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Continuous Evaluation of Shear Wave Velocity from Bender Elements during Monotonic Triaxial Loading
Ahmed Khalil1, Zahid Khan1, Mousa Attom1
1Department of Civil Engineering, American University of Sharjah, Sharjah P.O. Box 26666, United Arab Emirates.
Low-strain shear wave velocity (Vs) in sand remains stable during large deformations, unaffected by axial strain. Micro-mechanical models confirm mean effective stress and inter-particle stiffness control this behavior.
Area of Science:
- Geotechnical Engineering
- Soil Mechanics
- Wave Propagation in Soils
Background:
- Low-strain shear wave velocity (Vs) is a key soil property.
- Experimental data on Vs during large strain deformations is limited.
- The insensitivity of Vs to large strains is not fully understood.
Purpose of the Study:
- To continuously measure low-strain Vs during monotonic shearing of sand specimens.
- To investigate the relationship between Vs and large strain deformations.
- To analyze the underlying micro-mechanical reasons for Vs stability.
Main Methods:
- Continuous measurement of low-strain Vs using bender elements (BE).
- Monotonic shearing of sand specimens in a triaxial device.
- Analysis using a micro-mechanical model based on contact theory.
Main Results:
- Low-strain Vs measurements were unaffected by increasing axial strains.
- The micro-mechanical model accurately predicted Vs values.
- Mean effective stress and inter-particle stiffness were identified as key controlling factors for low-strain stiffness.
Conclusions:
- Confirms that low-strain shear wave velocity is independent of large axial strains in sand.
- Highlights the importance of mean effective stress and inter-particle stiffness in controlling soil stiffness.
- Provides a validated micro-mechanical framework for understanding soil behavior under varying strain conditions.
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