Understanding wave propagation through soils is essential for site response analysis in earthquake engineering, interpretation of geophysical surveys and SASW (Spectral Analysis of Surface Waves), interpretation of laboratory bender element tests, etc. Analysis of wave propagation has largely been based on continuum descriptions and two dimensional analyses. This study presents recent developments in multiaxial testing that permit the combination of laboratory seismic testing with exploration of three-dimensional principal stress space. A Cubical Cell Apparatus with bender-extender piezoceramic elements fitted in all six faces are used so that wave propagation velocities of an analogue granular material can be determined. The results of a f...
The stiffness of soil is an important parameter that has implications on soil-structure interaction,...
In the manuscript "Investigate on the Compression-shear Coupled Stress Waves Propagating in Heteroge...
Small strain stiffness and anisotropic nature of two snads with different geological origin have bee...
Laboratory geophysical techniques using waves transmitted by piezoceramic elements have become popul...
In this study high quality experimental studies on an analogue soil in a cubical cell are compared w...
The (small-strain) elastic moduli of soil can be determined from stress wave velocity measurements. ...
The exact determination of seismic waves ’ propagation velocities has great importance in the geotec...
Recently developed equipment allows measurement of the shear modulus of soil in situ as a function o...
In recent years, an ever increasing interest in reducing seismic risk is developing. Innovative solu...
The objective of this thesis is to evaluate bender elements as a source and receiver of elastic wav...
The bender element (BE) test has been widely used for the dynamic characterization of soil specimens...
Due to increasing complexity of the infrastructure in urban living environment, the determination of...
The ultimate objective of the research conducted by the authors is to explore the feasibility of det...
Piezoceramic elements have been used for laboratory measurement of wave velocity in soil and rock sp...
The bender element test has shown to be a reliable tool to determine the shear wave velocity. This p...
The stiffness of soil is an important parameter that has implications on soil-structure interaction,...
In the manuscript "Investigate on the Compression-shear Coupled Stress Waves Propagating in Heteroge...
Small strain stiffness and anisotropic nature of two snads with different geological origin have bee...
Laboratory geophysical techniques using waves transmitted by piezoceramic elements have become popul...
In this study high quality experimental studies on an analogue soil in a cubical cell are compared w...
The (small-strain) elastic moduli of soil can be determined from stress wave velocity measurements. ...
The exact determination of seismic waves ’ propagation velocities has great importance in the geotec...
Recently developed equipment allows measurement of the shear modulus of soil in situ as a function o...
In recent years, an ever increasing interest in reducing seismic risk is developing. Innovative solu...
The objective of this thesis is to evaluate bender elements as a source and receiver of elastic wav...
The bender element (BE) test has been widely used for the dynamic characterization of soil specimens...
Due to increasing complexity of the infrastructure in urban living environment, the determination of...
The ultimate objective of the research conducted by the authors is to explore the feasibility of det...
Piezoceramic elements have been used for laboratory measurement of wave velocity in soil and rock sp...
The bender element test has shown to be a reliable tool to determine the shear wave velocity. This p...
The stiffness of soil is an important parameter that has implications on soil-structure interaction,...
In the manuscript "Investigate on the Compression-shear Coupled Stress Waves Propagating in Heteroge...
Small strain stiffness and anisotropic nature of two snads with different geological origin have bee...