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16 pages, 4811 KiB  
Article
Discovery of a New Cyanobacterial Genus (Paludothrix gen. nov.) from the Sanyang Wetland in Eastern China, Reflecting the Latest Taxonomic Status in Coleofasciculaceae
by Yangyang Wu, Yao Cheng, He Zhang, Ruozhen Geng, Peng Xiao, Baiyu Cui and Renhui Li
Diversity 2025, 17(1), 15; https://doi.org/10.3390/d17010015 (registering DOI) - 26 Dec 2024
Abstract
As our comprehension of cyanobacterial classification in diverse ecosystems broadens, it becomes essential to explore the biodiversity of lesser-known areas for a thorough understanding of both global and local diversity. This research, which is part of a larger investigation into soil biocrust algae [...] Read more.
As our comprehension of cyanobacterial classification in diverse ecosystems broadens, it becomes essential to explore the biodiversity of lesser-known areas for a thorough understanding of both global and local diversity. This research, which is part of a larger investigation into soil biocrust algae diversity in the Sanyang Wetland located in Zhejiang Province, China, introduces a novel taxon of non-heterocystous filamentous cyanobacteria employing a polyphasic approach for cyanobacterial classification, integrating morphological, molecular, ecological, and biogeographical considerations. The findings from morphological analysis, 16S rRNA gene sequencing, and the identification of the 16S-23S ITS rRNA region have led to the discovery of a new genus, Paludothrix, which is categorized within the family Coleofasciculaceae. The proposed generic name and specific epithet of these new taxa adhere completely to the guidelines established by the International Code of Nomenclature for algae, fungi, and plants. The modern taxonomic system of cyanobacteria is constantly being updated and improved. The description of new taxa using the polyphasic approach can enrich the relevant knowledge in the field of cyanobacteria classification. The results of this study will increase our understanding of terrestrial cyanobacteria within wetland environments. Full article
(This article belongs to the Special Issue Studies on Biodiversity and Ecology of Algae in China—2nd Edition)
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Figure 1

Figure 1
<p>Sanyang Wetland in Zhejiang Province, China, with the sampling site marked on the map (<b>S1</b>).</p>
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<p>Light microscopy of <span class="html-italic">Paludothrix granulosa</span> strains (<b>A</b>–<b>F</b>). Ultrastructure of <span class="html-italic">Paludothrix granulosa</span> strains. (Cd, cell division—formation of new cell wall; Th, thylakoids; Cg, cyanophycin granules; Nu, nuclear region). (<b>G</b>,<b>I</b>) Transverse section. (<b>H</b>) Longitudinal sections. Scale bars: (<b>A</b>) = 20 µm, (<b>B</b>–<b>G</b>) = 10 µm, (<b>G</b>–<b>I</b>) = 5 µm, and (<b>H</b>) = 2 µm.</p>
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<p>The phylogenetic tree of Coleofasciculaceae and outgroup strains was constructed using the maximum likelihood (ML) approach based on 16S rRNA gene sequences. On the BI tree, bootstrapping values exceeding 50% are displayed for both NJ and ML methods, along with Bayesian posterior probabilities. Asterisks (*) denote bootstrapping values of 100 in the ML analysis, NJ method, and BI posterior probabilities of 1.00. The new filamentous strains identified in this research is highlighted in bold.</p>
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<p>Secondary structures of the D1–D1′ helix in close Coleofasciculaceae species. (<b>a</b>–<b>f</b>) D1–D1′ helices: (<b>a</b>) <span class="html-italic">Paludothrix granulosa</span> WZU 2010. (<b>b</b>) <span class="html-italic">Coleofasciculus chthonoplastes</span> PCC 7420. (<b>c</b>) <span class="html-italic">Limnofasciculus baicalensis</span> BBK-W-15. (<b>d</b>) <span class="html-italic">Allocoleopsis franciscana</span> PCC 7113. (<b>f</b>) <span class="html-italic">Pycnacronema arboriculum</span> 41PC. (<b>g</b>) <span class="html-italic">Wilmottia murrayi</span> FBCC-A402. In the secondary structure diagram of simulated folding, the ring structure is shown in blue, the stem structure is shown in green, and the bilateral bulges are shown in yellow.</p>
Full article ">Figure 5
<p>Secondary structures of the Box-B helix in close Coleofasciculaceae species. (<b>a</b>–<b>f</b>) Box-B helices: (<b>a</b>) <span class="html-italic">Paludothrix granulosa</span> WZU 2010. (<b>b</b>) <span class="html-italic">Coleofasciculus chthonoplastes</span> PCC 7420. (<b>c</b>) <span class="html-italic">Limnofasciculus baicalensis</span> BBK-W-15. (<b>d</b>) <span class="html-italic">Allocoleopsis franciscana</span> PCC 7113. (<b>f</b>) <span class="html-italic">Pycnacronema arboriculum</span> 41PC. (<b>g</b>) <span class="html-italic">Wilmottia murrayi</span> FBCC-A402. In the secondary structure diagram of simulated folding, the ring structure is shown in blue, the stem structure is shown in green, and the bilateral bulges are shown in yellow.</p>
Full article ">Figure 6
<p>Secondary structures of the V3 helix in close Coleofasciculaceae species. (<b>a</b>–<b>f</b>) V3 helices: (<b>a</b>) <span class="html-italic">Paludothrix granulosa</span> WZU 2010. (<b>b</b>) <span class="html-italic">Coleofasciculus chthonoplastes</span> PCC 7420. (<b>c</b>) <span class="html-italic">Limnofasciculus baicalensis</span> BBK-W-15. (<b>d</b>) <span class="html-italic">Allocoleopsis franciscana</span> PCC 7113. (<b>f</b>) <span class="html-italic">Pycnacronema arboriculum</span> 41PC. (<b>g</b>) <span class="html-italic">Wilmottia murrayi</span> FBCC-A402. In the secondary structure diagram of simulated folding, the ring structure is shown in blue, the stem structure is shown in green, and the bilateral bulges are shown in yellow.</p>
Full article ">
20 pages, 4020 KiB  
Article
UAV-Multispectral Based Maize Lodging Stress Assessment with Machine and Deep Learning Methods
by Minghu Zhao, Dashuai Wang, Qing Yan, Zhuolin Li and Xiaoguang Liu
Agriculture 2025, 15(1), 36; https://doi.org/10.3390/agriculture15010036 (registering DOI) - 26 Dec 2024
Abstract
Maize lodging is a prevalent stress that can significantly diminish corn yield and quality. Unmanned aerial vehicles (UAVs) remote sensing is a practical means to quickly obtain lodging information at field scale, such as area, severity, and distribution. However, existing studies primarily use [...] Read more.
Maize lodging is a prevalent stress that can significantly diminish corn yield and quality. Unmanned aerial vehicles (UAVs) remote sensing is a practical means to quickly obtain lodging information at field scale, such as area, severity, and distribution. However, existing studies primarily use machine learning (ML) methods to qualitatively analyze maize lodging (lodging and non-lodging) or estimate the maize lodging percentage, while there is less research using deep learning (DL) to quantitatively estimate maize lodging parameters (type, severity, and direction). This study aims to introduce advanced DL algorithms into the maize lodging classification task using UAV-multispectral images and investigate the advantages of DL compared with traditional ML methods. This study collected a UAV-multispectral dataset containing non-lodging maize and lodging maize with different lodging types, severities, and directions. Additionally, 22 vegetation indices (VIs) were extracted from multispectral data, followed by spatial aggregation and image cropping. Five ML classifiers and three DL models were trained to classify the maize lodging parameters. Finally, we compared the performance of ML and DL models in evaluating maize lodging parameters. The results indicate that the Random Forest (RF) model outperforms the other four ML algorithms, achieving an overall accuracy (OA) of 89.29% and a Kappa coefficient of 0.8852. However, the maize lodging classification performance of DL models is significantly better than that of ML methods. Specifically, Swin-T performs better than ResNet-50 and ConvNeXt-T, with an OA reaching 96.02% and a Kappa coefficient of 0.9574. This can be attributed to the fact that Swin-T can more effectively extract detailed information that accurately characterizes maize lodging traits from UAV-multispectral data. This study demonstrates that combining DL with UAV-multispectral data enables a more comprehensive understanding of maize lodging type, severity, and direction, which is essential for post-disaster rescue operations and agricultural insurance claims. Full article
10 pages, 2442 KiB  
Communication
Residual Trifluorosulfonic Acid in Amino-Functionalized Covalent Triazine Frameworks for Boosting Photocatalytic Hydrogen Evolution
by Chengxiao Zhao, Zhaolin Li and Weiping Xiao
Catalysts 2025, 15(1), 12; https://doi.org/10.3390/catal15010012 (registering DOI) - 26 Dec 2024
Abstract
The utilization of covalent triazine frameworks (CTFs) as photocatalysts has witnessed rapid advancements in the field of photocatalysis. However, the presence of residual components in certain CTFs materials is widely ignored as regards their influence on photocatalytic performance. In this study, we find [...] Read more.
The utilization of covalent triazine frameworks (CTFs) as photocatalysts has witnessed rapid advancements in the field of photocatalysis. However, the presence of residual components in certain CTFs materials is widely ignored as regards their influence on photocatalytic performance. In this study, we find that trifluorosulfonic acid (TfOH) molecules stably exist in the amino-functionalized CTF-NH2 framework, which enhance the affinity for water. The experimental results indicate that the residual TfOH elevates the VB position of CTF-NH2, facilitating the oxidization of both water and sacrificial agents. Moreover, the present of TfOH accelerates the separation and transfer of photogenerated charge carriers to the Pt cocatalyst. Consequently, CTF-NH2-F containing residual TfOH molecules demonstrates a significant enhancement in the photocatalytic hydrogen evolution, achieving about 250 µmol over a duration of 3 h of illumination, which represents a 2.5-fold increase compared to that observed for CTF-NH2. This research underscores the substantial impact that residues exert on photocatalytic performance. Full article
(This article belongs to the Special Issue Recent Advances in Environment and Energy Catalysis)
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Figure 1

Figure 1
<p>(<b>a</b>) FT-IR spectra, (<b>b</b>) XPS survey spectra, (<b>c</b>) high-resolution N 1s XPS spectra and (<b>d</b>) TG spectra of CTF-NH<sub>2</sub>-10 and CTF-NH<sub>2</sub>-10-F.</p>
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<p>SEM images and water contact angles of (<b>a</b>,<b>c</b>,<b>e</b>) CTF-NH<sub>2</sub>-10-F and (<b>b</b>,<b>d</b>,<b>f</b>) CTF-NH<sub>2</sub>-10.</p>
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<p>(<b>a</b>) H<sub>2</sub>-evolving rates of CTF-NH<sub>2</sub> and CTF-NH<sub>2</sub>-F (the values along the horizontal axis represent the mole ratio between dicyanobenzene and amino monomer), (<b>b</b>) photocatalytic H<sub>2</sub> evolution of CTF-NH<sub>2</sub>-10, CTF-NH<sub>2</sub>-10-F, CTF-1 and CTF-1-F, (<b>c</b>) wavelength-dependent AQY values (at 420 nm, 450 nm, 520 nm) and (<b>d</b>) photostability test of CTF-NH<sub>2</sub>-10-F.</p>
Full article ">Figure 4
<p>(<b>a</b>) EIS Nyquist plots, (<b>b</b>) photocurrent response curves, (<b>c</b>) steady-state PL spectra, (<b>d</b>) and time-resolved PL decay spectra of CTF-NH<sub>2</sub>-10 and CTF-NH<sub>2</sub>-10-F.</p>
Full article ">Figure 5
<p>(<b>a</b>) EIS Nyquist plots, (<b>b</b>) photocurrent response curves, (<b>c</b>) steady-state PL spectra, and (<b>d</b>) time-resolved PL decay spectra of CTF-NH<sub>2</sub>-10/Pt and CTF-NH<sub>2</sub>-F-10/Pt.</p>
Full article ">Figure 6
<p>(<b>a</b>) UV–vis diffuse reflectance spectra, (<b>b</b>) Tauc plots, (<b>c</b>,<b>d</b>) Mott–Schottky plots, (<b>e</b>) XPS-valence spectra, and (<b>f</b>) band diagrams of CTF-NH<sub>2</sub>-10 and CTF-NH<sub>2</sub>-10-F.</p>
Full article ">
23 pages, 7666 KiB  
Article
The Impact of the Urban Heat Island Effect on Ground-Level Ozone Pollution in the Sichuan Basin, China
by Xingtao Song, Haoyuan Shi, Langchang Jin, Sijing Pang and Shenglan Zeng
Atmosphere 2025, 16(1), 14; https://doi.org/10.3390/atmos16010014 (registering DOI) - 26 Dec 2024
Abstract
With urbanization, ozone (O3) pollution and the urban heat island (UHI) effect have become increasingly prominent. UHI can affect O3 production and its dilution and dispersion, but the underlying mechanisms remain unclear. This study investigates the spatial and temporal distribution [...] Read more.
With urbanization, ozone (O3) pollution and the urban heat island (UHI) effect have become increasingly prominent. UHI can affect O3 production and its dilution and dispersion, but the underlying mechanisms remain unclear. This study investigates the spatial and temporal distribution of O3 pollution and the UHI effect, as well as the influence of UHI on O3 pollution in the Sichuan Basin. Atmospheric pollution data for O3 and NO2 from 2020 were obtained from local environmental monitoring stations, while temperature and single-layer wind field data were sourced from ERA5-Land, a high-resolution atmospheric reanalysis dataset provided by the European Centre for Medium-Range Weather Forecasts (ECMWF). The results indicate the following: (1) O3 concentrations in the Sichuan Basin exhibit distinct seasonal variations, with the highest levels in spring, followed by summer and autumn, and the lowest in winter. In terms of spatial variation, the overall distribution is highest in western Sichuan, second highest along the Sichuan River, and lowest in central Sichuan. (2) There are significant regional differences in UHII across Sichuan, with medium heat islands (78.63%) dominating western Sichuan, weak heat islands (82.74%) along the Sichuan River, and no heat island (34.79%) or weak heat islands (63.56%) in central Sichuan. Spatially, UHII is mainly distributed in a circular pattern. (3) Typical cities in the Sichuan Basin (Chengdu, Chongqing, Nanchong) show a positive correlation between UHII and O3 concentration (0.071–0.499), though with an observed temporal lag. This study demonstrates that UHI can influence O3 concentrations in two ways: first, by altering local heat balance, thereby promoting O3 production, and second, by generating local winds that contribute to the diffusion or accumulation of O3, forming distinct O3 concentration zones. Full article
(This article belongs to the Section Air Quality)
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Figure 1

Figure 1
<p>Administrative divisions and topographic elevation map of the Sichuan Basin.</p>
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<p>Administrative divisions and topographic elevation map of the Sichuan Basin.</p>
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<p>Day-by-day O<sub>3</sub> concentration values in the Sichuan Basin in 2020 ((<b>a</b>): Western Sichuan, (<b>b</b>): Sichuan River, (<b>c</b>): Central Sichuan).</p>
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<p>Intraday variation of O<sub>3</sub> concentration in Sichuan Basin in 2020 ((<b>a</b>): Western Sichuan, (<b>b</b>): Sichuan River, (<b>c</b>): Central Sichuan).</p>
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<p>O<sub>3</sub> concentration in the Sichuan Basin by season in 2020 ((<b>a</b>): Western Sichuan, (<b>b</b>): Sichuan River, (<b>c</b>): Central Sichuan).</p>
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<p>Distribution of O<sub>3</sub> concentration (µg/m<sup>3</sup>) in the Sichuan Basin by season in 2020 ((<b>a</b>): spring, (<b>b</b>): summer, (<b>c</b>): autumn, (<b>d</b>): winter).</p>
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<p>Change in daily average ambient air temperature in the Sichuan Basin in 2020 ((<b>a</b>): Western Sichuan, (<b>b</b>): Sichuan River, (<b>c</b>): Central Sichuan).</p>
Full article ">Figure 7
<p>Spatial distribution of seasonal changes in ambient air temperature (°C) in the Sichuan basin ((<b>a</b>): spring, (<b>b</b>): summer, (<b>c</b>): autumn, (<b>d</b>): winter).</p>
Full article ">Figure 8
<p>Daily variation of UHII in different areas of the Sichuan Basin in 2020 ((<b>a</b>): Western Sichuan, (<b>b</b>): Sichuan River, (<b>c</b>): Central Sichuan).</p>
Full article ">Figure 9
<p>Intraday variation of UHII in different areas of the Sichuan Basin in 2020 ((<b>a</b>): Western Sichuan, (<b>b</b>): Sichuan River, (<b>c</b>): Central Sichuan).</p>
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<p>Local UHII distribution (°C) by season in the Sichuan Basin in 2020 ((<b>a</b>): spring, (<b>b</b>): summer, (<b>c</b>): autumn, (<b>d</b>): winter).</p>
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<p>Daily variation of O<sub>3</sub> concentration and UHII in typical cities in the Sichuan basin ((<b>a</b>): Chengdu, (<b>b</b>): Chongqing, (<b>c</b>): Nanchong; (<b>1</b>): spring, (<b>2</b>): summer, (<b>3</b>): autumn, (<b>4</b>): winter).</p>
Full article ">Figure 12
<p>Spatial distribution of O<sub>3</sub> concentration (left) and heat island intensity (right) under the influence of the heat island effect in Nanchong city at each level ((<b>a</b>–<b>c</b>) are in order of no heat island, weak heat island, and medium heat island).</p>
Full article ">Figure 13
<p>Spatial distribution of O<sub>3</sub> concentration (left) and heat island intensity (right) under the influence of the heat island effect in Chengdu (left) and Chongqing (right) city at various levels ((<b>a</b>–<b>e</b>) are in order of no heat island, weak heat island, medium heat island, strong heat island, and very strong heat island).</p>
Full article ">Figure 14
<p>Spatial distribution of NO<sub>2</sub> concentration (left) and wind field (right) under the influence of heat island effect at each level in Chengdu (left) and Chongqing (right) city ((<b>a</b>–<b>e</b>) are in order of no heat island, weak heat island, medium heat island, and strong heat island).</p>
Full article ">Figure 15
<p>Spatial distribution of NO<sub>2</sub> concentration (left) and wind field (right) under the influence of heat island effect in Nanchong at each level ((<b>a</b>–<b>c</b>) are in order of no heat island, weak heat island, and medium heat island).</p>
Full article ">
12 pages, 4075 KiB  
Article
Dual-Band Gysel Filtering Power Divider with a Frequency Transform Resonator and Microstrip/Slotline Phase Inverter
by Yongping Xu, Chaoyi Sun, Zhe Chen, Huayan Sun, Zeyu Huang, Runfeng Tang, Jinxiao Yang and Weilin Li
Electronics 2025, 14(1), 61; https://doi.org/10.3390/electronics14010061 (registering DOI) - 26 Dec 2024
Abstract
This paper presents a novel dual-band Gysel filtering power divider (FPD) with an excellent isolation performance and a significantly wide isolation bandwidth. Although Gysel power dividers have been extensively studied in the field of radio frequency (RF), the integration of filtering functionality and [...] Read more.
This paper presents a novel dual-band Gysel filtering power divider (FPD) with an excellent isolation performance and a significantly wide isolation bandwidth. Although Gysel power dividers have been extensively studied in the field of radio frequency (RF), the integration of filtering functionality and the expansion of isolation bandwidth remain challenging. The proposed design addresses these challenges by incorporating frequency transform resonators (FTRs) and a microstrip/slotline (M/S) phase inverter into the classic Gysel topology. The FTR is directly connected to the output port to provide a dual-band response, enabling the Gysel FPD to operate without external coupling between the resonator and the port. The M/S phase inverter is a dual-layer 180 phase shifter, designed to replace the conventional 180 transmission lines loaded between the two isolation resistors of the Gysel FPD, achieving a wide isolation bandwidth. To validate the proposed design method, a dual-band Gysel FPD with center frequencies of 1.4 GHz and 1.7 GHz is designed, fabricated, and measured. The measured results show that the in-band return loss is greater than 20 dB, and the in-band insertion loss is about 0.6 dB, and the amplitude and phase imbalance characteristics are good. In addition, the 20 dB-isolation fractional bandwidth achieves 97% (0.78–2.25 GHz). The measured results show excellent agreement with the simulation results, validating the effectiveness of the proposed design methodology. Full article
(This article belongs to the Special Issue Analog/RF Circuits: Latest Advances and Prospects)
11 pages, 778 KiB  
Article
LA PULSE: Evaluating Left Atrial Function Pre- and Post-Atrial Fibrillation Ablation Using PULSEd Field Ablation
by Noha Mahrous, Florian Blaschke, Doreen Schöppenthau, Gerhard Hindricks, Leif-Hendrik Boldt and Abdul Shokor Parwani
J. Clin. Med. 2025, 14(1), 68; https://doi.org/10.3390/jcm14010068 (registering DOI) - 26 Dec 2024
Abstract
Background: Atrial fibrillation (AF) is a common cardiac arrhythmia associated with left atrial dysfunction. The impact of pulmonary vein isolation (PVI) using pulsed field ablation (PFA) on left atrial function has not been previously quantified. This study aims to evaluate the effects of [...] Read more.
Background: Atrial fibrillation (AF) is a common cardiac arrhythmia associated with left atrial dysfunction. The impact of pulmonary vein isolation (PVI) using pulsed field ablation (PFA) on left atrial function has not been previously quantified. This study aims to evaluate the effects of PVI using PFA on left atrial function in patients with AF. Methods: Thirty-four patients undergoing PVI with PFA between July 2022 and November 2023 were included. The left atrial function was assessed using echocardiography pre-procedure and at 6 months post-procedure. Results: The mean age of the patients was 66.5 ± 9.76 years, with 70.6% being male. The cohort included 44% of patients with paroxysmal AF. PVI was successfully achieved in all patients, with a significant improvement in all aspects of left atrial strain at an average of six-month follow-up. The left atrial strain reservoir (LASr) increased from 12.5 ± 5.8% to 21.7 ± 8.1% (p < 0.001). Notably, patients with paroxysmal AF exhibited a greater increase in LASr compared to those with persistent AF. Additionally, pre-procedural sinus rhythm was a significant predictor of better LASr outcomes. Conclusions: PFA is associated with significant improvement in left atrial reservoir strain, suggesting a positive impact on atrial function. These findings have important implications for the therapeutic management of AF and warrant further research. Full article
28 pages, 16945 KiB  
Review
Review on Repair Technologies for Underwater Concrete Structure Damage of Infrastructures
by Zhaogeng Wang, Jijian Lian, Hui Liu, Chao Liang, Kaifang Zou, Liang Chen, Suiling Wang, Nan Shao and Ye Yao
Water 2025, 17(1), 35; https://doi.org/10.3390/w17010035 (registering DOI) - 26 Dec 2024
Abstract
This paper comprehensively summarizes and discusses the latest research progress in the underwater concrete structure damage repair technology of infrastructures. The prompt application of underwater concrete structure repair technology can effectively deal with the damaged parts of underwater concrete structures, and it can [...] Read more.
This paper comprehensively summarizes and discusses the latest research progress in the underwater concrete structure damage repair technology of infrastructures. The prompt application of underwater concrete structure repair technology can effectively deal with the damaged parts of underwater concrete structures, and it can ensure the safe and stable operation of infrastructure and extend its service life. Firstly, this study uses bibliometric methods to analyze the characteristics of the literature on research into underwater concrete repair in the past 30 years (1993–2023), and expounds the research status and hotspots of this field. Then, we conduct a comprehensive classification and discussion of the underwater concrete structure damage repair technologies at the current stage. This technology can be divided into two major types: direct underwater type and dry environment type. Further, the development history of these technologies is systematically sorted out and, combined with practical engineering application cases, the operation processes, applicability, limitations, and economy of these technologies are analyzed. Finally, the challenges and future development trends of the current underwater concrete structure damage repair technology are pointed out, which provides a direction for future research on the intelligent maintenance of underwater concrete structures. Full article
(This article belongs to the Section Hydraulics and Hydrodynamics)
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<p>Trend of annual publication quantity from 1993 to 2023.</p>
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<p>Keyword co-occurrence analysis.</p>
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<p>Timelines for the developments of underwater repair technology.</p>
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<p>Daily rates for diving operations at different operating depths and environments.</p>
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<p>Underwater operation process of the “Yulong” submersible for the deep-water inspection of the dam [<a href="#B62-water-17-00035" class="html-bibr">62</a>,<a href="#B63-water-17-00035" class="html-bibr">63</a>,<a href="#B64-water-17-00035" class="html-bibr">64</a>].</p>
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<p>Case study of multi-tasking robot: (<b>a</b>) modular rapid-switching interface design for various end-effectors: ① lightweight underwater manipulator, ② underwater electric cutting tool, ③ underwater electric brush, ④ underwater electric drill, ⑤ underwater electric gripper. ⑥ underwater marking tool, ⑦ underwater electric glue applicator, ⑧ modular mechanical and electrical rapid-switching interfaces; (<b>b</b>) overall composition of underwater robot and the structure of tool changer system [<a href="#B58-water-17-00035" class="html-bibr">58</a>,<a href="#B83-water-17-00035" class="html-bibr">83</a>].</p>
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<p>GIRONA 500 structure diagram [<a href="#B97-water-17-00035" class="html-bibr">97</a>,<a href="#B99-water-17-00035" class="html-bibr">99</a>,<a href="#B100-water-17-00035" class="html-bibr">100</a>,<a href="#B101-water-17-00035" class="html-bibr">101</a>,<a href="#B102-water-17-00035" class="html-bibr">102</a>,<a href="#B103-water-17-00035" class="html-bibr">103</a>].</p>
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<p>Example of complete dry environmental inspection and restoration.</p>
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<p>Example of dry environment equipment operation flow chart: (<b>a</b>) the specific repair operation processes of the Pressure Caisson in Gezhouba Hydropower Station; (<b>b</b>) the specific repair operation processes of the slope corridor steel structure assembly cofferdam in China’s south-to-north water diversion project’s central route.</p>
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16 pages, 16640 KiB  
Article
Experimental Study of Steady Blowing from the Trailing Edge of an Open Cavity Flow
by Naser Al Haddabi, Konstantinos Kontis and Hossein Zare-Behtash
Aerospace 2025, 12(1), 7; https://doi.org/10.3390/aerospace12010007 (registering DOI) - 26 Dec 2024
Abstract
Cavity flows have a wide range of low-speed applications (M0.3), such as aircraft wheel wells, ground transportations, and pipelines. They induce strong flow oscillations which can substantially increase noise, drag, vibration, and lead to structural fatigue. In the current [...] Read more.
Cavity flows have a wide range of low-speed applications (M0.3), such as aircraft wheel wells, ground transportations, and pipelines. They induce strong flow oscillations which can substantially increase noise, drag, vibration, and lead to structural fatigue. In the current study, a steady jet was forced from the cavity trailing edge with different momentum fluxes (J = 0.11 kg/m·s2, 0.44 kg/m·s2, and 0.96 kg/m·s2). The aim of this study was to investigate the impact of the steady jet on the time-averaged flow field and the cavity separated shear layer oscillations for an open cavity with a length-to-depth ratio of L/D=4 at Reθ=1.28×103. Particle image velocimetry, surface oil flow visualisation, constant temperature anemometry, and pressure measurements were performed. The study found that increasing the jet momentum flux caused a significant increase in thickness and deflection of the cavity separated shear layer. Due to the counterflow interaction between the jet and cavity separated shear layer, the growth rate (dδω/dx) of the cavity separated shear layer increased significantly from 0.193 for the no-jet case to 0.273 for the J = 0.96 kg/m·s2 case. As a result, the return flow rate increased, causing the separation point on the cavity floor to shift upstream from x/L0.2 for the no-jet case to x/L0.1 for the J = 0.96 kg/m·s2 case. Furthermore, increasing the jet momentum flux increased the broadband level of the cavity separated shear layer oscillations. Full article
(This article belongs to the Special Issue Fluid Flow Mechanics (4th Edition))
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<p>Typical flow topology in a shallow open cavity.</p>
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<p>Side view drawing of the experimental model.</p>
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<p>The experimental set-up for the two-dimensional PIV.</p>
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<p>Surface oil flow visualisations for <math display="inline"><semantics> <mrow> <mi>R</mi> <msub> <mi>e</mi> <mi>θ</mi> </msub> <mo>=</mo> <mn>1.28</mn> <mo>×</mo> <msup> <mn>10</mn> <mn>3</mn> </msup> </mrow> </semantics></math> and different <span class="html-italic">J</span>’s: (<b>a</b>) no-jet, (<b>b</b>) <span class="html-italic">J</span> = 0.11 kg/m·s<sup>2</sup>, (<b>c</b>) <span class="html-italic">J</span> = 0.44 kg/m·s<sup>2</sup>, and (<b>d</b>) <span class="html-italic">J</span> = 0.96 kg/m·s<sup>2</sup>. The red Arrows indicate flow direction at cavity floor, while the hollow arrow indiates the free stream flow direction.</p>
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<p>The time-averaged <math display="inline"><semantics> <mrow> <msub> <mi>ω</mi> <mi>z</mi> </msub> <mi>L</mi> <mo>/</mo> <msub> <mi>U</mi> <mi>f</mi> </msub> </mrow> </semantics></math> and the instantaneous raw images for <math display="inline"><semantics> <mrow> <mi>R</mi> <msub> <mi>e</mi> <mi>θ</mi> </msub> <mo>=</mo> <mn>1.28</mn> <mo>×</mo> <msup> <mn>10</mn> <mn>3</mn> </msup> </mrow> </semantics></math> and different <span class="html-italic">J</span>’s.</p>
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<p>Snapshots of the instantaneous <math display="inline"><semantics> <mrow> <mi>R</mi> <mo>/</mo> <msub> <mi>U</mi> <mi>f</mi> </msub> </mrow> </semantics></math> for <math display="inline"><semantics> <mrow> <mi>R</mi> <msub> <mi>e</mi> <mi>θ</mi> </msub> <mo>=</mo> <mn>1.28</mn> <mo>×</mo> <msup> <mn>10</mn> <mn>3</mn> </msup> </mrow> </semantics></math>, <span class="html-italic">J</span> = 0.96 kg/m·s<sup>2</sup>.</p>
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<p>Contours of the time-averaged <math display="inline"><semantics> <mrow> <mi>U</mi> <mo>/</mo> <msub> <mi>U</mi> <mi>f</mi> </msub> </mrow> </semantics></math> for <math display="inline"><semantics> <mrow> <mi>R</mi> <msub> <mi>e</mi> <mi>θ</mi> </msub> <mo>=</mo> <mn>1.28</mn> <mo>×</mo> <msup> <mn>10</mn> <mn>3</mn> </msup> </mrow> </semantics></math> and different <span class="html-italic">J</span>’s.</p>
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<p>Distribution of the time-averaged <math display="inline"><semantics> <mrow> <mi>U</mi> <mo>/</mo> <msub> <mi>U</mi> <mi>f</mi> </msub> </mrow> </semantics></math> along <math display="inline"><semantics> <mrow> <mi>y</mi> <mo>/</mo> <mi>D</mi> <mo>=</mo> <mo>−</mo> <mn>0.9</mn> </mrow> </semantics></math> for <math display="inline"><semantics> <mrow> <mi>R</mi> <msub> <mi>e</mi> <mi>θ</mi> </msub> <mo>=</mo> <mn>1.28</mn> <mo>×</mo> <msup> <mn>10</mn> <mn>3</mn> </msup> </mrow> </semantics></math> and different <span class="html-italic">J</span>’s.</p>
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<p>Contours of the dimensionless Reynolds shear stress for <math display="inline"><semantics> <mrow> <mi>R</mi> <msub> <mi>e</mi> <mi>θ</mi> </msub> <mo>=</mo> <mn>1.28</mn> <mo>×</mo> <msup> <mn>10</mn> <mn>3</mn> </msup> </mrow> </semantics></math> and different <span class="html-italic">J</span>’s.</p>
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<p>Time- averaged <math display="inline"><semantics> <mrow> <mi>U</mi> <mo>/</mo> <msub> <mi>U</mi> <mi>f</mi> </msub> </mrow> </semantics></math> profiles at different axial stations for <math display="inline"><semantics> <mrow> <mi>R</mi> <msub> <mi>e</mi> <mi>θ</mi> </msub> <mo>=</mo> <mn>1.28</mn> <mo>×</mo> <msup> <mn>10</mn> <mn>3</mn> </msup> </mrow> </semantics></math> and different <span class="html-italic">J</span>’s.</p>
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<p>The time-averaged boundaries and vorticity thickness of the cavity separated shear layer along the x-axis for <math display="inline"><semantics> <mrow> <mi>R</mi> <msub> <mi>e</mi> <mi>θ</mi> </msub> <mo>=</mo> <mn>1.28</mn> <mo>×</mo> <msup> <mn>10</mn> <mn>3</mn> </msup> </mrow> </semantics></math> and different <span class="html-italic">J</span>’s.</p>
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<p>The unsteady wall pressure power spectra at <math display="inline"><semantics> <mrow> <mi>x</mi> <mo>/</mo> <mi>L</mi> <mo>=</mo> <mn>0.5</mn> </mrow> </semantics></math> for <math display="inline"><semantics> <mrow> <mi>R</mi> <msub> <mi>e</mi> <mi>θ</mi> </msub> <mo>=</mo> <mn>1.28</mn> <mo>×</mo> <msup> <mn>10</mn> <mn>3</mn> </msup> </mrow> </semantics></math> and different <span class="html-italic">J</span>’s.</p>
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<p>Snapshot of the instantiation vorticity and the fluctuating velocity streamlines. The dashed arrow indicates the free stream direction. <math display="inline"><semantics> <mrow> <mi>R</mi> <msub> <mi>e</mi> <mi>D</mi> </msub> <mo>≈</mo> <mn>50</mn> <mo>,</mo> <mn>000</mn> </mrow> </semantics></math>, sharp edge at LE, no-jet.</p>
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15 pages, 4988 KiB  
Article
Inchworm Robots Utilizing Friction Changes in Magnetorheological Elastomer Footpads Under Magnetic Field Influence
by Yun Xue and Chul-Hee Lee
Micromachines 2025, 16(1), 19; https://doi.org/10.3390/mi16010019 (registering DOI) - 26 Dec 2024
Abstract
The application of smart materials in robots has attracted considerable research attention. This study developed an inchworm robot that integrates smart materials and a bionic design, using the unique properties of magnetorheological elastomers (MREs) to improve the performance of robots in complex environments, [...] Read more.
The application of smart materials in robots has attracted considerable research attention. This study developed an inchworm robot that integrates smart materials and a bionic design, using the unique properties of magnetorheological elastomers (MREs) to improve the performance of robots in complex environments, as well as their adaptability and movement efficiency. This research stems from solving the problem of the insufficient adaptability of traditional bionic robots on different surfaces. A robot that combines an MRE foot, an electromagnetic control system, and a bionic motion mechanism was designed and manufactured. The MRE foot was made from silicone rubber mixed with carbonyl iron particles at a specific ratio. Systematic experiments were conducted on three typical surfaces, PMMA, wood, and copper plates, to test the friction characteristics and motion performance of the robot. On all tested surfaces, the friction force of the MRE foot was reduced significantly after applying a magnetic field. For example, on the PMMA surface, the friction force of the front leg dropped from 2.09 N to 1.90 N, and that of the hind leg decreased from 3.34 N to 1.75 N. The robot movement speed increased by 1.79, 1.76, and 1.13 times on PMMA, wooden, and copper plate surfaces, respectively. The MRE-based intelligent foot design improved the environmental adaptability and movement efficiency of the inchworm robot significantly, providing new ideas for the application of intelligent materials in the field of bionic robots and solutions to movement challenges in complex environments. Full article
(This article belongs to the Special Issue Magnetorheological Materials and Application Systems)
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<p>Schematic diagram of the MRE fabrication process: from mixing to molding and curing.</p>
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<p>Multi-scale microscopic observations of MRE structures (<b>i</b>) at 50× magnification, (<b>ii</b>) at 200× magnification, (<b>iii</b>) at 500× magnification, and (<b>iv</b>) at 1000× magnification.</p>
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<p>Surface topography analysis of MRE under varying magnetic field conditions. (<b>a</b>) Surface topography mapping of MRE at initial magnetic field condition. (<b>b</b>) Surface topography mapping of MRE under enhanced magnetic field intensity.</p>
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<p>Design and components of the inchworm-inspired robot with MRE footpads.</p>
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<p>Locomotion mechanism and control system of the MRE-based inchworm robot: (<b>a</b>) Illustration of the crawling sequence showing (i) anchor pull and (ii) anchor push motions. (<b>b</b>) Hierarchical control system schematic.</p>
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<p>Detailed assembly of the inchworm robot foot: (<b>a</b>) Integration of the electromagnet and the MRE footpad. (<b>b</b>) Arrangement of magnetic fillers in the magnetorheological elastomer without a magnetic field. (<b>c</b>) Arrangement of magnetic fillers in the magnetorheological elastomer with a magnetic field.</p>
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<p>Detailed assembly of the inchworm robot foot: (<b>a</b>) Integration of the electromagnet and the MRE footpad. (<b>b</b>) Arrangement of magnetic fillers in the magnetorheological elastomer without a magnetic field. (<b>c</b>) Arrangement of magnetic fillers in the magnetorheological elastomer with a magnetic field.</p>
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<p>Experimental setup for friction measurements of the MRE footpads. (<b>a</b>) Front leg measurement configuration and (<b>b</b>) rear leg testing arrangement.</p>
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<p>Velocity measurement setup for the MRE-based inchworm robot: integrated system with real-time data acquisition and control.</p>
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<p>Comparative analysis of friction force in MRE footpads with and without a magnetic field. (<b>a</b>) Front leg on PMMA surface; (<b>b</b>) hind leg on PMMA surface; (<b>c</b>) front leg on copper plate surface; (<b>d</b>) hind leg on copper plate surface; (<b>e</b>) front leg on wooden surface; (<b>f</b>) hind leg on wooden surface.</p>
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<p>Locomotion performance of an MRE-based inchworm robot on various surfaces: (<b>a</b>) baseline translation dynamics without field activation and (<b>b</b>) enhanced locomotion performance under an applied field stimulus.</p>
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<p>Comparative analysis of MRE-based inchworm robot average speeds on various surfaces.</p>
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16 pages, 10249 KiB  
Article
Early Vegetation Recovery After the 2008–2009 Explosive Eruption of the Chaitén Volcano, Chile
by Ricardo Moreno-Gonzalez, Iván A. Díaz, Duncan A. Christie and Antonio Lara
Diversity 2025, 17(1), 14; https://doi.org/10.3390/d17010014 (registering DOI) - 26 Dec 2024
Abstract
In May 2008, Chaitén volcano entered an eruptive process, leading to one of the world’s largest eruptions in recent decades. The magnitude of tephra ejected by the eruption left different types of disturbances and caused diverse forms of environmental damage that were heterogeneously [...] Read more.
In May 2008, Chaitén volcano entered an eruptive process, leading to one of the world’s largest eruptions in recent decades. The magnitude of tephra ejected by the eruption left different types of disturbances and caused diverse forms of environmental damage that were heterogeneously distributed across the surrounding area. We went to the field to assess the early vegetation responses a year after the eruption in September 2009. We evaluated the lateral-blast disturbance zone. We distributed a set of plots in three disturbed sites and one in an undisturbed site. In each of these sites, in a rectangular plot of 1000 m2, we marked all standing trees, recording whether they were alive, resprouting, or dead. Additionally, in each site of 80 small plots (~4 m2), we tallied the regenerated plants, their coverage, and the log volume. We described whether the plant regeneration was occurring on a mineral or organic substrate (i.e., ash or leaf litter, respectively). In the blast zone, the eruption created a gradient of disturbance. Close to the crater, we found high levels of devastation marked by no surviving species, scarcely standing-dead trees and logs, and no tree regeneration. At the other extreme end of the disturbance zone, the trees with damaged crowns were resprouting, small plants were regrowing, and seedlings were more dispersed. The main form of regeneration was the resprouting of trunks or buried roots; additionally, a few seedlings were observed in the small plots and elsewhere in disturbed areas. The results suggest that the early stages of succession are shaped by life history traits like dispersion syndrome and regeneration strategy (i.e., vegetative), as was found after other volcanic eruptions. Likewise, the distribution of biological legacies, which is related to disturbance intensity, can cause certain species traits to thrive. For instance, in the blow-down zone, surviving species were chiefly those dispersed by the wind, while in the standing-dead zone, survivors were those dispersed by frugivorous birds. Additionally, we suggest that disturbance intensity variations are related to the elevation gradient. The varying intensities of disturbance further contribute to these ecological dynamics. The early succession in the blast zone of Chaitén volcano is influenced by the interaction between species-specific life history, altitudinal gradient, and biological legacies. Further studies are required to observe the current successional patterns that occur directly in the blast zone and compare these results with those obtained following other volcanic disturbances. Full article
(This article belongs to the Special Issue Plant Succession and Vegetation Dynamics)
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<p>Map of the study site. (<b>Left panel</b>) indicates the position of Chaiten Volcano (red triangle) in relation to the main cities (black dots). (<b>Right panel</b>) shows a close-up of the volcano’s blast zone, the plots’ distribution along the disturbance/elevation gradient (total-destruction plot, blow-down plot, and standing-dead plot), and the undisturbed sector (old-growth plot).</p>
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<p>Photographic records of the study site. (<b>A</b>) showing impressive impacts close to the crater. Comparison of the volcanic dome and vegetation cover before (<b>B</b>) and during the 2008–2009 eruption (<b>C</b>). Red dot indicates the approximate position of the researcher (Dr. Díaz) in panel (<b>A</b>). Images (<b>D</b>–<b>G</b>) represent a disturbance condition where plots were established: (<b>D</b>) Total-destruction, (<b>E</b>) blow-down, (<b>F</b>) standing-dead, and (<b>G</b>) old-growth plots.</p>
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<p>Rarefaction analysis shows the relationship between the number of tree seedling species (<b>A</b>) and small vascular plant species (<b>B</b>) as a function of the number of individuals. In both panels, the shaded area indicates one standard error. All sites affected by the eruption of Chaitén old-growth, standing-dead, and blow-down plots are compared, except for the total-destruction plot, which was not included because of the absence of plants.</p>
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<p>Diameter at the breast height (dbh) distribution for living and standing-dead trees in the study sites. Each panel represents a plot condition influenced by the eruption of Chaitén Volcano.</p>
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<p>Volume of fallen dead trees (logs) in the study sites influenced by the eruption of Chaitén Volcano in the study sites.</p>
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<p>Number of individuals or colonies per relative coverage range at the ground level of the study areas affected by Chaitén Volcano, including vascular and non-vascular species. Panels correspond to the plots distributed in the different disturbance zones.</p>
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12 pages, 4365 KiB  
Article
Modulating Perception in Interior Architecture Through Décor: An Eye-Tracking Study of a Living Room Scene
by Weronika Wlazły and Agata Bonenberg
Buildings 2025, 15(1), 48; https://doi.org/10.3390/buildings15010048 (registering DOI) - 26 Dec 2024
Abstract
The visual perception of interior architecture plays a crucial role in real estate marketing, influencing the decisions of buyers, interior architects, and real estate agents. These professionals rely on personal assessments of space, often drawing from their experience of using décor to influence [...] Read more.
The visual perception of interior architecture plays a crucial role in real estate marketing, influencing the decisions of buyers, interior architects, and real estate agents. These professionals rely on personal assessments of space, often drawing from their experience of using décor to influence how interiors are perceived. While intuition may validate some approaches, this study explores an under-examined aspect of interior design using a mobile eye-tracking device. It investigates how decorative elements affect spatial perception and offers insights into how individuals visually engage with interior environments. By integrating décor into the analysis of interior architecture, this study broadens the traditional scope of the field, demonstrating how décor composition can modulate spatial perception using eye-tracking technology. Results show that effective styling can redirect attention from key architectural elements, sometimes causing them to be overlooked during the critical first moments of observation commonly known as the “first impression”. These findings have important implications for interior design practice and architectural education. Full article
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<p>Keywords map, created in VOSViewer. The set of 392 connected items. Source: W. Wlazly.</p>
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<p>Keywords map, zoomed to keyword “interior design”, presenting 43 links, created in VOSViewer. Source: W. Wlazly.</p>
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<p>Study conditions. (by Authors).</p>
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<p>Scene 1. Basic living room scene (control trial). Aggregated Heat Map for 18 participants. Source: Authors.</p>
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<p>Scene 2. Styled living room scene. Aggregated Heat Map for 18 participants. Source: Authors.</p>
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<p>Scene 3. Styled living room scene. Aggregated Heat Map for 18 participants. Source: Authors.</p>
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<p>Scene 1—Areas of Interest: furniture with no décor. Control trial. Source: Authors.</p>
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<p>Scene 2—Areas of Interest: furniture with décor, version 1, subdued colors. Source: Authors.</p>
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<p>Scene 3—Areas of Interest: furniture with décor, version 2, expressive colors. Source: Authors.</p>
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18 pages, 2505 KiB  
Review
From Species to Varieties: How Modern Sequencing Technologies Are Shaping Medicinal Plant Identification
by Mingcheng Wang, Haifeng Lin, Hongqiang Lin, Panyue Du and Shuqiao Zhang
Genes 2025, 16(1), 16; https://doi.org/10.3390/genes16010016 (registering DOI) - 26 Dec 2024
Abstract
Background/Objectives: Modern sequencing technologies have transformed the identification of medicinal plant species and varieties, overcoming the limitations of traditional morphological and chemical approaches. This review explores the key DNA-based techniques, including molecular markers, DNA barcoding, and high-throughput sequencing, and their contributions to enhancing [...] Read more.
Background/Objectives: Modern sequencing technologies have transformed the identification of medicinal plant species and varieties, overcoming the limitations of traditional morphological and chemical approaches. This review explores the key DNA-based techniques, including molecular markers, DNA barcoding, and high-throughput sequencing, and their contributions to enhancing the accuracy and reliability of plant identification. Additionally, the integration of multi-omics approaches is examined to provide a comprehensive understanding of medicinal plant identity. Methods: The literature search for this review was conducted across databases such as Google Scholar, Web of Science, and PubMed, using keywords related to plant taxonomy, genomics, and biotechnology. Inclusion criteria focused on peer-reviewed studies closely related to plant identification methods and techniques that contribute significantly to the field. Results: The review highlights that while sequencing technologies offer substantial improvements, challenges such as high costs, technical expertise, and the lack of standardized protocols remain barriers to widespread adoption. Potential solutions, including AI-driven data analysis and portable sequencers, are discussed. Conclusions: This review provides a comprehensive overview of molecular techniques, their transformative impact, and future perspectives for more accurate and efficient medicinal plant identification. Full article
(This article belongs to the Special Issue Advances in Genetics and Genomics of Plants: 2nd Edition)
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<p>Overview of traditional and modern techniques for medicinal plant identification.</p>
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<p>Commonly used DNA-based identification pipeline for medicinal plants.</p>
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<p>Integration of multi-omics approaches for comprehensive identification of medicinal plants.</p>
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29 pages, 7351 KiB  
Article
Two-Step Deep Learning Approach for Estimating Vegetation Backscatter: A Case Study of Soybean Fields
by Dong Zhu, Peng Zhao, Qiang Zhao, Qingliang Li, Jinpeng Zhang and Lixia Yang
Remote Sens. 2025, 17(1), 41; https://doi.org/10.3390/rs17010041 (registering DOI) - 26 Dec 2024
Abstract
Precisely predicting vegetation backscatter involves various challenges, such as complex vegetation structure, soil–vegetation interaction, and data availability. Deep learning (DL) works as a powerful tool to analyze complex data and approximate the nonlinear relationship between variables, thus exhibiting potential applications in microwave scattering [...] Read more.
Precisely predicting vegetation backscatter involves various challenges, such as complex vegetation structure, soil–vegetation interaction, and data availability. Deep learning (DL) works as a powerful tool to analyze complex data and approximate the nonlinear relationship between variables, thus exhibiting potential applications in microwave scattering problems. However, few DL-based approaches have been developed to reproduce vegetation backscatters owing to the lack of acquiring a large amount of training data. Motivated by a relatively accurate single-scattering radiative transfer model (SS-RTM) and radar measurements, we, for the first time to our knowledge, introduce a transfer learning (TL)-based approach to estimate the radar backscatter of vegetation canopy in the case of soybean fields. The proposed approach consists of two steps. In the first step, a simulated dataset was generated by the SS-RTM. Then, we pre-trained two baseline networks, namely, a deep neural network (DNN) and long short-term memory network (LSTM), using the simulated dataset. In the second step, limited measured data were utilized to fine-tune the previously pre-trained networks on the basis of TL strategy. Extensive experiments, conducted on both simulated data and in situ measurements, revealed that the proposed two-step TL-based approach yields a significantly better and more robust performance than SS-RTM and other DL schemes, indicating the feasibility of such an approach in estimating vegetation backscatters. All these outcomes provide a new path for addressing complex microwave scattering problems. Full article
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<p>Photograph of the (<b>a</b>) truck-mounted scatterometer system; (<b>b</b>) test site on 9/30.</p>
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<p>Vegetation parameters for CRIRP 2018, Yueh 1992 [<a href="#B49-remotesensing-17-00041" class="html-bibr">49</a>], and Wigneron 1999 [<a href="#B50-remotesensing-17-00041" class="html-bibr">50</a>].</p>
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<p>Variation in C-band radar data with (<b>a</b>) incidence angles and (<b>b</b>) vegetation parameters.</p>
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<p>The designed architecture of the proposed two-step TL-based approach for estimating vegetation backscatters.</p>
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<p>Comparison between the values of backscattering coefficients simulated by the SS-RTM and the radar data for (<b>a</b>) 9/11, (<b>b</b>) 9/30 of S-band.</p>
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<p>Comparison between the values of backscattering coefficients simulated by the SS-RTM and the radar data for (<b>a</b>) 8/14, (<b>b</b>) 9/12 of C-band.</p>
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<p>Schematic diagram of (<b>a</b>) a DNN, (<b>b</b>) a neuron.</p>
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<p>Schematic diagram of LSTM.</p>
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<p>Correlation plot between predictions and validation data for S-band: (<b>a</b>) SVM; (<b>b</b>) linear; (<b>c</b>) PT-DNN; (<b>d</b>) PT-LSTM.</p>
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<p>Correlation plot between predictions and validation data for S-band: (<b>a</b>) SVM; (<b>b</b>) linear; (<b>c</b>) PT-DNN; (<b>d</b>) PT-LSTM.</p>
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<p>Correlation plot between predictions and validation data for C-band: (<b>a</b>) SVM; (<b>b</b>) linear; (<b>c</b>) PT-DNN; (<b>d</b>) PT-LSTM.</p>
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<p>Box plot of the estimated differences between model predictions and simulated data.</p>
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<p>Validation loss on the radar data for (<b>a</b>) S-band and (<b>b</b>) C-band.</p>
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<p>Correlation of the backscattering coefficients between the measured data and other methods for (<b>a</b>) SVM; (<b>b</b>) Linear; (<b>c</b>) PT-DNN; (<b>d</b>) FT-DNN; (<b>e</b>) PT-LSTM; and (<b>f</b>) FT-LSTM.</p>
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<p>Comparison of backscattering coefficients among the measured data and SS-RTM simulations, PT-LSTM, and FT-LSTM for (<b>a</b>) S-band, (9/13, CRIRP 2018) and (<b>b</b>) C-band, (9/03, Yueh 1992).</p>
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<p>Comparison of the backscattering coefficients between SS-RTM and WCM.</p>
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<p>Comparison for S-band data (9/12, CRIRP 2018).</p>
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21 pages, 16438 KiB  
Article
Characterizing Changes in Geometry and Flow Speeds of Land- and Lake-Terminating Glaciers at the Headwaters of Yarlung Zangbo River, Western Himalayas
by Min Zhou, Yuzhe Wang, Tong Zhang, Weijun Sun and Yetang Wang
Remote Sens. 2025, 17(1), 40; https://doi.org/10.3390/rs17010040 (registering DOI) - 26 Dec 2024
Abstract
The glaciers of the Himalayas are essential for water resources in South Asia and the Qinghai–Tibet Plateau, but they are undergoing accelerated mass loss, posing risks to water security and increasing glacial hazards. This study examines long-term changes in the geometry and flow [...] Read more.
The glaciers of the Himalayas are essential for water resources in South Asia and the Qinghai–Tibet Plateau, but they are undergoing accelerated mass loss, posing risks to water security and increasing glacial hazards. This study examines long-term changes in the geometry and flow speeds of both land- and lake-terminating glaciers at the headwaters of the Yarlung Zangbo River, using field measurements, remote sensing, and numerical ice flow modeling. We observed significant heterogeneity in glacier behaviors across the region, with notable differences between glacier terminus types and even among neighboring glaciers of the same type. Between 1974 and 2020, glacier thinning and mass loss rates doubled in the early 21st century (0.57±0.05 m w.e. a−1) compared to 1974–2000 (0.24±0.11 m w.e. a−1). While lake-terminating glaciers generally experienced more rapid retreat and mass loss, the land-terminating N241 Glacier displayed comparable mass loss rates. Lake-terminating glaciers retreated by over 1000 m between 1990 and 2019, while land-terminating glaciers retreated by less than 750 m. The ITS_LIVE velocity dataset showed higher and more variable flow speeds in lake-terminating glaciers. Numerical modeling from 2000 to 2017 revealed divergent changes in flow regimes, with lake-terminating glaciers generally experiencing acceleration, while land-terminating glaciers showed either a slowing down or stable flow behavior. Our findings underscore the significant role of lake-terminating glaciers in contributing to ice mass loss, emphasizing the need for advanced glacier models that incorporate dynamic processes such as frontal calving and longitudinal coupling. Full article
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Graphical abstract

Graphical abstract
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<p>Overview of the study area. Glacier outlines from the CGI2 are shown in blue. Stakes are marked with yellow circles, and representative glaciers are labeled in red. The background image is a Landsat 8 scene. The inset map indicates the location of the study area within the HMA region.</p>
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<p>Comparison between ITS_LIVE velocities and measured velocities at the stakes (<b>a</b>) and along the glacier centerline (<b>b</b>). Stakes A and B are indicated by triangle and square.</p>
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<p>Comparison of region geodetic mass balances between 1974–2000 and 2000–2020. (<b>a</b>) Regional geodetic mass balances for individual glaciers during the period 1974–2000. (<b>b</b>) Regional geodetic mass balances for individual glaciers during the period 2000–2020. Note that panels (<b>a</b>,<b>b</b>) share the same colorbar scale. (<b>c</b>) Altitudinal distributions of geodetic mass balances separated into 50 m elevation bins during the two intervals. Shaded areas indicate the standard error of the mean.</p>
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<p>Comparison of geodetic mass balances along the centerlines of four glaciers for the periods 1974–2000 (black), 2000–2010 (cyan), and 2010–2020 (red). (<b>a</b>) JMYZ Glacier. (<b>b</b>) ASJG Glacier. (<b>c</b>) N241 Glacier. (<b>d</b>) N171 Glacier.</p>
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<p>Region-wide glacier velocity maps for the periods 1990–1999 (<b>a</b>), 2000–2009 (<b>b</b>), and 2010–2018 (<b>c</b>).</p>
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<p>Comparison of surface velocities along the centerlines of four glaciers for the periods 1990–1999 (black), 2000–2009 (cyan), and 2010–2018 (red). (<b>a</b>) JMYZ Glacier. (<b>b</b>) ASJG Glacier. (<b>c</b>) N241 Glacier. (<b>d</b>) N171 Glacier. The shaded areas indicate the standard deviations.</p>
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<p>Temporal changes in glacier termini from 1990 to 2019 for four glaciers. (<b>a</b>) JMYZ Glacier, (<b>b</b>) ASJG Glacier, (<b>c</b>) N241 Glacier, (<b>d</b>) N171 Glacier. The background in each panel is a Landsat 8 image.</p>
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<p>Comparison of temporal variations in flow regimes for lake-terminating glaciers in 2000 and 2017. (<b>a</b>,<b>c</b>) JMYZ Glacier. (<b>b</b>,<b>d</b>) ASJG Glacier.</p>
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<p>Comparison of temporal variations in flow regimes for land-terminating glaciers in 2000 and 2017. (<b>a</b>,<b>c</b>) N241 Glacier. (<b>b</b>,<b>d</b>) N171 Glacier.</p>
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<p>Modeled surface and basal velocities for four glaciers. (<b>a</b>) JMYZ Glacier. (<b>b</b>) ASJG Glacier. (<b>c</b>) N241 Glacier. (<b>d</b>) N171 Glacier. Black and blue lines indicate the velocities in 2000 and 2017, respectively. Solid and dot-dashed lines indicate the surface and basal velocities, respectively.</p>
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<p>Modeled driving stresses for four glaciers. (<b>a</b>) JMYZ Glacier. (<b>b</b>) ASJG Glacier. (<b>c</b>) N241 Glacier. (<b>d</b>) N171 Glacier. Black and blue lines indicate the the results in 2000 and 2017, respectively.</p>
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<p>Modeled basal shear stresses for four glaciers. (<b>a</b>) JMYZ Glacier. (<b>b</b>) ASJG Glacier. (<b>c</b>) N241 Glacier. (<b>d</b>) N171 Glacier. Black and blue lines indicate the the results in 2000 and 2017, respectively. Note that the <span class="html-italic">y</span>-axis is on a logarithmic scale, representing <math display="inline"><semantics> <mrow> <mo form="prefix">log</mo> <mo>(</mo> <msub> <mi>τ</mi> <mi>b</mi> </msub> <mo>)</mo> </mrow> </semantics></math>.</p>
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22 pages, 9786 KiB  
Article
Determination of Sequential Well Placements Using a Multi-Modal Convolutional Neural Network Integrated with Evolutionary Optimization
by Seoyoon Kwon, Minsoo Ji, Min Kim, Juliana Y. Leung and Baehyun Min
Mathematics 2025, 13(1), 36; https://doi.org/10.3390/math13010036 (registering DOI) - 26 Dec 2024
Abstract
In geoenergy science and engineering, well placement optimization is the process of determining optimal well locations and configurations to maximize economic value while considering geological, engineering, economic, and environmental constraints. This complex multi-million-dollar problem involves optimizing multiple parameters using computationally intensive reservoir simulations, [...] Read more.
In geoenergy science and engineering, well placement optimization is the process of determining optimal well locations and configurations to maximize economic value while considering geological, engineering, economic, and environmental constraints. This complex multi-million-dollar problem involves optimizing multiple parameters using computationally intensive reservoir simulations, often employing advanced algorithms such as optimization algorithms and machine/deep learning techniques to find near-optimal solutions efficiently while accounting for uncertainties and risks. This study proposes a hybrid workflow for determining the locations of production wells during primary oil recovery using a multi-modal convolutional neural network (M-CNN) integrated with an evolutionary optimization algorithm. The particle swarm optimization algorithm provides the M-CNN with full-physics reservoir simulation results as learning data correlating an arbitrary well location and its cumulative oil production. The M-CNN learns the correlation between near-wellbore spatial properties (e.g., porosity, permeability, pressure, and saturation) and cumulative oil production as inputs and output, respectively. The learned M-CNN predicts oil productivity at every candidate well location and selects qualified well placement scenarios. The prediction performance of the M-CNN for hydrocarbon-prolific regions is improved by adding qualified scenarios to the learning data and re-training the M-CNN. This iterative learning scheme enhances the suitability of the proxy for solving the problem of maximizing oil productivity. The validity of the proxy is tested with a benchmark model, UNISIM-I-D, in which four oil production wells are sequentially drilled. The M-CNN approach demonstrates remarkable consistency and alignment with full-physics reservoir simulation results. It achieves prediction accuracy within a 3% relative error margin, while significantly reducing computational costs to just 11.18% of those associated with full-physics reservoir simulations. Moreover, the M-CNN-optimized well placement strategy yields a substantial 47.40% improvement in field cumulative oil production compared to the original configuration. These findings underscore the M-CNN’s effectiveness in sequential well placement optimization, striking an optimal balance between predictive accuracy and computational efficiency. The method’s ability to dramatically reduce processing time while maintaining high accuracy makes it a valuable tool for enhancing oil field productivity and streamlining reservoir management decisions. Full article
(This article belongs to the Special Issue Evolutionary Multi-Criteria Optimization: Methods and Applications)
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Figure 1

Figure 1
<p>The flowchart of the proposed hybrid proxy to solve a sequential well placement problem. The optimum well locations are determined using the multi-modal convolutional neural network (M-CNN) incorporated with particle swarm optimization (PSO) and iterative learning.</p>
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<p>Schematic diagram of the PSO and M-CNN. (<b>a</b>) The PSO evolves solutions that are utilized as learning data of the M-CNN; (<b>b</b>) The M-CNN learns a pattern between inputs (i.e., petrophysical properties) and outputs (i.e., field cumulative oil production) extracted from the PSO solutions (modified from Chu et al. [<a href="#B29-mathematics-13-00036" class="html-bibr">29</a>]).</p>
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<p>Three-dimensional distributions of petrophysical properties of the UNISIM-I-D. (<b>a</b>) Porosity; (<b>b</b>) permeability I; (<b>c</b>) pressure; (<b>d</b>) oil saturation. The total number of grid blocks is 93,960, with 36,403 of those being active.</p>
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<p>Two-dimensional porosity distribution maps of the UNISIM-I-D. (<b>a</b>) The 1st layer (2282 active grid blocks); (<b>b</b>) 10th layer (2312 active grid blocks); (<b>c</b>) 20th layer (65 active grid blocks).</p>
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<p>Two-dimensional permeability distribution maps of the UNISIM-I-D. (<b>a</b>) The 1st layer (2282 active grid blocks); (<b>b</b>) 10th layer (2312 active grid blocks); (<b>c</b>) 20th layer (65 active grid blocks).</p>
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<p>Two-dimensional pressure distribution maps of the UNISIM-I-D. (<b>a</b>) The 1st layer (2282 active grid blocks); (<b>b</b>) 10th layer (2312 active grid blocks); (<b>c</b>) 20th layer (65 active grid blocks).</p>
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<p>Two-dimensional oil saturation distribution maps of the UNISIM-I-D. (<b>a</b>) The 1st layer (2282 active grid blocks); (<b>b</b>) 10th layer (2312 active grid blocks); (<b>c</b>) 20th layer (65 active grid blocks).</p>
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<p>The box plots to show the evolution of well placement scenarios for the 1st well through PSO. Note that this study acquired the learning data for M-CNN through PSO. The PSO process initially improved solution quality, with increasing highest values and decreasing dispersion, but stagnated after the 10th epoch when (near-)optimal solutions were identified, concluding with 280 reservoir simulation results after 14 epochs. Small circles indicate outliers of the box plots.</p>
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<p>Scatter plots to compare the reference and predicted production for test data scenarios and top ten qualified scenarios for the 1st well placement problem. (<b>a</b>) Basecase (<math display="inline"><semantics> <mrow> <msup> <mrow> <mi>R</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msup> <mo>=</mo> <mn>0.87</mn> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>ε</mi> </mrow> <mrow> <mi>a</mi> <mi>v</mi> <mi>g</mi> </mrow> </msub> <mo>=</mo> <mn>13.34</mn> <mi mathvariant="normal">%</mi> </mrow> </semantics></math>); (<b>b</b>) 1st iterative learning (<math display="inline"><semantics> <mrow> <msup> <mrow> <mi>R</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msup> <mo>=</mo> <mn>0.77</mn> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>ε</mi> </mrow> <mrow> <mi>a</mi> <mi>v</mi> <mi>g</mi> </mrow> </msub> <mo>=</mo> <mn>7.13</mn> <mi mathvariant="normal">%</mi> </mrow> </semantics></math>); (<b>c</b>) 2nd iterative learning (<math display="inline"><semantics> <mrow> <msup> <mrow> <mi>R</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msup> <mo>=</mo> <mn>0.84</mn> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>ε</mi> </mrow> <mrow> <mi>a</mi> <mi>v</mi> <mi>g</mi> </mrow> </msub> <mo>=</mo> <mn>2.64</mn> <mi mathvariant="normal">%</mi> </mrow> </semantics></math>).</p>
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<p>Scatter plots to compare reference and predicted production for test data scenarios and top ten qualified scenarios for the 2nd well placement problem. (<b>a</b>) Basecase (<math display="inline"><semantics> <mrow> <msup> <mrow> <mi>R</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msup> <mo>=</mo> <mn>0.93</mn> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>ε</mi> </mrow> <mrow> <mi>a</mi> <mi>v</mi> <mi>g</mi> </mrow> </msub> <mo>=</mo> <mn>5.31</mn> <mi mathvariant="normal">%</mi> </mrow> </semantics></math>); (<b>b</b>) 1st iterative learning (<math display="inline"><semantics> <mrow> <msup> <mrow> <mi>R</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msup> <mo>=</mo> <mn>0.90</mn> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>ε</mi> </mrow> <mrow> <mi>a</mi> <mi>v</mi> <mi>g</mi> </mrow> </msub> <mo>=</mo> <mn>1.66</mn> <mi mathvariant="normal">%</mi> </mrow> </semantics></math>).</p>
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<p>Scatter plots to compare reference and predicted production for test data scenarios and top ten qualified scenarios for the 3rd well placement problem. (<b>a</b>) Basecase (<math display="inline"><semantics> <mrow> <msup> <mrow> <mi>R</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msup> <mo>=</mo> <mn>0.87</mn> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>ε</mi> </mrow> <mrow> <mi>a</mi> <mi>v</mi> <mi>g</mi> </mrow> </msub> <mo>=</mo> <mn>21.53</mn> <mi mathvariant="normal">%</mi> </mrow> </semantics></math>); (<b>b</b>) 1st iterative learning (<math display="inline"><semantics> <mrow> <msup> <mrow> <mi>R</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msup> <mo>=</mo> <mn>0.94</mn> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>ε</mi> </mrow> <mrow> <mi>a</mi> <mi>v</mi> <mi>g</mi> </mrow> </msub> <mo>=</mo> <mn>0.68</mn> <mi mathvariant="normal">%</mi> </mrow> </semantics></math>).</p>
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<p>Scatter plots to compare reference and predicted production for test data scenarios and top ten qualified scenarios for the basecase of the 4th well placement problem (<math display="inline"><semantics> <mrow> <msup> <mrow> <mi>R</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msup> <mo>=</mo> <mn>0.86</mn> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>ε</mi> </mrow> <mrow> <mi>a</mi> <mi>v</mi> <mi>g</mi> </mrow> </msub> <mo>=</mo> <mn>2.23</mn> <mi mathvariant="normal">%</mi> </mrow> </semantics></math>).</p>
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<p>Oil productivity and relative error (<math display="inline"><semantics> <mrow> <mi>ε</mi> </mrow> </semantics></math>) maps obtained using M-CNN and reservoir simulation (RS). (<b>a</b>) <math display="inline"><semantics> <mrow> <msubsup> <mrow> <mi>Q</mi> </mrow> <mrow> <mi>o</mi> </mrow> <mrow> <mi>N</mi> <mi>N</mi> </mrow> </msubsup> </mrow> </semantics></math> (1st well); (<b>b</b>) <math display="inline"><semantics> <mrow> <msubsup> <mrow> <mi>Q</mi> </mrow> <mrow> <mi>o</mi> </mrow> <mrow> <mi>R</mi> <mi>S</mi> </mrow> </msubsup> </mrow> </semantics></math> (1st well); (<b>c</b>) <math display="inline"><semantics> <mrow> <mi>ε</mi> </mrow> </semantics></math> (1st well); (<b>d</b>) <math display="inline"><semantics> <mrow> <msubsup> <mrow> <mi>Q</mi> </mrow> <mrow> <mi>o</mi> </mrow> <mrow> <mi>N</mi> <mi>N</mi> </mrow> </msubsup> </mrow> </semantics></math> (2nd well); (<b>e</b>) <math display="inline"><semantics> <mrow> <msubsup> <mrow> <mi>Q</mi> </mrow> <mrow> <mi>o</mi> </mrow> <mrow> <mi>R</mi> <mi>S</mi> </mrow> </msubsup> </mrow> </semantics></math> (2nd well); (<b>f</b>) <math display="inline"><semantics> <mrow> <mi>ε</mi> </mrow> </semantics></math> (2nd well); (<b>g</b>) <math display="inline"><semantics> <mrow> <msubsup> <mrow> <mi>Q</mi> </mrow> <mrow> <mi>o</mi> </mrow> <mrow> <mi>N</mi> <mi>N</mi> </mrow> </msubsup> </mrow> </semantics></math> (3rd well); (<b>h</b>) <math display="inline"><semantics> <mrow> <msubsup> <mrow> <mi>Q</mi> </mrow> <mrow> <mi>o</mi> </mrow> <mrow> <mi>R</mi> <mi>S</mi> </mrow> </msubsup> </mrow> </semantics></math> (3rd well); (<b>i</b>) <math display="inline"><semantics> <mrow> <mi>ε</mi> </mrow> </semantics></math> (3rd well); (<b>j</b>) <math display="inline"><semantics> <mrow> <msubsup> <mrow> <mi>Q</mi> </mrow> <mrow> <mi>o</mi> </mrow> <mrow> <mi>N</mi> <mi>N</mi> </mrow> </msubsup> </mrow> </semantics></math> (4th well); (<b>k</b>) <math display="inline"><semantics> <mrow> <msubsup> <mrow> <mi>Q</mi> </mrow> <mrow> <mi>o</mi> </mrow> <mrow> <mi>R</mi> <mi>S</mi> </mrow> </msubsup> </mrow> </semantics></math> (4th well); (<b>l</b>) <math display="inline"><semantics> <mrow> <mi>ε</mi> </mrow> </semantics></math> (4th well).</p>
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<p>Well production profiles at the selected four well locations based on the M-CNN results. (<b>a</b>) Oil production; (<b>b</b>) water cut; (<b>c</b>) bottom-hole pressure.</p>
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<p>Well production profiles at the selected four well locations based on the PSO with early stopping (ES) results. (<b>a</b>) Oil production; (<b>b</b>) water cut; (<b>c</b>) bottom-hole pressure.</p>
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<p>Well production profiles at the four original well locations in the original study from the original study [<a href="#B38-mathematics-13-00036" class="html-bibr">38</a>]. (<b>a</b>) Oil production; (<b>b</b>) water cut; (<b>c</b>) bottom-hole pressure.</p>
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