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Hydro-Mechanical Properties of an Unsaturated Frictional Material

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9.4. COMPARISON OF SIMULATION RESULTS AND EXPERIMENTAL RESULTS 189<br />

Saturation (-)<br />

Saturation (-)<br />

1.0<br />

0.8<br />

0.6<br />

0.4<br />

0.2<br />

0.0<br />

Saturation (-)<br />

1.0<br />

0 200 400 600 800 1000 1200 1400 1600<br />

1.0<br />

Time (min)<br />

0.8<br />

0.8<br />

0.6<br />

0.4<br />

0.2<br />

0.0<br />

Results simulation<br />

Results experiment Depth 70 mm<br />

Saturation (-)<br />

Results simulation<br />

Results experiment Depth 260 mm<br />

0 200 400 600 800 1000 1200 1400 1600<br />

Time (min)<br />

1.0<br />

0.8<br />

0.6<br />

0.4<br />

0.2<br />

0.0<br />

0.6<br />

0.4<br />

0.2<br />

0.0<br />

Results simulation<br />

Results experiment Depth 160 mm<br />

0 200 400 600 800 1000 1200 1400 1600<br />

Time (min)<br />

Results simulation<br />

Results experiment Depth 360 mm<br />

0 200 400 600 800 1000 1200 1400 1600<br />

Time (min)<br />

Figure 9.3: Comparison <strong>of</strong> pore-water pressure measurements <strong>an</strong>d simulation including hysteresis<br />

model from Parker <strong>an</strong>d Lenhard (1987) - tr<strong>an</strong>sient state test<br />

time as well as pressure versus time measurements at several depths in the column.<br />

The simulation results including the hysteresis concept from Parker <strong>an</strong>d Lenhard that<br />

considers also entrapped air compared to the experimental results are given in Fig. 9.3<br />

<strong>an</strong>d 9.4. The comparison between the predicted <strong>an</strong>d measured saturation <strong>an</strong>d pressure<br />

is illustrated for four measurement depths. The results for the measurement point near<br />

the bottom <strong>of</strong> the column are not presented as saturated conditions are maintained there<br />

in both the experiment <strong>an</strong>d the numerical simulation. As the comparison <strong>of</strong> the results<br />

shows, the numerical simulation provides a good prediction <strong>of</strong> the experiment both in<br />

terms <strong>of</strong> saturation <strong>an</strong>d pressure. For the entire sequence <strong>of</strong> drainage <strong>an</strong>d imbibition<br />

events, the numerical simulation predicts the starting values <strong>of</strong> saturation <strong>an</strong>d pressure<br />

for each event (that strongly relate to the amount <strong>of</strong> trapped air) as well as to variation<br />

<strong>of</strong> pressure <strong>an</strong>d saturation in time. This c<strong>an</strong> also be illustrated by plotting the resulting<br />

soil-water characteristic curves from the experiment <strong>an</strong>d the simulation (see Fig 9.5).<br />

The simulation uses a rather simple scaling hysteresis concept <strong>an</strong>d therefore achieved a<br />

good prediction <strong>of</strong> the entire flow behavior in the tr<strong>an</strong>sient state test.

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