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Hydro-Mechanical Properties of an Unsaturated Frictional Material

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62 CHAPTER 2. STATE OF THE ART<br />

Vertical strain (-)<br />

0.000<br />

0.002<br />

0.004<br />

0.006<br />

0.008<br />

0.010<br />

Logarithm vertical strain (-)<br />

-4<br />

-5<br />

-6<br />

-7<br />

-8<br />

Experimental results<br />

loading path<br />

Experimental results<br />

unloading path<br />

0.1 1 10 100 1000<br />

Vertical net stress (kPa)<br />

Regression loading path<br />

Regression unloading path<br />

-4 -3 -2 -1 0 1<br />

Logarithm stress ratio (-)<br />

Figure 2.29: One dimensional compression <strong>an</strong>d rebound results for Hostun s<strong>an</strong>d <strong>an</strong>d appropriate<br />

regression functions<br />

well as matric suction (Alosnso et al. 1987, Delage 2002, Rahardjo & Fredlund 2003). When<br />

dealing with experiments on unsaturated soils special test features are required, e.g. ceramic<br />

disk for separation <strong>of</strong> air phase <strong>an</strong>d water phase, equipment for application <strong>of</strong> pore-air pressure<br />

as well as pore-water pressure for application <strong>an</strong>d control <strong>of</strong> matric suction. Among others,<br />

oedometer cells for investigation <strong>of</strong> unsaturated soils were developed by Kassiff & Shalom<br />

(1971), Escario & Saez (1973), Romero (1999), Rampino et al. (1999). Most <strong>of</strong> these cells<br />

were used to investigate the volume ch<strong>an</strong>ge behavior <strong>of</strong> unsaturated silts or clays. Several<br />

authors (Cui & Delage 1996, Rahardjo & Fredlund 2003) have been demonstrated that the<br />

suction has a signific<strong>an</strong>t influence on the mech<strong>an</strong>ical unsaturated soil behavior <strong>of</strong> cohesive<br />

soils as volume ch<strong>an</strong>ge <strong>an</strong>d stiffness. For inst<strong>an</strong>ce Cui & Delage (1996), Rampino et al. (2000)

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