TY - GEN

T1 - Viscoelastic stress relaxation for estimating Shmin magnitude in deep sedimentary formations

AU - Mandal, P. P.

AU - Sarout, J.

AU - Rezaee, R.

AU - Finkbeiner, Thomas

N1 - KAUST Repository Item: Exported on 2023-03-14
Acknowledgements: The authors would like to acknowledge DMIRS and Finder Pty Ltd for providing relevant datasets to carry forward this work. We want to thank CSIRO’s Geomechanics and Geophysics Laboratory team members for their support to conduct the creep deformation study. PPM is financially supported by Australian Government’s RTP scholarship, Curtin University’s completion scholarship and PESA’s postgraduate scholarship.

PY - 2022/6/26

Y1 - 2022/6/26

N2 - General adaptability of viscoelastic stress relaxation from laboratory time-dependent deformation (creep) measurement to derive the least principal stress Shmin magnitudes at depths in sedimentary rocks is proposed. It is based upon a simple viscous rheological model and steady-state tectonic strain loading. Creep data reveals different viscoelastic behavior of rocks mostly controlled by the varying mineral composition and the direction of creep measurement (perpendicular/parallel to the bedding plane). First, this approach is applied in a vertical drilled well then verify in another vertical well located in the Canning Basin where the target resources are ultralow permeable unconventional gas shale reservoirs. A continuous Shmin magnitude profile at depth is obtained from wireline logs through the following: (i) combination of laboratory power-law fitting coefficients, (ii) geological horizontal stress accumulation by constant tectonic loading, and (iii) relatively uniform stress variation of principal stress components (Equation presented). along with depth. Eaton's extended model could not capture the stress layering effect precisely and may introduce more uncertainty because of its dependency on several unpredictable parameters while the proposed rheology model relies upon laboratory constituent parameters (B, n) where B is the inverse of static Young's modulus E and n describes time dependency of rock deformation under a given stress.

AB - General adaptability of viscoelastic stress relaxation from laboratory time-dependent deformation (creep) measurement to derive the least principal stress Shmin magnitudes at depths in sedimentary rocks is proposed. It is based upon a simple viscous rheological model and steady-state tectonic strain loading. Creep data reveals different viscoelastic behavior of rocks mostly controlled by the varying mineral composition and the direction of creep measurement (perpendicular/parallel to the bedding plane). First, this approach is applied in a vertical drilled well then verify in another vertical well located in the Canning Basin where the target resources are ultralow permeable unconventional gas shale reservoirs. A continuous Shmin magnitude profile at depth is obtained from wireline logs through the following: (i) combination of laboratory power-law fitting coefficients, (ii) geological horizontal stress accumulation by constant tectonic loading, and (iii) relatively uniform stress variation of principal stress components (Equation presented). along with depth. Eaton's extended model could not capture the stress layering effect precisely and may introduce more uncertainty because of its dependency on several unpredictable parameters while the proposed rheology model relies upon laboratory constituent parameters (B, n) where B is the inverse of static Young's modulus E and n describes time dependency of rock deformation under a given stress.

UR - http://hdl.handle.net/10754/690314

UR - https://onepetro.org/ARMAUSRMS/proceedings/ARMA22/All-ARMA22/ARMA-2022-0172/510243

UR - http://www.scopus.com/inward/record.url?scp=85149202027&partnerID=8YFLogxK

U2 - 10.56952/ARMA-2022-0172

DO - 10.56952/ARMA-2022-0172

M3 - Conference contribution

SN - 9780979497575

BT - All Days

PB - ARMA

ER -