104 research outputs found
Analyse quantitative de l'hétérogénéité de la fracturation : application aux carrières souterraines
Changes in composition and pore space of sand rocks in the oil water contact zone (section YU[1] {3-4}, Klyuchevskaya area, Tomsk region)
The article provides an analysis of specific features in changes of rocks in the oil water contact zone. The object of study is the formation YU[1] {3-4} (J[3]o[1]) of Klyuchevskaya oil deposit (West Siberian oil-gas province, Tomsk region). The research data allow the authors to determine vertical zoning of the surface structure and identify the following zones: oil saturation (weak alteration), bitumen-content dissolution, non-bitumen-content dissolution, cementation, including rocks not affected by hydrocarbon deposit. The rocks under investigation are characterized by different changes in composition, pore space, as well as reservoir filtration and volumetric parameters. Detection of irregularity in distribution of void- pore space in oil-water contact zones is of great practical importance. It helps to avoid the errors in differential pressure drawdown and explain the origin of low-resistivity collectors
Contribution à la modélisation des vitesses de propagation des ondes P et S dans les formations sédimentaires argileuses
Monitoring of water and heat transfer in the vadose zone of a carbonate formation: An example of an underground quarry in Gironde, France
Diagenetic signature of the Mid-Paleocene exposure surface in the southeastern Pyrenean platform
Electrokinetic Characterization of Natural Stones Coated with Nanocomposites for the Protection of Cultural Heritage
Protective coatings, in recent years also from nanocomposite formulations, are commonly applied onto architectural stone and stone artefacts, mainly to prevent absorption of condensed water and dissolved atmospheric pollutants into the porous stone structure. While standard protocols to assess a coating’s performance are available, understanding the response of the coating-stone system is a complex task, due to the interplay of various factors determining the overall behaviour. Characterization techniques allowing one to correlate the extent and nature of surface modification upon treatment with the most relevant physical properties (i.e., water absorption and surface wettability) are thus of great interest. Electrokinetic analysis based on streaming current measurements, thanks to its sensitivity towards even minor changes in the surface chemical composition, may fulfil such requirement. Indeed, by involving the interaction with a testing aqueous electrolyte solution, this technique allows one to probe not only the outer surface, but also the outermost layer of the pore network, which plays a crucial role in the interaction of the stone with condensed atmospheric water. In this work, a correlation was found between the extent of surface modification, as determined by streaming current measurements, surface wettability and capillary water absorption, for three lithotypes with different mineralogical and microstructural properties treated with two nanocomposite formulations (one water based and one in alcoholic solvent) containing organosilica precursors and titania nanoparticle
Shear banding in drained and undrained triaxial tests on a saturated sandstone: Porosity and permeability evolution
Radon-222 as a tracer of water–air dynamics in the unsaturated zone of a geological carbonate formation: Example of an underground quarry (Oligocene Aquitain limestone, France)
Méthode d’évaluation quantitative de l’hétérogénéité de la fracturation dans les carrières souterraines de calcaire à astéries
Méthode d’évaluation quantitative de l’hétérogénéité de la fracturation dans les carrières souterraines de calcaire à astéries
Durant ces dix dernières années, l’analyse quantitative de l’hétérogénéité de la fracturation par le Système d’information géographique (SIG) devient intéressante pour étudier la stabilité des carrières souterraines et des propriétés réservoirs induites par la fracturation et ses relations avec les écoulements souterrains. Cet article propose une méthode d’analyse quantitative de la fracturation du calcaire en carrières souterraines. Plus de 1 000 fractures dans trois carrières souterraines carbonatées ont été relevées, mesurées, cartographiées et numérisées. L’analyse de l’hétérogénéité et de la connexité de la fracturation est fondée sur la répartition spatiale des paramètres géométriques de chaque fracture, tels que : ouverture, longueur, direction, orientation, écartement et distribution spatiale des familles de fractures
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