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Instability Conditions of a Silty Sand under Monotonic Loads in Simple Shear Tests
In order to improve the understanding on static liquefaction phenomenon, this paper presents an insight into the instability mechanism of a silty sand originating from the Sakarya region (Turkey). Monotonic undrained simple shear tests were performed in either strain-controlled or stress-controlled modes. The interpretation of the experimental results allowed us to draw three interesting conclusions on instability conditions: (1) Hill’s stability postulate can be conveniently used to identify the onset of instability for strain-controlled tests, whereas in stress-controlled conditions, an alternative new parameter (modified apparent viscosity) was introduced. Depending on the strain rate, allows to identify stability conditions more clearly than second-order work; (2) the value of the pore pressure ratio at the onset of instability (), ranging between 0.30 and 0.50, is linearly linked to the state parameter ; and (3) at the onset of instability, the dependence of both the major and minor principal stress directions ( and ) and Lode’s angle () on was also observed. These findings are expected to be of some help for a more consistent approach to the constitutive modeling of the static instability mechanism.
Instability Conditions of a Silty Sand under Monotonic Loads in Simple Shear Tests
In order to improve the understanding on static liquefaction phenomenon, this paper presents an insight into the instability mechanism of a silty sand originating from the Sakarya region (Turkey). Monotonic undrained simple shear tests were performed in either strain-controlled or stress-controlled modes. The interpretation of the experimental results allowed us to draw three interesting conclusions on instability conditions: (1) Hill’s stability postulate can be conveniently used to identify the onset of instability for strain-controlled tests, whereas in stress-controlled conditions, an alternative new parameter (modified apparent viscosity) was introduced. Depending on the strain rate, allows to identify stability conditions more clearly than second-order work; (2) the value of the pore pressure ratio at the onset of instability (), ranging between 0.30 and 0.50, is linearly linked to the state parameter ; and (3) at the onset of instability, the dependence of both the major and minor principal stress directions ( and ) and Lode’s angle () on was also observed. These findings are expected to be of some help for a more consistent approach to the constitutive modeling of the static instability mechanism.
Instability Conditions of a Silty Sand under Monotonic Loads in Simple Shear Tests
J. Geotech. Geoenviron. Eng.
Mele, Lucia (author) / Kocaman, Kadir (author) / Özocak, Aşkın (author) / Flora, Alessandro (author)
2024-11-01
Article (Journal)
Electronic Resource
English
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