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Data Publication

Acoustic, mechanical, and microstructure data used in: Coda-Wave Based Monitoring of Pore-Pressure Depletion-driven Compaction of Slochteren Sandstone Samples from the Groningen Gas Field

Reuben Zotz-wilson

4TU.ResearchData

(2019)

Pore-pressure depletion in sandstone reservoirs is well known to cause both elastic and inelastic compaction, often resulting in notable surface subsidence and induced seismicity. Recent studies indicate that in such cases inelastic strain, which is often neglected in geomechanical models, represents a significant proportion of the total strain throughout reservoir production. While there has been considerable effort to quantify the proportion of continuous inelastic deformation from the mechanical response of laboratory samples, there has been little focus to date on the associated acoustic response throughout compaction. With this in mind, we employ three coda-wave based processing methods for the active source monitoring of ultrasonic velocity, scattering power, and intrinsic/scattering attenuation during the pore-pressure depletion of core samples from the Slochteren sandstone reservoir in the Groningen gas field (the Netherlands). Our results corroborate previous studies suggesting that initially, inelastic deformation occurs primarily along intergranular boundaries, with intergranular cracking developing towards the end of depletion and particularly for the highest porosity samples. Furthermore, analysis of Biot type intrinsic attenuation indicates that this compaction occurs in several stages of predominately intergranular closure, transitioning into primarily intergranular slip/cracking, and eventually porosity-dependent intragranular cracking. We demonstrate how this segmentation of pore-pressure driven compaction can be used to characterise differences in sample properties, and monitor the evolution of microstructural inelastic deformation throughout depletion. We further discuss the feasibility of in/cross-borehole monitoring of reservoir compaction, for both improved geo-mechanical modelling and early warning detection of induced seismicity.

Keywords


Originally assigned keywords
Environmentally Sustainable Mineral Resource Activities
Geology
Geophysics
Other Earth Sciences
Compaction
Inelastic deformation
Intrinsic Attenuation
Seismicity

Corresponding MSL vocabulary keywords
strain
strain
inelastic deformation

MSL enriched keywords
Measured property
strain
Measured property
strain
Inferred deformation behavior
deformation behaviour
inelastic deformation
sedimentary rock
sandstone
wacke
Slochteren sandstone
antropogenic setting
gas field
subsurface energy production
hydrocarbon energy production
gas field
Ancillary equipment
acoustic measurement - active source
ultrasonic imaging equipment
inelastic strain
porosity
microphysical deformation mechanism
intragranular cracking
intergranular cracking
intergranular slip
Ancillary equipment
model structure monitoring (3D)
acoustic measurement - active source
ultrasonic imaging equipment
inelastic strain
porosity
Induced seismicity
surface subsidence
Analyzed feature
deformation microstructure
brittle microstructure
intragranular crack
intergranular slip
induced seismicity
surface subsidence
Equipment
borehole monitoring
borehole drilling
drill core

MSL enriched sub domains i

rock and melt physics
analogue modelling of geologic processes
microscopy and tomography
geo-energy test beds


Source publisher

4TU.ResearchData


DOI

10.4121/uuid:45955068-7b0b-4b51-84f0-500a1c4cf63a


Authors

Reuben Zotz-wilson


Contributers

Nederlandse Aardolie Maatschappij

Other

TU Delft, Faculty of Civil Engineering and Geosciences, Department of Geoscience and Engineering

Other


References

References


Citiation

Zotz-wilson, R. (2019). Acoustic, mechanical, and microstructure data used in: Coda-Wave Based Monitoring of Pore-Pressure Depletion-driven Compaction of Slochteren Sandstone Samples from the Groningen Gas Field (Version 1) [Data set]. 4TU.Centre for Research Data. https://doi.org/10.4121/UUID:45955068-7B0B-4B51-84F0-500A1C4CF63A


Geo location(s)

Groningen gas field