Flexible sweat sensor patch integrating graphene‑interfaced gold microelectrodes functionalized with bio‑receptors and ion‑selective membrane, coupled with a capillary‑driven microfluidic layer and portable potentiostat electronics for multiplexed monitoring of inflammatory, metabolic, and electrolyte biomarkers in microliter sweat volumes.
Roomia Memon +4 more
wiley +1 more source
Isotropic components of microseismic moment tensors at Utah FORGE reveal a diversity of fluid pathway creation processes in EGS development. [PDF]
Niemz P +4 more
europepmc +1 more source
This study shows that a lightweight blackbox neural network provides a practical, cost‐effective solution for bidirectional process prediction in laser‐induced graphene (LIG) fabrication. Achieving high predictive performance with minimal overhead, the approach democratizes machine learning (ML) for resource‐limited environments.
Maxim Polomoshnov +3 more
wiley +1 more source
Multidisciplinary approaches to lithological discrimination and structural mapping for mineral resource assessment. [PDF]
Elfadly MA +8 more
europepmc +1 more source
Research on an islanding detection method suitable for distributed generation grid-connection complex system. [PDF]
Sun W, Yu S, Jiang Z.
europepmc +1 more source
A reproducible workflow for 3D finite-element modeling of strike-slip duplex deformation in Abaqus. [PDF]
Khalifeh-Soltani A +2 more
europepmc +1 more source
Spatiotemporal Evolution and Drivers of Highway Surface Deformation Based on SBAS-InSAR and Geodetector. [PDF]
Chen Z, Li J, Zhang X, Bi J.
europepmc +1 more source
The effects of normal fault movement on the failure mechanism of water conveyance tunnels considering multi-field interaction. [PDF]
Xinwei Z, Zhanxiang C, Weiheng L.
europepmc +1 more source
Delineating the Central Anatolia Transition Zone (CATZ): Constraints from Integrated Geodetic (GNSS/InSAR) and Seismic Data. [PDF]
Kutoğlu ŞH, Akgün E, Softa M.
europepmc +1 more source
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Fault zone fabric and fault weakness
Nature, 2009Geological and geophysical evidence suggests that some crustal faults are weak compared to laboratory measurements of frictional strength. Explanations for fault weakness include the presence of weak minerals, high fluid pressures within the fault core and dynamic processes such as normal stress reduction, acoustic fluidization or extreme weakening at ...
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