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Emergence of Strain Localization in Porous Rocks Characterized by Full-Field Measurement in Plane Strain Condition
Abstract The development of a new true triaxial cell which contains a device to observe the specimen under loading for full field measurement, has allowed studying the emergence of strain localisation in rock specimens. Two porous rocks have been investigated, a sandstone and a clayey rock. Both show similarities in the strain localization process, with an early diffuse strain localization pattern well before the stress peak that evolves progressively toward a reduced number of shear bands pattern. This final pattern, being usually reported in the literature, is associated to the stress peak and initiation of strain softening.
Emergence of Strain Localization in Porous Rocks Characterized by Full-Field Measurement in Plane Strain Condition
Abstract The development of a new true triaxial cell which contains a device to observe the specimen under loading for full field measurement, has allowed studying the emergence of strain localisation in rock specimens. Two porous rocks have been investigated, a sandstone and a clayey rock. Both show similarities in the strain localization process, with an early diffuse strain localization pattern well before the stress peak that evolves progressively toward a reduced number of shear bands pattern. This final pattern, being usually reported in the literature, is associated to the stress peak and initiation of strain softening.
Emergence of Strain Localization in Porous Rocks Characterized by Full-Field Measurement in Plane Strain Condition
Bésuelle, Pierre (author) / Lanatà, Patrizia (author)
2017-01-01
7 pages
Article/Chapter (Book)
Electronic Resource
English
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