Summary
Rising commodity prices have resulted in an increase in secondary recovery
projects that are associated with lower permeability reservoirs. These
processes often inject fluids above the parting pressure for the duration of
the life of the flood, and pressurization takes place as fluids leak off from
the exposed surface area of the induced fracture into the surrounding moderate
or low-permeability reservoir matrix. The primary difference between these
situations and conventional flooding is that matrix fluid migration is
initiating off an induced fracturing plane, as opposed to point-source
initiation.
During the early history of a flood, mass-balance issues are often ignored,
as average reservoir pressures are typically low, and injection rates can
dramatically exceed production. As pressures rise, some localized portions of
the reservoir not only can exceed virgin static pressures, but volumes near
existing induced fractures can approach or equal the pressure in those
fractures. When this occurs, vertical fracturing initiates within the
reservoir, and can migrate either above or below the reservoir, depending upon
the location of the closest lower stress interval.
A new method to detect the location of vertical "leakage" has been
developed. This method uses existing surface tiltmeter (STM) technologies and a
new surface deformation calculation regime to zero in on volumetric changes
that occur above or below the limits of the given reservoir. This method uses
measured surface deformation from observed tilt to extrapolate the volumetric
change at different specified depths. With a number of constraints and using a
linear geophysical model based on poroelastic equations, an inversion routine
is used to find the reservoir compaction or expansion at different depths. When
volumetric change best fits the measured deformation data (or tilt) at the
surface, the depth and aerial location is then correlated to the area near a
specific well or wells.
© 2009. Society of Petroleum Engineers
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History
- Original manuscript received:
13 February 2008
- Meeting paper published:
20 April 2008
- Revised manuscript received:
22 October 2008
- Manuscript approved:
25 February 2009
- Published online:
28 October 2009
- Version of record:
28 October 2009