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Hydro-Mechanical Properties of an Unsaturated Frictional Material

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6.4. VOLUMETRIC BEHAVIOR 129<br />

Depth (cm)<br />

0<br />

10<br />

20<br />

30<br />

40<br />

50<br />

6<br />

4<br />

state 30 min 120 min 180 min Initial<br />

min 300 min 360 min 420 min 240<br />

Pore - water pressure (kPa)<br />

2<br />

0<br />

-2<br />

-4<br />

-6<br />

0<br />

10<br />

20<br />

30<br />

40<br />

50<br />

50<br />

Volumetric water content (%)<br />

40<br />

30<br />

20<br />

10<br />

1st drainage<br />

Loose specimen<br />

Initial void ratio = 0.89<br />

Figure 6.14: Pore-water pressure <strong>an</strong>d volumetric water content pr<strong>of</strong>iles for 1 st drainage process<br />

(loose specimen)<br />

6.4 Volumetric Behavior<br />

For determination <strong>of</strong> the mech<strong>an</strong>ical behavior <strong>of</strong> unsaturated Hostun s<strong>an</strong>d stress-strain re-<br />

lationships derived from one dimensional compression rebound tests <strong>an</strong>d collapse tests were<br />

investigated. The results are give in the section below.<br />

6.4.1 Stress-Strain Relationship<br />

Experimental results from one dimensional compression <strong>an</strong>d rebound tests are presented in<br />

Fig. 6.15 for loose specimens <strong>an</strong>d in Fig. 6.16 for dense specimens. Volumetric strain versus<br />

applied vertical net stress as well as void ratio versus applied vertical net stress results are<br />

given in the diagrams. For s<strong>an</strong>ds the following typical observations in the stress-strain curve<br />

are made (Lambe & Whitm<strong>an</strong> 1969):<br />

- Observation during loading path:<br />

As c<strong>an</strong> be seen in the stress strain diagrams in Figs. 6.15 <strong>an</strong>d 6.16 the s<strong>an</strong>d becomes<br />

stiffer with increasing vertical stress. As the stress increases within the soil sample<br />

loose arrays collapse followed by denser arrays. Each movement results in a stiffer<br />

packed specimen <strong>an</strong>d thus decreasing void ratio. With increasing stress the stress-strain<br />

curvature becomes concave to the strain axis resulting from fracturing <strong>of</strong> individual s<strong>an</strong>d<br />

particles. Whereas sliding between particles occurs at all stress levels, fracturing <strong>an</strong>d<br />

crushing becomes increasingly import<strong>an</strong>t with increase in vertical stress.<br />

0

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