Description: Pore pressure reduction in sandstone reservoirs generally leads to small elastic plus inelastic strains. These small strains (0.1 – 1.0% in total) may lead to surface subsidence and induced seismicity. In current geomechanical models, the inelastic component is usually neglected, though its contribution to stress-strain behaviour is poorly constrained.To help bridge this gap, we performed deviatoric and hydrostatic stress-cycling experiments on Slochteren sandstone samples from the seismogenic Groningen gas field in the Netherlands. We explored in-situ conditions of temperature (T = 100°C) and pore fluid chemistry, porosities of 13 to 26% and effective confining pressures (≤ 320 MPa) and differential stresses (≤ 135 MPa) covering and exceeding those relevant to producing fields. The findings of our work are outlined in the corresponding paper. The data presented here are the measured mechanical tabular data and microstructural data (stitched mosaic of backscatter electron images) provided as uncompressed jpg images. In addition, for one sample we include chemical element maps obtained through Electron Dispersive X-ray spectrometry (EDX).
Global identifier:
Doi( "10.5880/fidgeo.2019.013", )
Origins: /Wissenschaft/GFZ
Tags: Blei ? Papier ? Sandstein ? Karte ? Induzierte Seismizität ? Daten ? Modellversuch ? Verdichtung ? Chemisches Element ? Cam clay ? Composition ? EARTH SCIENCE > SOLID EARTH > EARTH GASES/LIQUIDS ? EARTH SCIENCE > SOLID EARTH > ROCKS/MINERALS/CRYSTALS > SEDIMENTARY ROCKS > SEDIMENTARY ROCK PHYSICAL/OPTICAL PROPERTIES > STABILITY ? EARTH SCIENCE > SOLID EARTH > TECTONICS > EARTHQUAKES ? EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS > STRAIN ? EPOS ? Elasticity ? European Plate Observing System ? Scanning Electrone Microscope ? Strain gauge ? Strength ? Thermocouple ? Triaxial ? mechanisms ? multi-scale laboratories ? plasticity ? poroelasticity ? rock and melt physical properties ? strain partitioning ?
License: cc-by/4.0
Language: Englisch/English
Issued: 2019-01-01
Time ranges: 2019-01-01 - 2019-01-01
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