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Hydro-Mechanical Properties of an Unsaturated Frictional Material

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CHAPTER 7. ANALYSIS AND INTERPRETATION OF THE EXPERIMENTAL<br />

RESULTS<br />

Unsat. hydr. conductivity (10 -4m/s)Initial<br />

3.0<br />

2.5<br />

2.0<br />

1.5<br />

void ratio e = 0.89<br />

1.0 large scale tests: Results<br />

0.5<br />

0.0<br />

0.1 1<br />

Results small scale tests: Fredlund et al. (1994) Drainage Imbibition<br />

10<br />

drying - layer (310 mm) 2nd drying - layer (310 mm) Inst<strong>an</strong>t<strong>an</strong>eous Pr<strong>of</strong>il Method 1st<br />

Matric suction (kPa)<br />

large scale tests: Fredlund et al. (1994) Initial, 1st <strong>an</strong>d 2nd drainage Results<br />

<strong>an</strong>d 2nd wetting Flow rate » 30 ml/min Flow rate » 100 ml/min 1st<br />

Figure 7.15: Comparison <strong>of</strong> unsaturated hydraulic conductivity curves resulting from modified<br />

pressure plate apparatus (steady state test) <strong>an</strong>d s<strong>an</strong>d column test I (loose specimen, tr<strong>an</strong>sient<br />

state test)<br />

Unsat. hydr. conductivity (10 -4m/s)<br />

3.0<br />

2.5<br />

2.0<br />

1.5<br />

1.0<br />

0.5<br />

0.0<br />

void ratio e = 0.66 Initial<br />

small scale tests: Fredlund et al. (1994) Results<br />

0.1 1<br />

Drainage Imbibition Flow rate » 100 ml/min<br />

10 drying - layer (310 mm) Results large scale tests: Inst<strong>an</strong>t<strong>an</strong>eous Pr<strong>of</strong>il Method 2nd<br />

Matric suction [kPa]<br />

large scale tests: Fredlund et al. (1994) Initial, 1st <strong>an</strong>d 2nd drainage Results<br />

<strong>an</strong>d 2nd imbibition Flow rate » 30 ml/min 1st<br />

1st drying - layer (310 mm)<br />

Figure 7.16: Comparison <strong>of</strong> unsaturated hydraulic conductivity curves resulting from modified<br />

pressure plate apparatus (steady state test) <strong>an</strong>d s<strong>an</strong>d column test I (dense specimen, tr<strong>an</strong>sient<br />

state test)<br />

first increases for the dense specimen. The smaller voids more easily absorb the water. Again<br />

the unsaturated hydraulic conductivity function for the dense specimen is located above the

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