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Hydro-Mechanical Properties of an Unsaturated Frictional Material

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8.3. SUMMARY 183<br />

Volumetric water content (%)<br />

50<br />

40<br />

30<br />

20<br />

10<br />

0<br />

Experimental drainage results (Initial void ratio 0.66) Experimental imbibition results (Initial void ratio 0.66) Drainage fit <strong>an</strong>d Imbitioin fit using<br />

0.1 1 10 100<br />

Suction (kPa)<br />

drainage results (Initial void ratio 0.89) Experimental imbibition results (Initial void ratio 0.89) Experimental<br />

proposed model<br />

Figure 8.10: Model validation results from main drainage <strong>an</strong>d main imbibition curve derived<br />

from steady state tests in the modified pressure plate apparatus (loose <strong>an</strong>d dense specimen)<br />

Figure 8.11: Model validation results from sc<strong>an</strong>ning imbibition curves derived from steady<br />

state tests in the modified pressure plate apparatus (loose specimen-left, dense specimen-right)<br />

in upper part <strong>of</strong> the soil-water characteristic curve. Modifications <strong>of</strong> the proposed model may<br />

be necessary, using the above described procedure.<br />

8.3 Summary<br />

Following a well understood statistical method (process modeling) new soil-water character-<br />

istic curve models were proposed for drainage <strong>an</strong>d imbibition process. The procedure was<br />

introduced in detail in Chapter 3 <strong>an</strong>d easily could be applied in this chapter for <strong>an</strong>y suction-<br />

volumetric water content (saturation, gravimetric water content) measurements derived from<br />

40<br />

30<br />

20<br />

10

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