas concentration cloud map in vertical direction of goaf.</p>
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<p>Gas concentration cloud map when v = 2.0 m/s under U-type ventilation mode: (<b>a</b>) Gas concentration cloud map in goaf from floor z = 3 m; (<b>b</b>) Gas concentration cloud map in goaf from floor z = 10 m; (<b>c</b>) Gas concentration cloud map in vertical direction of goaf.</p>
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<p>Gas concentration cloud map when v = 2.5 m/s under U-type ventilation mode: (<b>a</b>) Gas concentration cloud map in goaf from floor z = 3 m; (<b>b</b>) Gas concentration cloud map in goaf from floor z = 10 m; (<b>c</b>) Gas concentration cloud map in vertical direction of goaf.</p>
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<p>Curve of gas concentration change in upper corner under U-type ventilation mode.</p>
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<p>Geometric model of goaf under U + I-type ventilation mode.</p>
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<p>Gas concentration in different horizontal sections of goaf under U + I-type ventilation mode: (<b>a</b>) Gas concentration distribution at horizontal section z = 0 m; (<b>b</b>) Gas concentration distribution at horizontal section z = 3 m; (<b>c</b>) Gas concentration distribution at horizontal section z = 8 m.</p>
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<p>Gas concentration in different vertical sections of goaf under U + I-type ventilation mode: (<b>a</b>) Gas concentration distribution at vertical section z = 20 m; (<b>b</b>) Gas concentration distribution at vertical section z = 265 m.</p>
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<p>Geometric model of goaf under U + L-type ventilation mode.</p>
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<p>Gas concentration of different horizontal sections in goaf under U + L-type ventilation mode when air distribution volume is 2:1: (<b>a</b>) Gas concentration distribution at horizontal section z = 0 m; (<b>b</b>) Gas concentration distribution at horizontal section z = 3 m.</p>
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<p>Gas concentration of different horizontal sections in goaf under U + L-type ventilation mode when air distribution volume is 3:1: (<b>a</b>) Gas concentration distribution at horizontal section z = 0 m; (<b>b</b>) Gas concentration distribution at horizontal section z = 3 m.</p>
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<p>Gas concentration of different horizontal sections in goaf under U + L-type ventilation mode when air distribution volume is 4:1: (<b>a</b>) Gas concentration distribution at horizontal section z = 0 m; (<b>b</b>) Gas concentration distribution at horizontal section z = 3 m.</p>
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<p>The curve of gas concentration at 0.5 m away from the working face under U-type ventilation mode.</p>
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<p>The curve of gas concentration at 0.5 m away from the working face under U + I-type ventilation mode.</p>
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<p>The curve of gas concentration at 0.5 m away from the working face under U + L-type ventilation mode.</p>
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<p>Gas concentration curve of goaf cross-section under U + L-type ventilation mode.</p>
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15 pages, 22927 KiB  
Article
Application of Aeromagnetic Survey in Detecting Potential Mineralization Zones Around Dongzhongla Deposit, Gangdese Metallogenic Belt
by Ning Lu, Junfeng Li, Qingmin Meng, Weidong Gao, Junjie Liu, Yongbo Li, Yongzai Xi and Hongshan Zheng
Appl. Sci. 2024, 14(22), 10452; https://doi.org/10.3390/app142210452 - 13 Nov 2024
Viewed by 325
Abstract
The Dongzhongla deposit is a skarn-type lead–zinc ore deposit located in the eastern segment of the Gangdese metallogenic belt, situated in the Xizang province, China. The high-altitude mountainous terrain of the region poses significant challenges to ground-based exploration. To facilitate more accurate mineral [...] Read more.
The Dongzhongla deposit is a skarn-type lead–zinc ore deposit located in the eastern segment of the Gangdese metallogenic belt, situated in the Xizang province, China. The high-altitude mountainous terrain of the region poses significant challenges to ground-based exploration. To facilitate more accurate mineral exploration in the deposit and its surrounding area, a high-resolution airborne magnetic survey was conducted over the mining area and its periphery. The airborne magnetic data were processed using derivative and Euler deconvolution methods, yielding results that reflect the geological structural features of the study area. By integrating the geological characteristics of the ore deposit, we inferred that the areas of magnetic anomaly extensions and the peripheries of other magnetic anomalies are favorable zones for mineralization, providing positive leads for further mineral exploration. Full article
(This article belongs to the Section Earth Sciences)
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<p>The location of the study area and its tectonic outline map (modified from [<a href="#B7-applsci-14-10452" class="html-bibr">7</a>]). (<b>a</b>) The location of the Himalayan orogenic belt. (<b>b</b>) The location of the Gangdese metallogenic belt. (<b>c</b>) The location of the Lhasa terrane and the characteristics of ore deposit distribution. IYZSZ—Yarlung Zangbo suture zone; BNSZ—Bangong–Nujiang suture zone; JSSZ—Jinsha River suture zone; SNMZ—Shiquanhe–Nam Tso Melange zone; LMF—Luobadui–Milashan fault zone; SLS—southern Lhasa subterrane; CLS—central Lhasa subterrane; NLS—northern Lhasa subterrane. DZL—Dongzhongla deposit; LML—Longmala deposit; MYA—Mengya’a deposit; YGL—Yaguila deposit; SR—Sharang deposit.</p>
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<p>A simplified geological map of the study area (modified from a 1:250,000 geological map provided by the client).</p>
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<p>A geological map and geological cross-section of the DZL deposit (modified from data provided by the client). (<b>a</b>) The geological map of the DZL deposit. Points “A” and “B” are the endpoints of the geological section in (<b>b</b>). (<b>b</b>) The geological section crossing the main mining body; the lithology of the geological section is controlled by drill holes, and the ore body develops in the skarn band on the south side of the intrusive rock.</p>
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<p>A satellite image of the study area with overlaid topographic contour lines. The contour interval is 100 m, the number at the star location represents the main peak, and the inverted triangle location represents the elevation of the valley lowlands. The dashed box represents the area of the geological map in <a href="#applsci-14-10452-f003" class="html-fig">Figure 3</a>a.</p>
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<p>The helicopter-borne magnetic survey system used in this survey. CS-VL represents the high-precision cesium vapor magnetometer, GNSS represents the Global Navigation Satellite System, AARC510 is the airborne compensation and recording system used in the project, and Radar represents the radar altimeter.</p>
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<p>The reduced-to-the-pole magnetic field map of the DZL area. The contour map was created based on the gridded reduced-to-magnetic-pole data, with the gridding method being minimum curvature and the grid spacing being 50 m. The contour line spacing on the map is 10 nT. The white dashed lines indicate the approximate extent of the SMAs and BMA.</p>
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<p>The tilt angle map of the DZL area. The purple dashed lines represent the zero value of the tilt angle, which is approximately demarcated by the yellow zero-value line in the grid map.</p>
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<p>Color range symbols’ map of located AN-EUL deconvolution depths of the DZL area. The symbols are overlaid on the tilt angle with 40% transparency. The symbol colors range from cool to warm, and the sizes from small to large represent increasing-in-depth values.</p>
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<p>Color range symbols’ map of located Euler deconvolution depths of the DZL area.</p>
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<p>Forward modeling using Euler deconvolution solutions from the L3400 line. Sus. represents the magnetic susceptibility assigned to a geological unit.</p>
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<p>Proposed exploration zones of the DZL area.</p>
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22 pages, 1648 KiB  
Review
Presence of Potentially Toxic Elements in Historical Mining Areas in the North-Center of Mexico and Possible Bioremediation Strategies
by Victor Manuel Escot-Espinoza, Susana Rodríguez-Márquez, Jorge Briseño-Bugarín, Maria Argelia López-Luna and Juan Armando Flores de la Torre
Toxics 2024, 12(11), 813; https://doi.org/10.3390/toxics12110813 - 13 Nov 2024
Viewed by 726
Abstract
This paper provides an overview of the impacts of mining-related environmental liabilities on humans, soils, sediments, surface water and groundwater across various mining districts in Zacatecas, Mexico. An analysis has been carried out on the areas of the state most affected by the [...] Read more.
This paper provides an overview of the impacts of mining-related environmental liabilities on humans, soils, sediments, surface water and groundwater across various mining districts in Zacatecas, Mexico. An analysis has been carried out on the areas of the state most affected by the presence of potentially toxic elements (PTEs) such as arsenic, lead, cadmium, copper, chromium and zinc, identifying priority areas for environmental assessment and remediation. Likewise, a review of the concentrations of PTEs reported in different environmental matrices of the state’s mining areas with the presence of environmental liabilities was carried out, most of which exceed the maximum permissible limits established by Mexican and international regulations, generating an environmental risk for the populations near these districts due to their potential incorporation into the food chain. Additionally, this study explores research focused on the biostabilization of PTEs using microorganisms with specific metabolic activities. Phytoremediation is presented as a viable tool for the stabilization and elimination of PTEs, in which endemic plants from arid–semi-arid climates have shown favorable results in terms of the phytostabilization and phytoextraction processes of the PTEs present in mining waste. Full article
(This article belongs to the Section Toxicity Reduction and Environmental Remediation)
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<p>Map of the study area showing (<b>a</b>) the main mining districts of the state of Zacatecas, (<b>b</b>) the sediment accumulation zone in the Calera-Francisco I. Madero-Zacatecas valley and (<b>c</b>) the area of the Zacatecas and Vetagrande mining districts and La Zacatecana lagoon.</p>
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<p>Isoconcentration maps generated for (<b>a</b>) As, (<b>b</b>) Pb, (<b>c</b>) Cr, (<b>d</b>) Cd, (<b>e</b>) Cu and (<b>f</b>) Zn using the Kriging interpolation method. The degree of contamination is presented based on the MPL established in Mexico by the Federal Official Gazette (known by its Spanish abbreviation—DOF) and the World Health Organization (WHO) [<a href="#B56-toxics-12-00813" class="html-bibr">56</a>,<a href="#B57-toxics-12-00813" class="html-bibr">57</a>], as well as the probable effect level (PEL) and the interim sediment quality guideline (ISQG) established by the Canadian Council of Miners of the Environment (CEQG) [<a href="#B55-toxics-12-00813" class="html-bibr">55</a>].</p>
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19 pages, 602 KiB  
Article
WKNN-Based Wi-Fi Fingerprinting with Deep Distance Metric Learning via Siamese Triplet Network for Indoor Positioning
by Jae-Hyeon Park, Dongdeok Kim and Young-Joo Suh
Electronics 2024, 13(22), 4448; https://doi.org/10.3390/electronics13224448 - 13 Nov 2024
Viewed by 241
Abstract
Weighted k-nearest neighbor (WKNN)-based Wi-Fi fingerprinting is popular in indoor location-based services due to its ease of implementation and low computational cost. KNN-based methods rely on distance metrics to select the nearest neighbors. However, traditional metrics often fail to capture the complexity of [...] Read more.
Weighted k-nearest neighbor (WKNN)-based Wi-Fi fingerprinting is popular in indoor location-based services due to its ease of implementation and low computational cost. KNN-based methods rely on distance metrics to select the nearest neighbors. However, traditional metrics often fail to capture the complexity of indoor environments and have limitations in identifying non-linear relationships. To address these issues, we propose a novel WKNN-based Wi-Fi fingerprinting method that incorporates distance metric learning. In the offline phase, our method utilizes a Siamese network with a triplet loss function to learn a meaningful distance metric from training fingerprints (FPs). This process employs a unique triplet mining strategy to handle the inherent noise in FPs. Subsequently, in the online phase, the learned metric is used to calculate the embedding distance, followed by a signal-space distance filtering step to optimally select neighbors and estimate the user’s location. The filtering step mitigates issues from an overfitted distance metric influenced by hard triplets, which could lead to incorrect neighbor selection. We evaluate the proposed method on three benchmark datasets, UJIIndoorLoc, Tampere, and UTSIndoorLoc, and compare it with four WKNN models. The results show a mean positioning error reduction of 3.55% on UJIIndoorLoc, 16.21% on Tampere, and 16.49% on UTSIndoorLoc, demonstrating enhanced positioning accuracy. Full article
(This article belongs to the Special Issue Next-Generation Indoor Wireless Communication)
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<p>Overview of our proposed method.</p>
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<p>The Siamese network for distance metric learning. The network learns an embedding space where similar fingerprints are positioned closer together.</p>
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<p>Triplets in the position space and embedding space (A: anchor; N: negative; EP: easy positive; HP: hard positive; EN: easy negative; SHN: semi-hard negative; HN: hard negative).</p>
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<p>Cumulative distribution function of positioning errors with UJIIndoorLoc.</p>
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<p>Cumulative distribution function of positioning errors with Tampere.</p>
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<p>Cumulative distribution function of positioning errors with UTSIndoorLoc.</p>
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22 pages, 14522 KiB  
Article
Spatial Remodeling of Industrial Heritage from the Perspective of Urban Renewal: A Case Study of Coal Mine Site in Jiaozuo City
by Jiahui Ai and Myun Kim
Land 2024, 13(11), 1901; https://doi.org/10.3390/land13111901 - 13 Nov 2024
Viewed by 277
Abstract
Resource-oriented cities are faced with the problems of the decline of traditional industries, exhaustion of resources, and wastage of space. Faced with these problems, urban renewal has become an important role and is widely used in the reuse of old and abandoned spaces. [...] Read more.
Resource-oriented cities are faced with the problems of the decline of traditional industries, exhaustion of resources, and wastage of space. Faced with these problems, urban renewal has become an important role and is widely used in the reuse of old and abandoned spaces. As a historical witness of the industrial revolution and urbanization process, coal mine industrial heritage not only has the value of material heritage but also carries rich historical and cultural information. However, with the adjustment of industrial structure, much coal mine industrial heritage has gradually lost its original production function and become neglected idle space in cities, and industrial buildings and equipment in these spaces have been abandoned or dismantled. The study takes the Wangfeng Mine site in Jiaozuo City, Henan Province as an example, combined with the urban development history and current situation of Jiaozuo city, it discusses the remodeling strategy of industrial heritage space from the perspective of urban renewal. Firstly, through case analysis, historical data sorting, and field research, the study integrated the historical development context of the Jiaozuo coal mine site and its impact on the urban spatial pattern, secondly, discussed the practical problems in the reuse process of industrial sites, and finally proposed specific spatial remodeling strategies based on the conjugation theory. This included determining how to deal with the three pairs of conjugated relations between protection and development, function and ecology, and history and modernity so as to make the spatial remodeling strategy of industrial sites more scientific and sustainable. To promote the sustainable and healthy development of urban industrial heritage space. Full article
(This article belongs to the Section Urban Contexts and Urban-Rural Interactions)
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<p>Park space analysis of Landschaftspark Duisburg-Nord (layout based on data, own elaboration).</p>
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<p>Landschaftspark Duisburg-Nord <a href="https://en.wikipedia.org/wiki/Landschaftspark_Duisburg-Nord" target="_blank">https://en.wikipedia.org/wiki/Landschaftspark_Duisburg-Nord</a> (accessed on 3 October 2010).</p>
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<p>Park space analysis of Mayfield Park (layout based on data, own elaboration).</p>
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<p>Landscape space of Mayfield Park <a href="https://www.dezeen.com/2022/09/30/mayfield-park-studio-egret-west-manchester/" target="_blank">https://www.dezeen.com/2022/09/30/mayfield-park-studio-egret-west-manchester/</a> (accessed on 10 September 2022).</p>
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<p>Park space analysis of Barangaroo Reserve Park (layout based on data, own elaboration).</p>
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<p>Jiaozuo city location. Located in the north of Henan Province, China. Data source: <a href="https://map.tianditu.gov.cn/2020/" target="_blank">https://map.tianditu.gov.cn/2020/</a> (accessed on 1 September 2024).</p>
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<p>(<b>a</b>) Topographic map of Jiaozuo from 1898–1905. Data source: The Formation and Development of Jiaozuo City. History of Jiaozuo, 4th issue, 1985. (<b>b</b>) Early composition of Jiaozuo city (Layout based on data, own elaboration).</p>
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<p>(<b>a</b>) Map of Jiaozuo, 1906–1915. Data source: ≪Jiaozuo Coal Mine≫, Henan People’s Publishing House, 1989. (<b>b</b>) Early composition of Jiaozuo city (layout based on data, own elaboration).</p>
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<p>(<b>a</b>) Map of Jiaozuo, 1916–1925. Data source: ≪Research on Inner Spatial Structure of Jiaozuo City≫ 2007. (<b>b</b>) Early composition of Jiaozuo city (layout based on data, own elaboration).</p>
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<p>(<b>a</b>) Map of Jiaozuo, 1956. Data source: ≪Research on Inner Spatial Structure of Jiaozuo City≫ 2007. (<b>b</b>) Early composition of Jiaozuo city (layout based on data, own elaboration).</p>
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<p>Industrial distribution and urban relation 1925–2010 (layout based on data, own elaboration).</p>
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<p>Aerial view analysis of Wangfeng mine (photo time: September 2024).</p>
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<p>Plane analysis diagram of Wangfeng mine (layout based on data, own elaboration). Photo time: September 2024.</p>
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<p>Industrial heritage transformation strategy based on conjugation theory.</p>
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<p>The balance of the three conjugate relationships.</p>
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<p>Wangfeng mine protection area planning map (layout based on data, own. Elaboration).</p>
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<p>Industrial plant heritage scale change (layout based on data, own. elaboration).</p>
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<p>Wang Feng mine vertical interface simulation diagram (layout based on data, own elaboration).</p>
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<p>(<b>a</b>) Current situation of Wangfeng mine. (<b>b</b>) The modified design drawing (layout based on data, own elaboration).</p>
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<p>(<b>a</b>) Current situation of Wangfeng mine. (<b>b</b>) The modified design drawing (layout based on data, own elaboration).</p>
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14 pages, 4348 KiB  
Article
Impact of Power Quality on the Efficiency of the Mining Process
by Tomasz Siostrzonek, Jakub Wójcik, Mateusz Dutka and Wojciech Siostrzonek
Energies 2024, 17(22), 5675; https://doi.org/10.3390/en17225675 - 13 Nov 2024
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Abstract
There are currently more than 30 underground mines operating in Poland. These are mines extracting hard coal, salt, and metal ores. Each of these plants has its own specifics for operation, but all operate under the same regulations. The basic principle is to [...] Read more.
There are currently more than 30 underground mines operating in Poland. These are mines extracting hard coal, salt, and metal ores. Each of these plants has its own specifics for operation, but all operate under the same regulations. The basic principle is to ensure the safety of the crew and equipment. The progressive mechanization and automation of the mining process results in the installation of power electronic converters in the networks of mining plants, which significantly deteriorate the quality of the power in the plant supply networks. In addition, the constant reconfiguration of these networks related to the progress of the work can affect the safety conditions of the plant. This article describes problems occurring at one underground mining plant that are related to the structure of the power grid. Failures and interruptions in the production process were the result of poor power quality. They directly translated into increased production costs and significantly affected the safety level of the workforce, which could result in further consequences, not only in the financial sphere. The article also addresses the issue of existing legal regulations, the provisions of which may be insufficient in assessing the current state of power quality in mining plants. Full article
(This article belongs to the Special Issue Energy Consumption at Production Stages in Mining)
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<p>A perspective on power quality problems.</p>
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<p>Connection of the energy source to the consumer through a power electronic circuit.</p>
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<p>The waveforms of the three-phase voltages of the MV network.</p>
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<p>Voltage collapse (decrease in voltage value).</p>
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<p>The waveform of phase voltages when the line voltage increases.</p>
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<p>Change in the frequency of phase voltage waveforms in the MV network.</p>
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<p>Disturbance (increase in network voltage).</p>
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<p>The installation sites of recorders used for measurements.</p>
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<p>Diagram of the connection of the recorder at a selected point in the network.</p>
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<p>THD coefficient on the medium voltage side at point P4.</p>
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