Dynamic testing of free field response in stratified granular deposits
Introduction
The shearing stress–strain behaviour of soils is key to understanding how sites and buildings respond to earthquakes. The effect of local soil conditions on the observed magnitude and patterns of seismic damage to buildings has been studied extensively in the last four decades [2], [3], [4], [5], [6], [7]. The shearing behaviour of soils, notably the shear modulus and damping ratio were found to be the properties that govern dynamic soil-structure interaction at all strain levels. The measurement of these properties has been the central objective in numerous laboratory and field studies [8], [9], [10], [11], [12], [13]. Among the various tools employed in the dynamic analysis of granular media, shaking table testing is an important one, due to its capability of reproducing a wide set of real and artificial seismic inputs with relevance for the free field response. A large number of shaking table studies [14], [15], [16], [17], [18] employ flexible container boxes (‘shear stacks’) designed to replicate the free field response of a soil in plane strain conditions. Their role is to shear the soil via vertically propagating shear waves produced by the accelerating shaking table. In a large scale shear stack a large volume of soil can be tested, therefore the results may be more representative of the prototype field conditions. The boundary effects in a large shear stack are smaller than in table-top shear devices and the volume of soil situated in the central part of the container reproduces better the free field conditions for a given wavelength. It is also known that the design of a shear stack can be tuned to operate over wide strain ranges with granular materials of different stiffness value [19]. This, in particular, makes the shear stack useful for studying the large-strain dynamic moduli under seismic excitation. Several laminar shear box designs have been reported for both uniaxial and biaxial loading [20], [21], [22], [23], [24], [25], [26]. While there is a large body of literature on tests on homogeneous soils, experimental data on stratified deposits is scarce. This paper presents an experimental programme of dynamic testing carried out on three deposits of dry granular material at Bristol University. An homogeneous deposit of sand and two bi-layered deposits of sand and rubber granules were tested in a uniaxial shear stack. The shear stack was assembled rigidly on the platform of a shaking table. Pulse tests and random white noise tests were carried out to measure the natural frequency of the individual layers. The fundamental periods of the stratified deposits were evaluated and compared to an analytical solution from the literature [1]. The influences brought by the particulate material characteristics and the dynamic input parameters on the free field response were analysed. Aspects such as container-deposit coupling and deposit mode shapes were interpreted in relation to the deposit stiffness and the applied dynamic inputs.
Section snippets
Shear stack
The shear stack employed in this study was a medium-sized uniaxial laminar container of length 1.2 m, width 0.5 m and height 0.8 m. The shear stack was built at Bristol University in 1993 [20] and has been since subjected to several design improvements directed in particular towards lowering its stiffness [27]. Previous investigations of the shear stack have shown that its fundamental frequency when empty is about 6 Hz. The stack is active in one direction only, with its eight aluminium rings
Modal testing
Modal testing techniques that measure the shear wave velocity of the materials in ‘as-pluviated’ state in the shear stack can reveal a more realistic value of stiffness than the laboratory techniques employing small material samples confined in simplified boundary conditions (e.g. resonant column tests). Modal techniques employed ‘in-situ’ are believed to be less disturbing for the granular texture, therefore having more chance of capturing the small strain stiffness of the deposits.
In pulse
Concluding remarks
Shaking table test results of granular materials sheared in plane strain conditions in a large uniaxial shear stack were reported. The shear stress–strain behaviour of three configurations (one witness mono-layered deposit and two bi-layered deposits) was analysed under a set of seismic inputs with different frequency content. Two modal testing techniques (i.e. pulse testing and random white noise testing) were successful in measuring the fundamental periods of the individual layers. The
Acknowledgements
The financial support from ReLUIS (Rete di Laboratori Universitari Ingegneria Seismica) for conducting this research is gratefully acknowledged. The authors would like to thank Eleonora Iannacce and Domenico Lombardi for their contribution to the experimental work and to Professor David Muir Wood for his advice on granular material testing.
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