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16 pages, 3108 KiB  
Article
An Analysis of Combined Molecular Weight and Hydrophobicity Similarity between the Amino Acid Sequences of Spike Protein Receptor Binding Domains of Betacoronaviruses and Functionally Similar Sequences from Other Virus Families
by Jamie D. Dixson, Lavanya Vumma and Rajeev K. Azad
Microorganisms 2024, 12(10), 2021; https://doi.org/10.3390/microorganisms12102021 - 5 Oct 2024
Viewed by 459
Abstract
Recently, we proposed a new method, based on protein profiles derived from physicochemical dynamic time warping (PCDTW), to functionally/structurally classify coronavirus spike protein receptor binding domains (RBD). Our method, as used herein, uses waveforms derived from two physicochemical properties of amino acids (molecular [...] Read more.
Recently, we proposed a new method, based on protein profiles derived from physicochemical dynamic time warping (PCDTW), to functionally/structurally classify coronavirus spike protein receptor binding domains (RBD). Our method, as used herein, uses waveforms derived from two physicochemical properties of amino acids (molecular weight and hydrophobicity (MWHP)) and is designed to reach into the twilight zone of homology, and therefore, has the potential to reveal structural/functional relationships and potentially homologous relationships over greater evolutionary time spans than standard primary sequence alignment-based techniques. One potential application of our method is inferring deep evolutionary relationships such as those between the RBD of the spike protein of betacoronaviruses and functionally similar proteins found in other families of viruses, a task that is extremely difficult, if not impossible, using standard multiple alignment-based techniques. Here, we applied PCDTW to compare members of four divergent families of viruses to betacoronaviruses in terms of MWHP physicochemical similarity of their RBDs. We hypothesized that some members of the families Arteriviridae, Astroviridae, Reoviridae (both from the genera rotavirus and orthoreovirus considered separately), and Toroviridae would show greater physicochemical similarity to betacoronaviruses in protein regions similar to the RBD of the betacoronavirus spike protein than they do to other members of their respective taxonomic groups. This was confirmed to varying degrees in each of our analyses. Three arteriviruses (the glycoprotein-2 sequences) clustered more closely with ACE2-binding betacoronaviruses than to other arteriviruses, and a clade of 33 toroviruses was found embedded within a clade of non-ACE2-binding betacoronaviruses, indicating potentially shared structure/function of RBDs between betacoronaviruses and members of other virus clades. Full article
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<p>Dendrogram of betacoronavirus spike protein RBD sequences and arterivirus GP2 sequences constructed using MWHP PCDTW with Euclidean distance and UPGMA hierarchical clustering. ACE2-binding betacoronavirus sequences are highlighted in red, and non-ACE2-binding betacoronavirus sequences are highlighted in blue. In most cases, the host organism is encoded into the taxa label. In some cases, the host was labeled as “UnkArtV.” In those cases, the Uniprot record should be consulted for additional information concerning the host organism. The three arterivirus sequences that cluster near the ACE2-binding betacoronaviruses have blue text labels and are from Oliver’s Shrew. All black text labels not in a colored box represent Arterivirus GP2 sequences that did not cluster closely with the betacoronavirus sequences.</p>
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<p>Dendrogram of betacoronavirus spike protein RBD sequences, arterivirus GP2 sequences and torovirus sequences constructed using MWHP PCDTW with Euclidean distance and UPGMA hierarchical clustering. ACE2-binding betacoronavirus sequences are highlighted in red, and non-ACE2-binding betacoronavirus sequences are highlighted in blue. Three Arterivirus GP2 sequences that are unique within this study, in that they cluster very closely with ACE2-binding betacoronavirus sequence, are labeled with blue text. This combined dendrogram underscores the similarity of the three arterivirus GP2 sequences to those of the ACE2-binding betacoronavirus sequences.</p>
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<p>(<b>A</b>) Pairwise global alignment identity matrix showing identities for all pairwise comparisons of 51 betacoronavirus spike protein RBD sequences and three arterivirus GP2 sequences. (<b>B</b>) Pairwise distance matrix showing MWHP PCDTW distances which have been scaled to 100 for all pairwise comparisons of 51 betacoronavirus spike protein RBD sequences and three arterivirus GP2 (ArtVGP2) sequences. The Pearson Correlation Coefficient for the values in A and B is 0.44 with a <span class="html-italic">p</span>-Value of 4.98 × 10<sup>−140</sup>.</p>
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<p>Scatterplot of pairwise global alignment identity percentages and MWHP PCDTW distances scaled to 100 for all comparisons made between arterivirus GP2 sequences and betacoronavirus sequences underlying the dendrogram shown in <a href="#microorganisms-12-02021-f001" class="html-fig">Figure 1</a>. The line shown is a polynomial regression line. This shows that, in general terms, the two signals are not different ways of measuring the same signal. In other words, there is additional information in the MWHP PCDTW signal that is not in the identities.</p>
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<p>Superimposition of the SARS-CoV-2 RBD (6MOJ) and a synthetic construct homology model which has 0% identity to 6MOJ. The synthetic model exhibits an extremely low pruned RMSD value of 0.21 (~96% of residues considered) and also a very low TM-Score indicating that the two structures are nearly identical [<a href="#B15-microorganisms-12-02021" class="html-bibr">15</a>,<a href="#B18-microorganisms-12-02021" class="html-bibr">18</a>].</p>
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21 pages, 626 KiB  
Article
Algorithm for Designing Waveforms Similar to Linear Frequency Modulation Using Polyphase-Coded Frequency Modulation
by Pengpeng Wang, Zhan Wang, Peng You and Mengyun An
Remote Sens. 2024, 16(19), 3664; https://doi.org/10.3390/rs16193664 - 1 Oct 2024
Viewed by 451
Abstract
Linear frequency modulation (LFM) waveforms have been widely adopted due to their excellent performance characteristics, such as good Doppler tolerance and ease of physical implementation. However, LFM waveforms suffer from high autocorrelation sidelobes (ACSLs) and limited design flexibility. Phase-coded frequency modulation (PCFM) waveforms [...] Read more.
Linear frequency modulation (LFM) waveforms have been widely adopted due to their excellent performance characteristics, such as good Doppler tolerance and ease of physical implementation. However, LFM waveforms suffer from high autocorrelation sidelobes (ACSLs) and limited design flexibility. Phase-coded frequency modulation (PCFM) waveforms can be used to design waveforms similar to LFM, offering greater design flexibility to optimize ACSLs. However, it has been found that the initial PCFM waveform experiences spectral expansion during the ACSL optimization process, which reduces its similarity to LFM. Therefore, this article jointly optimizes the ACSLs and spectrum of the initial PCFM waveform, establishes an optimized mathematical model, and then solves it using the heavy-ball gradient descent algorithm. Numerical experiments indicate that the proposed method effectively addresses the problem of waveform similarity degradation caused by spectral expansion while reducing waveform ACSLs. At the same time, a balance between reducing waveform ACSLs and preserving waveform similarity can be achieved by adjusting the parameters. Full article
(This article belongs to the Special Issue Array and Signal Processing for Radar)
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<p>PCFM radar waveform implementation.</p>
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<p>Convergence curves. (<b>a</b>) Convergence curve of ISL. (<b>b</b>) Convergence curve of PSL. (<b>c</b>) Convergence curve of Isim.</p>
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<p>Autocorrelation function of LFM, initial PCFM and optimized PCFM under different <span class="html-italic">L</span>. (<b>a</b>) Global graph. (<b>b</b>) Local graph.</p>
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<p>Bandwidth of initial PCFM under different values of <span class="html-italic">L</span>.</p>
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<p>Bandwidth of initial and optimized PCFMs under <math display="inline"><semantics> <mrow> <mi>L</mi> <mo>=</mo> <mn>1</mn> </mrow> </semantics></math>.</p>
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<p>The performance of different values of <math display="inline"><semantics> <mi>σ</mi> </semantics></math>. (<b>a</b>) Similarity of optimized PCFM. (<b>b</b>) ISL and PSL of optimized PCFM.</p>
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<p>Bandwidth of optimized PCFM under different values of <math display="inline"><semantics> <mi>σ</mi> </semantics></math>.</p>
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<p>Autocorrelation functions optimized by different algorithms.</p>
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<p>Autocorrelation functions optimized by different gradient descent algorithms.</p>
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13 pages, 2068 KiB  
Article
Kinematic, Neuromuscular and Bicep Femoris In Vivo Mechanics during the Nordic Hamstring Exercise and Variations of the Nordic Hamstring Exercise
by Nicholas Ripley, Jack Fahey, Paul Comfort and John McMahon
Muscles 2024, 3(3), 310-322; https://doi.org/10.3390/muscles3030027 - 18 Sep 2024
Viewed by 412
Abstract
The Nordic hamstring exercise (NHE) is effective at decreasing hamstring strain injury risk. Limited information is available on the in vivo mechanics of the bicep femoris long head (BFLH) during the NHE. Therefore, the purpose of this study was to observe [...] Read more.
The Nordic hamstring exercise (NHE) is effective at decreasing hamstring strain injury risk. Limited information is available on the in vivo mechanics of the bicep femoris long head (BFLH) during the NHE. Therefore, the purpose of this study was to observe kinematic, neuromuscular and in-vivo mechanics of the BFLH during the NHE. Thirteen participants (24.7 ± 3.7 years, 79.56 ± 7.89 kg, 177.40 ± 12.54 cm) performed three repetitions of the NHE at three horizontal planes (0°, 20° and −20°). Dynamic ultrasound of the dominant limb BFLH, surface electromyography (sEMG) of the contralateral hamstrings and sagittal plane motion data were simultaneously collected. Repeated measures analysis of variance with Bonferroni post hoc corrections were used on the in vivo mechanics and the kinematic and sEMG changes in performance of the NHE. Likely differences in ultrasound waveforms for the BFLH were determined. Significant and meaningful differences in kinematics and in vivo mechanics between NHE variations were observed. Non-significant differences were observed in sEMG measures between variations. Changes to the NHE performance angle manipulates the lever arm, increasing or decreasing the amount of force required by the hamstrings at any given muscle length, potentially changing the adaptive response when training at different planes and providing logical progressions ore regressions of the NHE. All NHE variations result in a similar magnitude of fascicle lengthening, which may indicate similar positive adaptations from the utilization of any variation. Full article
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<p>Nordic hamstring exercise variations: flat (0°), decline (−20°) and incline (20°).</p>
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<p>Custom-designed cast, housing a 10 cm ultrasound probe.</p>
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<p>Individual, mean, interquartile range, minimum, maximum and outliers within box-and-whisker plots for the kinematic measures of knee angle. (<b>A</b>) Knee angle at break point, (<b>B</b>) change in knee angle, (<b>C</b>) knee angle at break point relative to the horizontal.</p>
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<p>Individual absolute fascicle length waveforms with upper- and lower-bound 95% confidence intervals (shaded) between performance angles (INC = incline; DEC = decline).</p>
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<p>Individual relative fascicle length waveforms with upper- and lower-bound 95% confidence intervals (shaded) between performance angles.</p>
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<p>Time–knee extension angle and time–knee extension angular velocity graphs, identifying the moment of break point &gt;20°/s threshold.</p>
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12 pages, 4460 KiB  
Article
Identification and Application of Wave Field Characteristics of Channel Waves in Extra-Thick Coal Seams
by Tao Ding, Yanhui Wu, Yiran Hu, Zhen Nie, Xianhua Hou and Mianping Zheng
Appl. Sci. 2024, 14(18), 8286; https://doi.org/10.3390/app14188286 - 14 Sep 2024
Viewed by 358
Abstract
Channel wave seismic activity often occurs with thin and medium-thick coal seams being the main target layer. To address the problem of channel wave applicability detection in extremely thick coal seams, the propagation and identification characteristics of channel waves remain the focus of [...] Read more.
Channel wave seismic activity often occurs with thin and medium-thick coal seams being the main target layer. To address the problem of channel wave applicability detection in extremely thick coal seams, the propagation and identification characteristics of channel waves remain the focus of research. Therefore, this paper takes the in-seam wave exploration of a 27 m extremely thick coal seam as an example and uses the staggered mesh finite difference method to construct a three-dimensional medium model for numerical simulation. An analysis of the physical parameters of coal and rock, along with the dispersion characteristics of channel waves in extra-thick coal seams, is utilized, through the Zoeppritz equation and the total reflection propagation method, to calculate the imaging. We found the following: (1) The dispersion areas and weak dispersion areas along the detection direction are extremely thick coal seams. (2) There are apparent channel waves in extra-thick coal seams, with a waveform similar to body waves; the length of the wave train is shorter than that of the conventional channel wave, and the arrival time can be estimated accurately. The amplitude of the apparent channel wave is affected by the degree of dispersion, with lower attenuation and higher resolution. The characteristic of total reflection in extremely thick coal seams is that the incident angle is equal to the critical angle, and the dispersion characteristics are weak. (3) The channel waves with weak dispersion characteristics in extra-thick coal seams are mainly Love-type waves. Full article
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<p>Diagram of the three-dimensional staggered grid.</p>
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<p>Three-dimensional model of the extra-thick coal seam: (<b>a</b>) model of a stable extra-thick coal seam; (<b>b</b>) model of an extra-thick coal seam with a collapse column.</p>
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<p>Wavefield snapshots of the x component propagating through the extra-thick coal seam: (<b>a</b>) 20 ms; (<b>b</b>) 40 ms; (<b>c</b>) 60 ms; (<b>d</b>) 80 ms.</p>
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<p>Wavefield snapshots of the y and z components at 80 ms: (<b>a</b>) y component; (<b>b</b>) z component.</p>
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<p>Wavefield snapshot of the x component at 80 ms in the presence of a collapse column.</p>
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<p>Relationships between the P- and S-wave reflection coefficients and the incident angle.</p>
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<p>Total reflection path of a ray in the extra-thick coal seam.</p>
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<p>Channel wave transmission survey layout.</p>
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<p>Shot 1 raw record.</p>
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<p>Dispersion analysis of the x and y components of the 33rd channel of shot 1. (<b>a</b>) x-component. (<b>b</b>) y-component.</p>
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<p>Image of the apparent channel wave velocity.</p>
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29 pages, 32138 KiB  
Article
Seismic Identification and Characterization of Deep Strike-Slip Faults in the Tarim Craton Basin
by Fei Tian, Wenhao Zheng, Aosai Zhao, Jingyue Liu, Yunchen Liu, Hui Zhou and Wenjing Cao
Appl. Sci. 2024, 14(18), 8235; https://doi.org/10.3390/app14188235 - 12 Sep 2024
Viewed by 486
Abstract
Through hydrocarbon explorations, deep carbonate reservoirs within a craton were determined to be influenced by deep strike-slip faults, which exhibit small displacements and are challenging to identify. Previous research has established a correlation between seismic attributes and deep geological information, wherein large-scale faults [...] Read more.
Through hydrocarbon explorations, deep carbonate reservoirs within a craton were determined to be influenced by deep strike-slip faults, which exhibit small displacements and are challenging to identify. Previous research has established a correlation between seismic attributes and deep geological information, wherein large-scale faults can cause abrupt waveform discontinuities. However, due to the inherent limitations of seismic datasets, such as low signal-to-noise ratios and resolutions, accurately characterizing complex strike-slip faults remains difficult, resulting in increased uncertainties in fault characterization and reservoir prediction. In this study, we integrate advanced techniques such as principal component analysis and structure-oriented filtering with a fault-centric imaging approach to refine the resolution of seismic data from the Tarim craton. Our detailed evaluation encompassed 12 distinct seismic attributes, culminating in the creation of a sophisticated model for identifying strike-slip faults. This model incorporates select seismic attributes and leverages fusion algorithms like K-means, ellipsoid growth, and wavelet transformations. Through the technical approach introduced in this study, we have achieved multi-scale characterization of complex strike-slip faults with throws of less than 10 m. This workflow has the potential to be extended to other complex reservoirs governed by strike-slip faults in cratonic basins, thus offering valuable insights for hydrocarbon exploration and reservoir characterization in similar geological settings. Full article
(This article belongs to the Special Issue Seismic Data Processing and Imaging)
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<p>(<b>a</b>) The location of the Tarim Basin and its subdivisions. The location of the research area is marked by a red rectangle. The location of the seismic section is marked by a pink line. (<b>b</b>) The seismic section in the north-central Tarim Basin. This seismic section shows that the deep structure in Tarim is very complicated and controlled by faults.</p>
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<p>Geological structure of a strike-slip fault33. (<b>a</b>) Structural zones of strike-slip faults, including the principal displacement zone (PDZ), restraining band, and horsetail splay. The zone or plane of dip-slip or strike-slip accounts for the greatest proportion of accumulated strain. Subsidiary structures such as synthetic and antithetic faults and folds (e.g., fault splays, back thrusts, fracture zones, and en echelon folds) will be kinematically linked to the PDZ. (<b>b</b>) Outcrop of strike-slip fault. (<b>c</b>) Strike-slip fault interpretation (red lines) based on the outcrop. The strike-slip displacement in the fault zone causes various structural deformations in the surrounding area.</p>
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<p>Quality improvement of the seismic data. (<b>a</b>) The original seismic profile. The burial depth map of the Tarim Ordovician strata is in the upper left corner, and the red line shows the location of the seismic section. The green arrow indicates the north direction. (<b>b</b>) The seismic profile after PCA+ structure-oriented filtering. This methodology involves calculating and analyzing the covariance matrix of seismic traces within a defined time window, facilitating a robust denoising process and improving the overall quality of seismic data for further analysis and interpretation. (<b>c</b>) The seismic profile of PCA+ structure-oriented filtering + fault-focused imaging. By maintaining the essential characteristics of the original seismic signal while improving its signal-to-noise ratio, this method effectively emphasizes the discontinuity along the in-phase axis.</p>
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<p>Attributes of seismic energy. Most areas are significantly disturbed by “non-fault” areas, and a small number of branch faults can be shown but are not obvious. (<b>a</b>) Map of the RMS amplitude attribute. It has a good correlation with the rock density and is often used in lithologic phase transition analysis. (<b>b</b>) Plane graph of the low-frequency energy attribute. (<b>c</b>) Map of the high-frequency attenuation attribute. Due to the seismic response characteristic of high-frequency absorption shown by the faults, characteristics similar to “low-frequency enhancements” appear, and the waveform characteristics show little variation with depth.</p>
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<p>Attributes of seismic curvature. The data points of the strike-slip faults are relatively clear, but there is little difference between them and the data points in the non-fault areas; that is, the boundary between the faults and non-faults is not clear. (<b>a</b>) Map of the maximum positive curvature attribute. The largest positive curvature in the normal curvature is called the maximum positive curvature. This curvature can amplify fault information and some small linear structures in the plane. (<b>b</b>) Map of the minimum negative curvature attribute. (<b>c</b>) Map of the dip attribute. The dip attribute reflects the change in the dip angle, and it is effective in depicting the dominant section with a large fault distance.</p>
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<p>Attributes of seismic correlation. Several major branch faults can be seen, but the whole branch is a network that is significantly affected by false faults, and it is difficult to distinguish true and false faults. (<b>a</b>) Map of coherent attribute. The coherence attribute is used to calculate the similarity between adjacent seismic tracks and analyze the transverse changes in strata and lithology in the same phase axis to achieve fault identification. (<b>b</b>) Map of the likelihood attribute. The likelihood attribute enhances the difference between fault and non-fault responses. The likelihood attributes of inclination and dip of each data sample point are scanned, and the maximum value is obtained when accurate inclination and dip are scanned. (<b>c</b>) Map of the ant tracking attribute. (<b>d</b>) Map of the AFE attribute. AFE is directional weighted coherence, which is obtained by further directional filtering based on sharpening.</p>
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<p>Attributes of seismic gradient. Many details in the trunk fault can be detected with minimal interference from non-breaks. (<b>a</b>) Map of the amplitude variance attribute. It describes the geological structure data mainly through the similarity attribute of adjacent seismic signals. (<b>b</b>) Map of the amplitude gradient attribute. By searching the disorder of the seismic amplitude gradient vector in each azimuth and dip angle in three-dimensional space, the most disordered surface is found to be the fault location.</p>
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<p>Fault identification comparison of preferred attributes. (<b>a</b>) Map of the ant track. (<b>b</b>) Fault interpretation of the ant tracking attribute. When applied to heterogeneous deep carbonate reservoirs in cratonic basins, the tracking attribute exhibits limitations, such as reduced recognition ability for carbonate faults and challenges in identifying micro-faults. (<b>c</b>) Map of the amplitude gradient attribute. (<b>d</b>) Fault interpretation (red lines) of the amplitude gradient attribute. The amplitude gradient attribute successfully reflects the trends and locations of these faults, whereas the ant tracking attribute often exhibits excessive disorder and interferes with the accurate determination of branch fault locations.</p>
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<p>Fault identification comparison of preferred attributes. (<b>a</b>) Map of the ant track. (<b>b</b>) Fault interpretation of the ant tracking attribute. When applied to heterogeneous deep carbonate reservoirs in cratonic basins, the tracking attribute exhibits limitations, such as reduced recognition ability for carbonate faults and challenges in identifying micro-faults. (<b>c</b>) Map of the amplitude gradient attribute. (<b>d</b>) Fault interpretation (red lines) of the amplitude gradient attribute. The amplitude gradient attribute successfully reflects the trends and locations of these faults, whereas the ant tracking attribute often exhibits excessive disorder and interferes with the accurate determination of branch fault locations.</p>
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<p>Extraction of the amplitude gradient attribute fault confidence region. (<b>a</b>) The spatial range of the fault was divided based on the fault threshold. Because K-means can cluster similar data based on the distance between the data points, the data were classified into 2 clusters through K-means clustering: fault clusters and non-fault clusters. (<b>b</b>) The fault range of high probability was obtained by ellipsoid expansion. By setting the structural unit, the range of the extracted attribute points can be expanded according to geological theory to obtain the data body of the fault location.</p>
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<p>Fault map based on the fusion of the amplitude gradient attribute (blue) and ant tracking attribute (black). Shallow parts of the fault are primarily formed by oblique structures, while deeper sections are predominantly influenced by compressional and torsional faults.</p>
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<p>Strike-slip fault segment interpretations. The fault section interpretation consists of 6 sections, each of which includes the original seismic dataset, amplitude gradient attribute, ant tracking attribute, fusion attribute, and fault interpretation (red lines): (<b>a</b>) the tensile section, located at the tail of the fault, contains a relay-type fault in the tensile environment; (<b>b</b>) the extrusion section, located in the transition region from the tail of the fault to the middle of the fault, is affected by the extrusion environment and has an obvious internal structure of the fault; (<b>c</b>) the extrusion section, located in the middle of the fault, has more intense extrusion action; (<b>d</b>) the main displacement section, located in the middle of the fault, has a few branch faults; (<b>e</b>) the main displacement section, located in the transition region from the middle of the fault to the tail, has obvious strike-slip and no branch faults; and (<b>f</b>) the tensile section, located in the tail of the fault, has a large branch fault.</p>
Full article ">Figure 11 Cont.
<p>Strike-slip fault segment interpretations. The fault section interpretation consists of 6 sections, each of which includes the original seismic dataset, amplitude gradient attribute, ant tracking attribute, fusion attribute, and fault interpretation (red lines): (<b>a</b>) the tensile section, located at the tail of the fault, contains a relay-type fault in the tensile environment; (<b>b</b>) the extrusion section, located in the transition region from the tail of the fault to the middle of the fault, is affected by the extrusion environment and has an obvious internal structure of the fault; (<b>c</b>) the extrusion section, located in the middle of the fault, has more intense extrusion action; (<b>d</b>) the main displacement section, located in the middle of the fault, has a few branch faults; (<b>e</b>) the main displacement section, located in the transition region from the middle of the fault to the tail, has obvious strike-slip and no branch faults; and (<b>f</b>) the tensile section, located in the tail of the fault, has a large branch fault.</p>
Full article ">Figure 11 Cont.
<p>Strike-slip fault segment interpretations. The fault section interpretation consists of 6 sections, each of which includes the original seismic dataset, amplitude gradient attribute, ant tracking attribute, fusion attribute, and fault interpretation (red lines): (<b>a</b>) the tensile section, located at the tail of the fault, contains a relay-type fault in the tensile environment; (<b>b</b>) the extrusion section, located in the transition region from the tail of the fault to the middle of the fault, is affected by the extrusion environment and has an obvious internal structure of the fault; (<b>c</b>) the extrusion section, located in the middle of the fault, has more intense extrusion action; (<b>d</b>) the main displacement section, located in the middle of the fault, has a few branch faults; (<b>e</b>) the main displacement section, located in the transition region from the middle of the fault to the tail, has obvious strike-slip and no branch faults; and (<b>f</b>) the tensile section, located in the tail of the fault, has a large branch fault.</p>
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18 pages, 2222 KiB  
Article
Frequency-Domain Features and Low-Frequency Synchronization of Photoplethysmographic Waveform Variability and Heart Rate Variability with Increasing Severity of Cardiovascular Diseases
by Anton R. Kiselev, Olga M. Posnenkova, Anatoly S. Karavaev, Vladimir A. Shvartz, Mikhail Yu. Novikov and Vladimir I. Gridnev
Biomedicines 2024, 12(9), 2088; https://doi.org/10.3390/biomedicines12092088 - 12 Sep 2024
Viewed by 584
Abstract
Objective—Heart rate variability (HRV) and photoplethysmographic waveform variability (PPGV) are available approaches for assessing the state of cardiovascular autonomic regulation. The goal of our study was to compare the frequency-domain features and low-frequency (LF) synchronization of the PPGV and HRV with increasing [...] Read more.
Objective—Heart rate variability (HRV) and photoplethysmographic waveform variability (PPGV) are available approaches for assessing the state of cardiovascular autonomic regulation. The goal of our study was to compare the frequency-domain features and low-frequency (LF) synchronization of the PPGV and HRV with increasing severity of cardiovascular diseases. Methods—Our study included 998 electrocardiogram (ECG) and finger photoplethysmogram (PPG) recordings from subjects, classified into five categories: 53 recordings from healthy subjects, aged 28.1 ± 6.2 years, 536 recordings from patients with hypertension (HTN), 49.0 ± 8.8 years old, 185 recordings from individuals with stable coronary artery disease (CAD) (63.9 ± 9.3 years old), 104 recordings from patients with myocardial infarction (MI) that occurred three months prior to the recordings (PMI) (65.1 ± 11.0 years old), and 120 recordings from study subjects with acute myocardial infarction (AMI) (64.7 ± 11.5 years old). Spectral analyses of the HRV and PPGV were carried out, along with an assessment of the synchronization strength between LF oscillations of the HRV and of PPGV (synchronization index). Results—Changes in all frequency-domain indices and the synchronization index were observed along the following gradient: healthy subjects → patients with HTN → patients with CAD → patients with PMI → patients with AMI. Similar frequency-domain indices of the PPGV and HRV show little relationship with each other. Conclusions—The frequency-domain indices of the PPGV are highly sensitive to the development of any cardiovascular disease and, therefore, are superior to the HRV indices in this regard. The S index is an independent parameter from the frequency-domain indices. Full article
(This article belongs to the Section Biomedical Engineering and Materials)
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<p>Cumulative distribution curves of frequency-domain indices (LF%, HF%, and LF/HF) of heart rate variability (HRV) (<b>a</b>,<b>c</b>,<b>e</b>) and photoplethysmographic waveform variability (PPGV) (<b>b</b>,<b>d</b>,<b>f</b>) in healthy subjects, patients with hypertension (HTN), patients with coronary artery disease (CAD), patients with previous myocardial infarction (PMI), and patients with acute myocardial infarction (AMI).</p>
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<p>Scatterplot of LF%<sub>PPGV</sub> vs. HF%<sub>PPGV</sub>.</p>
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<p>Cumulative distribution curves of the S index in healthy subjects, patients with hypertension (HTN), patients with coronary artery disease (CAD), patients with previous myocardial infarction (PMI), and patients with acute myocardial infarction (AMI).</p>
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16 pages, 46185 KiB  
Article
Contribution of Metastable Oxygen Spectra to Fluctuated Waveform Tails after Breakdown Time in Air under Positive and Negative Impulse Voltages
by Muhammad Ikhwanus and Takeshi Morimoto
Eng 2024, 5(3), 2264-2279; https://doi.org/10.3390/eng5030117 - 9 Sep 2024
Viewed by 349
Abstract
In this study, we explored the correlation between fluctuated waveform tails under both positive and negative impulse voltages and their corresponding spectral lines during millisecond observations of arc discharge. We examined impulse voltages in ±100, ±125, and ±150 kV across 3, 3.5, and [...] Read more.
In this study, we explored the correlation between fluctuated waveform tails under both positive and negative impulse voltages and their corresponding spectral lines during millisecond observations of arc discharge. We examined impulse voltages in ±100, ±125, and ±150 kV across 3, 3.5, and 4 cm gaps using spectroscopic analysis focused on oxygen excitations. Six selected spectra in ±100, ±125, and ±150 kV at 3.5 cm and two negative spectra of −100 kV at 3 and 4 cm were analyzed by identifying spectral lines in the wavelength range of 200–900 nm. The results revealed a correlation between the fluctuated waveform tails and spectral lines in positive voltage discharges, which were almost similar, while in negative voltage discharges, this correlation was found only in −100 kV at 3 and 4 cm. We concluded that during the spark phase for both positive and negative voltage discharges, symmetrical fluctuation in the waveform tails was observed after breakdown time, especially above the voltage level of the recombination phase. This suggested the presence of energetic oxygen excited states in the 200–400 nm range, with higher peak intensity than the O I line at 777.417 nm, observed in most positive impulse voltage discharges and at −100 kV with 3 and 4 cm gaps, contributing to rapid breakdown. Full article
(This article belongs to the Section Electrical and Electronic Engineering)
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<p>Experimental platform.</p>
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<p>Impulse breakdown voltages in the 200–400 nm, and 400–900 nm spectra. (<b>a</b>) Positive impulse voltages of ±100, ±125, and ±150 kV at 3, and 3.5 cm gap distances; (<b>b</b>) Negative impulse voltages with additional spectra of −100, −125, and −150 kV at 4 cm.</p>
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<p>Impulse breakdown voltages in the 200–400 nm, and 400–900 nm spectra. (<b>a</b>) Positive impulse voltages of ±100, ±125, and ±150 kV at 3, and 3.5 cm gap distances; (<b>b</b>) Negative impulse voltages with additional spectra of −100, −125, and −150 kV at 4 cm.</p>
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<p>Various oxygen distributions in positive and negative voltages at 3, 3.5, and 4 cm gaps.</p>
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<p>t<sub>o</sub> = static breakdown time, t<sub>a</sub> = build-up time for the avalanche, t<sub>arc</sub> = start arc discharge time; in spark phase with oxygen distributions. (<b>a</b>) +100 kV at 3.5 cm; (<b>b</b>) −100 kV at 3 cm.</p>
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<p>The symmetrical fluctuated waveform tails. (<b>a</b>) Positive impulse voltage; (<b>b</b>) negative impulse voltage.</p>
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32 pages, 10548 KiB  
Article
GAN-SkipNet: A Solution for Data Imbalance in Cardiac Arrhythmia Detection Using Electrocardiogram Signals from a Benchmark Dataset
by Hari Mohan Rai, Joon Yoo and Serhii Dashkevych
Mathematics 2024, 12(17), 2693; https://doi.org/10.3390/math12172693 - 29 Aug 2024
Cited by 1 | Viewed by 443
Abstract
Electrocardiography (ECG) plays a pivotal role in monitoring cardiac health, yet the manual analysis of ECG signals is challenging due to the complex task of identifying and categorizing various waveforms and morphologies within the data. Additionally, ECG datasets often suffer from a significant [...] Read more.
Electrocardiography (ECG) plays a pivotal role in monitoring cardiac health, yet the manual analysis of ECG signals is challenging due to the complex task of identifying and categorizing various waveforms and morphologies within the data. Additionally, ECG datasets often suffer from a significant class imbalance issue, which can lead to inaccuracies in detecting minority class samples. To address these challenges and enhance the effectiveness and efficiency of cardiac arrhythmia detection from imbalanced ECG datasets, this study proposes a novel approach. This research leverages the MIT-BIH arrhythmia dataset, encompassing a total of 109,446 ECG beats distributed across five classes following the Association for the Advancement of Medical Instrumentation (AAMI) standard. Given the dataset’s inherent class imbalance, a 1D generative adversarial network (GAN) model is introduced, incorporating the Bi-LSTM model to synthetically generate the two minority signal classes, which represent a mere 0.73% fusion (F) and 2.54% supraventricular (S) of the data. The generated signals are rigorously evaluated for similarity to real ECG data using three key metrics: mean squared error (MSE), structural similarity index (SSIM), and Pearson correlation coefficient (r). In addition to addressing data imbalance, the work presents three deep learning models tailored for ECG classification: SkipCNN (a convolutional neural network with skip connections), SkipCNN+LSTM, and SkipCNN+LSTM+Attention mechanisms. To further enhance efficiency and accuracy, the test dataset is rigorously assessed using an ensemble model, which consistently outperforms the individual models. The performance evaluation employs standard metrics such as precision, recall, and F1-score, along with their average, macro average, and weighted average counterparts. Notably, the SkipCNN+LSTM model emerges as the most promising, achieving remarkable precision, recall, and F1-scores of 99.3%, which were further elevated to an impressive 99.60% through ensemble techniques. Consequently, with this innovative combination of data balancing techniques, the GAN-SkipNet model not only resolves the challenges posed by imbalanced data but also provides a robust and reliable solution for cardiac arrhythmia detection. This model stands poised for clinical applications, offering the potential to be deployed in hospitals for real-time cardiac arrhythmia detection, thereby benefiting patients and healthcare practitioners alike. Full article
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<p>Sample ECG beats in the AAMI classes. Zero padding was applied to standardize all segment lengths to 187.</p>
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<p>(<b>a</b>) Schema of Bi-LSTM architecture (<b>left</b>) and (<b>b</b>) schema of attention model architecture (<b>right</b>).</p>
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<p>Block diagram of the proposed methodology for the classification of cardiac arrhythmia.</p>
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<p>Proposed GAN architecture for minority ECG data augmentation.</p>
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<p>Layer-wise architectures of the proposed ECG classification deep models.</p>
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<p>Generation of ECG beats of the S class by the GAN model. Each graph depicts overlayed synthetic ECG signals with uniform fixed length (size 187) in common with the pre-processed input ECG signals; the graphs are shown from left to right and top to bottom in the temporal sequence of the generated signals at intervals of 900 training epochs. Compared with the beginning of training (<b>top left graph</b>), the synthetic signals demonstrate more convergence toward the end of training (<b>bottom right graph</b>).</p>
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<p>Real (<b>left</b>) and GAN-generated synthetic (<b>right</b>) ECG beats of the S class. The synthetic ECG beat appears visually realistic.</p>
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<p>Visual depiction of progressive discriminator training error (which quantifies differences between the real and synthetic ECG signals) and generator training error measured over 3000 epochs during ECG beat generation of the S class using the GAN model. The discriminator training error is reduced substantially with training, whereas the generator training error remains largely flat.</p>
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<p>Generation of ECG beats of the F class by the GAN model. Each graph depicts overlayed synthetic ECG signals with uniform fixed length (size 187) in common with the pre-processed input ECG signals; the graphs are shown from left to right and top to bottom in the temporal sequence of the generated signals at intervals of 900 training epochs. Compared with the beginning of training (<b>top left graph</b>), the synthetic signals demonstrate more convergence toward the end of training (<b>bottom right graph</b>).</p>
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<p>Real (<b>left</b>) and GAN-generated synthetic (<b>right</b>) ECG beats of the F class. The synthetic ECG beat appears visually realistic.</p>
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<p>Visual depiction of progressive discriminator training error (which quantifies differences between the real and synthetic ECG signals) and generator training error measured over 3000 epochs during ECG beat generation of the F class using the GAN model. The discriminator training error is reduced substantially with training, whereas the generator training error increases initially but then decreases and remains flat.</p>
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<p>Randomly selected real (<b>left</b>) and synthetic (<b>right</b>) ECG signals of the S class, with corresponding calculated similarity matching scores MSE, SSIM, and r.</p>
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<p>Randomly selected real (<b>left</b>) and synthetic (<b>right</b>) ECG signals of the F class, with corresponding calculated similarity matching scores MSE, SSIM, and r.</p>
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<p>Loss function curves (<b>left</b>) and performance metrics curves (<b>right</b>) during 100 epochs of training with the SkipCNN model.</p>
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<p>SkipCNN classification performance for individual ECG beat classes and across all arrhythmia classes in the test dataset.</p>
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<p>Loss function curves (<b>left</b>) and performance metrics curves (<b>right</b>) during 100 epochs of training with the SkipCNN+LSTM model.</p>
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<p>SkipCNN-LSTM classification performance for individual ECG beat classes and across all arrhythmia classes in the test dataset.</p>
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<p>Loss function curves (<b>left</b>) and performance metric curves (<b>right</b>) during 100 epochs of training with the SkipCNN+LSTM+Attention model.</p>
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<p>Arrhythmia detection outcomes in terms of performance metrics using the proposed SkipCNN+LSTM+Attention model.</p>
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<p>Confusion matrix of arrhythmia detection using the ensemble model.</p>
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14 pages, 549 KiB  
Communication
Joint Constant-Modulus Waveform and RIS Phase Shift Design for Terahertz Dual-Function MIMO Radar and Communication System
by Rui Yang, Hong Jiang and Liangdong Qu
Remote Sens. 2024, 16(16), 3083; https://doi.org/10.3390/rs16163083 - 21 Aug 2024
Viewed by 671
Abstract
This paper considers a terahertz (THz) dual-function multi-input multi-output (MIMO) radar and communication system with the assistance of a reconfigurable intelligent surface (RIS) and jointly designs the constant modulus (CM) waveform and RIS phase shifts. A weighted optimization scheme is presented, to minimize [...] Read more.
This paper considers a terahertz (THz) dual-function multi-input multi-output (MIMO) radar and communication system with the assistance of a reconfigurable intelligent surface (RIS) and jointly designs the constant modulus (CM) waveform and RIS phase shifts. A weighted optimization scheme is presented, to minimize the weighted sum of three objectives, including communication multi-user interference (MUI) energy, the negative of multi-target illumination power and the MIMO radar waveform similarity error under a CM constraint. For the formulated non-convex problem, a novel alternating coordinate descent (ACD) algorithm is introduced, to transform it into two subproblems for waveform and phase shift design. Unlike the existing optimization algorithms that solve each subproblem by iteratively approximating the optimal solution with iteration stepsize selection, the ACD algorithm can alternately solve each subproblem by dividing it into multiple simpler problems, to achieve closed-form solutions. Our numerical simulations demonstrate the superiorities of the ACD algorithm over the existing methods. In addition, the impacts of the weighting coefficients, RIS and channel conditions on the radar communication performance of the THz system are analyzed. Full article
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<p>RIS-aided THz dual-function MIMO radar and communication system with multiple targets and UEs.</p>
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<p>Sum rate versus the transmit SNR for different algorithms.</p>
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<p>Beampatterns of the transmit waveforms achieved by different algorithms.</p>
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<p>Auto-correlation functions achieved by different algorithms.</p>
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<p>Sum rate versus the transmit SNR of our algorithm under different weighting coefficients and RIS conditions.</p>
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<p>Beampatterns of the transmit waveforms of our algorithm under different weighting coefficients and RIS conditions.</p>
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<p>Average detection probability versus the radar transmit SNR of our algorithm under different weighting coefficients and RIS conditions.</p>
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<p>Auto-correlation functions of the transmit waveforms of our algorithm under different weighting coefficients and RIS conditions.</p>
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<p>Sum rate versus the transmit SNR under different channel conditions of THz system.</p>
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17 pages, 1193 KiB  
Article
An Intrinsically Explainable Method to Decode P300 Waveforms from EEG Signal Plots Based on Convolutional Neural Networks
by Brian Ezequiel Ail, Rodrigo Ramele, Juliana Gambini and Juan Miguel Santos
Brain Sci. 2024, 14(8), 836; https://doi.org/10.3390/brainsci14080836 - 20 Aug 2024
Viewed by 947
Abstract
This work proposes an intrinsically explainable, straightforward method to decode P300 waveforms from electroencephalography (EEG) signals, overcoming the black box nature of deep learning techniques. The proposed method allows convolutional neural networks to decode information from images, an area where they have achieved [...] Read more.
This work proposes an intrinsically explainable, straightforward method to decode P300 waveforms from electroencephalography (EEG) signals, overcoming the black box nature of deep learning techniques. The proposed method allows convolutional neural networks to decode information from images, an area where they have achieved astonishing performance. By plotting the EEG signal as an image, it can be both visually interpreted by physicians and technicians and detected by the network, offering a straightforward way of explaining the decision. The identification of this pattern is used to implement a P300-based speller device, which can serve as an alternative communication channel for persons affected by amyotrophic lateral sclerosis (ALS). This method is validated by identifying this signal by performing a brain–computer interface simulation on a public dataset from ALS patients. Letter identification rates from the speller on the dataset show that this method can identify the P300 signature on the set of 8 patients. The proposed approach achieves similar performance to other state-of-the-art proposals while providing clinically relevant explainability (XAI). Full article
(This article belongs to the Special Issue Emerging Topics in Brain-Computer Interface)
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<p>P300-speller matrix used in the ex periment. The 7 five-letter words, divided into train and testing, are shown on top. These are used in the P300 experiment for the copy-spelling task.</p>
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<p>Two alternatives pipelines are used: (<b>top</b>) with channel selection, (<b>bottom</b>) bundling the information from all the channels together.</p>
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<p>The three architectures proposed in this work. (<b>a</b>) VGG16: First version of the CNN. The input is a binary image plot of a signal of size <math display="inline"><semantics> <mrow> <mn>150</mn> <mo>×</mo> <mn>150</mn> </mrow> </semantics></math>. Then follows a set of 6 convolutional layers, followed by 4 fully connected layers, and a final layer activated using a sigmoid function. (<b>b</b>) The second, SV16 is similar to VGG16, with the same input but has 4 convolutional layers and 3 dense layers. (<b>c</b>) Finally, MSV16 has the same architecture as the SV16, but now the input layer is modified for an 8-channel input, with one binary image plotted with a signal waveform per channel. MaxPool layers are shown in dark orange.</p>
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<p>Side-by-side comparison of letter identification rate (<span class="html-italic">y</span>) per number of letter intensifications (<span class="html-italic">x</span>) for all the three architectures proposed in this work and one more for comparison: (<b>a</b>) VGG16, (<b>b</b>) SV16 and (<b>c</b>) MSV16, (<b>d</b>) SIFT method [<a href="#B45-brainsci-14-00836" class="html-bibr">45</a>].</p>
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<p>Learning curve, showing loss, training accuracy and validation accuracy of subject 5 on channel PO8 with an intensification level of 4 using (<b>a</b>) VGG16 and (<b>b</b>) SV16.</p>
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<p>Images of P300 waveforms (<b>a</b>,<b>c</b>) from the first <math display="inline"><semantics> <mrow> <mn>0.700</mn> </mrow> </semantics></math> ms of stimulus-locked segments of channel Cz of subject 8, obtained by averaging the signal segments triggered from 5 intensifications. Images (<b>b</b>,<b>d</b>) are the obtained shape when this waveform is not present.</p>
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<p>Accuracy of MSV16 on subject 8; the red dotted line shows a normal prediction using real labels on the training set, while the pink line shows the predictions of the CNN by training it with randomized labels on the training set. We can see that the accuracy on the pink line hovers around the chance level of 3%.</p>
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21 pages, 7707 KiB  
Article
Prototype Implementation of a Digitizer for Earthquake Monitoring System
by Emad B. Helal, Omar M. Saad, M. Sami Soliman, Gamal M. Dousoky, Ahmed Abdelazim, Lotfy Samy, Haruichi Kanaya and Ali G. Hafez
Sensors 2024, 24(16), 5287; https://doi.org/10.3390/s24165287 - 15 Aug 2024
Viewed by 500
Abstract
A digitizer is considered one of the fundamental components of an earthquake monitoring system. In this paper, we design and implement a high accuracy seismic digitizer. The implemented digitizer consists of several blocks, i.e., the analog-to-digital converter (ADC), GPS receiver, and microprocessor. Three [...] Read more.
A digitizer is considered one of the fundamental components of an earthquake monitoring system. In this paper, we design and implement a high accuracy seismic digitizer. The implemented digitizer consists of several blocks, i.e., the analog-to-digital converter (ADC), GPS receiver, and microprocessor. Three finite impulse response (FIR) filters are used to decimate the sampling rate of the input seismic data according to user needs. A graphical user interface (GUI) has been designed for enabling the user to monitor the seismic waveform in real time, and process and adjust the parameters of the acquisition unit. The system casing is designed to resist harsh conditions of the environment. The prototype can represent the three component sensors data in the standard MiniSEED format. The digitizer stream seismic data from the remote station to the main center is based on TCP/IP connection. This protocol ensures data transmission without any losses as long as the data still exist in the ring buffer. The prototype was calibrated by real field testing. The prototype digitizer is integrated with the Egyptian National Seismic Network (ENSN), where a commercial instrument is already installed. Case studies shows that, for the same event, the prototype station improves the solution of the ENSN by giving accurate timing and seismic event parameters. Field test results shows that the event arrival time and the amplitude are approximately the same between the prototype digitizer and the calibrated digitizer. Furthermore, the frequency contents are similar between the two digitizers. Therefore, the prototype digitizer captures the main seismic parameters accurately, irrespective of noise existence. Full article
(This article belongs to the Section Remote Sensors)
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<p>System wiring diagram.</p>
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<p>(<b>a</b>) System front panel; (<b>b</b>) system top view.</p>
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<p>Ring server as a simple SeedLink server.</p>
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<p>Multistage multi-rate filter design.</p>
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<p>The FIR magnitude response for (<b>a</b>) the first stage, (<b>b</b>) the second stage, and (<b>c</b>) the third stage.</p>
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<p>Real-time waveform using the implemented digitizer.</p>
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<p>Health tab of the system.</p>
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<p>GPS control tab.</p>
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<p>Test station with the calibrated digitizer.</p>
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<p>Acquired data from three sensor channels.</p>
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<p>Data comparison between test digitizer (<b>a</b>) and centaur digitizer (<b>b</b>).</p>
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<p>Zooming in on the event interval.</p>
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<p>Comparison between the two waveforms.</p>
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<p>Amplitude spectrum for the prototype (<b>a</b>) and calibrated (<b>b</b>) digitizers.</p>
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<p>Spectrogram for prototype (<b>a</b>) and calibrated (<b>b</b>) digitizers.</p>
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<p>Case study #1 event map.</p>
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<p>Case study #2 event map.</p>
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15 pages, 6609 KiB  
Article
Simulation on Operating Overvoltage of Dropping Pantograph Based on Pantograph–Catenary Arc and Variable Capacitance Model
by Dazuo Jiang, Huanqing Zou, Yike Guo, Fuqiang Tian, Hongqi Liu and Yufeng Yin
Appl. Sci. 2024, 14(16), 6861; https://doi.org/10.3390/app14166861 - 6 Aug 2024
Viewed by 465
Abstract
When the electric locomotive pantograph is dropping, the interruption of pantograph catenary contact causes electromagnetic oscillation and arcing. The frequent arc burning that occurs due to charge accumulation results in the amplitude of overvoltage increasing gradually, posing a threat to locomotive high-voltage equipment. [...] Read more.
When the electric locomotive pantograph is dropping, the interruption of pantograph catenary contact causes electromagnetic oscillation and arcing. The frequent arc burning that occurs due to charge accumulation results in the amplitude of overvoltage increasing gradually, posing a threat to locomotive high-voltage equipment. However, the physical mechanisms and characteristics of overvoltage are still unclear. This paper proposes a simulation model of operating overvoltage due to a dropping pantograph based on the pantograph–catenary arc and variable capacitance. Distributed RLC electromagnetic oscillation is considered, which allows the real-time calculation of arc resistance and capacitance. Under the same working conditions, the error between the simulation and test results is less than 4.0%, which proves the credibility of the model. The variation law of overvoltage under different dropping speeds or catenary phases was investigated, which shows the max amplitude is 298.20 kV and steepness is 2096.80 kV/μs at 0.30 m/s speed. The waveform shows the characteristics of high amplitude and high steepness, similar to very fast transient overvoltage (VFTO). There is a sinusoidal relationship between the catenary phase and overvoltage amplitude. The closer the catenary phase to 90°, the higher the overvoltage amplitude. The research has important guiding significance for the overvoltage formation mechanism of a traction power supply system and the insulation coordination design of high-voltage equipment. Full article
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<p>Three stages of arc development.</p>
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<p>Multiple arc reignitions in dropping pantograph operating overvoltage scenario.</p>
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<p>Arc reignition and extinguishing. (<b>a</b>) Reignition. (<b>b</b>) Extinguishing.</p>
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<p>Actual structure and equal-proportion simulated structure of HX<sub>D</sub>1 electric locomotive pantograph. (<b>a</b>) Actual pantograph model. (<b>b</b>) Simulated pantograph model.</p>
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<p>Equivalent circuit of pantograph and catenary.</p>
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<p>Locomotive simulation circuit.</p>
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<p>Pantograph–catenary distance control module.</p>
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<p>Arc burning detection module.</p>
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<p>Arc resistance and variable capacitance calculation module.</p>
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<p>Testing system.</p>
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<p>Comparison of simulated and test waveforms. (<b>a</b>) First time. (<b>b</b>) Second time. (<b>c</b>) Third time.</p>
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<p>Relationship between operating overvoltage of dropping pantograph amplitude and pantograph dropping speed.</p>
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<p>Overvoltage waveforms at different pantograph dropping speeds.</p>
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<p>Relationship between the amplitude of the dropping pantograph’s operating overvoltage and the catenary voltage phase.</p>
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17 pages, 791 KiB  
Article
Using Transfer Learning to Realize Low Resource Dungan Language Speech Synthesis
by Mengrui Liu, Rui Jiang and Hongwu Yang
Appl. Sci. 2024, 14(14), 6336; https://doi.org/10.3390/app14146336 - 20 Jul 2024
Viewed by 694
Abstract
This article presents a transfer-learning-based method to improve the synthesized speech quality of the low-resource Dungan language. This improvement is accomplished by fine-tuning a pre-trained Mandarin acoustic model to a Dungan language acoustic model using a limited Dungan corpus within the Tacotron2+WaveRNN framework. [...] Read more.
This article presents a transfer-learning-based method to improve the synthesized speech quality of the low-resource Dungan language. This improvement is accomplished by fine-tuning a pre-trained Mandarin acoustic model to a Dungan language acoustic model using a limited Dungan corpus within the Tacotron2+WaveRNN framework. Our method begins with developing a transformer-based Dungan text analyzer capable of generating unit sequences with embedded prosodic information from Dungan sentences. These unit sequences, along with the speech features, provide <unit sequence with prosodic labels, Mel spectrograms> pairs as the input of Tacotron2 to train the acoustic model. Concurrently, we pre-trained a Tacotron2-based Mandarin acoustic model using a large-scale Mandarin corpus. The model is then fine-tuned with a small-scale Dungan speech corpus to derive a Dungan acoustic model that autonomously learns the alignment and mapping of the units to the spectrograms. The resulting spectrograms are converted into waveforms via the WaveRNN vocoder, facilitating the synthesis of high-quality Mandarin or Dungan speech. Both subjective and objective experiments suggest that the proposed transfer learning-based Dungan speech synthesis achieves superior scores compared to models trained only with the Dungan corpus and other methods. Consequently, our method offers a strategy to achieve speech synthesis for low-resource languages by adding prosodic information and leveraging a similar, high-resource language corpus through transfer learning. Full article
(This article belongs to the Special Issue Computational Linguistics: From Text to Speech Technologies)
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<p>The framework of Tacotron2+WaveRNN-based Dungan speech synthesis.</p>
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<p>Procedure of Dungan text analysis.</p>
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<p>Structure of a Dungan character.</p>
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<p>The framework of BLSTM_CRF-based Dungan Prosodic Boundary Prediction. The input is a Dungan sentence with prosodic information.</p>
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<p>The framework of Transformer-based Dungan character-to-unit conversion. The input is a Dungan sentence with prosodic information (<b>left</b>) and its corresponding Pinyin sequence (<b>right</b>). The output is the Pinyin sequence with prosodic information.</p>
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<p>Procedure of training the Dungan language acoustic model with transfer learning.</p>
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<p>The average MOS scores of synthesized Dungan speech under 95% confidence intervals.</p>
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<p>The average MOS scores of synthesized Mandarin speech under 95% confidence intervals.</p>
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<p>The average DMOS scores of synthesized Dungan speech under 95% confidence intervals.</p>
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<p>The average DMOS scores of synthesized Mandarin speech under 95% confidence intervals.</p>
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16 pages, 14753 KiB  
Article
Fabrication and Dielectric Validation of an Arm Phantom for Electromyostimulation
by Katja Uhrhan, Esther Schwindt and Hartmut Witte
Bioengineering 2024, 11(7), 724; https://doi.org/10.3390/bioengineering11070724 - 17 Jul 2024
Viewed by 881
Abstract
Electromyostimulation (EMS) is an up-and-coming training method that demands further fundamental research regarding its safety and efficacy. To investigate the influence of different stimulation parameters, electrode positions and electrode sizes on the resulting voltage in the tissue, a tissue mimicking phantom is needed. [...] Read more.
Electromyostimulation (EMS) is an up-and-coming training method that demands further fundamental research regarding its safety and efficacy. To investigate the influence of different stimulation parameters, electrode positions and electrode sizes on the resulting voltage in the tissue, a tissue mimicking phantom is needed. Therefore, this study describes the fabrication of a hydrogel arm phantom for EMS applications with the tissue layers of skin, fat, blood and muscle. The phantom was dielectrically validated in the frequency range of 20 Hz to 100 Hz. We also conducted electromyography (EMG) recordings during EMS on the phantom and compared them with the same measurements on a human arm. The phantom reproduces the dielectric properties of the tissues with deviations ranging from 0.8% to more than 100%. Although we found it difficult to find a compromise between mimicking the permittivity and electrical conductivity at the same time, the EMS–EMG measurements showed similar waveforms (1.9–9.5% deviation) in the phantom and human. Our research contributes to the field of dielectric tissue phantoms, as it proposes a multilayer arm phantom for EMS applications. Consequently, the phantom can be used for initial EMS investigations, but future research should focus on further improving the dielectric properties. Full article
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<p>Schematic representation of the layered gelatin phantom.</p>
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<p>Measuring setup for dielectric validations of the samples. (<b>a</b>) Placing the phantom sample on the copper plate; (<b>b</b>) parallel plate setup with sandwiched sample; (<b>c</b>) measurement setup with parallel plate method and LCR meter.</p>
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<p>Possible equivalent circuits of the sample during dielectric measurement. (<b>a</b>) Parallel circuit and (<b>b</b>) series circuit of capacitance and resistance.</p>
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<p>Measurement setup for electromyography (EMG) recordings during electromyostimulation (EMS) on the arm phantom.</p>
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<p>Comparison of the measured dielectric properties of a 25% gelatin sample with reference data from the study of Kalra et al. [<a href="#B21-bioengineering-11-00724" class="html-bibr">21</a>]: (<b>a</b>) relative permittivity, (<b>b</b>) electrical conductivity.</p>
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<p>Dielectric properties of different tissue phantoms compared to reference values of biological tissue from IT’IS database [<a href="#B23-bioengineering-11-00724" class="html-bibr">23</a>].</p>
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<p>Relative deviations in conductivity and permittivity of the selected phantom samples over the course of frequency.</p>
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<p>EMG signal section during electrical stimulation on the arm phantom vs. on a human arm: (<b>a</b>) phantom, 50 Hz, intensity level 15; (<b>b</b>) human, 50 Hz, intensity level 15; (<b>c</b>) phantom, 100 Hz, intensity level 23; (<b>d</b>) human, 100 Hz, intensity level 23. Pulse width: 300 µs, sampling rate: 4 kHz.</p>
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Article
Geomagnetic Disturbances and Pulse Amplitude Anomalies Preceding M > 6 Earthquakes from 2021 to 2022 in Sichuan-Yunnan, China
by Xia Li, Rui Qu, Yingfeng Ji, Lili Feng, Weiling Zhu, Ye Zhu, Xiaofeng Liao, Manqiu He, Zhisheng Feng, Wenjie Fan, Chang He, Weiming Wang and Haris Faheem
Sensors 2024, 24(13), 4280; https://doi.org/10.3390/s24134280 - 1 Jul 2024
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Abstract
Compelling evidence has shown that geomagnetic disturbances in vertical intensity polarization before great earthquakes are promising precursors across diverse rupture conditions. However, the geomagnetic vertical intensity polarization method uses the spectrum of smooth signals, and the anomalous waveforms of seismic electromagnetic radiation, which [...] Read more.
Compelling evidence has shown that geomagnetic disturbances in vertical intensity polarization before great earthquakes are promising precursors across diverse rupture conditions. However, the geomagnetic vertical intensity polarization method uses the spectrum of smooth signals, and the anomalous waveforms of seismic electromagnetic radiation, which are basically nonstationary, have not been adequately considered. By combining pulse amplitude analysis and an experimental study of the cumulative frequency of anomalies, we found that the pulse amplitudes before the 2022 Luding M6.8 earthquake show characteristics of multiple synchronous anomalies, with the highest (or higher) values occurring during the analyzed period. Similar synchronous anomalies were observed before the 2021 Yangbi M6.4 earthquake, the 2022 Lushan M6.1 earthquake and the 2022 Malcolm M6.0 earthquake, and these anomalies indicate migration from the periphery toward the epicenters over time. The synchronous changes are in line with the recognition of previous geomagnetic anomalies with characteristics of high values before an earthquake and gradual recovery after the earthquake. Our study suggests that the pulse amplitude is effective for extracting anomalies in geomagnetic vertical intensity polarization, especially in the presence of nonstationary signals when utilizing observations from multiple station arrays. Our findings highlight the importance of incorporating pulse amplitude analysis into earthquake prediction research on geomagnetic disturbances. Full article
(This article belongs to the Collection Seismology and Earthquake Engineering)
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Figure 1

Figure 1
<p>Tectonic map of the study area. The yellow circles indicate the M &gt; 6 earthquakes in this region from 2021 to 2022 (1: 2022 Malcolm M6.0; 2: 2022 Lushan M6.1; 3: 2022 Luding M6.8; 4: 2021 Yangbi M6.4). The triangles represent the nine stations of the newly constructed Sichuan-Yunnan regional testbed station array used in this study (1: Deyang; 2: Chongzhou; 3: Renshou; 4: Xingjing; 5: Fushun; 6: Xichang; 7: Muli; 8: Shimenkan; 9: Nanshan).</p>
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<p>Geomagnetic anomalies observed on November 20, 2021. (<b>a</b>) Geomagnetic vertical intensity polarization value (<span class="html-italic">y</span>-axis, this study) with a precision of seconds; (<b>b</b>–<b>d</b>) geomagnetic vertical intensity polarization value (<span class="html-italic">y</span>-axis, this study) with a precision of 0.01 s: (<b>b</b>) northward; (<b>c</b>) eastward; (<b>d</b>) vertical.</p>
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<p>Geomagnetic vertical intensity polarization values (<span class="html-italic">y</span>-axis, this study) of the Sichuan-Yunnan station array before the Luding M6.8 earthquake on 5 September 2022. (<b>a</b>) Geomagnetic vertical intensity polarization pulse amplitude variations. Upper: Xichang station; middle: Xingjing station; lower: Deyang station. (<b>b</b>) Cumulative number of times per day that the pulse amplitude exceeds the threshold value. Upper: Xichang station; middle: Xingjing station; lower: Deyang station.</p>
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<p>Geomagnetic vertical intensity polarization values (<span class="html-italic">y</span>-axis, this study) of the Sichuan-Yunnan station array before the 2021 Yangbi M6.4 earthquake on 21 May 2021. (<b>a</b>) Geomagnetic vertical intensity polarization pulse amplitude variations. Upper: Xichang station; middle: Muli station; lower: Nanshan station. (<b>b</b>) Cumulative number of times per day that the pulse amplitude exceeds the threshold value. Upper: Xichang station; middle: Muli station; lower: Nanshan station.</p>
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<p>Geomagnetic vertical intensity polarization values (<span class="html-italic">y</span>-axis, this study) of the Sichuan-Yunnan station array before the 2021 Yangbi M6.4 earthquake on 21 May 2021. (<b>a</b>) Geomagnetic vertical intensity polarization pulse amplitude variations. Upper: Xichang station; middle: Muli station; lower: Nanshan station. (<b>b</b>) Cumulative number of times per day that the pulse amplitude exceeds the threshold value. Upper: Xichang station; middle: Muli station; lower: Nanshan station.</p>
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<p>Geomagnetic vertical intensity polarization values (<span class="html-italic">y</span>-axis, this study) before the 2022 Lushan M6.1 and 2022 Malcolm M6.0 earthquakes. (<b>a</b>) Geomagnetic vertical intensity polarization pulse amplitude variations. Upper: Xichang station; lower: Fushun station. (<b>b</b>) Cumulative number of times per day that the pulse amplitude exceeds the threshold value. Upper: Xichang station; lower: Fushun station.</p>
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