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Hydro-Mechanical Properties of an Unsaturated Frictional Material

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11.5. FUTURE WORK 211<br />

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

the 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 soil-water characteristic 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 was observed. The numerical simulation carried out here incorporates the Parker <strong>an</strong>d<br />

Lenhard hysteresis. However, the simulation c<strong>an</strong>not correctly predict the flow process in the<br />

tr<strong>an</strong>sient state experiment due to the inappropriate input suction-water content curve.<br />

It is demonstrated that the implementation <strong>of</strong> a simple scaling approach for hysteresis<br />

c<strong>an</strong> provide a good prediction <strong>of</strong> hysteretic unsaturated flow including phase trapping effects.<br />

However, this needs to be combined with reliable information <strong>of</strong> the input soil-water charac-<br />

teristic curve parameters that is commonly measured in the laboratory. It is shown that this<br />

is possible by using direct saturation <strong>an</strong>d pressure measurements from the s<strong>an</strong>d column test I.<br />

The investigation showed that a single pair <strong>of</strong> TDR <strong>an</strong>d tensiometer sensors in combination<br />

with the implemented scaling concept for hysteresis provides good prediction <strong>of</strong> the flow in<br />

the entire 0.54 m high porous medium column, for all drainage <strong>an</strong>d imbibition events. If TDR<br />

<strong>an</strong>d tensiometer data were not available, the traditional steady state method would be used<br />

for the determination <strong>of</strong> the suction water content relationship. Although the specimens used<br />

in the steady state outflow/ inflow experiments correspond to the same spatial scale as the<br />

TDR-T pairs, they provide different information on the amount <strong>of</strong> air trapping <strong>an</strong>d conse-<br />

quently a misleading prediction <strong>of</strong> flow in the tr<strong>an</strong>sient state test. This observation suggests<br />

that the amount <strong>of</strong> phase trapping strongly depends on the methodology used <strong>an</strong>d the time<br />

scales linked to it. When predicting hysteretic flow by me<strong>an</strong>s <strong>of</strong> numerical simulations, it is<br />

therefore necessary to use hysteretic suction-water content curves that are determined under<br />

conditions (i.e. fast or slow imbibition) similar to those <strong>of</strong> the application they are purposed<br />

for.<br />

11.5 Future Work<br />

Due to the reason that the majority <strong>of</strong> civil engineering problems are related to unsaturated<br />

soils, there is a strong motivation to underst<strong>an</strong>d their hydro-mech<strong>an</strong>cial behavior <strong>an</strong>d the im-<br />

pact <strong>of</strong> suction vice versa water content on the stress-strain, shear strength <strong>an</strong>d flow behavior.<br />

To support the investigations carried out in the present study <strong>an</strong>d to complete the present<br />

study following tests are proposed to carry out:<br />

- Perform<strong>an</strong>ce <strong>of</strong> triaxial tests for investigation <strong>of</strong> the influence <strong>of</strong> suction on the shear<br />

strength.<br />

- Perform<strong>an</strong>ce <strong>of</strong> biaxial tests for investigation <strong>of</strong> the influence <strong>of</strong> suction on shear<br />

strength.

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