Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Lutz Riepe"'
Autor:
Dr. Lutz Riepe
Publikováno v:
Proc. Indon Petrol. Assoc., 33rd Ann. Conv..
Publikováno v:
IPTC 2014: International Petroleum Technology Conference.
Abstract For the planning of an EOR project in a major mature oil field in East Malaysia, an extensive Routine and Special Core Analysis (RCA/SCAL) programme has been performed on unconsolidated clastic reservoir rocks. In view of the limited availab
Autor:
Mark Alexander Knackstedt, Alexandra Golab, Anna Carnerup, Tim Senden, Alan Butcher, Lutz Riepe
Publikováno v:
All Days.
Abstract Tight unconventional rocks have become an increasingly common target for hydrocarbon production. Exploitation of these resources requires a comprehensive reservoir description and characterization program to accurately estimate reserves and
Publikováno v:
All Days.
The paper provides a case history of the application of 3D imaging and Pore Network Modeling (PNM) technology to establish a direct relationship between rock micro-structure parameters from 3D via micro-tomographic images, and the simulation of petro
Publikováno v:
Colloids and Surfaces. 27:97-122
A theory has been developed for calculating interlayer conductivity for natural porous systems, such as sedimentary rocks. As the materials investigated are mainly made up of silica and alumina minerals, an electrical double layer can be presumed, wh
Publikováno v:
Particle & Particle Systems Characterization. 1:66-73
Besides the knowledge of material constants of the homogeneous phases of a disperse system, a good understanding of its geometrical properties is necessary for describing physical processes. In order to characterize the shape of the interface between
Publikováno v:
Journal of Microscopy. 148:121-147
SUMMARY Based on self organized growth, a self-similar geometrical model of rock materials is established. The structural mode of the internal surface is carried over to the three-dimensional structure of the pore space and solid phase, which can be
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Akademický článek
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