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Search Results (5,064)

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11 pages, 691 KiB  
Article
Sub-Tenon’s Block in Patients with Previous Encircling Band Surgery—A Feasibility Study
by Johannes Harte, Gesar Ugen, Joana Berger-Estilita, Andreas Ebneter and Friedrich Lersch
J. Clin. Med. 2024, 13(24), 7735; https://doi.org/10.3390/jcm13247735 - 18 Dec 2024
Abstract
Introduction: During the COVID-19 pandemic, reducing aerosol-generating procedures became fundamental, particularly in ophthalmic surgeries traditionally performed under general anesthesia (GA). Regional anesthesia, such as sub-Tenon’s block (STB), is widely used in vitreoretinal surgeries, offering a safer alternative by avoiding airway manipulation. However, the [...] Read more.
Introduction: During the COVID-19 pandemic, reducing aerosol-generating procedures became fundamental, particularly in ophthalmic surgeries traditionally performed under general anesthesia (GA). Regional anesthesia, such as sub-Tenon’s block (STB), is widely used in vitreoretinal surgeries, offering a safer alternative by avoiding airway manipulation. However, the altered orbital anatomy in patients with previous scleral explant surgery creates unique challenges to STB application. This study aims to evaluate the effectiveness, safety, and feasibility of STB in patients after encircling band surgery. Methods: This retrospective analysis included 46 patients with a history of scleral explant surgery, undergoing vitreoretinal procedures at the Bern University Hospital. All procedures were conducted under STB with either analgosedation or GA for additional support when required. An ophthalmic surgeon or an experienced anesthesiologist performed the STBs. Data collected included block success rate, procedural difficulty, incidence of chemosis, and patient satisfaction. The Institutional Ethics Committee approved this study, and all participants provided informed consent. Results: STB was successfully administered in 93.5% of cases, with only three unsuccessful blocks. Block placement was rated as easy in 55% of cases, moderately difficult in 28%, and difficult in 17%. Chemosis was observed in 24% of patients, with severe cases in only 4%. Patient satisfaction scores were high, with most patients expressing satisfaction with the STB procedure. Conversion to GA was required in only one case due to alcohol withdrawal-related agitation. Discussion: The high success rate and minimal complications suggest that STB is a feasible and safe alternative to GA in patients with prior scleral buckling surgery. The altered orbital anatomy presents potential challenges, including scar tissue and compartmentalization, which may lead to patchy anesthesia. However, the use of STB avoids the risks associated with GA and may be especially beneficial for elderly or frail patients. Future studies should further investigate the hemodynamic implications of STB in these cases and the potential for ultrasound-guided techniques to improve accuracy and safety. Full article
(This article belongs to the Special Issue Advances in Regional Anaesthesia and Acute Pain Management)
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Graphical abstract

Graphical abstract
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<p>Comparing sub-Tenon block (STB) cannula trajectory vs. retrobulbar needle trajectory in a previously encircled, elongated eye; bulbar length is a serious risk for sharp-needle injury. The retrobulbar block, in contrast to the STB, penetrates the sclera. Legend: CO = cornea, VB = vitreous body, SB = scleral buckle, ON = optical nerve, RM = rectal muscle, OB = orbital bone.</p>
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<p>Scarring scaled from 1 to 3 (1 = easy, 2 = moderately difficult, 3 = difficult placement), chemosis after STB-administration also rated from 1 to 3 (1 = no chemosis, 2 = intermediate; 3 = heavy chemosis.</p>
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<p>Patient satisfaction after surgery, 5 = completely satisfied, 4 = very satisfied, 3 = satisfied, 2 = dissatisfied, 1 = very dissatisfied.</p>
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16 pages, 2382 KiB  
Article
Encapsulation of Nanocrystals in Mannitol-Based Inhalable Microparticles via Spray-Drying: A Promising Strategy for Lung Delivery of Curcumin
by Luca Casula, Emanuela Fabiola Craparo, Eleonora Lai, Cinzia Scialabba, Donatella Valenti, Michele Schlich, Chiara Sinico, Gennara Cavallaro and Francesco Lai
Pharmaceuticals 2024, 17(12), 1708; https://doi.org/10.3390/ph17121708 - 18 Dec 2024
Abstract
Background/Objectives: Curcumin is well known for its great anti-inflammatory and antioxidant efficacy, representing a potential strategy for the treatment of respiratory disorders. However, several drawbacks, such as chemical instability, poor water solubility and rapid metabolism, result in low bioavailability, limiting its clinical applications. [...] Read more.
Background/Objectives: Curcumin is well known for its great anti-inflammatory and antioxidant efficacy, representing a potential strategy for the treatment of respiratory disorders. However, several drawbacks, such as chemical instability, poor water solubility and rapid metabolism, result in low bioavailability, limiting its clinical applications. In this study, curcumin nanocrystals were incorporated into mannitol-based microparticles to obtain an inhalable dry powder. Methods: A curcumin nanosuspension was produced by wet-ball media milling and thoroughly characterized. Spray drying was then used to produce mannitol microparticles incorporating curcumin nanocrystals. In vitro release/dissolution tests were carried out in simulated lung fluids, and the aerosolization properties were evaluated using a Next-Generation Impactor (NGI, Apparatus E Ph. Eu.). Results: The incorporation of curcumin nanocrystals into mannitol-based microparticles influenced their morphological properties, such as geometric diameters, and flowability. Despite these changes, nebulization studies confirmed optimal MMAD values (<5 µm), while multi-step dissolution/release studies evidenced the influence of mannitol. Conclusions: The developed curcumin nanocrystals-loaded mannitol microparticles show promise as an inhalable treatment for respiratory diseases, combining effective aerodynamic properties with controlled drug release. Full article
(This article belongs to the Special Issue Recent Advances in Inhalation Therapy)
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Graphical abstract
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<p>(<b>A</b>) Composition and DLS data of the CUR-nanosuspension and (<b>B</b>) SEM micrographs of (<b>a</b>) curcumin raw powder and (<b>b</b>) CUR-nanosuspension.</p>
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<p>SEM images of (<b>A</b>) the produced empty microparticle samples M10, M10_AB1 and M15, and (<b>B</b>) the produced curcumin-loaded microparticle samples C0.5_M10, C1_M10, C1_M10_AB1, C0.5_M15 and C1_M15. (magnification 3000×; the bar represents 20 µm).</p>
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<p>Representative DSC thermograms of (<b>A</b>) raw curcumin, P188 and CUR-nanosuspension; (<b>B</b>) mannitol, C0.5_M10, C1_M10_AB1 and C1_M15 samples.</p>
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<p>Release/dissolution profiles of pure CUR-nanosuspension and the CUR-NC loaded microparticles in simulated lung fluid (SLF) at 37 °C. (<span class="html-italic">n</span> = 3).</p>
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<p>Deposition of (<b>A</b>) empty MP and (<b>B</b>) CUR-NP MP on the stages of the NGI after testing with Breezhaler<sup>®</sup> at a flow rate of 90 l min<sup>−1</sup> (* <span class="html-italic">p</span> &lt; 0.05) (MOC = micro-orifice collector).</p>
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20 pages, 28423 KiB  
Article
Optical–Physical Characteristics of Low Clouds and Aerosols in South America Based on Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation
by Bo Su, Dekai Lin, Ziji Liu, Qingyan Wu, Wenkai Song and Miao Zhang
Atmosphere 2024, 15(12), 1513; https://doi.org/10.3390/atmos15121513 - 17 Dec 2024
Viewed by 224
Abstract
Clouds and aerosols, as important factors in the Earth’s climate system, have significant impacts on the atmospheric environment and global climate. This study investigated the optical and physical properties of clouds and aerosols over South America from 2006 to 2021 using CALIPSO Level [...] Read more.
Clouds and aerosols, as important factors in the Earth’s climate system, have significant impacts on the atmospheric environment and global climate. This study investigated the optical and physical properties of clouds and aerosols over South America from 2006 to 2021 using CALIPSO Level 2 products. South America was divided into four regions: A (Western Andean Mountains), B (Northern Orinoco and Amazon plains), C (Southern La Plata Plains), and D (Eastern Brazilian Highlands). Seasonal variations in the optical properties of low clouds and their interactions with the lowest-layer aerosols were analyzed and compared. The results indicate that Region C had the highest OPlc (probability of low clouds) and AODlc (AOD (Aerosol Optical Depth) of low clouds, likely due to its flat terrain and westerly influences. Both AODlc and OPlc were higher in September–November compared to other seasons. DRlc (depolarization ratio of low clouds) values were higher in Regions C and D, particularly in September–February, possibly due to topographic effects and more precipitation and higher humidity during this period. The elevated CRlc (color ratio of low clouds) in Region A may be attributed to the Andes blocking warm, moist air, leading to increased precipitation and cloud particle content. HLlc (top height of low clouds) and BLlc (base altitude of low clouds) were positively correlated with geographic elevation, while Tlc (thickness of low clouds) was greater at night, potentially due to enhanced atmospheric stability. Furthermore, strong correlations among certain parameters suggested significant interactions between aerosols and clouds. Full article
(This article belongs to the Section Atmospheric Techniques, Instruments, and Modeling)
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Figure 1
<p>The geographical location and zoning of South America. The color bar represents the altitude (elevation). Divided into four regions: A, B, C, and D.</p>
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<p>Seasonal spatial distribution of probability of occurrence of low clouds (OP<sub>lc</sub>), AOD of low clouds (AOD<sub>lc</sub>), percentage of AOD for low clouds (PAOD<sub>lc</sub>), and depolarization ratio of low clouds (DR<sub>lc</sub>) over South America during the day.</p>
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<p>Seasonal spatial distributions of OP<sub>lc</sub>, AOD<sub>lc</sub>, PAOD<sub>lc</sub>, and DR<sub>lc</sub> over South America at night.</p>
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<p>Seasonal variation of AOD<sub>lc</sub>, PAOD<sub>lc</sub>, and DR<sub>lc</sub> over South America during the day and at night ((<b>a</b>) AOD<sub>lc</sub> daytime; (<b>b</b>) PAOD<sub>lc</sub> daytime; (<b>c</b>) DR<sub>lc</sub> daytime; (<b>d</b>) AOD<sub>lc</sub> nighttime; (<b>e</b>) PAOD<sub>lc</sub> nighttime; (<b>f</b>) DR<sub>lc</sub> nighttime).</p>
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<p>Seasonal spatial distributions of the probability of color ratio of low clouds (CR<sub>lc</sub>), base altitude of low clouds (B<sub>lc</sub>), top height of low clouds (H<sub>lc</sub>), and thickness of low clouds (T<sub>lc</sub>) over South America during the day.</p>
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<p>Seasonal spatial distributions of CR<sub>lc</sub>, B<sub>lc</sub>, H<sub>lc</sub>, and T<sub>lc</sub> over South America at night.</p>
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<p>Seasonal variation in CR<sub>lc</sub>, B<sub>lc</sub>, H<sub>lc</sub>, and T<sub>lc</sub> over South America during the day and at night ((<b>a</b>) CR<sub>lc</sub> daytime; (<b>b</b>) B<sub>lc</sub> daytime; (<b>c</b>) H<sub>lc</sub> daytime; (<b>d</b>) T<sub>lc</sub> nighttime; (<b>e</b>) CR<sub>lc</sub> nighttime; (<b>f</b>) B<sub>lc</sub> nighttime; (<b>g</b>) H<sub>lc</sub> nighttime; (<b>h</b>) T<sub>lc</sub> nighttime).</p>
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<p>Correlation of PAOD<sub>lc</sub> and AOD<sub>lc</sub> over South America from 2006 to 2021: (<b>a</b>) MMA daytime; (<b>b</b>) JJA daytime; (<b>c</b>) SON daytime; (<b>d</b>) DJF nighttime; (<b>e</b>) MMA nighttime; (<b>f</b>) JJA nighttime; (<b>g</b>) SON nighttime; (<b>h</b>) DJF nighttime.</p>
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<p>Correlation of Tlc and Hlc over South America from 2006 to 2021: (<b>a</b>) MMA daytime; (<b>b</b>) JJA daytime; (<b>c</b>) SON daytime; (<b>d</b>) DJF nighttime; (<b>e</b>) MMA nighttime; (<b>f</b>) JJA nighttime; (<b>g</b>) SON nighttime; (<b>h</b>) DJF nighttime.</p>
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<p>Correlation of B<sub>lc</sub> and H<sub>lc</sub> over South America from 2006 to 2021: (<b>a</b>) MMA daytime; (<b>b</b>) winter daytime; (<b>c</b>) SON daytime; (<b>d</b>) DJF nighttime; (<b>e</b>) MMA nighttime; (<b>f</b>) JJA nighttime; (<b>g</b>) SON nighttime; (<b>h</b>) DJF nighttime.</p>
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<p>Correlation of B<sub>lc</sub> and DR<sub>lc</sub> over South America from 2006 to 2021: (<b>a</b>) MMA daytime; (<b>b</b>) JJA daytime; (<b>c</b>) SON daytime; (<b>d</b>) DJF nighttime; (<b>e</b>) MMA nighttime; (<b>f</b>) JJA nighttime; (<b>g</b>) SON nighttime; (<b>h</b>) DJF nighttime.</p>
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<p>Correlation of AODR<sub>lc</sub> and DR<sub>lc</sub> over South America from 2006 to 2021: (<b>a</b>) MMA daytime; (<b>b</b>) JJA daytime; (<b>c</b>) SON daytime; (<b>d</b>) DJF nighttime; (<b>e</b>) MMA nighttime; (<b>f</b>) JJA nighttime; (<b>g</b>) SON nighttime; (<b>h</b>) DJF nighttime.</p>
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<p>Correlation of PAODR<sub>lc</sub> and DR<sub>lc</sub> over South America from 2006 to 2021: (<b>a</b>) MMA daytime; (<b>b</b>) JJA daytime; (<b>c</b>) SON daytime; (<b>d</b>) DJF nighttime; (<b>e</b>) MMA nighttime; (<b>f</b>) JJA nighttime; (<b>g</b>) SON nighttime; (<b>h</b>) DJF nighttime.</p>
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<p>Correlation of B<sub>la</sub> and B<sub>lc</sub> over South America from 2006 to 2021: (<b>a</b>) MMA daytime; (<b>b</b>) JJA daytime; (<b>c</b>) SON daytime; (<b>d</b>) DJF nighttime; (<b>e</b>) MMA nighttime; (<b>f</b>) JJA nighttime; (<b>g</b>) SON nighttime; (<b>h</b>) DJF nighttime.</p>
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<p>Correlation of H<sub>la</sub> and H<sub>lc</sub> over South America from 2006 to 2021: (<b>a</b>) MMA daytime; (<b>b</b>) JJA daytime; (<b>c</b>) SON daytime; (<b>d</b>) DJF nighttime; (<b>e</b>) MMA nighttime; (<b>f</b>) JJA nighttime; (<b>g</b>) SON nighttime; (<b>h</b>) DJF nighttime.</p>
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<p>Correlation of T<sub>la</sub> and T<sub>lc</sub> over South America from 2006 to 2021: (<b>a</b>) MMA daytime; (<b>b</b>) JJA daytime; (<b>c</b>) SON daytime; (<b>d</b>) DJF nighttime; (<b>e</b>) MMA nighttime; (<b>f</b>) JJA nighttime; (<b>g</b>) SON nighttime; (<b>h</b>) DJF nighttime.</p>
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<p>Correlation of PAOD<sub>la</sub> and PAOD<sub>lc</sub> over South America from 2006 to 2021: (<b>a</b>) MMA daytime; (<b>b</b>) JJA daytime; (<b>c</b>) SON daytime; (<b>d</b>) DJF nighttime; (<b>e</b>) MMA nighttime; (<b>f</b>) JJA nighttime; (<b>g</b>) SON nighttime; (<b>h</b>) DJF nighttime.</p>
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26 pages, 2704 KiB  
Article
Vegetation Effects on Air Pollution: A Comprehensive Assessment for Two Italian Cities
by Mihaela Mircea, Gino Briganti, Felicita Russo, Sandro Finardi, Camillo Silibello, Rossella Prandi, Giuseppe Carlino, Massimo D’Isidoro, Andrea Cappelletti and Giuseppe Cremona
Atmosphere 2024, 15(12), 1511; https://doi.org/10.3390/atmos15121511 - 17 Dec 2024
Viewed by 194
Abstract
The role of urban vegetation in urban air quality is usually assessed by considering only the pollutant removal capacity of the plants. This study aims to show, for the first time, the effects of vegetation on air pollutant concentrations through its effects on [...] Read more.
The role of urban vegetation in urban air quality is usually assessed by considering only the pollutant removal capacity of the plants. This study aims to show, for the first time, the effects of vegetation on air pollutant concentrations through its effects on meteorology, separately from its biogenic emissions. It also investigates how air quality changes when only biogenic emissions are altered by using plants with different emission factors, as well as the potential effects of introducing new vegetation into urban areas. These assessments were conducted using atmospheric modelling systems currently employed for air quality forecasting and planning, configured specifically for the cities of Bologna and Milan. Simulations were performed for two representative months, July and January, to capture summer and winter conditions, respectively. The variability in air concentrations of ozone (O3), nitrogen dioxide (NO2), and particulate matter (PM10) within the municipal boundaries was assessed monthly. When evaluating the impact of future vegetation, changes in temperature, wind speed, and relative humidity were also considered. The results indicate that vegetation influences air quality more significantly through changes in meteorological conditions than through biogenic emissions. Changes in biogenic emissions result in similar behaviours in O3 and PM10 concentrations, with the latter being affected by the changes in the concentrations of secondary biogenic aerosols formed in the atmosphere. Changes in NO2 concentrations are controlled by the changes in O3 concentrations, increasing where O3 concentrations decrease, and vice versa, as expected in highly polluted areas. Meteorologically induced vegetation effects also play a predominant role in depositions, accounting for most of the changes; however, the concentrations remain high despite increased deposition rates. Therefore, understanding only the removal characteristics of vegetation is insufficient to quantify its effects on urban air pollution. Full article
(This article belongs to the Section Air Quality)
13 pages, 2944 KiB  
Article
Development of a Wearable Electromyographic Sensor with Aerosol Jet Printing Technology
by Stefano Perilli, Massimo Di Pietro, Emanuele Mantini, Martina Regazzetti, Pawel Kiper, Francesco Galliani, Massimo Panella and Dante Mantini
Bioengineering 2024, 11(12), 1283; https://doi.org/10.3390/bioengineering11121283 - 17 Dec 2024
Viewed by 326
Abstract
Electromyographic (EMG) sensors are essential tools for analyzing muscle activity, but traditional designs often face challenges such as motion artifacts, signal variability, and limited wearability. This study introduces a novel EMG sensor fabricated using Aerosol Jet Printing (AJP) technology that addresses these limitations [...] Read more.
Electromyographic (EMG) sensors are essential tools for analyzing muscle activity, but traditional designs often face challenges such as motion artifacts, signal variability, and limited wearability. This study introduces a novel EMG sensor fabricated using Aerosol Jet Printing (AJP) technology that addresses these limitations with a focus on precision, flexibility, and stability. The innovative sensor design minimizes air interposition at the skin–electrode interface, thereby reducing variability and improving signal quality. AJP enables the precise deposition of conductive materials onto flexible substrates, achieving a thinner and more conformable sensor that enhances user comfort and wearability. Performance testing compared the novel sensor to commercially available alternatives, highlighting its superior impedance stability across frequencies, even under mechanical stress. Physiological validation on a human participant confirmed the sensor’s ability to accurately capture muscle activity during rest and voluntary contractions, with clear differentiation between low and high activity states. The findings highlight the sensor’s potential for diverse applications, such as clinical diagnostics, rehabilitation, and sports performance monitoring. This work establishes AJP technology as a novel approach for designing wearable EMG sensors, providing a pathway for further advancements in miniaturization, strain-insensitive designs, and real-world deployment. Future research will explore optimization for broader applications and larger populations. Full article
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Graphical abstract
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<p>Design solutions chosen for the creation of the sensor with <span class="html-italic">AJP</span> technology: (<b>a</b>) eight-pole sensor in plane view; (<b>b</b>) eight-pole sensor in 3D view.</p>
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<p>Sensor deposed with AJPs onto a Kapton<sup>®</sup> sheet.</p>
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<p>Frequency–impedance trend for the CALLIBRI<sup>®</sup> sensor with conductive gel. The average and standard deviation for each set of measurements are shown.</p>
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<p>Frequency–impedance trend for the AJP sensor without conductive gel. The average and standard deviation for each set of measurements are shown.</p>
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<p>Experimental setup for analyzing the deformation/impedance properties for the sensor realized with the AJP technique.</p>
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<p>The impedance–frequency trend for the AJP sensor with the <span class="html-italic">X</span>-axis oriented parallel to the long side of the plate and glued to an aluminum bar. (<b>a</b>) Trend of the sensor in undeformed bar condition; (<b>b</b>) trend of the sensor in deformed bar condition.</p>
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<p>Impedance–frequency trend for the AJP sensor with the <span class="html-italic">Y</span>-axis oriented orthogonal to the long side of the plate and glued to an aluminum bar. (<b>a</b>) Trend of the sensor in undeformed bar condition; (<b>b</b>) trend of the sensor in deformed bar condition.</p>
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<p>EMG signal throught the Callibri and AJP printed sensor; (<b>A</b>) Callibri resting state timecourse; (<b>B</b>) Callibri resting state power spectrum; (<b>C</b>) Callibri MVC timecourse; (<b>D</b>) Callibri MVC power spectrum; (<b>E</b>) AJP sensor resting state; (<b>F</b>) AJP sensor power spectrum; (<b>G</b>) AJP sensor MVC resting state; (<b>H</b>) AJP sensor power spectrum.</p>
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16 pages, 41766 KiB  
Article
Methodology for Removing Striping Artifacts Encountered in Planet SuperDove Ocean-Color Products
by Brittney Slocum, Sherwin Ladner, Adam Lawson, Mark David Lewis and Sean McCarthy
Remote Sens. 2024, 16(24), 4707; https://doi.org/10.3390/rs16244707 - 17 Dec 2024
Viewed by 277
Abstract
The Planet SuperDove sensors produce eight-band, three-meter resolution images covering the blue, green, red, red-edge, and NIR spectral bands. Variations in spectral response in the data used to perform atmospheric correction combined with low signal-to-noise over ocean waters can lead to visible striping [...] Read more.
The Planet SuperDove sensors produce eight-band, three-meter resolution images covering the blue, green, red, red-edge, and NIR spectral bands. Variations in spectral response in the data used to perform atmospheric correction combined with low signal-to-noise over ocean waters can lead to visible striping artifacts in the downstream ocean-color products. It was determined that the striping artifacts could be removed from these products by filtering the top of the atmosphere radiance in the red and NIR bands prior to selecting the aerosol models, without sacrificing high-resolution features in the imagery. This paper examines an approach that applies this filtering to the respective bands as a preprocessing step. The outcome and performance of this filtering technique are examined to assess the success of removing the striping effect in atmospherically corrected Planet SuperDove data. Full article
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Figure 1
<p>SuperDove 3 m true-color of the West Florida Shelf, 30 September 2022 15:07:50 GMT (<b>left</b>), and Venice 14 April 2020 09:15:21 GMT (<b>right</b>), overlaid onto a VIIRS 750 m resolution scene for spatial comparison.</p>
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<p>West Florida Shelf <span class="html-italic">L<sub>t</sub></span> product for (<b>a</b>) 491 nm, (<b>b</b>) 708 nm, and (<b>c</b>) 867 nm.</p>
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<p>Venice <span class="html-italic">L<sub>t</sub></span> product for (<b>a</b>) 491 nm, (<b>b</b>) 708 nm, and (<b>c</b>) 867 nm.</p>
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<p>West Florida Shelf <span class="html-italic"><sub>n</sub>L<sub>w</sub></span> product for (<b>a</b>) 491 nm, (<b>b</b>) 708 nm, and (<b>c</b>) 867 nm.</p>
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<p>Venice <span class="html-italic"><sub>n</sub>L<sub>w</sub></span> product for (<b>a</b>) 491 nm, (<b>b</b>) 708 nm, and (<b>c</b>) 867 nm.</p>
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<p><span class="html-italic">L<sub>a</sub></span> product for the West Florida Shelf: (<b>a</b>) 491 nm, (<b>b</b>) 708 nm, and (<b>c</b>) 867 nm.</p>
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<p>Aerosol model product for Venice: (<b>a</b>) 491 nm, (<b>b</b>) 708 nm, and (<b>c</b>) 867 nm.</p>
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<p>Log-scaled power spectrum of the above average power components in the West Florida Shelf data (<b>left</b>) and Venice data (<b>right</b>).</p>
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<p>Masked Frequency components for the middle 400 frequencies of the spectrum after the application of the notch and low-pass filters.</p>
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<p>Application of SciPy Uniform filter with kernel size 301 vs. 601 for 5 iterations on the <span class="html-italic">L<sub>t</sub></span> (top) and resulting <span class="html-italic">L<sub>a</sub></span> (bottom) at 708 nm where (<b>a</b>,<b>d</b>) are the original, striped, images; (<b>b</b>,<b>e</b>) are the 301 × 301 kernel filtered images; and (<b>c</b>,<b>f</b>) are the 601 × 601 kernel filtered images.</p>
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<p>Application of SciPy Uniform filter with kernel size 301 vs. 601 for 5 iterations on the <span class="html-italic">L<sub>t</sub></span> (top) and resulting <span class="html-italic">L<sub>a</sub></span> (bottom) at 867 where (<b>a</b>,<b>d</b>) are the original, striped, image; (<b>b</b>,<b>e</b>) are the 301 × 301 kernel filtered images; and (<b>c</b>,<b>f</b>) are the 601 × 601 kernel filtered images.</p>
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<p><span class="html-italic"><sub>n</sub>L<sub>w</sub></span> at 491 nm after application of SciPy Uniform filter with kernel size 301 for up to 5 iterations to the West Florida Shelf data.</p>
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<p><span class="html-italic"><sub>n</sub>L<sub>w</sub></span> at 491 nm after application of SciPy Uniform filter with kernel size 301 for up to 5 iterations to the Venice data.</p>
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<p><span class="html-italic"><sub>n</sub>L<sub>w</sub></span> at 491 nm after application of SciPy Uniform filter with kernel size 601 for up to 5 iterations to the West Florida Shelf data.</p>
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<p><span class="html-italic"><sub>n</sub>L<sub>w</sub></span> at 491 nm after application of SciPy Uniform filter with kernel size 601 for up to 5 iterations to the Venice data.</p>
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<p><span class="html-italic">L<sub>t</sub></span>, <span class="html-italic">L<sub>a</sub></span>, and <span class="html-italic"><sub>n</sub>L<sub>w</sub></span> after the application of the notch filter to the <span class="html-italic">L<sub>t</sub></span> for the West Florida Shelf (<b>top</b>) and Venice (<b>bottom</b>) scenes.</p>
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26 pages, 13796 KiB  
Article
The BIRDIES Experiment: Measuring Beryllium Isotopes to Resolve Dynamics in the Stratosphere
by Sonia Wharton, Alan J. Hidy, Thomas S. Ehrmann, Wenbo Zhu, Shaun N. Skinner, Hassan Beydoun, Philip J. Cameron-Smith, Marisa Repasch, Nipun Gunawardena, Jungmin M. Lee, Ate Visser, Matthew Griffin, Samuel Maddren and Erik Oerter
Atmosphere 2024, 15(12), 1502; https://doi.org/10.3390/atmos15121502 - 17 Dec 2024
Viewed by 361
Abstract
Cosmogenic beryllium-10 and beryllium-7, and the ratio of the two (10Be/7Be), are powerful atmospheric tracers of stratosphere–troposphere exchange (STE) processes; however, measurements are sparse for altitudes well above the tropopause. We present a novel high-altitude balloon campaign aimed to measure these isotopes in [...] Read more.
Cosmogenic beryllium-10 and beryllium-7, and the ratio of the two (10Be/7Be), are powerful atmospheric tracers of stratosphere–troposphere exchange (STE) processes; however, measurements are sparse for altitudes well above the tropopause. We present a novel high-altitude balloon campaign aimed to measure these isotopes in the mid-stratosphere called Beryllium Isotopes for Resolving Dynamics in the Stratosphere (BIRDIES). BIRDIES targeted gravity waves produced by tropopause-overshooting convection to study their propagation and impact on STE dynamics, including the production of turbulence in the stratosphere. Two custom-designed payloads called FiSH and GASP were flown at altitudes approaching 30 km to measure in situ turbulence and beryllium isotopes (on aerosols), respectively. These were flown on nine high-altitude balloon flights over Kansas, USA, in summer 2022. The atmospheric samples were augmented with a ground-based rainfall collection targeting isotopic signatures of deep convection overshooting. Our GASP samples yielded mostly negligible amounts of both 10Be and 7Be collected in the mid-stratosphere but led to design improvements to increase aerosol capture in low-pressure environments. Observations from FiSH and the precipitation collection were more fruitful. FiSH showed the presence of turbulent velocity, temperature, and acoustic fluctuations in the stratosphere, including length scales in the infra-sonic range and inertial subrange that indicated times of elevated turbulence. The precipitation collection, and subsequent statistical analysis, showed that large spatial datasets of 10Be/7Be can be measured in individual rainfall events with minimum terrestrial contamination. While the spatial patterns in rainfall suggested some evidence for overshooting convection, inter-event temporal variability was clearly observed and predicted with good agreement using the 3D chemical transport model GEOS-CHEM. Full article
(This article belongs to the Special Issue Feature Papers in Atmospheric Techniques, Instruments, and Modeling)
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<p>Schematic of berylium-7 and -10 production and wet deposition as well as estimated ratios of 10Be/7Be in the stratosphere and troposphere. Our airborne (GASP) and ground-based wet deposition (Raincube) aerosol collection methods are also illustrated. Figure modified from [<a href="#B17-atmosphere-15-01502" class="html-bibr">17</a>].</p>
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<p>(<b>a</b>) External view of FiSH showing the cold- and hot-wire anemometers and tail fin; (<b>b</b>) internal view of FiSH showing the onboard electronics; (<b>c</b>) schematic of the single-balloon configuration with the FiSH payload; (<b>d</b>) photograph of FiSH launched during BIRDIES.</p>
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<p>(<b>a</b>) GASP external and internal views; (<b>b</b>) close–up view of GASP’s interior showing the onboard electronics, pump, and filter system; (<b>c</b>) schematic of the tandem-balloon configuration with GASP; (<b>d</b>) photograph of GASP launched during BIRDIES.</p>
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<p>Schematic of major pre-flight, flight, and post-flight activities for BIRDIES. These steps are for both the single- and tandem-balloon platforms.</p>
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<p>(<b>a</b>) Photograph of the Raincube at E36 which shows a typical deployment during BIRDIES; (<b>b</b>) Raincube deployment map (blue stars) in the DOE ARM SGP domain centered on the Central Facility; (<b>c</b>) regional map showing central Oklahoma and Kansas and the locations of the Salina airport (SAL) and the ARM Central Facility (CF) Raincubes (as well as the boundaries of the ARM Raincube domain), and the IMS station RN74.</p>
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<p>Schematic of the Accelerated Mass Spectrometry (AMS) analytical procedure for 10Be and 7Be including the sample preparation for the precipitation (Raincube) samples and aerosol (GASP filter) samples. Also shown are the split samples for anion, cation, and isotopes of H and O analysis.</p>
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<p>One-hour precipitation amounts measured at three of the ARM sites (E32, I10, CF) to show that some events contained more than one storm system during the collection duration. The sample collection events are labeled and highlighted in gray. Collection durations differ between sites because the collection was performed manually. Event 1 is not shown.</p>
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<p>Example of (<b>a</b>) flight trajectory and (<b>b</b>) altitude information, shown for BIRDIES-05a (GASP), BIRDIES-05b (FiSH payload), and BIRDIES-07 (GASP).</p>
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<p>BIRDIES-05b (<b>a</b>) hot-wire, (<b>b</b>) cold-wire, and (<b>c</b>) microphone power spectrum from FiSH shown for three altitudes in the lower-mid-stratosphere.</p>
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<p>FiSH measurements of (<b>a</b>) Brunt–Väisälä frequency, (<b>b</b>) wind shear, and (<b>c</b>) Richardson number on the ascent phase from BIRDIES-05b. Altitudes plotted range from 10 to 26 km (upper troposphere to mid-stratosphere). Dashed line is the critical Richardson number, <span class="html-italic">Ri<sub>crit</sub></span> = 0.25.</p>
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<p>Measured mean (+/− one standard deviation) and modeled concentrations of 10Be, 7Be, and their ratio (10Be/7Be) by event number. Each measured event contains up to 11 ARM SGP Raincube observations.</p>
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<p>(<b>a</b>) Time series of daily 7Be measured at the IMS RN74 station in Ashland, Kansas; (<b>b</b>) difference between GEOS-Chem modeled and observed value; and (<b>c</b>) difference focused on the BIRDIES period with the collection Events 2-6 highlighted. Note in panel (<b>c</b>) that the collection durations of Events 3 and 4 overlap with the daily IMS record as indicated by bracketed lines. Average concurrent BIRDIES precipitation collection events are highlighted in (<b>c</b>). The dashed box in (<b>b</b>) represents the BIRDIES period shown in detail in panel (<b>c</b>).</p>
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<p>Pearson correlation coefficients (R) for a subset of the analyzed chemical species in the BIRDIES precipitation dataset. Precipitation is event– and site-specific and is the value measured by the rain gauge. Precipitation weight is the amount of water in each sample received at the laboratory.</p>
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<p>Agglomerative clustering with a median linkage function applied to the BIRDIES precipitation dataset. The colors represent the z-score, where the standard deviation from the median is calculated by column. The clustering shows three main groups (Clusters A–C).</p>
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24 pages, 10007 KiB  
Article
Levels, Sources and Risk Assessment of Carbonaceous and Organic Species Associated with PM2.5 in Two Small Cities of Morelos, Mexico
by Brenda L. Valle-Hernández, José de Jesús Figueroa-Lara, Miguel Torres-Rodríguez, Noé Ginéz-Hernández, Tamara Álvarez-Lupercio and Violeta Mugica-Álvarez
Atmosphere 2024, 15(12), 1496; https://doi.org/10.3390/atmos15121496 - 15 Dec 2024
Viewed by 727
Abstract
A study of carbonaceous species, polycyclic aromatic hydrocarbons (PAHs), and nitro-PAHs associated with PM2.5 was conducted to assess their carcinogenic potential and associated health risks in the two main cities of the State of Morelos: Cuernavaca and Cuautla. The annual median concentrations [...] Read more.
A study of carbonaceous species, polycyclic aromatic hydrocarbons (PAHs), and nitro-PAHs associated with PM2.5 was conducted to assess their carcinogenic potential and associated health risks in the two main cities of the State of Morelos: Cuernavaca and Cuautla. The annual median concentrations in Cuernavaca of organic carbon (OC) and elemental carbon (EC) were 6.2 µg m−3 and 0.6 µg m−3, respectively, whereas in Cuautla, OC concentrations averaged 4.8 µg m−3 and EC 0.6 µg m−3. OC/EC ratios, total carbonaceous aerosols (TCA), primary (POC) and secondary organic carbon (SOC), as well as elemental carbon reactive (ECR) were estimated, also showing prevalence of primary emissions such as biomass burning. The seventeen PAHs recommended by the EPA and twelve nitro-PAHs were measured using gas chromatography–mass spectrometry. The annual median sum of PAHs was 9.7 ng m−3 in Cuernavaca and 11.2 ng m−3 in Cuautla, where carcinogenic high-molecular-weight compounds were the most dominant; the annual median sums of nitro-PAHs were 287 pg m−3 and 432 pg m−3, respectively. Diagnostic ratios were applied to identify potential sources of PAH emissions, suggesting that fuel combustion is the major contributor in both sites, followed by coal biomass burning and agricultural activities. The annual carcinogenic potential as benzo(a)pyrene equivalent was 2.2 ng m−3 for both sites. The lifetime excess cancer risk from PAH inhalation was estimated to range from 1.8 × 10−4 to 2 × 10−4 in Cuernavaca and from 1.5 × 10−4 to 2.2 × 10−4 in Cuautla, similar to values observed in other urban regions globally. Full article
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<p>Sampling sites (Cuernavaca and Cuautla) in the State of Morelos, Mexico.</p>
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<p>Time series graph of OC and EC concentrations from the two sampling sites.</p>
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<p>Medians of OC and EC concentrations by season and site. Box: 25–75%; Whisker: 10–90%.</p>
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<p>Concentration charts of OC, EC, and PAHs for Cuernavaca (CUE).</p>
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<p>Concentration charts of OC, EC, and PAHs for CUA.</p>
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<p>Relationships of organic carbon (OC) and elemental carbon (EC) in PM<sub>2.5</sub> correlations for (<b>a</b>) Cuernavaca (CUE) and (<b>b</b>) Cuautla (CUA).</p>
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<p>OC/EC ratio in Cuernavaca (CUE) and Cuautla (CUA) by season.</p>
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<p>Median Primary Organic Concentration (POC) and Secondary Organic concentration (SOC), and % SOC/OC by season and site.</p>
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<p>Median concentration of PAHs associated with PM<sub>2.5</sub> in Cuernavaca by season.</p>
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<p>Median concentration of PAHs associated with PM<sub>2.5</sub> in Cuautla by season.</p>
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<p>Median concentration of PAHsum and PAHcarcinogenic; Box: 25–75%; Whisker: 10–90%.</p>
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<p>Seasonal median concentration of nitro-PAHs in PM<sub>2.5</sub> in Cuernavaca (<b>a</b>) and Cuautla (<b>b</b>).</p>
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<p>Flt vs. 2-NFlt in CUE. (<b>a</b>) Warm-dry and (<b>b</b>) Rainy seasons.</p>
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<p>Median concentrations (10 and 90 percentiles) of nitro-PAHs in PM<sub>2.5</sub> in CUE and CUA, during R, WD, and CD seasons. Median; Box: 25–75%; Whisker: 10–90%.</p>
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<p><b>Seasonal</b> BaPeq concentrations in Cuernavaca and Cuautla.</p>
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16 pages, 5216 KiB  
Article
Shape Accuracy Improvement of the Flange Turning Process in Aluminum Aerosol Can Production
by Istvan Sztankovics, Csaba Felho, Krisztina Kun-Bodnar and Zsolt Maros
Eng 2024, 5(4), 3381-3396; https://doi.org/10.3390/eng5040176 - 15 Dec 2024
Viewed by 278
Abstract
This study investigates the flange turning process in the production of aluminum aerosol bottles. Aluminum discs are lubricated, extruded, trimmed, washed, painted, and lacquered before undergoing necking, where flange turning ensures a secure, aesthetically pleasing fit. Errors in flange turning, such as uneven [...] Read more.
This study investigates the flange turning process in the production of aluminum aerosol bottles. Aluminum discs are lubricated, extruded, trimmed, washed, painted, and lacquered before undergoing necking, where flange turning ensures a secure, aesthetically pleasing fit. Errors in flange turning, such as uneven or tapered surfaces, can compromise bottle functionality and appearance. To address this, experiments were performed with different tool geometries, feed rates, and rotational speeds. The investigations aimed to achieve flat, consistent flange surfaces with minimal deviation from the desired geometry. Two main variables were examined: a 1 s waiting time at the end position and variations in feed rate and cutting depth. The waiting time improved flatness, halving surface deviations, while regrinding the tool reduced flatness errors to a tenth of the original values. Higher feed rates and speeds also enhanced surface quality, with flatness errors ranging from 371 μm to 75 μm. Overall, this study demonstrates that optimizing parameters like cutting angle, feed rate, and rotational speed, along with a waiting period, significantly enhances surface accuracy. These findings support more efficient production processes for aluminum aerosol bottles. Full article
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<p>Specimen workpiece (<b>a</b>) and its clamping in the lathe (<b>b</b>).</p>
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<p>Mechanical drawing of the studied aluminum aerosol bottle.</p>
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<p>Flatness error of the studied aluminum aerosol bottle.</p>
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<p>Grinding process of the cutting tool. (Clamping of the cutting insert (<b>a</b>) and orientaion of the tool (<b>b</b>)).</p>
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<p>Flatness error of the studied aluminum aerosol bottle machined with the original setup.</p>
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<p>Flatness error of the studied aluminum aerosol bottle machined with the original cutting tool and a 1 s waiting time at the end of the flange turning.</p>
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<p>Flatness error of the studied aluminum aerosol bottle with the modified cutting insert and a 1 s waiting time at the end of the flange turning procedure.</p>
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<p>The maximum material deviation from the fitted reference plane (<span class="html-italic">FLTp</span>) in function of the rotation speed and feed.</p>
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<p>The maximum deviation inward into the material from the fitted reference plane (<span class="html-italic">FLTv</span>) in function of the rotation speed and feed.</p>
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<p>The distance between the highest peak and the deepest valley (<span class="html-italic">FLTt</span>) in function of the rotation speed and feed.</p>
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<p>Main effect of the feed and rotation speed on the maximum material deviation from the fitted reference plane (<span class="html-italic">FLTp</span>).</p>
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<p>Main effect of the feed and rotation speed on the maximum deviation inward into the material from the fitted reference plane (<span class="html-italic">FLTv</span>).</p>
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<p>Main effect of the feed and rotation speed on the distance between the highest peak and the deepest valley (<span class="html-italic">FLTt</span>).</p>
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20 pages, 5308 KiB  
Article
Atmospheric Modulation Transfer Function Calculation and Error Evaluation for the Panchromatic Band of the Gaofen-2 Satellite
by Zhengqiang Li, Mingjun Liang, Yan Ma, Yang Zheng, Zhaozhou Li and Zhenting Chen
Remote Sens. 2024, 16(24), 4676; https://doi.org/10.3390/rs16244676 - 14 Dec 2024
Viewed by 454
Abstract
In the optical satellite on-orbit imaging quality estimation system, the calculation of Modulation Transfer Function (MTF) is not fully standardized, and the influence of atmosphere is often simplified, making it difficult to obtain completely consistent on-orbit MTF measurements and comparisons. This study investigates [...] Read more.
In the optical satellite on-orbit imaging quality estimation system, the calculation of Modulation Transfer Function (MTF) is not fully standardized, and the influence of atmosphere is often simplified, making it difficult to obtain completely consistent on-orbit MTF measurements and comparisons. This study investigates the effects of various factors—such as edge angle, edge detection methods, oversampling rate, and interpolation techniques—on the accuracy of MTF calculations in the commonly used slanted-edge method for on-orbit MTF assessment, informed by simulation experiments. A relatively optimal MTF calculation process is proposed, which employs the Gaussian fitting method for edge detection, the adaptive oversampling rate, and the Lanczos (a = 3) interpolation method, minimizing the absolute deviation in the MTF results. A method to quantitatively analyze the atmospheric scattering and absorption MTF is proposed that employs a radiative transfer model. Based on the edge images of GF-2 satellite, images with various atmospheric conditions and imaging parameters are simulated, and their atmospheric scattering and absorption MTF is obtained through comparing the MTFs of the ground and top atmosphere radiance. The findings reveal that aerosol optical depth (AOD), viewing zenith angle (VZA), and altitude (ALT) are the primary factors influencing the accuracy of GF-2 satellite on-orbit MTF measurements in complex scenarios. The on-orbit MTF decreases with the increase in AOD and VZA and increases with the increase in ALT. Furthermore, a collaborative analysis of the main influencing factors of atmospheric scattering and absorption MTF indicates that, taking the PAN band of the GF-2 satellite as an example, the atmospheric MTF values are consistently below 0.7905. Among these, 90% of the data are less than 0.7520, with corresponding AOD conditions ranging from 0 to 0.08, a VZA ranging from 0 to 50°, and an ALT ranging from 0 to 5 km. The results can provide directional guidance for the selection of meteorological conditions, satellite attitude, and geographical location during satellite on-orbit testing, thereby enhancing the ability to accurately measure satellite MTF. Full article
(This article belongs to the Section Atmospheric Remote Sensing)
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<p>The PAN band image of the GF-2 satellite on 24 October 2021 at the Baotou site.</p>
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<p>Overall flowchart of this study.</p>
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<p>Flow chart of the quantitative calculation of atmospheric effects based on the atmospheric radiation transfer model.</p>
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<p>Frequency variations in (<b>a</b>) system MTF, (<b>b</b>) detector MTF, (<b>c</b>) aberration ATF, and (<b>d</b>) diffraction-limited optics OTF in the PAN band of the GF2 satellite for edge tilt angles of 0.5–44.5°.</p>
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<p>Variation in MTF in polar coordinates at edge inclination angles of 0.5–44.5°, with angular intervals of 0.2°, where (<b>a</b>) is the case of the adaptive oversampling rate under the Gaussian fitting method, (<b>b</b>) is the adaptive oversampling rate under the error fitting method, and (<b>c</b>) is the adaptive oversampling rate under the centroid detection method.</p>
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<p>Group diagram of the effect of doubling rate on MTF, where (<b>a</b>–<b>d</b>) are the Gaussian fitting method, (<b>e</b>–<b>h</b>) are the error fitting method, and (<b>i</b>–<b>l</b>) are the centroid detection fitting method. The first column of each row of images represents the case of no oversampling, the second column represents the case of 2× oversampling, the third column represents the case of 4× oversampling, and the fourth column represents the case of 8×oversampling.</p>
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<p>Group diagram of the effect of interpolation methods on MTF, where (<b>a</b>) is the Lanczos (a = 3) interpolation method, (<b>b</b>) is the continuum magic interpolation method, (<b>c</b>) is the Lanczos (a = 2) interpolation method, (<b>d</b>) is the f Lanczos (a = 1) interpolation method, (<b>e</b>) is the Bin average interpolation method, and (<b>f</b>) is the Mitchell kernel interpolation method.</p>
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<p>Group diagram of the results of atmospheric scattering and absorption MTF variations in various bands calculated based on satellite images, where (<b>a</b>) AOD, (<b>b</b>) CWV, (<b>c</b>) SZA, (<b>d</b>) ALT, (<b>e</b>) RAZ, and (<b>f</b>) SZA.</p>
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<p>(<b>a</b>) The distribution of MTF values of different edge detection methods, (<b>b</b>) the distribution of MTF values of different interpolation methods, and (<b>c</b>) the distribution of MTF values for different oversampling rates. (<b>d</b>) The distribution of ΔMTF values of different edge detection methods, (<b>e</b>) the distribution of ΔMTF values of different interpolation methods, and (<b>f</b>) the distribution of ΔMTF values for different oversampling rates. For (<b>b</b>) and (<b>e</b>), Lanczos (a = 3), Continuum magic, Lanczos (a = 2), Lanczos (a = 1), Bin average, and Mitchell kernel are abbreviated, respectively, as L (a = 3), CM, L (a = 2), L (a = 1), BA, MK; for (<b>c</b>) and (<b>f</b>), adaptive oversampling, no oversampling, 2× oversampling, 4× oversampling, and 8× oversampling is abbreviated, respectively, as AO, NO, 2×O, 4×O, 8×O. The red solid line in the middle of the box plot represents the median MTF value, the blue lines at the top and bottom respectively indicate the first and third quartiles of the MTF value, and the red dashed line at 0.1283 indicates the theoretical value of <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>M</mi> <mi>T</mi> <mi>F</mi> </mrow> <mrow> <mi>s</mi> <mi>y</mi> <mi>s</mi> </mrow> </msub> </mrow> </semantics></math>.</p>
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<p>(<b>a</b>) The distribution of MTF values of different edge detection methods, (<b>b</b>) the distribution of MTF values of different interpolation methods, and (<b>c</b>) the distribution of MTF values for different oversampling rates. (<b>d</b>) The distribution of ΔMTF values of different edge detection methods, (<b>e</b>) the distribution of ΔMTF values of different interpolation methods, and (<b>f</b>) the distribution of ΔMTF values for different oversampling rates. For (<b>b</b>) and (<b>e</b>), Lanczos (a = 3), Continuum magic, Lanczos (a = 2), Lanczos (a = 1), Bin average, and Mitchell kernel are abbreviated, respectively, as L (a = 3), CM, L (a = 2), L (a = 1), BA, MK; for (<b>c</b>) and (<b>f</b>), adaptive oversampling, no oversampling, 2× oversampling, 4× oversampling, and 8× oversampling is abbreviated, respectively, as AO, NO, 2×O, 4×O, 8×O. The red solid line in the middle of the box plot represents the median MTF value, the blue lines at the top and bottom respectively indicate the first and third quartiles of the MTF value, and the red dashed line at 0.1283 indicates the theoretical value of <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>M</mi> <mi>T</mi> <mi>F</mi> </mrow> <mrow> <mi>s</mi> <mi>y</mi> <mi>s</mi> </mrow> </msub> </mrow> </semantics></math>.</p>
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<p>Histogram of the atmospheric scattering and absorption MTF for the PAN band, accompanied by a cumulative data curve. Three vertical black dashed lines indicate the positions at which the cumulative percentages reach 50%, 80%, and 90%, respectively.</p>
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<p>Group diagram illustrating ranges of atmospheric conditions that satisfy the different requirements for atmospheric impact, including (<b>a</b>) an atmospheric scattering and absorption MTF above 0.75, (<b>b</b>) an atmospheric scattering and absorption MTF above 0.78, and (<b>c</b>) an atmospheric scattering and absorption MTF above 0.79, depicted in three-dimensional positions.</p>
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19 pages, 6499 KiB  
Article
Innovative Ultrasonic Spray Methods for Indoor Disinfection
by Andrey Shalunov, Olga Kudryashova, Vladimir Khmelev, Dmitry Genne, Sergey Terentiev and Viktor Nesterov
Appl. Syst. Innov. 2024, 7(6), 126; https://doi.org/10.3390/asi7060126 - 13 Dec 2024
Viewed by 316
Abstract
This study explores the challenges associated with dispersing disinfectant liquids for sanitizing individuals, indoor spaces, vehicles, and outdoor areas. Among the various approaches, fine aerosol sprays with a high particle surface area emerge as a particularly promising solution. Ultrasonic spraying, which leverages diverse [...] Read more.
This study explores the challenges associated with dispersing disinfectant liquids for sanitizing individuals, indoor spaces, vehicles, and outdoor areas. Among the various approaches, fine aerosol sprays with a high particle surface area emerge as a particularly promising solution. Ultrasonic spraying, which leverages diverse mechanisms of ultrasound interaction with liquids, offers several distinct advantages. Notably, it enables the production of fine aerosols from liquids with a broad range of physical and chemical properties, including variations in purity, viscosity, and surface tension. This capability is especially critical for disinfectant liquids and suspensions, which often exhibit low surface tension and/or high viscosity. The article provides a comprehensive review of ultrasonic spraying methods and technologies developed by the authors’ team in recent years. It highlights innovative ultrasonic sprayers, including the latest designs, which are capable of generating aerosols with precise dispersion characteristics and high productivity from disinfectant liquids. Full article
(This article belongs to the Section Industrial and Manufacturing Engineering)
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<p>Piezoelectric oscillatory system of ultrasonic atomizer. 1—radiating pad-concentrator; 2—spray surface; 3—piezoceramic elements; 4—reflective pad; 5—internal channel for supplying sprayed liquid; 6—housing; 7—housing flange; 8—threaded hole for supplying liquid; 9—ultrasonic sprayer power cable; 10—power cable connector.</p>
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<p>Spray surface with additional channels for liquid supply (γ is the root angle of the torch): (<b>a</b>) diagram of liquid spreading over the spray surface; (<b>b</b>) diagram of the arrangement of additional channels along the generatrix of the spray surface cone; (<b>c</b>) diagram of the arrangement of additional channels on the spray surface; and (<b>d</b>) angles of the arrangement of additional channels relative to the central channel.</p>
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<p>Spraying liquid without air flows (<b>a</b>) and using air flows to form a torch (<b>b</b>).</p>
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<p>Ultrasonic sprayers: (<b>a</b>) high-performance coarse atomizers with an operating frequency of 22 kHz; (<b>b</b>) sprayers with air flow generation system; (<b>c</b>) spray nozzles for forming a spray torch of arbitrary shape (e.g., flat); and (<b>d</b>) high-frequency fine mist atomizers. (FOG-N UZR-0.15/22-O, FOG-N UZR-0.15/22-OSv, FOG-N UZR-0.1/35-OSv, FOG-V UZR-0.1/160-OM, Center of Ultrasound Technologies LLC, Biysk, Russia).</p>
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<p>Ultrasonic wearable atomizer for forming an aerosol with an average particle size of no more than 50 μm and a capacity of up to 20 mL per second: (<b>a</b>) three-dimensional model, (<b>b</b>) structural diagram. 1—piezoelectric transducer; 2—booster link; 3—concentrator; 4—flexural–oscillating disk (atomizing surface); 5—internal channel for atomized liquid; 6, 7—internal channels of the atomizing tool; 8—atomizer body; 9—handle; 10—trigger for starting the atomizer; 11—outlet of the power cable combined with the atomized liquid supply tube.</p>
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<p>Ultrasonic wearable aerosol sprayer with an average particle size of 65 microns and a capacity of no more than 60 mL per second: (<b>a</b>) three-dimensional model, (<b>b</b>) structural diagram. 1—piezoelectric transducer; 2—flexural–oscillating disk (spray surface); 3—sprayer body; 4—fan for cooling the piezoelectric transducer of the atomizer; 5—handle; 6—flow regulators; 7—holder of the disinfectant liquid distributor; 8—tubes for supplying liquid; 9—distributor of the sprayed liquid; 10—nipple for connecting the liquid supply system.</p>
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<p>Conceptual diagram of multi-stage ultrasonic atomization.</p>
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<p>Ultrasonic tubular emitter: (<b>a</b>) drawing of tubular emitter; (<b>b</b>) vibration waveform. 1—emitting element in the form of a bending and vibrating tube; 2—piezoelectric transducer concentrator (emitting plate); 3—piezoceramic elements; 4—reflecting plate; 5—housing; 6—flange; <span class="html-italic">L</span>—emitter length; <span class="html-italic">D</span><sub>1</sub>—inner diameter; <span class="html-italic">D</span><sub>2</sub>—outer diameter.</p>
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<p>The developed emitter: (<b>a</b>) distribution of vibrations inside the emitter; and (<b>b</b>) photo of the ultrasonic emitter.</p>
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<p>Scheme of cavitation combined spraying method. 1—supply of sprayed liquid, 2—cylindrical volume for liquid under increased pressure, 3—ultrasonic emitter, 4—cavitation area, 5—outlet, 6—large drops, 7—cavitation bubbles, 8—atomized liquid droplets.</p>
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<p>Ultrasonic atomizer for cavitation combined method: (<b>a</b>) sketch of ultrasonic atomizer; (<b>b</b>) atomizer assembled with electronic generator. 1—Langevin piezoelectric transducer; 2—radiating pad-concentrator; 3—reflecting pad; 4—piezoceramic elements; 5—working tool; 6—technological volume; 7—nozzle; 8—fitting; A–cavitation area.</p>
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<p>Structural diagram of the experimental setup. 1—Tested sprayer; 2—Ultrasonic generator; 3—Peristaltic pump; 4—Receiver; 5—Air compressor; 6—Flow meter; 7—Nozzle; 8—Malvern SprayTec analyzer; 9—Vacuum aspirator; 10—Sound pressure level meter.</p>
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<p>Particle size distribution of water aerosols with ultrasonic atomization at 180 kHz and 25 kHz, and (for comparison) by the hydraulic method.</p>
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<p>Water aerosol particle size distribution by multi-stage ultrasonic atomization 165 dB and 182 dB.</p>
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<p>Dependence of the Sauter diameter of the resulting aerosol: (<b>a</b>) on the sound pressure level; and (<b>b</b>) on the flow velocity of the incoming aerosol.</p>
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<p>Dependences of the critical ultrasound amplitude (<b>a</b>) and the Sauter diameter (<b>b</b>) of the aerosol in the optimal mode on the hydraulic pressure.</p>
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<p>Histograms of particle size distribution in the combined cavitation spraying method: (<b>a</b>) at a pressure of 6 atm (amplitude 33 μm); and (<b>b</b>) at a pressure of 11 atm (amplitude 47 μm).</p>
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20 pages, 7358 KiB  
Article
Research on the Estimation of Air Pollution Models with Machine Learning in Urban Sustainable Development Based on Remote Sensing
by Wenqian Chen, Na Zhang, Xuesong Bai and Xiaoyi Cao
Sustainability 2024, 16(24), 10949; https://doi.org/10.3390/su162410949 - 13 Dec 2024
Viewed by 370
Abstract
Air quality is directly related to people’s health and quality of life and has a profound impact on the sustainable development of cities. Good air quality is the foundation of sustainable development. To solve the current problem of air quality for sustainable development, [...] Read more.
Air quality is directly related to people’s health and quality of life and has a profound impact on the sustainable development of cities. Good air quality is the foundation of sustainable development. To solve the current problem of air quality for sustainable development, we used high-resolution (1 km) satellite-retrieved aerosol optical depth (AOD), meteorological, nighttime light and vegetation data to develop a spatiotemporal convolution feature random forest (SCRF) model to predict the PM2.5 concentration in Shandong from 2016 to 2019. We evaluated the performance of the SCRF model and compared the results of other models, including neural network (BPNN), gradient boosting (GBDT), and random forest (RF) models. The results show that compared with the other models, the improved SCRF model performs best. The coefficient of determination (R2) and root mean square error (RMSE) are 0.83 and 9.87 µg/m3, respectively. Moreover, we discovered that the characteristic variables AOD and air temperature (TEM) data improved the accuracy of the model in Shandong Province. The annual average PM2.5 concentrations in Shandong Province from 2016 to 2019 were 74.44 µg/m3, 65.01 µg/m3, 58.32 µg/m3, and 59 µg/m3, respectively. The spatial distribution of air pollution increases from northeastern and southeastern to western Shandong inland. In general, our research has significant implications for the sustainable development of various cities in Shandong Province. Full article
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<p>Overview of the study area and distribution map of PM<sub>2.5</sub> stations (AOD data on 26 December 2018).</p>
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<p>Schematic diagram of the SCRF model.</p>
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<p>Histogram and descriptive statistics of the independent model variables (mean, median and standard deviation).</p>
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<p>Average PM<sub>2.5</sub> concentrations at ground monitoring stations in Shandong Province.</p>
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<p>Heatmap and Pearson correlation coefficient histogram of the correlation analysis between the PM<sub>2.5</sub> concentration and other characteristic variables: (<b>a</b>) Correlation analysis heatmap; (<b>b</b>) Pearson correlation coefficient histogram.</p>
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<p>Changes in overall R<sup>2</sup> and RMSE with the number of decision trees from 2016 to 2019.</p>
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<p>Model-based feature importance ranking.</p>
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<p>Fitting diagram of the annual PM<sub>2.5</sub> concentrations predicted by the RF (<b>a</b>–<b>d</b>) and SCRF (<b>e</b>–<b>h</b>) models in Shandong Province from 2016 to 2019.</p>
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<p>Fitting diagram of the seasonal PM<sub>2.5</sub> concentrations predicted by the RF (<b>a</b>–<b>d</b>) and SCRF (<b>e</b>–<b>h</b>) models in Shandong Province from 2016 to 2019.</p>
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<p>Annual average PM<sub>2.5</sub> concentration in Shandong Province from 2016 to 2019.</p>
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<p>Seasonal average PM<sub>2.5</sub> concentrations in spring, summer, autumn and winter in Shandong Province from 2016 to 2019.</p>
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<p>Average total concentration of PM<sub>2.5</sub> in spring, summer, autumn and winter in Shandong Province from 2016 to 2019.</p>
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12 pages, 1032 KiB  
Article
Rapid In-Field Detection of Airborne Pathogens Using Loop-Mediated Isothermal Amplification (LAMP)
by Alessia Bani, Corinne Whitby, Ian Colbeck, Alex J. Dumbrell and Robert M. W. Ferguson
Microorganisms 2024, 12(12), 2578; https://doi.org/10.3390/microorganisms12122578 - 13 Dec 2024
Viewed by 427
Abstract
Multiple human and plant pathogens are dispersed and transmitted as bioaerosols (e.g., Mycobacterium tuberculosis, SARS-CoV-2, Legionella pneumophila, Aspergillus fumigatus, Phytophthora spp., and Fusarium graminearum). Rapid, on-site methods to detect airborne pathogens would greatly enhance our ability to monitor exposure [...] Read more.
Multiple human and plant pathogens are dispersed and transmitted as bioaerosols (e.g., Mycobacterium tuberculosis, SARS-CoV-2, Legionella pneumophila, Aspergillus fumigatus, Phytophthora spp., and Fusarium graminearum). Rapid, on-site methods to detect airborne pathogens would greatly enhance our ability to monitor exposure and trigger early mitigation measures across different settings. Analysis of air samples for microorganisms in a regulatory context is often based on culture-based methods, which are slow, lack specificity, and are not suitable for detecting viruses. Molecular methods (based on nucleic acids) could overcome these challenges. For example, loop-mediated isothermal amplification (LAMP) is rapid, sensitive, specific, and may detect microbial pathogens from air samples in under 60 min. However, the low biomass in air samples makes recovering sufficient nucleic acids for detection challenging. To overcome this, we present a simple method for concentrating bioaerosols collected through liquid impingement (one of the most common methods for bioaerosol collection). This method paired with LAMP (or other molecular approaches) offers simple, rapid, and sensitive detection of pathogens. We validated this method using three airborne pathogens (Mycobacterium tuberculosis, Legionella pneumophila, and Aspergillus fumigatus), and we were able to detect fewer than five cells in a 15 mL liquid impinger air sample in under 60 min. This simple method offers rapid pathogen detection without the use of specialist equipment, and it can be used across healthcare, education, environmental monitoring, and military settings. Full article
(This article belongs to the Special Issue Detection and Identification of Pathogenic Bacteria and Viruses)
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<p>Workflow for rapid detection of airborne pathogens, from the air sample to the result in under 60 min.</p>
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<p>(<b>A</b>) Gel electrophoresis image of LAMP products and (<b>B</b>) reaction tubes at 0, 30, and 50 min for LAMP assay for the <span class="html-italic">E. coli malB</span> gene. Yellow color indicates positive LAMP reaction, orange indicates negative reaction. L = ladder (1 KB); the number indicates the number of cells in the reaction. <span class="html-italic">Rhodococcus</span> sp. negative control contained (10<sup>4</sup> cells reaction<sup>−1</sup>). NTC = No template control (i.e., PCR-grade water in place of DNA template/cells).</p>
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17 pages, 2453 KiB  
Article
Development and Characterization of Novel Combinations and Compositions of Nanostructured Lipid Carrier Formulations Loaded with Trans-Resveratrol for Pulmonary Drug Delivery
by Iftikhar Khan, Sunita Sunita, Nozad R. Hussein, Huner K. Omer, Abdelbary Elhissi, Chahinez Houacine, Wasiq Khan, Sakib Yousaf and Hassaan A. Rathore
Pharmaceutics 2024, 16(12), 1589; https://doi.org/10.3390/pharmaceutics16121589 - 12 Dec 2024
Viewed by 580
Abstract
Background/Objectives: This study aimed to fabricate, optimize, and characterize nanostructured lipid carriers (NLCs) loaded with trans-resveratrol (TRES) as an anti-cancer drug for pulmonary drug delivery using medical nebulizers. Methods: Novel TRES-NLC formulations (F1–F24) were prepared via hot, high-pressure homogenization. One solid lipid (Dynasan [...] Read more.
Background/Objectives: This study aimed to fabricate, optimize, and characterize nanostructured lipid carriers (NLCs) loaded with trans-resveratrol (TRES) as an anti-cancer drug for pulmonary drug delivery using medical nebulizers. Methods: Novel TRES-NLC formulations (F1–F24) were prepared via hot, high-pressure homogenization. One solid lipid (Dynasan 116) was combined with four liquid lipids (Capryol 90, Lauroglycol 90, Miglyol 810, and Tributyrin) in three different ratios (10:90, 50:50, and 90:10 w/w), with a surfactant (Tween 80) in two different concentrations (0.5 and 1.5%), and a co-surfactant, soya phosphatidylcholine (SPC S-75; 50 mg). Results: Amongst the analyzed 24 TR-NLC formulations, F8, F14, and F22 were selected based on their physicochemical stability when freshly prepared and following storage (4 weeks 25 °C), as well as in terms of particle size (<145 nm), polydispersity index (PDI; <0.21) and entrapment efficiency (>96%). Furthermore, F14 showed greater stability at 4 and 25 °C for six months and exhibited enhanced aerosolization performance, demonstrating the greater deposition of TRES in the later stages of the next-generation impactor (NGI) when using an air-jet nebulizer than when using an ultrasonic nebulizer. The F14 formulation exhibited greater stability and release in acetate buffer (pH 5.4), with a cumulative release of 95%. Conclusions: Overall, formulation F14 in combination with an air-jet nebulizer was identified as a superior combination, demonstrating higher emitted dose (ED; 80%), fine particle dose (FPD; 1150 µg), fine particle fraction (FPF; 24%), and respirable fraction (RF; 94%). These findings are promising in the optimization and development of NLC formulations, highlighting their versatility and targeting the pulmonary system via nebulization. Full article
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<p>Transmission electron microscopy (TEM) images of TRES-NLC formulations (with 200 nm scale bar): (<b>A</b>) F8, (<b>B</b>) F14, and (<b>C</b>) F22. These images are typical of the three different batches.</p>
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<p>Deposition and analysis of aerosol droplets containing TRES-NLC particles of various formulations (F8, F14, and F22) in the various stages of a next-generation impactor (NGI) using (<b>A</b>) air-jet and (<b>B</b>) ultrasonic nebulizers at an airflow rate of 15 L/min. Data are presented as mean ± SD, n = 3.</p>
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<p>Deposition of TRES using TRES-NLC formulation F14 in various stages (1–8) of NGI via air-jet and ultrasonic nebulizers. Data are mean ± SD, n = 3.</p>
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<p>Nebulization performance, including the (<b>A</b>) nebulization time to “dryness” (min), (<b>B</b>) mass output (%), and (<b>C</b>) output rate (mg/min) of TRES-NLC formulation F14. Data are mean ± SD, n = 3.</p>
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<p>In vitro release of TRES from TRES-NLC formulation F14 (solid lines) and TRES as a free drug alone (doted lines) in two dissolution media, including water (pH 7) and acetate buffer (pH 5.4). Data are mean ± SD, n = 3.</p>
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20 pages, 13045 KiB  
Article
A Sequence-to-Sequence Transformer Model for Satellite Retrieval of Aerosol Optical and Microphysical Parameters from Space
by Luo Zhang, Haoran Gu, Zhengqiang Li, Zhenhai Liu, Ying Zhang, Yisong Xie, Zihan Zhang, Zhe Ji, Zhiyu Li and Chaoyu Yan
Remote Sens. 2024, 16(24), 4659; https://doi.org/10.3390/rs16244659 - 12 Dec 2024
Viewed by 368
Abstract
Aerosol optical and microphysical properties determine their radiative capabilities, climatic impacts, and health effects. Satellite remote sensing is a crucial tool for obtaining aerosol parameters on a global scale. However, traditional physical and statistical retrieval methods face bottlenecks in data mining capacity as [...] Read more.
Aerosol optical and microphysical properties determine their radiative capabilities, climatic impacts, and health effects. Satellite remote sensing is a crucial tool for obtaining aerosol parameters on a global scale. However, traditional physical and statistical retrieval methods face bottlenecks in data mining capacity as the volume of satellite observation information increases rapidly. Artificial intelligence methods are increasingly applied to aerosol parameter retrieval, yet most current approaches focus on end-to-end single-parameter retrieval without considering the inherent relationships among multiple aerosol properties. In this study, we propose a sequence-to-sequence aerosol parameter joint retrieval algorithm based on the transformer model S2STM. Unlike conventional end-to-end single-parameter retrieval methods, this algorithm leverages the encoding–decoding capabilities of the transformer model, coupling multi-source data such as polarized satellite, meteorological, model, and surface characteristics, and incorporates a physically coherent consistency loss function. This approach transforms traditional single-parameter numerical regression into a sequence-to-sequence relationship mapping. We applied this algorithm to global observations from the Chinese polarimetric satellite (the Particulate Observing Scanning Polarimeter, POSP) and simultaneously retrieved multiple key aerosol optical and microphysical parameters. Event analyses, including dust and pollution episodes, demonstrate the method’s responsiveness in hotspot regions and events. The retrieval results show good agreement with ground-based observation products. This method is also adaptable to satellite instruments with various configurations (e.g., multi-wavelength, multi-angle, and multi-dimensional polarization) and can further improve its spatiotemporal generalization performance by enhancing the spatial balance of ground station training datasets. Full article
(This article belongs to the Section Atmospheric Remote Sensing)
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<p>Installation diagram of GF5-02 satellite polarization instruments.</p>
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<p>Schematic diagram of the S2STM structure.</p>
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<p>Comparison of model accuracy metrics under different input feature parameters.</p>
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<p>Scatter plots of S2STM model retrieval results validated against AERONET and SONET data.</p>
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<p>Global aerosol characteristics distribution and comparison with MODIS products. (<b>a</b>) Terra MODIS DTB AOD at 550 nm, (b) Terra MODIS DT AOD at 550 nm, (c) Terra MODIS DB AOD at 550 nm, (d) POSP retrieved AOD at 550 nm, (e) POSP retrieved <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>V</mi> </mrow> <mrow> <mi>c</mi> </mrow> </msub> </mrow> </semantics></math>, (f) POSP retrieved <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>V</mi> </mrow> <mrow> <mi>f</mi> </mrow> </msub> </mrow> </semantics></math>, (g) POSP retrieved SSA at 670 nm, (h) POSP retrieved <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>m</mi> </mrow> <mrow> <mi>r</mi> </mrow> </msub> </mrow> </semantics></math> at 670 nm, and (i) POSP retrieved <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>m</mi> </mrow> <mrow> <mi>i</mi> </mrow> </msub> </mrow> </semantics></math> at 670 nm.</p>
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<p>Similar to <a href="#remotesensing-16-04659-f005" class="html-fig">Figure 5</a> but showing the global distribution of various parameters for each season in 2022.</p>
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<p>Satellite remote sensing retrieval results of aerosol parameters over the Indian region on 21 April 2022.</p>
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<p>Satellite remote sensing retrieval results of aerosol parameters over the Amazon rainforest region on 1 September 2022.</p>
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