
Oil and Natural Gas Supply
Improved Recovery at Eva South Unit

Improved Recovery at Eva South Unit
By David Wheeler, Jerry A. Pope, and William A. Miller, Ensign Operating
Company
Eva South Unit in Texas County, Oklahoma is a new project funded under
the DOE Reservoir Class Field Demonstration Program (Class Revisit). Eva
South Unit
produces from transgressive, fluvial valley-fill sandstones of the Pennsylvanian
age Morrow Formation. The reservoir displays both lateral and vertical
heterogeneity due to episodic channel abandonment during deposition and
subsequent faulting. This has resulted in reservoir compartmentalization
that interferes with waterflood sweep efficiency. Ensign Operating Company
has acquired high resolution, P-wave and P-S wave three-dimensional (3C3D)
data to enhance reservoir characterization of Eva South Unit. These data
are being used to reduce drilling risks and determine the optimal placement
of horizontal wells.
Field History
Ensign acquired the 30-year old Eva South field in 1992 and began waterflooding
in 1993. Incremental secondary recovery as of September 1999 was 601 MBO.
Ultimate recovery based on the waterflood was projected at 1,276 MBO or
17.7% of original-oil-in-place (OOIP). Ensign has determined that an additional
450 MBO could be recovered through improved sweep efficiency.
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| Figure 4 Eva South amplitude with locations of seismic lines. |
Characterization has shown that Eva South Unit
has four compartments divided by the Teepee Creek fault on the west, and
by abandoned channel-fill deposits on the south and east. The reservoir
is active channel-fill sandstone at the base, overlain by abandoned channel-fill
sandstones. The SW compartment is dominantly shaley abandoned channel-fill
with tow thin beds of sandstone. Compartmentalization and heterogeneity
caused by the abandoned channel-fill deposits and faulting have impeded
the sweep efficiency of the waterflood.
Goal
The goal of the 3C3D seismic survey is to resolve
the geometry of the compartments and permeabilities, locate any that have
not been identified, an look for additional areas of undrilled reservoir
for development. The plan is to drill a horizontal well to improve sweep
efficiency from the compartments.
Seismic Evaluation
Most of the wells at Eva South Unit have sonic
logs. These logs were used to construct models showing that seismic imaging
was possible. Surface-generated shear-wave seismic has been used in a Morrow
reservoir nearby in Sorrento field in southeast Colorado. Ensign had the
high-resolution 3C3D seismic survey ran in May 1999. To date, only the
P-wave portion of the survey has been evaluated. The S-wave data had been
processed and is being evaluated.
Morrow Structure at Eva South
Unit
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| Figure 5 Net sandstone isopach with locations of cross sections |
Within the core area of the Unit the structure
was well defined through drilling and log data. In addition to the Teepee
Creek fault two fault systems were mapped. The faults west of Teepee Creek
do not effect the Unit, but a third fault system on the eastern edge of
the field appears to separate one of the injector wells from its producers.
Shuting-in the injector for three weeks and running pressure tests indicates
that there is effective communication despite the presence of the fault.
The amplitude maps and arbitrary lines show that
the Eva South Unit valley system is recognizable on the P-wave data. Discrepancies
with the well control include the weak amplitude response of two wells,
the best reservoir development and best production in the field and the
strong amplitude response west of the Teepee Creek fault where there is
currently no reservoir development. Based on the structural enhancement
(Figure 5) provided by the seismic survey, Ensign is planning a
horizontal well approximately parallel to the east side of the Teepee Creek
fault. That well is planned to tap reserves that are trapped south of an
existing injection well and improve the overall sweep efficiency of the
west side of the field.
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| Figure 6 Ensign's upper Morrow waterflood units. |
Conclusion
The P-wave data has proven to be effective at
defining Morrow valleys at an exploration level. S-Wave data is able to
further define reservoir heterogeneity and compartmentalization. Ensign
believes that an additional 450 MBO (6.2% of
OOIP) can be recovered. These
improvements in reservoir characterization increase the possibility of
a future CO2 flood that could add an additional 723 MBO (10% of OOIP) of
reserves. If the technology is successful at Eva South Unit, Ensign will
apply it to three other upper Morrow fields (Figure 6) which have
reserves of 1.775 MMBO.
The Class Act Summer 2000 Edition Volume
6/2
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