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Premium member Presentation Transcript Observations on Chaotic Failure Surface Trajectories in Bimrocks (Block-in-Matrix Rocks): Observations on Chaotic Failure Surface Trajectories in Bimrocks (Block-in-Matrix Rocks) Dr. Edmund Medley, PE, CEG GeoSyntec Consultants, Oakland, California emedley@geosyntec.com AEG Annual Meeting, Las Vegas, Nevada September, 2005Melanges and Similar Bimrocks: Melanges and Similar Bimrocks Bimrocks: block-in-matrix rocks mixtures of rocks composed of geotechnically significant blocks within a bonded matrix of finer texture Often severe spatial variability and mechanical/lithological heterogeneity: cost $$$$ e.g.: melanges, fault rocks , weathered rocks, etc.Slide3: Limestone Olistolith (Block) Embedded in an Irregularly Foliated Matrix of Shale, Siltstone and Sandstone Egnatia Motorway, Greece Photo by Prof. Gunter RiedmuellerSlide4: Slope debris Sandstone Marble / Shale Tectonic Melange Typical Melange Showing Diverse Elongate Blocks and Irregular Foliated Matrix (S-M-C-Cataclasites) (Photo C) Melange Fabric in a Slope Bolu Tunnel, Turkey Shears negotiate around blocks tortuously Not smooth rotational “failure surfaces” but chaotic trajectoriesSlide5: Melange: shears negotiate blocks Franciscan Complex melange: Franciscan Complex melangeBlock/matrix contacts weakest: Block/matrix contacts weakest Fault Rocksand Shear Rocks : Fault Rocks and Shear Rocks Riedmueller et al, 2001 Fault zones and Shear zones may have blocks millimeters to 100s of meters wide: Slide9: Mixture of weaker soil and strong blocks (decomposed granite at Hwy 50, California) DG: a weathered rock bimrockMotivation: analysis of slopes in bimrocks: Motivation: analysis of slopes in bimrocks Photo: ExponentWhat are the influences on slope stability in bimrocks?: What are the influences on slope stability in bimrocks? Block/matrix vol. proportion; matrix c,ϕ?? Medley & Sanz, 2004 i.e: really complex problem – how then should we analyze slope stability in bimrocks??One Approach: Perform simple analysis of increases in Factors of Safety for Slope Stability in a bimrock: One Approach: Perform simple analysis of increases in Factors of Safety for Slope Stability in a bimrockSimple analysis of increases in Factors of Safety for Slope Stability: Simple analysis of increases in Factors of Safety for Slope StabilityAbstract failure surfaces, perform slope stability analyses: Abstract failure surfaces, perform slope stability analysesBlocks increase slope stability: Blocks increase slope stability Q: How do blocks add to slope stability? A: Tortuosity of failure surfaces negotiating blocks (little to do with block strength)BUT: We cannot even characterize the actual block distribution in bimrocks, so we can never predict the actual trajectories of tortuous failure surfaces in slopes!(as now shown….): BUT: We cannot even characterize the actual block distribution in bimrocks, so we can never predict the actual trajectories of tortuous failure surfaces in slopes! (as now shown….)Review failed physical model melanges: Review failed physical model melanges 150 mm diameter Tx specimens (Lindquist, 1994) Lindquist, 1994; Medley, 2004Failure surfaces in sectioned TX Specimens: Failure surfaces in sectioned TX Specimens Lindquist, 1994; Medley, 2004 Measure lengths of failure surfaces at circumference of specimens: Measure lengths of failure surfaces at circumference of specimens Medley, 2004 trace of matrix-only failure surface actual failure surface Contact between block and failure surfaceProfiles from many specimens: Profiles from many specimens Medley, 2004 15 cm not “joint roughness”Calculate several parameters……: Calculate several parameters…… Medley, 2004 One ME measure of tortuosity Lengthening of tortuous failure surfaces: Lengthening of tortuous failure surfaces Lengthening apparently not much sensitive to block proportion nor block orientation Tortuosity (as ME measure “roughness”): Tortuosity (as ME measure “roughness”) Tortuosity ~ 5%-15% of characteristic dimension and more sensitive to block proportion than orientation??Block contacts along tortuous surfaces: Block contacts along tortuous surfaces Conservative to assume block/shear surface (%) contact is ~ volumetric proportion (%)Slope Analysis Cartoon: Slope Analysis Cartoon HSlope Analysis Cartoon continued: Slope Analysis Cartoon continued H c, γ, φ of bimrock (α Vol. Prop. Blocks) c, γ, φ of failure zone dependent on block/shear contact ratio (α Vol. Prop Blocks)Conclusions: Conclusions Increases in tortuosity are most influenced by block volumetric proportion Rather than analyzing individual tortuous failure surfaces in bimrocks, analyze trial failure zones with a width 5% to 15% of slope height or other characteristic dimension scaling the problem at hand Use mechanical properties based on estimates of Volumetric Block Proportion (taking into account uncertainty) Beware consistent adverse block orientations that result in adverse shear fabric Determinaistic Investigation of the Mechanical Effect of Tortuosity at Slope Scale: Determinaistic Investigation of the Mechanical Effect of Tortuosity at Slope ScalePrecedent: slope stability of Hong Kong Boulder Colluvium: Precedent: slope stability of Hong Kong Boulder Colluvium Hong Kong GEO TN 4/92Trial tortuous failure surfaces with blocks oriented out-of-slope: Trial tortuous failure surfaces with blocks oriented out-of-slope After Irfan & Tang, 1993 Inclined blocks, all same size, regular array, spacing, etc. Critical failure surface without blocks and model failure surface with blocksTry Improving Hong Kong Approach Step 1: matrix critical failure surface: Try Improving Hong Kong Approach Step 1: matrix critical failure surface Φ = 25º c = 10 kPa FS ~ 1.26 Using Slope/WStep 2: Create random arrays of blocks: Step 2: Create random arrays of blocks 50% 25% 13%Step 3: Create Model Tortuous Failure Surfaces: Step 3: Create Model Tortuous Failure Surfaces 5mStep 4: Perform slope stability analyses on the model tortuous failure surfaces: Step 4: Perform slope stability analyses on the model tortuous failure surfaces 50% block proportion You do not have the permission to view this presentation. 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AEG2005 Rina Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 74 Category: Education License: All Rights Reserved Like it (0) Dislike it (0) Added: January 23, 2008 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Observations on Chaotic Failure Surface Trajectories in Bimrocks (Block-in-Matrix Rocks): Observations on Chaotic Failure Surface Trajectories in Bimrocks (Block-in-Matrix Rocks) Dr. Edmund Medley, PE, CEG GeoSyntec Consultants, Oakland, California emedley@geosyntec.com AEG Annual Meeting, Las Vegas, Nevada September, 2005Melanges and Similar Bimrocks: Melanges and Similar Bimrocks Bimrocks: block-in-matrix rocks mixtures of rocks composed of geotechnically significant blocks within a bonded matrix of finer texture Often severe spatial variability and mechanical/lithological heterogeneity: cost $$$$ e.g.: melanges, fault rocks , weathered rocks, etc.Slide3: Limestone Olistolith (Block) Embedded in an Irregularly Foliated Matrix of Shale, Siltstone and Sandstone Egnatia Motorway, Greece Photo by Prof. Gunter RiedmuellerSlide4: Slope debris Sandstone Marble / Shale Tectonic Melange Typical Melange Showing Diverse Elongate Blocks and Irregular Foliated Matrix (S-M-C-Cataclasites) (Photo C) Melange Fabric in a Slope Bolu Tunnel, Turkey Shears negotiate around blocks tortuously Not smooth rotational “failure surfaces” but chaotic trajectoriesSlide5: Melange: shears negotiate blocks Franciscan Complex melange: Franciscan Complex melangeBlock/matrix contacts weakest: Block/matrix contacts weakest Fault Rocksand Shear Rocks : Fault Rocks and Shear Rocks Riedmueller et al, 2001 Fault zones and Shear zones may have blocks millimeters to 100s of meters wide: Slide9: Mixture of weaker soil and strong blocks (decomposed granite at Hwy 50, California) DG: a weathered rock bimrockMotivation: analysis of slopes in bimrocks: Motivation: analysis of slopes in bimrocks Photo: ExponentWhat are the influences on slope stability in bimrocks?: What are the influences on slope stability in bimrocks? Block/matrix vol. proportion; matrix c,ϕ?? Medley & Sanz, 2004 i.e: really complex problem – how then should we analyze slope stability in bimrocks??One Approach: Perform simple analysis of increases in Factors of Safety for Slope Stability in a bimrock: One Approach: Perform simple analysis of increases in Factors of Safety for Slope Stability in a bimrockSimple analysis of increases in Factors of Safety for Slope Stability: Simple analysis of increases in Factors of Safety for Slope StabilityAbstract failure surfaces, perform slope stability analyses: Abstract failure surfaces, perform slope stability analysesBlocks increase slope stability: Blocks increase slope stability Q: How do blocks add to slope stability? A: Tortuosity of failure surfaces negotiating blocks (little to do with block strength)BUT: We cannot even characterize the actual block distribution in bimrocks, so we can never predict the actual trajectories of tortuous failure surfaces in slopes!(as now shown….): BUT: We cannot even characterize the actual block distribution in bimrocks, so we can never predict the actual trajectories of tortuous failure surfaces in slopes! (as now shown….)Review failed physical model melanges: Review failed physical model melanges 150 mm diameter Tx specimens (Lindquist, 1994) Lindquist, 1994; Medley, 2004Failure surfaces in sectioned TX Specimens: Failure surfaces in sectioned TX Specimens Lindquist, 1994; Medley, 2004 Measure lengths of failure surfaces at circumference of specimens: Measure lengths of failure surfaces at circumference of specimens Medley, 2004 trace of matrix-only failure surface actual failure surface Contact between block and failure surfaceProfiles from many specimens: Profiles from many specimens Medley, 2004 15 cm not “joint roughness”Calculate several parameters……: Calculate several parameters…… Medley, 2004 One ME measure of tortuosity Lengthening of tortuous failure surfaces: Lengthening of tortuous failure surfaces Lengthening apparently not much sensitive to block proportion nor block orientation Tortuosity (as ME measure “roughness”): Tortuosity (as ME measure “roughness”) Tortuosity ~ 5%-15% of characteristic dimension and more sensitive to block proportion than orientation??Block contacts along tortuous surfaces: Block contacts along tortuous surfaces Conservative to assume block/shear surface (%) contact is ~ volumetric proportion (%)Slope Analysis Cartoon: Slope Analysis Cartoon HSlope Analysis Cartoon continued: Slope Analysis Cartoon continued H c, γ, φ of bimrock (α Vol. Prop. Blocks) c, γ, φ of failure zone dependent on block/shear contact ratio (α Vol. Prop Blocks)Conclusions: Conclusions Increases in tortuosity are most influenced by block volumetric proportion Rather than analyzing individual tortuous failure surfaces in bimrocks, analyze trial failure zones with a width 5% to 15% of slope height or other characteristic dimension scaling the problem at hand Use mechanical properties based on estimates of Volumetric Block Proportion (taking into account uncertainty) Beware consistent adverse block orientations that result in adverse shear fabric Determinaistic Investigation of the Mechanical Effect of Tortuosity at Slope Scale: Determinaistic Investigation of the Mechanical Effect of Tortuosity at Slope ScalePrecedent: slope stability of Hong Kong Boulder Colluvium: Precedent: slope stability of Hong Kong Boulder Colluvium Hong Kong GEO TN 4/92Trial tortuous failure surfaces with blocks oriented out-of-slope: Trial tortuous failure surfaces with blocks oriented out-of-slope After Irfan & Tang, 1993 Inclined blocks, all same size, regular array, spacing, etc. Critical failure surface without blocks and model failure surface with blocksTry Improving Hong Kong Approach Step 1: matrix critical failure surface: Try Improving Hong Kong Approach Step 1: matrix critical failure surface Φ = 25º c = 10 kPa FS ~ 1.26 Using Slope/WStep 2: Create random arrays of blocks: Step 2: Create random arrays of blocks 50% 25% 13%Step 3: Create Model Tortuous Failure Surfaces: Step 3: Create Model Tortuous Failure Surfaces 5mStep 4: Perform slope stability analyses on the model tortuous failure surfaces: Step 4: Perform slope stability analyses on the model tortuous failure surfaces 50% block proportion