Numerical study on the impact of coal fractures on seismic wave dispersion and attenuation: anisotropic WIFF effects. [PDF]
Li B, Zou G, Wang J, Chen H, Zhu G.
europepmc +1 more source
Abstract The United Kingdom's shallow aquifers offer significant but underdeveloped geothermal energy resource. Seismic methods can help address this by improving the understanding of aquifer heterogeneity and potentially allowing long‐term monitoring of thermal plumes.
Adam D. Booth +10 more
wiley +1 more source
The Preparation and CO<sub>2</sub>-Resistant Performance of a Smart Responsive Polymer Gel for CO<sub>2</sub> Flooding Channel Blocking. [PDF]
Meng X +9 more
europepmc +1 more source
Vacuum Infusion as a Processing Route for Transparent Wood Laminates
Schematic representation of the fabrication route for transparent wood laminates, including wood veneer delignification, epoxy resin impregnation by vacuum infusion processing, and the final TW‐1 transparent wood laminate. ABSTRACT Transparent wood (TW) has attracted increasing attention as a bio‐based material for daylighting and building‐envelope ...
Letícia Zimermann Pires +7 more
wiley +1 more source
CO<sub>2</sub>-responsive terpolymer hydrogels with adjustable dynamic networks for fractured plugging in the reservoir. [PDF]
Yan Y, Tao Y, Zhou S, Fan Y, Zhang P.
europepmc +1 more source
In Situ Curing‐Enabled 3D Printing of Continuous Fiber‐Reinforced Thermosetting Composites
In situ curing‐enabled the 3D printing of continuous fiber/thermoset composites, which were reviewed. Particularly, four types of in situ curing, were discussed, including Radiation‐induced curing, photothermal curing, electrothermal curing, and frontal polymerization. AI‐integrated printing was also analyzed.
Xiaofei Wu +2 more
wiley +1 more source
Horizontal well-assisted depressurization method for geothermal exploitation from fractured granite reservoir at Yangbajing geothermal field. [PDF]
Zeng Y +8 more
europepmc +1 more source
ABSTRACT Pingos are large mounds with cores formed of intrusive ice that form in periglacial landscapes. These ice structures can form in regions of discontinuous permafrost, commonly as hydraulic or open‐system pingos, or in locations of continuous permafrost, commonly as hydrostatic or closed‐system pingos.
Venezia M. Follingstad +12 more
wiley +1 more source
Numerical simulation of hydraulic-natural fracture interaction based on the continuous-discontinuous element method. [PDF]
Yang K +5 more
europepmc +1 more source
Gas Channeling Identification in Fractured Condensate Gas Reservoirs: Methodology and Application. [PDF]
Zhang L +5 more
europepmc +1 more source

