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This study covers three wells of the Sauerlach site with highly deviated reservoir sections.
Waterdrive in macroscopic reservoir sections occurs on the scale of flooding in hillsides rather than core plugs.
Equation 2 is considered to be more representative of the full reservoir sections (Fig. 6; bold line).
All stress indicator data are measured in the borehole coordinate system against TOH due to high well inclination in the reservoir sections.
For gas displacing oil and dry gas displacing wet gas in recycling, the emphasis is on presenting useful analytical techniques for describing the sweep efficiency of both processes in macroscopic reservoir sections.
Liquid permeability measured parallel to the bedding plane of 20 core samples from various reservoir sections, at connate water saturation, give a geometric mean of approximately 37.1 mD (Nadeason et al. 2001).
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Figure 3 Digital elevation map of the study reservoir section.
It helps rank and screen the major waste discharge outlets within the study reservoir section.
Data originate from the main reservoir section, i.e. the upper part of the Gassum formation.
Figure 12 shows the log data for case #2; the reservoir section is limestone.
The logs are available for the uppermost 140 m of the reservoir section.
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