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Data Publication

Intergranular clay films control inelastic deformation in the Groningen gas reservoir: Evidence from split-cylinder deformation tests

Pijnenburg, Ronald | Verberne, Berend Antonie | Hangx, Suzanne | Spiers, Christopher James

YoDa Data Repository, Utrecht University, Netherlands

(2019)

Production of oil and gas from sandstone reservoirs leads to small elastic and inelastic strains in the reservoir, which may induce surface subsidence and seismicity. While the elastic component is easily described, the inelastic component, and any rate-sensitivity thereof remain poorly understood in the relevant small strain range (≤ 1.0%). To address this, we performed a sequence of five stress/strain-cycling plus strain-marker-imaging experiments on a single split-cylinder sample (porosity 20.4%) of Slochteren sandstone from the seismogenic Groningen gas field. The tests were performed under in-situ conditions of effective confining pressure (40 MPa) and temperature (100°C), exploring increasingly large differential stresses (up to 75 MPa) and/or axial strains (up to 4.8%) in consecutive runs. At the small strains relevant to producing reservoirs (≤ 1.0%), inelastic deformation was largely accommodated by deformation of clay-filled grain contacts. High axial strains (>1.4%) led to pervasive intragranular cracking plus intergranular slip within localized, conjugate bands. Using a simplified sandstone model, we show that the magnitude of inelastic deformation produced in our experiments at small strains (≤ 1.0%) and stresses relevant to the Groningen reservoir can indeed be roughly accounted for by clay film deformation. Thus, inelastic compaction of the Groningen reservoir is expected to be largely governed by clay film deformation. Compaction by this mechanism is shown to be rate-insensitive on production time-scales, and is anticipated to halt when gas production stops. However, creep by other processes cannot be eliminated. Similar, clay-bearing sandstone reservoirs occur widespread globally, implying a wide relevance of our results. The data is provided in a folder with 3 subfolders for 5 experiments/samples. Detailed information about the files in these subfolders as well as information on how the data is processed is given in the explanatory file Pijnenburg-et-al_2019_data-description.docx. Contact person is Ronald Pijnenburg - Researcher - r.p.j.pijnenburg@uu.nl.

Keywords


Originally assigned keywords
Natural Sciences Earth and related environmental sciences 15
Induced seismicity
Compaction
Poroelasticity
Plasticity
Sandstone
Strain partitioning
Mechanisms
Clay
Earthquakes
Earth Gasses Liquids
Stability
Scanning Electrone Microscope
Triaxial
Strength
Thermocouple
Strain gauge
EPOS
multiscale laboratories
rock and melt physics properties

Corresponding MSL vocabulary keywords
Induced seismicity
induced seismicity
strain
strain
poroelastic deformation
ductile deformation
sandstone
strain partitioning
clay
clay
scanning electron microscope (SEM)
thermometer

MSL enriched keywords
antropogenic setting
Induced seismicity
induced seismicity
Measured property
strain
Measured property
strain
Inferred deformation behavior
deformation behaviour
poroelastic deformation
ductile deformation
sedimentary rock
sandstone
strain partitioning
minerals
silicate minerals
phyllosilicates
clay
unconsolidated sediment
clastic sediment
clay
Apparatus
electron microscopy
scanning electron microscope (SEM)
Ancillary equipment
measurement of temperature
thermometer
inelastic deformation
gas field
subsurface energy production
hydrocarbon energy production
gas field
wacke
Slochteren sandstone
porosity
microphysical deformation mechanism
intragranular cracking
intergranular slip
time-dependent mechanism
porosity
surface subsidence
Analyzed feature
deformation microstructure
brittle microstructure
intragranular crack
intergranular slip
surface subsidence

MSL original sub domains

rock and melt physics

MSL enriched sub domains i

rock and melt physics
analogue modelling of geologic processes
microscopy and tomography


Source publisher

YoDa Data Repository, Utrecht University, Netherlands


DOI

10.24416/UU01-8AVM9K


Authors

Pijnenburg, Ronald

0000-0003-0653-7565

Utrecht University;

Verberne, Berend Antonie

0000-0002-1208-6193

National Institute of Advanced Industrial Science and Technology, Geological Survey of Japan, Tsukuba, Japan;

Hangx, Suzanne

0000-0003-2253-3273

Utrecht University;

Spiers, Christopher James

0000-0002-3436-8941

Utrecht University;


Contributers

Pijnenburg, Ronald

ContactPerson

0000-0003-0653-7565

Utrecht University;

Verberne, Berend Antonie

Researcher

0000-0002-1208-6193

National Institute of Advanced Industrial Science and Technology, Geological Survey of Japan, Tsukuba, Japan;

Hangx, Suzanne

Supervisor

0000-0003-2253-3273

Utrecht University;

Spiers, Christopher James

Supervisor

0000-0002-3436-8941

Utrecht University;

Experimental rock deformation/HPT-Lab (Utrecht University, The Netherlands)

HostingInstitution

Utrecht University;


References

Pijnenburg, R. P. J., Verberne, B. A., Hangx, S. J. T., & Spiers, C. J. (2019). Intergranular Clay Films Control Inelastic Deformation in the Groningen Gas Reservoir: Evidence From Split‐Cylinder Deformation Tests. Journal of Geophysical Research: Solid Earth, 124(12), 12679–12702. Portico. https://doi.org/10.1029/2019jb018702

10.1029/2019JB018702

IsSupplementTo

Preibisch, S., Saalfeld, S., & Tomancak, P. (2009). Globally optimal stitching of tiled 3D microscopic image acquisitions. Bioinformatics, 25(11), 1463–1465. https://doi.org/10.1093/bioinformatics/btp184

10.1093/bioinformatics/btp184

IsReferencedBy


Contact

Experimental rock deformation/HPT-Lab (Utrecht University, The Netherlands)

Utrecht University;


Citiation

Pijnenburg, R., Verberne, B. A., Hangx, S., & Spiers, C. J. (2019). Intergranular clay films control inelastic deformation in the Groningen gas reservoir: Evidence from split-cylinder deformation tests. Utrecht University. https://doi.org/10.24416/UU01-8AVM9K


Collection Period

2017-01-01 - 2019-01-01


Geo location(s)

53.14228274279933, 6.447993994041667, 53.460706452448434, 7.041255712791667