Talk Abstract:
Coupled Geomechanics and Flow Simulation for Time-lapse Seismic
Modeling
Susan
E. Minkoff
Sandia National Laboratories
seminko@santafe.mp.sandia.gov
Joint work with Charles M. Stone, J.
Guadalupe Arguello, Sandia National Labs,
Steve Bryant, Joe Eaton, Malgo Peszynska, Mary Wheeler,
University of Texas at Austin.
Time-lapse seismic feasibility studies for compactible reservoirs
such as Ekofisk in the North Sea require coupled flow simulation
and geomechanical deformation modeling. We present an algorithm
for 2-way coupling of flow and geomechanics and indicate what
impact the coupled code has on calculation of seismic velocities
and density. Each of the simulators --- the reservoir simulator
from the University of Texas and the geomechanics code from
Sandia National Labs --- was developed under the US DOE's ACTI
program. The codes use 3D finite element discretizations and
can be run in parallel. The flow simulator can account for faults
and multiple flow models in a single simulation. The geomechanics
code models contacts and large, inelastic deformations. We modify
the black oil system to include changes in the reservoir geology
(porosity) during a single simulation while still maintaining
conservation of mass. Modifications to the geomechanics code
allow changes in pore pressure to be included in the total stress
calculation. The geomechanics code produces volumetric strain-induced
porosity updates for the flow simulator. By allowing the two
simulators to have different spatial grids and to take different
time steps, we are able to account for physical differences
in resolution between flow and geomechanics. A plastic cap constitutive
model provides a realistic mechanism for capturing subsidence
due to production-induced pressure drops. We demonstrate the
coupled code with a synthetic example based on a diatomite reservoir
in the Belridge Field, California. Ten years of primary production
results in about 10 feet of subsidence at the wells. Correspondingly,
we see a 2-4% change in reservoir porosity during the simulation.
Calculation of saturated rock seismic velocities and density
using the coupled simulation are more realistic than calculation
of elastic rock properties from flow only.
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1999-2000
Reactive Flow and Transport Phenomena
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