Rock dilation process is a complex behaviour that is influenced by material properties, stress conditions, and surface characteristics. In this study, we used twenty direct shear tests on four rock types under a constant normal load (CNL) condition to investigate rock dilation. Shear and normal displacements measured in these tests were used to understand shear induced dilation as a function of surface geometry. We focus our investigation on the ultimate dilation (ξult), which is defined as a constant value that the dilation (ξ) approaches with increasing shear displacement (δ). Results show that ξult is influenced by compressive strength, applied normal stress, and surface geometry.
%0 Generic
%1 zhou2018dilation
%A Zhou, Hongyuan
%A Zhao, Qi
%A Grasselli, Giovanni
%D 2018
%K conference grasselli zhao zhou
%T Dilation of rock joints based on quantified surface description
%U https://www.geoconvention.com/archives/2018/130_GC2018_Dilation_of_rock_joints_based_on_quantified_surface_description%20pdf.pdf
%X Rock dilation process is a complex behaviour that is influenced by material properties, stress conditions, and surface characteristics. In this study, we used twenty direct shear tests on four rock types under a constant normal load (CNL) condition to investigate rock dilation. Shear and normal displacements measured in these tests were used to understand shear induced dilation as a function of surface geometry. We focus our investigation on the ultimate dilation (ξult), which is defined as a constant value that the dilation (ξ) approaches with increasing shear displacement (δ). Results show that ξult is influenced by compressive strength, applied normal stress, and surface geometry.
@conference{zhou2018dilation,
abstract = {Rock dilation process is a complex behaviour that is influenced by material properties, stress conditions, and surface characteristics. In this study, we used twenty direct shear tests on four rock types under a constant normal load (CNL) condition to investigate rock dilation. Shear and normal displacements measured in these tests were used to understand shear induced dilation as a function of surface geometry. We focus our investigation on the ultimate dilation (ξult), which is defined as a constant value that the dilation (ξ) approaches with increasing shear displacement (δ). Results show that ξult is influenced by compressive strength, applied normal stress, and surface geometry.},
added-at = {2019-02-15T22:55:35.000+0100},
author = {Zhou, Hongyuan and Zhao, Qi and Grasselli, Giovanni},
biburl = {https://www.bibsonomy.org/bibtex/2f87d8583cab5bf4129c9f2ffcd139fae/geogroup_uoft},
eventdate = {May 7-11, 2018},
eventtitle = {Geoconvention},
interhash = {629ccf68df466c17a7ecb66b0941ced0},
intrahash = {f87d8583cab5bf4129c9f2ffcd139fae},
keywords = {conference grasselli zhao zhou},
month = may,
timestamp = {2019-02-15T22:55:35.000+0100},
title = {Dilation of rock joints based on quantified surface description},
url = {https://www.geoconvention.com/archives/2018/130_GC2018_Dilation_of_rock_joints_based_on_quantified_surface_description%20pdf.pdf},
venue = {Calgary, Canada},
year = 2018
}