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Hydro-Mechanical Properties of an Unsaturated Frictional Material

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192 CHAPTER 9. NUMERICAL SIMULATION OF COLUMN TEST BY FEM<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 />

Results simulation Results experiment Depth 70 mm<br />

Saturation (-)<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 Results experiment Depth 160 mm<br />

1.0 0 200 400 600 800 1000 1200 1400 1600<br />

1.0<br />

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

Time (min)<br />

Time (min)<br />

0.8<br />

0.8<br />

0.6<br />

0.4<br />

0.2<br />

0.0<br />

Results simulation Results experiment Depth 260 mm<br />

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

Time (min)<br />

Results simulation Results experiment Depth 360 mm<br />

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

Time (min)<br />

Figure 9.6: 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) - steady state test<br />

In general, it c<strong>an</strong> be stated that a good prediction <strong>of</strong> the flow process in the tr<strong>an</strong>sient state<br />

test has been obtained with a conceptually simple scaling approach for hysteresis.<br />

In a further investigation <strong>an</strong> additional soil-water characteristic curve is determined from<br />

steady state experiment on Hostun s<strong>an</strong>d specimens <strong>an</strong>d consequently used for a numerical<br />

simulation. This is a common procedure in applications involving unsaturated flow. However,<br />

the suction-water content curve determined with this approach demonstrates absence <strong>of</strong> air<br />

residual saturation in imbibition, in contrast to the tr<strong>an</strong>sient state test where a strong trapping<br />

effect is observed. The numerical simulation carried out here incorporates the Parker <strong>an</strong>d<br />

Lenhard (1987) hysteresis, however c<strong>an</strong>not predict correctly the flow process in the tr<strong>an</strong>sient<br />

state experiment due to the inappropriate input soil-water characteristic curve.

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