Skip to main content

Research Repository

Advanced Search

Nanoindentation of Horn River Basin Shales: The Micromechanical Contrast Between Overburden and Reservoir Formations

Charlton, T.S.; Rouainia, M.; Aplin, A.C.; Fisher, Q.J.; Bowen, L.

Nanoindentation of Horn River Basin Shales: The Micromechanical Contrast Between Overburden and Reservoir Formations Thumbnail


Authors

T.S. Charlton

M. Rouainia

Q.J. Fisher

Leon Bowen leon.bowen@durham.ac.uk
Senior Manager (Electron Microscopy)



Abstract

We present a micromechanical characterization of shales from the Horn River Basin, NW Canada. The shales have contrasting mineralogy and microstructures and play different geomechanical roles in the field: the sample set covers an unconventional gas reservoir and the overburden unit that serves as the upper fracture barrier. Composition and texture were characterized using X-ray diffraction, mercury injection porosimetry, and scanning electron microscopy (SEM). Grid nanoindentation testing was used to obtain the mechanical response of the dominant phases in the shale microstructure. Samples were indented parallel and perpendicular to the bedding plane to assess mechanical anisotropy. Chemical analysis of the grids with SEM-EDS (energy dispersive X-ray spectroscopy) was undertaken and the coupled chemo-mechanical data was used in a statistical clustering procedure (Gaussian mixture model) to reveal the mechanical properties of each phase. The results show that the overburden consists of a soft clay matrix with highly anisotropic elastic stiffness, and stiffer but effectively isotropic inclusions of quartz and feldspar; the significant anisotropy of the overburden has been previously observed on a much larger scale using microseismic data. Creep displacement is concentrated in the clay matrix, which is the key phase for fracture barrier and seal applications. The reservoir units are harder and have more isotropic mechanical responses, primarily due to their lower clay content. Despite varied compositions and microstructures, the major phases of these shales (clay/organic matrix, quartz/feldspar, dolomite, and calcite) have unique mechanical signatures, which will aid identification in future micromechanical characterizations and facilitate their use in upscaling schemes.

Citation

Charlton, T., Rouainia, M., Aplin, A., Fisher, Q., & Bowen, L. (2023). Nanoindentation of Horn River Basin Shales: The Micromechanical Contrast Between Overburden and Reservoir Formations. Journal of Geophysical Research. Solid Earth, 128(3), Article e2022JB025957. https://doi.org/10.1029/2022jb025957

Journal Article Type Article
Acceptance Date Mar 7, 2023
Online Publication Date Mar 17, 2023
Publication Date Mar 17, 2023
Deposit Date Mar 24, 2023
Publicly Available Date Mar 24, 2023
Journal Journal of Geophysical Research: Solid Earth
Print ISSN 2169-9313
Electronic ISSN 2169-9356
Publisher American Geophysical Union
Peer Reviewed Peer Reviewed
Volume 128
Issue 3
Article Number e2022JB025957
DOI https://doi.org/10.1029/2022jb025957
Public URL https://durham-repository.worktribe.com/output/1177642

Files

Published Journal Article (28.9 Mb)
PDF

Publisher Licence URL
http://creativecommons.org/licenses/by/4.0/

Copyright Statement
© 2023. The Authors.

This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.





You might also like



Downloadable Citations