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A fracture face image analysis procedure was employed to quantify asphalt dispersion, which was key to establishing the relationships between material microstructural features and measured strengths.
Here we present an experimental investigation based on a coreflood sequence that simulates fluid invasion, flowback, and hydrocarbon production within the rock near the fracture face.
The flow of gas in tight, low-pressure gas wells can be partially blocked by the water saturation build-up near the hydraulic fracture face if the drawdown pressure does not exceed the capillary pressure.
To early observers, the fracture from such a crack evoked ideas of a phenomenon of degradation over time, which was supported in the minds of the proponents of this interpretation by the smooth fracture face redolent of a fracture in a brittle material; this led them to postulate that the material had suffered an instantaneous fracture.
Although this study puts forward the theoretical basis of the hydraulic permeability modelling under combined effect of compaction and embedment, more fundamental studies are required to investigate the contact behaviour between the proppant packs and the fracture face under various conditions.
Particle deposition around the wellbore and the fracture face, modeled using filtration theory.
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Lipid droplets that are cross-fractured reveal a simple homogeneous content or stacked internal fracture faces.
The fracture faces and the corrosion were observed by optical microscopy and SEM.
Both theory and observations indicate that fractures can significantly increase spontaneous imbibition in unsaturated sedimentary rock by capillary action and surface spreading on rough fracture faces.
After the tests, the fracture faces of the specimens were examined by SEM to analyse the fracture type (brittle or ductile).
The proppant particles are modelled as rigid spheres and the deformation of the fracture faces is assumed to be purely elastic.
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