Abstract
The shear strength of bedding planes was measured from direct shear testing of natural and artificialsurfaces. All testing was conducted at natural moisture content with very slow shear strain to permitpore pressure dissipation. All stresses were dilation corrected to estimate the basic friction angle ofbedding and artificial surfaces. The mineralogy of bedding surfaces presents very good relationshipwith dilation corrected friction angles, as derived from laboratory testing. In fresh and slightlyweathered shales, bedding planes present pre-shearing history that causes low dilation angles.Within moderately and highly weathered shales, bedding planes are coated by decomposed rock
Original language | English |
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Qualification | Doctor of Philosophy |
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Award date | 23 Aug 2023 |
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Publication status | Unpublished - 2022 |