2013
DOI: 10.1007/s11440-013-0208-9
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Localized deformation in intensely fissured clays studied by 2D digital image correlation

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Cited by 36 publications
(20 citation statements)
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“…The natural micro-to meso-structure of natural fissured and unfissured clays has been dealt with as an internal state variable adding to void ratio in controlling the clay response (e.g., Leroueil 1988;Burland 1990;Leroueil and Vaughan 1990;Nagaraj et al 1998;Cotecchia and Chandler 2000;Vitone and Cotecchia 2011;Vitone et al 2013a;b). It has been found that, if unfissured, the natural structure (i.e., the combination of fabric and bonding) makes the clay enter the structure permitted space as recalled by Leroueil and Vaughan (1990), so that, at the same consolidation pressure, the natural unfissured clay can be stable at higher water content than the same clay when reconstituted in the laboratory (Fig.…”
Section: Behavioural Trends In Compression Of the Treated Claysmentioning
confidence: 99%
“…The natural micro-to meso-structure of natural fissured and unfissured clays has been dealt with as an internal state variable adding to void ratio in controlling the clay response (e.g., Leroueil 1988;Burland 1990;Leroueil and Vaughan 1990;Nagaraj et al 1998;Cotecchia and Chandler 2000;Vitone and Cotecchia 2011;Vitone et al 2013a;b). It has been found that, if unfissured, the natural structure (i.e., the combination of fabric and bonding) makes the clay enter the structure permitted space as recalled by Leroueil and Vaughan (1990), so that, at the same consolidation pressure, the natural unfissured clay can be stable at higher water content than the same clay when reconstituted in the laboratory (Fig.…”
Section: Behavioural Trends In Compression Of the Treated Claysmentioning
confidence: 99%
“…Vitone et al (2013) observed that pre-existing fissures play an important role in the strain localisation while shearing samples of scaly clay in a plane strain apparatus. Vitone & Cotecchia (2011) introduced a fissuring characterisation chart, in order to classify and evaluate the fissuring identity (F-ID) of the fissured clays with respect to those features that affect their mechanical behaviour, such as intensity (I) and orientation (F) of fissures.…”
Section: Introductionmentioning
confidence: 98%
“…In particular, the fissures are organized into a peculiar intense network that splits the clay into millimetre lens-shaped elements (known as scales -which is the origin of their being referred to as scaly clays in the literature). This paper reports a further step of a long lasting experimental research, which entails the experimental investigation of the geomechanical properties of several differently fissured clays, aiming at their modelling as a single class of geomaterials [8][9][10][11][12][13]. During previous laboratory studies, the SCM scaly clay [9][10][11] were tested in plane strain compression tests at zero confining pressure in the plane of deformation.…”
Section: Introductionmentioning
confidence: 99%
“…This paper reports a further step of a long lasting experimental research, which entails the experimental investigation of the geomechanical properties of several differently fissured clays, aiming at their modelling as a single class of geomaterials [8][9][10][11][12][13]. During previous laboratory studies, the SCM scaly clay [9][10][11] were tested in plane strain compression tests at zero confining pressure in the plane of deformation. The experiments have shown that, when the fissure orientation in the specimen is either random or horizontal, i.e., normal to the direction of the maximum principal stress, the development of localized deformation throughout plane strain compression tests, is not dictated by pre-existing fissures.…”
Section: Introductionmentioning
confidence: 99%