2017
DOI: 10.1007/s11440-017-0588-3
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Monotonic and cyclic tests on kaolin: a database for the development, calibration and verification of constitutive models for cohesive soils with focus to cyclic loading

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Cited by 79 publications
(112 citation statements)
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“…In several test series performed by Wichtmann & Triantafyllidis [36], the stress amplitude q 0 , the displacement rate _ s, the initial mean pressure p 0 , the OCR, the initial stress ratio g 0 ¼ q 0 =p 0 and the cutting direction of the samples have been varied as described in [36,37]. Each of these tests has been simulated with the AVISA model and showed a good agreement with the experimental results (see the following sections).…”
Section: Simulations With Kaolin Claymentioning
confidence: 96%
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“…In several test series performed by Wichtmann & Triantafyllidis [36], the stress amplitude q 0 , the displacement rate _ s, the initial mean pressure p 0 , the OCR, the initial stress ratio g 0 ¼ q 0 =p 0 and the cutting direction of the samples have been varied as described in [36,37]. Each of these tests has been simulated with the AVISA model and showed a good agreement with the experimental results (see the following sections).…”
Section: Simulations With Kaolin Claymentioning
confidence: 96%
“…Furthermore, experiments show that under undrained triaxial conditions after a stress reversal first an increase in the mean pressure occurs in some clays [36] in contrast to sand where the reversal starts with the highest contractancy. This can also present a reason why most clays do not reach liquefaction p ¼ 0 kPa.…”
Section: Inclusion Of Inherent Anisotropy For Claysmentioning
confidence: 99%
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“…The earthquake load applied to the base of models is that of the 1995 Kobe earthquake, i.e., 0.83 g PGA (peak ground acceleration) (as recorded at KJMA station); then, this is scaled down to 0.4 g to investigate the effect of this parameter on the dynamic soil-tunnel behavior. There are various methods [35][36][37][38][39] used for the boundary conditions of models to ensure that these conditions prevent the return of earthquake waves, and we use the viscous spring boundary method to surround our soil models. The acceleration time history of the Kobe earthquake, and the power amplitude and Fourier amplitude spectra used in this study, are presented in Figure 9.…”
Section: Model Descriptionsmentioning
confidence: 99%