2014
DOI: 10.1680/geores.14.00003
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Advanced laboratory testing in research and practice: the 2nd Bishop Lecture

Abstract: NotationCc gradient in oedometer e-log z σ ¢ relationship Cu coefficient of uniformity = d90/d10 D diameter; Dchamber and Dpile are the calibration chamber and pile diameters, respectively d10, d50, d90 particle diameters at 10%, 50% and 90% points, respectively, on particle-

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Cited by 22 publications
(10 citation statements)
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“…1. Elastic -Cyclic stress remains within the small Y 1 region, as described for example by Jardine (2014). This region behaviour could not be resolved unambiguously within the present experiments.…”
Section: Clay Response and Shakedown Behaviourcontrasting
confidence: 61%
See 1 more Smart Citation
“…1. Elastic -Cyclic stress remains within the small Y 1 region, as described for example by Jardine (2014). This region behaviour could not be resolved unambiguously within the present experiments.…”
Section: Clay Response and Shakedown Behaviourcontrasting
confidence: 61%
“…2. Elastic shakedown -Higher levels of cyclic loading lead to the specimen undergoing Y 1 yielding first, but remaining within the Y 2 kinematic yield surface reported by Jardine (2014) and exhibiting slight plastic deformation such as that seen up to the CSR ≥ 0.03 limit. 3.…”
Section: Clay Response and Shakedown Behaviourmentioning
confidence: 77%
“…Following earlier geophysical and triaxial stiffness studies of the Gault and Oxford clays by Butcher & Lord (1993), Butcher & Powell (1995), Hird & Pierpoint (1997), Pennington et al (1997) and Ng et al (1998), the new work allows direct comparisons to be made between the stiffness properties of the four Jurassic-toEocene clays, which are reported within the framework set out below. Arup (2007) (2) Pierpoint (1996) 100 mm UU (1) Framework for test interpretation Jardine (1992Jardine ( , 2013 emphasises that behaviour can only be considered elastic within a very small area of the permissible stress space that is limited by a kinematic hardening (Y 1 ) true yield surface. The latter is dragged with the current effective stress point, growing and shrinking with p′ and changing in shape with proximity to the outer Y 3 surface, which corresponds to the yield surface recognised in classical critical state soil mechanics.…”
Section: Discussionmentioning
confidence: 99%
“…Axial capacity predictions are crucial to many applications, especially those involving offshore tension leg, tripod or jacket structures (e.g. Overy, 2007;Merritt et al, 2012;Jardine, 2013). Foundation stiffness can also be important to both structural fatigue life and wind turbine operations.…”
Section: Introductionmentioning
confidence: 99%