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Data Publication

Data and software used in: “Non-Hertzian stress fields in simulated sandstone grains and implications for compactive brittle failure - a high-resolution FEM approach”

Shinohara, Takahiro

YoDa Data Repository, Utrecht University, Netherlands

(2024)

Globally, sandstone formations are typically targeted for hydrocarbon extraction. However, these activities often lead to surface subsidence or even induced seismicity. The cause lies in reservoir compaction driven by pore pressure depletion and the associated increase in effective overburden stress. Such compaction is partly elastic, but can additionally be caused by instantaneous plastic and rate/time-dependent processes, such as subcritical crack growth. Compaction due to grain breakage, either via critical or subcritical crack growth, is driven by tensile stresses acting on surface and volume flaws. Therefore, we performed high-resolution 3D linear elastic FEM simulations on simplified grain assemblies to investigate the effect of stress-strain boundary conditions, porosity and mineralogical variations on grain-scale stress fields. We found that compactive failure of sandstone due to grain breakage is related to the probability of pre-existing surface flaws with size up to 30 μm falling in a pore surface region with sufficiently high tensile stress where the Griffith criterion is satisfied. Using the tensile stress distribution observed in the 3D FEM simulations, a preliminary, time-independent failure probability model was developed, which qualitatively predicts a non-linear increase in grain cracking during deviatoric loading. The detailed findings of our work are found in the corresponding paper. The data presented here are the input geometry and output (results) for the 3D FEM simulations, an in-house python code for 2D FEM simulations performed to obtain polynomial functions employed to describe appropriate boundary conditions for some of the 3D simulations, the input geometry and output (results) for the 2D FEM simulations and a MATLAB script for the failure probability model.

Keywords


Originally assigned keywords
Rock and melt physical properties
grain scale stress field
crack growth
porous sandstone compaction
local porosity variation
probabilitytype sandstone failure model
Finite Element Modelling
sandstone
deformation testing
elasticity
strain
vacuum
bulk sample deformation behavior
intragranular cracking

Corresponding MSL vocabulary keywords
sandstone
deformation testing
elasticity
elasticity
strain
strain
vacuum
intragranular cracking
intragranular crack

MSL enriched keywords
sedimentary rock
sandstone
Apparatus
deformation testing
Measured property
elasticity
Measured property
elasticity
strain
strain
vacuum
Inferred deformation behavior
microphysical deformation mechanism
intragranular cracking
Analyzed feature
deformation microstructure
brittle microstructure
intragranular crack
pore fluid pressure
coupled mechanical-chemical effects
rate of crack growth
porosity
time-dependent mechanism
sub-critical crack growth
porosity
antropogenic setting
Induced seismicity
surface subsidence
induced seismicity
surface subsidence

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/uu01-1yqpu8


Authors

Shinohara, Takahiro

Utrecht University;


Contributers

Thieulot, Cedric

Supervisor

Utrecht University;

Spiers, Christopher

Supervisor

Utrecht University;

Hangx, Suzanne

Supervisor

Utrecht University;


Citiation

Shinohara, T. (2024). Data and software used in: “Non-Hertzian stress fields in simulated sandstone grains and implications for compactive brittle failure - a high-resolution FEM approach” (Version 1.0). Utrecht University. https://doi.org/10.24416/UU01-1YQPU8


Collection Period

2020-07-01 - 2023-12-31