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No Small Observer Can Verify a Black Hole Firewall
Michael Timothy Bennett
Posted: 04 March 2026
Development Of A Comprehensive Method For Diagnosing Electrical Machines Based On Artificial Neural Networks
Jasurbek Nizamov
,Sultanbek Issenov
,Zailobiddin Boihanov
,Dainius Steponavičius
,Felix Bulatbayev
,Gulim Nurmaganbetova
Posted: 04 March 2026
The Role of Spiritual and Religious Practices, Pet Ownership, and Contemplative Practices in Successful Aging: A Literature Review
Deborah Tessitore McManus
Posted: 04 March 2026
Characterization of Extracellular Vesicle-Enriched Populations in B-Cell Acute Lymphoblastic Leukemia from Peripheral Blood
Miguel Angel Carmona-Zamudio
,Francisco Sierra-López
,Carlos Emilio Miguel-Rodríguez
,Maricarmen Hernández-Rodríguez
,Gustavo Acosta-Altamirano
,Mónica Sierra-Martínez
Posted: 04 March 2026
Streaming Transformer Networks: Unified Hearing-to-Speech Recognition and Intelligent Text Generation Systems
P. Selvaprasanth
Posted: 04 March 2026
Dynamics of Corruption as a Social Pathogen: A Two-Patch Resource-Competition Model with Endogenous Enforcement and Migration
Abadi Abraha Asgedom
,Yohannes Yirga Kefela
,Hailu Tkue Welu
Posted: 04 March 2026
Spatial and Socioeconomic Feedbacks Driving Rice Farmers’ Marginalization in Peri-Urban Landscapes: Evidence from Bandung Regency, Indonesia
Adzani Ameridyani
,Izuru Saizen
Posted: 04 March 2026
Growth of Supermassive Black Holes in a Decaying Vacuum
Yuanxin Li
Posted: 04 March 2026
Explainable Machine Learning Reveals Persistent Carbon Sink in Xishuangbanna Tropical Forests Under Future Climate Scenarios
Chenjia Zhang
,Dingman Li
,Luping Zhang
,Yuxuan Zhu
,Zhengquan Zhou
,Daokun Ma
,Yan Zhang
,Feiri Ali
,Yusheng Han
Posted: 04 March 2026
Toward Human-Robot Sharing Space: A Conceptual Framework and Scoping Review of Spatial Design Knowledge
Zhenyu Li
,Mengying Tang
,Qiuchi Mao
,Mengxun Liu
Posted: 04 March 2026
Quantum-Inspired and Non-Classical Approaches to Consciousness: Models, Evidence and Constraints
Oscar Arias-Carrión
,Emmanuel Ortega-Robles
,Elías Manjarrez
Posted: 04 March 2026
Measuring Velocity Using Moving Clocks—The Surprising Test of Tangherlini’s Theory
Andrew Wutke
Posted: 04 March 2026
Emerging 4D-Printed pH-Responsive Nanofiber Implants for Spatiotemporal Breast Cancer Therapy: Design Principles, Tumour Microenvironment Modulation, Translational Barriers, and Future Perspectives
Akash Sharma
,Chimpiri Srujani
,Reena Singh
,Mohammad Azeem
,Brijesh Shukla
,Vandana Tiwari
Posted: 04 March 2026
Do Ecological Patterns Persist in Highly Impacted Urban Wetlands? A Spatiotemporal Analysis of Aquatic Macrophytes and Limnological Variability in a Peruvian Coastal Wetland
Flavia Rivera-Cáceda
,José Arenas-Ibarra
,Sofía Urrutia-Ramírez
Urban coastal wetlands along the Peruvian Pacific coast are increasingly affected by urban expansion, pollution, and hydrological alterations, compromising their ecological integrity. In this context, the spatiotemporal variation of the aquatic macrophyte community and its relationship with limnological conditions and drivers of change were evaluated in the Santa Rosa wetland (Chancay, Lima). The objective is to evaluate the spatiotemporal variation of the aquatic macrophyte community in the Santa Rosa wetland and analyze its relationship with physicochemical limnological variables and drivers of change. Sampling was conducted during two contrasting hydrological seasons in 2022: T1 (summer) and T2 (winter), at six sampling points (P1–P6). Physicochemical variables (water depth, temperature, pH, conductivity, TDS, TSS, dissolved oxygen, turbidity, nitrate, ammonium, phosphorus, and dissolved organic matter) were measured, and the relative abundance of aquatic macrophytes was evaluated. Drivers of change were identified through direct observation and a structured matrix, with a PCoA performed to summarize spatiotemporal trends. Data were analyzed using Principal Component Analysis (PCA), Co-inertia analysis, and Multi-Response Permutation Procedures (MRPP). Significant spatiotemporal variation was observed in physicochemical parameters (p < 0.05), with moderate covariation between the two matrices (RV = 0.47). A total of ten aquatic macrophyte species were recorded, with higher abundance of Pontederia crassipes and Pistia stratiotes in T1, and Hydrocotyle ranunculoides and Bacopa monnieri in T2. The most relevant drivers of change were solid waste, livestock grazing, organic contamination, and urban expansion. Spatial heterogeneity was observed in the drivers of change affecting the Santa Rosa wetland, forming a mosaic of areas with different impact profiles. Despite multiple anthropogenic pressures, the Santa Rosa wetland maintains a limnological structure and a functionally coupled macrophyte community, evidencing ecological resilience to environmental degradation. The observed covariation between physicochemical conditions and vegetation confirms the persistence of essential ecological processes, even within an altered urban context. This study demonstrates that integrating biotic components, limnological variables, and drivers of change is fundamental to understanding and monitoring the ecological dynamics of urban wetlands along the Peruvian coast.
Urban coastal wetlands along the Peruvian Pacific coast are increasingly affected by urban expansion, pollution, and hydrological alterations, compromising their ecological integrity. In this context, the spatiotemporal variation of the aquatic macrophyte community and its relationship with limnological conditions and drivers of change were evaluated in the Santa Rosa wetland (Chancay, Lima). The objective is to evaluate the spatiotemporal variation of the aquatic macrophyte community in the Santa Rosa wetland and analyze its relationship with physicochemical limnological variables and drivers of change. Sampling was conducted during two contrasting hydrological seasons in 2022: T1 (summer) and T2 (winter), at six sampling points (P1–P6). Physicochemical variables (water depth, temperature, pH, conductivity, TDS, TSS, dissolved oxygen, turbidity, nitrate, ammonium, phosphorus, and dissolved organic matter) were measured, and the relative abundance of aquatic macrophytes was evaluated. Drivers of change were identified through direct observation and a structured matrix, with a PCoA performed to summarize spatiotemporal trends. Data were analyzed using Principal Component Analysis (PCA), Co-inertia analysis, and Multi-Response Permutation Procedures (MRPP). Significant spatiotemporal variation was observed in physicochemical parameters (p < 0.05), with moderate covariation between the two matrices (RV = 0.47). A total of ten aquatic macrophyte species were recorded, with higher abundance of Pontederia crassipes and Pistia stratiotes in T1, and Hydrocotyle ranunculoides and Bacopa monnieri in T2. The most relevant drivers of change were solid waste, livestock grazing, organic contamination, and urban expansion. Spatial heterogeneity was observed in the drivers of change affecting the Santa Rosa wetland, forming a mosaic of areas with different impact profiles. Despite multiple anthropogenic pressures, the Santa Rosa wetland maintains a limnological structure and a functionally coupled macrophyte community, evidencing ecological resilience to environmental degradation. The observed covariation between physicochemical conditions and vegetation confirms the persistence of essential ecological processes, even within an altered urban context. This study demonstrates that integrating biotic components, limnological variables, and drivers of change is fundamental to understanding and monitoring the ecological dynamics of urban wetlands along the Peruvian coast.
Posted: 04 March 2026
Open Pilonidal Excision as a Translational Human Model for Wound Healing and Skin Regeneration Research
Dimitrios Vardakostas
,Zoe Garoufalia
,Anastassios Philippou
,Dimitrios Mantas
Posted: 04 March 2026
Visualization of Lubrication Conditions Using the Electrical Impedance Method Considering Surface Roughness
Daichi Kosugi
,Fumiaki Aikawa
,Shunsuke Iwase
,Taisuke Maruyama
,Satoshi Momozono
Posted: 04 March 2026
EPHB4-Targeted CAR-T Cells Demonstrate Potent Antitumor Activity in an Orthotopic Tongue PDX Model of Oral Squamous Cell Carcinoma
Masaya Kinjo
,Kazunobu Ohnuki
,Kazumasa Takenouchi
,Toshihiro Suzuki
,Afsana Islam
,Larina Tzu-Wei Shen
,Daiki Fujita
,Mikio Suzuki
,Kazuto Matsuura
,Kenji Nakamaru
+1 authors
Posted: 04 March 2026
Fiscal Rule Stretching in the European Union: The Impact of Elections, Financial Stress, and Excessive Deficit Procedures on Government Debt Revisions
Apeksha Bhuekar
Posted: 04 March 2026
Decision-Grade Risk and Cost Mapping for Illegal Gold Mining at Crucitas, Costa Rica: Prioritization, Phased Remediation Portfolios, and Uncertainty-Aware Policy Ranking
Andrea Navarro Jiménez
Posted: 04 March 2026
Comparative Performance of Gaussian Plume and Backward Lagrangian Stochastic Models for Near-Field Methane Emission Estimation Using a Single Controlled Release Experiment
Aashish Upreti
,Kira Shonkwiler
,Stuart N. Riddick
,Daniel Zimmerle
Methane (CH4) is a major component of natural gas and a potent greenhouse gas. Increasing atmospheric methane concentrations are attributed to emissive anthropogenic activities by an average of 13 ppb per yr since 2020 and are linked to a changing global climate. Mitigating CH4 emissions from oil and gas production sites has recently become a target to reduce overall greenhouse gas emissions, however, monitoring the efficacy of mitigation strategies depends on accurate quantification of CH4 emissions at the facility-level. Near-field quantification of methane (CH4) emissions from oil and gas (O&G) facilities remains challenging due to the effects of atmospheric variability and sensor configuration on atmospheric dispersion models. This study evaluates the performance of two atmospheric dispersion models, the Gaussian Plume (GP) and backward Lagrangian Stochastic (bLS), by comparing calculated CH4 emissions to controlled single-point emissions of between 0.4 and 5.2 kg CH4 h-1. Emissions were calculated by both models using 121 individual sets of measurements comprising five-minute averaged downwind methane mixing ratios and matching meteorological data. Comparison shows the bLS approach showed better predictive performance with twice as many emission estimates were within a factor of two (FAC2) of the known emission rates compared to those calculated using the GP approach. The emissions calculated by the bLS model also had a lower multiplicative error and reduced bias relative to GP. Other error-based metrics further confirmed the bLS model performed better, as it yielded lower RMSE and MAE than GP. Statistical analysis of the emission data shows the lateral and vertical alignment of source and sensor plays a critical role in emission estimations as measurements made closer to the plume centerline and at a distance between 40 to 80 m downwind yielded the best FAC2 agreement. High wind meander degraded ability of both approaches to generate representative emissions particularly with the GP approach as it violates the modelling approach’s assumption of steady-state emissions. Data suggest emissions calculated by the bLS model are comprehensively in better agreement but the computational demands of the modeling approach and integration into fenceline systems limit real-time applicability. While it is likely that the results presented here are suitable for informing leak detection technology in relatively flat unvegetated environments, it is currently unknown if these findings will be applicable in more vertiginous or heavily vegetated oil and gas producing regions of the Marcellus or Uinta Basins.
Methane (CH4) is a major component of natural gas and a potent greenhouse gas. Increasing atmospheric methane concentrations are attributed to emissive anthropogenic activities by an average of 13 ppb per yr since 2020 and are linked to a changing global climate. Mitigating CH4 emissions from oil and gas production sites has recently become a target to reduce overall greenhouse gas emissions, however, monitoring the efficacy of mitigation strategies depends on accurate quantification of CH4 emissions at the facility-level. Near-field quantification of methane (CH4) emissions from oil and gas (O&G) facilities remains challenging due to the effects of atmospheric variability and sensor configuration on atmospheric dispersion models. This study evaluates the performance of two atmospheric dispersion models, the Gaussian Plume (GP) and backward Lagrangian Stochastic (bLS), by comparing calculated CH4 emissions to controlled single-point emissions of between 0.4 and 5.2 kg CH4 h-1. Emissions were calculated by both models using 121 individual sets of measurements comprising five-minute averaged downwind methane mixing ratios and matching meteorological data. Comparison shows the bLS approach showed better predictive performance with twice as many emission estimates were within a factor of two (FAC2) of the known emission rates compared to those calculated using the GP approach. The emissions calculated by the bLS model also had a lower multiplicative error and reduced bias relative to GP. Other error-based metrics further confirmed the bLS model performed better, as it yielded lower RMSE and MAE than GP. Statistical analysis of the emission data shows the lateral and vertical alignment of source and sensor plays a critical role in emission estimations as measurements made closer to the plume centerline and at a distance between 40 to 80 m downwind yielded the best FAC2 agreement. High wind meander degraded ability of both approaches to generate representative emissions particularly with the GP approach as it violates the modelling approach’s assumption of steady-state emissions. Data suggest emissions calculated by the bLS model are comprehensively in better agreement but the computational demands of the modeling approach and integration into fenceline systems limit real-time applicability. While it is likely that the results presented here are suitable for informing leak detection technology in relatively flat unvegetated environments, it is currently unknown if these findings will be applicable in more vertiginous or heavily vegetated oil and gas producing regions of the Marcellus or Uinta Basins.
Posted: 04 March 2026
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