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22 pages, 12234 KiB  
Article
Enhanced Continental Weathering and Intense Upwelling Drove the Deposition of Organic-Rich Shales in the Late Permian Dalong Formation, South China
by Yin Gong, Yiming Li, Peng Yang, Meng Xiang, Zhou Zhou, Zhongquan Zhang, Xing Niu and Xiangrong Yang
J. Mar. Sci. Eng. 2025, 13(2), 357; https://doi.org/10.3390/jmse13020357 - 15 Feb 2025
Viewed by 416
Abstract
Marine black shales are important to geologists, because they are not only potential sources and reservoir rocks for shale gas/oil, but also, their deposition could influence the climatic and oceanic environments. Here, a detailed study of the shales in the Dalong Formation in [...] Read more.
Marine black shales are important to geologists, because they are not only potential sources and reservoir rocks for shale gas/oil, but also, their deposition could influence the climatic and oceanic environments. Here, a detailed study of the shales in the Dalong Formation in South China was conducted to understand the changes in continental weathering and upwelling and their influences on organic matter accumulation in the late Permian. The results revealed that the deposition of the Dalong and Daye Formations could be divided into five stages, with the highest TOC values (>2%) being observed in stages 2 and 4, intermediate TOCs (~1% to 2%) being observed in stages 1 and 3, and the lowest TOC values (<1%) being observed in stage 5. This study attributed the enhanced organic matter accumulation in stages 2 and 4 to enhanced continental weathering (high CIA values and δ26Mg values) and intense upwelling (high Mo/TOC ratios and low δ13Corg and CoEF × MnEF values), both of which contributed to high primary productivity and increased anoxia of the bottom waters, further leading to the accumulation of organic matter. Overall, both enhanced continental weathering and upwelling contributed to the development of anoxia, even euxinia, of the seawater and further triggered an end-Permian mass extinction (EPME). Full article
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Graphical abstract

Graphical abstract
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<p>(<b>a</b>) Global paleogeography during the late Permian interval; (<b>b</b>) late Permian paleogeographic map, indicating the location of the studied section (Shuanghe section); (<b>c</b>) stratigraphic correlation map of Guadalupian series–Lopingian series in the western Hubei and Sichuan areas.</p>
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<p>(<b>a</b>) Boundary between lower and middle Dalong Formation; (<b>b</b>) siliceous shales with high organic matter contents in middle Dalong Formation; (<b>c</b>,<b>d</b>) yellowish-gray shales in Daye Formation; (<b>e</b>) black to gray-white shales in upper Dalong Formation; (<b>f</b>) yellowish-brown shales in lower Dalong Formation; (<b>g</b>) organic-rich shales in middle Dalong Formation; (<b>h</b>) organic-lean shales in lower Dalong Formation.</p>
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<p>Cross-plots of (<b>a</b>) Sc versus Th, (<b>b</b>) Hf versus La/Th, and (<b>c</b>) Zr versus Ti. (<b>d</b>) Plots of analyzed samples of SH on A-CN-K diagram. A: Al<sub>2</sub>O<sub>3</sub>; CN: CaO* + Na<sub>2</sub>O; K: K<sub>2</sub>O; To: tonalite; Gd: granodiorite; Gr: granite; Kln: kaolinite; Gbs: gibbsite; Chl: chlorite; Ilt: Illite; Ms: muscovite; Kfs: K-feldspar; Sme: Smectite. The arrows indicate the weathering trends for SH rocks.</p>
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<p>Cross-plots of CIA<sub>corr</sub> versus (<b>a</b>) Al<sub>2</sub>O<sub>3</sub>/SiO<sub>2</sub>, (<b>b</b>) CIW, (<b>c</b>) PIA, and (<b>d</b>) TOC; cross-plots of δ<sup>26</sup>Mg<sub>silicate</sub> versus (<b>e</b>) Al<sub>2</sub>O<sub>3</sub>/SiO<sub>2</sub> and (<b>f</b>) CIA<sub>corr</sub>.</p>
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<p>Stratigraphic TOC, δ<sup>26</sup>Mg<sub>silicate</sub>, CIA<sub>corr</sub>, CIA, δ<sup>13</sup>C<sub>org</sub>, Mo/TOC, and Co<sub>EF</sub> × Mn<sub>EF</sub> in the Shuanghe section.</p>
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<p>Stratigraphic C<sub>org</sub>/P, U<sub>EF</sub>, Mo<sub>EF</sub>, V<sub>EF</sub>, Mo/U, Si<sub>bio</sub>, and Ni/Al<sub>2</sub>O<sub>3</sub> data from the Shuanghe section.</p>
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<p>Cross-plots of vanadium enrichments against (<b>a</b>) molybdenum (Mo) and (<b>b</b>) uranium(U) enrichments for within and beneath perennial oxygen-minimum zones (P-OMZs) and normal oxic depositional environments [<a href="#B86-jmse-13-00357" class="html-bibr">86</a>].</p>
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<p>Deposition model for the Dalong to Daye Formations.</p>
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14 pages, 4866 KiB  
Article
Application of Composite Dry Powders for Simultaneous Fire Extinguishment and Liquid Solidification of Methanol
by Xiaomin Ni, Kai Zhang, Zhong Zheng, Wenjie Wang and Shi Hu
Fire 2025, 8(2), 69; https://doi.org/10.3390/fire8020069 - 7 Feb 2025
Viewed by 287
Abstract
Extinguishing methanol fires poses significant challenges due to methanol’s high toxicity, polarity, and fluidity. While conventional fire suppressants, such as alcohol-resistant firefighting foam, water mist and dry powders, can extinguish methanol fires, they fail to prevent the spread of liquid methanol, creating a [...] Read more.
Extinguishing methanol fires poses significant challenges due to methanol’s high toxicity, polarity, and fluidity. While conventional fire suppressants, such as alcohol-resistant firefighting foam, water mist and dry powders, can extinguish methanol fires, they fail to prevent the spread of liquid methanol, creating a risk of environmental contamination as the mixture of suppressants and methanol flows into surrounding soil and water resources. To address this issue, a novel kind of composite dry powder has been developed to effectively combat methanol pool fires. The powder can not only rapidly extinguish flames but also transform liquid methanol into gel-like substances, significantly reducing the hazards caused by the flow of harmful liquids. Laboratory experiments identify an optimal mass ratio of 0.16 between the composite powder and methanol to achieve complete flame extinction and liquid solidification. The superior performance of as-prepared composite powder could be mainly ascribed to the cooperation of metallic salts, polymers, and silica additives. Additionally, the powder is effective for extinguishing ethanol fires, making it a valuable tool for the emergency management of alcohol fires in leakage incidents. Full article
(This article belongs to the Special Issue Composite Fire Suppressants)
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<p>(<b>a</b>,<b>b</b>) SEM images of the KC-AC composite without silica addition; (<b>c</b>–<b>e</b>) SEM images of the composite with the addition of silica; (<b>f</b>) EDS pattern of the particle surface as marked in (<b>e</b>).</p>
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<p>Images of the contact angle (<b>top row</b>), SEM (<b>middle row</b>), and the repose angle (<b>bottom row</b>) of the samples with different contents of silica: MPS-1 (<b>a</b>,<b>f</b>,<b>k</b>); MPS-2 (<b>b</b>,<b>g</b>,<b>l</b>); MPS-3 (<b>c</b>,<b>h</b>,<b>m</b>); MPS-4 (<b>d</b>,<b>i</b>,<b>n</b>); MPS-5 (<b>e</b>,<b>j</b>,<b>o</b>).</p>
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<p>Typical images of fire suppression process with different composite powders: (<b>a</b>) MPS-7, (<b>b</b>) MPS-8.</p>
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<p>Temperature variations recorded by thermocouples in the tests with the two samples as fire-extinguishing agents: (<b>a</b>) MPS-7, (<b>b</b>) MPS-8.</p>
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<p>Images of the mixture of methanol and different composite powders in the fuel pan of 3 fire tests: (<b>a</b>) MPS-6, (<b>b</b>) MPS-7, and (<b>c</b>) MPS-8.</p>
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<p>Typical SEM images of the gel-like product after fire tests: (<b>a</b>) a panoramic image, (<b>b</b>) image of the linked particles, (<b>c</b>) magnified image of the particle surface, (<b>d</b>) details of the particle surface.</p>
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<p>Schematic illustration of the behaviors of composite particles in flame extinguishment and the solidification of alcohol liquid.</p>
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14 pages, 4800 KiB  
Article
Design and Analysis of Compact High–Performance Lithium–Niobate Electro–Optic Modulator Based on a Racetrack Resonator
by Zixin Chen, Jianping Li, Weiqin Zheng, Hongkang Liu, Quandong Huang, Ya Han and Yuwen Qin
Photonics 2025, 12(1), 85; https://doi.org/10.3390/photonics12010085 - 17 Jan 2025
Viewed by 729
Abstract
With the ever-growing demand for high-speed optical communications, microwave photonics, and quantum key distribution systems, compact electro-optic (EO) modulators with high extinction ratios, large bandwidth, and high tuning efficiency are urgently pursued. However, most integrated lithium–niobate (LN) modulators cannot achieve these high performances [...] Read more.
With the ever-growing demand for high-speed optical communications, microwave photonics, and quantum key distribution systems, compact electro-optic (EO) modulators with high extinction ratios, large bandwidth, and high tuning efficiency are urgently pursued. However, most integrated lithium–niobate (LN) modulators cannot achieve these high performances simultaneously. In this paper, we propose an improved theoretical model of a chip-scale electro-optic (EO) microring modulator (EO-MRM) based on X-cut lithium–niobate-on-insulator (LNOI) with a hybrid architecture consisting of a 180-degree Euler bend in the coupling region, double-layer metal electrode structure, and ground–signal–signal–ground (G-S-S-G) electrode configuration, which can realize highly comprehensive performance and a compact footprint. After parameter optimization, the designed EO-MRM exhibited an extinction ratio of 38 dB. Compared to the structure without Euler bends, the increase was 35 dB. It also had a modulation bandwidth of 29 GHz and a tunability of 8.24 pm/V when the straight waveguide length was 100 μm. At the same time, the proposed device footprint was 1.92 × 104 μm2. The proposed MRM model provides an efficient solution to high-speed optical communication systems and microwave photonics, which is helpful for the fabrication of high-performance and multifunctional photonic integrated devices. Full article
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<p>(<b>a</b>) A schematic diagram of the proposed racetrack resonator with a double-layer electrode. Inset: the cross-section of coupling area. (<b>b</b>) A top view of the racetrack microring resonator. (<b>c</b>) The optical mode field and intensity distribution of the Euler bend with a waveguide width of 0.8 µm, simulated by FDTD.</p>
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<p>(<b>a</b>) Lumerical MODE simulation of the fundamental TE<sub>0</sub> optical mode of the waveguide. (<b>b</b>) The calculated optical effective index of the waveguide.</p>
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<p>(<b>a</b>) The coupling coefficient <span class="html-italic">κ</span><sup>2</sup> and (<b>b</b>) the transmission coefficient <span class="html-italic">t</span><sup>2</sup> vary with w<sub>gap</sub> in the coupling region at the wavelength of 1550 nm.</p>
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<p>(<b>a</b>) The coupling coefficient <span class="html-italic">κ</span><sup>2</sup> and (<b>b</b>) the transmission coefficient <span class="html-italic">t</span><sup>2</sup> vary with w<sub>1</sub> in the coupling region at the wavelength of 1550 nm.</p>
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<p>The BW and <span class="html-italic">Q</span> factor performances with the variation in <span class="html-italic">Lc</span> of the resonator.</p>
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<p>(<b>a</b>) The coupling and transmission coefficients with a variation in wavelength, when w<sub>gap</sub> = 0.7 μm and w<sub>1</sub> = 0.6 μm. (<b>b</b>) Transmission spectrum of the resonator with different bends used in the coupling region at the wavelength of 1550 nm.</p>
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<p>(<b>a</b>) A top view of the proposed tunable racetrack resonator with double-layer electrodes. (<b>b</b>) The simulated TE optical mode field profile at 1550 nm and the electric field between the double-layer electrodes. Here, the TFLN waveguide was formed by a 300 nm × 0.8 µm LN loading ridge. (<b>c</b>) A schematic of a unit cell of the electrode structure. (<b>d</b>) The simulation result of the influence of h and d on metal loss.</p>
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<p>Metal loss analysis for different electrode designs. (<b>a</b>) Metal electrodes were placed directly on the waveguide. (<b>b</b>) A 2.8 μm-wide layer of SiO<sub>2</sub> was added between the double metal electrode and the waveguide.</p>
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<p>(<b>a</b>) The simulated transmission spectrum of the TE mode of the passive racetrack resonator. (<b>b</b>) The detailed spectrum at 1550.118 nm. (<b>c</b>) The spectrum under different voltages of the TE mode at 1550.118 nm. (<b>d</b>) Resonant wavelength shifts as a function of the applied voltage.</p>
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22 pages, 6110 KiB  
Article
Air–Ice–Water Temperature and Radiation Transfer via Different Surface Coverings in Ice-Covered Qinghai Lake of the Tibetan Plateau
by Ruijia Niu, Lijuan Wen, Chan Wang, Hong Tang and Matti Leppäranta
Water 2025, 17(2), 142; https://doi.org/10.3390/w17020142 - 8 Jan 2025
Viewed by 526
Abstract
There are numerous lakes in the Tibetan Plateau (TP) that significantly impact regional climate and aquatic ecosystems, which often freeze seasonally owing to the high altitude. However, the special warming mechanisms of lake water under ice during the frozen period are poorly understood, [...] Read more.
There are numerous lakes in the Tibetan Plateau (TP) that significantly impact regional climate and aquatic ecosystems, which often freeze seasonally owing to the high altitude. However, the special warming mechanisms of lake water under ice during the frozen period are poorly understood, particularly in terms of solar radiation penetration through lake ice. The limited understanding of these processes has posed challenges to advancing lake models and improving the understanding of air–lake energy exchange during the ice-covered period. To address this, a field experiment was conducted at Qinghai Lake, the largest lake in China, in February 2022 to systematically examine thermal conditions and radiation transfer across air–ice–water interfaces. High-resolution remote sensing technologies (ultrasonic instrument and acoustic Doppler devices) were used to observe the lake surface changes, and MODIS imagery was also used to validate differences in lake surface conditions. Results showed that the water temperature under the ice warmed steadily before the ice melted. The observation period was divided into three stages based on surface condition: snow stage, sand stage, and bare ice stage. In the snow and sand stages, the lake water temperature was lower due to reduced solar radiation penetration caused by high surface reflectance (61% for 2 cm of snow) and strong absorption by 8 cm of sand (absorption-to-transmission ratio of 0.96). In contrast, during the bare ice stage, a low reflectance rate (17%) and medium absorption-to-transmission ratio (0.86) allowed 11% of solar radiation to penetrate the ice, reaching 11.70 W·m−2, which increased the water temperature across the under-ice layer, with an extinction coefficient for lake water of 0.39 (±0.03) m−1. Surface coverings also significantly influenced ice temperature. During the bare ice stage, the ice exhibited the lowest average temperature and the greatest diurnal variations. This was attributed to the highest daytime radiation absorption, as indicated by a light extinction coefficient of 5.36 (±0.17) m−1, combined with the absence of insulation properties at night. This study enhances understanding of the characteristics of water/ice temperature and air–ice–water solar radiation transfer through effects of different ice coverings (snow, sand, and ice) in Qinghai Lake and provides key optical radiation parameters and in situ observations for the refinement of TP lake models, especially in the ice-covered period. Full article
(This article belongs to the Special Issue Ice and Snow Properties and Their Applications)
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<p>(<b>a</b>) Overview of Qinghai Lake, with the observation location marked by a red pentagram. (<b>b</b>) Layout of the observational instrumentation. (<b>c</b>–<b>f</b>) Instrument setup, manual snow thickness measurements, and lake ice thickness measurements via drilling.</p>
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<p>(<b>a</b>,<b>c</b>) Daily and (<b>b</b>,<b>d</b>) diurnal variations in (<b>a</b>,<b>b</b>) temperature and (<b>c</b>,<b>d</b>) wind speed at Qinghai Lake in 6–24 February 2022. The shaded areas in (<b>a</b>,<b>c</b>) correspond to the standard stages of lake cover: blue for snow, green for sand, and yellow for bare ice. Panels (<b>b</b>,<b>d</b>) display stage-averaged data for each variable. Note: Consistent with this article’s approach, the color coding in panels (<b>a</b>,<b>c</b>) is applied across all figures to represent the three distinct stages of the lake’s cover.</p>
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<p>Terra/MODIS images during the stable freezing period of Qinghai Lake in 6–24 February 2022, along with snapshots from the automatic weather station during the snow, sand, and bare ice stages. Two images from the automatic weather station are provided for each stage. The MODIS images are shown daily, except for 20 February, which has been removed due to distortion. Red corresponds to Band 3 (459–479 nm), green corresponds to Band 6 (1628–1652 nm), and blue corresponds to Band 7 (2105–2155 nm). Red areas represent ice and snow, cyan represents exposed soil, and white indicates small liquid water droplets in clouds. The lake surface is covered by a stable frozen ice layer.</p>
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<p>High-precision ultrasonic measurements of lake ice surface distances and thicknesses. The (<b>top</b>) graph depicts the distance from the sub-ice ultrasonic sensor to the underside of the ice, referred to as ’Under-ice’. The (<b>middle</b>) graph illustrates the distance from the ice surface ultrasonic sensor to the ice surface (or covering surface, if present), referred to as ’Surface-ice’. The (<b>bottom</b>) graph presents the combined thickness of the ice and any covering, measured from the top to the bottom surface, referred to as ’Ice and covering’.</p>
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<p>Temporal profiles of water temperature at various depths: (<b>a</b>) 12-hourly smoothed temperatures at 0.4 m, 0.5 m, 6.7 m, 8.7 m, and 12.7 m depths in February 2022; (<b>b</b>) 12-hourly smoothed temperatures at a depth of 2.1 m from February to April 2023, with the shaded area indicating the ice-covered period.</p>
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<p>(<b>a</b>) Thirty-minute average lake ice temperature and (<b>b</b>) vertical temperature profile.</p>
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<p>(<b>a</b>,<b>c</b>) Long-term trends and (<b>b</b>,<b>d</b>) daily variations in (<b>a</b>,<b>b</b>) solar shortwave radiation and (<b>c</b>,<b>d</b>) albedo. The lines in (<b>a</b>) denote downward (blue), upward (green), and net (yellow) shortwave radiation The shaded areas in (<b>b</b>,<b>d</b>) correspond to the snow (blue), sand (green), and bare ice (yellow) periods.</p>
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<p>(<b>a</b>) Long-term trend and (<b>b</b>–<b>d</b>) daily variations in underwater radiation at depths of 0.7 m, 2.1 m, and the ice bottom.</p>
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<p>Temporal variation in the attenuation coefficients of the lake water (blue) and lake ice (yellow). Dots represent values at 10-minute intervals, and lines represent the daily average.</p>
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<p>(<b>a</b>) Long-term trend and (<b>b</b>) daily variation in lake ice transmittance.</p>
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<p>Schematic diagram depicting radiation transfer within the air–ice–water system of Qinghai Lake. The blue dashed box shows the absorption-to-transmission ratio.</p>
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35 pages, 5466 KiB  
Article
A Comparison of Machine Learning-Based Approaches in Estimating Surface PM2.5 Concentrations Focusing on Artificial Neural Networks and High Pollution Events
by Shijin Wei, Kyle Shores and Yangyang Xu
Atmosphere 2025, 16(1), 48; https://doi.org/10.3390/atmos16010048 - 5 Jan 2025
Viewed by 967
Abstract
Surface PM2.5 concentrations have significant implications for human health, necessitating accurate estimations. This study compares various machine learning models, including linear models, tree-based algorithms, and artificial neural networks (ANNs) for estimating PM2.5 concentrations using the MERRA-2 dataset from 2012 to 2023. [...] Read more.
Surface PM2.5 concentrations have significant implications for human health, necessitating accurate estimations. This study compares various machine learning models, including linear models, tree-based algorithms, and artificial neural networks (ANNs) for estimating PM2.5 concentrations using the MERRA-2 dataset from 2012 to 2023. Mutual information and Spearman cross-feature correlation scores are used during feature selections. The performance of models is evaluated using metrics including normalized Nash–Sutcliffe efficiency (NNSE), root mean standard deviation ratio (RSR), and mean percentage error (MPE). Our results show that ANNs outperform linear and tree models, particularly in estimating daily PM2.5 concentrations of 35–1000 µg/m3. ANNs improve NNSE by 119% and 46%, RSR by 40% and 24%, and MPE by 44% and 30% from linear and tree models, respectively, indicating ANN’s superior estimation performance during high pollution days. The sensitivity analysis of features that interpret the models suggests that the total extinction AOD at 550 nm and surface CO concentrations are the most important features in the Western and Eastern U.S., respectively. The findings suggest that even the simplest NNs provide better air quality estimates, especially during high pollution events, which is beneficial for long-term exposure analysis. Future research should explore more sophisticated NN architectures with spatial and temporal variations in PM2.5 to improve the model performance. Full article
(This article belongs to the Section Atmospheric Techniques, Instruments, and Modeling)
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<p>Spearman cross-feature correlation scores of 15 final features after filtering the features with strong covariances, except for the first column that indicates the correlation between features and the target variable (PM<sub>2.5</sub>). Note that PM<sub>2.5</sub> is included in the correlation plot for reference, but the main purpose of the plot is to filter features with covariance. The correlation score of 0 means there is no monotonic relationship between features. Features with correlation scores closer to 1 or − 1 are considered to have a stronger monotonic relationship among them.</p>
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<p>(<b>a</b>) Kernel density distribution of PM<sub>2.5</sub> concentration estimated on the test set by individual ML models and the actual values in MERRA-2 from 0 to 50 µg/m<sup>3</sup> on the ln scale. (<b>b</b>) histogram density distribution of estimates from the averages of each model category and the actual values in MERRRA-2 from 0 to 50 µg/m<sup>3</sup>; (<b>c</b>) kernel density distribution of estimates from the averages of each model category and the actual values in MERRRA-2 from 1 to 100 µg/m<sup>3</sup> on the log10 scale; (<b>d</b>) kernel density distribution of estimates from the averages of each model category and the actual values in MERRRA-2 during high pollution days from 35 to 1000 µg/m<sup>3</sup> on the log10 scale. In panel (<b>a</b>), the blue, purple, red, and green colors represent linear models, tree models, ANN models, and true values, respectively. In panels (<b>b</b>–<b>d</b>), the blue, purple, and red bins and lines represent the average estimates of linear models, tree models (excluding AdaBoost), and ANN models, respectively; the dashed green bin and line represent true values. In panels (<b>b</b>,<b>c</b>), the yellow box represents the area where models overestimated the actual PM<sub>2.5</sub> concentrations, while the dark blue box represents the area where models underestimated the actual PM<sub>2.5</sub> concentrations.</p>
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<p>Scatter plots comparing the estimated PM<sub>2.5</sub> concentrations against the true PM<sub>2.5</sub> concentrations for averages of linear, tree, and ANN models under 3 scenarios. (<b>a</b>) Estimates from the averages of each model category and the actual values from 0 to 50 µg/m<sup>3</sup>; (<b>b</b>) estimates from the averages of each model category and the actual values from 1 to 100 µg/m<sup>3</sup> on the log10 scale; (<b>c</b>) estimates from the averages of each model category and the actual values during high pollution days from 35 to 1000 µg/m<sup>3</sup> on the log10 scale. The color gradient indicates the density of data points. Performance metrics (R<sup>2</sup>, RMSE, NNSE, RSR, MAE, and MPE) are displayed for each model category. The dashed line represents the unity line (y = x), and the solid line represents the best-fit line for each model category. The transition between the colors of light blue, medium blue, purple, pinkish purple, orange, and yellow defines the density visual range, moving from low to high density. The shadows in the figure occur in areas of overlapping density where the darker colors (purple, pinkish purple, orange, and yellow) dominate due to the higher concentrations of data.</p>
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<p>Spatial distribution of 2-year average actual concentrations of PM<sub>2.5</sub> and the mean percentage error (%) of model-averaged estimated concentrations of PM<sub>2.5</sub> in the scenarios of (<b>a</b>) actual PM<sub>2.5</sub> from 0 to 50 µg/m<sup>3</sup>; (<b>b</b>) log10 PM<sub>2.5</sub> from 0 to 2 (1–100 µg/m<sup>3</sup>); and (<b>c</b>) log10 PM<sub>2.5</sub> from 1.54 to 3 (35–1000 µg/m<sup>3</sup>).</p>
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<p>Spatial distribution of the seasonal mean percentage error (%) of model-averaged estimated concentrations of PM<sub>2.5</sub> in the scenario of PM<sub>2.5</sub> from 35 to 1000 µg/m<sup>3</sup> with log10 transformation. Panels (<b>a</b>–<b>d</b>) represent spring, summer, fall, and winter, respectively. The first plot in each panel represents the performance of linear models at each location; the middle plot shows the error difference between tree and linear models; and the last plot shows the error difference between ANN and tree models.</p>
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<p>Feature importance scores across four tree-based models (random forest, extra trees, gradient boosting, and XGBoost). Each bar represents the importance score of a specific feature as calculated by the model’s inherent feature importance method. The scores represent the relative contribution of each feature to the models’ predictions. Features are sorted in descending order of their total importance across all models, with grouped bars showing the individual contributions from each model for direct comparison.</p>
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<p>Spatial distribution of the 2-year average SHAP values at each location under the scenario when PM<sub>2.5</sub> ranges from 1 to 100 µg/m<sup>3</sup>. The positive SHAP values (red areas) indicate that the feature can increase the average estimated PM<sub>2.5</sub> concentrations, while the negative SHAP values (blue areas) indicate that the feature can decrease the average PM<sub>2.5</sub> estimations at certain locations. The white areas mean the feature has non-distinct impacts on the estimations.</p>
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14 pages, 13287 KiB  
Article
Large-Bandwidth Lithium Niobate Electro-Optic Modulator for Frequency-Division Multiplexing RFID Systems
by Xueting Luo, Zhenqian Gu, Chong Wang, Chao Fan and Weijia Zhang
Electronics 2024, 13(24), 5054; https://doi.org/10.3390/electronics13245054 - 23 Dec 2024
Viewed by 637
Abstract
In the face of increasingly complex application scenarios, there is an urgent need for (Radio Frequency Identification) RFID systems that are capable of accurately identifying microwave signals of different frequency bands. Based on the acumen detection characteristics of microwave signals by lithium niobate [...] Read more.
In the face of increasingly complex application scenarios, there is an urgent need for (Radio Frequency Identification) RFID systems that are capable of accurately identifying microwave signals of different frequency bands. Based on the acumen detection characteristics of microwave signals by lithium niobate electro-optic modulators, applying large-bandwidth thin-film lithium niobate electro-optic modulation to RFID systems can achieve efficient operation across multiple frequency bands. This study discusses, in detail, the design, simulation, fabrication, and testing process of the electro-optic modulator to obtain a high-performance, large-bandwidth lithium niobate electro-optic modulator. By using multilayer lithography techniques to prepare thick traveling-wave electrodes, the problem of irregular cross-sections during the fabrication of thick electrodes has been successfully reduced, improving the stability and controllability of the device. Test results show that the insertion loss of the electro-optic modulator is about 6 dB, the extinction ratio is 36.5 dB, the optical waveguide mode field is 1 μm, the full-band characteristic impedance is 50 Ω, the test bandwidth is 50 GHz, and the half-wave voltage is 1.8 V. Compared with existing optimization schemes, this design not only achieves a large bandwidth and a small half-wave voltage, but also proposes a new fabrication process scheme, optimizing the process and resulting in samples with stable performance. Full article
(This article belongs to the Special Issue RFID Applied to IoT Devices)
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<p>Cross-sectional view of the thin-film lithium niobate electro-optic modulator.</p>
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<p>Analysis diagrams of the electric field patterns generated by electrodes with different thicknesses: (<b>a</b>) the electric field pattern for an electrode thickness of 1 μm, (<b>b</b>) 3 μm, (<b>c</b>) 5 μm, and (<b>d</b>) 10 μm.</p>
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<p>(<b>a</b>) The influence of different electrode structure parameters on the effective refractive index; (<b>b</b>) the impact of different electrode structure parameters on the characteristic impedance.</p>
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<p>Lithium niobate electro-optic modulator fabrication process diagram.</p>
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<p>Traveling-wave electrode mask pattern.</p>
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<p>Under the microscope, the development effect of MZ optical waveguides.</p>
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<p>(<b>a</b>) A top view of the electrode surface under the metallographic microscope; (<b>b</b>) a top view of the electrode surface under the scanning electron microscope.</p>
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<p>(<b>a</b>) The left electrical signal introduction area; (<b>b</b>) the proper electrical signal introduction area.</p>
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<p>Photos of the prepared samples, with the left side showing the sample to be tested taken out from the self-adhesive box, and the right side showing the sample stored inside the self-adhesive box.</p>
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<p>Primary sources of insertion loss.</p>
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<p>Schematic diagram of the insertion loss testing system.</p>
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<p>Schematic diagram of near-field scanning technology for testing mode field.</p>
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<p>S-parameters test system schematic diagram.</p>
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<p>Test results of S-parameters for G-1, G-2, and G-3.</p>
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<p>Diagram of the half-wave voltage system tested by the frequency-doubling modulation method.</p>
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27 pages, 8318 KiB  
Article
Enhanced Continental Weathering Triggered the Anoxia of Seawater and Mass Extinctions During the Late Ordovician
by Pan Tang, Xiangrong Yang and Detian Yan
J. Mar. Sci. Eng. 2024, 12(12), 2237; https://doi.org/10.3390/jmse12122237 - 5 Dec 2024
Viewed by 759
Abstract
During the Late Ordovician period, changes in climate and mass extinctions were observed; however, the factors influencing these phenomena have not been fully understood. In order to understand the relationships among redox water conditions, climates, and mass extinctions in the Late Ordovician, this [...] Read more.
During the Late Ordovician period, changes in climate and mass extinctions were observed; however, the factors influencing these phenomena have not been fully understood. In order to understand the relationships among redox water conditions, climates, and mass extinctions in the Late Ordovician, this study analyzes the chemical index of alteration (CIA) in shales and 87Sr/86Sr in carbonate leachates as proxies of changes in chemical weathering intensity and chemical weathering rate in the Late Ordovician (mainly from Katian to Hirnantian). The results show that an enhanced chemical weathering rate (increased 87Sr/86Sr ratios) and decreased chemical weathering intensity (decreased CIA values) characterized the late Katian, which might be attributed to the global orogenesis and enhanced precipitation/runoff under the warming climate (late-Boda warming). This enhanced chemical weathering rate contributed to the CO2 drawdown in the P. pacificus biozone, corresponding to the initiation of cooling and further glaciation. Meanwhile, the enhanced weathering-induced high primary productivity could have contributed to the expansion of anoxic seawater in the Katian, which further caused the Katian extinction. The Hirnantian Glaciation was characterized by high 87Sr/86Sr ratios in carbonates and extremely low CIA values in shales, which were likely related to the exposure of continents during low sea level and the glacial grinding of unweathered rocks. This study shows that the highest denudation rate and lowest chemical weathering intensity in the Hirnantian stage might have resulted in enhanced CO2 release and contributed to the end of glaciation. Full article
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<p>(<b>A</b>) Global paleogeography(~440 Ma, modified after <a href="http://deeptimemaps.com" target="_blank">http://deeptimemaps.com</a>, accessed on 1 January 2023) during the Late Ordovician and Early Silurian period. 1: Dob’s Linn section, Scotland; 2: Vinini Creek section, Nevada; 3: Monitor Range, Nevada; 4: Holy Cross Mountains; 5: Parahio Valley India Himalaya section, India. (<b>B</b>) Early Silurian paleogeographic map showing the distribution of the lithofacies of the Yangtze area [<a href="#B43-jmse-12-02237" class="html-bibr">43</a>] showing the sites Wuke (WK), Shuanghe (SH), Tianjiawan (TJW), Mouchuangou (MCG), Qiliao (QL) sections and DY3, XY-1, YD1, Yihuang-1 (YH-1), Shenci-1 (SC-1) boreholes. (<b>C</b>) Time scale and graptolite biozones are from [<a href="#B46-jmse-12-02237" class="html-bibr">46</a>,<a href="#B47-jmse-12-02237" class="html-bibr">47</a>]; generic diversity across Late Ordovician to Early Silurian is from [<a href="#B10-jmse-12-02237" class="html-bibr">10</a>].</p>
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<p>Stratigraphic CIA, CIA<sub>corr</sub>, CIW, PIA, K/Rb, ICV, and Al/Si of the Wufeng Formation and Guanyinqiao Member in DY3 and YD1 boreholes. The orange area represents the period of late-Boda warming climate, the black dotted lines represents 210 for K/Rb ratio and 1 for ICV [<a href="#B56-jmse-12-02237" class="html-bibr">56</a>,<a href="#B57-jmse-12-02237" class="html-bibr">57</a>], with high K/Rb ratios indicating minor potassium metasomatism and low ICV values indicating mature mudstones. Sil.: Silurian, Rhu.: Rhuddanian, LMX: Longmaxi Formation.</p>
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<p>δ<sup>13</sup>C profiles of the Late Ordovician–Early Silurian strata in the Wuke, TJW, QL, Vinini Creek, and Parahio Valley India Himalaya [<a href="#B59-jmse-12-02237" class="html-bibr">59</a>,<a href="#B60-jmse-12-02237" class="html-bibr">60</a>,<a href="#B61-jmse-12-02237" class="html-bibr">61</a>]. The sea surface temperature is based on the clumped oxygen isotope data [<a href="#B62-jmse-12-02237" class="html-bibr">62</a>]. The pink and orange areas represent the periods of early and late-Boda warming climates, respectively. Sil.: Silurian, Rhu.: Rhuddanian, GYQ: Guanyinqiao Formation.</p>
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<p>Crossplots of CIA<sub>corr</sub> versus (<b>A</b>) CIA, (<b>B</b>) PIA, and (<b>C</b>) CIW. (<b>D</b>) Plots of analyzed samples of DY3 and YD1 on the A-CN-K diagram [<a href="#B49-jmse-12-02237" class="html-bibr">49</a>,<a href="#B50-jmse-12-02237" class="html-bibr">50</a>,<a href="#B51-jmse-12-02237" class="html-bibr">51</a>]. A: Al<sub>2</sub>O<sub>3</sub>, CN: CaO* + Na<sub>2</sub>O, K: K<sub>2</sub>O, To: tonalite, Gd: granodiorite, Gr: granite, Kln: kaolinite, Gbs: gibbsite, Chl: chlorite, Ilt: Illite, Ms: muscovite, Kfs: K-feldspar. The arrows represent the weathering trends for YD1 and DY3 rocks. Crossplots of CIA<sub>corr</sub> versus (<b>E</b>) ICV, (<b>F</b>) Al/Si. The black dotted line in (<b>D</b>) represents 1 for ICV [<a href="#B67-jmse-12-02237" class="html-bibr">67</a>], with low ICV values indicating mature mudstones.</p>
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<p>Crossplots of (<b>A</b>) Hf versus La/Th, (<b>B</b>) Sc/Th versus La/Sc, and (<b>C</b>) Mo<sub>EF</sub> versus U<sub>EF</sub>; the SW means the ratio of Mo<sub>EF</sub>/U<sub>EF</sub> in modern seawater, the solid lines reflect the changes in redox water conditions, restricted and upwelling settings [<a href="#B70-jmse-12-02237" class="html-bibr">70</a>,<a href="#B71-jmse-12-02237" class="html-bibr">71</a>]. (<b>D</b>) Mn × Co versus Al<sub>2</sub>O<sub>3</sub>; the dotted line represents the boundary value (0.4) between restricted and upwelling settings [<a href="#B72-jmse-12-02237" class="html-bibr">72</a>]. All the major and trace elements used above are analyzed for whole rocks from [<a href="#B58-jmse-12-02237" class="html-bibr">58</a>].</p>
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<p>Stratigraphic δ<sup>13</sup>C<sub>org</sub>, δ<sup>13</sup>C<sub>carb</sub>, <sup>87</sup>Sr/<sup>86</sup>Sr, Mn/Sr, Sr/Ca, and mineralogy of the Linxiang and Tiezufeike formations in WK section. The sea surface temperature is based on the clumped oxygen isotope data [<a href="#B62-jmse-12-02237" class="html-bibr">62</a>]. The pink and orange areas represent the periods of early and late-Boda warming climates, respectively. Sil.: Silurian, Rhu.: Rhuddanian.</p>
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<p>Crossplots of <sup>87</sup>Sr/<sup>86</sup>Sr versus (<b>A</b>) Mn/Sr, (<b>B</b>) Sr/Ca, (<b>C</b>) δ<sup>18</sup>O, and (<b>D</b>) Mg/Ca.</p>
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<p>Correlation of CIA and CIA<sub>corr</sub> in the SD1, DY3 (this study), SH, QL, XY-1, YD1(this study), and Dob’s Linn [<a href="#B16-jmse-12-02237" class="html-bibr">16</a>,<a href="#B59-jmse-12-02237" class="html-bibr">59</a>]. The orange area represents the period of late-Boda warming climates. Sil.: Silurian, Rhu.: Rhuddanian, LMX: Longmaxi.</p>
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<p>Stratigraphic <sup>87</sup>Sr/<sup>86</sup>Sr of the Late Ordovician sediments in WK (this study), Swift Current core, Copenhagen Canyon sections [<a href="#B79-jmse-12-02237" class="html-bibr">79</a>,<a href="#B81-jmse-12-02237" class="html-bibr">81</a>]. The orange area represents the period of late-Boda warming climates. Sil.: Silurian, Rhu.: Rhuddanian, LMX: Longmaxi.</p>
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<p>Trends in CIA<sub>corr</sub>, <sup>87</sup>Sr/<sup>88</sup>Sr (this study), and δ<sup>34</sup>S in carbonate-associated sulfate (CAS). Generic diversity, Katian, and Hirnantian extinctions are based on [<a href="#B10-jmse-12-02237" class="html-bibr">10</a>]. Global anoxia event is based on [<a href="#B17-jmse-12-02237" class="html-bibr">17</a>]. The gray brand represents the CIA values for UCC (upper continental crust). Grap.: Graptolite Biozone, <span class="html-italic">D. compla.</span>-<span class="html-italic">D.comple.</span>: <span class="html-italic">Dicellograptus complanatus</span>-<span class="html-italic">Dicellograptus complexus</span>, <span class="html-italic">M.e.</span>-<span class="html-italic">M. p.</span>: <span class="html-italic">Metabolograptus extraodinarius</span>-<span class="html-italic">Metabolograptus persculptus</span>.</p>
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<p>Relationship between denudation rate and chemical weathering rate [<a href="#B28-jmse-12-02237" class="html-bibr">28</a>,<a href="#B32-jmse-12-02237" class="html-bibr">32</a>]. The gray line shows a linear relation under mineral-supply limited regimes and a nonlinear relation in kinetically limited regimes. Peak weathering rate and CO<sub>2</sub> drawdown occurs with moderate erosion rate; in contrast, low and high erosion rates would decrease or even reverses CO<sub>2</sub> sequestration. The red square represents the early Kaitan, with low denudation rate and high chemical weathering intensity. The orange square represents the late Kaitan, with intermediate denudation rate and intermediate chemical weathering intensity. The blue square represents the Hirnantian with high denudation rate and low chemical weathering intensity.</p>
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<p>Scheme illustrating redox dynamics during the Ordovician and Silurian transition; the data are from [<a href="#B14-jmse-12-02237" class="html-bibr">14</a>,<a href="#B16-jmse-12-02237" class="html-bibr">16</a>,<a href="#B59-jmse-12-02237" class="html-bibr">59</a>].</p>
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8 pages, 3202 KiB  
Communication
Optimization Design and Simulation of Coin-Slot-Type Anti-Resonant Fiber Structure for 2 μm Transmission
by Boyue Zhang, Zhaoyang Tian, Yu Li, Xinyang Su, Hongxiang Chi, Zikun Nie, Xiaoyu Luo, Bohan Li, Tianran Sun, Sergey Sarkisov and Sergey Kobtsev
Photonics 2024, 11(12), 1109; https://doi.org/10.3390/photonics11121109 - 23 Nov 2024
Viewed by 801
Abstract
In this work, we propose a new type of hollow-core anti-resonant fiber (HC-ARF) structure called a coin-slot structure. In this type of structure, two more layers of glass walls are added into the outer cladding capillary, which can effectively prevent light from leaking [...] Read more.
In this work, we propose a new type of hollow-core anti-resonant fiber (HC-ARF) structure called a coin-slot structure. In this type of structure, two more layers of glass walls are added into the outer cladding capillary, which can effectively prevent light from leaking out of the fiber. In aiming to explore the influence of the outer resonant tube on loss at a wavelength of 2 μm, the fundamental mode loss, high-order mode loss, and higher-order mode extinction ratio (HOMER) under different geometric parameters are studied. Full article
(This article belongs to the Special Issue Advanced Fiber Laser Technology and Its Application)
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<p>Schematic diagram of circular coin-slot-type HC-ARF optical fiber structure.</p>
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<p>Transmission loss diagram of circular coin-slot HC-ARF.</p>
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<p>(<b>a</b>) Transmission loss spectra of coin-slot-type HC-ARF at different bending radii; (<b>b</b>) the transmission loss of coin-slot-type HC-ARF under different bending radii at a wavelength of 2 μm.</p>
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<p>Schematic diagram of the structure of the coin-slot-type HC-ARF.</p>
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<p>(<b>a</b>) Transmission loss at different cutting depths; (<b>b</b>) HOMER at different cutting depths; (<b>c</b>) Transmission losses corresponding to different wavelengths at the optimal cutting depth.</p>
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11 pages, 9793 KiB  
Article
High-Extinction Photonic Filters by Cascaded Mach–Zehnder Interferometer-Coupled Resonators
by Hao-Zhong Chen, Kung-Lin Ho and Pei-Hsun Wang
Photonics 2024, 11(11), 1055; https://doi.org/10.3390/photonics11111055 - 10 Nov 2024
Viewed by 1639
Abstract
In this study, we demonstrate high-extinction stop-band photonic filters based on Mach–Zehnder interferometer (MZI)-coupled silicon nitride (Si3N4) resonators fabricated using I-line lithography technology. Leveraging the low-loss silicon nitride waveguide, our approach enables the creation of stable, high-performance filters suitable [...] Read more.
In this study, we demonstrate high-extinction stop-band photonic filters based on Mach–Zehnder interferometer (MZI)-coupled silicon nitride (Si3N4) resonators fabricated using I-line lithography technology. Leveraging the low-loss silicon nitride waveguide, our approach enables the creation of stable, high-performance filters suitable for applications in quantum and nonlinear photonics. With destructive interference at the feedback loop, photonic filters with an extinction ratio of 35 dB are demonstrated with four cascaded MZI-coupled resonators. This cascading design not only enhances the filter’s extinction but also improves its spectral sharpness, providing a more selective stop-band profile. Experimental results agree well with the theoretical results, showing linear scaling of extinction ratios with the number of cascaded MZI-coupled resonators. The scalability of this architecture opens the possibility for further integration and optimization in complex photonic circuits, where high extinction ratios and precise wavelength selectivity are critical for advanced signal processing and quantum information applications. Full article
(This article belongs to the Special Issue Silicon Photonics Devices and Integrated Circuits)
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<p>Schematic diagram of MZI-coupled resonator structure.</p>
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<p>(<b>a</b>) Simulation modal of the Si<sub>3</sub>N<sub>4</sub> waveguides; (<b>b</b>) simulated mode profiles of TE modes with the waveguide width of 1 μm and 3 μm, respectively.</p>
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<p>Exemplary schematics of (<b>a</b>) single-ring and (<b>b</b>) 4-cascaded MZI-coupled resonators.</p>
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<p>Simulated transmission spectra of (<b>a</b>) single-ring and (<b>b</b>) 2-, (<b>c</b>) 3-, and (<b>d</b>) 4-cascaded MZI-coupled resonators. (<b>e</b>) The zoom-in spectrum of a resonance in (<b>d</b>).</p>
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<p>Simulated transmission spectrum of a single-ring MZI-coupled resonator.</p>
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<p>Simulated transmission spectra of a single-ring MZI-coupled resonator by tuning the parameters of the feedback loop with (<b>a</b>) effective index = 1.68 and (<b>b</b>) feedback length = 2πR.</p>
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<p>The fabrication process of cascaded MZI-coupled resonators.</p>
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<p>Layout designs of (<b>a</b>) single-ring and (<b>b</b>) 4-cascaded MZI-coupled resonators.</p>
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<p>OM images of (<b>a</b>) single-ring and (<b>b</b>) 4-cascaded MZI-coupled resonators.</p>
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<p>Experimental setup for optical characterization.</p>
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<p>(<b>a</b>) OM image of the single-ring resonator; (<b>b</b>) measured transmission spectra of the single-ring resonator; (<b>c</b>) zoomed-in spectrum and fitted curve.</p>
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<p>Transmission spectra and zoomed-in spectra of (<b>a</b>) single-ring and (<b>b</b>) 4-cascaded MZI-coupled resonators.</p>
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<p>Simulated transmission and the zoomed-in spectra of 4-cascaded MZI resonators with difference effective indices.</p>
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10 pages, 1304 KiB  
Article
Theoretical Analysis on Active Polarization Control of Fiber Laser Based on Root Mean Square Propagation Algorithm
by Yifei Shi, Yunfeng Qi, Hui Shen, Zhao Quan and Ming Tang
Appl. Sci. 2024, 14(21), 9691; https://doi.org/10.3390/app14219691 - 23 Oct 2024
Viewed by 1063
Abstract
High-power linearly polarized fiber lasers are widely used in coherent beam combination, nonlinear frequency conversion, and gravitational wave detection. With the increase in output power, it is challenging for fiber lasers to maintain a high polarization extinction ratio (PER). Combined with intelligent techniques, [...] Read more.
High-power linearly polarized fiber lasers are widely used in coherent beam combination, nonlinear frequency conversion, and gravitational wave detection. With the increase in output power, it is challenging for fiber lasers to maintain a high polarization extinction ratio (PER). Combined with intelligent techniques, active polarization control is a prospective method to obtain the laser output with high PER and high stability. We demonstrate a comprehensive model of an active polarization control system. The root mean square propagation (RMS-Prop) algorithm is used to control the non-polarization-maintaining (non-PM) fiber laser to generate linearly polarized laser. The parameters of the RMS-Prop algorithm are theoretically analyzed, including cost function, perturbation amplitude, and global learning rate. The simulation results show that PER is the optimal cost function. When the perturbation amplitude is 0.06 and the global learning rate is 0.6, the system can achieve the optimal control speed and accuracy. By comparison with the stochastic parallel gradient descent (SPGD) algorithm, the RMS-Prop algorithm has an advantage in obtaining higher PER. Full article
(This article belongs to the Special Issue Smart Fiber Lasers)
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<p>Schematic diagram of active polarization control system of fiber laser: PM, phase modulator; PC, polarization controller; CO: collimator; PBS: polarization beam splitter; PD: photo detector; RF-AMP, radio frequency amplifier.</p>
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<p>Convergence curves for different cost functions: (<b>a</b>) DOP curves; (<b>b</b>) PER curves.</p>
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<p>Convergence curves for different perturbation amplitudes: (<b>a</b>) DOP curves; (<b>b</b>) PER curves.</p>
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<p>Convergence curves for different global learning rates: (<b>a</b>) DOP curves; (<b>b</b>) PER curves.</p>
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<p>Convergence curves of DOP and PER of SPGD algorithm with different cost functions (<b>a</b>,<b>b</b>), perturbation amplitudes (<b>c</b>,<b>d</b>) and global learning rates (<b>e</b>,<b>f</b>).</p>
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<p>Comparison of RMS-Prop and SPGD algorithms.</p>
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11 pages, 5235 KiB  
Article
High-Sensitivity Refractive Index Sensing Based on an SNPNS Composite Structure
by Di Wu, Jingwen Zhou, Xiang Yu and Yue Sun
Photonics 2024, 11(10), 941; https://doi.org/10.3390/photonics11100941 - 7 Oct 2024
Cited by 1 | Viewed by 760
Abstract
In this paper, we design and demonstrate an all-fiber-sensitive refractive index (RI) sensor based on the Mach–Zehnder interferometer (MZI). It is constructed by splicing two no-core fibers (NCFs) and a photonic crystal fiber (PCF) between two single-mode fibers (SMFs) to obtain an SMF–NCF–PCF–NCF–SMF [...] Read more.
In this paper, we design and demonstrate an all-fiber-sensitive refractive index (RI) sensor based on the Mach–Zehnder interferometer (MZI). It is constructed by splicing two no-core fibers (NCFs) and a photonic crystal fiber (PCF) between two single-mode fibers (SMFs) to obtain an SMF–NCF–PCF–NCF–SMF composite structure (SNPNS). A study of the effect of varying PCF lengths on the RI reveals that the shorter the length, the higher the sensitivity. The maximum RI sensitivity of 176.9 nm/RIU is attained within the RI range of 1.3365–1.3767 when the PCF length in the SNPNS structure is 3 cm. Meanwhile, the sensor exhibits a high stability in water, with an RSD of only 0.0019% for the interference trough over a duration of two hours. This proposed sensing structure offers the advantages of a large extinction ratio, small size, low temperature sensitivity, and simple fabrication, exhibiting a great potential in RI measurements. Full article
(This article belongs to the Section Lasers, Light Sources and Sensors)
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<p>Schematic diagram of the MZI sensor based on the SNPNS composite structure.</p>
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<p>Cross-section of PCF under the electron microscope.</p>
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<p>Simulated field distributions of SNPNS composite structure with lengths of NCF<sub>1</sub>, PCF, and NCF<sub>2</sub> equal to 3 cm.</p>
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<p>Diagram of the experimental setup.</p>
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<p>Transmission spectra of SNPNS composite structure sensors for PCF lengths of 3 cm, 4 cm, and 5 cm.</p>
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<p>Spatial spectra of SNPNS composite structure sensors for PCF lengths of 3 cm, 4 cm, and 5 cm.</p>
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<p>The SNPNS composite structure sensor with PCF length of 3 cm and (<b>a</b>–<b>c</b>) transmission spectra responses for dips A, B, and C with different RI values; (<b>d</b>) relationships between interference dips and RI values.</p>
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<p>The SNPNS composite structure sensor with PCF length of 4 cm and (<b>a</b>) transmission spectra responses with different RI values and (<b>b</b>) relationships between interference dips and RI values.</p>
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<p>The SNPNS composite structure sensor with PCF length of 5 cm and (<b>a</b>) transmission spectra response with different RI values and (<b>b</b>) relationships between interference dips and RI values.</p>
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<p>(<b>a</b>) Transmission spectrum of the sensor with PCF length of 3 cm in water; (<b>b</b>) stability lines of different dips at the water temperature of 23 °C; (<b>c</b>) relationships between interference dips and water temperature.</p>
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17 pages, 12981 KiB  
Article
Vertical Distribution of Water Vapor During Haze Processes in Northeast China Based on Raman Lidar Measurements
by Tianpei Zhang, Zhenping Yin, Yubin Wei, Yaru Dai, Longlong Wang, Xiangyu Dong, Yuan Gao, Lude Wei, Qixiong Zhang, Di Hu and Yifan Zhou
Remote Sens. 2024, 16(19), 3713; https://doi.org/10.3390/rs16193713 - 6 Oct 2024
Cited by 1 | Viewed by 964
Abstract
Haze refers to an atmospheric phenomenon with extremely low visibility, which has significant impacts on human health and safety. Water vapor alters the scattering properties of atmospheric particulate matter, thus affecting visibility. A comprehensive analysis of the role of water vapor in haze [...] Read more.
Haze refers to an atmospheric phenomenon with extremely low visibility, which has significant impacts on human health and safety. Water vapor alters the scattering properties of atmospheric particulate matter, thus affecting visibility. A comprehensive analysis of the role of water vapor in haze formation is of great scientific significance for forecasting severe pollution weather events. This study investigates the distribution characteristics and variations of water vapor during haze weather in Changchun City (44°N, 125.5°E) in autumn and winter seasons, aiming to reveal the relationship between haze and atmospheric water vapor content. Analysis of observational results for a period of two months (October to November 2023) from a three-wavelength Raman lidar deployed at the site reveals that atmospheric water vapor content is mainly concentrated below 5 km, accounting for 64% to 99% of the total water vapor below 10 km. Furthermore, water vapor content in air pollution exhibits distinct stratification characteristics with altitude, especially within the height range of 1–3 km, where significant water vapor variation layers exist, showing spatial consistency with inversion layers. Statistical analysis of haze events at the site indicates a high correlation between the concentration variations of PM2.5 and PM10 and the variations in average water vapor mixing ratio (WVMR). During haze episodes, the average WVMR within 3 km altitude is 3–4 times higher than that during clear weather. Analysis of spatiotemporal height maps of aerosols and water vapor during a typical haze event suggests that the relative stability of the atmospheric boundary layer may hinder the vertical transport and diffusion of aerosols. This, in turn, could lead to a sharp increase in aerosol extinction coefficients through hygroscopic growth, thereby possibly exacerbating haze processes. These observational findings indicate that water vapor might play a significant role in haze formation, emphasizing the potential importance of observing the vertical distribution of water vapor for better simulation and prediction of haze events. Full article
(This article belongs to the Section Atmospheric Remote Sensing)
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<p>The topographic maps of (<b>a</b>) Jilin Province and (<b>b</b>) Changchun City.</p>
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<p>(<b>a</b>) Schematic diagram of water vapor calibration experiment; (<b>b</b>) from left to right are the range corrected signal (RCS), WVMR, and the absolute deviation between the lidar and the radiosonde (with ±0.3 g/kg line marked), measured at 20:00 CST on 18 October 2023.</p>
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<p>From left to right are the RCS, RH, and the deviation of RH between the lidar and the radiosonde (with a ±5% line marked), measured at 20:00 CST on 18 October 2023.</p>
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<p>Flowchart for aerosol optical parameter retrieval.</p>
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<p>The proportion of daily PWV at 0.25–5 km in October.</p>
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<p>Representative measurement instances of WVMR during the nighttime of October 2023. The red-shaded areas within the dashed boxes indicate the height ranges where abrupt changes in water vapor. The weather conditions from left to right are (<b>a</b>) cloudy, (<b>b</b>) sunny, (<b>c</b>) light haze, and (<b>d</b>) moderate haze.</p>
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<p>MODIS Terra true-color images during the haze event period. The red dot is the measuring station. The top left corner of the images indicates the average PM<sub>2.5</sub> (μg/m<sup>3</sup>) concentration for the day.</p>
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<p>Wind field maps (altitude of 100 m) during the haze event period. The green dot is the measuring station.</p>
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<p>WVMR profiles from 25 October to 5 November 2023, obtained by lidar, averaged between 19:00 and 21:00 CST on each day. The red shading indicates the days when haze weather occurred.</p>
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<p>The daily average WVMR and the concentrations of PM<sub>2.5</sub> and PM<sub>10</sub> for October 2023.</p>
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<p>The correlation between the daily average (0–3 km) WVMR and the concentrations of PM<sub>2.5</sub> (<b>a</b>) and PM<sub>10</sub> (<b>b</b>) in October 2023.</p>
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<p>(<b>a</b>) Aerosol backscattering coefficient, (<b>b</b>) WVMR, and (<b>c</b>) RH continuously detected by lidar from 18:00 CST on October 29 to 02:00 CST on 30 October 2023.</p>
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<p>Vertical profiles at 20:00 CST on 29 October 2023. From left to right, (<b>a</b>) extinction coefficients, (<b>b</b>) particle depolarization ratio, (<b>c</b>) RH, and (<b>d</b>) potential temperature, in which the shaded area denotes the uncertainty. Products at the lowest heights from the surface to 500 m are filtered out due to the incomplete overlap factor of the lidar system.</p>
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19 pages, 3356 KiB  
Article
The First Validation of Aerosol Optical Parameters Retrieved from the Terrestrial Ecosystem Carbon Inventory Satellite (TECIS) and Its Application
by Yijie Ren, Binglong Chen, Lingbing Bu, Gen Hu, Jingyi Fang and Pasindu Liyanage
Remote Sens. 2024, 16(19), 3689; https://doi.org/10.3390/rs16193689 - 3 Oct 2024
Viewed by 719
Abstract
In August 2022, China successfully launched the Terrestrial Ecosystem Carbon Inventory Satellite (TECIS). The primary payload of this satellite is an onboard multi-beam lidar system, which is capable of observing aerosol optical parameters on a global scale. This pioneering study used the Fernald [...] Read more.
In August 2022, China successfully launched the Terrestrial Ecosystem Carbon Inventory Satellite (TECIS). The primary payload of this satellite is an onboard multi-beam lidar system, which is capable of observing aerosol optical parameters on a global scale. This pioneering study used the Fernald forward integration method to retrieve aerosol optical parameters based on the Level 2 data of the TECIS, including the aerosol depolarization ratio, aerosol backscatter coefficient, aerosol extinction coefficient, and aerosol optical depth (AOD). The validation of the TECIS-retrieved aerosol optical parameters was conducted using CALIPSO Level 1 and Level 2 data, with relative errors within 30%. A comparison of the AOD retrieved from the TECIS with the AERONET and MODIS AOD products yielded correlation coefficients greater than 0.7 and 0.6, respectively. The relative error of aerosol optical parameter profiles compared with ground-based measurements for CALIPSO was within 40%. Additionally, the correlation coefficients R2 with MODIS and AERONET AOD were approximately between 0.5 and 0.7, indicating the high accuracy of TECIS retrievals. Utilizing the TECIS retrieval results, combined with ground air quality monitoring data and HYSPLIT outcomes, a typical dust transport event was analyzed from 2 to 7 April 2023. The results indicate that dust was transported from the Taklamakan Desert in Xinjiang, China, to Henan and Anhui provinces, with a gradual decrease in the aerosol depolarization ratio and backscatter coefficient during the transport process, causing varying degrees of pollution in the downstream regions. This research verifies the accuracy of the retrieval algorithm through multi-source data comparison and demonstrates the potential application of the TECIS in the field of aerosol science for the first time. It enables the fine-scale regional monitoring of atmospheric aerosols and provides reliable data support for the three-dimensional distribution of global aerosols and related scientific applications. Full article
(This article belongs to the Section Atmospheric Remote Sensing)
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<p>A flowchart of the TECIS retrieval algorithm.</p>
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<p>Trajectory of CALIPSO and TECIS.</p>
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<p>Total attenuated backscatter coefficient obtained from TECIS and CALIPSO. (<b>a</b>) TECIS, (<b>b</b>) CALIPSO.</p>
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<p>SNR of total attenuated backscatter coefficient obtained from TECIS and CALIPSO. (<b>a</b>) TECIS, (<b>b</b>) CALIPSO.</p>
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<p>A comparison of total attenuation backscatter coefficient mean profiles between the TECIS and CALIPSO at 13° to 14°N; the shaded area represents the standard deviation of the two satellites. The blue solid line represents the TECIS result, and the red solid line represents the CALIPSO result.</p>
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<p>(<b>a</b>) Profile of aerosol depolarization ratio of TECIS, (<b>b</b>) profile of aerosol depolarization ratio of CALIPSO, (<b>c</b>) profile of aerosol backscatter coefficient of TECIS, (<b>d</b>) profile of aerosol backscatter coefficient of CALIPSO, (<b>e</b>) profile of aerosol extinction coefficient of TECIS, (<b>f</b>) profile of aerosol extinction coefficient of CALIPSO.</p>
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<p>A comparison of aerosol optical parameter mean profiles between the TECIS and CALIPSO at 13° to 14°N, where the blue solid line represents the TECIS result, the red solid line represents the CALIPSO result, and the shaded area represents the standard deviation within the average range of the two satellites. (<b>a</b>) Aerosol depolarization ratio, (<b>b</b>) aerosol backscatter coefficient, (<b>c</b>) aerosol extinction coefficient.</p>
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<p>Relative error of retrieval results between TECIS and CALIPSO.</p>
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<p>TECIS 532 nm AOD retrievals against AERONET AOD during April to June 2023; the dashed line is the linear fit described by the regression equation; the black line is the 1:1 line.</p>
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<p>A scatterplot comparison of TECIS AOD data against MODIS AOD data during April to June 2023; the color scale represents the fraction of the total data. (<b>a</b>) North Africa, (<b>b</b>) the Middle East, (<b>c</b>) North America, (<b>d</b>) Central Asia.</p>
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<p>TECIS 1064 nm total attenuation backscattering coefficient and HYSPLIT backward tracking from 2 to 7 April 2023 (blue, red, and black represent backward tracking at heights of 3 km, 2 km, and 1 km, respectively).</p>
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<p>Variations in PM10 and PM2.5 concentrations from 2 to 7 April 2023. (<b>a</b>) PM10, (<b>b</b>) PM2.5.</p>
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<p>Optical parameters obtained by TECIS inversion from 2 to 7 April 2023. (<b>a</b>,<b>c</b>,<b>e</b>,<b>g</b>,<b>i</b>,<b>k</b>) show backscattering coefficient; (<b>b</b>,<b>d</b>,<b>f</b>,<b>h</b>,<b>j</b>,<b>l</b>) show depolarization ratio.</p>
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<p>Optical parameters obtained by TECIS inversion from 2 to 7 April 2023. (<b>a</b>,<b>c</b>,<b>e</b>,<b>g</b>,<b>i</b>,<b>k</b>) show backscattering coefficient; (<b>b</b>,<b>d</b>,<b>f</b>,<b>h</b>,<b>j</b>,<b>l</b>) show depolarization ratio.</p>
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13 pages, 5165 KiB  
Article
All-Optical Switching Using Cavity Modes in Photonic Crystals Embedded with Hyperbolic Metamaterials
by Chang Liu, Dong Wei, Xiaochun Lin and Yaoxian Zheng
Crystals 2024, 14(9), 787; https://doi.org/10.3390/cryst14090787 - 4 Sep 2024
Viewed by 696
Abstract
Hyperbolic metamaterials (HMMs) are highly anisotropic materials with the unique property of generating electromagnetic modes. Understanding how these materials can be applied to control the propagation of light waves remains a major focus in photonics. In this study, we inserted a finite-size HMM [...] Read more.
Hyperbolic metamaterials (HMMs) are highly anisotropic materials with the unique property of generating electromagnetic modes. Understanding how these materials can be applied to control the propagation of light waves remains a major focus in photonics. In this study, we inserted a finite-size HMM rod into the point defect of two-dimensional photonic crystals (PhCs) and investigated the unique cavity modes of this hybrid system. The HMM enhances the efficiency of the cavity system in controlling light transmission. Numerical results demonstrate that the cavity modes based on HMMs can be categorized into various types, showing high Q-factors and promising potential for resonant modulation. Furthermore, the switching performance of the cavity with an HMM rod was examined, revealing that the finite-size HMM modes are highly frequency-sensitive and suitable for nonlinear controlled all-optical switching. These switches, characterized by low power consumption and high extinction ratios, are highly suitable for integration into photonic systems. Our investigation on the new type of HMM cavity illustrates that anisotropic materials can be effectively applied in cavity systems to generate highly efficient modes for filtering and switching. Full article
(This article belongs to the Special Issue Nonlinear Optical Properties and Applications of 2D Materials)
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<p>(<b>a</b>) A schematic of the proposed PhC HMM cavity, composed of rectangular air holes within a dielectric background. (<b>b</b>) A schematic of the HMM rod inside the cavity, with dielectric and metal layers oriented in the <span class="html-italic">y–z</span> plane. (<b>c</b>) A schematic of the HMM rod inside the cavity, with dielectric and metal layers oriented in the <span class="html-italic">x–y</span> plane.</p>
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<p>Transverse (blue) and longitudinal (orange) components of the effective permittivity of HMMs with different filling factors: (<b>a</b>) <span class="html-italic">f</span> = 0.1, (<b>b</b>) <span class="html-italic">f</span> = 0.2, (<b>c</b>) <span class="html-italic">f</span> = 0.3, (<b>d</b>) <span class="html-italic">f</span> = 0.4, (<b>e</b>) <span class="html-italic">f</span> = 0.5, (<b>f</b>) <span class="html-italic">f</span> = 0.6, (<b>g</b>) <span class="html-italic">f</span> = 0.7, (<b>h</b>) <span class="html-italic">f</span> = 0.8, and (<b>i</b>) <span class="html-italic">f</span> = 0.9. Only the real parts of the effective permittivities of the HMMs are shown in the figure.</p>
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<p>Profiles of the magnetic fields (<b>H</b><sub>z</sub>) when light propagates in the PhC HMM cavity system. (<b>a</b>) Incident light frequency: 455 THz, HMM filling factor: 0.1. (<b>b</b>) Incident light frequency: 452 THz, HMM filling factor: 0.2. (<b>c</b>) Incident light frequency: 488 THz, HMM filling factor: 0.3. (<b>d</b>) Incident light frequency: 466 THz, HMM filling factor: 0.3. (<b>e</b>) Incident light frequency: 438 THz, HMM filling factor: 0.3. (<b>f</b>) Incident light frequency: 496 THz, HMM filling factor: 0.5. (<b>g</b>) Incident light frequency: 522 THz, HMM filling factor: 0.7. (<b>h</b>) Incident light frequency: 469 THz, HMM filling factor: 0.8. (<b>i</b>) Incident light frequency: 539 THz, HMM filling factor: 0.9.</p>
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<p>Transmission spectra of the resonant cavity as a function of frequency for different filling factors of the HMM rod inside the cavity: (<b>a</b>) <span class="html-italic">f</span> = 0.1, (<b>b</b>) <span class="html-italic">f</span> = 0.2, (<b>c</b>) <span class="html-italic">f</span> = 0.3, (<b>d</b>) <span class="html-italic">f</span> = 0.4, (<b>e</b>) <span class="html-italic">f</span> = 0.5, (<b>f</b>) <span class="html-italic">f</span> = 0.6, (<b>g</b>) <span class="html-italic">f</span> = 0.7, (<b>h</b>) <span class="html-italic">f</span> = 0.8, and (<b>i</b>) <span class="html-italic">f</span> = 0.9.</p>
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<p>Transverse (blue) and longitudinal (orange) components of the effective permittivity of the HMM rod inside the cavity as functions of the filling factor <span class="html-italic">f</span> when operating at frequencies (<b>a</b>) 400 THz, (<b>b</b>) 450 THz, and (<b>c</b>) 500 THz, respectively. The figure displays only the real parts of the effective permittivities of the HMMs.</p>
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<p>(<b>a</b>–<b>c</b>) Transverse (blue) and longitudinal (orange) components of the effective permittivity of HMMs as a function of frequency, corresponding to a different pumping of the Ag nonlinear layers: 0 V/m, 5 × 10<sup>7</sup> V/m, and 1 × 10<sup>8</sup> V/m, respectively. The filling factor of the HMM is 0.4. Only the real parts of the effective permittivities of the HMMs are shown in the figure. (<b>d</b>–<b>f</b>) Transmission spectra of the resonant cavity corresponding to the same pumping powers of the Ag nonlinear layers: 0 V/m, 5 × 10<sup>7</sup> V/m, and 1 × 10<sup>8</sup> V/m, respectively.</p>
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<p>(<b>a</b>) Transverse (blue) and longitudinal (orange) components of the effective permittivity of HMMs as they change with the pumping power applied to the Ag nonlinear layers. The operating frequency is 440 THz. (<b>b</b>) The transmission of the resonant cavity as a function of the pumping power. (<b>c</b>–<b>e</b>) Profiles of the magnetic fields (<b>H</b><sub>z</sub>) of light propagating in the PhC cavity when the pumping powers are 0 V/m, 5.5 × 10⁷ V/m, and 8.0 × 10⁷ V/m, respectively.</p>
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18 pages, 6707 KiB  
Article
Geometric Factor Correction Algorithm Based on Temperature and Humidity Profile Lidar
by Bowen Zhang, Guangqiang Fan and Tianshu Zhang
Remote Sens. 2024, 16(16), 2977; https://doi.org/10.3390/rs16162977 - 14 Aug 2024
Viewed by 933
Abstract
Due to the influence of geometric factors, the temperature and humidity profile of lidar’s near-field signal was warped when sensing the air environment. In order to perform geometric factor correction on near-field signals, this article proposes different correction solutions for the Mie and [...] Read more.
Due to the influence of geometric factors, the temperature and humidity profile of lidar’s near-field signal was warped when sensing the air environment. In order to perform geometric factor correction on near-field signals, this article proposes different correction solutions for the Mie and Raman scattering channels. Here, the Mie scattering channel used the Raman method to invert the aerosol backscatter coefficient and correct the extinction coefficient in the transition zone. The geometric factor was the ratio of the measured signal to the forward-computed vibration Raman scattering signal. The aerosol optical characteristics were reversed using the corrected echo signal, and the US standard atmospheric model was added to the missing signal in the blind zone, reflecting the aerosol evolution process. The stability and dependability of the proposed algorithm were validated by the consistency between the visibility provided by the Environmental Protection Agency and the visibility acquired via lidar retrieval data. The near-field humidity data were supplemented by the interpolation method in the Raman scattering channel to reflect the water vapor transfer process in the temporal dimension. The measured transmittance curve of the filter, the theoretical normalized spectrum, and the sounding data were used to compute the delay geometric factor. The temperature was retrieved and the near-field signal distortion issue was resolved by applying the corrected quotient of the temperature channel. The proposed algorithm exhibited robustness and universality, enhancing the system’s detection accuracy compared to the temperature and humidity data constantly recorded by the probes in the meteorological gradient tower, which have a high correlation with the lidar observation data. The comparison between lidar data and instrument monitoring data showed that the proposed algorithm could effectively correct distorted echo signals in the transition zone, which was of great value for promoting the application of lidar in the meteorological monitoring of the urban canopy layer. Full article
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Graphical abstract

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<p>Flow chart for geometric factor correction of Mie scattering channel.</p>
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<p>Structural design of humidity chamber.</p>
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<p>Structural design of temperature chamber.</p>
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<p>Flow chart for geometric factor correction of Raman scattering channel.</p>
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<p>Single profile measurement results (00:12 on 2 February 2024, in Harbin): (<b>a</b>) Range-squared-corrected signal; (<b>b</b>) Ångström exponent; (<b>c</b>) aerosol optical parameters; (<b>d</b>) lidar ratio.</p>
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<p>Geometric factor calculation and signal correction. (<b>a</b>) Range-squared-corrected signal; (<b>b</b>) geometric factor (<b>c</b>) echo signal correction; (<b>d</b>) aerosol optical parameters correction.</p>
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<p>Humidity channel calibration (02:07 on 27 December 2023, in Guangzhou). (<b>a</b>) Measured quotient value; (<b>b</b>) Relative humidity correction.</p>
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<p>Normalized spectra and transmittance curves of pure rotational Raman scattering channels.</p>
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<p>Temperature channel calibration (21:16 on 28 December 2023, in Guangzhou). (<b>a</b>) CO<sub>R</sub>(z); (<b>b</b>) delay geometric factor O<sub>R</sub>(z); (<b>c</b>) temperature quotient correction; (<b>d</b>) temperature correction.</p>
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<p>Pseudo-color map of the spatiotemporal distribution of the aerosol extinction coefficient (from 00:00 on 1 February 2024 to 03:30 on 2 February 2024, in Harbin). (<b>a</b>) Extinction coefficient before correction; (<b>b</b>) corrected and supplemented extinction coefficient.</p>
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<p>Comparison of visibility results. (<b>a</b>) Lidar data and meteorological data; (<b>b</b>) statistical error distribution between the lidar and meteorology (where the vertical axis represents the occurrence number); (<b>c</b>) correlation analysis.</p>
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<p>Relative humidity correction (from 00:00 on 26 December 2023 to 00:00 on 29 December 2023, in Guangzhou). (<b>a</b>,<b>b</b>) Relative humidity before and after calibration; (<b>c</b>–<b>e</b>) comparison results of meteorology.</p>
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<p>Comparison of the relative humidity between Lidar data and meteorological data. (<b>a</b>–<b>c</b>) Statistical error distribution at different heights (at 118 m, 168 m, 488 m); (<b>d</b>–<b>f</b>) correlation analysis.</p>
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<p>Temperature correction (from 00:00 on 26 December 2023, to 00:00 on 29 December 2023, in Guangzhou). (<b>a</b>,<b>b</b>) Temperature before and after calibration; (<b>c</b>–<b>e</b>) Comparison results of meteorology.</p>
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<p>Comparison of the temperature between Lidar data and meteorological data. (<b>a</b>–<b>c</b>) Statistical error distribution at different heights (at 118 m, 168 m, 488 m); (<b>d</b>–<b>f</b>) Correlation analysis.</p>
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